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GM 44377 REPORT ON GROUND GEOPHYSICAL SURVEYS AND REVERSE CIRCULATION DRILLING, JOUTEL PROJECT
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GM 44377REPORT ON GROUND GEOPHYSICAL SURVEYS AND REVERSE CIRCULATION DRILLING, JOUTEL PROJECT
REPORT
ON
GROUND GEOPHYSICAL SURVEYS
AND
REVERSE CIRCULATION DRILLING
ON THE
JOUTEL PROJECT
NORTHWESTERN QUEBEC
for
HOMESTAKE MINERAL DEVELOPMENT COMPANY
p~~~ }}:: tt ~. '~ t~ ~i p7 . 1YlfYi:~,sii Û Cu. ~ ~,ti'tâil ~So Sri2 dos f ' ~v~'i.7:13. ~ Service de la Géoinformation
,, Date: 2 7 en loR7
No Gm.: 44377 Toronto, Ontario J.P. Rollinson, B.Sc.
August, 1986
J. Roth, M.A.
MPH Consulting Limited
SUMMARY
An integrated exploration program of ground geophysical surveys and re-
verse circulation drilling was completed by MPH Consulting Limited during
the months of June, July and August 1986, on behalf of Homestake Mineral
Development Company on the latter's Joutel project in northwestern
Quebec.
The Joutel project encompasses portions of Joutel, Montgolfier and
Aloigny Township within the northern sector of the Abitibi Greenstone
Belt. Limited prior exploration indicated the presence of extensive iron
formations accompanied by regional, probably graphitic conductors hosted
by mafic volcanics with intercalated felsic volcanics and sediments.
Geologic trends vary from east-west in Joutel Township to northwest-
southeast in Aloigny Township.
The exploration program was carried out with the objective of defining
and evaluating geophysical targets and geologic environments judged
favourable for gold and/or polymetallic sulphide deposits.
MaxMin HLEM surveys, the principal geophysical technique employed, were
carried out over four portions of the property, designated grids A, AA, C
and D. The surveys disclosed six probable to definite bedrock conductors
(zones H, M, N, LL, R and S) plus a further seven possible bedrock con-
ductors (HH, T, U, V, W, X and Y), largely consistent with prior Input
AEM results.
IP/resistivity surveys, carried out selectively over portions of Grids A,
AA and D, confirmed several weaker MaxMin anomalies as probable bedrock
sources. In particular, MaxMin zones S and T on Grid D were validated;
one of these zones may be the continuation of the so-called Casa Berardi
break.
One hundred and twenty-four reverse circulation holes were drilled
immediately down-ice from (and in some cases directly into) MaxMin con-
ductive zones. In general, a single well developed till derived from the
northwest was encountered (Matheson Till). In areas of deeper overbur-
den, a second, lower till derived from the north-northeast was also en-
countered.
Seventy-two of the holes contained a total of 333 gold grains, consisting
of 273 abraded, 39 irregular and 21 delicate grains. Sample H-86-76-10
contained the maximum number of gold grains (13). Analytical values for
gold in heavy mineral concentrates ranged up to 78,000 ppb (sample H-86-
78-08) and generally correlated with the presence of visible gold
grains.
Many of the holes containing anomalous gold are found in a bedrock depre-
ssion in the central flexure zone. The general preponderance of abraded
gold grains, the nearly equal abundance of gold in upper and lower tills,
the absence of a well-defined dispersion train(s) and the lack of gold
values attributable to immediately up-ice MaxMin conductors points to a
regional high background dispersion of gold in the tills rather than
discrete local sources.
Anomalous base metal values in heavy mineral concentrates were detected
down-ice from various MaxMin conductive zones on the property; these in-
dicate possibly favourable targets for base metals.
Bedrock geology as determined by the reverse circulation drilling supp-
orts the general lithologic interpretation of mafic volcanics interspers-
ed with bands of altered sediments and felsic volcanics. Reverse circul-
ation drill holes which directly penetrated MaxMin conductors encountered
predominantly graphitic material.
The results of diamond drilling currently underway should be integrated
into the existing information base to determine if changes to present in-
terpretations are warranted.
TABLE OF CONTENTS Page
SUMMARY
1.0 INTRODUCTION 1
2.0 LOCATION, ACCESS AND INFRASTRUCTURE 2
3.0 PROPERTY 4
4.0 HISTORY AND PRESENT EXPLORATION ACTIVITY 7
5.0 GEOLOGY AND MINERAL DEPOSITS 5.1 Regional Geology 10 5.2 Mineral Deposits 12 5.3 Exploration Models 26 5.4 Property Geology 27 5.5 Regional Glacial Geology 28
6.0 EXPLORATION PROCEDURES 6.1 Geophysical Surveys
6.1.1 Horizontal Loop EM Survey 30 6.1.2 Induced Polarization/Resistivity 31
6.2 Reverse Circulation Drilling Method 6.2.1 General 31 6.2.2 Glacial Sediments and Dispersion Trains 32 6.2.3 Drilling and Sampling 37 6.2.4 Sample Processing and the Heavy Minerals
Concentrate 39 6.2.5 Applications 42 6.2.6 Interpretational Considerations 43
7.0 EXPLORATION PROGRAM 7.1 Geophysical Surveys 46 7.2 Reverse Circulation Drilling, Sample Processing and
Analytical 50 7.3 Sample Statistics and Data Processing 52
8.0 GEOPHYSICAL RESULTS 8.1 MaxMin Survey 55 8.2 IP/Resistivity Survey 61 8.3 Discussion 66
9.0 REVERSE CIRCULATION DRILLING RESULTS 9.1 General 68 9.2 Local Glacial Geology 68 9.3 Visual Gold Grains 70 9.4 Analytical Results - Overburden
9.4.1 Gold 70 9.4.2 Arsenic 77 9.4.3 Copper, Zinc, Silver 79
9.5 Analytical Results - Bedrock 81 9.6 Discussion 81
TABLE OF CONTENTS
Page
10.0 CONCLUSIONS AND RECOMMENDATIONS
88
References
LIST OF TABLES
Table 1: Coefficients of Variations for Heavy Mineral Concentrate
Analyses: Till Samples 53
Table 2: Gold Grain Summary 71
Table 3: Summary Statistics for Heavy Mineral Concentrates:
Till Samples 80
Table 4: Calculated Element Thresholds Reverse Circulation:
Till Samples 82
Table 5: Bedrock Trace Element Analyses 83
Table 6: Heavy Mineral Concentrates from Bedrock Samples:
Summary Statistics 85
LIST OF PLATES
Plate 1: Gold Grains, sample H-86-80-06, 07
76
LIST OF FIGURES
Figure 1: Location Map 3
Figure 2: Property Map 6
Figure 3: Generalized Geology and Mineral Deposits 11
Figure 4: Glacial Dispersion of Mineralization 33
Figure 5: Glacial Sediments and Landforms 35
Figure 6: Overburden Drilling and Sampling Procedures 38
Figure 7: Grain Shape Parameters 40
Figure 8: IP/Resistivity:. Interpretive Format 49
LIST OF MAPS
(Volume II)
Map 1:
Map 2:
Map 3:
Map 4:
Map 5a:
Map 5b:
Map 6a:
Map 6b:
Map 7a:
Map 7b:
Map 8a:
Map 8b:
Map 9:
Reverse Circulation Drilling and Geophysical
Compilation
Glacial Stratigraphy
Till Geochemistry Results
Till Geochemistry - Equivalent Values
Grid A: MaxMin Profiles, S=150 m, 444 Hz
Grid A: MaxMin Profiles, S=150 m, 1777 Hz
Grid AA: MaxMin Profiles, S=150 m, 444 Hz
Grid AA: MaxMin Profiles, S=150 m, 1777 Hz
Grid C: MaxMin Profiles, S=150 m, 444 Hz
Grid C: MaxMin Profiles, S=150 m, 1777 Hz
Grid D: MaxMin Profiles, S=200 m, 444 Hz
Grid D: MaxMin Profiles, S=200 m, 1777 Hz
Grid D: Contoured Chargeability N=3 with
Interpretation
1:10,000
1:10,000
1:10,000
1:10,000
1:2,500
1:2,500
1:2,500
1:2,500
1:2,500
1:2,500
1:2,500
1:2,500
1:2,500
LIST OF APPENDICES
(Volume III)
Appendix A:
Appendix B:
Appendix C:
Appendix D:
Appendix E:
Appendix G:
Appendix H:
Appendix I:
Drill Bit Statistics
Heavy Mineral Processing Results
Certificates of Analyses
Reverse Circulation Drill Logs
Overburden and Bedrock Geology
Geophysical Instrument Specifications
Notes on IP/Resistivity
IP/Resistivity Pseudosections
(Volume IV)
Appendix F: Statistical Analyses
1.0 INTRODUCTION
This report presents and discusses the results of a combined ground geo-
physics and reverse circulation drilling program carried out by MPH Con-
sulting Limited of Toronto on behalf of Homestake Mineral Development
Company over portions of the latter's Joutel Project in northwestern
Quebec.
The geophysical surveys, consisting of MaxMin horizontal loop EM and IP/
resistivity, were undertaken to detect and define zones of conductive
and/or polarizable sulphides that could reflect economic gold or poly-
metallic sulphide mineralization.
The reverse circulation drilling program was carried out to test the geo-
physically defined targets and/to detect indicators of gold and/or poly-
metallic sulphides in the glacial overburden.
The report includes a description of the various exploration techniques,
a discussion of the individual results as well as integrated evaluation
of the gold and polymetallic sulphide potential of the property.
- 2 -
2.0 LOCATION, ACCESS AND INFRASTRUCTURE
The project area is located within Joutel, Montgolfier and Aloigny town-
ships some 15 km north of the town of Joutel in northwestern Quebec.
The property is most conveniently accessed by helicopter from Joutel.
The Selbaie Road transects the eastern part of the property. Alterna-
tively, access to much of the property can be gained via tractor roads,
preferably in the winter when the extensive swamps are frozen.
Terrain is typical of this portion of the Abitibi with extensive swamps
and muskeg containing restricted islands of slightly higher ground.
The principal mining operation in the area is the Agnico-Eagle gold mine
just west of Joutel. The nearest base metal smelter is that of Noranda
Mines Ltd. at Noranda, Quebec approximately 100 km to the south.
Cnleoupomou -50•
ONTARIO
Timmins
MOtOp9m1
;O• 79 •
300
SCALE 100 0 100 200
KILONE TRE!
REGIONAL LOCATION MAP
PROPERTY LOCATION
o,OnOo
• • QUEBEC
eO•
• • ^. •
OTTAWA
QUEBEC
MONTREAL
70•
MONTGOLFIER
DESMAZURES
PROPERTY LOCATION
VAL RENNES
RAINBOTH 79•30'
DETAILED LOCATION MAP
SCA LE 5 O !
9rL0NETRE]
HOMESTAKE MINERAL DEVELOPMENT COMPANY
JOUTEL
LOCATION JOINT VENTURE
MAP Pro)•Ct No. C— 878 By J.Roth , P. Rolllnson
Scow Drown. M P H
Droving No Figur• 1 Dot.. August, 1966
'G`) MPH Consulting Limited
4
3.0 PROPERTY
The property consists of 306 unpatented mining claims in Joutel, Montgol-
fier and Aloigny townships. The property was staked by Lenora Explora-
tion Ltd. and Argentex Resources Exploration Corp. in 1983 and the claims
transferred to the Homestake Mineral Development Company (HMDC) under a
joint venture agreement. The property totals some 4,896 hectares as
shown in Figure 2 and is more properly described as follows:
Claim No. Claim No.
413326 (2-5) 407991 (1-5) 413327 (1-5) 407992 (1-5) 413328 (1-5) 407989 (1-3) 413329 (1-5) 407995 (1-5) 413330 (1-5) 407996 (1-5) 413332 (1-5) 407997 (1-5) 413333 (4-5) 408000 (1-5) 413334 (1-5) 409002 (4-5) 413335 (1-5) 413101 (1-5) 413336 (1-5) 413102 (1-5) 413337 (1-3) 413307 (1-5) 413061 (1-5) 413308 (1-5) 413062 (1-5) 413309 (1-5) 413063 (1-5) 413310 (1) 413064 (1-5) 413310 (2-5) 413065 (1-5) 413311 (1-4) 413066 (1-5) 413311 (5) 413067 (1-5) 413312 (1-5) 413068 (1-5) 413313 (1-2) 413069 (1-5) 413313 (3-5) 413070 (1-5) 413314 (1-5) 413071 (1-5) 413315 (1-5) 413072 (1-5) 413316 (1-4) 413073 (1-5) 413317 (1-5) 413074 (1-5) 413318 (1,2,4,5) 413075 (1-5) 413318 (3) 413076 (1-5) 413319 (1-4) 413077 (1-5) 413319 (5) 413078 (1-5) 413320 (1-5) 413079 (1-5) 413321 (1-2) 413080 (1-5) 413321 (3-5) 413081 (1-5) 413323 (1-5) 409002 (1-5) 413324 (1-5) 407990 (1-5) 413325 (1-5)
- 5 -
Claim No. (coned)
413326 (1)
413331 (1-5)
413333 (1-3)
422991 (1-5)
422991 (1-4)
428383 (4-5)
428384 (1-5)
428384 (1-5)
426733 (1-3)
To maintain the claims in good standing, assessement work is required by
the Quebec government or, in lieu, an annual payment as follows:
First year: $5/hectare (i.e. $80/claim)
Second to tenth: $10/hectare (i.e. $160/claim)
Work performed on one claim may be applied to other claims of the same
group provided the claims are contiguous and the claim grouping does not
exceed 480 hectares (1,200 acres).
The holder of a claim(s) who wishes to retain his rights must apply for a
development licence no later than 10 days prior to the expiration of a
claim. The licence is valid for one year and must be renewed each year.
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7
4.0 HISTORY AND PRESENT EXPLORATION ACTIVITY
Previous work on the HMDC Joutel property is summarized in the report by
D. Bending (1985) as follows:
"The area was subject to geophysical surveys and reconnaissance drilling
as early as the mid 1960's, primarily directed toward massive sulphide
deposits. This work is summarized in the geoscientific compilation for
NTS areas 32E/9 and 32E/10 (revised 1983). The most significant work in
terms of the present gold exploration program was conducted by Dome
Mines, Patino Mines and Canico.
Dome conducted EM and magnetic surveys in 1977 (File GM 33318, 34554),
which outlined several regional conductors. These conductors were tested
by drilling in 1979, in the Lac Laurin area. Sampling in this hole was
restricted to short intervals which were rich in pyrite and graphite,
while extensive intervals of 'quartz-carbonate stringers' were not assay-
ed. The gold values encountered were. very low, and the property was
allowed to lapse.
Patino Mines conducted EM and magnetic surveys in the eastern portion of
the property area. In 1979, one diamond drill hole tested one of the
conductive zones outlined. The gold values reported ranged up to 0.07
oz/ton (across 2 ft) with extensive intervals (tens of feet) in the range
of 0.01 to 0.04 oz/ton. The property was subsequently allowed to lapse.
Canico has been working actively in the area since 1976. Their Douay
Township property, immediately east of the HMDC/LA group, has been sub-
ject to detailed drilling which has defined two small but geologically
significant gold mineralized zones. Numerous other holes were completed
in the course of their regional exploration program.
8
The property was staked by Lenora-Argentex in 1983, and the claims trans-
ferred to the Homestake Mineral Development Company under a joint venture
agreement. Homestake subsequently performed EM and magnetic surveys
(Hansen, 1984), geological review, overburden drilling and one diamond
drill hole (Curtis, 1985). The geophysical surveys confirmed and refined
the definition of the conductive zones defined by previous work, and pro-
vided much of the basis for the 1985 drilling program. The overburden
and diamond drilling programs failed to corrobate the gold values report-
ed in the Patino drill hole, and strongly suggested that the encouraging
results were analytical errors (Averill, 1984, Curtis, 1985)."
The following companies are also presently active in the immediate
property area:
(a) Placer/Golden Shield
The property of Golden Shield Resources Ltd. tied onto the west/
northwest corner of the present claim block is held under option by
Placer Development Ltd. Placer has released the results of a
diamond drill hole into the "Casa Berardi Break" several kilometers
west of the Homestake ground which returned 0.1 ounces gold per ton
over 10 ft (Northern Miner, June 2, 1986). This value is within a
100 ft section of highly altered core containing quartz stringers in
immediate proximity to the Casa Berardi graphitic fault zone.
(b) Tandem Resources Ltd.
Tandem Resources, which hold a large property to the northwest of
the Homestake ground, have encountered a sulphide zone which they
believe to be geologically similar to the Kuroko-type polymetallic
deposits of Japan. Tandem's discovery hole cut 25.2 ft averaging
1.68% copper, 3.35% zinc, 0.65 oz silver and a trace of gold. A
hole drilled 50 m east of the discovery hole contained a 16.2 ft
section averaging 4.41% zinc, 0.36%- copper, 0.21 oz silver with a
trace of gold (Northern Miner, June 16, 1986).
9
(c) Canico Douay Deposit
Three hundred and four claims held by Inco (60%) and Soquem (now
Cambior) (40%) are located to the east of the HMDC property in Douay
and Vezza townships.
Gold is reported to occur in three horizons within mixed felsic vol-
canics and sedimentary rocks along the contact separating the Gale
group from the Taibi group. The best grades are found within two
exhalite units composed of laminated silica, sulphides and carbon-
ates. Lower grades have been intersected in a tuffaceous sandstone
unit. One hundred and sixteen thousand tons grading 0.536 oz/ton Au
are reported for the main exhalite unit and 130,700 tons grading
0.101 oz/ton Au are reported for the sandstone unit.
Canico announced in the September 1, 1986 Northern Miner that a
55,000 ft diamond drill program has started on the Douay Township
property in an attempt to double reserves.
- 10 -
5.0 GEOLOGY AND MINERAL DEPOSITS:
DETOUR-MATAGAMI SECTOR, ABITIBI GREENSTONE BELT
5.1 Regional Geology
The Homestake Mineral Development Company Joutel property is located
in Montgolfier, Aloigny and Joutel Townships within the Abitibi
Greenstone Belt, as indicated in Figure 3. The Abitibi is the larg-
est and most productive of several east-west trending metavolcanic-
metasedimentary belts within the Superior Structural Province of the
Canadian Shield. These supracrustal rocks are dominantly of Archean
age, generally greater than 2 billion years B.P.
The general area of interest is a rectangular zone 200 km long by
125 km wide bounded approximately by the Detour mine in the north-
west, the Burntbush area in the southwest, the Joutel area in the
southeast and the Matagami area in the northeast.
The area is generally flat and monotonous with extensive black
spruce swamp and muskeg cover. Outcrop exposure is typically 1% or
less so that the geology is imperfectly known. A further corollary
of this is that additional undiscovered major deposits likely exist
beneath overburden in the region.
Mafic metavolcanics are interpreted to be the predominant lithology.
Scattered throughout this mafic "sea" are several centres of felsic
volcanism such as in the Mat_agami area and around the Selbaie Mine.
However, extensive assessment research indicates that there are far
more felsic rocks in this region than presently recognized. This is
very important from an exploration viewpoint in that massive sulph-
ide gold-base metal deposits are typically hosted by felsic volcan-
ics.
Intercalated with the mafic rocks are regional sedimentary-tuffa-
ceous units with abundant graphite, argillite, sulphides and oxide
iron formation. These units typically appear as zones of airborne
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- 12 -
EM conductors which may extend for tens of kilometers across coun-
try. As such, they provide valuable stratigraphic marker horizons.
This sedimentary-tuffaceous setting can also be a fertile one for
mineral deposits. Inco's Casa Berardi gold deposit and the Agnico-
Eagle Mine are found in such settings.
Intrusive into all of these rocks are various intermediate to felsic
plutons, some of which may be broadly coeval with volcanism, i.e.
synvolcanic, and hence of interest from an exploration viewpoint.
5.2 Mineral Deposits
After the Republic of South Africa's Witwatersrand, which produced
some 1,114 million ounces of gold between 1884 and 1978, the great-
est gold mining area of the western world is Canada's Abitibi belt.
Composed mainly of Archean volcanic and sedimentary rocks, the
Abitibi has produced more than 133 million ounces of gold between
1906 and 1981.
Several major gold and base metal deposits are present in the gener-
al region. The characteristics of some of these deposits, pertinent
to further exploration in the region, are described below:
(a) Detour Mine - Ontario
The Detour gold (+ copper) deposit, located 70 km west of the
present property, was discovered in 1974 by Amoco Canada
Petroleum Company Ltd. during a geophysically oriented search
for base metal massive sulphide deposits. The original drill
target was a strong electromagnetic conductor with a directly
coincident magnetic high. These geophysical responses are now
known to relate primarily to the cherty sulphide (pyrite,
pyrrhotite + chalcopyrite) iron formation which hosts much of
the gold ore.
- 13 -
Present reserves are quoted at approximately 10.9 million
tons averaging approximately 0.128 oz Au per ton and 0.15% Cu.
These reserves extend to the 1,800 foot level and the deposit
is completely open to depth. The mine went into official pro-
duction on November 4, 1983 at a rate of 2,500 tons per day.
Initial production was by open pit although operations are
currently suspended due to a lower than expected gold grade and
weak gold prices. Shaft sinking is currently underway to
determine the economic feasibility of the underground mining of
the deposit.
The "main zone" of gold mineralization at Detour is essentially
an auriferous quartz fracture zone centered on a cherty tuff
unit and extending into the immediately overlying basalts.
Gold values also extend beneath the cherty tuff into underlying
altered ultramafics. The overall mineralized zone plunges 45
degrees west.
The main zone is generally 20 to 40 feet in width and consists
of a system of narrow quartz veins which contain 10 to 15%
pyrrhotite, 0.5 to 1% chalcopyrite and 1 to 5% pyrite within
the veins and selvages.
Four gold zones are found in the hangingwall basalts above the
main zone and are referred to as the quartz-vein zones. The
mineralization is similar to the main zone in that the gold
occurs within quartz veins with associated pyrrhotite and chal-
copyrite with biotite selvages. Most of the quartz vein zones
are interpreted to occur in structures that parallel the main
zone.
There are several zones of mineralization in underlying talc-
carbonate rocks. In these zones, the gold occurs as blebs and
specks in close association with pyrrhotite and chalcopyrite.
- 14 -
Quartz veins are occasionally present but are not essential for
the presence of gold.
The Detour ore body occurs at a local, gentle anticlinal warp
on the north limb of the Detour anticlinal fold, the axis of
which is located well south of the mine. The plunge of the ore
is exactly that of the fold and appears to occupy a fracture
zone which is axial planar to the subsidiary warp. It is
therefore suggested that there is a very strong structural
influence at Detour in addition to the obvious stratigraphic
control.
(b) Selbaie Mine - Brouillan Township
The Selbaie zinc-copper (+ gold, silver) mine was discovered in
1974 by a Selco Exploration - Pickands Mather joint venture.
The deposit was discovered by diamond drilling of a very weak
horizontal loop EM anomaly in follow-up to an airborne EM
survey. Production began in mid-1981 at 1,500 metric tonnes
per day (B-Zone). The mine is currently undergoing a major
expansion, funded in part by the Quebec government.
The Selbaie deposit occurs within acid pyroclastic and volcani-
clastic rocks which form part of the Matagami section of the
Archean Abitibi orogenic belt.
Ore reserves in the B Zone at December, 1982 consisted of 2.83
million tonnes averaging 3.5% Cu, 0.7% Zn, 33 g Ag, 1.2 g Au
per metric tonne. Reserve figures quoted for the A-2 Zone
(1978) were 5 million tons in grading 2.02% Cu, 1.33% Zn,
0.36 oz Ag and 0.036 oz Au per ton.
This base metal deposit is somewhat atypical in that it con-
sists mainly of epigenetic quartz-carbonate-base metal vein
- 15 -
systems resulting from hydrothermal activity related to late
stages of acid volcanism rather than the standard massive
sulphides emplaced in syngenetic fashion.
The host rocks consist of rhyolitic tuffs and breccias, bedded
chert-pyrite and volcaniclastic debris. An overlying quartz
porphyry unit, which is weakly mineralized, may have acted as
an impermeable cap rock during the mineralization event.
Veining and minor replacement occur in preferred but variable
steeply dipping fracture/fault systems. The vein systems
(Zones A-1 and A-2) are concentrated within subhorizontal,
permeable rhyolitic units.
Principal hypogene minerals are pyrite, sphalerite and chalco-
pyrite. Galena, tetrahedrite, polybasite, and native silver
occur in minor amounts together with native gold. Supergene
chalcocite, digenite, covellite, bornite and native copper
occur as fracture fillings and replacement rims around hypogene
sulphides.
Important characteristics of the Selbaie deposit include the
relatively weak nature of the related EM target and the epi-
genetic nature of the mineralization as compared to the classi-
cal stratiform massive sulphide model.
(c) Agnico-Eagle Mine, Joutel Township
Located near Joutel, this gold mine has produced 610,000 ounces
of gold from 3,300,000 tons of ore from 1974 to 1984. Reserves
at December 31, 1984 were 1,401,592 tons of 0.203 oz gold per
ton. Barnet et al. (1982) report on the deposit as follows:
- 16 -
"Investigations leading to the discovery of the deposit began
in February, 1962 during early exploration of the Joutel-
Poirier district for base metal sulphide deposits. Ground geo-
physical surveys outlined coincident magnetic and electromag-
netic anamalies which were tested by diamond drilling in late
spring of the same year. Exploration continued, and by 1967 it
was apparent that a potentially mineable deposit of auriferous
pyrite existed, and underground development was initiated.
Regular and substained production began in 1974.
Unlike most Archean gold deposits, Agnico-Eagle has many simi-
larities to massive base metal sulphide deposits, suggesting a
common volcanogenic origin. The gold is contained within the
sulphide facies of a stratabound to stratiform carbonate-
sulphide-silicate-oxide facies iron formation which immediately
overlies a sequence of partially welded felsic tuff and lapilli
tuff. A carbonaceous schist containing pyrite bands and
nodules occurs immediately overlying the ore zone.
The ore-bearing sequence is distinctly zoned with an outward
change from an iron silicate facies exhalite at the center of
the ore body to iron carbonate facies exhalite. Although chal-
copyrite and sphalerite are present only in accessory quanti-
ties, analytical data indicates that copper and zinc exhibit
both lateral and vertical zonation. The only important ore
mineral is native gold with a fineness of approximately 830.
The gold occurs as microscopic-size inclusions and veinlets in
and around pyrite in the carbonate facies exhalite, and pyrite
and pyrrhotite in the silicate facies exhalite. It is proposed
that like many massive base metal sulphide bodies, the Agnico-
Eagle deposit formed by volcanogenic and exhalative process."
A key observation concerning the Agnico-Eagle mine is that it
- 17 -
is essentially a massive pyrite deposit which carries economic
gold values. This deposit is reminiscent of the Horne Mine in
Noranda which, although generally thought of as a base metal
mine (mainly copper), is a massive sulphide gold deposit which
produced 11 million ounces of gold from 58 million tons of
ore.
Any pyrite + pyrrhotite zone in this region should therefore be
thoroughly evaluated for its gold potential. It is our finding
that many such zones have not been assayed for gold in the
past.
(d) The Golden Pond Gold Deposits, Casa Berardi Township
Four separate gold deposits are now indicated on the Golden
Pond property located 60 km southeast of the present property.
Estimated reserves at the Golden Pond and Golden Pond East
deposits currently total some 6.3 million tons of 0.255 oz gold
per ton with approximately equivalent tonnages in both zones.
The initial discovery was made by INCO in 1981 by diamond
drilling of a ground electromagnetic-magnetic anomaly. The
initial discovery hole was drilled on what is now known to be a
small satellitic zone to the south of the main Golden Pond
deposit. Three holes drilled as follow-up to the discovery
hole were blanks. It was only by continued drilling of targets
in the immediate area that the Golden Pond deposit was eventu-
ally discovered.
Golden Knight Resources Inc. of Vancouver subsequently farmed
into the entire 882 claim property to earn a 40% interest in
the property by spending $3,000,000 on exploration with INCO
remaining as operator.
- 18 -
The property lies on the south limb of a regional synclinorium
and straddles the contact between a lower sequence of volcanics
and an overlying thick sedimentary pile. The contact generally
trends E-W and dips almost vertically.
The geology of the property has been differentiated into var-
ious units using regional iron formations and graphitic hori-
zons as marker horizons. The main rock units from stratigraph-
ic top to bottom are given below:
Unit Description
3 Clastic sediments, mostly sandstone, siltstone.
2e Upper banded iron formation, ferruginous sediments.
2d Golden Pond pyroclastic unit, agglomerate, lapilli
tuff, tuffaceous sediments (ore-bearing).
2a Volcaniclastic conglomerates.
1 Lower iron formation, magnetite, ferruginous
sediments, clastic sediments.
Both geological and geophysical data clearly show that the
Golden Pond gold-bearing zone lies within a major east-west
trending conductive zone and an overlying complex pyroclastic
unit. The conductive unit is traced without ambiguity west to
the Turgeon River for a strike length of 20 km. At this point,
the conductive unit bifurcates and correlation is less certain.
West of the river, a double conductive horizon continues to the
Ontario-Quebec border.
It should be noted that there appears to be a major zone of
east-we'st faulting, shearing and alteration, designated the
"Casa Berardi Break", which extends through the deposit area
and which may have played a role in ore localization.
- 19 -
In detail, the geology of the Golden Pond area, based on drill-
ing to November 1983, can conveniently be considered in terms
of a sequence of four mini-cycles. The cycles (from south to
north) are briefly described as follows:
The base of Cycle I consists of a thick polymictic volcani-
clastic conglomerate. Clasts of pyritic grey chert and white
bedded chert are characteristic. The basal unit is overlain by
graphitic mudstone-siltstone which is capped by a discontinuous
lens of bedded sulphide facies (chert-pyrite) iron formation.
Cycle I hosts three distinct types of gold occurrences de-
scribed below:
1. A weak but continuous gold zone that straddles the contact
between the polymictic conglomerate and graphitic sedi-
ments.
2. A high-grade quartz-tourmaline-arsenopyrite-pyrite zone in
mudstone-siltstone containing visible gold.
3. Disseminated auriferous arsenopyrite in the pyrite-chert
exhalite.
The base of Cycle II consist of a variety of dacitic volcanic
and volcaniclastic rock with intraformational conglomerates.
The bulk of the cycle consists of a very thick sequence of
turbidite greywacke, sandstone, siltstone, mudstone, containing
nodular pyrite graphite and chert. Variable quantities of
intermediate to felsic volcaniclastic material are associated
with one or more apparently transgressive, carbonate-sericite
alteration zones which cut diagonally across the units. The
alteration is intense and pervasive and may represent fossil
hydrothermal conduits.
Ore grade mineralization in Cycle II is associated with this
-20 -
alteration and is also associated with graphite-pyrite-chert-
arsenopyrite zones at the top of the cycle.
Cycle III is dominantly pyroclastic. The cycle begins with a
thin, somewhat discontinuous, lapilli-tuff horizon overlain by
a thick, felsic agglomerate unit. The agglomerate is overlain
by a mixed sequence of lapilli-to-ash tuffs, green chloritic
mudstone, cherts and a thin dacitic flow (?). The cycle ends
with a magnetite quartz-chlorite-carbonate-pyrite iron forma-
tion.
Gold mineralization in Cycle III has been located on both the
south and north contacts of the agglomerate unit and in one
thin bed of pyritic iron formation.
Cycle IV is imperfectly defined and consists of well-bedded
calcareous sandstone-mudstone.
Some of the best gold mineralization found so far is in the
central and western part of the Golden Pond area. Values high-
er than 0.15 ounces gold per ton over 10 feet were intersected
by 16 out of 22 holes along a strike length of 720 meters
(2,360 feet). Most of the holes in this sector returned two or
more sections of economic interest.
An on-going, aggressive exploration effort has subsequently
resulted in the discovery and partial delineation of the Golden
Pond East deposit and more recently, the Golden Pond West
zone.
The significance of the Golden Pond East zone is emphasized by
an article in the Northern Miner (December 13, 1984) which
notes that:
- 21 -
"Hole 71747 returned an impressive 44.2 ft. grading 0.78 oz
gold per ton from 693.5-737.7 ft. This section included 19.3
ft. grading 1.27 oz. gold per ton."
A $7,200,000 underground evaluation program is in progress on
the Golden Pond east zone. A ramp has already progressed some
700 meters from the collar (Northern Miner - January 13,
1986) .
The above issue of the Miner also released details of an ini-
tial hole into what may be another discovery in the Golden Pond
West area, a hole impressive by any standards. The hole con-
tained three separate intersections as follows: 66.3 feet of
0.41 oz Au/ton; 47.6 feet of 0.1 oz Au/ton and 19.8 feet 0.46
oz Au/ton.
Key points at Golden Pond in our opinion include the crosscut-
ting, quartz-sulphide vein nature of the mineralization, its
occurrence near a regional INPUT-magnetic zone reflective of
sulphide-graphite-oxide iron formation. The abundance of
arsenopyrite in the deposit indicates that arsenic may be a
very useful pathfinder element in this region.
(e) The Estrades Deposit, Estrades Township
The Estrades deposit located west of the present property was
discovered by the Golden Hope-Teck Corporation joint venture in
late 1985. The deposit occurs in an Archean clastic sediment-
ary and felsic volcaniclastic sequence'(locally graphitic and
pyritic) with interbedded mafic to intermediate volcanic flows
and associated pyroclastics. The discovery would appear to be
in the same broad regional stratigraphic package which contains
the Golden Pond deposits and possibly the Agnico-Eagle mine.
-22-
Information from drilling to-date suggests a steeply dipping,
tabular massive sulphide deposit striking east-west. The dis-
covery hole, spotted approximately 400 ft south of the north
Golden Hope boundary cut a 35.1 ft section grading 0.2 oz gold
per ton and 9.15 oz silver with high copper and zinc values
(Northern Miner, December 2, 1985).
Drilling is being concentrated on two weakly conductive zones
which probably represent a common horizon. The western part of
the conductor has a strike component of more than 600 meters,
while the eastern part extends for approximately 1,100 meters.
Both are separated by a narrow gap occupied by a magnetic high
which appears to represent a cross-cutting diabase dyke em-
placed along a fault.
Thin section studies of the first core are indicated to reveal
a quartz-sericite schist in the hangingwall and a volcani-
clastic sediment comprising the footwall. These horizons form
a thin but persistent unit in an environment generally charact-
erized by mafic to intermediate volcanics.
Of importance to other exploration in this area in the fact
that Teck drilled an extremely weak, albeit discrete, airborne
conductor. A similarity to the Selbaie discovery is suggested
in this regard.
Recently released figures based on extensive drilling indicate
2.4 million tonnes at 0.14 oz Au/T, 3.5 oz Ag/T, 0.84% Cu and
7.7% Zn (Northern Miner, June 6/86) .
Matagami Camp
The first discovery and still the largest deposit approximate-
ly 25 million tons) in the Matagami Camp is the Matagami Lake
- 23 -
massive sulphide base metal deposit discovered in 1957. The
deposit was found in follow-up to airborne geophysical surveys
flown in 1956. A number of other massive sulphide deposits (12
in all) were found over a three township area, subsequent to
the main discovery, including the Orchan, Norita, New Hosco,
Bell Allard, Radiore A, Radiore B, Bell Channel and Garon Lake.
At least five of the deposits became producing mines.
The Matagami Lake mine has been in production since 1964. In
the year to December 31, 1985, the Matagami Lake mill treated
1,208,000 tons of ore to produce 9,453 tons of copper, 42,325
tons of zinc, 250,000 oz silver and 4,044 oz gold. Reserves
at the main Matagami Lake Mine at December, 1985 were indicated
to be 1,805,000 tons grading 0.42% Cu, 4.86% Zn, 0.60 oz Ag/ton
and 0.01 oz Au/ton. There is no production from most of the
other smaller deposits, at this time. Some of the smaller de-
posits have been mined out (e.g. Bell Allard [production:
258,124 tons at 9,30% Zn, 1.15% Cu, 1.08 oz Ag/ton and 0.012 oz
Au/ton). Noranda Mines has controlled most of the production
from this camp.
A major new discovery was reported by Noranda in October, 1985
on the Isle-Dieu Matagami Mine property, 1.5 km west of the
Matagami shaft. The discovery hole (N. 85-2) gave 18 ft (1702-
1820 ft) of 0.59% Cu, 26.36% Zn and 1.78 oz Ag/ton. Hole No.
85-3 gave 43.6 ft (1370-1413.6 ft) of 0.65% Cu, 27.51% Zn and
3.20 oz of Ag/ton and 14.6 ft (1583.4-1598 ft) of 0.93% Cu,
19.93% Zn and 1.03 oz Ag/ton.
In April (Northern Miner; April 21, 1986) Noranda announced a
hole (86-29) which intersected 104.8 ft (1705.4-1810.2 ft) of
1.08% Cu, 31.94% Zn and 3.92 oz Ag/ton and 18.3 ft (157.1-
1589.4 ft) of 19.3% Zn and 3.07 oz Ag/ton. This hole under-
- 24 -
lines the fact that significant new discoveries can be made even
within the heart of a major mining .camp.
District geology is described by MacGeehan et al (1981).
The Matagami mining district lies 150 km north of Noranda,
Quebec on the north side of the Abitibi Greenstone belt in the
Superior Province of the Canadian Shield. A series of twelve
pyrite-pyrrhotite-sphalerite-chalcopyrite-bearing massive
sulphide deposits occur clustered within a major Archean vol-
canic centre composed of a bimodal suite of basalts and rhyo-
lites intruded by contemporaneous gabbro dykes and sills and
underlain by the Bell River Igneous 'Complex, a high-level, sub-
volcanic layered gabbro-anorthosite pluton. This assemblage of
volcanic rocks, stratiform sulphide deposits and contemporan-
eous intrusions was then metamorphosed to the greenschist
facies and folded into a westward-plunging anticlinal struc-
ture. The Bell River Igneous Complex occupies the core of the
anticline and is flanked by volcanic rocks on either limb. A
series of granitic rocks were intruded at a later date. There
is poor outcrop in much of the district, and the geology has
mostly been established from drill-core correlation, geophysi-
cal interpretation and underground mapping in the mines.
On the south limb of the anticline, the massive sulphide de-
posits, including the Bell Allard, Orchan and Matagami Lake
mines, are all located at or toward the base of the 'key
tuffite', a thin semi-continuous mixed cherty tuffaceous unit
traced for over 10 km on strike along a rhyolite-andesite con-
tact. Sharpe (1968) divided this stratigraphy into the rhyo-
litic Watson Lake Group, underlying the 'key tuffite', and an
overlying Wabassee Group, composed predominantly of basalt and
andesite, but including several rhyolitic units, one of which
overlie the 'key tuffite' at the Orchan Mine.
- 25 -
On the north limb of the anticline these stratigraphic subdivi-
sions cannot be recognized, mainly because the 'key tuffite' is
not present. However, the volcanic stratigraphy there includes
seven basalt units, a pillowed feldspar porphyry (FP) and three
rhyolite flows. Most of the sulphide deposits are associated
with the Norita and Bell Channel rhyolites at the base of the
exposed volcanic succession, but the Garon Lake deposit is
developed above the stratigraphically higher Garon Lake rhyo-
lite. Above this mineralized rhyolite-basalt sequence, and
extending to the known top of the belt, is a thick section of
mainly pillowed basalt, loosely termed the 'Wabasee Group' cut
by numerous sills of similar composition. No ore deposits have
been found in this sequence to date.
Petrographic studies and chemical analyses of the basalt-rhyo-
lite sequence on the northern side of the camp show the volcan-
ic rocks to be of tholeiitic affinity. The basalts are iron-
rich, low-potassium tholeiites, and the rhyolites are quartz-
rich (75% Si02), but oligoclase-normative, tholeiitic rocks
termed dacite in some classification systems. Most of the vol-
canic rocks associated with mineralization were hyrdothermally
altered during sub-seafloor geothermal activity. The basalts
were spilitized, silicified and bleached to rocks of andesitic
or dacitic appearance, and the rhyolites frequently chlorit-
ized. However, the primary nature of the rocks can be identi-
fied from textures and by mapping individual altered flow-units
along strike into less altered domains.
La Gauchetière Deposit - Quebec
The deposit was found in 1974 during follow-up to airborne geophysi-
cal surveys in the region west of Matagami by Phelps Dodge. The
deposit is now owned by Noranda.
- 26 -
The deposit is indicated to be a stratiform, volcanogenic, massive
sulphide zone in felsic volcanic rocks. Drill indicated reserves as
of 1979 were 1,700,000 tons at 1.1% Cu, 4.9% Zn and 0.48 oz Ag/ton
with minor gold. Production was planned for 1982 but has been
postponed for some time.
5.3 Exploration Models
From the foregoing deposit descriptions, the probable types of gold
or gold/base metal deposits which can be expected in the area and
which serve as models to guide exploration are:
(a) stratiform/stratabound deposits + sulphides, quartz vein zones,
graphite, oxide iron formation in mafic volcanic environments
(Detour mine) or in felsic volcaniclastic-tuffaceous-sediment-
ary environments near volcanic contacts (Golden Pond).
(b) massive and stringer sulphide gold deposits without base
metals (Agnico-Eagle mine) or with base metals (Selbaie mine
and Estrades deposit) in a generally felsic volcanic-sediment-
ary environment.
The following models are also considered prospective in the area:
(c) Structurally-controlled, intrusive-associated, quartz stockwork
types of deposit localized along the margins of or within
intermediate to felsic•plutons. Such deposits are well repre-
sented in the Val d'Or area to the southwest.
(d) Disseminated gold deposits associated with carbonated, pyritic
mafic volcanics. Such deposits are important sources of gold
ore elsewhere in the Abitibi, noteably, in the Timmins area
(Owl Creek mine, Dome mine).
- 27 -
5.4 Property Geology
Outcrop on the property is limited. Bedrock geology is largely
interpreted from reverse circulation and diamond drill hole data.
Considerable ambiguity still exists regarding structure and strati-
graphy in the area.
Available evidence, including previous work by Homestake (Bending,
1985, pp. 11-12), indicates that the property is underlain by west-
northwest trending, steeply dipping, mafic metavolcanics and meta-
sedimentary rocks with minor intercalated felsic volcanics, chemical
sedimentary rocks and ironstones. The felsic volcanics and sedi-
ments appear to form a central unit flanked on either side by mafic
volcanics. These rocks are believed to comprise a portion of the
Taibi group and uppermost portions of the Gale group.
Two reverse circulation drill profiles carried out across strati-
graphy in the course of the present program correlate well with
these findings. A sequence of felsic volcanics with intercalated
sediments overlain by iron formation is sandwiched to the north and
south by intermediate to mafic volcanics. Sediments appear as thin
units throughout the sequence.
A central flexure zone can be discerned within the property upon
perusal of magnetic data. The axial portion of this flexure zone is
found between grids A and AA (Map 1).
In terms of gross regional structure, it is our interpretation that
the Homestake property is centred on the south limb and partially
within the axial region of a west-plunging anticline or antiform.
The nose of this fold appears to be located somewhere between Lac
Laurin and the Harricana river although a precise location is diffi-
cult to ascertain in that there appears to have been extensive shear
. transposition of bedding in the axial region.
- 28 -
Bedrock alteration consists of sericitization, carbonatization and
silicification and is most intensely developed in the central felsic
volcaniclastic/sedimentary unit. Felsic volcanics within the cen-
tral flexure zone appear to be sericitized and carbonatized. Meta-
sediments are often silicified or cut by quartz veins whereas mafic
intermediate volcanics are frequently carbonatized.
In terms of regional stratigraphy, the present property would appear
to encompass lithologies essentially up-section from those at Golden
Pond and broadly correlative with those at the Estrades deposit.
The "Casa Berardi Break" may cross the northwestern extremity of the
property.
5.5 Regional Glacial Geology
Glacial landforms and striae in the area suggest that two lobes of
the Laurentide ice sheet coalesced in the Joutel area during the
late Wisconsinan. A younger Hudson advance from the northwest
appears to have collided with a retreating Nouveau Quebec lobe from
the north-northeast. The so called "Mattagami esker" which passes
to the east of the present property is now recognized as an inter-
lobe moraine which marks the broad area of coalescence. This north
trending feature is of regional proportions and extends for some 100
km or more.
Till deposits of the older advance (Lower Till) from the north-
northeast are well preserved in bedrock depressions beneath younger
deposits (Matheson Till or Upper Till) from the north-northwest
glaciation. The presence of a number of even older pre-Wisconsinan
tills has been alluded to by workers in the region although their
origin and distribution remains uncertain.
-29-
In many cases two complete glacial sections consisting of upper
sediments (usually lacustrine clays) with underlying clastic sec-
tions are present. It is of course absolutely essential to be able
to differentiate between the tills of the two glaciations. The one
key distinguishing factor of the Upper Till is the presence of lime-
stone clasts derived from the Paleozoic terrain of the Hudson Bay
Lowlands.
It is also our experience in some parts of this area that the
earlier advance was a particularly erosive one which formed well
defined dispersion trains, while the younger glaciation was char-
acterized by ice that was often not in contact with bedrock and did
little more than disrupt existing patterns.
The Cochrane Till, a clay-rich till which incorporated and overlies
upper lacustrine clays was formed by a late re-advance from the
north-northwest. The Cochrane ice did not advance as far to the
southeast as the Joutel area such that Cochrane tills are generally
restricted to the northwest portion of the Casa Berardi-Selbaie
area.
-30-
6.0 EXPLORATION PROCEDURES
6.1 Geophysical Surveys
6.1.1 Horizontal Loop EM Survey
The horizontal loop electromagnetic method constitutes a
much-practiced technique for detection of conductive mineral-
ization and lithologies.
The basis of the technique consists of measurement of the
changes in EM coupling between two horizontal coils maintain-
ed at a fixed separation. These departures in the in-phase
and quadrature components are typically recorded as a percent
variation from a nulled setting.
Current instrumentation, exemplified by the Apex MaxMin
series of HLEM instruments, enables accurate measurement of
such variations at 5 or more frequencies.
The technique is generally amenable to thorough quantitative
analysis in terms of conductor geometry and conductivity.
This analysis enables identification of the characteristics
of tabular bedrock conductors arising from sulphide or graph-
ite sources. Such sources can generally be distinguished
from conductive overburden. However, weakly conductive bed-
rock sources (such as faults and shear zones) can yield res-
ponses substantially similar to narrow troughs of conductive
overburden. IP/resistivity surveys provide a means of re-
solving such ambiguities.
Data is normally presented as stacked profiles of the in-
phase and quadrature values with a separate plot for each
frequency.
A more complete description of the horizontal loop electro-
magnetic method may be found in Appendix G.
- 31 -
6.1.2 Induced Polarization/Resistivity
IP/resistivity is a galvanic electrical method developed
circa 1950 specifically to facilitate the search for non-
conductive deposits of disseminated sulphides. Other.polar-
izable minerals such as
yield similar responses.
graphite, magnetite and zeolites
Earth resistivity is normally measured as part of an IP sur-
vey. The two parameters together help characterize the
extent and nature of zones of sulphides or other polarizable
minerals.
IP/resistivity surveys may be conducted in the frequency or
time-domain. Modern IP systems, such as the Huntec time-
domain equipment employed in the present survey, enable pre-
cise measurements even under electrically noisy measurements.
A variety of arrangements of IP transmitter and receiver
electrodes may be employed. The present survey used an in-
line dipole-dipole array measured at multiple spacings.
Data from such a survey is typically plotted in pseudo-
section from and contoured to display significant variations
as a function of location and depth.
A more complete description of the IP/resistivity method may
be found in Appendix H.
6.2 Reverse Circulation Drilling Method
6.2.1 General
Overburden or reverse circulation drilling consists of drill-
ing through the overburden section with dual-tube rods and a
tricone bit using a water-air mixture as, drill fluid. The
resultant slurry is visually monitored, collected, sampled
- 32 -
and then is usually processed to obtain a heavy minerals con-
centrate. This concentrate is then analysed optically and
geochemically to detect ore or indicator particles. The op-
tical examination is particularly important in gold work
where the size and shape of gold grains may be highly dia-
gnostic of the distance to the bedrock gold source and even
the nature of the source.
The method is based on the principle that there are disper-
sion trains created in till during glacial over-riding which
can be detected and followed back up-ice to the bedrock
source area. The use of heavy mineral concentrates greatly
enhances anomalous metals concentrations making the method
extremely sensitive to distant deposits.
One of the most important applications of the method is in
the detailed follow-up to airborne and/or ground geophysical
surveys and evaluations along favourable geological trends.
6.2.2 Glacial Sediments and Dispersion Trains
Approximately 97% of Canada's land surface was glaciated dur-
ing the Quaternary. Figures 4 and 5 summarize the environ-
ments of glacial deposition, the types of glacial sediments
and associated land forms.
Lodgement till is the most favourable drift exploration med-
ium because in general, the source of clasts in the till will
be directly up-ice. In till, the concentration of ore clasts
usually shows a sharp peak at or near the source followed by
a rapid then gradual, i.e. approximately exponential, decline
in the down-ice direction. The size, shape and continuity
(and therefore detectability) of a dispersion train will de-
pend on many factors. These include size and composition of
source, bedrock topography, vigour of glacial quarrying and
- 33 -
GLACIAL SEDIMENTS INTERRELATIONSHIP
LANDFORMS
Groups Subgroups Subgroups Groups
Till
lodge cnl I11
Ablolion 171
G ovnd mo one
End morose Moraines
/
hummocky oblolion drift
ridge,
Elbert
Kelllet
Ovt•.roth he ods
Kamm'
Kome terrace'
Collopxd fed.mcnit
'j. D;sinlcgrotion
Ice - disintegration
features
q tr ~
Stratified
Drift
Ice - conlocl tlroGGed dill
Prog10ciol
slrolil.cd drill:
CSI wo ill
Glot'ol_b6e sedmertls
Glaciol - rnorine ted.menss
'1
~
~1
O,l...ash ploint and Ions
Deliot
bollomsedmenr (loll
• ProglaciaLforms
Mnn contlilvenl
Coo-v.-non conslilvenl
. - Ro.e Contliluenl
Figure 4: Relationship between glacial sediments and land forms.
-34-
abrasion, etc. Boulders closest to source will be larger and
more angular. Down-ice comminution leads to a decrease in
average clast size and increase in sphericity.
There is a recognizable indicator train almost 10 miles long
down-ice from the George Lake Zn deposit in northern Saskat-
chewan. In the Noranda area, anomalous Cu-Zn values have
been recorded in till up to 1 mile down-ice from the Horne
deposit while geochemical anomalies in till are restricted to
within 1,000 ft. of the nearby West Macdonald low grade Zn
deposit. A dispersion train appears to extend for over 6
miles down-ice from the Kidd Creek Mine near Timmins based on
a 1970-71 G.S.C. overburden drilling program. The above pro-
gram also showed that the separation between anomalous lenses
in till and bedrock increases down-ice from the Kam-Kotia
deposit near Timmins. This is interpreted as representing
relict shear planes in the glacier in lateral and down-ice
extent.
In gold exploration, detectable dispersion trains may be
poorly developed and may be very limited. This is due to a
number of reasons chief among which are local bedrock topo-
graphy, orientation of mineralized source relative to ice
direction and relative erodability of source. Trains may be
very narrow and have a distinct pencil-like form, e.g. Dome
Mine near Timmins and the Komis deposit in Saskatchewan; this
effect is usually a reflection of source orientation/topogra-
phic constraints.
The effect of bedrock topography on down-ice glacial disper-
sion can be profound. At the Golden Pond deposit, for
example, the recognizable gold train seems to be no more than
200 m long in the down-ice direction and is closely contained
within Lower Tills within a local east-west valley. At the
INGIACIAL
MATI RIAL ACÇU MUI Al ION
-35-
,- / ~ 0 / / IIoW e
/ , .' d'o.o,6 paR. o ~, • • . • ' .
-1 ~.r .f~~7,I~jl~~il .? '```\`\`♦, • `;;`';;♦
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`` ;; ♦ ♦ ;;♦`; ;;; ; ;`;`;;~l.:i~♦♦;; ```♦; ` ♦ ♦ ` ♦♦,♦`,`, ♦`A1♦PLUCKING ll . ♦ . ♦♦..♦ ♦ ♦ , ♦♦;`♦, ♦
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A
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ICf !tow
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OUI WASII AND/OR VALUT TRAIN
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-~s.► , ~ •i ~ • • r, n ~ .
6 *. ..~ssaflr / R~ô'Ô~~Lri~~~{%~AjŸ~~~-
a
• ♦~ ~"♦i♦ ` ♦♦♦♦ ♦ ♦„ „ • ..~♦♦.♦♦, ;"~ ;~..~ ~~ ```♦ ♦~♦ `~~i~~~~~~~`:
~ ~ ' " ~`~♦♦..)♦ ~~)~~:: ♦♦::` ♦♦ ♦ ♦. `` ..)♦~::` .:` ..... ♦ (NO MORAIN[ RIC II ``~
.. . .. "
~~//i~%~~.~j:i,•~/~/%
•0 0: 0 '0~.. ••rl:0/ R
................. ~~~♦ "~~;" ♦ ~.~;;♦ (SSIONAI MOI AIN( GROUND MORAINE 1000M NI Illl
Alt AIION Illt
A IlAIION
C VAS S ( fl t tINGS
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S IACNANI ICI
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-36 -
nearly Golden Hope Estrades deposit, a bedrock ridge immedi-
ately down-ice from the deposit has completely blocked the
formation of any significant dispersion fans.
When in very close proximity to the source, anomalous values
are generally concentrated in the basal part of the till
sheet so that this area of the overburden column is of prime
importance during sampling. Spectacular sulphide concentra-
tions may occur down-ice from a sulphide deposit. In such
cases, it is not necessary to await geochemical analyses.
Additional overburden drilling can progress directly on the
visual results.
The stratified varieties of drift, i.e. bedded gravels,
sands, silts and clays, are a less favourable sampling medium
because the fluvial re-working inherent in their formation
may make it difficult or impossible to identify the bedrock
source area. Placer-like concentrations, in which normal
background values are upgraded, may develop during the melt-
water re-working of glacial debris. This often produces
spurious anomalies in an overburden drilling program.
Varved lake clays representing rock flour washed out of glac-
ial drift and deposited in proglacial lakes are virtually
useless in minerals exploration (to date) and are not sampled
during the drilling process. Analyses on varved clays over
the Kidd Creek and South Bay polymetallic massive sulphide
orebodies, for example, show no signs of the immediately
underlying mineralization.
During drilling, the clays serve the useful purpose of seal-
ing the hole resulting in good sample return. Also, sulphide
minerals survive well in the reducing environment beneath the
-37 -
clay cap. Oxidation and leaching of sulphides can be a pro-
blem in some exposed tills.
6.2.3 Drilling and Sampling
The reverse ciculation method uses an approximately 3 inch
O.D. dual-tube drill pipe. The drill fluid consisting of
water and air is pumped down between the inner and outer
tubes, past the drill bit and back up the inner tube with the
cuttings which are then collected and sampled. The return
water overflows the sampling pail and is collected in the
underlying tank. This water may then be re-used as drilling
fluid or water may be pumped or hauled from some external
source.
The drill and accessory equipment such as pumps and compres-
sors may weigh 30 tons or more. These are generally mounted
either on the back of a large tracked carrier such as a
Nodwell or on skids so that it can be towed from drill site
to drill site by a medium-sized tractor. A permanent or
removable drillshack erected around the drill protects
drillers and geologists from the elements and allows for
year-round operation (24 hours per day if desired).
Figure 6 illustrates the drilling-sampling procedure.
Three drillers are normally required to carry out the drill-
ing, haul water if necessary, make roads, repairs, etc. A
geologist and an assistant are also present. The geologist
logs the overburden section by "feeling" the return and moni-
toring the material collecting on a 10 mesh screen. The
helper bags samples and generally assists the geologist.
THE OVERBURDEN
DRILLING METHOD Or MPH Consulting Limited
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- 39 -
Although it will emerge in the geochemical results, the visu-
al monitoring in the field, however, is very important since
the recognition of an ore clast during the drilling allows
the geologist to modify/extend the program while the drill is
in the immediate area.
The return is normally sampled at 5 ft intervals or at major
sedimentological boundaries. The bulk of the +10 mesh mater-
ial is discarded after inspection during the drilling as is
the return from most boulders. An overburden hole is usually
continued 2-5 ft or more into bedrock to try and ensure that
the bit is not in a boulder. A five foot run normally yields
about 15 lbs (6.8 kg) of -10 mesh material.
6.2.4 Sample Processing and the Heavy Minerals Concentrate
At the processing laboratory, a standard approach would be to
first wet screen the field samples at 10 mesh. The -10 mesh
material is then passed across a shaking or concentrating
table to produce a heavy minerals preconcentrate. Any grains
of native gold present in the samples, other than extremely
fine material, will ideally be seen on the table and recorded
by the laboratory technician during this operation. Samples
containing gold grains are then subjected to a careful
panning operation in which the gold grains are isolated for
microscopic inspection, measurement and micro-photography if
desired.
Some operators, such as Overburden Drilling Management Ltd.
of Ottawa classify gold grains as being abraded, "irregular"
or "delicate". These shapes are felt to be generally indica-
tive of transport distance with delicate grains being closest
to source, perhaps a few tens of metres, with highly abraded
grains having travelled much longer distances on the order of
a kilometer or more.
- 40 -
Figure 7 illustrates these grain shape parameters.
The table preconcentrates are then passed through a heavy
media (e.g. methylene iodide; S.G. = 3.3) to effect the true
heavy minerals separation. This will contain mainly the
common sulphides, free gold, magnetite, garnet and epidote.
The magnetic fraction is removed either before or after this
step. A 3/4 split is sent for geochemical analysis with a
split retained for reference purposes in the case of destruc-
tive analytical techniques while the entire heavies sample
may be submitted for analysis in the case of nondestructive
(e.g. neutron activation) methods.
Individual grains can be further subjected to Scanning
Electron Microscope or microprobe work to determine the
presence of trace elements (which may "fingerprint" a source
area), morphological features such as folding of grains,
re-crystallization, etc. The value of the microscope was
amply demonstrated in one instance around Timmins where some
highly anomalous Cu values were shown with the microscope to
be due to copper filings from 0-rings on a water pump and not
copper mineralization. This sort of contamination has been
virtually eliminated in overburden drilling work. Also,
heavy mineral concentrates can be lamped with ultraviolet or
examined by a scintillometer in the case of uranium explora-
tion.
Concentration ratios for the "heavies" vary between 100:1 to
200:1. This concentration greatly enhances anomalous metal
values making the method extremely sensitive. For example,
if Cu background in till was 100 ppm, the addition of a few
grains of chalcopyrite constituting another 100 ppm Cu to the
sample would only double the standard -80 mesh anomaly but
- 41 -
DELICATE
0-100 m ice transport. Primary crystal faces, pitted leaf surfaces & ragged leaf edges intact.
IRREGULAR
00_-1000 m ice transport. ( ;s primary shape a pitted surface ntact.
ABRADED 0 500 1 1
v
IRREGULAR
Curled leaf variety,
ABRADED Microns OOr)+ m ice transport. r ;e primary leaf auced to smaller
lakes with polished 'aces.
Spindled leaf variety,
o ~ 00 o ROUNDED
1000+ m ice + stream transport. Polished ecuidimensional E.rains.
Figure 7: Grain Shape Parameters
- 42 -
would produce a huge heavy minerals anomaly of 10,000 to
20,000 ppm because of the concentration ratio.
Occasionally, the "lights" are of interest as in exploration
for asbestos or the common lithium-beryllium minerals.
Appropriate heavy media can be used to isolate specific
gravity ranges of interest.
6.2.5 Applications
There are applications for reverse circulation drilling on
both the regional and detail scale. Regional work involves
wider hole spacings, up to 1 km or more. Such large step-
outs are allowed by the high sensitivity of the method. The
usual purpose of regional work is to intersect a large indi-
cator train which can then be traced back up-ice and the pro-
bable source area explored by detailed overburden drilling,
geophysics and diamond drilling.
A very important use of the method is in follow-up to air-
borne and/or ground geophysical surveys to assist diamond
drilling in anomaly evaluation. In this way all or most of
the anomalies located during a survey can be evaluated, not
only those with the highest geophysical rating. The overbur-
den drilling approach is also very useful in evaluating long,
formational anomalies.
A standard approach in the case of EM conductors is to drill
a string of holes immediately down-ice from the conductive
zone with a hole spacing of 100 to 300 m. This results in a
geochemical appraisal of the entire conductive zone. This is
particularly desirable since the actual economic deposit may
be in a less conductive or non-conductive area off or beside
the main conductor. In addition, it is common practice to
drill an overburden hole(s) directly into the conductor.
- 43 -
Another detailed application is to further explore a property
where a favourable contact or productive geological trend or
rock unit is known from previous work.
The bedrock information gained during overburden drilling is
very important for lithologic correlation and rock geochemis-
try. Also, there have been instances of direct ore intersec-
tions during overburden drilling (Asarco gold deposit,
Timmins, Ontario).
6.2.6 Interpretational Considerations
The drilling technology is now fairly advanced and more
sophisticated improvements, e.g. computer monitoring during
the drilling process, are already on the drawing boards.
Likewise the sample processing and analytical techniques are
now fairly rapid, effective and accurate.
One of the great problems of overburden drilling is in the
interpretation of the analytical/processing results. This is
particularly so in the case of gold exploration where the
"nugget effect" of a single large grain of gold in a small
heavy minerals sample may give rise to a very high yet possi-
bly meaningless gold value. It may also be difficult in some
cases to distinguish between high background levels of gold
and a truly significant anomaly. In geophysics, this would
be a question of trying to separate the "signal" from the
"noise" when the two can be of the same order of magnitude.
These problems are further complicated in areas of extremely
complex glacial geology as in portions of the Clay Belt of
northern Ontario-Quebec.
- 44 -
It is hoped that collected overburden samples will all be of
the same size but, of course, this is not always the case due
to lithologic changes and/or combining of samples for pro-
cessing.
One technique that we at MPH Consulting have used to advant-
age to overcome the effects that this can cause, is to cal-
culate, generally by computer, an "equivalent metal" value.
This takes into account the analytical value and weight of
the HMC and the original sample weight utilizing a formula of
the form:
Analysis ug/g* x Proportion Heavy Mineral ug/g = Equivalent
1,000 concentrate
of metal
(ng/g)*
This, in effect, is a reflection of the metal content per
gram of original till sample. Such equivalent values often
project a much more meaningful picture of metal distribution
in overburden.
We recognize however that such calculations are, in part, a
reflection of glacial lithology. A fluvial sand, for
example, would have a much larger heavy minerals endowment,
reflecting the fluvial concentration process inherent in its
formation, than a clay-rich till. The former would give a
higher equivalent number, other things being equal.
*An original value would be in ng/g resulting in an equival-
ent concentration in pg/g.
-45-
A further problem is the failure to recognize that the over-
burden material may not be giving the desired "reading" on
the up-ice bedrock stratigraphy. This will be the case if
the desired tills are absent or only poorly developed or if
the over-riding glaciers were not in contact with bedrock.
This latter effect may be much more common than previously
thought. Such overburden samples, no matter how carefully
processed and analyzed, will not be indicative of the up-ice
bedrock. For example, if drilling immediately down-ice from
a strong EM conductive zone, one should expect to see some
indication of that conductor, e.g. graphite or sulphide
chips, to be confident that the method is indeed working.
Another problem in the case of gold work is the potential
loss of fine gold during the drilling and processing and the
potential loss of gold in compound grains (e.g. gold in
quartz) during.t_he heavy media separation.
In summary, however, there is similarly little doubt that if
glacial conditions are correctly interpreted and if the
method is properly applied, the reverse circulation technique
can be extremely effective one in mineral exploration in
glaciated terrain.
- 46 -
7.0 EXPLORATION PROGRAM
7.1 Geophysical Surveys
Two contiguous cut line grids were established by Homestake on the
property prior to commencing the geophysical surveys. For the grid
covering the northwestern half of the property, the baseline was
established at an azimuth of 090° with crosslines at 200 m inter-
vals. The grid covering the southeastern half of the property has a
baseline oriented at an azimuth of 301°, with crosslines at 200 m.
The survey grids and topographic information together with the claim
locations were then compiled to constitute base maps at a scale of
1:2,500.
The geophysical program consisted of MaxMin II HLEM surveys carried
out over areas A/AA, C and D on both grids. IP/resistivity surveys
were then executed on a selective basis in areas A/AA and D.
The HLEM survey was carried out with an Apex Parametrics MaxMin II
instrument measuring the in-phase and quadrature components of the
secondary electromagnetics field at 444 and 1777 Hz at a station
interval of 25 m. Reconnaissance coverage was carried out with a
150 or 200 m coil separation. Instrument specifications for the
horizontal loop equipment are presented in Appendix G.
The MaxMin survey was carried out in four separate portions of the
overall property. These sectors are designated grid A in the east-
central part of the property (lines 74+OON through 88+OON); grid AA
adjacent to grid A to the west (lines 8+00W through 10+00E south of
the baseline); grid C in the north-central part of the property
(portions of lines 0+00 through 36+00W north of the baseline); and
on grid D in the northwest corner of the property west of Harricana River (lines- 66+00W through 78+00W). A total of 58.5 km of HLEM
survey was completed in these areas.
-47-
The IP/resistivity surveys, intended to selectively evaluate certain
weak MaxMin anomalies as well as to search for horizons containing
disseminated sulphides, were carried out on lines 82+OON and 86+OON
on grid A, line 8+00E on grid AA and lines 66+00W through 78+00W in
grid D.
The IP/resistivity survey was carried out in a time-domain mode em-
ploying Huntec IP equipment consisting of a 2.5 kw transmitter and a
MK IV receiver.
The pole-dipole array was predominantly used with a dipole length of
50 m and read to N=4. Line 74+00W in grid D was initially surveyed
with a dipole-dipole array but repeat pole-dipole coverage esta-
blished this array as optimal in detecting bedrock sources. Con-
siderable care was taken to ensure that transmitter currents were as
high as could be reasonably attained.
The standard parameters of primary voltage and total chargeability
were recorded as well as the chargeability values of five individual
decay windows of the IP curve to ensure recognition of any non-stan-
dard IP decays such as might be caused by electromagnetic coupling
of cultural interference. Primary and secondary voltages were mea-
sured to a sensitivity of 1 part per thousand and displayed a gener-
al repeatability of + 10%.
Complete equipment specifications may be found in the attached
Appendix G. A more detailed description of the IP/resistivity tech-
nique may be found in Appendix H.
Data acquisition was carried out by a MPH geophysical crew under the
direction of Simon Bate, B.Sc., geophysicist. Other members of the
crew included:
-48 -
Michael Zang, B.Sc., Geophysicist
John Foster, Technician
Raymond George, Technician
Larry Petrie, B.Sc.
Logistics were co-ordinated by Derek Hall, senior geophysical techn-
ician. The geophysical program was under the overall direction of
Dave Jones, Vice-President.
The MaxMin survey was completed during the period June 14-24, 1986
and the IP survey was completed during the period July 23 - August
9, 1986.
The in-phase and quadrature HLEM readings are presented in profile
form on the base map at a profile scale of 1 cm = 10%, comprising
Maps 5, 6, 7 and 8 for grids A, AA, C and D, respectively. Conduc-
tive features are identified on each of these plans and characteri-
zed as to the quality of the discerned anomaly, with the more im-
portant conductive zones designated alphabetically.
For the IP/resistivity survey, the primary (Vp) and secondary (Vs)
voltages measured in the IP/resistivity survey have been converted
to apparent resistivity in ohm-m and apparent chargeability in
milliseconds using standard formulae.
Of the various chargeability windows recorded, the total chargeabil-
ity integrated over the entire decay window was selected for presen-
tation since possible electromagnetic coupling was judged small.
The apparent resistivity and chargeability values for the dipole-
dipole and pole-dipole arrays have been plotted in standard pseudo-
section format at a horizontal scale of 1:2,500 and appropriately
contoured (Appendix I).
IP/RESISTIVITY INTERPRETATION
Resistivity Lows (nm) ► Limits
Undef ined
<10
10-100
100 —1000
<1000
Resistivity low at surface
Est. Dip
Resistivity low
at Depth
70
Estimated Intrinsic resistivity (nm)
Z 10
Estimated depth (metres)
Chargeability Highs (msec) Limits Undefined
•
> 50 msecs
50-25
25-10
<10
3
Estimated intrinsic chargeability (msecs)
IP anomaly at surface
IP onomaly at depth
3
Estimated Intrinslc chargeability (msecs)
Z ^- 20m
Estimated depth (metres)
Figure 8
-50 -
Anomalous resistivity lows and/or chargeability highs have been in-
dicated on each pseudosection using the interpretive format shown in
Figure 8. This interpretive format enables discrimination as to
intrinsic character and geometry of the chargeability or resistivity
feature.
In addition, the interpreted resistivity lows and chargeability
highs for both arrays have been compiled in plan form as seen in
Maps 9 and 10. The individual resistivity and chargeability anoma-
lies on each line have been linked where warranted to form resistiv-
ity or chargeability zones. The principal zones have been assigned
ana appropriate alphabetic designation and will be discussed in
Section 8.0.
Finally, the significant geophysical features, indicated targets and
prior exploration have been compiled and presented in Map 1 for the
property as a whole at 1:10,000 and in detailed fashion for the cen-
tral flexure zone on Map 2.
7.2 Reverse Circulation Drilling, Sample Processing and Analyses
Reverse circulation drilling was carried out in two phases on the
property. Initially, 112 holes totalling 9,135 ft (2784.3 m) were
completed between May 31 and June 25, 1986. A further 12 holes
totalling 1304.5 ft (397.6 m) were drilled in a follow-up program
between July 22 and July 28, 1986. Holes were normally spotted at
200-300 m intervals on fences approximately 100 m down-ice from EM
conductors established by the MaxMin surveys. Several holes were
sited to penetrate directly into EM conductive zones.
The drill contractor was Heath & Sherwood Ltd. of Kirkland Lake,
Ontario who supplied an Acker dual tube reverse circulation drill
mounted on a FN60 Nodwell tracked vehicle along with a GT1000
tracked vehicle carrying a 500 gallon water tank. The drill crew
- 51 -
consisted of a drill operator or "runner", a runner's helper and a
water hauler to provide water for the drilling operations. A more
detailed breakdown of drilling statistics can be found in Appendix
A.
The following MPH personnel were involved with the reverse circula-
tion drilling phase of the project:
Consultant - W.E. Brereton, P.Eng.
Geochemical Consultant - J. Siriunas, P.Eng.
Geologist - J.P. Rollinson, B.Sc. (Hon)
Sampler - Andrew Kamo, B.Sc. (Hon)
Overburden samples collected during the drilling were sent to the
laboratory of Overburden Drilling Management Ltd. in Ottawa for
heavy minerals processing. Standard visual monitoring was carried
out during the tabling pre-concentration process. Any samples in
which gold was observed were subjected to a careful panning opera-
tion in order to isolate and characterize each individual grain.
Three quarter splits of resulting heavy mineral concentrates were
then sent to Bondar-Clegg and Co. Ltd. for Cu, Zn, Au, Ag, As anal-
yses. The remaining one quarter split was retained for microscopic
examination and as a permanent record. Sample processing results
can be found in Appendix B.
At Bondar-Clegg, any samples containing significant visible gold
grains were analyzed by the pulp and metallics method whereby the
coarser fraction of the sample (+150 mesh), which presumably con-
tains the gold grains, was analyzed separately from the fine frac-
tion (-150 mesh) and the results combined to give a final weighted
average value. Au was analyzed by fire assay preconcentration
followed by aqua regia dissolution and atomic absorption analysis;
Ag, Cu and Zn were analyzed by atomic absorption after a hydrochlor-
- 52 -
ic acid-nitric acid digestion and As was determined by a colourmetr-
ic determination after nitric acid-prechloric acid digestion. Cert-
ificates of analysis are presented in Appendix C.
The +10 mesh bedrock chip samples collected were submitted for mul-
ti-element ICP and gold analysis. A representative suite of bedrock
chip samples was sent to Chemex Labs Ltd. in Mississauga with the
remainder of the bedrock chips sent t:o Acme Analytical Laboratories
Ltd. in Vancouver.
At Acme Analytical Labs a 0.5 gram sample was digested with. 3 ml
3:1:2 HC1:HNO3:H20 while at Chemex Labs a similar digestion of a
0.5 gram sample was made with an HNO3-aqua regia (3HC1:1HNO3)
mixture prior to the ICP analyses. It should be realized that these
digestions are incomplete for many minerals, especially oxide and
silicate minerals, and as such a number of the reported values can
only be considered as semi-quantitative. Analyses for gold at both
laboratories were performed by a fire assay preconcentration with an
atomic absorption finish.
7.3 Sample Statistics and Data Processing
Weights of heavy mineral concentrate have been converted t:o ug/g
(ppm) of original sample material (i.e. table feed x 0.75 (void
factor)). "Equivalent" metal values (e.g. "eAu") have been calcu-
lated for all elemental values based on the amount of non-magnetic
heavy mineral concentrate recovered for each sample. Analytical
data, log10 - transformed data and "equivalent" data have been
examined using histograms. Summary statistics for Au, Ag, As, Cu
and Zn can be found in Table 3. Complete computer print outs are
available in Appendix F.
Comparison of the coefficients of variation for all samples and dup-
licate samples (Table 1) indicates that the intrasample variation is
- 53 -
TABLE 1
COEFFICIENTS OF VARIATION FOR HEAVY MINERAL CONCENTRATE ANALYSES REVERSE CIRCULATION TILL SAMPLES
Element Total
Population Average
Duplicates) Analytical Coefficents of Variation Replicate
Analyses2
Au 4.59 0.45 1.0 Ag 1.29 0.51 0.34 As 0.88 0.32 0.17 Cu 1.32 0.15 0.13 Zn 1.91 0.29 0.22 Non-Mag 1.3 0.23 - Mag 1.21 0.31 -
1 - including ten sets of duplicates: 1. 47-01, 47-01A 2. 51-01, 51-01A 3. 52-01, 52-01A 4. 62-01, 62-OlA 5. 65-01, 65-01A 6. 67-01, 67-01A 7. 68-01, 68-01A 8. 89-01, 89-01A 9. 96-01, 96-01A 10. 104-01, 104-01A
2 - including five sets of replicates from original samples: 1. 09-12 2. 12-01, 02, 03 3. 62-01A 4. 79-04, 05 5. 103-01
- 54 -
much less than the overall variation observed in the entire popula-
tion of till samples. The intrasample variation is therefore not
expected to contribute significantly to the overall variation of the
population even though Sopuck et al (1985) have alluded to possible
variabilities of 40% to 50% in field and analytical data as docu-
mented in their till sampling case history. The replicate analysis
of samples (see Table 1) has also shown that only a small portion of
the overall variation is due to the analytical variation. The
analytical variation is most pronounced for the analysis of Au.
From an examination of computer-generated histograms, all elements
and equivalent values can be approximated by login - normal dis-
tributions and for the purpose of establishing thresholds, log10
- normal distributions and probability-cumulative frequency plots
have been used. The thresholds that have. been selected include (a)
threshold for "elevated" background concentrations (50% probability
of occurrence); (b) threshold for "possibly anomalous" concentra-
tions (5% probability of occurrence); and (c) threshold for "pro-
bably anomalous" concentrations (2.5% probability of occurrence).
Thresholds for the individual elements are presented in Table 4.
"Elevated", "possibly anomalous" and "probably anomalous" concentra-
tions of elements in till samples are indicated on Map 3 and Map 4
(equivalent values). The relative (vertical) position of the in-
dividual samples in each hole is indicated by the stacked plots on
those maps. The discussion and interpretation that follow within
this report focus primarily on the equivalent value thresholds. A
summary of all analytical values and equivalent values is presented
in Appendix F.
Summary statistics for bedrock trace element analyses can be seen in
Table 5 and summary statistics for heavy mineral concentrates from
bedrock samples are found in Table 6.
-55-
8.0 GEOPHYSICAL RESULTS
8.1 MaxMin Survey
The MaxMin survey detected conductive features interpreted as possi-
ble to definite bedrock sources in each area surveyed.
On grid A, as seen on Maps 5a and 5b, the MaxMin survey conduct-
ed with a 150 m coil separation disclosed a long conductor designat-
ed zone H together with subsidiary zones HH', LL and R.
Zone H extends across the survey grid from line 74+00W near
9+OOS in a westerly direction as far as line 84+00W near 13+75S. It
is a strong, definite bedrock conductor, It displaying an average
dip of 80°S and a depth between 30 and 40 m. Conductivity-thick-
ness, where not affected by overburden-induced quadrature rotation,
generally lies in the range of 5 to 15 mhos.
Zone H is known from MaxMin surveying on adjacent grid AA to extend
further to the west as will be discussed below.
Zone HH is a weak, subsidiary conductor parallelling zone H
approximately 250 m to the north. It is defined primarily as a
quadrature response at 1777 Hz on lines 80+00W through 84+00W.
Because of the weak, dominantly quadrature response, it is assigned
to the possible bedrock category.
Zone LL is a modest but probable bedrock feature detected on
line 88+00W near 1+50S. The conductive zone is judged a probable
bedrock feature.
Zone LL apparently does not extend onto line 86+00W. to the east.
The zone may be related to a probable bedrock conductor detected on
line 10+00E on grid AA to the northwest that may be part of zone L.
- 56 -
As analyzed on line 88+00W, zone LL is consistent with a bedrock
conductor dipping 75°N at a depth of 55 m with a conductivity--thick-
ness of 12 mhos.
Zone R, detected on the southern portions of lines 78+00W and
80+00W, is a probable bedrock conductor indicated by moderate anoma-
lies of reasonably convincing character. Zone R may well extend
further to the west-northwest and east-southeast where survey cover-
age is lacking.
On grid AA, adjoining grid A to the west, the MaxMin surveys
disclosed a long, strong definite bedrock designated H plus subsidi-
ary conductive features designated HH' and R, as seen on Maps 6a and
6b.
As on grid A, zone H is a long, strong definite bedrock conduc-
tor that undoubtedly extends further to the west beyond the limits
of present survey coverage.
On lines 10+00E through 6+00W the conductor displays widths ranging
from narrow to 25 m, and approximately vertical dips.
There appears to be a change in strike or possibly even a gap in the
conductor on line 2+00E, although data is incomplete due to a major
stream.
Based on the data, there are reasonable grounds for inferring the
presence of a cross-fault near line 2+00E, judging from the apparent
offset in the trends of zone H west and east of the river.
Zone HH' is a subsidiary anomaly located immediately north of
zone H and detected in the present coverage on lines 4+00E and
6+00E. The zone is principally reflected as a weak, dominantly
- 57 -
quadrature response seen mainly at the higher frequency. Its chara-
cteristics support a possible bedrock conductor at this location.
Zone HH' may well be related to zone HH on Grid A discussed above.
On line 10+00E immediately south of the baseline, a moderate res-
ponse partially defines a possible conductor indicated to be a ex-
tension of zone L to the west.
Because of incomplete coverage, the characteristics of zone L are
not well defined.
There is a possibility that zone L may continue further to the
southeast to link-up with the weak response designated LL detected
on line 88+00W on grid A.
Zone R on grid AA is represented by a weak response detected on
line 10+00E near 20+OOS. It is judged to be a probable bedrock
source.
This response is considered a western extension of zone R as defined
on the southern ends of line 78+00W and 80+00W on grid A. No
equivalent response was detected 200 m to the west on line 8+00E.
On Grid C the MaxMin surveying disclosed a series of weak, im-
persistent conductive features of which the better are designated
zones U, V, W, X and Y, together with strong but isolated responses
reflecting previously defined conductors M and N, as seen in Maps 7a
and 7b. All of these zones are best revealed on the 1777 Hz data.
Zone M is seen at the southern ends of line 16+00W and 18+00W.
Despite the intentionally partial coverage, it is clearly a strong
definite conductor consistent with the results of previous surveys
which have fully defined this conductive feature.
-58-
Zone N was traversed in the present survey only on line 32+00W
where it is evident near 3+65N as a definite bedrock conductor.
This response and location are consistent with the results of prior
surveys which have defined this as a long, stratigraphie horizon as
seen on the compilation map.
Zone U is defined as extending from lines 30+00W near 8+50N to
line 36+00W near 9+00W with an arcuate strike.
The anomalies on line 32+00W and 34+00W are regarded as possible
bedrock sources while the weaker, less well defined responses on
lines 30+00W and 36+00W would by themselves be considered simply
conductive overburden.
As analyzed on line 32+00W, the anomaly is consistent with a bedrock
conductor of approximately vertical attitude at a depth of 60 m and
a conductivity-thickness of 2.5 mhos.
Zone V is principally defined in the present survey by a weak
response on line 20+00W near 8+OON. There is no distinguishable
equivalent anomaly on lines on either side of line 20+00W.
As analyzed on line 20+00W, zone V is judged a possible bedrock
conductor. It would be consistent with a sub-vertical source at a
depth of 55 m with a conductivity-thickness of 1.5 mhos.
Zone W is principally defined on line 14+00W near 7+75N with
weaker, less credible responses indicating possible extensions 200 m
on either side of this line.
As analyzed on line 14+00W the response is rated as a possible bed-
rock conductor. It would be consistent with a sub-vertical bedrock
source at a depth of 50 m with a conductivity-thickness of 2.5 mhos.
-59-
Zone X is speculatively inferred to exist between lines 8+00W
and 10+00W near 9+OON on the basis of an unusual positive inphase
and quadrature features seen on these lines. These responses are
consistent with the presence of an oblique conductor. They are
unlikely to be caused by any sort of short cable effects or coil
orientation as indicated by the change in response as a function of
frequency. They could, however, be caused by a broad bedrock high.
Zone X would require several additional MaxMin traverses (including
a traverse oriented transverse to the present survey orientation) to
confirm its existence and to fully define orientation and extent.
Zone Y is a weakly indicated response detected on line 4+00W
near 11+50N with even weaker, less credible responses detected on
adjacent lines to the east and west.
As analyzed on line 4+00W the response is judged to be indicative of
a possible conductor with an approximately vertical attitude, a
depth of 30 m and a low conductivity-thickness of 0.7 mhos.
In addition to the above-described zones on grid C a number of other
weaker, poorer MaxMin responses are attributed to conductive over-
burden. The results of reverse circulation drill holes that tested
some of these weak features are consistent with such an interpreta-
tion.
On grid D, in the northwest sector of the property, the MaxMin
survey defined two modest conductive zones designated S and T, as
seen on Maps 8a and 8b.
Zone S was principally detected on lines 76+00W near 9+75N and
78.+00W near 8+30N. The responses, while weak, are consistent with a
bedrock source. The zone likely continues further to the west
-60 -
beyond the limits of the present survey. To the east a weak contin-
uation is speculatively interpreted on line 74+00W.
As analyzed on line 78+00W where the response is strongest, the
anomaly is consistent with a bedrock conductor dipping approximately
80° to the north at a depth of 50 m with a conductivity-thickness of
19 mhos.
As will be examined in greater detail below in the section 11.2, the
IP/resistivity survey has confirmed the validity of a bedrock source
at this location.
Zone S is consistent with a weak pyritic or graphitic horizon possi-
bly accompanied by shearing or faulting. There is in fact some
possibility that this conductive feature represents a continuation
of the so-called "Casa Berardi Break".
Zone T is a series of weak responses detected on lines 76+00W
and 78+00W near 0+30N. The conductive feature is judged a possible
bedrock conductor.
As analyzed on both lines at the lower frequency, the weak, predom-
inantly quadrature response is consistent with sub-vertical conduc-
tor at a depth of 30 m with a conductivity-thickness of less than 1
mho.
As will be discussed further below, the IP/resistivity survey pro-
vided confirmation of a valid bedrock source at this location.
Zone T would be consistent with a weakly conductive graphitic or.
pyritic source. This zone may well extend further to the west
beyond the limits of the present survey.
- 61 -
In addition to the above-described conductive zones there are sever-
al considerably weaker, poorer responses which are presently inferr-
ed to reflect probable conductive overburden.
Thus the MaxMin survey was successful in defining a considerable
number of additional conductive horizons constituting targets for
subsequent evalution by reverse circulation drilling.
8.2 IP/Resistivity Survey
The IP/resistivity survey results detected a series of conductive
and polarizable features complementary to the results of the MaxMin
HLEM survey.
As seen in the individual pseudosections in Appendix H, all traver-
ses exhibit considerably lower resistivities at the N=1 separation
with values generally increasing sharply with increasing N spacing.
The low near-surface resistivity reflects the presence of prevalent
conductive overburden throughout the survey area, which has an
intrinsic resistivity of approximately 40 ohm-m.
On grid A/AA the resistivity data show conductive overburden
to vary considerably in thickness. While thicknesses of 20-25 m
appear typical, the northern portion of line 8+00E has a much reduc-
ed thickness of conductive overburden.
The resistivity results also show a number of distinct low resistiv-
ity features related to isolated confined overburden troughs or dis-
crete conductive bedrock sources.
On line 82+00W there is a distinct, strong resistivity low centered
near 0+35S. This shallow source could well reflect a thickening or
change in overburden character.
- 62 -
Further south on this line there is another discrete resistivity low
of lesser contrast indicated near 4+30S. This feature could also
reflect weakly conductive bedrock source.
It should also be noted that the IP traverse extends far enough
south to cross MaxMin zone HH located near 10+25S. No discrete
resistivity low is seen at this location, suggesting that zone HH
(itself a weak, poorly defined MaxMin feature) may well be caused by
conductive overburden. However, it should be cautioned that narrow
conductive features under thick overburden are only poorly resolved
with the IP/resistivity technique.
On line 86+00W an interval of distinctly lower resistivity probably
reflecting a bedrock source is seen at the northern end of the line
immediately north of the baseline. A second interval of more con-
ductive material at depth probably related to a bedrock source is
inferred to exist between 1+25S and 1+80S.
On line 8+00E on grid AA uniformly high bedrock resistivities are
present with the exception of a zone of distinctly lower resistivit-
ies south of 13+75S. This interval corresponds to the MaxMin zones
HH/H and therefore offers support for the presence of a valid bed-
rock conductor at this location.
The chargeability results on the lines surveyed on grids A/AA
show a series of broad, weak to modest polarizable sources which
correlate with the general stratigraphic trends evidenced by the
magnetic and HLEM data.
On line 82+00W an interval of moderate polarizability extends from
2+50S northwards to the northern extent of the survey coverage and
quite possibly beyond.
- 63 -
At least part of the chargeability features is associated with high
resistivities, suggesting a rather low sulphide content. However,
the northern portion may be associated with a distinct resistivity
low implying possibly higher sulphide content, although the
plete coverage hampers interpretability.
incom-
A second interval of weakly anomalous chargeability is interpreted
near 5+15S. Resistivities accompanying this chargeability feature
are uniformly high, suggesting a very low tenor of disseminated
sulphides as a plausible source.
At the southern end weakly anomalous chargeabilities are seen which
indicate, in all likelihood, the edge of a stronger polarizable
source associated with MaxMin zone H beyond the southern limits of
the IP survey. Thus MaxMin zone H is supported as a valid bedrock
source by the IP/resistivity survey.
On line 86+00W, a broad interval of weakly to moderately anomalous
chargeability is present extending from 0+65S to 4+85S. These
sources are inferred to lie at a depth of approximately 40 m. A
resistivity low is associated with the stronger part of the charge-
ability feature suggesting the presence of moderate tenor of sul-
phides as a plausible source for this portion of the response.
On line 8+00E on grid AA there are three credible chargeability
anomalies.
The first chargeability zone exhibits moderate intensity and is
partially defined at the northern end of the line north of 2+25N.
It is interpreted to lie at a depth of 40 m. It is associated with
relatively high resistivities consistent with a source containing a
low content of disseminated sulphides.
-64-
The second chargeability anomaly on line 8+00E is a narrow, moderate
amplitude feature interperted to be centered near 4+25S. It too is
accompanied by high resistivities suggesting a low content of
disseminated sulphides.
The third significant source on line 8+00E is only partially dis-
cerned at the southern end of the traverse near 14+OOS. From the
limited data the anomaly is indicated to have a low intrinsic
chargeability and is associated with distinctly low resistivities.
The location of this chargeability feature correlates with MaxMin
zones HH and H supporting their validity as bedrock features.
In addition to the above described three chargeability zones on line
8+00E there are two additional possible but suspect weakly anomalous
features centered near 6+15S and 7+30S. There characteristics are
such as to be consistent with a very near surface source. In view
of the considerable thickness of overburden this would tend to place
them within the glacial overburden and hence unlikely to be of
exploration interest.
On grid D, the IP/resistivity surveys disclosed two significant
zones of lower resistivity and increased chargeability that can be
followed with some consistency from line to line. These features
are identified as zones S and T and in fact correlate with the Max-
Min zones of the same designation.
Zone S can be traced from line 78+OON in a east-northeasterly
direction as far as line 68+OON.
The zone is characterized by distinctly lower resistivities estimat-
ed to be in the range of 50-75 ohm-m and weakly to modestly anomal-
ous chargeabilities estimated to be in the range of 10-20 mse.cs at
depths of 40-45 m. Because of this depth the zone could in fact
- 65 -
represent a considerably narrower zone with much lower resistivity
and higher chargeability than is resolvable by the IP measurements.
The IP/resistivity features correlate closely with conductive zones
defined by the MaxMin survey on lines 78+OON and 76+OON.
However, on line 74+OON, where the MaxMin zone was tentatively in-
ferred to bend to the southeast, the IP/resistivity feature contin-
ues in an east-northeasterly direction. This latter trend is viewed
as geologically more plausible than the rather abrupt change in
orientation suggested by the MaxMin data.
The location of zone S is such as to suggest that it is a possible
continuation of the Casa Berardi break across the northwest corner
of the property. Consequently this feature is considered an :intri-
guing target for further evaluation.
Zone T is defined by low to moderate chargeabilities detected on
lines 78+OON and 76+OON near 1+OON. The anomaly may extend onto
line 74+OON but the IP traverse did not extend far enough south to
delineate this feature.
On line 66+00W there is a broad interval of variably weak to strong
chargeability accompanied by resistivity low north of the baseline.
This could represent an eastern continuation of zone T.
No distinguishable bedrock resistivity low is observed on lines
78+00W that might correlate with the MaxMin zone T, although there
is an apparent edge to an interval of quite conductive overburden
located somewhat south of the location of zone T.
Thus zone T is a weakly polarizable feature consistent with a low
tenor of disseminated sulphides. In view of the possible continua-
- 66 -
tion of the Casa Berardi break in this area, it to offers an intri-
guing target. However, a narrow conductor could be screened by the
conductive overburden; it is not firmly establishable whether or not
there is an equivalent resistivity low corresponding to the MaxMin
conductor.
Two additional points are worth noting with the respect to the data
on line 74+00W.
The first is that the IP traverse crossed a probable MaxMin overbur-
den anomaly near 4+00N. No chargeability response was detected
associated with this feature. There is, however, a decrease in
near-surface resistivities consistent with a localized conductive
overburden source.
The second point is that line 74+00W was surveyed with both dipole-
dipole and pole-dipole coverage. The pole-dipole survey results are
superior in terms of signal-to-noise and in terms of amplitude of
anomalous chargeability response. For this reason the remainder of
the survey was carried out with a pole-dipole array.
8.3 Discussion
The present geophysical results have been compiled with the results
of prior MaxMin and magnetometer surveys to yield the composite
geophysical picture portrayed on Map 1.
This portrayal aids geological correlation of certain long persist-
ent conductive horizons such as L, M and N as well as H, K and 0.
These conductor trends, it will be noted, are largely coincident
with accompanying magnetic trends.
- 67 -
A number of transverse faults have been interpreted based on disrup-
tions to conductors as well as associated magnetic features. It
should be noted that these faults have been modified both as to
location and orientation from faults previously interpreted solely
from the magnetic data.
The compilation also highlights the complementary character of
MaxMin HLEM and IP/resistivity in that zones S and T, otherwise only
tentatively identifiable as bedrock features, are now confirmed as
definite bedrock features.
-68-
9.0 REVERSE CIRCULATION DRILLING RESULTS
9.1 General
The average thickness of overburden was found to be approximately 78
ft with a maximum depth to bedrock of 180 ft in hole 01. Holes 73,
112 and 120 did not reach bedrock due to drilling problems. Forty-
three tricone bits were used for an average of 242.7 ft per bit
indicating good drilling conditions. Drill bit statistics can be
found in Appendix A.
9.2 Local Glacial Geology
Quaternary stratigraphy on the property consists of a lower till,
lower sediments, upper till and upper sediments capped by recent
swamp and muskeg deposits. Reverse circulation drill logs can be
found in Appendix D.
Lower till is generally best preserved in bedrock depressions where
it was sheltered from the later, overriding glacial advance. This
is well illustrated in Map 2 which presents cross-sections of glaci-
al stratigraphy. This till has a silty sandy matrix with abundant
cobble-sized clasts. Clasts seem for the most part to be locally
derived indicating intense scour of the up-ice bedrock surface.
This lodgement character provides an excellent sampling medium for
exploration purposes.
The bedrock depressions containing Lower Till generally correspond
to regional MaxMin conductors. These depressions reflect zones of
recessive weathering, probably related to sedimentary lithologies.
Contoured overburden depths shown on Map 1 illustrate this point.
The lower till unit is well developed in the trough coincident: with
MaxMin conductor H, as well as in other deeper pockets such as
around holes 112 and 113 in the north-central part of the property
and around holes 48, 45 and 56 along the edge of the Harricana
River.
-69 -
Lower sediments generally consist of gritty, hard-packed lacustrine
clays, silty sand and gravel and lie directly on top of Lower Tills.
These lower sediments are also best preserved in the bedrock depres-
sion areas mentioned above.
Upper or Matheson Till is found in all the holes but one. The till
is sandy, pebbly to gravelly and is highly variable in thickness and
overall composition as well as size and shape of clasts. Volcanic
clasts with minor sediments, granitics, iron formation, etc. com-
prise the major portion of this till. Minor amounts of Paleozoic
limestone fragments were noted, a characteristic of this till.
Clasts range from subangular to subrounded. Isolated lenses of
boulders and cobbles are also common to this unit. These are pro-
bably fluvial lag deposits marking former glacial stream channels.
Upper portions of this till sequence seem to represent variably
water sorted, mainly ablationary material melted out of wasting ice.
In lower sections of this till, it appears that a significant part
of the detritus was locally derived.
Upper sediments consist of a thick lacustrine clay unit along with
silty sands and gravel units. The clay is generally dark to light
grey, well floculated and relatively homogeneous. Although of
little use as a sampling medium, the lacustrine clay does provide a
capping which allows for good return of sample material during the
drilling process. The clay unit often grades downwards into a silty
sand and gravel unit. The absence of the silty sand unit generally
coincides with the presence of a bedrock high.
Overburden and bedrock geology results are summarized in Appendix
E.
-70-
9.3 Visual Gold Grains
A total of 333 gold grains was visually detected during processing,
273 of which were classed as abraded, 39 as irregular and 21 as
delicate (Table 2, Plate 1).
The largest grain, measuring 375 x 400 microns, was found in hole
30; the sample which contained this grain also contained 20% pyrite.
Hole 76 had the greatest amount of visible gold - 25 gold grains;
one sample in particular from this hole contained 13 gold grains.
9.4 Analytical Results - Overburden
9.4.1 Gold
Gold values in heavy mineral concentrates range from 5 ppb to
greater than 20,000 ppb with an average of 376 ppb. The
highest recorded analytical value of 78,000 ppb (sample 08,
hole 78) was cut to 34,286 ppb (1 oz/ton) for purposes of
statistical calculations. A "probably anomalous" threshold
for gold in heavy mineral concentrates was calculated to be
3,000 ppb while the same threshold for "equivalent" values
was 8.8 ppb Au (8,800 ppt Au).
All the samples exhibiting "probably anomalous" levels of
"equivalent" gold values are from holes in the central area
of the flexure.
The highest "equivalent" gold value is from sample H-86-120-
04. The value of 166.8 ppb was greatly enhanced by the con-
version to equivalent values. The analytical value for gold
in HMC for this sample was a "possibly anomalous" 2,720 ppb.
From an exploration point of view, hole 78 seems most signi-
ficant. The two basal samples were both classed as probably
anomalous. The basal sample, number 08, produced an equival-
- 71 -
TABLE 2
GOLD GRAIN SUMMARY
Hole Number Sample Au ppb
Gold Grains
Abraded Irregular Delicate
H-86-01-03, 03A, 04, 04A 1800 2 1 5 -07 450 1 -09, 09A 100 1 -11, 11A, 12, 12A 490 6 -13, 13A, 14 100 1
-03-03, 04 10 1 -07, 08 1050 6 1 -09, 10 95 1 -12, 12A 10 1
-04-01, 02 1125 1 -05, 06 1580 1 -11, 12 1030 5. 1
-05-03 625 1 -07-01, 02 180 1
-03, 04 210 1 -08-08 380 1 -09-01, 02 55 1
-08, 09, 09A 360 5 1 -10, 11 260 1 -12 3580 1
-10-01, 02, 02A 650 1 -11-03, 04 760 1
-05, 06 420 1 -12-01, 02, 03 2690 2 -18-02, 02A 800 1
-03 25 1 -19-01 450 2 -21-03, 04 250 1
-05 60 2 -22-01 75 1 -27-02 330 1 -35-01, 02 450 1
-03, 04 760 1 -08, 09 380 2 - 1
-36-02 170 1 -05 265 1 -01 120 1
- 72 -
TABLE 2 (cont'd)
GOLD GRAIN SUMMARY
Hole Number Sample Au ppb
Gold Grains
Abraded Irregular Delicate
H-86-39-01 1090 6 1 1. -04 100 3 1. -05 170 3
-40-02 390 2 -43-01, 02 205 1
-03 300 1 -45-01, 02 250 5 1. -49-01, 02 2930 1 -50-01, 02 240 1 -52-01A wash 330 1 -53-02 320 1
-03 120 3 , -04 560 1 -54-01, 02 135 6 -55-01 365 4 2
-02, 03 135 1 -05 540 1
-56-01 810 3 1 -02, 03 130 4 1 -04, 05 1670 7 1
-57-01 120 4 2 -02, 03 920 8
-59-02, 03 640 3 -60-01 55 8 -62-01A wash 150 1 -65-01 290 1
-01A wash 840 1 -70-01A wash 270 2 -71-02 375 1 -73-01, 02 140 1 -74-01 800 2
-02 400 2 -75-03, 04 115 3
-05 185 3 -1 -06 15 1 1 -07 30 2 2 -09 155
- 73 -
TABLE 2 (cont'd)
GOLD GRAIN SUMMARY
Hole Number Sample Au ppb
Gold Grains
Abraded Irregular Delicate
H-86-76-02, 03 30
N
r-+
r-r N
r+ .-a
.-.1 r-1 ri r
+ .--1
.--I r-I r-I 0
0 r-I ir1
r-1
/-.I 1--I ~
t r-+
\O N
r-I N
r-I r-I ,4
r-+ r-I r-I
r-I r1
r-1
.-1
-04, 05 165 3 -08 145 -09 195 2 2 -10 515 1
-77-01 170 -02 75 -04, 05 255
-78-01 310 -08 78000
-79-03, 04 410 -80-01 200
-02 170 -06, 07 250 1 1 -09 95 -10, 11 200 1 -13 700
-81-01, 02 185 -03 235 -04, 05 8100 -08, 09 50 -10, 11 280 1 -14, 15 560 2 -17 545
-82-04; 05 50 -07 140
-84-02 95 -03 45 -04 120 -09 100
-86-01 515 -02, 03 625
-91-02 415 -03 135
-92-01 220 -94-01A wash 160 -95-02 95 1 2
- 74 -
TABLE 2 (cont'd)
GOLD GRAIN SUMMARY
Hole Number Sample Au ppb
Gold Grains
Abraded Irregular Delicate
H-86-96-01A wash 140 1 -97-01 165 1
-03 140 1 -100-01 1145 1 -103-01 2000 1 -105-02 225 1 -107-02 340 1
-04 2095 1 -05 250 1.
-108-01A wash 1670 1 -110-01 295 2
-06 1380 1 -111-02 240 1 -112-03 1865 1
-06 450 2 -08 490 2 -10 350 1
-113-02, 03 3520 1 -11 20 2
-114-01, 02 175 1 -03 15 1 -08 140 2 1 1 -10 160 1 -11 5 4 -14 345 1
-115-03, 04 810 1 -05, 06 880 5 1 -07 160 6
-116-01 135 1 -02 120 1 -04 110 1 -05 15 1 -10 550 1 -14 35 1 -15 130 2 1
-118-01 1r3î 1 -03 20 1 -14 165 1
- 75 -
TABLE 2 (cont'd)
GOLD GRAIN SUMMARY
Hole Number Sample Au ppb
Gold Grains
Abraded Irregular Delicate
H-86-119-01 15 1 -120-04 2720 1
-06 45 1 -121-05 350 1 -122-10 70 2 -123-02 120 1 -124-11 5660 1
-17 100 1
-76-
Plate 1: Gold grains in sample H-86-80-06, 07
Note: Large grain measures 200 x 275 microns
- 77 -
ent value of 40,336 ppt while the sample above produced a
value of 9,243 ppt.
The single sample hole H-86-85 produced a probably anomalous
equivalent gold value of 9,667 ppt. Conversion to equival-
ents highlighted this sample since the original analytical
value was an elevated background value of 300 pbb.
Hole H-86-115, sample 08, at about mid-depth in the hole, has
a probably anomalous equivalent gold value of 20,640 ppt.
This value appears to correspond with the 6 visible gold
grains detected in the sample.
Hole H-86-12 sample 11, at about mid-depth in the hole, has a
probably anomalous equivalent value of 24,427 ppt Au.
It should be noted that virtually none of the anomalous gold
values has obvious correlation with any of the other ele-
ments. This would imply a gold-only source for the grains
i.e. gold-quartz (+ pyrite) lode mineralization, rather than
massive sulphide type mineralization, e.g. Estrades deposit.
9.4.2 Arsenic
Arsenic values in heavy mineral concentrate range from 4 ppm
to greater than 2,000 ppm with an arithmetic mean of 352 ppm.
The highest recorded values (those greater than 2,000) were
cut to 2,000 ppm for statistical purposes. A "probably
anomalous" threshold for arsenic in heavy mineral concentrat-
es was calculated to be 1,300 ppm As (8.2 ppm As "equival-
ent").
- 78 -
The highest equivalent arsenic value is 47,104 ppt from
sample H-86-120-04 in the central flexure zone. This sample
was taken in the mid/upper region of hole 120.
From an exploration point of view, hole 39 is probable the
most interesting in terms of arsenic content. The bottom two
samples in this hole produced probably anomalous equivalent
arsenic values. The hole was drilled in a bedrock depression
down-ice from conductor P. Twenty to twenty-five percent
pyrite was also observed during the processing of these
samples.
A zone of elevated arsenic background is developed in tills
in the north-central part of the project area around holes
93, 94, 95, 96, 97, 98, 99, 100, 102, 103 and 104. Calcula-
tion of equivalent values reduced the significance of this
area somewhat by lowering some values. For example, sample
H-86-95-03 with a possibly anomalous value of 1,040 ppm was
reduced to an elevated background equivalent value of 4,452
ppb.
A second area where elevated arsenic values are located is in
the central flexure zone. Holes 75, 76, 79, 84, 114, 116,
117, 118, 119, 120, 121 and 122 produced elevated background
or higher values. Holes 118 and 116 were most noticeable
with several values in high background to anomalous ranges.
Samples that are considered probably anomalous within the
above zone include:
H-86-118-11 11,789 ppt
H-86-118-18 11,967 ppt
H-86-119-01 10,140 ppt
H-86-120-01 9,741 ppt
- 79 -
Hole 60, sample 01, which is down-ice from conductor J, con-
tained the probably anomalous equivalent value of 10,577
ppt.
Conversion of values in HMC to equivalents greatly enhanced
some arsenic values. Sample H-86-118-18 with an elevated
background value of 1,216 ppm As produced a probably anomal-
ous equivalent value of 11,967 ppt.
9.4.3 Copper, Zinc, Silver
Copper values ranged from 16 ppm to 2,600 ppm. A "probably
anomalous" threshold for copper was calculated as 560 ppm in
HMC and 4,500 ppb as an equivalent value.
Zinc values ranged from 13 ppm to 2,500 ppm. A probably
anomalous threshold for zinc was calculated as 480 ppm in HMC
with a corresponding equivalent value threshold of 1,800
ppb.
Silver values ranged from 0.05 to 6.8 ppm. A probably anoma-
lous threshold was calculated as 1.5 ppm in HMC with a
corresponding equivalent value threshold of 6.8 ppb.
Sample H-86-04-13 produced the highest copper and zinc values
as well as a probably anomalous silver value. A value of
16,000 ppt Cu, 15,384 Zn and 17.3 Ag makes this sample very
interesting from an exploration point of view, since the hole
was drilled directly down-ice from conductor H. This sample,
however, appears to have contained a substantial amount of
bedrock material. Bedrock in this hole was extremely soft
and behaved as overburden material during the drilling
process.
Calculation of equivalent values greatly enhanced some base
metal values down-ice from conductor H. Sample H-86-119-01
- 80-
TABLE 3
SUMMARY STATISTICS ANALYTICAL RESULTS
REVERSE CIRCULATION TILL SAMPLES
Element No. Samples
Arith Mean
Stnd Dey
Geom Mean
Stnd Dey
Min Max
Au (ppb) 454 376.03 1,724.33 125 .85 3.76 2.5 34,2861 eAu (ppt) 454 1,384.14 8,231.28 397.80 3.98 5.97 166,826.67 Ag (ppm) 454 0.37 0.48 0.21 ' 3.13 0.05 6.8
eAg (ppb) 454 1.36 2.05 0.65 3.60 0.03 21.27 As (ppm) 450 351.58 310.49 225.67 3.01 4.00 2,000 eAs (ppb) 450 1,418.09 2,729.87 720.62 3.53 11.59 47,104 Cu (ppm) 454 150.47 199.01 116.40 1.88 16.00 2,600 eCu (ppb) 454 607.66 1,153.28 367 .93 2.43 15.80 16,000 Zn (ppm) 454 84.13 160.35 56.90 2.04 13.00 2,500 eZn (ppb) 454 323.96 853.46 179.84 2.51 14.82 15,384.62 Non-mag (µg/g) 454 3,885.69 5,040.69 217.95 65,333.33
Mag (µg/g) 453 2,764.28 3,338.7 133.33 45,866.67
1 - maximum cut to 34,286 ppb
- 81 -
with values of 0.3 ppm silver, 246 ppm copper (elevated back-
ground) and 120 ppm zinc (elevated background) produced pro-
bably anomalous equivalent values of 12.3 ppb silver, 10,059
ppb copper and 4,907 ppb zinc, a reflection of the above ele-
vated values in large HMC samples.
9.5 Analytical Results - Bedrock
For the most part, values for Au, Cu, Zn, Ag and As are within back-
ground levels on the property.
Hole 100, 101, 102, 104, 108, 16, 15, 18, 19, 21, 24, 111, 72, 70
and 19 in t:he north-central part of the property and holes 124„ 123,
119, 118, 120, 113, 77, 80 and 74 in the central flexure zone dis-
play elevated arsenic values.
Elevated background gold values are present in hole 81 within the
central flexure zone.
9.6 Discussion
The bulk of the gold grains are of the abraded, i.e. long travelled
variety. Gold grains are also relatively well dispersed throughout
the two till sections. The suggestion is that much or most of the
abraded grains in the upper clastics have simply been re-cycled from
the lower tills. There are no markedly anomalous gold grain concen-
trations in the basal portions of any of the holes. This is not en-
couraging since reverse circulation drill holes were located immedi-
ately down-ice or intended to penetrate directly into MaxMin conduc-
tive zones. Under these conditions, the most encouraging results
would consist of an abundance of delicate gold grains at t:he base of
the holes (assuming that trills are of local derivation and any gold
deposits are in the immediate conductive environment). Because of
the abraded nature and irregular dispersion of gold grains it :is our
opinion that these grains were generally not derived from conductors
that the holes were intended to test.
- 82 -
TABLE 4
CALCULATED THRESHOLDS REVERSE CIRCULATION TILL SAMPLES
Element "Elevated" Threshold
"Possibly Anomalous" Threshold
"Probably Anomalous" Threshold
Au 160 ppb 1500 ppb 3000 ppb eAu 550 ppt 4200 ppt 8800 ppt Ag 0.3 ppm 1.1 ppm 1.5 ppm eAg 1.0 ppb 4.5 ppb 6.8 ppb
As 330 ppm 1000 ppm 1300 ppm eAs 1000 ppb 4400 ppb 8200 ppb Cu 135 ppm 330 ppm 560 ppm
eCu 500 ppb 2000 ppb 4500 ppb
Zn 60 ppm 260 ppm 480 ppm eZn 190 ppb 1000 ppb 1800 ppb
- 83 -
TABLE 5
SUMMARY STATISTICS
BEDROCK TRACE ELEMENT ANALYSES
Element1 No. Sample
Arith Mean
Stnd Dey
Geom Mean
Stnd Dey Min Max
Al(%) 125 2.65 2.1 1.79 2.7 0.13 9.37 K(Al)2 0.18 0.14 0.01 0.62 Fe3(%) 125 9.26 6.26 7.82 1.75 1.62 34.02 K(Fe3) 1.29 0.88 0.23 4.76 Mg(%) 125 5.42 3.78 4.07 2.29 0.32 17.32 K(Mg) 1.55 1.08 0.09 4.97 Ca(%) 125 2.74 1.9 2.33 1.75 0.43 14.06 K(Ca) 0.65 0.45 0.10 3.35 Na(%) 125 0.13 0.07 0.11 1.93 0.01 0.38 K(Na) 0.04 0.02 0 0.12 K(%) 125 0.11 0.08 0.08 2.51 0.01 0.31 K(K) 0.04 0.02 0 0.1 Ti(%) 125 0.04 0.07 0.02 1.93 0.01 0.44 K(Ti) 0.45 0.82 0.10 5.24 P(%) 125 0.12 0.05 0.11 1.63 0.02 0.36 K(P) 0.53 0.23 0.09 1.56 Mn(%) 125 0.15 0.12 0.12 1.9 0.04 0.82 K(Mn) 1.31 1.06 0.31 7.05 Cr 125 79.11 165.26 32.04 4.49 1 14.97 K(Cr) 0.4 0.83 0.01 7.49 Sr 125 91.1 90.05 55.29 3.1 0.5 444 K(Sr) 0.26 0.26 0 1.29 Ba 125 30.73 30.99 21.72 2.41 2 300 K(Ba) 0.07 0.07 0 0.69 W 125 8.7 57.62 2.07 2.79 1 640 K(W) 8.7 57.62 1 640 U 125 7.61 4.05 6.82 1.56 5 21 K(U) 2.54 1.35 1.67 7 Th 92 2.63 1.92 2.05 2.02 1 8 K(Th) 0.26 0.19 0.1 0.8 Cu 125 47.41 26.31 39.54 1.97 3 145 K(Cu) 0.79 0.44 0.05 2.42 Zn 125 90.9 107.41 73.07 1.79 18 1141 K(Zn) 1.3 1.54 0.26 16.32 Pb 125 8.97 5.19 7.52 1.88 1 26 K(Pb) 0.56 0.32 0.06 1.63 Ni 125 64.25 59.22 48.61 2.2 3 500
- 84 -
TABLE 5 (cont'd)
Elementl No. Sample
Arith Mean
Stnd Dev
Geom Mean
Stnd Dev Min Max
K(Ni) 0.8 0.74 0.04 6.25 Au(ppb) 125 2.54 5.2 1.69 1.98 1 50 K(Au) (ppb) 0.64 1.3 0.25 12.5
Ag 125 0.2 0.14 0.17 1.63 0.1 1.4 K(Ag) 2.86 2.02 1.43 20.01 As 125 32.35 85.44 13.25 3.17 2 760 K(As) 16.18 42.75 1 380 Co 125 22.62 36.27 16.98 2.0 1 407 K(Co) V 125 42.05 41.79 28.17 2.59 0.5 213 K(V) Sb 125 5.77 8.41 3.61 2.26 2 50 K( Sb) 11.54 16.81 4 100
1 - all values in ppm unless otherwise noted. - major elements (e.g. Al, Fe, Mg, etc.) as oxide equivalents.
2 - Clarke normalized values. Clarke indexes after Rickwood, 1983.
-85-
TABLE 6
SUMMARY STATISTICS
HEAVY MINERAL CONCENTRATES FROM BEDROCK SAMPLES
Element No. Samples Mean Stnd Dey Min Max
Au 6 59.58 101.51 2.5 265 Ag 6 2.24 2.93 0.05 6.4 As 6 560.67 733.5 31 2000 Cu 6 1833 2270.94 44 5800 Zn 6 1903.67 3049.04 20 8000 Nm 6 6551.86 7683.07 1103.45 18764.71 Mag 6 661.14 447.63 22.99 1294.12
- 86 -
Most of the gold encountered in the reverse circulation drilling on
the property is located within the trough of the central flexure
zone. Holes within the central flexure zone containing abundant
gold include holes 08, 75, 76, 77, 78, 79, 80, 81, 84, 113, 116 and
118. Gold is found in both of the till sheets present in this area.
Gold does not appear to be preferentially located within either of
the two till sheets nor does the nature of the gold grains (i.e.
abraded, irregular, delicate) vary significantly between the tills.
The gold found in the deepest portions within the lower till unit is
probably derived from the northeast. Gold grains found within the
upper till (Matheson) in mid to upper portions of holes are probably
derived from the northwest and in part due to a reworking of the
older, lower till unit.
Some of the gold within the Matheson till in the central flexure
zone may, in part, emanate from the source(s) of IP anomalies here.
This is, however, not strongly supported considering the widely
dispersed, abraded nature of most of the gold.
The reason that most of the gold found on the property is located
within the central flexure may be in part due to the fact that in
the trough area one might expect more background gold grains because
of a greater volume of till. In addition, more holes were drilled
in this area than any other and as such we may be seeing more gold
simply because of greater hole density. The presence of gold grains
in two separate till sheets is also contributing to the relative
abundance of grains in this area.
Other areas with significant amounts of gold include hole 39 down-
ice from conductor P and hole 56 on the edge of the Harricana River.
It is interesting to note that in these areas those holes with
significant amounts of gold were also drilled into bedrock depress-
ions.
- 87 -
There are higher than normal arsenic values in bedrock in both the
north-central part of the property and the central flexure zone,
where tills also have higher than normal arsenic values. These ele-
vated bedrock values are probable contributing directly to the
anomalies in till. Elevated arsenic values in basal tills may also
be reflecting arsenic content within the up-ice MaxMin conductive
zones.
A number of statistically anomalous base metal values is noted in
basal tills down-ice from conductor H. High base metal values were
found in basal tills of holes 04, 81 and 119. Conductor H is the
most probable source for these metals. Holes 120 and 122 immediat-
ely down-ice from conductor R as well as conductor H also show
anomalous base metal values. Other anomalous base metal values in
the central flexure zone include holes 84, 85 and 119. A number of
isolated anomalous base metal values are also noted in several other
areas on the property, also down-ice from MaxMin conductors. It is
not atypical that regional EM conductors may contain concentrations
of base metals sufficient to produce anomalous values in heavy min-
eral concentrates. The base metal values do not appear to be relat-
ed to anomalous gold concentrations and are thus not considered im-
portant in the present gold exploration context. There may be some
significance in a base metals exploration program.
-88-
10.0 CONCLUSIONS AND RECOMMENDATIONS
The results of the geophysical surveys and reverse circulation drilling
have substantially augmented previous magnetic surveys and geologic in-
formation. The compiled data indicate a mixed sedimentary/volcanic en-
vironment containing a number of banded iron formations and regional con-
ductors, a setting analogous to that hosting gold deposits within other
portions of this sector of the Abitibi.
The six probable to definite bedrock conductors on Grids A/AA, C and D
and the seven additional possible bedrock conductors partially to wholly
delineated by the MaxMin surveys constitute favourable exploration tar-
gets in this geological setting.
The selective IP/resistivity coverage has confirmed several weak MaxMin
conductors as definite bedrock features likely reflecting a modest tenor
of sulphides or graphite. In particular zone S or T on Grid D in the
northwest: corner of the property may reflect a continuation of the so
called "Casa Berardi Break".
The reverse circulation drilling, directed in part at the above geophysi-
cal targets, encountered a glacial strat:igraphic section typical of this
portion of the Abitibi consisting of upper Matheson tills of generally
ablationary character overlying lower lodgement tills where the latter
are locally preserved in bedrock depressions. We consider these tills to
be generally suitable exploration media for the effective utilization of
the reverse circulation drilling technique.
The reverse circulation drilling encountered gold grains in the glacial
tills in considerable abundance, particularly in the bedrock depression
marking the central flexure zone. The presence of visible gold is
supported generally by anomalous gold analyses.
- 89 -
The generally abraded character of gold grains and their distribution in
both upper and lower till sheets suggests source area(s) distant from the
property. There are no distinct gold dispersion trains emanating from a
substantial bedrock source within the present property boundary based on
the reverse circulation data. High equivalent gold values at the base of
hole 78 are interpreted by us to represent a nugget effect.
Conversion of raw gold values to equivalents has proved extremely useful
in enhancing the significance of certain samples. Likewise, certain
erratic nugget effect values have been substantially depressed via the
equivalent calculation.
Anomalous base metals encountered in heavy mineral concentrates of basal
tills are probably derived from regional electromagnetic conductors im-
mediately up-ice from the reverse circulation drill holes, suggesting a
potential for base metal mineralization on the property, athough these
values may also simply reflect increased background base metal endowments
within these conductors, a situation fairly common in the Abitibi. The
sample which returned the highest copper and zinc values in heavy mineral
concentrates (sample H-86-04-13) probably included a significant portion
of bedrock material.
Slightly elevated arsenic values do not indicate a distinct source or
alteration pattern. The source of high arsenic values at the base of
hole 39 is probable conductor P.
Based in large part on the preceding results, a diamond drilling program
is currently underway. These results should be integrated into the
existing exploration data base to determine if any changes to the fore-
going interpretation are warranted, particularly with respect to the geo-
chemical aspects.
-90-
More complete geophysical coverage may be helpful in identifying
additional targets. In particular, additional IP surveys to confirm the
possible targets on Grid C are merited.
Respectfully submitted,
, o-'& , s o
J.P. Rollinson, B.Sc.
J. Roth, M.A.
CITED AND MISCELLANEOUS REFERENCES
Averill, S.A., 1984, The Nugget Problem in Till Gold Exploration - Paper
10; Till Tomorrow '84 Symoposium, Kirkland Lake, Ontario.
Averill, S.A. and Zimmerman, J.R., 1986, The Riddle Resolved: The Dis-
covery of the Partridge Gold Zone Using Sonic Drilling in Glacial
Overburden at Waddy Lake, Saskatchewan; Can. Geol. Jour of CIMM,
volume 1, no. 1, pp. 14-20.
Bending, D., 1985, Summary Report, Joutel Concept Test, January and •
February, 1985.
Beus, A.A. and Grigorian, S.V., 1977, Geochemical Exploration Methods for
Mineral Deposits, Applied Publishing 287 p.
Brereton, W.E. and Elson, J.A., 1979, A Late Pleistocene Plant-bearing
deposit in Currie Township, near Matheson, Ontario; Can. Jour. Earth
Sci. v. 16, no. 5, pp. 1130-1136.
Brundin, N.H. and Bergstrom, J., 1977, Regional Prospecting for Ores
based on Heavy Minerals in Glacial Till; Jour. Geochem. Explor., v.
7, pp. 1-19.
Boyle, R.W., 1979, The Geochemistry of Gold and its Deposits; Geol. Surv.
Canada, Bull. 280, 584 p.
DiLabio, R.N.W., Newsome, J.W., and Mclvor, D.F., 1985, Gold Spheres in
Surficial Sediments; Episodes, v. 8, No. 139.
DiLabio, R.N.W., 1982, Gold and Tungsten Abundance vs. Grain Size in Till
at Waverley, Nova Scotia; in Current Research, Part B, Geol. Survey
Canada, Paper 82-1B, p. 57-62.
Dreimanis, A., 1976, Glacial Tills: Their Origin and Properties; Royal
Soc. Canada, Spec. Publ. no. 12, pp. 11-49.
- 2 -
Eriksson, K., 1976, Heavy Metals in Different Till Fractions; Jour.
Geochem. Explor . , v. 5, pp. 383-387.
Flint, R.F., 1971, Glacial and quaternary Geology: John Wiley and Sons,
Inc., Toronto, 825 p.
Fortescue, J.A.C., 1983, Geochemical Prospecting for Gold in Ontario, p.
251-271; in The Geology of Gold in Ontario, edited by A.C. Colvine,
Ont. Geol. Survey, MP 110, 278 p.
Garrett, R.G., 1971, The Dispersion of Copper and Zinc in Glacial Over-
burden at the Louvem Deposit, Val d'Or, Quebec, C.I.M. Spec. Vol.
11, p. 157-158.
Geddes, R.S. and Kristjansson, F.J., 1986, Quaternary Geology of the
Hemlo Area: Constraints on Mineral Exploration; Can. Geol. Jour of
CIMM, v. 1, no. 1, pp. 14-20.
Gray, R.S., Tracing Reverse Circulation Gold Anomalies to their Source -
Paper 14; Till Tomorrow '84 Symoposium, Kirkland Lake, Ontario.
Harron, G.A., Middleton, R.S., Durham, R.B. and Philip, A., "Geochemical
and Geophysical Gold Exploration in the Timmins Area, Ontario: A
Case History" Paper 11; Till Tomorrow '84 Symoposium, Kirkland Lake
Ontario.
Hornbrook, E.H.W., Davenport, P.H. and Grant, D.R., 1975, Regional and
Detailed Exploration Studies in Glaciated Terrain in Newfoundland;
Dept. Mines and Energy Nfld., Report 75-2, 116 p.
3
Knight, J. and McTaggart, K.C., 1986, The Composition of Placer and Lode
Gold from the Fraser River Drainage Area, Southwestern British
Columbia; Can. Geol. Jour of CIM v. 1, no. 1, pp. 21-30.
Lee, H.A., 1963, Glacial Fans in Till from the Kirkland Lake Fault: A
Method of Gold Exploration; Geol. Survey Canada, Paper 63-45, 36 p.
Mann, A.W., 1984, Mobility of Gold and Silver in Lateritic Weathering
Profiles: Some Profiles from Western Australia; Econ. Geol., v. 79,
pp. 38-49.
Nichol, I. and Bjorklund, A., 1973, Glacial Geology as a Key to Geoc:hemi
cal Exploration in Areas of Glacial Overburden with Particular Re-
ference to Canada; Jour. Geochem. Explor., v. 2, pp. 133-170.
Peuraniemi, V. and Heinanen, K., 1985, Mineralogical Investigations in
the Interpretation of Heavy Mineral Geochemical Results from Till;
Jour Geochem. Explor., v. 23, p. 315-328.
Prest, V.K., 1970, Quaternary Geology of Canada; Geol. Surv. Canada,
Econ. Geol. Report 1, pp. 676-764.
Sauerbrei, J.A., Pattison, E.F. and Averill, S.A., 1985, Till Sampling in
the Casa Berardi Area, Quebec, A Case History in Orientation and
Discovery; Paper Presented at the 11th Geochemical Exploration
Symposium, Toronto, April 30, 1985.
Shilts, W.W., 1984, Important Principles and Recent Research in Drift
Prospecting Paper 1; Till Tomorrow '84 Symoposium, Kirkland Lake,
Ontario.
4
Shilts, W.W., 1976, Glacial Till and Mineral Exploration; Royal Soc.
Canada, Spec. Publ. no. 12, pp. 205-224.
Shilts, W.W., 1973, Glacial Dispersal of Rocks, Minerals and Trace
Elements in Wisconsinan Till, Southeastern Quebec, Canada; Geol.
Soc. Am., Mem. 136, pp. 189-219.
Smee, B.W., 1983, Laboratory and Field Evidence in Support of the Ele-
ctrogeochemically Enhanced Migrations of Irons through Glacio•-lacu-
strine Sediment; 9 IGES Program with Abstracts, pp. 25.26.
Sopuck, V., Schreiner, B. and Averill, S., 1985, Drift Prospecting for
Gold in Saskatchewan; Paper Presented at CIMM Symposium "Gold in the
Western Shield", Saskatoon, Sask., September, 1985.
Szabo, N.L., Govett, G.J.S. and Lajtai, E.Z., 1975, Dispersion Trends of
Elements and Indicator Pebbles in Glacial Till Around Mt. Pleasant,
New Brunswick, Canada; Can. Jour. Earth Sci., v. 12, pp. 1534-1556.
Theobald, P.K. Jr., 1957, The Gold Pan as a Quantitative Geologic Tool:
USGS Bull. 1071-A, 54 p.
Webster, J.G. and Mann, A.W., 1984, The Influence of Climate, Geomorphol-
ogy and Primary Geology on the Supergene Migration of Gold and
Silver; Jour Geochem. Explor., v. 22, pp. 21-42.
Zantop, H. and Nespereira, J., 1978, Heavy Mineral Panning Techniques in
the Exploration for Tin and Tungsten in Northwestern Spain, p.
329-336; in Geochemical Exploration 1978 ed. J.R. Watterson, P.K.
Theobald, Proceedings of the Seventh International Geochemical
Exploration Symposium, 504 p.
MINERALOGICAL AND TEXTURAL FEATURES, JOUTEL PROJECT OVERBURDEN SAMPLES
On behalf of David A. Bending
Homestake Mineral Development Company
Graham Wilson Turnstone Geological Services Ltd
P.O. Box 130, Station 'B', Toronto M5T 2T3
10 August 1986
ABSTRACT
Rock chippings from reverse circulation drilling program are dominated by variably carbonatized and silicified mineral assemblages, tentatively identified as metavolcanics and (in part volcaniclastic) metasediments. Samples are generally fairly well-sorted, all but one being dominated by one lithology visually estimated to comprise 90 percent or more of the chips. Quartz-carbonate veining is the most consistent minor component in the suite. Small amounts of relatively fresh intermediate-basic extrusives and intrusives also occur, as do traces of granitic rocks. Feldspars are present in rock-forming proportions in two samples, and as minor constituents in four others. Sericitization is the main form of feldspar alteration, with minor kaolinization and (possibly) albitization. Tourmaline was found as a rare trace in one sample only (Descr. 303), and significant quantities of sulphide (pyrite) occurred in only one sample (Descr. 310). With the exception of the two feldspathic samples, the suite is dominated by quartz, carbonate(s) and fine-grained sericitic white mica. Apart from mica-defined foliations, features indicative of substantial deformation are not prominent. Common brittle fractures are largely occupied by thin quartz-carbonate veins. Two samples (Descr.306,310) exhibit pressure shadows on equant, brittle substrate grains. The metamorphic grade is lower greenschist facies.
rriilbainro cl dUS ÎivsccurccS Service de la Géoinformation
; Date: 2 7 An. me1 No G.M.:
TurnsTone Geological Services Limited
METHODOLOGY
The relative importance of descriptions of textures (as opposed to mineral
species) is higher for these chip samples than for regular, single-slice
sections. This is reflected in the detailed descriptions; less is said
under the mineral listings, and emphasis is placed on the textures displayed
and lithological identifications. Textures are numbered in decreasing order
of abundance. In rarer types (say <5% of chip area) there is often
insufficient material for a complete optical description of each species,
e.g. igneous fragments in H86-08-10 (Descr. 304).
Individual rock chips are up to 9x3 mm in cross-section, falling mostly
in the 3-5 mm range, except for 86-78-09 (Descr. 308), in which the chip
sizes are 1-3 mm. A glossary of petrographic abbreviations is enclosed.
LITHOLOGIES
The rock types and the bulk mineralogy are summarized in Table 1. Further
notes on rock names and textures can be rapidly gleaned from the 'Summary'
and 'Texture' sections of each of the appended detailed descriptions (nos.
303-311).
MINERALOGY
Mineralogical data is summarized in Table 1. The limited quantities of
grains available in, some mounts limits the optical determination of some of
the phases, such as plagioclase. All mounts, with the exception of no. '88'
(Descr. 305), effervesced mildly in cold dilute hydrochloric acid.
Carbonates are ubiquitous, and are not satisfactorily identified by this
simple test, especially in the mounted format.
REFERENCES
In lieu of site-specific references, an annotated bibliography for the
Abitibi Belt in Quebec is placed at the end of this report.
TABLE 1; MINERALOGY AND ROCK TYPES OF NINE JOIITEL SAMPLES
Mineralogy Lithology
Sample Qz Feld Musc Bi Chl Amph Tour Epi Carb Ore Various MVo MSe QCV Int Descr.
H86-06-03 10 54 6 - - - Tr. - 30 Tr. - 95 - 5 - 303
H86-08-10 90 Tr. 5 Tr. Tr. Tr. - Tr. 5 Tr. - 3 90 6 1 304
H86-76-12 50 - 15 - - - - - 35 Tr. - 98 2 - 305
H86-77-06 25 48 18 - - - - - 7 2 Ap Tr. 97 3 - 306
H86-79-06 35 - 14 - Tr. - - - 50 1 - 95 - 5 - 307
H86-78-09 33 1 20 - Tr. Tr. - Tr. 45 Tr. Ctold I,Sph Tr. 93 - 2 5 308
H86-80-14 74 1 10 - Tr. Tr. Tr. 14 1 Px Tr.,Sph Tr. 97 - 2 1 309
H86-81 -20 85 Tr. 4 - - - - 6 5 - 47 - 52 1 310
H86-82-09 52 - 13 - - - - - 35 Tr. - 98 - 2 - 311
N.B.; 1. Feld = All feldspars; plus alteration products, such as ser.
2. Ore - all 'opaques'.
3. Ctold = chloritoid.
4. Tentative identifications of rock type (primary rock type, ln case of strong superposed alteration). Visually estimated proportions of different lithologies. MVo, MSe and QCV; metavolcanics, metasediments (incl. volcaniclastic deposits), quartz-carbonate veins. Int; acid and basic intrusives.
GLOSSARY OF ABBREVIATIONS USED IN PETROGRAPHIC DESCRIPTIONS
Dr Graham Wilson, Turnstone Geological Services Ltd, Box 130, Station "B", Toronto, Ontario M5T 2C0 CANADA
Glossary begun June 1984, Revision 29 October 1985.
The following are often obvious, but for the record most of the abbreviations used are given below, with some additional notes on the procedure used. This system is being evolved for detailed, standardised descriptions, and can be applied to handwritten or computer-based formats. For an example of a'very rigid, coded format (conceived for handling large numbers of samples on now-obsolete computer card input) see McRitchie (1969).
Colour; bl blue 5rn brown grn green or orange yl yellow etc
General; anh anhedral assoc associated balsam mounting medium; balsam or glue of similar RI.
eff in HC1 effervescence in (cold) dilute (10%) hydrochloric acid
EDS energy-dispersive spectrometry (of EPM) EPM electron microprobe analysis euh euhedral max maximum min minimum -el relatively (or 'relief'; discontinued) WDS wavelength-dispersive spectrometry (of EPM) staining Kfeld staining involves the HF - sodium cobaltinitrate
test (see e.g. Solar and Fahey 1972, Hayes and Klugman 1959), leaving a bright yellow colouration on the feldspar. For carbonate staining a variety of methods can serve to distinguish e.g. calcite, dolomite, ankerite and magnesite, the most important carbonates to differentiate when outlining gold-related alteration assemblages. See
the paper by Friedman (1959). symm symmetric(ally) tr trace
Grain size; dia diameter (v)cgr (very)coarse-grained mgr medium-grained fgr fine-grained
gs grain size
mm
1 mm-0.03937 inch um
1 micron-0.001 mm
Minerals; ab albite amph amphibole an anorthite ap apatite asp arsenopyrite cal calcite carb carbonate chalc chalcopyrite chi chlorite clzo clinozoisite cord cordierite cpx clinopyroxene cumm cummingtonite di diopside dol dolomite epi epidote gar garnet grp graphite hb hornblende hem hematite hyp hypersthene ilm ilmenite Kfeld alkali feldspars;orthoclase,microcline,sanidine.. lim limonite mag magnetite moly molybdenite musc muscovite neph nepheline oliv olivine opx orthopyroxene pent pentlandite plag plagioclase feldspar py pyrite pyrr pyrrhotite qz quartz rieb riebeckite rut rutile serp serpentine tour tourmaline ves vesuvianite woll wollastonite zir zircon zo zoisite
Miscellaneous; QAM quartz-ankerite-mariposite rock (Mother Lode)
Mode.; A rough visual estimate. Accessory phases <1Q are annotated 'Tr.'
(trace). An attempt is made to counteract the common tendency to
overestimate the frequency of the dark phases. Minerals are described in
order of decreasing modal abundance.
Optical Properties; bin birefringence - relative retardation is often written
shorthand,e.g. 1st-o yl = first-order yellow. The
maximum birefringence is estimated from the thickness (calculated from colours of dependable minerals, such as quartz) and the highest colours observed in the section.
birl bireflectance ext extinction. May be 'str' (straight, parallel to length)
or 'clean', meaning that the whole grain goes dark at once, c.f. strained quartz, for instance.
int interference MEA Specifically, Maximum Extinction Angle (degrees) in the
Michel-Levy test for plagioclase composition. Where available, a minimum of 6 suitable grains is used. ^.7A is also used of EA in other minerals.
LF/LS orientation: length fast/slow
Pleo pleochroism PPL plane polarized light
refl reflectance RI refractive index RL reflected light
ST sensitive tint plate, for determination of orientation and of optical sign.
TL transmitted light XP cross-polarized light; usually with exact alignment of
polarizer and analyser. In RL one is sometimes rotated a few degrees in order to emphasise anisotropy bireflectance. Some properties, such as pleochroism and relief, are described with respect to the orientation of the polarizer (the phrase 'vibration plane cf the lower nicol' is equivalent to the polarizer).
For optical properties in reflected light 'see Craig and Vaughan (1981), which tabulates about 100 opaque minerals. Properties such as scratch and polishing hardness, bireflectance and reflection pleochroism are also briefly discussed (ibid. pp.36-43).
Photomicrographs and figures; Colour Photomicrographs are made by either a)using
daylight-balanced colour film and a blue filter, or b)using film balanced for tungsten lighting, without a blue filter. Photos taken in RL may thus have bluish-grey backgrounds (method (a), preferred) or brownish backgrounds (method (b), used in many of the earlier descriptions). Slide film is used for maximum flexibility, and for quality control; two or more exposures are made per subject due to high rejection rates, and use of negative film would result in an expensive number of unwanted prints at this stage.
FOV field of view in mm (long axis of photo); the primary scale indicator, as magnification (for a given FOV) is dependent on equipment used. FOV is approximate; prints often show only 95% of so of the FOV on the original transparency. Quoted FOV may sometimes be further reduced by extra enlargement and/or cropping of the print.
Sample format; CTS covered thin section, nominal thickness 30um (D)PTS(C) (doubly-) polished thin section (C=>circular, in 25mm dia.
form for microprobe work; some rectangular PTS are also microprobe-compatible). Suitable for reflected light study. For the purpose of high-current ion beam analysis, only, such glass-backed mounts may be made up with a thickness of about 500um or more; 'ThPTS(C)'.
PM polished mount, for reflected light microscopy, also microprobe-compatible unless qualified.
Thickness gauged by quartz interference colour in quartzose sections. Excludes the slide margins, which commonly taper somewhat.
References;
Craig,JR and Vaughan,DJ (1981) Ore Microscopy and Ore Petrography. Wiley-Interscience, 406pp.
Friedman,GM (1959) Identification of carbonate minerals by staining methods. J.Sed.Petrol. 29, 87-97.
Hayes,JR and Klugman,MA (1959) Feldspar staining methods. J.Sed.Petrol. 29, 227-232.
McRitchie,WD (1969) A petrologic data sheet for use in the laboratory. Geol.Surv.Manitoba Geol.Pap. 1/69, 8pp.
Sclar,CB and Fahey,JJ (1972) The staining mechanism of potassium feldspar and the origin of hieratLt'e. Amer.Mineral. 57, 287-291.
TURNSTONE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-06-03 (mount '85') Description; 303 Client/job ; Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format ; CTS, Geoplastech, TO - 25-30um
Hand specimen data; one epoxy mount of drill chippings. White siliceous fragments with variable (nil to strong) ironstaining.
Major Minerals; * Plagioclase and alteration products; relatively cgr (max gs 2.Ox1.3mm), albite-twinned, with dominant flaky sericitic alteration. Ser shows 1st-o yl interference colours. Also minor alteration / replacement by granular carb and vfgr turbid kaol. Phenocrysts and smaller shards. Sometimes as 6-sided euh sections, sometimes with clear signs of zoning. M-L MEA (4 small laths, RI<qz) =>An6 albite. Not a definitive measurement, especially since the larger grains often seem to be concentricaly zoned. 54%. * Carbonate- often as tiny grains, with high but variable relief. Twinkling, habit and extreme bir are distinctive, even for 25um grains. Also as thin veinlets with qz. 30%. * Quartz- fgr qz, occasionally quite coarse in veins (max gs 900x700um). 10%. * White mica- LS, str ext musc. Max gs 180x4Oum in wispy stringers. Lath length generally <50um. 6%.
Minor and Accessory Minerals (Tr.); * Fe oxides- in part translucent and red. Tr. * Sulphide- only 2 grains >100um. Largest grain (700x250um) is veined by Fe oxides, as seen in 'RL'. Tr. * Tourmaline- one 1200x200um sheaf of rather fibrous pale yl-neutral LF mineral. Somewhat resembles a sheet silicate, but it is pleo with max absorption normal to the polarizer, and bir is higher than normal chl. Tour, probably (from the colour scheme) quite magnesian (intermediate to Mg end of schorl-dravite series). Tr.
Textural Features; 1. Feld-phyric felsic metavolcanics with variable carbonatization. Groundmass of fgr (50um or less) rounded equant qz with subordinate feld (plag), musc randomly oriented along qz grain boundaries. 95% of chips. 2. Unzoned qz-carb veining, max dia 1mm, max gs 200x100um. Anh, unstrained crystals. 5% of chips.
Summary of Lithologies and Textures; dominant lithology is a FELSIC FELDSPARPHYRIC METAVOLCANIC. No strong foliation. Minor QUARTZ-CARBONATE VEINING. Carbonatization, lesser sericitization, some degree of silicification and albitization, and likely late addition of minor tourmaline have affected the rock. The primary igneous texture is preserved. No strong foliation is evident, nor other features suggestive of intense deformation.
Age; Archean. Petrography; GCW, Turnstone Geological Services Ltd, TO Thu 07-Aug-86
TURNSTONE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample
H86-08-10 (mount '84') Description; 304 Client/job
Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format ; CTS, Geoplastech, TO - 25-30um
Hand specimen data; one epoxy mount of drill chippings. Extremely fgr dark grey chips, minor amounts of milky qz and limonite.
Major Minerals; * Quartz- one chip in single 600x350um grain. Another chip shows extensive recrystallization, with prominent mortar textures of subgrains in larger grains; 10-250um gs range (variable gs, and mutual alignment of grain long axes). This last is probably a chip from a qz-(carb) veinlet. 90%. * Carbonate- anh grains in qz-carb veinlets, and scattered granules in the dominant lithology. 5%. * White micas- LS, str ext musc, mostly fine (20-30um) flakes in qz-rich metasediment. 5%.
Minor and Accessory Minerals (Tr.); * Opaque phases- one 800x600um area consists mostly of opaque sulphide-oxide intergrown with silicates, principally hb (see below). Tr. * Plagioclase- max gs 600x250um, with albite and pericline twinning, wide but inadequately determined MEA suggests intermediate-calcic composition. Quite fresh, with only minor sericitization. Tr. * Amphibole- LS, inclined ext, bl-grn to brn pleo, moderate bir amph found in lithology (3). Core resembles hb; fibrous margin closer to act. Lithology (6) contains a paler, feathery act. Tr. * Biotite- max dia 50um, deep brn, assoc with amph. Tr. * Epidote- fgr, granular, pale yl, relatively high bir. Tr. * Chlorite- max gs 180x160um, very low bir, anomalous purplish-brn int colours in XP. Tr.
Textural Features; 1. Vfgr qz-rich banded rock. May be banded in terms of qz gs or of mica content. 'Coarse' bands show 20-30um gs, while in fine bands gs<15um. Curving laminae of coarser qz in the vfgr qz suggestive of sedimentary structures. Perhaps 10% of this dominant lithology is distinctly micaceous. Metasediment, variable from siltstone to (subordinate) argillite. Pervasive mica alignment; near-perfect metamorphic fabric, seen only in relatively micaceous chips. 90% of chips. 2. Qz-carb veins, max gs 250um, strained ext in larger grains, with minor musc (max gs 75x25um). Vein widths to 1.5mm. At least two sets, all proportions of qz:carb, occasionally cross-cutting. 6%. 3. Qz-plag-epi-hb-opaque assemblage; one chip of a fgr metavolcanic rock. 1% 4. One igneous fragment with twinned plag, pleo amph, brn bi and opaques. Rounded opaque granules in skeletal-type intergrowth with silicates (mainly amph). Possibly a metamorphosed diabase. 1%. 5. Metavolcanic rock with qz, epi, chl (ripidolite), py (100um square cross-section). Epi includes a 200x150um granular aggregate displaying
bright yl and bl-grey int colours. 1%.
6. Metavolcanic comprising 50-150um amph (act) laths with fgr clear (?) plag speckled by minor epi. The act shows pale grn to colourless pleo, elongate
LS sections, and moderate bir. 1%.
7. Single qz grain, unstrained, provenance unknown. Trace.
Summary of Lithologies and Textures; sample dominated by METASEDIMENTS
(SILTSTONE-ARGILLITE). Substantial amount of QUARTZ-CARBONATE VEINING. At least four igneous rocks, sparsely represented, apparently three
INTERMEDIATE-BASIC METAVOLCANICS and one coarser (?) DIABASE.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Thu 07-Aug-86
TURNSTJNE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample H86-76-12 (mount '88') Description; 305
Client/job
Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling.
Format ; CTS, Geoplastech, TO - 25-30um
Hand specimen data; one epoxy mount of drill chippings. Siliceous samples; dark and relatively uninformative mount, as in Descr. 304. Mount shows no
eff in dil HC1.
Major Minerals; * Quartz- max gs (in lithologies (1-3)) are 70x60, 200x140 and 350x250um
respectively. Vein qz contains numerous small (10um or less) fluid
inclusions. 50%. * Carbonate- rhombohedral cleavage, symm ext. Twinkles strongly against qz. Max gs 500x250um in single carb chip. Relief high when long axis of rhomb parallel to vibration plane of polarizer. 35%. * White micas- LS, str ext musc, max gs 180x15um. Mostly 30x1Oum or smaller;
int colour generally 1st-o yl. 15%.
Minor and Accessory Minerals (Tr.); * Opaques- incl. some py, max gs 90x6Oum, with one perfect 30um-dia euh
hexagonal section in lithology (1). Tr.
Textural Features; 1. Vfgr foliated rocks, variable proportions of white micas and granular
carb. Carb grains scattered through qz-muse matrix. Carb appears to be superposed on the rock fabric; it does not enclose other minerals. Carb
probably recrystallized, with grains either equant or slightly elongate parallel to rock foliation. Metasedimentary; a 'calcareous argillite'.
96%. 2. Relatively cgr rock, in sharp contact against (1), essentially qz-carb rock, 100-200um gs. Only one chip, apparently concordant against (1). Musc
laths are subparallel to the contact, and decrease in abundance into the qz-carb rock. Not clearly transgressive, unlike (3). 2%. 3. Carb veinlets, both parallel to and cross-cutting foliation. 2%.
Summary of Lithologies and Textures; Fine-grained METASEDIMENTS; SILTSTONE
with minor QUARTZ-CARBONATE VEINING. Possible component of sedimentary carbonate within the bulk rock, although remobilization possible on unknown scale.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Thu 07-Aug-86
TURNSTONE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-77-06 (mount '87'') Description; 306
Client/job ; Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format ; CTS, Geoplastech, TO - 28-31um
Hand specimen data; one epoxy mount of drill chippings. Fgr white siliceous rock, up to 10% of limonitic fragments, and trace of py.
Major Minerals;- * Relict feldspar and alteration products- flakes and aggregates of white mica. Vfgr (often <10um) ser and kaol with tr. carb and Fe oxides in grains of max gs 400x300um. Slightly turbid, biaxial +ve, untwinned. Low relief. Inferred to be mostly/wholly sodic plag. 48%. * Quartz- coarsest n the case of vein qz, max gs 900x500um, showing slightly strained ext. 25%. * White micas- may plate onto py or carb. May form anastomosing grain-crossing fracture fillings approx 50um wide, constituent flakes commonly oriented roughly normal to the veinlets, most flakes spanning the full width. 18%. * Carbonate- one unusual texture comprises stubby fibrous colourless carb pressure shadows on darker blocky (500x300um) carb grain. Thinner musc flakes may also occupy this position; lower-order (brighter) int colours. 7%.
Minor and Accessory Minerals (2%); * Fe oxides- some translucent and red, incl, a veinlet up to 350um wide. Red in PPL/XP, with no ext position. 2%. * Opaques- including py (square and 6-sided euh sections to 280x250um). Tr. * Apatite- single colourless, high relief, crudely hexagonal basal section. Isotropic, dia 70um, partially enclosed by carb. RI>carb,qz. Tr.
Textural Features; 1. Qz-feld-mica rock with prominent mica 'beards'. Plag-rich matrix with equant qz and subordinate mica on grain boundaries. Mica fibres define a discontinuous foliation, hence the 'beards'. Presumed to be an immature, feldspathic, volcaniclastic metasediment. 92%. 2. Qz-rich lithology, grain boundaries filled by Fe oxides. Grains commonly equant, approx 300um max gs. A relatively silicic, fractured, ironstained variant of lithology (1). 5%. 3. Qz-(carb) veinlets. Variable gs, generally qz-dominated. 3%.
Summary of Lithologies and Textures; Felsic VOLCANICLASTIC METASEDIMENTS, the minority of silicic samples relatively fractured and stained by limonite. Minor QUARTZ-RICH VEINING.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Fri 08-Aug-86
TJRNSTONE
PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-79-06 (mount '86') Description; 307
Client/job
Homestake Mineral Development Co.
Locality
Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format
CTS, Geoplastech, TO - 28-30um
Hand specimen data; one epoxy mount of drill chippings. Dominant lithology is vfgr, white and rathery powdery in appearance. Some fragments contain grey 1-2mm thick veinlets. "Local limonitic staining. Minor proportion of
grn-black (?) chloritic lithologies.
Major Minerals; * Carbonate- incl. minor (say 2% of mode) distinctly brn (Fe-rich?) carb. All carb twinkles on rotation, and often varies from pale brn to colourless. Blocky grains to 200x200um common, coarser than the adjacent qz. 50%. * Quartz- commonly vfgr, 5-40um. Max gs 700x600um in qz veins. 35%. * White micas- generates foliation between carb clumps. 1st-o yl int colours. Length generally <50um or so. 14%.
Minor and Accessory Minerals (1%); * Opaques- probable mixture of oxides and sulphides. sulphide grains, some possibly vfgr, 2)fluffy anh (?) Fe and 3)possible tabular ilmenite(?) in chloritic fragment, of mode. * Chlorite- low anomalous bir. Max gs 120x20um, LS, grn-colourless pleo. Chl var. penninite. Tr.
Includes 1)small oxide to 180x140um, max gs 70x40um. 1%
str ext, distinct
Textural Features; 1. Crowded array of subequant carb grains in fgr qz-rich matrix. A few rounded qz amygdules, max size 1.4x1.1mm. The amygdules are filled by qz with complex textures apparent only on slight rotations in XP. Sometimes with carb rims. 94%. 2. Qz-centred carb-rimmed veinlets. Distinct from vesicles in form and (sometimes) by elongation of qz during growth across vein fracture. 5%. 3. Foliated fgr chip with aligned chl and (?) ilm. 2.Ox0.7mm chip of qz-rich rock. 1%.
Summary of Lithologies and Textures; METAVOLCANICS, mostly strongly carbonatized, with minor VEIN QUARTZ.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Fri 08-Aug-86
TURNSTONE
Sample Client/ job
Locality Collection Format
details;
PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
H86-78-09 (mount '81') Description; 308 Homestake Mineral Development Co.
Joutel project, N.W. Quebec (NTS 32E/9,10). bedrock chips from reverse circulation drilling. CTS, Geoplastech, TO - 28-30um
Hand specimen data; one epoxy mount of drill chippings. Small (1-2mm) chippings, often white to pale yl and rather earthy in appearance; clay mineral alteration? Traces of lim.
Major Minerals; * Carbonate- twinkles in cgr areas. Max gs 300x300um in carb-qz veins and in metavolcanics; local aggregates to 1mm dia. 45%. * Quartz- mostly 30-50um, coarser (to 100um or more) with cgr carb, enclosing small carb granules. Also coarser in veins and in granitic fragments, max gs 700x600um. 33%. * White micas- musc, locally abundant in areas up to 500x100um, showing bright int colours. Individual flakes to 70x5Oum. 20%.
Minor and Accessory Minerals (2%); * Feldspar and alteration products- albite-twinned zoned crystal of plag with patchy kaol (turbid alteration) attached to and intergrown with qz crystals and trace of cgr musc in lithology (2). Max gs 1000x800um. May enclose specks of bi and chl. Possible traces of Kfeld too. Also turbid plag altering to epi in lithology (4). 1%(+). * Chloritoid- colourless LF laths, high relief, inclined ext (MEA21), bir approx 0.010. Single laths and subparallel aggregates to 250x70um. Shows lamellar twinning but (unusual) no pleo. Porphyroblastic. 1%(-). * Chlorite- low 1st-o bir with anomalous int colours. Esp common in lithology (4). Grn-neutral pleo, LS, str ext. Chl var. penninite. Tr. * Epidote- aggregates to 900um max length in (4), with very bright int colours, including odd yl and bl-grey tints in 1st-o. Tr. * Amphibole- inclined ext, pale grn pleo, LS, altering to chl in (4). Also in (5), max gs 500x120um. Tr. * Opaque phases- fgr, anh, max gs 120x100um; anh Fe oxide and equant py? Tr. * Sphene- extreme bir. 50x3Oum round brn grain in (5). Rare Tr.
Textural Features; 1. Metavolcanic with local overprinting of chloritoid. A few chips indicate some alignment in cgr carb and fgr qz. Variant comprises vfg:r (gs<20um) qz-musc rock with carb-qz amygdules. 91%. 2. Granitic fragments with plag (ser,kaol), qz, strongly pleo bi
and/or
colourless musc, and (?)Kfeld. 4%. 3. Cgr carb-qz veining. 2%. 4. Gabbroic fragment- plag and amph altering to epi and chl respectively. Rich in grn chl and bright granular epi. 1%. 5. Hb-rich foliated amphibolite- abundant pleo hb. Hb pleo in bl grn- grn-brn. Qz, ch, turbid feld and tr. sphene also present. 1%. 6. Rock rich in epi and chl, cut by qz-epi veinlet. 1%.
Summary of Lithologies and Textures; Intensely carbonatized METAVOLOANIC, with subordinate amounts of CARBONATE-QUARTZ VEINING, GRANITE-GRANODIORITE, and three other relatively fresh igneous rock types; two METAVOLCANICS and a
GABBROIC intrusive.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Sat 09-Aug-86
TURNSTONE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-80-14 (mount '83') Description; 309 Client/job ; Homestake Mineral Development Co.
Locality
Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format
CTS, Geoplastech, TO - 26-30um
Hand specimen data; one epoxy mount of drill chippings. Dominant lithology vfgr and siliceous. 10-15% mixture of variants, such as slight to pronounced ironstaining. Some grn-black (?) chloritic (?) metavolcanics.
Major Minerals; * Quartz- mostly of gs<30um, dominating vfgr goundmass of major rock type.
74%. * Carbonate- may display rhombic cleavage, twinkling, and faint brn hues in PPL. 14% * White micas- mostly vfgr, but foliated (micaceous) samples have coarser laths, max gs 80x10um. LS, str ext musc. 10%.
Minor and Accessory Minerals (2%); * Fe oxides- Red-brn translucent Fe oxide may form granular bands in the rock; foliation crosses between granules; pre-foliation limonitic joints?
1%(+). * Plagioclase and alteration products- turbid in lithology (4), smaller and less obvious in (2). 1%(-). * Hornblende- grn-brn pleo, inclined ext, found in (2). Also in (4), paler in colour, showing typical amph basal cleavage, max gs 500x300um. Tr. * Chlorite- penninite with anomalous bl tints in low 1st-o int colours. Found in lithologies (2,5). Tr. * Epidote- Max gs 50x40um, lithologies (2,5). Tr. * Clinopyroxene(?)- pale (?) aug, max gs 120x6Oum, inclined ext, found in (2). Tr. * Sphene- max gs 100x8Oum, extreme bir and relief, brn and granular. Found in (5). Tr.
Textural Features; 1. Felsic-intermediate metavolcanics, with carb clots in fgr qz-rich mica-foliated matrix. Some larger carb clots are pleo in brn; 50-250um masses in fgr (5-20um gs) qz-rich matrix. Some samples are foliated, with white micas appearing to grow around the carb, but the carb generally seems to be late, superposed on earlier fabric. Areas as large as 800x800um may be mostly carb. Variable proportions of qz-musc-carb. 94%. 2. Basic amph-rich metavolcanic. Hb, chl, qz, plag, px(?) and epi„ Encloses rounded qz-filled amygdule. 2%. 3. Qz-carb veinlets with variable qz:carb ratio. 2%. And two less-common chip types; a. Cgr pale pleo hb and turbid plag (with ser); altered gabbro. 1%. 5. Flag plus pale chl, with qz, sphene, epi. 1%.
Summary of Lithologies and Textures; Variably altered METAVOLCANICS with minor QUARTZ-CARBONATE VEINING and a trace of GABBROIC intrusive rock.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Sat 09-Aug-86
TURNSTCNE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-81-20 (mount '80') Description; 310
Client/job ; Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format ; CTS, Geoplastech, TO - 25-30um
Hand specimen data; one epoxy mount of drill chippings. Roughly 50:50 mix of dark fragments with milky vein qz. Abundant fgr granular py; PTS could usefully be made from this mount.
Major Minerals; * Quartz- max gs in lithologies (1-3) near 2mm, 50um and 250um respectively, although (2) is often vfgr (5-20um), except for scattered coarser patches.
85% * Carbonate- twinkles, extreme bir, traces of fgr, brn carb near qz veins. Max gs 300x300um in (3), to '00x80um in (2). 6%. * Opaque phases - largely sulphide (py) with lesser Fe oxides; three habits are 1)disaggregated fgr material, 2)rounded coarse grains (max gs 2.0x1.5mm), and 3)extremely fgr sulphide 'flour' within silica matrix to breccias. All but the finest sulphide material appears in 'RL' to be py. Some py is brecciated, with rounded clasts and fgr matrix comprising py-only breccia. Py often on vein margins. 5%.
Minor and Accessory Minerals (4%); * White micas- LS, str ext musc. Max gs 150x9Oum in micaceous patches within lithology (3). 4%. * Fe oxides- translucent red-brn. Tr. * Feldspar- traces of sodic plag and Kfeld (both with RI<qz) in granitic fragment. The Kfeld is relatively turbid and shows no sign of twinning, unlike the plag. Tr.
Textural Features; 1. Quartz-carbonate veins with all proportions of dominant minerals. Vein qz gs to 1.8x1.5mm, displaying mortar texture in polycrystalline aggregates in patches of variable gs. Some strained ext. Vein carb; anh, strained, locally forms monomineralic masses of carb, coarser than vein qz. May form elongate tabular grains with wavy margins. 50%. 2. Vfgr siliceous rock. Brecciated texture with qz veinlets cutting siliceous matrix. Mostly vfgr. May contain disseminated py. Some pressure shadows of qz or musc invest py grains, and may also infill fractures within the sulphide. The fibres cut across thin qz veinlets => generated late in deformation history. At least three sets of qz veinlets cut the matrix, which may be darkened by vfgr sulphide grains. 27%. 3. Locally micaceous (and foliated) carb-flecked lithology. Contains py in larger grains and in vfgr streaks parallel to mica foliation. The fine sulphide seems to have formed by disintegration of the coarser grains. Less siliceous than lithology (2). 20%.
2%. kaol and cart)
alteration. 1%.
4. Loose sulphide grains- rounded blebs, probably near-pure py.
5. Granitic fragment. 2 feld, qz and musc, with traces of ser,
Summary of Lithologies and Textures; Abundant QUARTZ-CARBONATE VEIN material, with two types of presumed ALTERED METAVOLCANIC rocks, one an intensely silicified 'jasperoid' rock, the other more carbonatized, with distinct foliation and deformation structures. Sample with significant SULPHIDE and a trace of GRANITIC material.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Sun 10-Aug-86
TURNSTONE PETROGRAPHIC DESCRIPTION Status; CONFIDENTIAL
Sample ; H86-82-09 (mount '82') Description; 311
Client/job ; Homestake Mineral Development Co.
Locality ; Joutel project, N.W. Quebec (NTS 32E/9,10). Collection details; bedrock chips from reverse circulation drilling. Format ; CTS, Geoplastech, TO - 28-30um
Hand specimen data; one epoxy mount of drill chippings. >95% comprises chips rich in milky vein qz. A few vfgr grey-black chips. Some grey (?) carb assoc with qz.
Major Minerals; * Quartz- max gs 400x250um in qz-carb veins, 70x5Oum in the dominant lithology. Intergrown with carb in veins, showing slightly strained ext. 52%. * Carbonate- aggregates to 500x500um (usually 100-200um) common in metavolcanic rock. Also in veins, some of which are pure carb. 35%. * White micas- defines foliation in carb-poor areas. LS, str ext musc, gs generally 50x1Oum or less. May also occur along thin fractures, foliae oriented along bulk rock foliation. 13%.
Minor and Accessory Minerals (Tr.); * Opaques- max gs 250x200um. Mixture of Fe oxides and (square and rectangular subh sections) py. Tr.
Textural Features; 1. Equigranular mosaic of carb and qz interspersed with sheaves of mica. Dominant lithology. Local qz-dominated ovoid patches up to 600um across may be small amygdules. 95%. 2. Fgr (10-30um gs) areas of equigranular qz, in contact with micaceous bands. Cut by late carb veinlets. Insufficient material to determine whether this forms bands of lenses (fgr amygdules?) in lithology (1), with which this qz presumed to have a common origin. 3%. 3. Locally monomineralic qz-carb veinlets, with all proportions of the two constituents. 2%.
Summary of Lithologies and Textures; Carbonatized and silicified METAVOLCANICS, with minor QUARTZ-CARBONATE VEINING.
Age; Archean.
Petrography; GCW, Turnstone Geological Services Ltd, TO Sun 10-Aug-86
QUEBEC - ABITIBI SEARCH FILE
Based on current (>5500 items) library
(c) Graham C. Wilson 1986
Dr Graham C. Wilson
Messages; (416)-626-5465 Turnstone Geological Services Ltd
Wed 06-Aug-86 Box 130, Station "B", Toronto
Ref: MINLIB/ESLIB Ontario, M5T 2T3 CANADA
On behalf of: David Bending. Homestake Mineral Development Co.
47 References output from MINLIB/ESLIB. (c) Graham C. Wilson 1986
Search Code 'Quebec - Abitibi' - covers all entries on Archean Abitibi greenstone belt in Quebec Enquiries about this document, or concerning use of the
search system, should be directed to the compiler
Not to be sold, lent or otherwise disseminated without written permission
Page 1
Avramtchev.L and Lebel-Drolet,S Catalogue des Gites Mineraux du Quebec. Region de l'Abitibi. Gouvernement du Quebec, Ministere de l'Energie et des Ressources,
DPV-744 (1981). Quebec Canada - 98pp. catalogue of mineral occurrences of numerous
metals and industrial minerals - includes 14 maps and key DPV-809 - Au camps of Abitibi - Noranda - Chibougamou etc - map sheets are: 31K Deep River - 31L North Bay - 31M Ville-Marie, incl. Belleterre Au - 31N Grand Lac Victoria - 32B Reservoir Gouin - 32C Senneterre. incl. Val d'Or/Bourlamaque Au granite volcanics - 32D Rouyn-Noranda, incl. Au granitic rocks, volcanics - 32E Riviere Harricana Superieure - 32F Lac Waswanapi. incl. Lac Cameron Au - 32G Chibougamau (Au) - 321 Riviere Mistassini Nord - 32J Lac Assinica - 32K Lac Evans - 32L Riviere Harricana Inferieure - much Archean geology on these sheets.
Bickle.NJ Suspect Sm-Nd whole-rock ages. Nature 312. 702-703 (1984). Age dating - Sm-Nd dating - Archean greenstone belts - Kambalda, W.A.ustral ia
U-Pb data - Pb isotopes - minimum age of Kambalda granodiorite is 2820+1-15 Ma - Fe Ni sulphide ores - Abitibi belt, Ontario and Quebec, Canada - komatiites - Sm-Nd date of 3260 Ma in Kambalda - heterogenous mantle or resetting of Pb isotope clock?
Blecha,N Estrades: a Canadian Kuroko? Northern Miner Magazine 1 no.5, 14-17,38 (June 1986). Quebec. Canada - Casa Berardi - Archean - Abitibi greenstone belt - Au Ag
values - massive sulphide, consisting (order of abundance) of sphalerite - pyrite - chalcopyrite - metavolcanics - Au Zn Cu profiles - minor minerals include freibergite, tetrahedrite and native Bi - similarity to Kuroko deposits.
Card,KD Subdivisions of the Superior Province of the Canadian Shield. Geoscience Canada 13 no.1, 5-13 (extended abs. in Fr.) (1986). Quebec. Ontario. Manitoba, NWT. Canada - Precambrian - Archean -
regional synthesis - greenstone belts - 8 maps - Abitibi, Uchi. Wabigoon, Wawa, Quetico. Pontiac. Berens River. Pikwitonei, Kapuskasing (etc) subprovincem - review - bibliography.
Coad.PR Nickel Sulphide Deposits associated with Ultramafic Rocks of the Abitibi
Belt and Economic Potential of Mafic-Ultramafic Intrusions. OGS Study 20, 84pp. (1979). Ontario. Canada - Ni sulphides - Archean - deposits may be in extrusive
ultramafic flows (Langmuir, Texmont, Hart) and in (?extrusive) dunite lenses with pyroxene-rich peridotitic margins (e.g. Alexo) - all related to komatiitic magmatism - all except Alexo occur at one etratigraphic level near the base of the Tisdale Group - volcariogenic exhalative origin - Ni deposits of Canada and elsewhere may be found in both intrusive and extrusive komatiites: the latter seem to be a more common host - Cu and Ni may also be hosted in mafic and layered intrusions of tholeiitic affinity - Abitibi geology. from
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Timmins E. into Quebec - photomicrographs - ore textures - petrography - net texture - ■pinifex texture - colloform sulphides serpentine - Ni sulphides elsewhere: Manitoba. NAT. Zimbabwe and (especially) Australia.
Daigneault.R and Allard,G0 Structural evolution of the Chibougamau greenstone belt: Archean vs Grenville
tectonics. GAC/MAC Prog.w.Abs. 11. 61 (1986). Archean Abitibi greenstone belt - Chibougamau. Quebec, Canada - four
periods of deformation - structural geology - Grenville Front - foliations and lineations.
Dimroth.E Sedimentological contrast between the external and internal zones of the
Archean Abitibi Belt. Abs. IAS 11th Int.Congr.Sed., Hamilton. Ontario. August 1982, 2 (1982). Archean - greenstone belts - Quebec. Canada - Chibougamau - paleogeography -
sedimentary facies - turbidites. conglomerates, black shales.
Dimroth,E and Rocheleau,M Archean wrench fault tectonics and structural evolution of the
Blake River Group, Abitibi Belt, Quebec: discussion. CJES 22. 941-943 (1985). Abitibi greenstone belt - Archean - Quebec. Canada - maps - folds,
faults and lineations - structural geology - rock strain increases toward Porcupine-Destor and Cadillac Breaks - varioles - see also note by Archambault,G: ibid. pp.943-945.
Dimroth.E. lmreh.L. Rocheleau,M and Goulet.N Evolution of the south-central segment of the Archean Abitibi belt. Quebec.
Part l: stratigraphy and paleogeographic model. CJES 19, 1729-1758 (1982). Abitibi greenstone belt - Archean - Ontario and Quebec. Canada -
volcanic stratigraphy - paleogeography: five phases are recognized - - 'the stratigraphic and paleogeographic evolution of the Abitibi Belt is comparable to the evolution of immature oceanic island arcs in the Cenozoic' - plate tectonics - maps - ultramafics - tholeiitis ■etasediments - Destor and Noranda volcanic centres - turbidites, conglomerate and greywacke - many references.
Dimroth,E. Imreh.L, Goulet,N and Rocheleau,M Evolution of the south-central segment of the Archean Abitibi belt, Quebec.
Part ill: plutonic and metamorphic evolution and geotectonic model. CJES 20. 1374-1388 (1983). Abitibi greenstone belt. Quebec Canada - volcanics underwent three types of
pre-Kenoran metamorphism; pervasive alteration. contact metamorphism. and intense hydrothermal alteration affecting cross-cutting pipes in central volcanic complexes - synkinematic metamorphism upto amphibolite faciem - plutonics - Kenoran metamorphism - plate tectonics.
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Douglas,RJW (editor) Geology and Economic Minerals of Canada. GSC Econ.Geol.Rep. 1, 2 vole, 838pp. (1976). Canada - review of geology and mineral deposits - a third volume is a folio
of charts and maps - Vol.A: topography of the Shield - Yukon. BC. NWT - Alberta - Saskatchewan - Manitoba - Ontario - Quebec - Nova Scotia - Newfoundland - Prince Edward Island - New Brunswick - Canadian mineral production to 1968 - Archean geology - K-Ar and Rb-Sr age dates (p.49) - stratigraphy - orogenies - Abitibi and other greenstone belts. Slave province, etc - stromatolites (p.79) - Muskox basic layered intrusion - dyke swarms - fold belts - Huronian and Grenville - tectonic evolution of Quebec (p.124) - many sketch maps and aerial photos. e.g. Clearwater Lake structure (p.136) - section on metallogeny by Lang,AR et al - iron formation - BIF - Fe deposits - Ni - Sudbury. Thompson - Co Cr Ti Cu Zn Pb - Au Ag and ** PGE -
PGE production - other metals such as Be Li Mo Ta Nb - beryllium - industrial minerals - S.E.Canadian stratigraphy - Cambrian. Ordovician, Silurian. Devonian - sedimentary basins - oil, gas and coal - Vol.B: W.Canada - Proterozoic. Paleozoic (w. Carboniferous. Permian) - paleogeography - ultramafic and plutonic rocks (pp.422-428) - mullion structures and agmatites - photomicrographs of sediments from the Cassiar Mountains (pp.402,441) - Mesozoic (Triassic. Jurassic, Cretaceous) - Cenozoic - Laramide orogeny - Little,HW et al on western mineral deposits - Pb Zn Ag - Sullivan orebody. BC - Au - porphyry Cu -
other deposits: Mo W Hg etc - potash mining in Saskatchewan - coal and petroleum - Arctic Canada - fossils and geochronology: many photos and correlation charts; corals. brachiopode, ammonites etc - paleobotany - glacial geology - retreat of Wisconsin Ice (opp. p.706. on) - drumlins, glaciers. hydrogeology. indices - age dating.
Duke.JM Petrology and economic geology of the Dumont Sill: an Archean intrusion
of komatiitic affinity in northwestern Quebec. GSC Economic Geology Report 35. 56pp. (1986). Quebec, Canada - Dumont sill - poorly exposed Archean differentiated
mafic-ultramafic sill in the Abitibi greenstone belt, 62 km N.E. of Rouyn - material from 57 drill holes - komatiitic synvolcanic intrusion in Fe tholeiites - cumulates - dunite - olivine cumulates with chromite or sulphide - quartz gabbro near top of sill includes some nonc:umulate
facies - sulphide concentrations formed by filter pressing of S -rich intercumulus liquid, which was expelled upward from accumulating basal layer of intratellutic olivine crystals - serpentinization - magnetic survey - maps - petrography and photomicrographs - pseudomorphs - lizardite hourglass texture - antigorite - EPM of olivine, clinopyroxene, chromite, serpentine, chlorite, diopside, actinolite - magmatic sulphides - mobility of Cu in serpentinization - pentlandite, magnetite, awaruite, native Cu - Ni mineralization - spinifex peridotites - model parent magma composition - layered intrusions - exploration guides (pp.47-48) - references -
whole-rock analyses.
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Flanagan,JT Lithium deposits and potential of Quebec and Atlantic Provinces. Canada. In 'Lithium Needs and Resources' (Penner,SS, editor), Pergamon Press,
pp.391-398 (1978). Quebec and Nova Scotia. Canada - spodumene dykes have been found in
every major Archean greenstone belt between 47 and 53 degrees N. - Abitibi belt - Archean - the Li dyke deposit■ usually occur between the ipper contacts of late-stage granitic intrusives (e.g. the 2635 Na Preissac-Lacorne batholith, late muscovite granite phase) and metamorphosed volcanic and sedimentary rocks - pegmatite dykes.
Franklin.JJ1. Lydon.JV and Sangster.DF Volcanic-associated massive sulfide deposits. Econ.Geol. 75th Anniversary Vol., 485-627 (1981). Massive sulphide ores - massive review - characteristically >60%
sulphide, mostly pyrite and/or pyrrhotite, plus variable ephalerite. chalcopyrite. galena - zoning - two groups. one rich in Cu and Zn and the other Zn Pb Cu - oxide facies iron formation is more often associated with the latter - BIF - the groups can be differentiated by S isotopes but not Pb isotopes with one exception. the 0 isotopes of altered rocks associated with these ores are lighter than those of the unaltered equivalents - Sr isotopes - alteration pipes under Pb Zn Cu deposits generally have a sericite-quartz core and a chlorite outer edge. whereas pipes under Cu Zn deposits typically have a chloritic core and a sericitic margin - deposits fro■ Canada (Ontario,Quebec: Abitibi greenstone belt, Noranda. the Kidd Creek mine near Timmins. the Geco sine near Manitouwadge - Flin Flon. Manitoba) - Finland - Sweden - Cyprus (ophiolites - Troodos) - Italy (Liguria ophiolites) - Newfoundland - Norway (Trondheim, Caledonides) - Besshi deposits - Japan - Turkey - Morocco - the Kieslager district (Austria. Italy) - the Bathurst camp. New Brunswick - Kuroko ores - Sudbury.Ontario - Buchans. Newfoundland - Mattagami.Quebec - hydrothermal fluids - H isotopes - pyrite - zoned deposits - 16pp. of references.
Frarey.MJ and Krogh.TE U-Pb zircon ages of late internal plutons of the Abitibi and eastern
Wawa subprovinces. Ontario and Quebec. GAC Pap. 86-1A. 43-48 (1986). Wawa district. Ontario. Canada - Archean Abitibi greenstone belt -
U-Pb zircon age dating - excluding the Taschereau stock in Quebec. dates from 11 sites all fall in the 2700-2675 Na range sites fro■ the Opemisca pluton near Chibougamau to the Ash Lake pluton near Wawa - Timmins area - Franquet. Launay, Garrison. Bernhardt, Dunmore. McEvay, Baden. Keith and Copenace townships (amongst others) - Watabeag batholith.
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Gariepy.0 and Allegre,CJ The lead isotope geochemistry and geochronology of late-kinematic intrusives
from the Abitibi greenstone belt, and the implications for late Archaean crustal evolution.
GCA 49, 2371-2383 (1985). Abitibi greenstone belt - Quebec, Canada - Pb isotopes - age dates suggest
that Abitibi orogeny ended 2710-2700 Ma, and that granitization followed for a period of 80-100 Ma - granitoids as partial melts of pre-existing continental crust.
Gaudreau.R and Rocheleau.M Petrologie, geochimie et gito-metallogenie des indices auriferes de
l'intrusif de Mooshla, canton de Bousquet. Abitibi. GAC/MAC Prog.w.Abs. 11, 72 (in Fr.) (1986). Quebec, Canada - tholeiitic and calc-alkaline lavas - the Mooshla
dioritic-granodioritic intrusion - Au in quartz veins - structural geology - hydrothermal alteration - mineralogy.
Gelinas,L and Trudel,P Archean mafic metavolcanics from the Rouyn-Noranda district. Abitibi
greenstone belt, Quebec. 1.Mobility of the major elements: reply. CJES 21, 263-255 (1984). Quebec Canada - in the Abitibi belt carbonatization is a late local event,
'intimately associated with fault and shear zones' - there is no direct correlation between the degree of chloritization and the content of CO2 in the fluid phase (c.f. Walsh,JJ 1984) - seawater and alteration of the volcanic pile - the successive disappearance of actinolite and epidote in altered basalte is due to an increasing seawater/rock mass ratio - carbonatization is superimposed on all types of alteration - hydrothermal fluids.
Gelinas,L. Brooks,C and Trzcienski,VE Archean variolites - quenched immiscible liquids. CJES 13. 210-230 (1976). Liquid immiscibility - Archean - variolitic lavas in a tholeiitic series
around Rouyn-Noranda - Abitibi - Quebec Canada - large well-defined spheroidal felsic varioles up to 5 cm in diameter occur in a more mafic ferruginous matrix - quench texture and flow differentiation studies - pillow lavas and massive flows - textures - alteration.
Gelinas,L, Brooks,C. Perrault.G. Carignan,J. Trudel.P and Grasso.F Chemo-stratigraphic divisions within the Abitibi volcanic belt.
Rouyn-Noranda district. Quebec. In 'Volcanic Regimes in Canada' (Baragar.WRA, Coleman.LC and Ha11.JM.
editors). GAC Spec.Publ. 16. 476pp.. pp.265-295 (1977). Abitibi greenstone belt - Archean - Quebec. Canada - volcanic
stratigraphy - tholeiite, basalt. andesite, rhyolite - a compositional gap exists between 64-71% Si02 in the rocks of the Blake River Group - plate tectonic model: continental island arc similar to that responsible for Pleistocene volcanism in the Taupo province of New Zealand - most of the volcanics thought to be derived from shallow depths (15-20 km) - maps - petrography and textures - komatiite - variolitic lavas - pseudomorphous textures - prehnite-pumpellyite and biotite zones
Page 6
4 photomicrographs - whole rock chemistry.
Goodwin. AM Archean volcanism in Superior province. Canadian Shield. In 'Volcanic Regimes in Canada' (Baragar,WRA, Coleman,LC and HaIl,JN,
editors), GAC Spec.Publ. 16, 476pp., pp.205-241 (1977). Archean volcanism - 1629 rock analyses - review of volcanics from three
areas of the Superior province. with mean rock analyses - weighted mean of Superior volcanics includes 1.69 Vt.% CO2 - 220ppm Cr - 0.6ppm Ga - 0.45ppa Ag - 237pp■ Ba etc - individual volcanic cycles commonly vary fro■ tholeiitic basaltic lower sections through calc-alkalic andesites to local /mimic tops - Abitibi greenstone belt - Blake River Group - plate tectonics - Ontario and Quebec, Canada - Timmins, Kirkland Lake and Noranda - Lake of the Woods-Vabigoon region - Birch Lake-Uchi Lake region.
Goodwin,AM and Ridler,RH The Abitibi orogenic belt. GSC Pap. 70-40. 1-30 (1970). Ontario and Quebec. Canada - the Archean Abitibi greenstone belt is some
500 x 150 miles in size: the largest single continuous belt in the Canadian shield - low-medium greenschist facies metamorphism prevails recognized mafic-felsic volcanic centres and associated clastics and iron formation are concentrated in 2 main E.-trending bands. each 50 miles across. forming the N. and S. margins of the belt - the centre is underlain by tholeiitic basalte, fine-grained clastics and major granitic batholiths - plate tectonics - Abitibi belt is viewed as an intra-tectonic orogen rather than a more conventional asymmetric continent-ocean island arc structure - with comments by Naldrett.AJ on the komatiites and other ultramafic rocks - BIF.
Gorman, BE The Bousquet-Cadillac district. In 'Structure and Gold. Rouyn to Val d'Or, Quebec (Hubert,C and Robert.F
editors). GAC/MAC Field Trip Guide Book 14, 70pp., 43-52 (1986). Quebec, Canada - Archean - Abitibi greenstone belt - Fiche group -
Cadillac-Larder Lake Fault (Cadillac Break) - Au deposits - stratigraphy - lithologies - aetavolcanics and metasediments - field trip road log - whole-rock analyses - diorite sills - BIF - sulphide reduction zones - structural geology - intense folding in magnetite BIF - hydrothermal alteration - carbonatization.
Guha.J Hydrothermal systems and correlations of mineral deposits in the
Chibougamau mining district - an overview. In 'Chibougasau - Stratigraphy and Mineralization' (Guha,J and Chown,EH
editors), CIM Spec.Vol. 34. 517-534 (1984). Chibougasau. Quebec. Canada - structural control on mineralization -
multi-stage history of ore formation - Au Ag Zn Pb As veins. Berrigan Lake and elsewhere - arsenic - Bourbeau sill - lode Au Ag mineralization - shear/fault/fracture-controlled Au Ag Cu ore - Opemiska - Dore Lake - minor U mineralization is described as 'post-Archean' - local geology - etratigraphy - table of mineralization styles (p.521) - maps - porphyry systems Archean - Abitibi greenstone belt.
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Guha.J and Chown,EH Chibougamau stratigraphy and mineralization: an Archean belt with a
difference. In 'Chibougamau - Stratigraphy and Mineralization' (Guha.J and Chowri.EH
editors), CHI Spec.Vol. 34, 1-4 (1984). Quebec, Canada - Archean - Abitibi greenstone belt - Chibougamau
is at the eastern extremity of the belt . in the 'internal zone' or 'Chibougamau-Matagami greenstone belt' - local geology - shear-related vein deposits - Au deposits - Gwillim Mine - Lac Shortt Mine - diverse features in a single area.
Hebert,R, Perrier.B, Giguere,C, Rocheleau,M, Gaudreau.R and Lacoste,P Gold mineralization related to a differentiated sill in the Abitibi
greenstone belt: the case of Sigma-2 project. GAC/MAC Prog.w.Abs. 11, 79 (1986). Quebec, Canada - Sigma-2 (formerly Vicour Gold Mines) is 10 km S.E. of
Val d'Or - ore confined to a differentiated mafic-to-felsic sill 360 m thick - from base to top; gabbro, amphibole gabbro, quartz diorite and granophyre - petrography. trace elements - shear zone - Au associated with sulphides - pyrite and arsenopyrite - tourmaline.
Hubert.0 and Ludden,JN Archaean wrench-fault tectonics in the Abitibi greenstone belt of Canada. In 'Workshop on the Tectonic Evolution of Greenstone Belts',
LPI Contrib. 584, 136+41pp.. 59-61 (1986). Archean Abitibi greenstone belt - structural geology - Quebec. Canada -
wrench faults - shear zones - age dates - sketch map.
Jolly, WT Relations between Archean lavas and intrusive bodies of the Abitibi
greenstone belt, Ontario-Quebec. In 'Volcanic Regimes in Canada' (Baragar,WRA. Coleman.LC and HalI,JM,
editors), GAC Spec.Publ. 16, 476pp., pp.311-330 (1977). Archean - Abitibi greenstone belt, Ontario and Quebec, Canada -
3-level volcanic stratigraphy; Mg spinifex and tholeiite at the base. Fe-enriched tholeiites in the middle, upper part with Fe-depleted rocks with similarities to orogenic caic-alkaline lavas - mafic end-members of the three suites thought to have undergone fractionation at high levels - rock analyses, EPM of pyroxene (partial analyses) - petrologic calculations - layered intrusions: Dore Lake.
Knuckey,MJ, Comba,CDA and Riverin,G Structure, metal zoning and alteration at the Millenbach deposit,
Noranda, Quebec. In 'Precambrian Sulphide Deposits' (Hutchinson,RW. Spence,CD and Franklin,JM,
editors). H.S. Robinson Memorial Vol., GAC Spec.Pap. 25. 791pp.. 255-295 (1982).
Quebec. Canada - Millenbach deposit in Archean andesitic and rhyolitic flows - rhyolite domes and massive sulphide lenses - individual lenses have cores rich in Cu grading out to margns rich in Zn - zoned deposits - zoned alteration: the alteration pipes under the lenses have a core of cordierite-anthophyllite or massive
Page 8
chlorite grading outward into a spotted biotite-rich zone Abitibi greenetone belt - maps - volcanic stratigraphy - massive sulphide - Cu Zn Ag Au grades and reserves - hydrothermal fluids - mass balance calculation - alteration on veinlete.
Lesher,CN, Goodwin.AN, Campbell.IH and Gorton.1P Trace-element geochemistry of ore-associated and barren. felsic metavolcanic
rocks in the Superior Province, Canada. CJES 23. 222-237 (1986). Archean felsic ■etavolcanics - Ontario and Quebec, Canada - relationship
between trace element distributions and massive sulphide ores - rocks divided into 3 major groups - REE - Y Zr Hf - Sr - Eu anomalies greenstone belts - REE patterns - Kidd Creek aine, Timmins - Confederation Lake - Sturgeon Lake - Kaaiskotia - Natagami Lake - Noranda - barren sites; Shoal Lake - Kakagi Lake - Lake of the Woods Wabigoon Lake - Bowman - Garrison - lisema - Skead - the Uchi. Abitibi and Wabigoon belts - La/Yb against Yb plots - variation diagrams - no systematicrelation between degree of HREE enrichment and size of an ore deposit.
Ludden.J. Hubert.0 and Gariepy.0 The tectonic evolution of the Abitibi greenetone belt of Canada. Geol.nag. 123. 153-166 (1986). Archean Abitibi greenstone belt. Ontario and Quebec. Canada - age dates
- plate tectonics - southern volcanic zone of belt is dominated by komatiitic to tholeiitic volcanic plateau and large bimodal mafic-felsic volcanic centres - the northern volcanic zone comprises 'basaltic to andesitic and dacitic subaqueous massive volcanics which are cored by comagmatic sill complexes and layered mafic-anorthositic plutonic complexes' - maps - variation diagrams - REE - trace elements - Grenville 'Front.
Ontario Geological Survey Lithostratigraphic map of the Abitibi subprovince. OGS Hap 2484 / Quebec HER map DV83-16 (1984). Nap of the Abitibi granite-greenstone belt, Ontario and Quebec. Canada -
bounded to the N. by the Quetico subprovince (mostly paragneisses) - bounded to the S. by the Grenville Front - it can be divided into a northern Internal Zone and a southern External zone - komatiite, tholeiite, calc-alkaline and alkaline volcanics - stratigraphy - map extends E. from Timmins. Kirkland Lake and Gowganda to Chibougamou.
Picard,C and Piboule.N Petrologic des roches volcaniques du sillon de roches vertes archeenes de
Natagami - Chibougamau a l'ouest de Chapais (Abitibi est. Quebec). 1. Le groupe basal de Roy.
CJES 23, 561-578 (in Fr.) (1986). Archean Abitibi greenstone belt, Quebec. Canada - basal volcanic Roy group
11 km thick volcanic series - initial calc-alkaline cycle followed by two more dominated by tholeiitic basaltic lavas - REE - trace elements - Th Ta Nb Zr - igneous petrogenesis - maps - igneous stratigraphy - whole-rock analyses - variation diagrams - HORB - metavolcanice.
Page 9
Robert.F and Brown.AC Progressive alteration associated with gold-quartz-tourmaline veins
at the Sigma mine, Abitibi greenstone belt, Quebec. Econ.Geol. 79, 393-399 (1984). Quebec.Canada - Sigma Au mine host rocks include andesitic flows.
porphyritic diorite intrusives and feldspar porphyry dykes - hostrocks have undergone greenechist metamorphism. but the veine are late and were less affected - three vein systems are chiefly composed of quartz and tourmaline - single and multiple generation veins occur - cryptic alteration occurs, incl. carbonate replacement of epidote - tourmaline may form upto 50% of the mode - it is often fractured, and veined by carbonate and locally by pyrrhotite - replacement textures - white mica may be replaced by carbonate and albite - the introduction of Au to wallrocks is closely associated with visible alteration - Au may occur in albite grains, in carbonate aggregates and in pressure shadows where quartz and carbonate fill in around porphyroblastic pyrite - it is assoc. with carbonate alteration and with second generation sulphides - carbonatization and Au postdate regional deformation and metamorphism - a timeecale is i)cryptic alteration, 2/tourmaline, 3)metasomatic pyrite and 4)visible alteration: Au came in during (4) and to some extent (3) - pyrite - structural and microstructural geology.
Robert.F and Brown.AC Archean gold-quartz vein formation and mineral deposition at the
Sigma Mine. Abitibi region, Quebec. GSA Abs.w.Progs. 16. 536 (1984). Sigma Mine, Abitibi greenstone belt - Quebec. Canada - veins emplaced
in late compressional tectonic event contain quartz. tourmaline. carbonates etc - native Au - richest veins occupy flat tension fractures and were emplaced by open space filling - paragenesis - Au was late - no evidence for remobilization - petrography - hydrothermal alteration.
Robert,F and Kelly,WC Gold mineralizing fluid at the Sigma Mine, Abitibi region, Quebec:
a fluid inclusion investigation. GSA Abs.w.Progs. 16, 636 (1984). Sigma Mine, Abitibi greenstone belt. Quebec, Canada - two generations
of pre-ore porphyries - ore paragenesis - three types of fluid inclusions of variable H2O and CO2 contents - hydrothermal fluids.
Rocheleau.M and Dimroth.E Petrology of the Archean Pontiac and Kewagama sediments and implications
for the stratigraphy of the southern Abitibi belt: discussion. CJES 22, 1374-1377 (1985). Quebec, Canada - Abitibi Belt - Archean greenstone belts - metasediments
greywacke - paragneiss - petrography - photomicrographs - chemistry of Archean sandstones - REE - microstructural geology - see also Lajoie and Ludden (ibid. 1377-1379).
Page 10
Sanefacon.R The Malartic district. In 'Structure and Gold. Rouyn to Val d'Or. Quebec (Hubert.0 and Robert,F
editors). GAC/MAC Field Trip Guide Book 14, 7Opp., 27-41 (1986). Malartic Au district. Quebec. Canada - Archean stratigraphy - Abitibi
greenetone belt - mineralogy - field trip road log - references - maps - Malartic nine.
Sawkins.FJ Metal Deposits in Relation to Plate Tectonics. Springer-Verlag. 325pp. (1984). Mineralization and plate tectonics - textbook review in terms of convergent and
divergent environments. collisional settings. etc - e.g. Archean greenetone belts. such as Abitibi (Ontario.Quebec) - Kidd Creek mine - Murchison belt, ** S.Africa - Yilgarn.Auetralia - Au - Hoaestake mine. S.Dakota - S isotopes - 34pp. of references.
Schoell.M and Wellmer.F-W Anomalous 13C depletion in early Precambrian graphites from Superior
Province. Canada. Nature 290. 696-699 (1981). Ontario and Quebec, Canada - graphite - C isotopes - Wabigoon. Wawa
and Abitibi greenetone belts - Archean C - very light C ascribed to organisms living on CO2 oxidized from CH4 formed by CH4-producing bacteria in stratified Precambrian seas - Michipicoten. Batchawana - kerogen. hydrocarbons - graphitic interflow sediments formed as relatively small pools: one horizon extend■ 1400 m. but the rest cover no more than a few hundred m each - this is in contrast to large sedimentary basins with extensive BIF - values of dl3C from -21.0 to -43.8o/oo, the latter the lightest reported Precambrian graphite. from Languedoc township - greenschist facies host rocks - graphitic nature of C indicated by pleochroism visible in individual flakes - 24 references. •
Springer. JS Carbon in Archean rocks of the Abitibi belt (Ontario - Quebec) and its
relation to gold distribution. CJES 22. 1945-1951 (1985). Archean Abitibi grsenstone belt. Ontario and Quebec. Canada - Au in
sedimentary black argillites with upto 5% C - Au in graphitic sediments occurs along quartz vein margins in sheared. altered areas - preferential deposition of Au in carbonaceous rocks by reduction at vein margins - natural carbons ■ay become surface-activated by shearing antby hydrohermal fluids - Owl Creek Mine. Timmins - Agnico Eagle - Moneta Porcupine - Coniaurum - Dome - McIntyre - Kerr Addison - black shales - gold in carbonaceous rocks.
Page 11
Tourigny,G and Hubert,C The Bousquet property. In 'Structure and Gold, Rouyn to Val d'Or. Quebec (Hubert,C and Robert.F
editors). GAC/MAC Field Trip Guide Book 14. 7Opp.. 12-25 (1986). Bousquet mining district, Archean Abitibi greenstone belt. Quebec. Canada
- pyrite found in eight lenticular auriferous bands on the Bousquet property - Au values associated with highly strained sections of Blake River volcanic pile - local geology - structural control on Au - field trip road log - glouroporphyritic basalt - two whole-rock analyses of basalte - chloritoid - tuffs - faults and shear zones - folds - tectonic layering - structural geology.
Tourigny.G, Hubert.C. Brown.AC and Crepeau.R Stratigraphy and structural geology of the Blake River Group at the
Bousquet Mine, Abitibi. Quebec. GAC/NAC Prog.w.Abs. 11. 137 (1986). Quebec. Canada - Archean Abitibi greenstone belt - greenschist facies
metavolcanics - Bousquet Au Mine - structural geology - shearing - mylonite zones.
Valliant.R1 and Barnett,RL Manganiferous garnet underlying the Bousquet gold orebody,Quebec:
metamorphosed manganese sediment as a guide to gold ore. CJES 19, 993-1010 (1982). Garnet - Au - Mn - Quebec Canada - prospecting - Mn/Fe in manganiferous
sediment near hydrothermal vent rises toward Au ore - Abitibi.
Valliant,R1, Mongeau.0 and Doucet.R The Bousquet pyritic gold deposit. Bousquet region, Quebec: descriptive
geology and preliminary interpretations on genesis. In CIN Spec.Vol. 24, 'Geology of Canadian Gold Deposits' (Hodder.RW and
Petruk,W editors). 41-49 (1982). Quebec Canada - stratiform pyrite lenses with native Au and Au Te ore -
Archean Abitibi greenstone belt - 3 lenses described - calaverite, petzite, altaite, chalcopyrite - rhyolite - breccia - Mn garnet - petrography - exhalite model - maps - photomicrographs - tuffs. chert, carbonaceous materials - pyrite.
Walker.SD and Cregheur.P The Chadbourne Mine, Noranda, Quebec: a gold-bearing breccia. In 'Geology of Canadian Gold Deposits' (Hodder,RW and Petruk,W editors),
CIMM Spec.Pub. 24, 58-66 (1982). Quebec Canada - Au deposit in breccia cutting mafic and felsic metavolcanics
in the Abitibi greentone belt - outcrop is 300x120 m and plunge is 80 degrees - cleats are of andesite (minor rhyolite) with quartz- sericite-carbonate rims and upto 30% pyrite - almost totally matrix- supported: matrix is quartz, albite, calcite, ankerite and dolomite, with accessory magnetite, hematite and tourmaline - the ore zone is funnel-shaped, cutting off abruptly against andesite and gradually into barren breccia - the lathlike clast forms. lack of comminution and en-echelon orientation of clasts deny an explosive origin - breccia formed by hydrofracturing by fluids along faults - pyrite - metals were leached from volcanic host rocks.
Page 12
Waleh,JJ Archean mafic metavolcanics from the Rouyn-Noranda district, Abitibi
greenstone belt, Quebec. l.hobility of the major elements: discussion. CJES 21. 261-253 (1984). Quebec Canada - alteration of pillow lavas - preferential growth of chlorite
relative to epidote may be controlled by high CO2 concentrations in the mobile phase (but see Colinas and Trudel 1984) .
APPENDIX A
Drill Bit Statistics
Ezr.;;q2,uçczs
Sarvice Oe la GOoinforrnation
l Date 27 MR. 1987
No G.M. 44:177
APPENDIX A
Bits Consumed
Bit Number Footage (ft) Number of Holes
CB68040 CB68041 CB68043 CB68044 CB68034
(42 sent back)
188.5 244.5 249 233 106.5
1 2 3 2 3/4 lâ
CB68035 265 3 CB68036 445.5 8 CB68037 304 3 CB68038 474 5 CB68039 546 6 CB67802 361 3 CB67803 216 2 CB67804 404 5 CB67805 291 4 CB67806 368 5 CB67807 217 2 CB67796 340 3 CB67797 494.5 6 CB67798 403 6i CB67799 88 12 CB67800 229 2 3/4 CB67801 (50 sent back) 250 3 CB67851 146 2! CB67852 101 1! CB67853 81 14 CB67854 250 4 CB67855 371 6 CB67856 212 4 CB67857 208 4 CB67858 325 4 CB67859 368 4 CB67860 356 3 C000176 81 2/3 C000177 28.5 1/3 C000178 205 2 C000179 120 1
- 2 -
Bit Number Footage (ft) Number of Holes
B67920 27 1/8 B67921 198 1 3/4 B67922 191 2 1/8 B67923 1 0 B67924 133 1 B67925 107 1 B67906 210 2
43 Bits 10,437 124
Average Depth = 84.2 ft
Average Footage/Bit = 10437 divided by 43 = 242.7 ft
Note: 33 days drilling time = 316 ft/day
APPENDIX B
Heavy Mineral Processing Results
TABLE *10 TABLE TABLE SPLIT CHIPS FEED CONC
M.I. CONC. NON LIGHTS TOTAL MAO MAE V.S. PPB
ViS GR LS OT SC'
NO. CALC SIZE ; S/•.; SO ST CY COLOR
-ILL TILL
TI!L T
ILL IrL
-IL- TILL TILL TILL TILL TILL TILL TILLf2DK
TILLTILL :AND SAND _ A4,_
TILL rl Br=:
TILL TILL SAND
uFH-v-2i8
M=;H7v°.;d. 36
SA=L2';EIGHT (K3.WET)
OVERBURDEN DRILLING MANAGEMENT _:MiTE.,
LABORATORY SAMPLE LOG
WEIGHT (GRAMS DRY) AU DESCRIPTION
!1. I. CONC CLAST MAiK I :Z
NA 353 NA 57
533 NA 49 NA
01-1▪ ,2,2A 13.2 0.4 17.8 -3. :i, 4, A 12.0 0.1 17.5
-5.5A,6 11.8 .." 11.3 -
~..^:..f1 13. : üa l: 13.4
-5.A, 1 :', iû: Z. : 0.3 22.0 -11.12.ri 15.7 ..4 15.3 -114 ..4 0.1 7.3
-,_,14 12.9 0.2 i' 1~.7 -1_fi 1- 2.0 +1.0 2.0 -15,16 11.2 0.4 11.4
-17,IE.r+ 14,2 0.6 12.6 -19 ;,.. 0.1 5.3 -r. ,.._ .,. 6.0 --_ 6.1 0.2 5.9 -22 8.2 11.2 6.6 -r. 1.1 0.1 1.0 - ' : 6.'
..-~,~_ ~. ..r . -02 0.7 0L5 6.= 0_ 5.7 0.0 J.. -04 6.2 0.0 6.8
- - 6'6 'Ÿ'., 0.6 - _ ..._ 0.2 6.0
-07,7A 7A ,2.0 0.7 11.3
.7-01.:2 ..... ..' 12.6 -. n4 6.7 0.2 6.7
-05.06 11.7 0.1 11.6
-7.72 .7.4 ..4 1..0
-07:10 10-7 0.4 ?. -11.11A 1::.. ... 7.0 -12,12A 10.2 1.2 3.6
1
r - r 1r
-17,17A - ,r . ,: , ..- .~ 04-::1.02 . -.1. r 14. :.
-07,04 _... 0.6 '__..
-02.:6 .-.3 0.4 .`,.1 1:
-070-23 --•_ .._ 11.2 -.- ,r.r -." 12,2 -. r 11.. 0.5 11t1.
-i4 5.9 0.1 5.2
~Ç-....r . ... ..4
-.. .:, ..- 6.9
-.. ..r _.4
-02,02A .-. ..r 9.7
263.7 297.6 103.8 85.7 158.9 316.6 49.7 152.5 39._
J 186e ~ 1?C
121.. 106.3 104.1 13L, ~n ._ 72.3 109.4 17A n 1t4.? 106.` 107.5 97.5 97.3 175.1 016 r,e7.r
121.1 205.7 12,.".., 1_,..5 102.0 i1-.:. 277.2 ,..C" 123.0 r27..
~ L42.2 •64.: 44.7 a0.r
i36.117.4
,2^v..: 147.5
'r` 223 .3 4ti1.4 22.1 :3.3 0 238.4 61.2 35.4 25.3 79.2 24.6 12.4 12.2 0 54.2 31.5 17.6 13.9 I 106.1 52.8 32.0 20.8 1 278.9 37.7 18.6 19.1 1
37.1 12.6 6.2 5.8 0 137.5 25.4 13.1 12.3 29.9 9.4 6.6 2.8 171.0 15.3 7.7 8.1 190.0 35.0 18.7 20.3 107.1. 14.6 7.8 6.8 88.0 13.3 9.7 2.6 77.6 26.5 15.7 11.2 106.1 26.1 15.5 10.6 70.3 2.0 1.7 0.7 83.8 25.6 12.3 13.3 148.4 26.5 15.9 10.0 79.7 27.2 19.8 7.4 C 87.5 20.0 12.6 7.4 0 79.3 17.7 11.6 6.1 '0 77.4 20.4 12.4 2.0 113.9 25.2 14.9 10.3 152.2 45.4 25.4 20.0 60.0 19.6' .12.1 7.5 100.0 21.1 14.4 6.7
1 17.4 iv7. 4 .w3. 3 20.9 71.2 71.4 19.0 12.4
.03.. 28.2 11.3 16.9 46.3 56.3 70.0 36.7 189.0 30.5 15.5 15.0 211.0 22.2 13.6 15.2 95.2 42.7 24. T 12.0 177.: i.. 47. :' 24.3 22.3 132.5 96.3 42.6 54.2 103.1 37.7 27.5 16.2 105.4 59.3 32.3 r.._ ._.. 6.6 2.6 4.0 --•- 4.9 1.E 0.1
107.1 _,.r 15.4 15.4 101. - .2.1 11,4 ,. 74.. 10.7 7.4 3.5 ..., r.... 17.5 12.0
117.2 :.1.., 16.7 13,6
Oli' 40 90 8^ J 20 80 7! 75 NA
NA J 90 NA G/BL j5 NA $/P 70 NA r 70 NA C 70 NA G Bl.% NA C.'Bt' 98 NA F 60 y NA P 75 NA TF, NA NA NA NA NA TR NA NA F .:r1 NA Cirk: 9E AA 'P 70 5ÿ P 60
946~ D 75
F 70 57 G 30 NA O; DL 75
312 ?/BL 90 NA C 90 27 F' 9': NA P 732 P NA P NA P 847 F NA TR NA % NA n'r ^ L r_. L NA ..n r ~~~.l:
NA C 1 1 1_ _
ü
20 60 10 20 20 20 25 Y
Np 10
~~ 30 30 20
4;; 25 NA NA NA 20
Y Y Y si
F
,, ,,
30 NA NA Y 40 NA C? 25 NA A F 30 NA NA 1{1'} „A ~ NA
7; ,ir. }i: 10 NA N1? Y 10 NA NA 10 NA NA Y 10 NA NA 5 NA NA Li
.ti
U 5 NANA ` !~' ', } ~' • A i Li
' ,.
.: \ . NA NA J v Nx? NA . . . . S M i: .... AM 4 i 1
15 _-
NA ,l. i+y U
10 NA NA ... NM NA L' ,. NA ...
.ÿ .
70 NA NA U
NA NA N'r`. Nx~~. NA NA NA NA N;., NA
NA NA NA ,r 11h
NN NA NA ..n i•ir.
NA NA ~
NA NA
NA NA NA NA NA NA NA NA NA NA NA NA NA RA
NA NA NA NA NA. NA NA NA NN
Y
Y
Y Y E Y Y Y Y P
Y Y` B Y Y B
Y Y = 7
E , :
Y _ C_ B
y w R
. . B E Y `i : YYB _ '` :i i E . Y` : _
Y 3: 32 Y YB E Yl r _
' 3B 33 Y ..,
Y -: a Y Y "_ S: Y Y R
Y i ✓
: : V GE 35
32 t3: Y S:
jj :.. _r
Y Y Y 53 53
, 2 J. _.
•!
Y
Y
E B
B
B
Y
TILLfELD T1, -.Hr_ -r~
~ T! TILL
TILL ,-_ TILL ?AND 2H!V. TILL .L-
DESCRIPTION .LAS_
OVERBURDEN DRILLING MANAGEMENT LIMITED
LABORATORY SAMPLE LOG
WEIGHT `GRAMS DRY) AU
CLAST MATRIX M. I. CONC
SAMPLE WEIGHT (h:G.W:T)
MFH-,.-878 06;27/ St .
===
TABLE +10 TABLE TABLE M.I. CONC. NON NO, CALC SIZE .. S/U SD SPLIT CHIPS FEED CONC LIGHTS TOTAL MAG MA6 V.G. PPB
VIS GR L5 OT ED
H-56 07-01,02 14.7 -03,04 13.8
-05,06 9.3 v8-01i" 11.6 ''' -03 ,04 14.4 -05,06 12.9
.r+7 7.8
-05 :i.v
-09 7.4 ri9-iJ 1,li_ . 14.8 -07,04 1:.E3
-05.06,07 2+A.22.5
-05.09,5A
-1J.11 12.9 . e~
-:~ o.9
-SJiT 3.1 w
-14 ~. r( 10-1,2,2A 21.4
-v3 11-01.02 14.: -03,04 14.5
if6 14.0 -05,06
-07 7.4
-tî6 c.5 12-1,2,3 ii'. ;} -04.05 14.3
0.6 0.6 0.3 0.6 0.6 0.5 0.3 0.4 0.7 0.9 0.4 ..0
1.0 0.3 .i C.2 0.3 0,5
0.3 0.4 O. 6 i;.4 0.4 ._
3.5 1:1.2
14.1 179.9
13.2 199.3
9.0 126.1
11.2 232.6
13.8 227.2
12.4 178.4
7.5 169.5
5.4 142.9
7.. 72.9
14.0 244.9
12.4 176.4
21.9 267.9
21.:; 231.5
12.b 189.9 ..,
6.5 :iJ.S
29 .7 84. ..
2.2 54.5
20.9 276.9
o.7 110.9
14.2 13:1.6 RT 13.5 c~:4.µ
i3.6 96.6
7.: 214.5
6.3 177.3
16.5 135.4
14.1 97.5
141.4 164.6 72.2
19` ^ J. r 190.0 147.7 146.5 117.9 57.2 193.7 141.0 229... 159.6 161.3 104.7 76.4 14.2
213.3 91.5 140.1 192.4 64.4 165.. 150.0 100.0 69.4
38.5 34` •J 35.5 37.4 :r.2 30.7 22.7 25.0 15.7 51.2 35.4 40.7 71.5 28.6 18.5
A,~J.:
4+~. Y 57.6 19.4 40.5 42.0 32._ 49... ..~
35.4 28.1
2Ÿ.J 19.1 18.8 22.4 22.6 15.4 14.0 16.7 12.1 28.0 18.. 19., 41:? 15.. 9.8 5.5
,:9.,. 72.8 1:.I 21.4 21.2 15.3 19.7 18.4 18.0 12.E
18.2 15.4 17.1 15.0 14.6 15.3 8.7 8.7 3.6
23. _
17.1 20.8 70.7 LJ.. 9.0 2.. 1.0
24.8 6.: 19.1 70.E 16.3 29.5 8.9 17.4 . 15.7
1 1 0 0 0 0 0 1 i+
:
= .
1
74 20 NA NA NA NA NA
235 NA 23 NA NA
482 98 295 NA j~ NA 236 NA NA
237 98 NA NA
1096 NA
C SO C 90 C 30 C 95 C 95 C 95 C 100 C 100 C 100 C 90 C 80 C 60 C 70 C 70 C 80
CiBL 95 C/L+K 95 P 75 C BO P 50 L 65 P 80
G 85 G 90 6 80 G 90
20 10 70 5 5 5
Tr; T~ TR 10 20 40 30 30 20 5 5 25 20 20 15 20 15 10 20 10
NA 14F1 NA lrr, NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA
NA NA NA
NA NA NA NA f~
NA NA NA NA NA NA NA NA NA NA NA L .f. NA NA NA NA NA NA
U U U U U {1 1~
U J
U
U U U
U
U ., i.,; !
L1
J
U
U ;? 1: L
Y Y Y Y Y Y Y
Y ,;
Y
Y
Y 'Y
Y
Y Y .
Y
Y Y
Y i
Y
Y Y Y
Y
Y
Y
i
Y
Y Y
Y
Y
Y
Y
i
B B
B .^"
1 n GB ~
B
~ E GE Ÿ9
:3::
SR Cr GE SE 63 GB EB
ST CY COLOR ~
yY.
r-1
B
58 58 9= GL! GB Gç iE GE
TIL .i.: ,
TILL TILL
b7 ta
a r
~ R
] R
a W
ts
+ [1
+ t
i t W
r„p
TILL TILL TILL TILL
TILL -Tr
7-
e+eee
22 CLA g 2Ig2a
2;23 22 FROM SHAKING 9@2 AND PANNING
ÆLiiiITLN.k NUMBS OF æ@Æ
ABRADED IRREGULAR DELICATE NON CALC V.5.
a93 # PANNED -----~ — MAS ASSAY 9N DIAMETER THICKNESS . P, F T PTUT% SÆ Fa REMARKS
ee 2& 3.& N NO VISIBLE ÆG
-3Æl 404 3X 3 !c 1 ! EST: RPYRITE D Z s 2: 1 1 ROTO RE #110 3 X 100 5 c ! 1 75 X 13 & [ 1 1 !æ w !m & : ! ! !m w 13 2 c ! ! : !m X 12 2 C ! !
TOTAL E 75.4 35:
2.5AJ N NO VISIBLE SOLD
gJ,g N 2 X 100 2 E 1 !.
TOTAL 1 17.6 .S
96JCA N &X 100 5c 1 1
TOTAL ! 32.0 2
&42/ i 3z 23 5 ! ! EST: 5% PYRITE 3X 3 æ2 . ! 50 50 SE I ! 2X 2 2: ! ! im t 150 3 [ i ! 13 X 200 2 e ! !
TOTAL 6 18.6 537
-11 ; S 22BLE SOLD
-17,14 & 2 K!S 3 2 1 1
TOTAL 1 13.1 R
M9 ; NC VISIBLE g2
-3d6 N NC VISIBLE SOLD
K7,E3
e7
e,
N
;
.
S VISIBLE SLD
NO G:IBL : SOLD
3 VISIBLE SS
MrÎH-C-Sf! S ,:i6/231H
GOLD CLASSIFICATION
..3:--- GOLD FROM EiiAK:E TABLE AND PANNING
M„ Hti23LN. S5 NUMBER OF 6FcA I NS
SAMPLE #
-21
PANNED YIN
N
ABBRADED •
IRkEGULAF :iELICATE UC:i !1A6 6MS
CALC V.6. ASSAY PPB REMARKS T F T P T F TOTAL DIAMETER TtIICKNESS
NO .SIBLE GOLD
-22 N NC VISIBLE GOLD
NO VISIBLE GOLD
02-01 N NO VISIBLE GOLD
-':C :r` NO VISIFLE BOLfi
=03 N NO VISIBLE GOLD
-04 N NO VISIBLE SOLD
N NO VISIBLE GOLD
-06 N NO VISIBLE SOLD
-07,07A .;.~ïA N NO VISIBLE GOLD
.7-01,02 N NO VISIBLE GOLD
N SO h 100 15 C 1 1
TOTAL 1 12.1 53
N NO 'iISIBLE GOLD
-07.36 25 X 25 5 C 1 1 EST. 3 PYRITE 25 X50 r--
C 1 1
25 75 .r'4 1 1 2
C•~ X. ,C
. iv i ii~ + 't. n
. 1 ..
125 250 36 1 1 r
15. Y 225 36 C 1 1
TOTAL 20.9 946
-.-._, F`. „i:. .. 125 13 ,., 1 :
r TOTAL . 1 19.0 53
-y 114. ": _ . _c:FLE 6Ou
r --:..:. 1:5 " -_. _ 1 1
• t~ini T-.-,- 1 -. _ : t. _.-
PA;. 7 MPH-C-275~-4-~!G 6i'_7186--
GOLD CLASSIFICATION
VISIBLE GOLD FnCM SHAKING TABLE AND FANNING
M-;4:2311N.B6 NUMBER OF GRAINS
ABBRf1trE) IRREGULAR DELICATE t NON CALC V. G. SA,... - MAG ASSAY • •rû 4; FANNED
Yi N DIAMETER THIC!t.NEâS T P T P T P TOTAL GMS FP: REMARKS
~vL
-1:.13A N NO VISIBLE GOLD
li4-01,+3a N aV X 75 13 C 1
TOTAL 1 13.6 27
-03,04 N NO 1,'ISIBLE GOLD
-055:6 N 175 X 300 44 C 1 1
TOTAL . 24.3
-07,0E N NO VISIBLE GOLD
-0.1+ N NO VISIBLE GOLD
25 X 25 S C 5i:: X 50 14 C
1.0 X 125 22 C 1
10e X 175 27 C
''~ X 250 44 C 1
1
2 1 ~ ~ 1
EST: ; 0,, . + . . _
TOTAL 6 78.8 642
-1: i 'rît VISIBLE GOLD
-14 "iO VISIBLE GOLD
EST: B4.: PYRITE
.,`-':1.02 N NO VISIBLE GOLD
ii~-,C ,
:. ~ .v`r ...~ R t~.+ _ ~ ,.
TOTAL 1 :6.4
-04 N "r:; VISIBLE GOLD
°`v VISIBLE -- -- .._L-
25 .. ~ 1 C
TOTAL - 16.7 11
TOTAL
=ti .. -5 ._ I
1
`HE 4 MPH-0-675 06/27:36 „_
130! _. CLASSIFICATION
VISIBLE SOLD FROM SHAKING TABLE AND FANNING
ii[Ln1.JL \.r56 NUMBER OF GRAINS
_ aitrFiA6ED IRREGULAR DELICATE NON CALC 'J. 6.
5AMFL: x PANNED - NAG ASSAY
YIN DIAMETER THICKNESS T F T F T F TOTAL 6MS PPB REMARKS
HBé
N
N
tiO NO VISIBLE
NO VISIBLE GOLD
TOTAL 1 19.1 20
-03,04 N NO VISIBLE GOLD
N NE VISIBLE GELD
-07 N NO VISIBLE GOLD
-05 I'; 75 X 200 27 C 1
TOTAL 1 18.3 235
-05 N NO VISIBLE GOLD
09-01.02 "= 50 X 100 15 C 1 1
TOTAL 1 26.0 .3
-03. 04 N NO VISIBLE GOLD
-05.06,07 N NO VISiBLE SOLD
-02.09,A 25 x 50 8 C 1 1 EST: 574 PYRITE 50 X. 75 13 1 1 2GnA3:IS 64^.LENF! 75 X 300 36 C 1 1
5,:. , 10,)~: :, _ . `_ _ •1 1 100 X 12.: ~._ C : 1 .25 % .75 29 ., i 1
TOTAL 41:2 482
.--...._ 50 1 150 20 1 1
r. TOTAL1 15.3 :C
-.- N _iÏ'+ :i __il 25! 0
TOTAL . 7.,. 29_
-.- N VI5IBLE GOLD
-_- . NV VISIBLE _-.L -.... _... PYRITE
LE: F¥SB7E
3017 Æ@sE@Sæ
Q£±E 32 FROM SHAKING TABLE a2 FANNING
¥+2æ.86
SAMPLE # FANNED ¥a DIAMETER THICKNESS
NUMBER OF GRAINS
ABBRADED IRREGULAR DELICATE NON MAG mS
CALE Y. G. ASSAY E2 REMARKS
~-- T P I P I P 2TÆ
10-1,2.A N 13 * 250 34 : 1 1
TOTAL ! 72. 26
-03 N K VISIBLE GOLD
1191,02 N Æ VISIBLE GOLD
-03.9 N 75 225 2 E I !
TOTAL 1 21.2 22
wtà N 7!l 'IC 2: 1 1
TOTAL 1 ~:3 a
27 N NO VISIBLE Gap
-OE N Æ VISIBLE GOLD
12-E2,3 Y 3«!m 2E 1 1 EST: •1m PYR I7
13 X 300 @ [ 1 1
TOTAL 2 18.0 1096
w405 N NO VISIBLE GOLD
,
,..7HH23siN.2.6 CVERSURDEN DRILLING MANA:EL:Y:NT LIMITE:
LTC 96 EAMPL; iCE
WEIGHT (BRAME DRY) AU n;SCRIPTIGN
r-^
74ELE: -10 SFLI7 CHIFS
TABLE 22NC LIGHTS
m L aL:Itia
V.G.
2LA5T MATRIX
EIU GD ST : 231L29 ======
2ONC. NON TOTAL MAG
7AL2 8IZS h
F877, ;FE =
VIS GR LE 7:7 E:
7!-S: 14.1 3703 :3.4 25.1 12.3 :f,: et( NA 3 90 10 NA NA !J Y 2:
11.1 C.: 10.9 79,3 56.3 23.0 12.4 9.: NA 2 30 20 Ni; NA L Y 25 T:LL 57.2 15.7 IO.: 5.: NA 2 90 10 ;VI NA 1.1 V GE 7:LL
17-01,02 17.5 0.2 17.: 131.0 106.1 44.9 22.6 NA F 40 60 NA Ni; GE TILL C:,4.5 .i.f 1.1 217.7 1:7.2 55.5 28.9 2.6.6 NA F. ,O 4:: NA NA Y Y 3: 22 7:
14.9 0,3 14.6 132.7 131.5 51.2 2:.7 24.5 NA : 70 30 Ni; 2: -0,E 7.: 0.2 7.0 141.: 112.5 29.1 12.2 IC. 5 1. NA CIEL Fi 7.0 Ni; Ni;
U
ii
5.2 35,9 72.4 10.5 4.: Ni; ClSK 95 5 t.A NA L 7 L.4 :3 7 14-01. iA 11.
5
fl
.9 i1.4 1:0.3 M.: 77.0 15.c IA 2 FO 10 NA NA Y Y 3E 33 7ILL
..:A :A
.8 11.:
3.4 0. 4
3.4 10,9
2210 'L'07.0
115.6 170.9
:07.3 :6.1
57.5 19.5 18.1
NA 2 :5 NA F 70
7 30
NA !'-iA
Ni; NA
V
Y Y 62,
52 TILL 7ILL
13.8 C;.: 13.2 1E:5.7 126.9 :1.8 15.3 16.7 IA 2 30 20 NA NA Y Y 3E GE 127.3 104.1 23.8 12.4 11.4 Ni; C 90 10 NA NA L Y Y 3E 23 7ILL
:4.1 146.4 115.3 30.5 • 15.0 15,5 67 P 50 20 NA MA U 6.3 92.1 :3.5 22.6 11.7 10.9 32 : 50 20 !,S1 NA 7-'
S -- -04 3.:
4.9 0.2 0.:
4.9 4.7
92:1 34.5
7.7 15.3
18.4 14.6
10.: 9.:
8.1 50)
Ni; 2 90 Ni; CIBK 20
10 20
NA Ni;
Ni;. NA Y
Y GE 32
22 2E TILL/22.:.
3-01 5.3 0.1 5.2 101.1 72.0 23.1 14.3 5.0 95 ; 90 10 NA Ni; -Y Y Y i3Ei 5.6 s:.: :1.5 21.3 12.7 S.: NA P 90 10 Ni; NA Y 7ILL
102.3 77.2 25.1 12.1 13.0 NA 9. 25 15 Ni; Ni; Y 'y Y 21-.'; 22 6.5 65.5 45.8 19.7 6.4 NA P 23. 15 NA NA Yi 35
21-01,11 -07,04
14,8 12.7 0.3
14.2 12.3
166.6 115,5
144.0 55.7
22.: 26.9
10. 77 14.2
11.; 12.:
NA 3 30
74E 2 30 10 10
Ni; NA
NA NA
Li Y Y Y af.
35 32
-05 2.9 0.2 J. 47.3 "Z.2 12.1 2.E 7.3 / 2 772 BK 100 o NA NA Y "7: GE 2 7:3 0.: 7.1 Bs .7 72.5 16.2 2.7 7.3 7.1 74 F 90 10 NA !%.14 Li EE ; 0.3 6.. 6 36.3 24,0 12.3 4.7 NA 90 10 NA NA J Y
5.7 110.5 26,4 24.4 10„3 NA G 30 10 - iPt N.A .11
.4.4 179,3 1:1.2 44.2 24.9 13.7, il Ni; 3 33 1 g. NA Y 7,4 48,0 40.0 8,0 5.1 2.; Ni; 3/ 100 NA Ni; J
-
GC:LC CLASSIFIOATION ================
r- J:74-.SLE SOL: FROM SHAING TABLE AND PANNING
%MEER, OF SRAINE
ASERADED IRREGULAR DELICATE NON CC V.G.
* FAAED ____---- MAG A55AY
DIAMETER THICKNESS T F T T P TOTAL GMS FRB REMARKS r•—•
7T.1 ',-ISISLB SOLD
N NO VIEIBLE GOLD
-)E N NO ABIEIF GOLL r-
N NO VISIBLE SOLD
-C,4,5 N NO VIEILE GOLD
N NC VISIBLE SOLD
r- NO VIEIELE SOLD
NO VIGIBLE GoL: r-
N NO VISIBLE GOLD
:5-C)1,1A NO VIEIELE GOLD FYRITE 77. ARSENCRYFITE , !-!:STL • FINS:
FvFAHOTITI
r- NO VISIBLE SOLD ) )
N NO VIRIP4 F SOLD
N NO VISIBLE GOLD
X IN 15 C 1 1 r-
i T';L I 15.
r- 5) X 75 17 C )
TOTAL 1 11.7
N 'THIELE
v:E:ELE OLD
Trrra, 14.5
NO VIE:ELE
r-
t
•2:L2 OLASEIFICATIO
:ISIS'R SDL: F3CM EHAKING TABLE AND PANNING
N4.'44'7
NUMBER OF GRAINS
ABBRADED IRRESULAR DELICATE NON :ALE Y.S.
* FAN7D ======== ========= ========
ME AY
Y/N DIAMETER THICKNESS T TPTPTOTAL GMS FRB REMARKS
NG ASISLE ELD
-C: N Ni VISIBLE GOLD
21-0:,02 N NO VISIBLE GOLD
-C3,04 N 100 X 200 29 r
TOTAL I14.2 748
2! X
CZ!. rrh,Lri:
75 X 175 :5 C 1
TOTAL 2 5.8
22-C1
75 X 7. iC
1
TOTAL I 8.7 74
-0: N VISIBLE GOLD
2:-01 NC VISIBLE SOLD EST: In PYRITE
Y NO VISIBLE ECU EST: :0% PYRITE
:5-01 N VI:I:LE :OLD
r-
r-
r-
:AMPLE • 2i4.T :.KG.WET) NEIEHT (BRANS DRY) AU .•••MnIfflf
r-
r-
r-
fr-
rr
r-
r-
r-
f--
:1-07
23-02. -04
-06
26-0 ..
23-01
77-01. )2 -07
74-01,02 75-01,02 -07.7)4 - :6
76-01
-f.:7,.04
77-1 12-01 72-C2
TALE +10 TABLE TABLE M.:. CON.C. NON SPLIT CHIPS FEED CONC ; 1EHTS TCTA.L NAG MAO
17:: 0.5 12.8 127.8 61.6 5.6 0.2 5.4 116.8 95.0
0.2 6.0 159.2 135.0 2.2 0.0 2.2 124.2 117.8
0.7 6.5 187.7 114.2 4.3 3 4.0 :01.6 191.2 6.1 0.7 5.2 111.: 86.0
24e. 4 203.2 7.2 0.2 7,0 155.7 126.5
:1.7 0.2 t.:1.5 11E.1 59.2 12.3 0.2 12.6 6.6.5 47.9 7.2 6.8 117.8 75.0 7.6 0.2 3.4 72.1 56.4
:1.5 0.1 11.4 140.5 101.1 12.6 0.4 12.2 116.2 82.5 :5.2 0.4 14.8 164.2 115.5 14.3 0.6 14.3 :51.5 107.3
0.1 7.4 74.: 55.3 11.2 0.3 10: :47.1 106.0 6.4 0.2 6.2 123.0 100.4
0.4 6.5 49.: 122.9 _5.7 0.4 14.9 157.5 3.E 0.! 5.7 47.9 41.2 7,5 0.1 7.3 - 104.3 6.9 0.1 6.8 207.1 168.5 7.0 0.: 6.7 161.4 134.7
14.1 245.; 136.4 :25.5 26.0
0.2 7.7 11..5 73.4 123.3 116.1
0.7 7.5 2712 : 107.. 80.0
7.1 16..5 131.1 4.1 126.6 1O0.1
o, 4 14.2 136.5 7.5 0.7 7.2 122.-
11,1 7 10.5 27..4 4,3 B0.4
1 2.3 75.6 66.2 5.6 62,0
.1, 31.3 70:5 6.5 7.f 32. G
77.4 7.4 7.. 1:1,7
172. -6
41.1 13.9 21.8 13.5 24.1 14.3 6.4 4.8
68.9 66.6 9.8 5.8
25.2 13.2 31.2 16.2 1E8 14.4 58.9 42.3 20.6 12.0 34.8 22.0 15.7 3.7
• 39.4 21.0 33.7 18.6 43.7 27.3 44.2 22.5 18.9 10.3 37.1 23.0 28.6 16.2 26.7 15.2 45.5 25.6 6.7 4.3.
27.1 15.5 74.7 20.4 26.7 15.9 52.5 26.5 47,7 27,6 38.5 17.3 77.2 57.5
143.. 120.5 29.1 16.1 70.4 16,4 26,5 15.6
34...1 26.1 17.: 3,4 6.7
2E 9 .6.7 L. 4 12.E 25: 7 15.3 74.4 20. ;
M. 1. CONC
27.3 3.7 9.; 1.6 n-
4.0 12.0 15.0 14.4 16.6 8.6
12.8 6.0
18.4 15.1 21.4 21.7 8.6
14.: 12.0 1C,.5 :9.9 1.8
11.6 14.3 10.8
20.7 ,/ :0.- .t.: ::.t 17. O< :A.
Afr
2,2 7.1
2.6 .,?" :..2 iL :
NO. 7.8.
or
AEE.. 1 - :7UTEL
'5-7!1L.L. 86 CVERBURDEN DRILLINE MA'ASEMENT LIMITED
LABORATORY 6 4FLE LOS
.=LRIPTION
7LAST
E
771X
St CALO 3:71 FFE4
V/S ER LS OT
NA G 90 10 NA NA Li Y Y 22 Si TIL NA 6 95 5 NA AA U Y 32 E TILL NA 3 93 5 NA NA U NA TP NA NA NA NA J Y 3 3 TILL NA BDK 100 0 NA NA U EY TILL/E,K NA 19 /8K 90 10 NA NA û Y Si GS AA P 35 15 NA NA il f Y i 23 P 50 10 NA NA U Y Y Y NA P 85 15 NA NA U NA GP 90 10 NA NA Li NA G/P SO 20 NA NA U Y Y 22 22 TILL NA P 90 10 NA NA Y Y E E 73i:4 NA P 30 10 NA NA U NA S/P 90 10 NA NA U Y Y 3 GY TILL
1960 SiF 30 10 NA MAUi S B - TILL 222 3/P 20 20 NA NA U Y '7' TIL1. NA GIF 60 20 NA NA ii : 3TILL NAG!P 60 20 NA NA. U Y Y i TILL 61 P 60 20 MA NA U TILL NA 6/P 50 20 NA NA U Y 3 2 TILL 41 F,1 95 5 NA NA Li Bri 3E TILL NA P/E 80 20 NA !A U Y Y 2B. 23 TILL
550 3 90 10 NA NA Y Y GY 22 7ILL 3279 F 60 20 NA NA û f Y 22 2E. TIL
NA P SO :0 NA lA U f- Y E 3: TILL NA P 80 20 NA NA U Y Y E 447 P 90 10 NA NA U
P 30 10 NA NA Y 387 F 6c.; NA NA 17: F 20 TO NA NA ? 6
NA F 30 IC NA NA Y Y NA P 90 10 NA NA !l Y
272 P 95 5 NA NA U Y Y Ni; F 90 10 NA NA f f 76 .3 7-• 95 NA .*4 7.7 36 7: P 30 10 NA NA Y-
I5Z P 50 :0 NA NA Y 2.2 22 7: LL. P 9f f 'AP. NP Y 32 32 7 :
NA P 100 TR NA AA: IJ 3Y 3Y Li.-
NA 7.
NA TF. 60 40 NA NA Y 3N 33' T NA NA 'A •
NA P TO 12 'Y 32 38 3 70 :0 NA :\iA il Y
FA27 2 .117+ - _T011E.
SALE NO.
ii2H ;,KG.677) W71347 (BRAME
OV;RBURDEN DRILLIN5
LABORATORY
DRY)
MANAHMENT LIMITEZ
EAMPI ;
AU DE52RIFTION A33
TAS' '674 17
,10 TABLE HI76 F77-0
TABLE CCNC
M.
M.1. CCN. 1 IGHT6 TOTAL
1. CONC
NO. V.S.
CLA3T !.147P,D.
2,,OLCE NON MAS MA5
CAL: SIZE PPE
ED 37 2.'!.
VIE GR LE .7 a: 2-
6.7 102.5 70.9 71.5 15.5 16.4 r NA P/G 80 20 NA LI Y Y Y 33 EE TiLL
17-01 2.7 0.2 2.5 06.0 54.1 11.7. 7.4 4.5 NA P 20 NA NA U Y Y Y E3 EE TILL
-01A 7.9 0.3 7.4 109.7 72.2 37.5 27.3 17.7 .1.r. NA PIS BO 20 NA NA U Y Y 9B 31 7:L_ 1E-01,0: 15.3 0,7 15.0 179.: 75.6 67.5 34.9 :5.6 NA P 20 20 NA NA \ 'Y Y 35 EE TILL
-07 6.0 0.5 7.5 17. b 147.6' 18.3 15.8 NA G 60 40 NA NA Y Y Ei EE TILL
-04 7.4 0.4 7.0 1;3.2 75.4 75.8 21.5 14.7 NA 6 50 20 NA NA L! Y Y Y SE 132
-05 T. 0.7 6.8 86.2 cA c 30.7 15.5 14.8 NA 5,0 .4A NA Li Y EB TILL -06 7.4
2.6 0.2 7.2 61.4 15.1 47.3 34.7 6.6 M NA 50 20 NA ,A
4M U Y Y EE Ei TILL
45-01,02 .. 2.0 77.0 51.0 26.0 15.0 11.0 1445 P SO X NA IA Y Y Ei Ei ?IL-
5c..--01.02 12.1 0.7 11.4 147.7 114.5 37.0 17.2 15.8 -1 87 P 80 20 NA NA y Y 32 EE TILL
31-01A 1.7 0.0 1. Z 3E.7 5.0 3.9 3.0 0.9 0 NA TR NA NA NA NA U 'Y Y 3E GE TILL
77.0 9,9 5.7 4.2 0 NA P 90 10 NA NA U Y 'Y Y EE EE TILL
52-01,g 6.7 0.4 6.3 36.6 7.2 19. 11 10.0 9.4 . 1 150 6 10 NA NA Y Y. Y 33 3E 'ILL
-01 7.7 0.2 .7.1 104.6 56.7 17.9 9.8 8.1 0 NA C 90 NA NA U Y Y 32 23 TILL
53-01 2.1 0.0 2.1 67.8 55.0 8.2 3.5 3.3 0 NA TR N4 NA lj Y Y 33 23 .7 L
-02 7.7 0.: ,1 10i3.5 87.6 20.9 14.2 6.7 .1 26 ELD 100 NA NA NA Li Y Y Y 33 EE
-03 5.7 , 0.1 5.6 105,1 31. 26.4 15.2 10,6 .7, 74 90 10 NA NA. U y Y. -04 1.2 0.1 1.1 54.6 47,9 6.7 5.1 1.6 --i 5 100 NA NA NA U y 8 8T
54-01,02 55'01
11.1 7. 6
.0.4 0.1
10.7 7.5
112.7 96.4
73.3 71:4
39.2 27.0 14.5 12.5
C.; L.
174 221
I.
IO NA
NA U
Y Y
v Y 3 B
5 TI; T I;
-02,07 12.7 1'2.6 1.42.7 103.6 39.1 19.; 17.2 10 90 10 NA NA u 71LL 7.6 142.5 93.4 44.1 15.5 25.2 NA 10 NA NA. O
E.: 5..3 102.7 75.7 27.0 15.7 11.3 ' • 12 80 NA NA .! Y 8 3 71 -05A. 7,1 0.1 7.0 105.5 79.0 26.5 16.2 10.3 ,0 NA 90 10 NA NA U Y 1 3 3TILL
Sc-')! 7:: 0.3 6.7 113.7 82.3 36.2 Z2.1 14.1 537 90 10 44 NA U `,." Y 5 2 TEL -02,03 14.0 0.2 17.3 171.8 50.5 41.3 21.3 20.0 `'• 49 20 20 NA MIL Y -04.03 12.3 0.6 12.3 160.6 115.4 45.2 27.7 19.5 1. 1002 90 NA MA Li. Y Y Y • -
57-0.1 6.7 0.2 6.5 145.2 100.6 45.6 4.7 20.7 6 165 20 NA %4 v ar TT: 53 7'. • ILL 14.'2 1.0 17.: :21.7 160.8 61.1 :1.0 70.1 778 70 NA -NA. Li S
-04.05 1:.7 0.5 11.8 152.1 173.2 42.7 23.2 17.7 o NA 75 5 NA
4 116.3 86,2 70.1 13.6 11.5 0 NA 10 NA NA il 33 33 TILL
-07 7.5 0.3 7,2 11.2. 52.3 73.: 19.7 15.5 0 NA .N» NA Li 32 33 7ILL 7.6 165,5 176.9 26.6 12.7 5. O NA 10 NA NA 1.! " 747-: 55 .1:
-05:10 14,0 0.4 17.6 231.7 12E0 47.7 24.4 19.2 0 NA '73 5 NA 4 v 337 T 55-01,02 9.6 5.: -76,5 17.2 NA 70 70 NA NA Li Y 33 H Ti
75.6 22.5 12.6 5.7 0 NA 70 .30 NA NA L Y Y Y 73 32 T I -12.0: 14.: 0.2 17.4 2i.1 41.7 73.5 18.0 21.E 773 73 30 NA NA v .•.!` 33 77 TiLL :0-01 5.7 0:1 5.6. 1.37.7 6:..3 121.7 110.5 11.4 3 14 4k; 60 NA NA .f Y 55: 55 T ILL
61-01.02 12.: 0:1 12.1 141.3 97.7 41.: 25.7 15.5 -.0 NA Y 77 32 77.LL 4.7 97.6. 62.7 24 14.: 10:6 NA 7 NA 4, U Y v 78 22 TILL
175.2 »7.1 25.7 2:.4 113 ;5 .7 NA NA Y TILL 6.7-01,02 10.6', 0.2 10.4 167..6 142.1 :5.5 14.7 lo,a o NA 25 NA NA ï-» 22 53 I LL
t 10.1 4.7 5.2 NA EC Y 23 22 :ILL -04 6.7 0.1 6.2 114,2 16.0 2.6 7.4 NA 35 13 NA NA UY YY 22 EE TILL
3A5E : Tr,,Tv
'.4PHILL:S6
S'AMPLE WEIEHT ;4EI3HT LIRAMS
OVERBURDEN DRILL
L45CPAT:PY
DRY)
INS MANAE;m;NT
5-AMPLE
AU
LIMITED
LOS
DEKRIPTION
M. I. CON: CLAST M4T.7TX
TALE -r1j.; TABLE TABLE M.1. CONC. NON NE. :ALC SIZE % 3/U SC 37 :Y 20LCP SPLIT CHIPS CONS LISTS TOTAL MAO MAS V.S. FF5 -- FEED ----------
VISER L3 C7 ED L7f:
-05 ).0 6.6 106.7 76.0 23.7 15.3 12.9 NA TR NA NA NA NA U Y Y 5 5 tL_ 5.6 û. 5. 96.0 77.5 22.5 14.3 7.6 0 NA is NA NA NA NALY YY5 sT:LL
c-t-,21 5.E 0.2 5.6 • 50.3 57.7 33.2 15.0 14.2 '0 NA P 30 10 NA NA U Y y Y E.5 3; 7IL -02 7.0 0.1 2.5 42.1 215 13.6 E.0 5.6 0 NA C 90 10 NA NA !i Y Y y 3N. 7.it TI1
65-01 6.o û.1 5.3 170.5 102.E 27.7 11.4 16.: .1 433 P 70 30 NA NA U Y 3 3 -01A 7.Q 6.9 ise.5 115.5 43.0 25.1 17.9 403 SC 20 NA NAJYY 55T::
66-01.0: 12.4 0.4 12.) 174.9 139.1 35.S 19.1 16.7.0 E5 15 NA NALY 03 7.1 C.1 7.0 144.7 105.2 39.5 :1.3 112 . 0 NA C 55 .5 NA NA U Y 5 5 TILL
67-01 1.1 0.0 1.1 44.9 36.5 14 4.3 3.6 NA TR NA NA NA NA U Y 5 1; 7I.L1 -01A 6.5 0,0 6.5 26.: 60.0 26.3 16.: 10.10 NA TR NA NA NA NA 3 ; YY55EAN1
3.3 0.1 1: 105.6 813 17.3 9.7 7.6 0 . NA P 50 10 NA NA U -01A C.2 6.: 143.: 125.9 17.4 14.5 2.5 0 NA G 90i0NANAJY
69-01 0.2 0.0 0.2 0.0 0.0 0.0 z).0 0.0 NA is NA NA NA NA NA NA NA NA fA ;:;A BELF..:L
7
MR'f! — 3.0TP
ESL: LASPIFI:ATION
r— IISIBLE SOLD FRO!'l SHAKING TABLE AND PANNING
MPH1:UL.36 NUMBER OF GRAINS
ABBRADED IRREGULAR OELICATE NCN CC VS.
EAMFLE PAE: -------- ------- MAG ASSAW
Y:N DIAMETER THICKNESS TFTP T TOTAL DS FRB REMARKS
FirEt NO VISIBLE aoL:
N NO VISIBLE SOLD
—OE N NC VISIBLE GOLD
—,7)6 N NO VISIBLE SOLD
— 7 Y NO VISIBLE SOLO
N NO VISIBLE GOLD
r N NO VISIBLE SOLD
r-
.17-01A N NO VISIBLE SOU r-
N NO VISIBLE ;OLD
N NO ',;ISIBLE SOLD
EET: P-FITE
TOTAL 1 16.2 23
- N 25 X if:0 1:2 1 1
N NO VISIBLE GOLD
r—
r'n
- N NO VISIBLE BOLD
N NO vISIGLE SOLD
TEO 54 :
:25 31 :
TOPL 1 1.bi960
TOTAL
— E.; v—E 3OL:
!•1 c'OLO
C EET: 75 X i00 IS
TOTAL :
MFH - jLTEL
SCL: CLASSIFICATION
r— VISIBLE SOLD Fr S'riAKIN G 7ALE AND FANNING
-11JME,ER OF GRAINS
AFERADEL IRREGULAR DELICATE N:N :AL:
Y..1 DIAMETER THICKNESS TPTPTPTOTAL EMS FP; R;":1ARFE,
N NE VISIBLE 221
-N 75 X 75 15 C
TOTAL 1 15.S 41
N NC VISIELE SOLD
N ICC X :50 25 C 1 1
TOTAL
550
70(.' X 775 59 C,
:75
N soL:
N NO VIEIF 7 20L2 r—
x 25 5 1
EST: IS 7'YRITE 10 C
,-- , 75 X 15j.; 222 I 1
X 100 2,:, C . I
1,...,0 X 175 :72 1 1 2
r- TOTAL 3 26.5 44:
-..7 N NO VISIBLE MILD ,-- ;
,
r- 12: ... 200 71 C I I
TOTAL 4 17.5 TS3
- 2
:1 1
r- TI.-2T
7:IKE -E:LD 2571. FYFITE
EST: F'!'RITE
:5 7
r— ABBRADED
EAMF:F t Pk4NED ========
YiN DIAMETER THICKNESS T P r--
:LAEKFICATI2%
7;:' im4ING TALE Ps,: FNING
1PHILL.L. NUMBER OF GRAIN;
r-
50 X 50 10 C'
:. 2
50 X 75 13L I
7 100 X 100 20 C 1
NC VISIBLE SOLD
r- 47.-01! 50 X :CA) 15 C
r—
.`;. X 100 15 C
:7-03 N NO VISIELE BOLD
2E-01.0:A I 10 VISIBLE BOLD
25-01 N NO VISIBLE OOLL
N 1,0 VISIBLE GOLD
r 45-07 .N NO VISIBLE SOLD
N NO VISIBLE COLD
N: VIEIBLE
r— NC VISIBLE GOLD
47-01 N NE VISIELE .33L0
—01A 10 ':I3IELE GOLD
7 N NO VISIBLE GOLD
r—
NO ViSIELE SOLD
NO IBLE GOLD
1 NO V:EIELE 3ELD
IRREGULAR DELICATE ========= ========
NCN MA3 OMS
CAL: V. B, ASSA1 PPB REMARKS T F TR TOTAL
TCTAL 2 16.; :3E
1
TOTAL I 7.9 19
1
TOTAL 1 20.2
3 ET: 100 ;"'fSITE '
1 2 1
ToTAL 6 18.2 —
EST: :07, PYRITE
ri -)2
- SOUTEL
12L: :E :I: .....
VISIBLE SOLD F::M SHAKINS TABLE AND FANNING
NUMBER OF GRAINS
ABBRADED IRREGULAR DELICATE ION CALC Y.E.
EA,'::iPLE# PAT:ET.: ............. -- ----- MAG A:SAY
.17N DiArt-TER THICKNESETPTFTPTOTAL GME PPE REMARKS
- Y NO V1E1E:LE SOLD EST: 15% FYRITE
N X C 1
TOTAL 1 :5.0 :445
:30x 10r.; 2;C 1
TOTAL 1 17.: E7
NO ''ISIELE GOLD
- N NC ',1EIELE GOLD
52-)iA :00 X 100 :0 C 1 1 r-
TOTAL 1 10.
- N NO VISIBLE BOLD
57-01 N NO VISIBLE BOLD
30 X 75 17 C 4 4 Er: 70% PYRITE
25X50 EC II 75 100 1E : 1
TOTAL 1 14.2
2 1
EST: 15% FAITE
r- T 15.B
1 EF: !':;.:7":
TOTAL I5.1
• 25 25 5 :
T 5.: X 75 1: : 1
50 X 10.; 15 : 75 'X 75 15 :
fr, ISO
1 EST: 15% :YRITE
7:TAL 19.1 174
LA:;IFICLTI:N ===================
,:E:ELE FR12'. EHWINE TALE AND 2ANNING
NUMBER OF BRAINS
'f7,4 DIAMETER THICKNESS
50 X 50 C
ABBFALED IRFFEULAR DF; ICATIT NON MAO
T P TOTk 23
CALC V.S. ASSAY ?FS REMARKS T P
1
7
TOTAL 14.5 221
TOTAL 1 1 .9 10
• -4 N NO VISIBLE SOLD
-ef E,:r X 50 10 C 1 1
TOTAL I 15.7 14
-e54 N Nr" VISIBLE GOLD
50 X .70 10 C 1 1 EET: 10% PY7ITE
, 5:x 75 17 C 1 1 100 X 150 25 C 1 1
r- 1770 X 200 , 34
TOTAL 4 ::.1 507
25 X :5 C EET: 0.57. P-;RITE
25 X 50 c 1 1
50 X 50 10 C •
5j2 X 75 17 C 1
*Ma., 3 21.7 10
rl••••• :5 25 5 C 4 EET: 15% P.!PIE
:5 E 1
5,0 125 13 X 1Y-. :5 C
150 X 750 4C C 1
:5 25 f C
TOTAL E '25.7 1002
EE T: 1 iTE
5-.; f 75 :
17
, i
75 Y 100 IE : 1
14:: 15
:5 : 1 EE7:
E r
9AEE MPH - jOUTEL r:r2:Et
E2L: CLAS9IFICATIE ===================
r..EISLE 21.2 F93. 9HA111. T 1 7 AND P4NNINE
M'7i1JUL.8à NUMBER OF GRAINS
ABRADE: IRREGULAR DELICATE NON CAL: ;1,3. Ir'rflPi 7 # PANNE) ======-- -=======- -------- MAZ AEEAY
?IN DIAMETER THICKNESS T F TPTPTOTAL GMS ;P3 REIARKS
-- X 75 10 :
5C- X 125 12 r 12f 150 Z7 C 1
275. 44 C 1
TOTAL 8 Z1.0 778
-04,Z N NO VISIBLE GOLD
N NC VISIBLE GOLD
-C7 N N: VISIBLE GOLD
N NO ','ISIBLE SOLD
N NO vIsaz GOLD
3-0102 N NO VISIBLE GU
59-01 N NO VISIBLE SOLD
-02.0: y 5,1: X 100 15C 1 :T 125 20 :
125 X 175 290 1
25X 25 5 E 4 25 3 C fr:r X 50 10 : 5Cr X 1:5 IS C 1
1
1
TOTAL 1. 19.0 79:
1
TOTAL E 110.5 14
EET: 51 PYRITE
EST: SO% PYRITE
NO VICIKE OLD
N ,jEILE 2CLC
-LA N X 15/: 25C. 1 1
TOTAL
r,,:EISLE SOLD
•
0",
r
ro'
===================
FR:M Tq4LE AND T-ANINS
?1F1,JUL.36 NUMBER OF BRAINS
ABBRADED IRREBULAR DELICATE NON CA1 q.. ---------- .14 ASSY
VA DiAmET;R THICKNEBSTPTPTPTOTAL EMS PPS REMARKS
NC' VISIBLE BOLD
N: VISIBLE GOLD
N NO VISIBLE SOLD
-0:N NO VISIBLE SOLD
N :50 X 150 27 C 1 1
TOTAL 1 11.4 4:7
N 50 '4. 115 IBC 1 1
TOTAL 1 25.1 40
N N: VISIBLE GOLD
-07 N NO ISIBLE SOLD
NO VISIBLE SOLD
-01A N VISIBLE BOLD
NO VISIBLE CE; D
A
NO VISIBLE GOL:
NO 0,SIBLE SOLD
PAGE •1
MPH - JG-1TF?
09 11: SA
1!>Rhh21u1. 86 OVERBURDEN DRILLING MANAGEMENT LIMITED
LABORATORY SAMPLE LOS
=AMPLE NO.
H-26
FIGHT 0(2.WET) WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS
TABLE +10 TABLE TABLE SPLIT CHIPS FEES}. CONC
M.I. LIGHTS
M. I. CONC
NO. V.G.
CALC PPB
CLAST MATRIX
CONC. NON TOTAL MAG MAS
SIZE '/. S/U SD ST CY COLOR
V/S GR LS OT SD GY
70-01 5.1 0.3 4.8 136.6 106.6 30.0 14.3 15.7 0 NA P 80 20 NA B TILL -01A 5.2 0.6 4.6 141.5 118.4 23.1 12.6 10.5 2 4 C 90 10 NA GB GB TILL 71-01 5.4 0.2 5.2 169.5 140.4 29.1 16.2 12.9 0 NA go 20 NA B B TILL -02 6.1 0.2 5.9 126.3 100.0 26.3 13.8 12.5 1 14 P 80 20 NA B B TILL
72-0! 3.2 0.1 3.1 119.4 101.8 17.6 9.3 B.3 0 NA 6 80 20 NA B B TILL -02 7.1 0.2 6.9 116.7 98.4 12.3 10.7 7.6 0 NA 6 70 30 NA B B TILL -0: 7.0 0.2 6.8 173.3 100.2 33.1 19.2 13.9 0 NA G 80 20 NA B B TILL -04 7.1 0.2 6.9 152.3 118.0 34.3 20.2 14.1 0 NA 80 20 NA B B TILL -05 7.1 0.3 6.8 145.3 118.2 27.1 16.4 10.7 0 NA c 80 20 NA B B TILL -06 5.3 0.2 5.1 139.0 113.5 25.5 15.0 10.5 0 NA 6 80 20 NA B B TILL
%,-01.02 11.8 0.6 11.2 253.4 215.4 38.0 20.4 17.6 1 31 c 80 20 NA B B TILL -03.(4 11.8 0.2 11.6 165.5 119.4 46.1 27.7 18.4 0 NA c 75 25 NA B B TILL
-05 5.4 0.2 5.2 205.5 125.8 79.7 33.1 46.6 0 NA 6 90 10 NA B BN TILL -06.07 13.0 0.6 12.4 116.2 37.8 72.4 53.3 25.1 0 NA C/BL 95 5 NA B • BN TILLL/BLD 74-01 3.4 0.1 3.3 52.7 32.2 14.5 9.9 4.6 2 357 P 80 20 NA B B TILL -02 5.9 0.2 5.7 80.2 51.8 28.4 8.8 19.6 2 890 6 50 50 NA GB B TILL -03 7.4 0.6 6.8 131.6 31.7 99.9 95.7 4.2 0 NA 6 60 40 NA BN TILL
75-01.02 12.2 0.4 12.4 176.1 124.1 52.0 27.2 24.8 0 NA 6 70 30 NA GB GB TILL -03.04 13.2 0,.3 12.9 177.3 127.4 49.9 32.2 17.7 4 150 6 so 20 NA GB GB TILL
-05 6.; 0.2 6.1 105.5 80.1 25.4 15.9 9.5 3 - P/BL 85 15 NA uB SB TILL -06 6.3 0.2 6.1 128.9 92.0 30.9 18.3 12.6 1 35 6 50 50 NA B B TILL -07 6.5 0.3 6.2 118.8 96.4 22.4 14.3 8.1 2 84 6 70 30 NA GB GB TILL -08 5.7 0.1 5.6 106.9 63.3 43.6 24.6 19.0 0 NA 6 70 30 NA GB ,B TILL
-09 ti.7 0.1 6.6 106.2 72.2 34.0 23.6 10.4 1 27 G 70 30 NA GB GB TILL 76-01 7.1 0.2 6.9 105.5 77.5 Z3.0 14.8 13.2 0 NA C 75 25 NA B B TILL
-02,03 12.6 0.5 12.1 166.3 120.9 45.4 23.0 22.4 1 16 C 80 20 NA GB GB TILL -04,05 13.5 0.4 13.1 169.9 132.7 37.2 23.2 14.0 4 53 C 80 20 NA GB GB TILL
,:7 -06.07 8.1 0.6 ..5 192.3 58.8 133.5 27.2 106.3 0 NA C/BL 25 75 NA GB 38 TILL -08 7.4 0.2 7.2 106.2 81.1 25.1 14.7 10.4 2 49 C so 20 NA GB GB TILL -;9 7.' (i.0 7.3 75.9 49.0 26.9 16.6 10.3 5 49 TR NA NA NA GB GB TILL -10 7.5 0.4 7.1 142.0 95.9 52.1 31.4 20.7 13 227 C 80 20 NA GB SB TILL -11 6.8 0.4 6.4 155.1 99.5 55.6 30.0 25.6 0 NA C 25 15 NA GB GB TILL
77-01 5.4 0.2 5.2 112.7 26.2 24.5 15.9 2.6 1 40 C 75 25 NA B TILL _;;2 5.7 ).2 5.5 96.7 22.6 14.1 8.3 5.8 1 23 C 60 40 NA B TILL _03 C.--'~. 0.2 6.0 82.6 63.0 25.6 16.7 8.9 rr NA C 90 10 NA B B TILL
04,05 5.6 f2.1 5.5 144.0 113.5 30._ 19.7 10.8 1 76 C 60 40 NA B TILL 78-01 5.6 0.2 5.6 140.1 116.8 23.3 13.1 10.: 1 49 C 60 40 NA GB GB TILL
-07.03 03 12.0 0.3 11.7 89.5 58.2 30.7 15.3 15.4 0 NA P 70 30 NA GB GB TILL -~ ;4 4.8 0.1 4.7 117.9 26.1 27.8 15.9 11.9 0 NA P 70 30 NA GB GE TILL -05 5.7 0.0 5.7 124.2 109.6 14.c' 9.0 5.6 0 NA TR NA NA NA 66 GB TILL _06 5.2 O.(' 5.2 106.4 1:0.5 7.9 5.3 2.6 0 NA TR NA NA NA GB GB SAND _n? 5 p :15 F. 177 1,._ .~ 117 A 24.2 3.2 14.4 (: NA P 20 15 5 GB SE TILL
7.0 0.2 6.8 142.1 122.2 19.3 9.2 10.7 1 41 P 80 20 NA GB 6B TILL -r9-i 11 0.1 6.9 209.0 183.9 25.1 15.. 10, ;t 0 NA F. 70 30 NA B B TIL!
PA ;t- 2
mahh2ju1.86
MPH - JOUTEL
OVERBURDEN DRILLING MANAGEMENT LIMITED
0Q'11 1a6
r--.
SAMPLE NO.
WEIGHT (F,6.6Æ7) WEIGHT (GRAMS
LABORATORY SAMPLE
DRY) AU
LOG
DESCRIPTION CLASS
TABLE +10 TABLE TABLE SPLIT CHIPS FEED CONC
M.I. LIGHTS
M. I. CONE
NO. V.6.
CALC PPB
CLAST MATRIX
CONC. NON TOTAL NAB MA6
SIZE L S/U SD ST CY COLOR
VIS GR LS OT SD CY
)?-Sc -02 7.0 0.3 6.7 66.7 40.1 26.6 12.9 13.7 0 NA C 80 20 NA NA Y B B TILL
-03 t.2 0.3 5.9 207.4 174.4 33.0 17.3 15.7 0 NA C 85 15 NA NA Y OC. O2. TILL
-04.05 14.0 0.8 13.2 302.6 220.0 82.6 40.1 42.5 1 37 C 85 15 NA NA Y B OC TILL
80-01 6.6 ~ ~. 2 6.4 179.3 146.6 32.7 18.4 14.3 1 55 C 70 30 NA NA Y GB GB TILL
-02 6.4 0.3 6.1 141.6 112.8 28.8 15.o 13.2 1 96 C 80 20 NA NA Y GN GN TILL
-03 5.8 0.2 5.6 167.9 146.0 21.9 13.5 8.4 0 NA C 80 20 NA NA Y B B TILL
-04 6.7 0.3 6.4 159.6 134.7 24.9 15.2 9.7 0 NA C 80 20 NA NA Y B OC TILL
-! ~5 6.1 0.1 6.0 203.5 174.1 29.4 15.8 13.6 0 NA 6 60 40 NA NA Y GB GB TILL
-06. e7 13.1 0.2 12.9 354.9 254.2 100.7 49.9 50.8 10 897 6/P 70 30 NA NA y B B TILL -OSA 6.2 0.1 6.1 182.9 151.3 31.6 19.7 11.9 0 NA P 90 10 NA NA Y GN 93 TILL
-09 6.7 0.2 6.5 230.4 190.0 40.4 23.1 17.3 1 166 P 75 25 NA NA Y GB B TILL
-10,11 13.3 0.6 12.7 92.7 29.2 63.5 31.9 31.6 6 945 G 70 30 NA NA y GG B TILL
-12 5.6 0.3 5.3 201.9 170.0 31.9 16.9 15.0 0 NA G 70 30 NA NA Y GB BN TILL
-13 6.0 0.2 5.8 289.2 248.5 40.7 20.2 20.5 1 564 BK 20 BO NA NA Y GB GB TILL JBDK
81-01.02 13.2 0.4 12.8 292.4 251.8 40.6 21.0 19.6 1 4S P 70 30 NA NA Y B B TILL
-;': 5.0 I 0.2 4.8 163.5 141.7 21.8 14.7 7.1 1 69 P /k1 60 NA Na Y B B TILL
-04,05 11.4 0.4 11.0 201.4 1-=.B 12.6 4.1 8.5 4 4773 P 80 20 NA NA Y GB GB TILL
-06,07 13.1 0.3 12.8 213.4 178.7 34.7 21.3 13.4 0 NA P 80 20 NA NA ,f GB G: TILL
-08,09 13.7 0.4 13.3 180.4 129.5 50.9 30.5 20.4 1 12 P 90 10 NA NA Y GB 3B TILL
-10 11 17.8 0.8 13.0 145.8 83.1 62.7 38.2 24.5 7 736 P 80 20 NA NA Y GB GB TILL
-12,1" 3.2 0.3 9.9 127.6 88.5 39.1 17.1 22.0 0 NA P 60 40 NA NA Y GB GB TILL
-14.15 ,.~ ,„.;~ ~ 0.5 12' .5 332.7 206.5 126.2 80.7 45.5 4 151 P 80 20 NA NA Y GB GP TIL
rft -16 6.3 0.3 6.6 167.8 1??.4 45.4 26.4 19.0 0 NA P 70 30 NA NA Y GB GB TILL -17 7.0 0.1 6.9 149.8 109.3 40.5 25.0 15.5 1 60 P 60 40 NA NA Y GB 98 TILL
-18 7.3 0.1 7.2 79.6 50.4 29.2 19.0 10.2 0 NA P 30 70 NA NA Y B B TILL
-19 6.3 0.: 6.0 126.7 82.0 44.7 32.0 12.7 0 NA P/BK 30 70 NA NA y B B TILL GDK
8^-01 5.7 0.2 5.5 109.5 8.7.5 1..2.0 13.2 8.8 0 NA 6 70 30 MA NA Y Fit GE TIII
--. _ 6. k t.0 142.3 105.1 37.2 25.7 11.5 0 NA G 90 10 NA NA 6B OB TILL
-~ ±3 0.8 0.2 6.6 92.0 61.1 29.9 18.9 11.0 0 NA G 80 20 NA NA Y Y 6B 'B TILL -A...2= 11.7 0.6 11.6 161. 8 75.7 86.1 47.0 :9.1 2 10 P/G 90 IO NA NA Y Y 8B GB TILL
-0:• 6.5 0.4 6.1 110.5 80.3 30.2 19.4 10.8 0 NA G 80 20 NA NA Y Y 98 SB TILT _.' 6.9 2.4 6.5 137.0 102.2 34.8 20.9 13.9 1 545 6/BL 50 50 NA NA Y Y B B TILL/817;
7.2 :.4 6.8 123.6 89.4 34.2 22.7 11.5 0 NA S/BK. 60 40 NA 6{n Y Y 3 D TILL: BDi.
6.7 .._ 6.0 118.8 91.9 26.9 16.4 10.5 0 tiA G 70 30 NA R
NA7
Y Y 29 GB TILL
-02 0.5 O._ `:'•- 11_._ 88.8 24.3 14.7 9.t 1 44 G 20 20 NA NA Y
Y GB GB T I I 1 -ti` _,5 i:.'' 6.1 82.6 61.6 27.0 16.6 10.4 1 39 h' 80 20 NA NA Y Y GB GB TILL - . _.':: ... a._ .21.- 84.5 36.7 2t.B 9.9 1 228 G 80 20 NA NA Y Y 2B G8 TILL
.1 .j.. c.: 1:8.6 102.5 36.1 2':.5 15.6 n NA G 80 20 44 NA Y Y S? GB TILL __;L . :'.: 6.7 ".l 72.7 24.4 14.4 10.0 0 NA C 95 5 NA NA Y 98 GB TILL
6.8 116.9 97.9 19.0 9.2 9.8 0 NA P/C 90 10 NA NA Y GB GE TILL
-:4: 6.3 :.2 6:.'_ 144.4 114.9 19.5 11.6 -,4 NA P 70 30 ~ NA Y Y` vG `B TII. ..
5.1 0.4 4.7 n07.6 157.4 50.1 41.9 8.3 I P 70 30 NA NA Y GB SB TILL . . ç tt. ~ 230.6 26.1 14.` J 11.6 ii NA p 75 25 NA NA Y B B TILL `_..' 1 _0.,T 149.:' 11.5 5.9 5.7 0 NA P 70 30 NA N
Y Y GB SB TILL
PAGE . MPH - JOUTEL 07/11/86
marn2iu1.8_ OVERBURDEN DRILLING MANAGEMENT LIMITED
LABORATORY SAMPLE LOG
SAMPLE NO.
WEIGHT ik:G.WET) -
WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS
TABLE +100 TABLE TABLE SPLIT CHIPS FEED CONC
M.I. LIGHTS
M. I. CONC
V.G. NO.
CLAST MATRIX
CONC. NON TOTAL MAG NAG
CALO SIZE PPB
7. S;U SD ST CV COLOR
V/S GR LS OT SD CY
N-86 86-Q1 6.9 0.2 6.7 159.6 132.2 27.4 15.4 12.0 1 97P 40 60 NA NA J Y .Y Y B r": TILL
-02.0: 12.9 0.2 12.7 187.8 164.2 23.6 11.6 12.0 1 183 P 40 60 NA NA U Y Y Y GR r TILL -04 6.8 0.2 6.6 1310 112.7 20.3 11.2 9.1 0 NA P 50 50 NA NA U Y Y Y 3B GE TILL -05 3.2 0.0 3.2 85.4 74.5 10.9 7.7 3.20 NA TR NA NA NA NA U V Y i' B GB TILL
87-01 8.7 0.0 6.7- 241.2 204.5 36.7 21.1 15.6 0 NATRNANANRNAUV V Y B E "ILL
-02 6.7 0.2 6.5 172.6 140.0 32.6 18.5 14.1 0 NA P 70 30 NA NA U Y Y Y GB G8 TIL- -0: 7.1 0.1 7.0 111.6 87.0 24.6 14.5 10.1 0 MAP EO 20 NA IIA U
Y Y Y GB :E 'ILL
-04.05 10.1 0.3 9.8 130.2 101.5 28.7 17.5 11.2 0 NA P 9O 10 NA NA U Y Y Y 8B Gr TILL 87-06 1.9 0.1 1.8 56.0 45.9 10.1 7.1 3.0 0 MA P 95 5 NA NA J Y Y Y GB 3B :TIL_
PaE= 1
MPH - JOUTEL u.
+vr LLASiIFI:,ŸTiON
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
mrh2aul.66 NUMBER OF GRAINS
ABBRADED IRREGULAR DELICATE NON CALC V.6. SAMPLE s PANNED so=— --= MAG ASSAY
Y/N DIAMETER THICKNESS T P T P T P TOTAL GMS FPB REMARKS
H-36 70-01
-01A
N
Y
NO VISIBLE GOLD
25 X 25 5 C 2 2 EST: 307. PYRITE
TOTAL 2 12.6 4
71-01 N NO VISIBLE GOLD
N 50 X 50 10 C 1 1
TOTAL 1 13.8
72 Al N NO VISIBLE GOLD
N NO VISIBLE SOLD
-03 N NO VISIBLE GOLD
-04 N NO VISIBLE SOLD
-05 N NO VISIBLE GOLD
-Ob N NO VISIBLE GOLD
01.02 N 50 :X 1t?i 15 C 1 1
TOTAL 1 20.4 31
-03.04 N 40 VISIBLE GOLD
I NO VISIBLE BOLD
-0S.07 N NO VISIBLE SOLD
74-01 v ÿv t 100 15 C 1 1 EST: 1;. PY.R.I TE - -,f., r':~ .~: L\rs) +'~~ i~f 1, , 1
TOTAL 2 5.9 357
:00 X 150 25 C 1 1 EST: 5.`•. = r'R'_ TE 150 .. 15. 29 C 1 1
TOTAL 8.5 _9i.
o :'_S'L 7 GOLD EST: 30% PYRITE
40 VISIBLE __:i P
PAR; , - MPH - JOUTEL 09/11/S6
SOLD CL.aSS"tFi_ATIC7d
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
actsn2jui.86
_MmP-E = PANNED
NUMBER OF GRAINS
ABBRADED IRREGULAR DELICATE NON CALE V.6. ASSAY MAD yiN
DIAMETER THICKNESS T P T P T P TOTAL SMS PPB REMARKS
w-3ti
-03.04 50 + 75 13 C 1 1 EST: 2. PYRITE 75 X 75 13 C 1 1 2 100 X 150 25 C 1 1
TOTAL 4 32.2 150
-05 Y 50 X 50 10 C 1 1 2 EST: 2'l. PYRITE 75 X 100 18 C 1 1 1 GRAIN GALENA
TOTAL 3 15.9 88
-06 N 50 :K .100 15 C 1 1
TOTAL 1 18.3 35
-07 50 X 50 10 C 1 1 EST: 5% PYRITE 50 X 125 18 C 1 1
TOTAL 2 14.3 84
-08 N NO VISIBLE GOLD
-09 "a 50 X 100 15 C 1 1
• TOTAL 1 23.6 27
7t-01 N NO VISIBLE GOLD
-02.03 v _il Y 75 13 C 1 1
TOTAL 1 2.0 16
-04,05 25 X 25 5 C 1 1 EST: 5'i PYRITE 50X 50 10C 1 1 50 X 75 13 C 1 1 75 X 75 15 C 1 1
TOTAL 4 23.2 53
-06,07 r4. NO .:=lFl.^. _OLD
-;:ç. ~5 i 50 B C 1 1 EST: 5 ;AFT 50:: 1::; 15 C 1 1
TOTAL 14.7 4
r-'
PA4: 3
MPH - 1DUTEL '.'`.'; 11!86
GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
mahh2u1.86
SAMPLE 4 PANNED YIN DIAMETER THICKNESS
NUMBER OF GRAINS
ABRADED IRREGULAR =in= ===----_
DELICATE -r----
NON MAG 8M5
CALC V.6. ASSAY PPB REMARKS T P T P T P TOTAL
H-26
-09 Y 25 X 25 5 C 2 2 EST: 1 PYRITE 50 X 50 10 C 1 1 2 50 h 75 13 C 1 1
TOTAL 5 16.6 49
-10 Y 25 X 25 5 C 3 3 EST: 3% P'rnITE 25 X 50 à C 1 2 1 4 100 GRAINS MARCASITE 50 X 50 10 C 1 1 2 PHOTO REF #120 SO X 75 13 C 1 1 75 X 75 15 C 1 I
100 X 100 20 C 1 1 125 X 150 27 C 1 1
TOTAL 13 31.4 227
-il N NO VISIBLE GOLD
77-01 N 75 X 75 15 C 1 1
TOTAL 1 15.9 40
-02 N 50 X 50 10 C 1 1
TOTAL 1 8.3 23
-03 N NO VISIBLE GOLD
N 100 X 100 20 C 1 1
TOTAL 1q.7 ;r
=-01 N 50 X 100 15 t, 1 1
TOTAL 1 13.1 49
-02.03 u NO V I y I GiP GOLD
-04 ;k NO VISIBLE GOLD
- ` N NO vISTB E GOLD
-06 N NO VISIBLE GOLD
-07 N NO VISII+LE SOLD
-05 N 50 n 75 17 C 1
PAGE 4 MPH - JOtlTEL
!GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
rpnh2.u1.96
SAMPLE * PAWED
NUMBER 0F GRAINS
ABBR.ADED IRREGULAR DELICATE NON CALO V.G. ASSAY MG
''!N DIAMETER THICKNESS T P T P T P TOTAL GMS PPB REMARKS
H-6c
TOTAL 1 9.2 41
79-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
-03 N NO VISIBLE GOLD
-04,05 N 75 X 125 20 C 1 1
TOTAL 1 40.1 37
80-01 N 75 z 100 19 C 1 1
TOTAL 1 18.4 55
-02 N 75 X 125 20 C 1 1
TOTAL 1 15.6 96
-03 N ND VISIBLE GOLD
-04 N NO VISIBLE GOLD
-05 N NO 'VISIBLE EOLD
-06.07 " Y 50 X 100 15 C 1 1 ET: 1% PYRITE 50 X 125 19 C 1 1 PHOTO REF *120
r 75 x 75 15 C 1 1 75 X 100 19 G 1 75 :z 125 20 G 1 1 100 X 175 27 G 1 1 100 X 225 31 G 1 -1 125 :X 200 31 C 1 i
.-~ 150 X 150 29 G 1 1 200 s 275 44 G 1 1
TOTAL 10 49.9 897
-'BA Ai NO VISIBLE GOLD
-no N 125 r 150 27 ~~ 1 1
TOTAL 1 23.1 166
5 C 2 2 EST: 1': PYRITE
:"i11;n6
PAGE 5
MPH — TOU:Q. 09;'11fSt
GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
1101h2ju1.86
SAMFLE * PANNED YIN DIAMETER THICKNESS
NUMBER OF
ABBRADED
GRAINS
IRREGULAR DELICATE NON MAG SMS
CALC V.G. ASSAY PPP REMARKS T P
21======
T P
MIS=
T P TOTAL
4-N4
100 7 125 22 C 1 125 X 150 27 C 1 150 X. 150 29 C 1 1 150 X 300 42 C 1 1
TOTAL 6 31.9 845
—12 N NO VISIBLE GOLD
-13 N 204 X 200 38 C 1 1
TOTAL 1 20.2 564
81-01.02 N 75 X 100 18 C 1 1
TOTAL 1 21 48
—03 N 75 X 100 18 C 1 1
TOTAL 1 14.7 69
—04,05 25 X 25 5 C 1 EST: 5% PYRITE
50 50 10C 1 75 X 75 15 C 1
225 :X 250 44 C 1
TOTAL 4 4.1 4773
—16.07 N NO VISIBLE SOLD
—~ i.s_s, 04 N 50 X 75 13 C 1 1
TOTAL 1 30.5 12
—10.:: Y 25 X 25 5 r 2 2 EST: 10% PYRITE 50 X 75 13 C 1 1 54 X 11:;_ 15 C 1 1 75X: z 15C 1 1 100 ii i X 100 i 20 C 1 1 125 X 400 48 f _ 1
TOTAL 7 36.2 i
—12.17 N NO VISIBLE '_OLD
—14.1` 50 X 50 10 C 1 1 EST: 25% PYRITE 75 X 175 25 C 1 1000 GRAINS MARCASITE
MPH - JOUTE. 09/11/86
GOLD VLASSIFICATION
r vISIBLE GOLD FROM SHAKINiG TABLE AND PAINING
no!~h23 11.96 NUMBER OF GRAINS
r—
S• *1uLE ;~
H-86
PANNED Y!N DIAMETER THICKNESS
125 X 125 25 C 150 X 175 31 C
ABBRADED ======u
IRREGULAR DELICATE ======= ~
NON MAG GMS
1 1
CALL V.G. ASSAY
PPB REMARKS
5 GRAINS ARSENOPYRITE
T P
1
T P T P TOTAL
1
TOTAL 4 80.7 151
-16 N NO VISIBLE GOLD
-17 N 75 x 125 20 G 1 r--
TOTAL 1 25.0 60
-18 N NO VISIBLE GOLD
-19 N NO VISIBLE GOLD
82-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
-03 N NO VISIBLE SOLD
-04,05 25 11 50 8 C 1 1 EST: 20% PYRITE
50 i( 75 :?•C 1 1 1 GGRAIN GALENA
TOTAL 2 47.0 10
-06 N NO VISIBI.E GOLD
-07 N 200 X 200 38 C 1 1
TOTAL 1 20.9 545
-OE N NO VISIBLE GOLD
=4-61 N NC VISIBLE GOLD .
-__ Pi 75 F. 75 15 G 1 1
TOTAL 1 14.7 44
-07 75 75 :5 G 1 1
TOTN_ 1 16.6
-~ ~~ . ~ ~ 1~.. . J~ _:,,r . `~ ÿ 1
TOTAL 1 16.8 225
PAGE 7 • . MPH - JOUTEL 09+11/6_
GOLD C..ASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
mahh.iul.86 - NUMBER OF GRAINS
SAmPiw #
H-66
-05
-V6
-07
-08
PANNED Y1N DIAMETER THICKNESS
N NO VISIBLE GOLD
N NO VISIBLE GOLD
N NO VISIBLE GOLD
N NO VISIBLE GOLD
ABBRADED IRREGULAR DELICATE NON MAG 6M5
CALC V.G. ASSAY PPB REMARKS T P T P
=—=---- T P TOTAL
-09 Y 50 X 75 13 C 1 1 EST: 4.0% PYRITE 2 GRAINS GALENA
TOTAL 1 41.9 9
85-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
86-01 N 75 X 125 20 C 1 1
TOTAL 1 15.4 97
-02,03 N 100 X 125 22 C 1 1
TOTAL 1 11.6 183
-04 N NO VISIBLE GOLD
-05 N NO VISIBLE GOLD
,•~ 87-01 N NO VISIBLE _OLD
-02 N NC VISIBLE GOLD
r--' -03 N NO VISIBLE GOLD
-:::4.05 `i NO +:ISIBLE GOLD r
8?-0k N NO VISIBLE GOLD
PAGE 1 . MPH - JOUTEL
s'37/ 10/66
r- MPHH3JUL.86 OVERBURDEN DRILLING MANAGEMENT LIMITED
_. _ SAMPLE NO.
WEIGHT (K6.üET)
LABORATORY SAMPLE LOG
WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS
TABLE +10 TABLE TABLE SPLIT CHIPS FEED CONC
M.I. LIGHTS
M. I. CONC
NO. V.B.
CLAST MATRIz ======
CONC. NON TOTAL MA6 MAG
CALC SIZE PPB
S/U SD ST CY COLOR
V/S SR LS OT SD CY
H-86 .-- 86-01 6.4 0.2 6.2 140.9 113.7 27.2 14.1 13.1 0 NA P 80 20 NA NA U Y Y Y 6B GB TILL -02 6.1 0.1 6.0 126.1 92.8 33.3 18.7 14.6 0 NA P 90 10 NA NA U Y Y Y GB B TILL
89-01 7.0 0.2 6.8 151.1 116.2 34.9 21.5 13.4 0 NA P 95 5 NA NA U Y Y Y B B TILL -01A 5.3 0.0 5.3 114.4 89.0 25.4 14.6 10.8 0 NA TR NA NA NA NA U Y Y Y fiB GB TILL 90-01 6.8 0.0 6.8 185.7 141.1 44.6 22.1 22.5 0 NA TR NA NA NA NA U Y Y Y 6B 68 TILL -01A 6.7 0.0 6.7 180.3 151.2 29.1 15.3 13.8 0 NA C 70 30 NA NA U Y Y Y GB GB TILL -02 3.3 0.0 3.3 50.9 39.0 11.9 7.3 4.6 0 NA TR NA NA NA NA U Y Y Y GY GY TILL
91-01 5.5 0.0 5.5 96.8 68.6 28.2 17.0 11.2 0 NA TR NA NA NA NA U Y Y Y B B TILL -02 5.7 0.1 5.6 152.7 122.2 30.5 18.6 11.9 3 94 C 80 20 NA NA U Y Y Y 6B GB TILL -03 4.1 0.0 4.1 67.3 46.4 20.9 14.3 6.6 1 26 TR NA NA NA NA U Y Y Y 6B GB TILL
r- 92-01 4.0 0.0 4.0 108.1 98.2 19.9 11.8 8.1 1 245 TR NA NA NA NA U Y Y Y GB 6B TILL -02 2.6 0.0 2.6 46.8 33.8 13.0 8.4 4.6 0 NA TR NA NA NA NA U Y Y Y GB GB TILL
93-01 5.7 0.0 5.7 65.9 39.9 26.0 15.9 10.1 0 NA TR NA NA NA NA U Y Y .Y
GB GB TILL -01A 6.9 0.1 6.8 86.8 56.8 30.0 16.8 13.2 0 NA C 80 20 NA NA U Y Y Y GB GB TILL ~ -02 2.1 0.0 2.1 36.6 26.7 9.9 6.3 3.6 0 NA TR NA NA NA NA U Y Y Y 6B B TILL
94-01 3.1 0.0 3.1 27.9 18.1 9.8 6.5 3.3 0 NA TR NA NA NA NA U Y Y Y GB GB TILL -01A 6.7 0.3 6.4 86.5 58.7 27.8 14.6 13.2 1 13 P 80 20 NA NA U Y Y Y GB GB TILL -02 6.7 0.0 6.7 85.6 58.1 27.5 15.5 12.0 0 NA TR NA NA NA NA U Y Y Y 6B GB TILL -03 5.5 0.3 5.2 78.7 55.7 23.0 13.5 9.5 0 NA P 70 30 NA NA U Y Y Y GB GB TILL
95-01 4.0 0.2 3.8 76.5 54.8 21.7 11.9 9.8 0 NAP 70 30 NA NA U Y Y Y r, GB TILL -02 4.1 0.0 4.1 94.1 69.5 24.6 14.1 10.5 2 28 TR NA NA NA NA U Y Y Y B B TILL
~ -03 3.7 0.3 3.4 70.6 49.9 20.7 10.5 10.2 0 NAP 70 30 NA NA U Y YYB GB TILL 96-01 4.0 0.2 3.8 99.4 76.5 22.9 12.2 10.7 0 NA P 80 20 NA NA U Y Y Y B GB TILL -01A 6.6 0.4 6.2 115.7 84.4 31.3 16.3 15.0 1 1 C 80 20 NA NA U Y Y Y GB GB TILL 97-01 6.6 0.1 6.5 190.3 153.3 37.0 20.1 16.9 1 106 6 80 20 NA NA U Y Y Y B B TILL -02 7.1 0.1 7.0 137.1 102.8 34.3 19.5 14.8 0 NA P 80 20 NA NA U Y Y Y B B TILL -03 7.; 0.1 7.2 91.0 62.7 28.3 17.0 11.3 1 11P BO 20 NA NA U Y YYBB TILL
98-01 7.3 0.2 7.1 139.8 97.0 42.8 22.5 20.3 0 NA P 70 30 NA NA U Y Y Y B GB TILL -02 7.2 0.2 7.0 140.0 102.9 37.1 18.4 18.7 0 NAP 70 30 NA NA U Y YYB B TILL -03 6.7 0.2 6.5 107.6 79.0 28.6 16.2 12.4 0 NAP 70 30 NA NA U Y YYB B TILL
99-01 2.1 0.1 2.0 61.0 48.4 12.6 8.1 4.5 0 NAP 70 30 NA NA U Y Y Y B B TILL -02 3.5 0.1 3.4 64.1 49.3 14.8 8.1 6.7 0 NA P 70 30 NA NA U Y Y Y B B TILL
100-01 6.3 0.2 6.1 118.4 87.2 31.2 16.6 14.6 1 297 P 60 40 NA NA U Y 'i Y B B TILL -02 7.6 0.2 7.4 115.5 79.3 36.2 18.3 17.9 0 NAP 60 40 NA NA U Y YYBBTILL
r. -03 6.7 0.2 6.5 86.0 58.9 27.1 15.3 11.8 0 NAP 60 40 NA NA U Y Y Y B B TILL 102-0l 6.9 0.3 6.6 136.3 111.4 24.9 14.4 10.5 0 NA P 60 40 NA NA U Y Y Y B B TILL
-02 7.4 0.3 7.1 185.7 158.4 27.3 16.2 11.1 0 NAP 60 40 NA NA U Y YYB B TILL -03 7.2 0.3 6.9 193.3 159.3 34.0 21.1 12.9 0 NAP 60 40 NA NA U Y Y Y B B TILL -04 4.5 0.1 4.4 87.6 68.1 19.5 12.5 7.0 0 NA P 60 40 NA NA U Y YYBBTILL
103-01 7.2 0.2 7.0 206.2 181.9 24.3 14.3 10.0 1 541 P 60 40 NA NA U Y Y Y B B TILL 104-01 6.8 0.2 6.6 205.4 172.3 33.1 19.5 13.6 0 NAP 60 40 NA NA U Y VVBGBTILL
,.. -01A 7.9 0.4 7.5 201.3 157.2 44.1 29.1 15.0 0 NA P 60 40 NA NA U Y Y Y GB 6B TILL 105-01 2.1 0.1 2.0 141.4 132.2 9.2 5.9 3.3 0 NA P 100 TR NA NA U Y Y 'r' GB 66 TILL
-+?2 5.8 0.2 5.6 166.3 141.1 25.2 16.0 9.2 1 23 BL 95 5 NA NA U Y Y Y G6 GN TILL/BL
PAGE 2
MPH - JOUTEL 07/10/86
MPHH3JUL.86
SAMPLE EIGHT (Ik6.WET) NO.
OVERBURDEN DRILLING MANAGEMENT LIMITED
LABORATORY SAMPLE LOS
WEIGHT (BRANS DRY) AU
M. I. CONC lISISSICA:=
MATRIX
DESCRIPTION CLASS
2161C111=1 S:111.1111111111===
TABLE +10 TABLE TABLE SPLIT CHIPS FEED CONC
M.I. CONC. LIGHTS TOTAL
NON MAS MAS
NO. V.S.
CALO PPB
SIZE Z S/U SD ST CY COLOP
V/S SR LS OT SD CY
H-86 -03 6.4 0.1 6.3 106.2 84.4 21.8 13.1 8.7 0 NA P 80 20 NA NA U Y Y Y B 6B TILL -04 3.7 0.2 3.5 136.8 124.7 12.1 7.8 4.3 0 NA P 90 10 NA NA U Y Y Y 6B SB TILL
106-01 5.8 0.1 5.7 170.5 137.2 33.3 21.0 12.3 0 NA P 80 20 NA NA U Y Y Y 68 66 TILL -OlA 8.1 0.3 7.8 205.7 166.9 38.8 20.0 18.8 0 NA P 90 10 NA NA U Y Y Y „ GB TILL -02 6.9 0.2 6.7 204.7 179.4 25.3 15.3 10.0 0 NA P 85 15 NA NA U Y YYB TILL -03 7.3 0.1 7.2 122.8 98.4 24.4 14.9 9.5 0 NA P 90 10 NA NA U Y Y Y GB :: TILL
107-01 4.4 0.0 4.4 135.4 112.5 22.9 14.2 8.7 0 NA TR NA NA NA NA U Y Y Y 68 TILL -02 2.5 0.0 2.5 63.5 52.2 11.3 6.6 4.7 1 227 TR NA NA NA NA U Y Y Y B B TILL -03 5.8 0.1 5.7 88.4 61.6 26.8 17.0 9.8 0 NA P 80 20 NA NA U Y Y Y B B TILL -04 5.6 0.1 5.5 66.9 45.7 21.2 11.5 9.7 1 252 6 80 20 NA NA U Y Y Y B B TILL -05 5.4 0.4 5.0 128.8 106.7 22.1 11.5 10.6 1 2 6 90 10 NA NA U Y Y Y SB SB TILL
108-OiA 1.0 0.0 1.0 29.1 28.7 0.4 0.3 0.1 1 .5000 TR NA NA NA NA U Y Y Y 6B 6B TILL/CLAY 109-01 3.4 0.0 3.4 85.1 68.4 16.7 9.4 7.3 0 NA TR NA NA NA NA U Y TILL
-02 4.1 0.1 4.0 42.7 27.1 15.6 8.5 7.1 0 NA P 80 20 NA NA U Y Y Y 6B 68 TILL -03 4.7 0.2 4.5 52.3 36.5 15.8 8.8 7.0 0 NA 6/BK 90 10 NA NA U Y Y Y B B TILL/BDik
110-01,02 9.4 0.4 9.0 120.9 92.4 28.5 16.0 12.5 2 453 P 80 20 NA NA U Y Y Y B B TILL -03 4.6 0.2 4.4 92.2 72.4 19.8 13.0 6.8 0 NA 6 80 20 NA NA U Y Y Y 68 68 TILL -04 7.5 0.2 7.3 117.4 88.4 29.0 15.8 13.2 0 NA 6 80 20 NA NA U Y Y Y GB 68 TILL -05 6.2 0.1 6.1 77.5 56.6 20.9 12.1 6.8 0 NA 6 80 20 NA NA U Y Y Y B B TILL -06 6.9 0.2 6.7 123.8 96.0 27.8 15.4 12.4 1 321 6 75 25 NA NA U Y Y Y B B TILL -07 4.5 0.2 4.3 71.3 50.7 20.6 12.8 7.8 0 NA 6 75 25 NA NA U Y Y Y 6B 6B TILL -08 7.9 0.5 7.4 88.1 59.3 28.8 17.4 11.4 0 NA 6 90 10 NA NA U Y Y Y 68 68 TILL
111-01 6.0 0.2 5.8 109.9 90.7 19.2 11.4 7.8 0 NA 6 75 25 NA NA U Y Y Y B B TILL -02 5.1 0.1 5.0 78.3 63.9 14.4 9.5 4.9 1 39 6 80 20 NA NA U Y Y Y 6B SB TILL
112-01 5.3 0.1 5.2 99.7 75.4 24.3 14.6 9.7 0 NA ,6 80 20 NA NA U Y Y Y 68 GB TILL -02 6.5 0.2 6.3 58.0 39.4 18.6 10.0 8.6 0 NAP 70 30 NA NA U Y VYGBGB TILL
-03 7.0 0.1 6.9 157.1 122.4 34.7 19.3 15.4 1 150 6 70 30 NA NA U Y Y Y 68 68 TILL -04 7.1 0.2 6.9 145.5 113.1 32.4 17.0 15.4 0 NA 6 80 20 NA NA U Y Y Y SB SB TILL -05 7.3 0.2 7.1 185.8 150.4 35.4 22.4 13.0 0 NA 6 75 25 NA NA U Y Y Y GB SB TILL -06 5.7 0.2 5.5 144.8 119.2 25.6 16.7 8.9 2 254 6 75 25 NA NA U Y Y Y SB 6B TILL -07 5.4 0.2 8.2 115.5 84.4 31.1 19.1 12.0 0 NA 6 80 20 NA NA U Y Y Y 6B 66 TILL -08 6.4 0.3 6.1 152.5 126.1 26.4 16.3 10.1 2 222 6 80 20 NA NA U Y Y Y GB B TILL -04 5.6 0.2 5.4 79.2 47.9 31.3 24.5 6.8 0 NA 6 80 20 NA NA U Y Y Y 68 6B TILL -10 4.3 0.1 4.2 97.1 83.9 13.2 8.5 4.7 1 75 6 70 30 NA NA U Y Y Y 6B 68 TILL
112-11 1.0 0.0 1.0 23.4 23.2 0.2 0.2 0.0 0 NA TR NA NA NA NA U Y Y Y 6Y 6Y TILL/CLAY
PAGE 1
MPH - JOUTEi. 07/10/86
GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
- MPHH3JUL.86. NUMBER OF GRAINS
SAMPLE ï PANNED Y/N
H-86
ABBRADED xammumou
T P
IRREGULAR ====
DELICATE NON NAG 8MS
CALC V.B. ASSAY PPB REMARKS T P
2SUMMMWOR
T P TOTAL DIAMETER THICKNESS
88-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
89-01 N NO VISIBLE GOLD
-01A N NO VISIBLE GOLD
90-01 N NO VISIBLE GOLD
-CIA N NO VISIBLE GOLD
-02 Y NO VISIBLE GOLD EST: 15% PYRITE
91-01 N NO VISIBLE GOLD
-02 Y 50 X 75 13 C 1 1 2 EST: 2% PYRITE 50 X 125 18 C 1 1
TOTAL 3 18.6 94
-03 N 50 X 75 13 C 1 1
TOTAL 1 14.3 2o
92-01 N 100 X 150 25 C 1 1
TOTAL 1 11.8 245
-02 N NO VISIBLE BOLD
93-01 N NO VISIBLE GOLD
-01A N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
94-01 N NO VISIBLE GOLD
-01A Y 25 X 75 10 C 1 1 EST: 2% PYRITE
TOTAL 1 14.6 13
-02 N NO VISIBLE GOLD
-03 N NO VISIBLE GOLD r —
PAGE 2
MPH - JOUTEL 0//10186
r- GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
- MPlW3JUL.B6 NUMBER OF GRAINS
,--
SAMPLE B PANNED Y/N DIAMETER THICKNESS
H-86
95-01 N NO VISIBLE SOLD
-02 Y 25 X 25 5 C 25 X 100 13 C
AIDED ======
IIDRESLAR DELICATE aNZIONINZ
NON
MA6 6MS
1
1
CALC V.S. ASSAY PPB REMARKS
EST: 20% PYRITE
5 GRAINS ARSENOPYRITE
T P T P T P TOTAL
1
1
TOTAL 2 14.1 26
-03 N NO VISIBLE SOLD
96-01 N NO VISIBLE SOLD
-01A 'i '25 X 25 5 C 1 1 EST: 20Z PYRITE
TOTAL 1 16.3 1
97-01 N 100 X 125 22 C 1 1
TOTAL 1 20.1 106
-02 N NO VISIBLE SOLD
-03 N 50 X 50 10 C 1 1
TOTAL 1 17.0 11
98-01 N NO VISIBLE SOLD
-02 N NO VISIBLE SOLD
-03 N NO VISIBLE GOLD
99-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
100-01 N 150 X 150 29 C 1 1
r- TOTAL 1 16.6 297
-02 N NO VISIBLE GOLD
-03 N NO VISIBLE GOLD
102-01 N NO VISIBLE GOLD
-o2 N NO VISIBLE GOLD
PAGE 3 MPH - JOUTEL '07i10/56
GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
- MPHH3JUL.86
SAMPLE 4 PRIED ViN DIAMETER THICKJESS
NUMBER OF
ABBRADED
T
GRAINS
IRREGULAR DELICATE NON NAG
T P TOTAL SMS
CALO V.G. ASSAY PPB REMARKS P T P
H-86 -03 N NO VISIBLE GOLD
-04 N NO VISIBLE GOLD r"""
103-01 N 125 X 225 34 C 1 1
TOTAL 1 14.3 541
104-01 N NO VISIBLE GOLD
-01A N NO VISIBLE GOLD
105-01 N NO VISIBLE GOLD
-02 N 50 X 75 13 C 1 1
TOTAL 1 16.0 23
-03 N NO VISIBLE GOLD
-04 N NO VISIBLE GOLD
106-01 N NO VISIBLE GOLD
-01A N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
-03 N NO VISIBLE SOLD
107-01 N NO VISIBLE GOLD
-02 N 100 X 100 20 C 1 1
r` TOTAL 1 6.6 227
-03 N NO VISIBLE GOLD
-04 N 100 X 150 25 C 1 1
TOTAL 1 11.5 252
-05 Y 25 X 25 5 C 1 1 EST: 25% PYRITE 30 GFAINS GALENA
TOTAL 1 11.5 2
106-01A v 100 X 100 20 C 1 1 EST: 40% PYRITE
r
PAGE 4
MPH - JOUTE- 07/10/86
GOLD CLASSIFICATION
VISIBLE SOLD FROM SHAKING TABLE AND PANNING
MFHH3JLJ<..86 NUMBER OF GRAINS
SAMPLE It PANNED Y/N
H-86
ABBRABED an=c1=
IiIL.AR DELICATE NON MAG GMS
CALC V.G. ASSAY PPB REMARKS T
101100011211= WNW=
P T • P T P TOTAL DIAMETER THICKNESS
TOTAL 1 0.3 5000
109-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
-03 • N NO VISIBLE GOLD
110-01.0 Y 50 X 125 18 C 1 1 EST: 15X PYRITE 150 X 175 31 C 1 1
TOTAL 2 16.0 453
-03 N NO VISIBLE BOLD
-04 N NO VISIBLE GOLD
-05 N NO VISIBLE GOLD
-06 N 150 X 150 29 C 1 1
TOTAL 1 15.4 321
-07 N NO VISIBLE GOLD
-08 N NO VISIBLE BID
111-01 N NO VISIBLE GOLD
-02 N 50 X 75 13 C 1 1
TOTAL. 1 9.5 39
112-01 N NO VISIBLE GOLD
-02 N NO VISIBLE GOLD
-03 N 100 X 150 25 C 1 1
TOTAL 1 19.3 150
-04 N NO VISIBLE GOLD
-05 N NO VISIBLE GOLD
-06 Y 75 ii 150 22 C 1 1 FST? IA% PVRITF
ABBRADED =MRS
T
1
IRRES)LAR DELICATE 1111111111== =OM=
NON NAG
GMS
CALC V.S. ASSAY
PPB REMARKS P T P T P TOTAL
1
TOTAL 2 16.7 254
. 1 EST: 15X PYRITE 1
TOTAL - 2 16.3 222
1
TOTAL 1 8.5 75
SAMPLE 4 PANNED
YIN DIArETEi? THICKtéSS
100 X 125 22 C
-07 N NO VISIBLE GOLD
-08 Y 50 X 175 22 C 100 X 100 20 C
-09 N NO VISIBLE GOLD
-10 N 50 X 100 15 C
112-11 N NO VISIBLE GOLD
r-.
PAGE 5
MPH - JOUTEL 07/10/86
GOLD CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
- MPH*/3JUL.86 NUMBER OF GRAINS
r--
r 1
, _ 7G'.1TE[
OVERBURDEN DRILLING MANAGEMENT LIMITE')
r^
r--'
: - - ~ NO.
-'.'4 -:5 _.,6
-05 -r,a -1'Y -11 lr
. :14-01.2 -:l? -414 -0C
-02,07_n8 -r1w -_0 -1: -12 -1_ -14
< 1_-~:_ , _ .r _ _ _. -03,04 -05,06
116-01
-03
-05 -06 -07 -02 -. 7
BT.~T C;'..1 .WET) N i~:.. .~.Wti. r:tiSHT iGFAM: DRY'
LABORATORY SAMPLE
AL
LOS
DC,vrr,iPTiL:'' __A:_
TABLE -1'. SPL:- CHIPE
TABLE TALE ~ rnir FEED.;,.~
M. I. LIGHTS
M. I. CONC
Ni). V.G.
CALC PFB
CLAST
c.'L!
n ~5•1' MATRIX i~Tti:
CY COLOR :ENC. TOTAL
!VCN F7AG MAS
SIZE CO ET
vi5 SR LB 07 :ï .Y
7.2 14.0 7.3
5
4.4
17. . 7.3 7. `r 8. 0
17.'? 9.• 7. ÿ 7. ii
G E. _'
16q..
jl. :I 16.2 10. 16.
E._
w.-
10.4
3.3 ..._
:1._ 0.4 0.2
ir._ 0.2 0.2 0.2 0.2 0.1 0.2 v'. 0.1 6.2 0.1 iv.. 0.2 0.2 0.2 o.: 0.1 4.00.3 "._ ... 0.3 ..1
0.0 0.0 ..r
• . r
0.1
_
.'.1 13.6 7.1 7.5
4.2 7.7 E.0 7.4 2.1 7.5 1c.o 1.7 0.8 7.9 16.1 8.9 7.7 6.2 3.Ç 7,9
li V . n .?
15.3 16.0 16.4 2.1
c~-
'3. 5:
1 t~~..•
10.7 5. 6 3.3
C: ü 6. . 5.v
200.4 266.2 2..79.9
204.9 156.8 114.5 276.7 137.1 146.2 139.6 207.0 .iJ:i. 8 .7t... 182.2
173.0 276.3 189.3 192.5 334.1 190._ 191.3 ?GO .1J4+' 16.0
401.6 ....1 466.3 :f7.1 'Rn
214.2 ^1.. 700.3 25.. 177, t
c 205.2 L60. } 1-6.: 16 .i 140. - ra,r 14_._ 1'.C.. r._.3
185.v 233.1 208.2 ia2.3 127.0 36.9 206.0 165.0 95.7 113.4 160.7 27E .E 150.9 169.0 142.7 2x=~.. .G 160.0 175.5 155.5 ..n .G n :4:: 147.9 295.1 43.4 747.7 r.r.r5 381.. 25t.2 _11..
..`., •1
1E:.! 267.5 T2.6 151.7r
22 ~
1:8.5 211.- •_..: 117.1 1;-.7
= lF,_
15.4 ,33.1 21.7 22.6 :9.8 25.6 70,7
72.1 50.9 26.2 46.3 55.0 20.4 13.2 30.3 41.3 ?4,ti
17.0 173.6 49.2 43.4 74.0 va. 6 54.. 78.8 94.6 50.9 7•.2 17.9 24.3 :4.9 ,...4 36.5 26.
T :6.7 4,0 uJ._ 40.2
26.2 :..6 J...
3.1 22.3 6.5 12.0 18.1 18.1 16.0 16.5 25.1 14.5
..Ç.3 10.7 7.5 16.8 21.7 14.5 8.0 77.0
5
25., 4G.: 21.1 27.7 41.5 44., 26.8 731.7 lz,,_
14.4 18.9 13.6 .:1.. i5.J 25.7 i7.0
18.: 5.4
17.: 1=..
17.
7.. 10.3 15.2 10.6 11.7 7.5 14.1 15.6 25.5 11.. 17.1 27.2 9.. J. 7
1J... 19.6 14.8 9.0
101.6 22.7 17.7 34.0 11.5 26.6 i7.. 39." 24.1 31.5
10.4 16.0 14.8 15.2 1iJ.. 3!:.Ù .7.1
54:4 16.1
12.E
3.8 8 19,3
0 1 0 0 0 0 0 0 V 2
C
:f
1
NA P 50
2004 G 60 P C,i
NA JV
NA 60
NA. 30
NA E 50
NA G ïti
NA P 60
NA 60
293 60 ~G+ 70
NA 4
76 P 70
60 F 6{;
NA F 70
NA 90
NA 90
157 P 60
NA P 85 19 8/BL 70
960 P 70
NA P 55
NA P 70
137 P 80
NA P BO
275 P BO
606 D 50
371 O 50
724 D 50
NA P 50
266 0'J
2~ ' D 80
1 70
NA F 80
96 D 90
148 F ;.7
NA Th; FrA '
NH I; 90 NA C/BL ';I
NA . 70
301 G 30
NA : .v
Ni:! P 50
.NA P ~:, _-,
162 8 30
50 40 50 40 20 50 30 40 40 40 30 30
40 30 .r i~~ 10 40 15 30 30 45 30 20 20 20 50 50 50 .11i 40 70 -,,
20 10
10 NA .. 70 ';; 20 20 ti.:' Ÿ:•_. vt 2..
NA NA. NA NA NA NA NA NA NA ,A NA NA NA NA 3~
NA NA NA NA NA NA NA NA NA NA NŸ x_A.
F'{t'. }Ÿt: NA NA NA NA NA NA NA NA NA !':; j !y, -. : . NA NA ï..: .i..
NA NA
fl
NA NA NA NA 14.,1..~ NA NA NA
NAj :'7.V .;AS.
NA NA NA NA NA NA NA NA NA NA NA NA Nti NA NA NA NA NA NA NA NA NA ;;i+. . Ar : i
NA m NA Fit! NA NA
L% 'j r
U U ;J
U
_ u
Li
U
U
U L:
3
~
L1
J
J
f.7
U ~
L '_ V •
_
. L .
Y
{h
'.(
Y L
'y t' y
y
.
`!
Y
V
Y
Y
V
r
.
Y
• f 'r
Y
Y
Y Y
~
. Y Y " ~ . ,
Y f
! V
`
1
';:"i v
❑J 'rr B
Y!'iY !: C51 .d
T.
H N. _B 3~ H :i
BE 4'B 1.
GB GB Gn SB H _. :. GB Gÿ B SN :P iB 3B J K
3.
A
Ÿ
GE = i i G: 3D :r _. _ .._ -- _. _. _:
v- - v : . H :B .. ât
45 _a i l'
_
i
TILL TI"~r
TILL TILL .:L_
TILL ILL
TILL TILL TiLr TILL 7ILL TiL-. BL_' TILL TILL TT:
:L- TILL TILL TILL
-- TILL _.
_ TILL TILL r _:_L. _ _. T .-- TILL
T
r-
MF- - .:CUiE2
yi rrfil7C _"' Rr-CÿOVERBURDEN DRILLIN6
LABORATORY SAMPLE L=_
=;MF-= S$EI2Î1T ;;:C.WETi
WEIGHT GRAMS DRY) Av DL6.R i F? i UN
CLA3T lA'^,n:~"°
M. I. CONC
TALE -10 TABLE TABLE SPLIT CHIPS FM CONC
M.I. CONC. ION MG. CALC LIGHTS TOTAL NAG MAS V.G. FE'B
SIZE % SN 3D 3T vY ;.OL...
LS ~„c = ~: GR~T Sr,
-15 3.: 0.7 8.8 191.8 151.5 40.3 25.7 10.6 3 -.t E.7 0.2 8.5 198.6 167.7 30.9 1Ç 7 3J.. 15.2 0 -1^ 2.: 1-~. ` 2 1.8 85.6 72.3 17.3 6.9 6.4 0
:17-01 9,1 t',.1 9.: 203.0 147.0 57.0 27.8 25.2 0
17 JS 6.: v 2..
r.' 3.3
6.1. 7.8
144.6 173.1
122.3 127.0
21.8 46.1
14.7 24.9
7.5 21.2
va 0
-;., ..B ..4 7.4 187.0 154.5 32.5 17.3 15.2 0 a.: 207.5 165.2 33.3 22.1 16.2 1
-0: :.3 .2 8.. 221.$ 179.8 " 12.5 9.5 ,.5 96.2 76.5 15.7 19.3 0.4 1
9.4 0.0 9.4 176.5 160.8 16.1 15.1 1.0 0 -.25 ,:,.5 v. ♦ ;:..i 141.1 127.5 17.6 1.:.5 5.1 0
~-- _ 9.3 311.9 247.6 64.. 36.6 27.. 0 -., 15,6 .. .J.3 32'.3 278.6 50.7 28.9 21.8 +', -08 4,: _.v 8... 255.2 220.7 38.5 20=.6 17.9 i'
.. ?'.t 149.8 117.4 32.4 19.4 13.0 -10 7.2 ..1 7.0 183.2 144.,, 38.9 21.6 17.: 0 -.2 .8 0.2 .6 156.5 106.2 50.: 33.6 16.7 0 -.a l.a V.:1 10.1 251.+. 1e7.7 57. 3 35.6 21.7 0
... 0.2 9.3 15 ~ ~.i 1,..~ 5c:.9 713.1 17.8 L7 -14 .5.1 t:.2 :5.2 442.7 :37.5 104.8 74.5 30._ 1 -ir' .v.. 'i.. 10.,. 162.7 108.. ..8 39.3 14.5 0
_.. -.:, i6.. C.: 16.1 271.0 200.; '1.0 . T 5,' ' 2..L =ï - 9.2 155.4 106.7 46.5 :5.0 11.5 0
-1E If:., ... l~ '.6~ 285.6 171.) 114.6 9.3.0 21._ ;1
r -.a 11=-C.1 4.4
v. 0.2 ...
.2 5.6
270.5 150.6
136.1 122.9
134.4 27.-
128.2 11.3
...C! 1).4
1 =i
.1a... 91.0 22.1 ...s 1i?.. 7.6 140.5 27.. 22.2 ._.
i'r 4,~25.5 .7 li.` 1:.. ) . 1 '.. 125.1 .r 28.. 16.9 ...2
154.0 127..1 _..= 13._ .:._ _r4. . _2..' 4G._ 26.7 :9.2 155.0 115.v 2... 16.9
7,7 4 207.9 167.3 ~_.r â?.1 a_.a 14n,5 1:.. 40.2 ._.. 1 7 ~._
3.1 165.6 :27.4 _=.2 ...8 2..,1
-.. . E. '._.,2 .12.7 . 4~5 ç.. 27.5 0.2 ..û.. .2.. . µ..3 :C.5 19,2 .
226,3 . . 41.1. a... LL,_ . 6.2 146.5 ....? _v._ 21.7 17.:
:21- .'2.> ..4
127.4
5E.! 2Y..
492 â 90 10 NA NA 6 80 20 NA NA P 90 10 NA NA G 80 20 :é« NA G {i{:' 23 NA NA G 80 20 NA NA 6
3580 20 ",,,A~~
7C750r ... i `,~ NA P 90 10 NA ;+:, TF: "JA NA NA
NA i r. NA NA NA NAir.r; NA NA NA NA F 85 15_ NA NA P 80 20 NA NA ' 80 20 NA NA F 75 25
/ NA NA
NA P 20 Ll' `` NA P 85 15 NA
NA 3IBL 90 10 NA NA Gr gL 9' ~ 10 NA
90 10 NA NA ô 90 1:' i iA NA G ?J 1,5 NA NA 6 80 20 N- `+A F24 20 NA ?f F: pp CL 90 10 NA
N F. r ~}~. fi
NA : : i~ 20 NA C 30 20 a^~
;#Ÿ r. a. 1~
.
NA . 20 NA F' 40 6: NA
F 50 5: 'v^r. NA U Y
NA P 50 50 NA NA a NA P 50 50 NA NA U NA P - 40 ,,,. NA NA U
3543 F 30 .`:} NA N:, \=4 P :0 40 Nr. ,:r. _ _
_ _ . . ~ . 5
e.€ ti :1 NA i.1 .it P 30 50 NA NA U
Na, v. r. N. NA
. .-
P . 7C, ..
_ -5 ' . . _ ..v
: 1!h :Ÿÿ~i NA r 65 75 N1 ':iri j
NA !''h C!
NA NA ~ 1~I7'1 NA NA NA ~ :rt NA ~: ": !~
.NA NA NA NA NA NA NA NA NA NA
NA NA NA NA NA ~ tJr NA
{Nf!
NA
. `' Y ?' _: _, 72LL U Y Y 33 ilL .- 1? Y Y .a „a .,_.. U Y
Y ï. 3: -.L_ L] . . . .._ .__ . Y Y ûB .
_: 1= Y Y Y aa _.
U Y Y Y _a .a U Y ( . 22 32 U Y Y J✓ =r'
L' ,.. Y Y -- .,: --- U Y Y Y 62 :_ _ -- L! Y __ :_ 7:1:- U . . . 52 32 ..-- L! . . 22 _. ar_
V Y , __ 22 U Y 62 38 ..._
~,... U . .y . C= _. .. Y . . 2. 22 4 Y . . _ . -__ U Y YYB
v Y Y . : U Y Ÿ
V - - -
v 32 22 33 32
Y Y 2
y Y 3?
Y OB GE
Y Y 78
' 28 i Y 71
i TILL SE TILL E TILL EP TILL 38 TILL • ELc TILL 3E TILL 22 TILL 22 TILL GE TILL
28 2E: TILL Y. Y 28 E TIL_ Y i TI_L Y Y B 2 TILL Y Y
Y P 9 i Y Y 3N 8N TILL
Y B E TILL Y TILL-'-5( Y Y 8 8 TILL Y Y B c TIL[ Y E E TILL
Y Y 7- 8 TILL Y Y E S 77:» Y Y : Y Y 8 '8 TILL
Y 2E 28 TILL '7'. Y 2E TILL
28 :2 TI_L Y 32 ZE TILL
:3 3: TILL 33 E? TILL 3E CE TILL
\.• Y CP EE TILL+311K •( eE TILL
Y E2 GE TILL
NA NA NA NA NA NA NA
NA NA NA NA NA NA NA NA
NA NA NA NA NA NA NA NA NA
0 y
U Y U
Y LI Y U Y L'Y
I v
U v U U Y
il Y U Y
Y U Y U Y
Li Y
hi
U
y
NA '2 Y NA Y
NA II .7" NA Li Y NA Y NA J NA Li NA NA Li NA
159.6 179.3 109.6 155.4 67.: ar IY11
ill •5
E.;.0
1419
95.1 141.2 100.0 :57.0 129.2 :08.7 109.6 110.0 155.7 106.4
•
151.5 177.6 168.9 275.4 177.4 95.2 100.4 148.1
115.6 1C2.9 53.6
142.6. 42.7
39.5 36.2 :4.0 34.8 7-•3 25.4 86.9 26.6 :1.5 27.6 7.7 Z5.: 30.7 25.9 29.5 42.7 107.2 77.8 7.8 34.7 3.3.3 16.6 21.c 14.6 19.1 17.0 16.6
19.0 16.7 21 1 21, T 15. _
16.2
" 44;80
16.3 23.1 25.4 27.6 17.3 38.4 16.8 19.8 14.a 21.5 21.6 13.7 14.7 19.7 14.0 90.4 22.0 4.5 18.7 15.5 9.1 12.Z 2.2 9.4 9.2 8.9 10.0 13.4
10.1 14.0 17.7 11.0 12.2 11.1
16.9 19.9 10.9 9.4 9.- 8.: 42.5 9.8 11.7 8.2 11.9 17.7 16.6 11.6 10.E 34.7 16.8 :1.2 7.3 16.4 14.8 7 r
9.6 6.4 9.7 7 .., • :a
7.7 3.3 9.: 6.7 6.6 9.1 8.2 E. 1 10.0 5. :
NA 130 NA NA NA NA NA NA NA NA NA NA NA NA
NA 47 NA NA NA NA NA NA NA NA NA NA
2027 NA NA NA NA 7 NA NA 7
70 TR NA
50 40 40 40 60
P 50 70
P 60 P 60 P SO
50 70
P 90 P 40 F 90 F 20 BK 100 P 80
80 G 60
30 50
P 50 P SO
70 70 20
TR NP NA
P 50 90
EK 50 FO
r 90
30 NA 50 60 60 60 40 50
40 40 20 20 30 10 60 10 20 NA 20 20 40 5C 50 50 20 30 ZO
NA NA 50 10 50 10 10
NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NP NA NA NA NA
MPH - :OUTEL 03!17:86
r--
riFH1ALE.816 OVERBURDEN DRILLIN2 MANAGEMENT LIMITE::
LAPORAT3RY SAMPLE L:2
l""
WEIGHT !4EPHT :GRAMS DRY)
M. I. CCN: ----------------
TABLE +10 TALE TABLE M.I. CCNC. NON SPLIT CHIPS FIE.) CON: LIGHTS TOTAL MAG MAS
AU -DES:RIPTI2N
:LAST MATRIY.
SIZE siu SD ET CV :DLO --------------- VlS BR L3 OT
NO. CALC il. S. FFE
H-36 -04 8.0 0.2 7.3 199.: -05 7.9 0.0 7.9 215.5 -06 5. 0.1 5.6 147.6 -07 6.9 0.2 6.7 190.2 -0.3 4.: 0.: 4.0 100.6
5.5 0.2 5.3 121.1 -10 11.9 0.5 11.4 198.4
1:2-01 6.:
126.6 -02' .6.9 0.3 6.6. 175.3 -03 5.6 0.2 5.4 :12.7 -04 7.4 0.2 7.2 175.1 -05 2.: 0.2 8.1 175.:
217.: -07 6.8 0.1 6. 7
1E5.1
6.5
1:7.9 -09 7.6
157.3 -10 7. : 0.7 6.8
217.2 127-:01 7.7 0.2 7.1 189.5
-02 3.3 0.1 3.2 114.2 124-C1 7. 0.2 6.8 257.9
184.8 -03 6.0 0. 1 5.9
194.2 -C4 6..9 0.1 6.8 21:;.8 -05 5.: 0.1 5.2 250.0 -06 6,8 Q.I 6.7 192.5 -07 7.2 0.2 7,0 112.8 -0E 7.7 0.1 7.6
166.4 -10 6.0 0.1 6.2 22.9.5
03.2 -I: 5.7 0.0 5.7 27.6 -1:
179.- -14
c -15 6.6 :.4 6.2 72.7
-16 6.2 6.4 164.2 -17 ' ' 0.2 2.7 52.9
0.0
r—
r—
7;5E 1 MPH - IOUTEL
r—
SOL: C; ;SEFIZATICN
r-- VISIBLE SOLD FROM SHAKINS TABLE AND PANNING
!.HH1AUS.26 NUMBER OF DRAINS
ABBPADED IRREGULAR DELICATE NON OP : V.5. SAMF4 P # PANNE) ======= ________ MAD ASSAY
UN DIAMETER THICKNESS r r TOIAL EMS FRB RE'ARKS
+Biz 117-01 N NS VISIBLE SOLD
r— -02.07 3)C 350 520 1
-04 N NO VISIBLE GOLD
TOTAL 1 n, 44.Z 2004
- -05 N NO VISIBLE SOLD
-OS N NO VISIBLE GOLD
-07 N NO VISIBLE GOLD
N NO VISIBLE SOLD
N NU VISIBLE GOLD
-'n N NO VISIBLE GOLD
100 X 125 220 2 2 957: 0.5% PYRITE 30 GRAINS ARGENOFVF:TE
TOTAL 2 14.5 293
-1: N NO VISIBLE SOLD
50 X 125 15 C 1 1
TOTAL 1 :7.8
-07 N 50 X 100 15
TOTAL 1 10.7 60
r-
r-
-04 N NC VISIBLE GOLD
-05 N NO VIGIBL7 GOLD
N NO VISIBLE GOLD
EST: 0.57. PYRITE
7GTAL E 14.5
r--
F-4
MPH - jOUTF1 05/17/E6
F..."." C. ;6'31:RIC:AT:ON ===================
VI57;L: Erin FROM EHAKI!-!S TABLE AND PANNING
MR+HIAUG.S6 NUMBER OF GRAINS
_ ;ArRLF 4
--"29
FANNFD .=....,---_-=
N NO VISIBLE ECLD
ABRADED IRREGULAR ..--L,-,•-.....===—
DELICATE --..._ ...-7.-.---.
NON NAB GME
CALC V. 3. ASSAY PPE REMARKS Y/N DIAMETER THICKNESSTPTPTPTOTAL
-10 N 75 X 125 20 C - 1
TOTAL 1 77.0
-11 50 X 50 10 C 1 I EST: 7% PRITE 75 X 75 is: 1 1. 750 GRAINS ARRENOPYRITE !:,-INE; 150X 150 290 1 1 225 X 2,70 44 C 1 1
TOTAL 4 . "m 960
-12 N NO VISIBLE GOLD
r- -17 N NO VISIBLE SOLD
-14 Y 100 X 150 250 1 1 EST: 30% PYRITE FINE - 730 GRAINS ARERNOFYFITE
T TOTAL 1 21.1 137 ,r1ARSE - MASSIVE
r""".
115-01.2 N NO VISIBLE mu
( 150 750 380 1 1
r- TOTAL 1 41.5 77F
.Y 50 Y 125 18 C I 1 EST: 60 GRAINS ARSEN:PYRITE 75X 75 150 , . 2 PHOTO REF 4126
r- 75 X 150 22 C 1 1 150 X 250 7E C 1- 1 200 X ZOO 3E : 1 1
TOTAL 6 44.9 60
-07 50 X 50 :0 C 1 1 EST: 60 ;RAINS F.BENGFRITE 50 X 7f ::c 1 04INS ETE S 75 X 100
100 12f
lE C n• .., I.
.... y 1
i
1 1
TOTAL
5C X 7;C: 10 C HET: 30 BRAINS FRITE EE 1 700 SR -A:NI AREZNOFT:72
125 :2 C 1fX: X 15:i :75 L
RASE 3
KPH -2:TEL 2523
33 CLASSIFICATION
2K£32 Sa SHAKING TABLEAND PANNING
MF:!- R4J6,e NUMBER OF GRA me
_ :. #
.
FAN33 VA DIAMETER 2ICKN EE
!e » 200 34 C 12*250 @[
Gm2E IRREGULAR ________ ===--
DELICATE :! #§ EMS
! !
~E«i ASSAY R§ REMARKS T P I.
! ,
—~— s F?7L
TOTAL 6 22 144
NO VISIBLE æ2
-10 !S k 13 27 C
TOTAL 1 14.4 266
26-0l :34 150 27 1 1
TOTAL 1 18.9 202
d2 m 2!125 3 c
TOTAL 22
m: N NO VISIBLE SOLD
i 5 X 13 20 : _ 1
TOTAL I 156 5
-05 m .wX 17 . 2:
w S VISIBLE ~ 2
TOTAL 1 32 148
; 3 SS§3 aciL :
k 2 VISIBLE GOLD
G Q2kE22
12 : 175
'TAL 1 b»
N: VISIBLE SOLD
S «2&E SLID
FA-,E - v'viJ TEL
SOLD CLASSIFICATION
VISIBLE .-:: FROM SHAKING TABLE AND PANNING
uFH H1-LG.- . NUMBER
t_ v!!iÿ:fi;
- AEER4DEIi IRREGULAR DELICATE NON CALO V. G. _=MEIF .. ^ ANNFn NAG ASSAk
.
YI1. DIAMETER THICKNESS T P T F P TOTAL GwS PPB REMARKS
N IN :x 150 :Ç L
TOTAL 1 i7.9 162
-i= , 25 X 25 C ,, v f . 100 .EC
175 'l.: 250 40 C
1 1 EST: 15:: PYRITE 1 100 FAINE ;;'r,SEAO'.R:-_ .. _,.:. 1 1 i C-RAIN ~],`4Lt'..fliA
TOTAL : 25.7 49
-:v rtj NO iii;PLi SOLD
-17 :4 NO VISIBLE SOLD
117-01 N NO VISIBLE GOLD
-._
N NO VISIBLE SOLD,~
-._ N NO VISIBLE GOLD-
-04 N NO VISIBLE TOLL'
iiv-:: ,, 1.:: r:M 34 0 1 1
TOTAL 1 22.1 7,5i
-02 ' NO VISIBLE SOLD
-i,_ è 50 Y 100 15 L 1 1
TOTAL 1 1ç.'
fw - EJTEE
GOLD CLASSIFICATION
VISIBLE SOLD FRCM SHAKING TABLE AD PANNING
i eÆae NUMBER OF GRAINS
ABRADED IRREGULAR DELICATE _ NON CALC 'SAMPLE « PANNE:
Ga GSAv 2A~~ mî2£2 T P. P T FTOTÆ EMS me 3%ys
:g PELLETS *3ÆI3 2 F@Æ RBINCP a:e
e: N 2 e@§3 GOLD
r•-• e7 N NC 2SDLE GOLD
-14 § 2 z SO 2 c 1
TOTAL 1 74.5
-: N Æ VISIBLE SOLD
®6 N K VISIBLE O3
«2 N Æ VISIBLE SG
«a N NO VISIBLE SOLD
23-01 f 3! 3 :E EST: 90% R:17: l9g:g!
TOTAL ! 122 0.2
m: N NC VISIBLE ;OLD
m. , NO VISIBLE SOL 2
N NO VISIBLE 22
-05 § NO VISIBLE MILD
� 2 Æ 22s3 SOLD.
s: J Æ VISIBLE e2
g VISIBLE ESL:
N £ 2s2a SOLD
m. : R gesE SOLD
w4 N :IC. z4EC e c
2TPS 752,E
3 VISIBLE 2s
..~t Giil~r~ r k - ~.~,_~;
._IEL GOLD CiO,M, Stlrif.IÎ`iG TAE+^ AND PANNING
%ME`R OF C•RAI„ÿ
r-- 4 • - nBERA.LED IRREGULAR DELICATE ,:^N CALC '.'.,r,-.
=='"- # :jr.ÿ°;E =====_— KAG ASSAY' YA DIA►'ETE', THICKNESS T G ' P T P TpTP jMS PPE REMARKS
!) '+' cfi 1:' 2 1
TOTAd. 1 DE.:` 8
NO VISIBLE GOLD
.S N NO VISIBLE 6OLi
-09 N NO UISIELE SOLD
N NO VISIBLE GOLD
-0C 'ti NO VISIBLE SOLD
-03 ,t ',ü VISIBLE GOLD
NO VISIBLE GOLD
-l.E N 100 X 1_5 2^ C 1
TOTAL . 1â.3 17,)
-..w N NO VISIBLE GOLD
-." N NO VISIBLE GOLD
NO VI°IBir GOLD
- NO N lISIBLE GOLD .
NC ,.S.SL_ 'LLD
~~u ' vi~r F ~. • .r_ . . . ~~ • • _- SOLD
-02 ;ÿ NO VISIBLE : GOLD D
-.. _ VISIBLE BOLD
._ .IEI_ GOLD,
NC vISIBLE SOLD
-_--L- -_r
NO ,_=IBL= GOLD
"'d_ ....___ BOLD
EST: vL.: PYRITE
+! z - JOLit
__AESI`.Er :ûN -------------------
___ =ROM SHAKING T4;L. AND PANNING
"HH1rL:L.66 NUMBER OF GRAINS
ABBRACED IRREGULAR DELICATE NON CAE. V.E. =~'r*R:E 4 PANNED =======_ --- NAG ASSAY
Y:',. DIA."E `R THICKNESS T F' T P T P TOTAL EMR ;-?s FaARKE
; NC : iSi: ! SOLE:
-1= Y 25 X 2E 5 C 2 2 EST. 90-% PYRITE [MASSIVE.
TOTAL 2 90.4
1E3-01 N NO ;ISISLE GOLD
-02 Y 50 ,? 50 • 10 C : 1 Es i "T . . ;,,'.t,. ~ PYRITE 30 GRAINS N=SE`cCPYF:I. _
TOTAL 1 4.5 47
124-01 N NO ;;ISIBLE GOLD
- `! NO VISibLE SOLD
- N ND VISIBLE GOLD
-04 N NO VISIBLE GOLD
-0 5 N NO VISIBLE GOLD
-;;t N NO VISIBLE SOLD
-07 N AO VISIB1 = GOLD
-0; N NO VISIBLE SOLD
-09 NO VISIBLE GOLD
'.. ,; '#O ';Iv_.LE DOL:
-.. ,` 2ÿ/. °_'5 sR C 1 1
TOTA'. 1 12.3 :02'
-i' ~' .tn -titi = rt
. .. :.; •.`.i. __ ~:;Li'
Nn ,`:S:` E 'rL~: -- --
-'.L NO vISIBLE SOL:
_.V N NC 'I_',~ ',:_:_L E Gî;L_
:5 . 50 E „ • _ET. 21. P `-R
I T E 1 GRi : t GALENA
MPH - 2U TEL :.,S;17 /C6
SC2DAS£EG22
23§2 2g =ROM SHAKING, TABS AND PANNING
7+:gG k NUMBER CF GRAINS
ABRADED IRREGULAR DELICATE NON CALC V.3. SAMPLE# FANNED me ASSAY
«N DIAMETER THICKNESS T F T P T F TOTAL æe 75 REMARKS
+-k TOTAL 1 11.1
3: 0
APPENDIX C
Certificates of Analyses
Ba.d.Cien • Company Lid.
5420 Canotek Rd., Ottawa, Ontario, Canada KIJ 8X5 Phone: (613) 749-2220 Telex: 053-3233
BONDAR--ÇLEGGw ~~ ~
( L
REPORT' 014-2186 ( COMPLETE )
REFERENCE INFO:
CLIENT: MPH CONSULTING
SUBMITTED BY: OVERBURDEN DRILLING PROJECT' NONE DATE PRINTED: 3-JUL-86
NUMBER OF LOYER ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD
1 Cu Copper 23 1 PPM HCI-H1103, (1:3) Atonic Absorption 2 Zn Zinc 73 1 PPJ HCI-HNO3. (1:3) Atonic Absorption
3 Ag Silver 23 0.:1 PPM HCI-HNO3, (1:3) Atonic Absorption 4 As .Arsenic 23 2 PPM HNO3-HC104 Colourinetric 5 Au Gold 23 S PPd AQUA REGIA FA-AA 0 10 la weight 6 TestYt Au Test Veight 16 0.01 go
SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER
HEAVY MINERAL CONC. 23 -200 23 PULVERIZE -200 23
REBARRb: t BEAKS LEbS THAN. > MEANS MORE THAN.
REPORT COPIES TO: BILL BRERETON INVOICE TO: BILL BRERETON
d))
Geochemical Lab Report
Bwdr{.lq{ k Company Lad.
5420 Canotek Rd., Ottawa, Ontario, Canada KIJ 8X5 Phone: 1613) 749-2220 Telex: 053-3233
CLIENT: MPH CONSULTING PRi1.iFCT: C-R7R
SUBMITTED BY: OVERBURDEN DRILLING DATE PRIMA: 27-.ii1N-Aa
REPORT: 41ë-2125 t COMPLETE )
NUMBER OF LOYER ANALYSES DETECTION LIMIT EXTRACTION METHOD
REFERENCE INFO:
ORDER ELEMENT
3 Ag Silver 4 As Arsenic 5 Au-150 Gold -150 Fraction 6 Au+150 Gold +150 Fraction 7 Au AN Gold Weight Average
10 0.1 PPM HC1-H103, (1:3) AtoAit Absorption 10 L'PPM HNO3-HC1O4 Colourisetric 10 0.01 PPM AQUA REGIA Fire Assay AA 10 0.01 PPM AQUA REGIA Fire Assag AA 11 0.01 PPM
B Testiit Au Test Weight -150 10 0.01 gis
9 -150Yt Weight -150 Obtained 10 0.01 gas
10 t150iit:Weight +150 Obtained 10 0..01 pis
INVOICE TO: BILL BRERETON REPORT COPIES TO: BILL BRERETON
SAMPLE TYPES HUMBER SIYE FRACTIONS dOMBa:R SAMPLE Pka:PARATItiiiS 411MB
HEAVY MINERAL CONC. 11
REMARKS: E MEANS LESS THAN.
+1501-150 11 METALI.ICS +150/-150 10
1 Cu Copper 2_ in Tint
10 1 PPM HCt-HNO3, (1:3) Atonic Absorption 10 1 PPM NC1-11NO3, Atnnit Ahsnrptinn
Geochemical~ Lab Report
Barba lee i Cower Lid. 5420 Canotek Rd., Ottawa, Ontario, Canada KIi 8X5 Phone: (613) 749-2220 Telex: 053-3233
Rï1,itGi : 1-bib REfGKI: vit-4126
LU tifRE?#; :AsiQii i~ fig A5 Au 1>:suf UNITS FF5 P?A . FFA ?PA FPO O4
s 0101-01,02,02A-3/4=,0.7t-314 01-13,034,04,04A-3/4 :1-05,054,06--3f4 01-0 ,Ÿû,DEf!-Jl~t
30 0.3 >s~ 20 (0.1 120 23 (0.1 78 2,4 40.1
172 30 89 1800 114 355 101 450
k:1-!?,171t111Ÿ.`-J:4 Gt 60 0.2 - ;<=1-1_.,;,.;4 33 •. 16_ <0.1 .
:1'.ti-3ï F l08 cf 90 J8
:1-22=3>rh 7i 60
<.1
10 15 3.00
48 35 §.a0
<0.1 105 IS B.00
0.4 152 20 9.00
01-2:-:' .450 404 0.0, 610 ÉA:5 i.5? 02-01-3fe 100 42 0.2 115 'r 7.J0 02-02-3;4
72 36 40.1 175 55 10.00
02 -03 23 !i <0.1 13 35 10,04 02-04-3/4 42 25 <0.1 24 55 7.00
- ~ _,.71_6;: ;. 02-06-314
: 02-07,47A-3/4 43-01,42-3/4
4Y w41
Jû
76 46
21
25 530 30 26
\Li <0.1 `•V.1 ,ti0.1
zsr.i
'.;.'-i1t1,,fC -,i: 4 iF3-ÿ,a';+ ~-ÿt4 . `:â :1iiN '1!
...• .,~_. .
32 160 130 -'. 132
58 40 ul: 0
:0.1 0.3 0.2 . ~0.1 <0.1
16 45 7.00 7
_0 40 10.00
300 30 10.00
,!i <.14 6.04
, 17 110 .00
145 95 10a40
16 25 5.40 J: 890 9.40
331 1i23 3.00
- iii-_~ + • ,. ..;, ,
0-,2:3 6 '; izc •+ - ,i,~l.,`rt ~4-13-8 :ILL-i+-'
~ .tÿ
114 11:
2300 • rri,`:`
;:v 3t+ • .t_
2500 1340;
`.t.'.~1
..i i.û'.1
2.8 6.4
05-41-02-314
- - -
. ._-.'j
.6-01-3:4
_. : ... r!-v'i
05-44-5/4 15001~'J~;
- ~~'
:74 72
4; 4~
38 60
. ~ i4.1 0.2
`•.4.1 <0.1
~ f~~?. ~ • • Jl,' 1a..4Ÿ •
• 55 105 li..00
~ .V8~ fŸ • ~ S5. 10.40s
270. 55 1.41 •350 :23 2.00
• 'r.' .â.Vl.,
_- ~~r
3:~ :t: • 14.00
235 1v 1.00
145 45 1:.0;
61 15 10.00
;xtiil.»-36 10.00 10.00 7.00 10.00
36 145 10.00
01 -0,0Y11,11,1011 ,4 40 01-11A-3/4 41-13,14 3:4 01-13A-3:'4 01-15,16-3ï4
48 24 <0.1 95 36 <0.1 46 28 <0.1 66 30 .40.1
0 10.00
<25 2.00
10 7.00
<L5 2.0C=
535 3.00
NUAGtE
REPORT; 416-2126
SAAP1.E t10!8ER
ELEAEtt E4
tHi'8 PP5
07-01,02-Jt4 62 07-03,04-.314 144 01-05,06-3, 4 184 05-01,02-314 60 0Ÿ-03,04-314 .64
in Ag
24 •:.0.1
28 1.1
100 <0.1
28 11.1
30 •,0.1
Boadmm.leu & Compaq Ltd.
5420 Canotek Rd.. • Ottawa. Ontario,
Canada KIJ 8X5 Phone: (613) 749-2220 Telex: 053-3233
1111/ABO NDAR-CI_E .
Geochetnical Lab Report
IRtiJtLi= L-ûi
!M0t
As PP9t
Au PP8
ttss2t ga
78 50 106 4? 130
160 210 50 115 65
10.04 10.00 10.00 10.00 10.00
Zâb 284 115 480 338
85 260
3580 50 10
10.00 1.0.00 4.50 2..00
10.00
iv-03-,lit Dv 1"t{ .4.1-. .1t1 GJ f....{tN 11t-3,.02-314 1:94 40 1.1 330 65 10.00.
11-4 j.iJ?-~1g 7i( .24 <0.1 v4G LL0 8.97 11-47-314 198 46 s0.1 159 100 10.00 11'08-31$ 94 100 ;0.1 940 20 10.00
12-=.4,0. 41,1 .J1tv f.V/
09-=7,06,0i-414 72 O9-10,11-3/4 120 '.f-12-3:4 1.16 09-15-31; 19.8 09-14-314 36
48-v5,ûg-sr 4Ÿ 0,5-07-314 14 08-09-s,.4 450 09-01,02 -314 90 9-45,44-3#4 144
7 139 312 274 322
,s45 70 15 55 95
9.00 .8.60 7.00
10.01
.44 '<ü.I
120 <0.1
790 <0.1
34p
:0.1 10.00
0 38i0.1
311 .0.1
31 i0.2
42 ;:0.1
250
:0.1,
66 t0.1
BO- bs C-878 PAGE 1 REPORT' 016-2125 ~
SAMPLE i10118ER
ELE14E1T Cu.
ü11IT5 PPa
Zn
PPl!
Ag.
1111
As Au-150 Au+150 Au AV Testfit -1501t +1501t PPM PPl1 PPM PP11 gas gas ga
Boasae[.1eu t Coi.o.ar LW. 5420 Canotek Rd., Ottawa, Ontario, Canada 1(13 8X5 Phone: (613) 749-2220 Telex: 053-3233
Geochemical Lab Report
PREFIX II-86-01-11,12,12A-3/4 86-03-•47,08-3/4 86-03-12,12A-3/4 8d-04-03,66 -3/4
86-04-11,12-3/4 ` 134 80 0.6 86-08-08-3J4 181 109 0.5 86-09-08,09,094-3/4 89 30 ' <0.1 86-10-01,01A,02A-314 153 30 0.8
86-12-01,02,03-3/4 125 44 f4.1
120 ` 48
45 161
0a61 0.37
C0.01 ttiti
<0.01 2.25 0.02 5_96
0.49 ' 1.05 <0.01 1..5A
8.00 7.00 7.00
16.1}6
10.80 9.24 9.71
12.42
2.59 5.28 3.95 4.39
163 1.14 0.30 1.03 20.00 23.44 3.64 168 0.46 0.12 0.38 7.00 9.26 2.91 198 0.40 {0.01 0.36 20.00 25a16< 3.11 134 0.35 1.79 0.65 17.00 18.97 4.98 k68. 1 07 0-46 0_76 6 00 8 4'g 7 99
480 0.18 7.93 2.119 6.00 8.71 4.16
48 25 0.6
85 30 O.1'
350 69 ' f0.1
260 30 < C6_1
86-11-07,11L-3/4 157 -; 27 <01
1111114 Geochemical Lab Report
Soedr-CYQ & Canonry Ltd.
5420 Canotek Rd.. Ottawa. Ontario: Canada KIJ 8X5 Phone: (5131 749-2220 Telex: 053-3233
PAGE I PRfl.IECT I NONE R[PORTi 814 2186
SABPLE ELEAENT Cu Zn Ag 'As Au TestYt NUABER UNITS PPa PPtt PPN PM! PPB Oi
H-86-12-06,07-3/4 93 111 4.3 315 155 7.00 H-86-12-08-3/4 57 96 0.8 314 285 4.00 H-86-13-01,02-3/4 44 112 0.6 520 90 H-86-13-03,04,05-3/4 40 88 0.5 262 145 11-86-11.16,07-f3/4 30 64 0.6 165 240
H-86-13-08-3/4 35 240 0.4 153 140 H-86-13-09-3/4 95 1375 0.7 378 90 2.00 11-86-14-01.01A-314 41 290 0.6 366 170 H-86-15-01,014-314 63 445 2.5 )2000 870 11-86-16-0t,e1I,3/4 59 139 0.8 704 300
H-86-11-01,01A,023/4 47 280 0.6 504 240 9.00 H-86-18-01-3/4 60 108 0.5 . 528 445 7.00 H-86-18-02,024-3/4 38 98 0.6 760 800 9.00 H-86-18-03-3/4 61 180 0.7 380 25 6.00 N-8d-111-04-1/4 60 142 0.5 238 40 5.00
H-86-18-05-3/4 103 165 0.4 - 177 30 5.00 H-86-19-01-3/4 32 40 0.4 664 450 8.00 H-86-19-02-3/4 75 265 1.8 379 305 7.00 R-86-20-01-3/4 64 115 0.6 808 180 7.00 H-84-20-02-3/4 tt4 ?b0 0.7 1280 485 6.00
H-86-21-01,02-3/4 119 450 1.2 656 485 6.00 H-86-21-05-3/4 37 475 3.1 920 60 5.00 H-86-22-01-3/4 81 156 0.8 314 75 4.00
Bondiw-Clasi& Cowpony Lid.
5420 Canotek Rd., Ottawa, Ontario, C:.nada KU 8X5 Phone: 1613) 749.2220 Telex: 053-3233
Geochemical Lab Report
REPORT; 1r'213: Rttvsÿi ; #Tt?¢t PCIc 1
iâAPLE ,
ELE3lE1iT £u in Ag As Au-150 . Au+150 Au AV Ti:st;it -1506it +l:J~;kt
+EUAEEP UNITS PPA PPA PPA PPA PPA PPA PPn gas gas ges
ii-B0-21—+l3 04 8 L.$ 942 9.48 0.04 0.25 2.50 ;,04 5.34
Bo.dorClegg t Coe.'..y Ltd. 5420 Canotek Rd., Ottawa. Ontario, Canada KU 8X5 Phone: (613) 749-2220 Telex: 053-3233
Geochemical Lab Report
REPORT' 016-2263 NONE PARE 1 .PRfllrrn
SAAPLE ELEAENT NUABER UNITS
Cu PPA
Zn PPA
Ag PPK
-As 110
Ar PPB
TestHt 9.
H-86-22-02-3/4 400 70 1.0 570 70 ' 4.00 H-86-23-01-3/4 230 79 0,8 1120 75 6.50 H-86-23-02,03-3/4 192 72 0.8 696 110 10.00 11-86-25-01-H 170 68 0.6 173 160 0.88 H-84-25-02,03-3/4 200 46- 1-6 3g6 230 R-Od
H-86-25-04-3/4 154 96 0.6 360 245 7.50 H-86-25-05-3/4 210 90 0.8 328 205 7.50 H-86-25-06-H 49 56 0.3 61 135 2.50 H-86-25-07-. 3/4 104 20 0.6 129 _ <5 10.00 H-86-26-01,01A-3/4 820 46 6-8 351 90 1.50
8-86-27-01-3/4 114 32 0.8 374 450 6.50 H-86-27-02-3/4 134 34 0.6 248 330 10.00 H-86-27-03-3/4 128 46 0.6 370 240 10,00 H-86-28-01,01A-3/4 1500 80 1.4 380 20 2.50 11-84-99-01-3/4 ISO 37 0.6 512 110 9.00
H-86-29-01A-3/4 68 43 0.4 392 165 8.50 H-86-29-02-3/4 80 35 0.6 334 <25 7.00 H-86-30-01,02-3/4 42 32 E0.1 141 230 10.00 0-86-33-01,02-3/4 200 80 0.8 472 80 6.00 8-86-33-63-3/4 106 104 0-6 384 175 10.00
H-86-33-04-314 108 100 0.6 552 230 150 8-86-34-01,02-3/4 100 40 <0.1 130 180 10.00 0-86-35-05,06-3/4 198 49 1.2 132 115 10.00 H-86-35-07-3/4 100 36 0.6 155 <150 0.32 11-86-35-08 09-3/4 104 71 0.8 264 380 10.00
H-86-36-01-3/4 130 56 0.6 308 <60 0.80 H-86-36-02-3/4 220 49 0.6 268 170 9.00 H-86-36-03-3/4 90 43 0.8 896 220 10.00 H-86-36-05-H 3100 1280 5.6 >2000 265 3.00 H-Ré-38-01-3/4 132 58 0.8 336 220 10.00
H-86-38-02-314 180 64 0.7 268 145 9.50 H-86-39-01,02-3/4 100 34 0.4 488 1090 10.00 H-86-39-03-3/4 190 65 0.6 382 60 10.00 H-86-39-06-314 62 40 0.6 512 10 10.00 H-sh-40-01-3/4 130 68 0.8 714 280 10.00
H-86-40-02-3/4 188 82 0.4 344 390 10.00 H-86-42-01-3/4 180 54 0.5 312 50 9.00 H-86-43-01,02-3/4 140 57 0.8 372 205 10.00 H-86-43-03-3/4 136 50 0.1 720 300 10.00 H-86-45-01,02-3/4 128 66 0.4 488 250 10.00
Bonder-Om & Catty Lid.
5420 Canotek Rd.. Ottawa, Ontario, Canada K11 8X5 Phone: 1613) 749-2220 Telex: 053-3233
GeochDem~icai Report port
REPORT: a16-2?63 PFO:IFf.T; iE0lfF PAGE 2
SAAPEf EtEHENT mUFBER Wig
Cu PPM
In - PP!►
Ag PPD
As PPM
Au PPB
Testltt gi►
0-86-45-03-3/4 80 54 0.6 280 50 9.50 H-66-45-04-3/4 108 48 0.4 568 195 10.00 11-66-45-05-3/4 110 40 0.4 332 245 10.00 H-86-46-01-3/4 330 94 1.2 588 380 9.00 H46-47-61-1/4 366 75 t_$ 542 15 3.06
H-66-47-014-3/4 260 64 0.6 332 55 10.00 H-86-48-01,02-3/4 134 43 0.4 336 210 10.00 H-86-48-03.3/4 120 2? 1.0 386 95 10.00 H-86-48-04-3/4 136 36 0.6 274 255 10.00 H -GA -46-05-314 250 49 1_0 1000 65 9.00
H-86-48-06-3/4 140 71 0.6 300 25 10.00 H-86-50-01,02-3E4 200 62 0.6 373 240 10.00 H-36-51-01-3/4 320 64 0.8 282 200 2.00 11-86-51-014-H 260 68 0.6 132 250 1.00 H-86-52-01-3/4 15R 6R 0-R 177 330 5.00.
H-66-52-014-3/4 184 80 0.6 318 135 5.50 H-86-53-01-3/4 340 66 0.6 134 <25 2.00 8-86-53-02-3/4 2200 43 1.4 356 320 8.50 H-86-53-03-3/4 172 47 1.4 336 120 10.00 4-86-. 53-04-314 176 60 1., 410 560 2.00
H-86-54-01,02-3/4 200 63 1.0 504 135 10.00 H-86-55-01-314 160 48 0.8 386 365 9.00 H-86-55-02,03-3/4 148 47 0.6 544 135 10.00 8-86-55-04-3/4 146 38 <0.1 368 55 10.00 H-86-55-05-3/4 88 44 (0.1 696 540 9.00
8-86-55-056-3/4 86 48 <0.1 352 360 10.00 H-86-56-02,03-3/4 28 23 <0r1 15 130 10.00 8-66-57-01-3/4 156 56 0.8 370 120 10.00 H-86-57-04,05-3/4 144 108 1.0 564 90 10.00 H46-57-06-3/4 104 57 0.8 272 105 10.00
H-86-57-07-3/4 114 48 0.6 302 <10 10.00 8-86-57-08-3/4 88 51 <0.1 380 40 10.00 H-86-57-09,10-3/4 110 45 0.8 284 60 10.00 H-86--58-01,02-3/4 200 68 0.8 616 440 5.00 H-86-59-01-3/4 170 66 0.8 824 285 7.50
H-86-59-02,03-3/4 142 4? 1.2 424 640 10.00
Bwmr.Ora & Cony. ;^" Lid.
5420 Canotek Rd.. Ottawa. Ontario, Canada K 1 8X5 Phone: (613) 749-2220 Telex: 053-3233
Geochemical Lab Report
REPORT: 016-2262 PROJECT. NONE SAGE 1
SAMPLE ELEMENT Cu Zn Ag As Au-i50 Au}150 Au AV TestRt t150Yt NUMBER UNITS PPM PPM PPM PPM PPM PPM PPM gas gas gas
H-86-35-01,02-3/4 134 37 0.1 346 0.43 v.y3 ; 4.4J r0.00 r1.0+3 0,41 H-86-35-03,04-314 90 36 0.6 284 0.78 <0.01 0.76 14.00 15.96 0.33 H-86-37-01-3/4 160 53 0.6 352 0..13 <0.01 0r12 7.00 8.39 0.56 H-86-34-04-3/4 66 42 0.4 290 0.10 <0.01 0.10 13.00 14.57 0.38 H-86-39-05-314 60 37 0.3 1072 0.18 0.01 0.17 20.00 41.46 1.51
8-86-44-01,07-3t4 200 52 0.5 384 0.23 106.78 ?.93 9.00 10.79 0.28 !l-86-56-01-3/4 158 37 0.6 672 0.96 0.04 Ell 12.00 13.46 2.68 H-86-56-04,05-314 160 36 0".6 536 0.56 14.93 1.67 15.00 16.69 1.40 H-86-57-02,03-3/4 176 64 0.6 " 428 0.40 39.66 '"ü`;9L-- 20.00 22.49 0.30
(50 1.50
95 9.00
35 4.00
110 8.00
170 8.00
270 B.00 450 375 170 175 9.00
265 5.60
30 6.50 70
155
140 1.00
100 <5 40
400 20
115 65
185 15 30
so•+rClan & Comma W.
764 Belfast Road Ottawa, Ontario Canada K1G 023 Phone: (613) 237-3110 Teb:: 053-4455
Geochemical Lab Report
REPORT: 016-2332
PROJECT: NONE PASE 1
SA1PiE ElEBENT Cu Is Ay; As Au TestYt NUMBER UN1TS PPM PPM PP1 PP1 " PPS p
0-66-60-01-3/4 160 60 0«2. _ ,~ 55 H-86-61-01,02-3/4 ~ ~ ~ 128 . 98 : " "0.1 ~ ~ ~ " :325 H-84-62-01-3/4 300 76 ' 0.2 210 8.00' H-86-62-01A-3/4 194 60 0.4 '356 150 H-84-63-01,02-314 250 60 4.5 .1446 70 8.00
H-86-63-03-H H-86-63-04-3/4 240 H-86-63-05-3/4 132 H-86-63-06-3/4 164 H-86-64-.01-3/4 148
0.7
0.3 0..2.
0.6
105 115 165 175
49 280
H-86-64-02-3/4 310 96 H-86-65-01-3/4 180 188 H-86-65-0111-3/4 184 290• H-86-66-01,02-314 196 128 H-86-66-03-3/4 160 76
0.7 672 0.9 008' 0.4 7
!~W
s~I •.
0.5 632 0.3 1112
95 ' . 3.00 840
A 290 195 110
H-86-67-01-11 160 •' H-86-67-01A-3/4 164
H-86-68-01-3/4 164 H-86-611-01A-3/4 . 200 H-86-70-01-3/4 190
H-B6-70-01A-3/4 176 H-86-71-01-3/4 80 8-66-71-02-3/4 128 H-86-72-01-3/4 112 0-86-72-02-3/4 64
H-86-72-03-3/4
160 H-86-72-.04-3/4
104 H-86-72-05-3/4
92 H-86-72-06-3/4
120 H-86-73-01,02-3/4
112
H-86-73-03,04-3/4 64 8-86-73-05-3/4 68 H-86-73-06,07-3/4 62 H-86-74-02-3/4 68 H-86-74-03-3/4 44
H-86-75-01,02-3/4 96 H-86-75-03,04-3/4 68 H-86-75-05-3/4 162 H-66-75-06-3/4 92 H-86-75-07-3/4 250
148 72 48
360 - 76
0,6 0.2 0.2 1.1. ' 0.4
104 106 71.
1352 186
120 0.7 286 44 0.5 232 58 0.3 664 96 0.3 512 42 0.2 36
46 1.3 504 32 <0.1 " 52 56 0.3 127 48 0.3. 167 68 0.2 > 584
36 <0.1 146 54 <0.1 57 40 0.2 68 34 0.3 7 42 <0.1 31
36 0.2 84 24 <0.1 28 29 0.1 36 26 <0.1 46 40 0.4 544
1.50 4.00 9.00 8.00'
1.7 712 )20000 5.50 0.1 40 580 0.2 ` 146 235 0.2 888 410 0.2 1072 35
Hadr•CIeQ &Company Ud.
764 Belfast Rad Ottawa, Omar- Canda 1C10025 Phone: (613)237.3110 Telex: O53.44 5
REPORT; 016-2332 PRO.N;CT: -10NE PAR 2
in Ag esiU1
PPA ?PA ' PPA ?PI p SAAPLE ËtfAplT NUABER UNITS
Ca ?PI
H-86-75-01-3/4 11-86-75-04-3/4 H-86-76-01-3/4 8-86-76-02,03-3/4 H-86-76-04,05-3/4 ;
130 36
124 110 120
1-86-76-04,07-1/4 "90 H-86-76-08-3/4 84 1-86-76-04-3/4 64 H-86-71-10-3/4 98: H-86-76-11=3/4 92
H-86-77-01-3/4 60
H-86-77-02-3/4 84 H-86-77-03-3/4 44 H-86-77-04-3/4 16 H-86-78-01.r3/4 98
0.1 ~ 0.4 168 0.2 ' " " 234"
s40...1 `` 512 f0.i 254
(0.1 170
0.2 15 75
1.1 ' 240 "50
0.6 ' 191 255
0.3 264 310
145 195 • 515 55
H-86-1842*03-314 H-86-78-04-3/4 H-86-78-05-3/4 H-86-78-04-3/4 H-86-78-07-3/4
36 ` (0.1 28 " 0.1 66 0.4 60 0.3 40 ' ~0..1
160 65
~ 35 20 30 5.00 33 (20 2.5!
44 3820
5.90
H-86-78-08-3/4 144 H-86-79-01-3/4 y120 H-86-79-02-3/4 192 0-86-79-03-3/4 124 H-88-79-04,05-3/4 132
36
9 36
14 40
52 54:
88 48 20 48 64
56 28 42 48 43
40.1 0.2 <'
C0.1 (0.1 <0.1
420 38 (0.1 60 32 ` 0.1
104 80 40.1 98 60 (0.1 80 38 <0.1
106 54 <0.1 170 ' 68 <0.1 192 74 0.2 152 52 0.2 132 58 0.2
84 200
226 170
186 15 8.00
45 410 4.00
143 55
61 100
20 95
13 50
109 185
129 235 ' 9.00
17 30
336 50
195 25 9.00
103 '560
144 25
N-86-80-01.3/4 H-86-80-02-3/4 H-86-80-03-3/4 H-86.80-04-3/4 H-86-80-05-3/4
H-86-80-08A-3/4 H-86-80-09-3/4 H-86-80-12-3/4 H-86-81-01,02-3/4 H-86-81-03-314
H-86-81-06,07-3/4 H-86-81-08,09-3/4 H-86-81-12,13-3/4 H-86-81-14,15-3/4 H-86-81-16-3/4
G LabCOClIeIIIIl~ll
Report
B.aiarL7eQ & Company Ltd.
764 Belfast Road Ottawa, Ontar» Canada 1C1G (Z3 Phone: (613)237-3110 Telex: 053-4455
95 8.00
45 9.00
120 9.00 12? 25 9.00 125 120 8.00
84 104 120
H-86-64-02-3/4 ii-86-84-03-3/4 H-86-84-04-3/4 H-86-84-05-3/4 H-86-84-06-3/4
PROJECT: HONE PAGE ; 4
SIMPLE HIlABER
H-8641-17-3/4 H-86-81-18-314 H-86-81-19-3/4 H-86-82-01-3/4 H-161212-3/4
H-86-82-03-3/4 90 1-86-82-. 04,05-3/4 132 H-86-82-06-3/4 170 H-86-82-08-3t4 320 H-86-84-01-3/4 80
34 84 '`.' "<0.1
320 0.9
68 <0.1
30 (0.1
68 : <0.1 141 "" ' 68 (0.1 96 <0.1 I6
144 0.2 296 .38 <0.1 338
545 390
40 200 9.00 10
40 70 30
130 9.00
ELEHEHT . Cy Zn Aq As Ay Iesütt OMITS PPA PPA PPA PPS PPB gi
84 96
220 96 88
131 98
121
REPORT: 016-2332
H-86-84-07-3/4 H-86-84.08-3/4 H-86-84-09-3/4 H-8645-01=3/4 H-86-85-02. -314
76 84
160 124 ` 104
32 ` <0.1 44 0.1 60 0.3 56 0.3 40 (0.1
238 10 544 25 190 100 214 300 354 15
H-86-86-01-3/4 40 34 H-86-86-02,03-3/4 88 38 H-86-86-04-3/4 160 48 H-86-86-05-3/4 ;} 1040 H-86-87-01-3/4 112 96
H-8647-02-3/4 47 48 H-86-87-03-3/4 98 64 H-86-87-04,05-3/4 180 80 H-86-87-06-3/4 1200 84 H-86-88-01-3/4 76 73
H-86-88-02-3/4 68 92 H-86-89-01-3/4 80 78 H-86-89-014-3/4 76 52
<0.1' Al 515 9.00
<0.1 12 625 6.00 0.5 544 265 . 7.00
0.6 218 150 4.00
0.2 ` 286 110
0.1 ` 174 30
(0.1 212 70 9.00
0.1 284 75
0.5 342 250 4.00
(0.1 324 185 9.00
0.2 194 60 0.5 254 450 0.1 254 500 8.00
96 0 0.:14 " 0.09 0.1.4.
8-86-74-01-3/4 220 162 <0.1 8.-85-80-06,07-3/4 ' 50 : 30 " 0.6 1-86-80-1041-3/4 60 26 t4.1 1-86-80-13-3/4 90 60 <0.1 1-86-81-04,05-1 230 52 0,
0.06 0.80 1.50 6.18 1.30 0.02 0.25 20.00 25.02 5.30
15.17 2.00 < 18.00 20.48 2.90 3.68 0.70 10.00 12.33 2.50
30.00 8.10 ' 1.00 2.75 1.00
0.08 0.28 20.00 22.70 4.60 0.01 0.14 4.00 5.98 4.80
0-86-81-1.0,11-3/4 240
0.32 H-86-82-07-3/4
62
40.1 188 0..24
REPORT: 016-2331 PROJECT: HONE `
PAGE 1
ELEHENT Cu; ,In , Al As Au-150 Anf1S4 Au AV TestYt. -1501t }1501t
UNITS PR PM PM! PPS RPA PPA PPA ,' gas gas gas
, . _
PROJECT: C-878 PAGE 1
SAKE EMBER
E1:EAEHT Cu Zn Al As ' Au Testi[t
UNITS ?PA PPA PPM PPA PPB 91
e Ba Geochemical Lab Report
Bodr-Clers t Coenvaar Lm.
764 Belfast Road Ottawa. Ontario Canada K1G 0Z5 Phone: (613) 237-3110 Tdec: 0534435
REPORT: 016-2335
34 0.4 185 280 10.00 40 0,4 326 120 10.00 240 0.4 334 65 3.50 58 0.3 368 70 ' 10.00 24 . 0.2 77 415 10.00
24 0.2 '` d7 . 135 8.00 46 0.4 196 220 6.00
108 0.3 ' 144 70 4.00 52 ; 0.4 193 65 10.00 64 . 0.4 312 150 10.00
51 0.2 226 30 3.0
106 0.6 464 45 3.00
116 0.6 1008 160 9.00
50 0.5 736 255 9.00
44 0.4 ` 512 110 8.00
0.4 856 110 6.00
0.5 740 95 7.50
0.4 ' 1040 390 5.00
0.6 1040 280 6.50
0.6 944 140 9.50
44 60 58 78 56
0.2 0.2 0.3 0.6
` 0.6
108 0.5 42 0.4 . 34 <0.1 ' 50 <0.1 64 0.8
36 <0.1 66 ' 0.4 ' 38 0.3 52 0.4 32 0.6
90 0.6 140 1.4 50. 0.6 48 0.8 44 <0.1
712 165 10.00 696, 135 10.00 528 140 10.00 880 170 10.00 592 165 10.00
608 105 10.00 920 145 4.00 344 265 3.00 832 1145 10.00 744 175 10.00
312 160 9.50 664 520 8.50 992 85 10.00 1112 235 10.00 369 115 5.50
648 50 6.00 544 65 10.00 504 175 2.50 364 225 8.50 688 95 8.00
H-86-90-01-3/4 H-16-90-014-3/4 H-86-90-02-3/4 H-86-91-01-3/4 N-86-91-02-3/4
95 102 95 83 40
H-86-91-03-3/4 32 H-86-92-01-314 80 H-86-92-02-3/4 82 H-8693-01-3/4 172 H-.86493-016-3/4 130
H-86-93-02-3/4 145 H-86-94-01-3/4 117 H-86-94-014-3/4 240 H-86-94-02-3/4 68 H-86-94-03-3/4 95
H-86-95-01-3/4 105 H-86-95-02-3/4 90 N-86-95-03-3/4 150 H-86-96-01-3/4 :160 H-86-96-01A-3/4 160
H-86.97-01-3/4 115 8-86-97=02-3/4 i'90 H-86-97-03-3/4 120 H-86-98-01-3/4 200 H-86-98-02-3/4 125
1-86-98-03-314 125 H-86-99-01-3/4 168 H-86-99-02-3/4 75 H-86-100-01-3/4 240 H-86-100-02-3/4 105
H-86-100-03-3/4 75 H-86-102-01-3/4 90 H-86-102-02-3/4 105 H-86-102-03-3/4 130 H-86-102-04-3/4 120
H-86-104-01-3/4 105 H-86-104-014-3/4 200 H-86-105-01-3/4 340 H-86-105-02-3/4 560 8-86-105-03-3/4 55
Boadswargi E Caa.pay Led. 764 BeUa. Rod om..a, Ontario
-Canada KIGOz5 Phone: (613)237-3110 Tebc: 0534455
LEGG Geochemical Lab Report
PROJECT: C-878 PAGE 2
SAMPLE ELEMENT NUMBER UNITS
Cu PPM
H-86-105-04-3/4 H-86-106-41.-3/4 11-84-104-01A-314 H-86-106-02-3f4 H-16-106-03-3/4
110 150 148 95 70
11-86-107-01-3/4 70 H-86-107-02-314 68 H-86-107-03-3/4 55 H-86-107-04-3/4 70 ". .H-86-107-. 05-314 '130
11-86-108=01A-3/4 164 H-86-109-01-3/4 140 11-116-109-02-3/4 130 H-86-109-03-3/4 90 H-86-110-01/02-3/4: 120
4.00 10.00 10.00 9.00
5T é.5 ' 316 8.00
386 310 528
58..;' 0.3 78 4.4 16 1.0 74 • 0.4•
600 : 1.2 104 0.6 .64 0.6 42 0.5 42 0.5
330.
370 145 632 180 664 105 212
8 (1670 0.03
240 5.04
1365 5.00
210 5.00
295 9.00
0.4 258 70 7.00 0.3 350 50 9.00 -0.2 248 185 6.00 0.4 334 1380 ` 9.00 0.4 480 90 7.00
".
H-86-110-08-3/4 140 76 0.4 238 60 10.00 8-86-111-41-3/4 ,106 112 0.4 496 100 6.00 11-86-1.11-02-. 3/4 77 56 0.2 1096 240 5.00 H-84-112-01-3/4 125 84 0.4 ' 320 110 8.00 H-86-112-02-3/4 290 104 0,5 ; 672 930 5.00
0.6 ':
4.3 _~"
10 0.6 44 0.4 52. 0.4
..
.- ` Zn , Al '• As Au Te3t#lt
PPM PPM PPM PPB It
° 308 340 3.00 ' 306 145 10.04
:356. 2045 5.00 168 250 5.00
H.-86-110-03-314 H-86-110-04-3/4 H-86-110-05-3/4 H-66-110-06-3/4 160 H-86-110-07-3/4 125
H-86-112-03-3/4 120 38 0.2 ` 352 1865 10.00 H-86-112-04-314 105 48 0.8 . 704 1305 10.00 H-86-112-05-3/4 168 84 1.0 1128 530 10.00 H-86-112-06-3/4 95 46 0.4 451 450 9.00 H-86-112-07-314 100 46 0.4 560 190 10.00
H-86-112-. 08-3/4 150 40 0.4 ` 728 490 10.00 H-86-112-09-3/4 75 64 0.3 ' 194 155 9.00 H-86-112-10-3/4 60 40 0,4 376 . 350 4.90 H-86-112-11-3/4 80 90 0.8 IS (145 0.07
REPORT: 445-2335 KKuJttT: C-diE F'HGE
Boadae-Geot& Capas Lid.
3420 Canotek Rd.. -.Ottawa, Ontario, Canada 1(1; 8X5 Phone: 1613{ 749-2220 Telex: 053-3233
Geochemical Lab Report
SaRPI E1EBERT Cu in Ag. as au+;50 Au AV ieStilt -1 Alt +,Ari;t
MU!4BEB UNITS PPB RP? PRA PPH RPM PPA PPR gis ÿe: gre.
N-26-103-0I-3f4 105 46 (4.1 420 0..29 6..93 2.00 3.tD ;.OY ÿ.~v
Rcar.OeU& °mow Lid.
5420 Canotek Rd., Ottawa, Ontario, Canada Kl./ 8X5 Phone: (613) 749.2220 Telex: 053-3233
.......NE)ARC!,LE: Qa-1 Geochemical Lab Report
2EP0ET: 016-2900
:PROECTI•:NONE - PAGE ,HUL, 4
SAMPLE ELEMENT Cu Zn A9 As Au lestWt NUMBER UNI78 PPN PPM PPM FPM PP8 sim
H26-113-01-3/4 147 45 <0.1 319 35 4.68 H96-113-04-3/4 117 22 <0.1 565 <15 3.48 H96-113-05-3/4 121 30 <0.1 84 15 7.74 H96-113-06-3/4 131 64 <0.1 250 20 10.00 H96-113-07-2/4 150 74 0.2 166 220 115.00
H96-113-08-3/4 100 32 0.2 179 145 10.00 H86-113-09-3/4 232 24 <0.1 167 115 10.00 H96-113-10-214 108 26 <0.1 51 20 10.00 H90 -113 -11 -2/4 46 26 <0.1 16 20 9.40 H96-113-12-314 176 56 <0.1 145 105 10.00
H96 -114 -02 -3/4 107 58 0.1 544 175 10.00 H96-114-03-3/4 92 36 <0.1 141 15 6.13 R96-714-04-3/4 157 68 0.1 164 160 3.73 -.96-114-05-2/4 29 30 <0.1 40 210 10.00 q96 -114 -06,07 -3/4 26 21 <0.1 72 20 10.00
i
H96-114-0E-3/4 67 24 <0.1 52 140 10.00 H96-114-09-3/4 116 30 0.2
39 170 4.26 H96-114-10-2/4 186 44 <0.1 5 163 10.00 H96-114-12-314 ' 99 24 0.2 22 <5 10.00 H96-114-12-3/4 246 40 <0.1 118 20 10.00
226 164 0.2 1300 345 10.00 H96-115-01.32-314
80 68 <0.1 37 40 10.00 -436-115-09-314 91 28 0.1 248 155 2.48
H3:1-115-10-314 83 55 <0.1 18 475 10.00 H36-116-01-3/4 169 120 <0.1 696 725 10.00
w7A3 -116702 -3/4 •.• • :102: ••• 72.•.• . • _0.1 ••• •••: .282 • • . .120 .10.00 •.
H3O -16-3 -511 7,• •
.136 • <0.1 ...230 • _170. 10,00
99 12 • 0.1. .87 110 10.00
-214 1:5 3o <0.1. E2 15 10.00
-11: -06 -3/4 121 .40 Q.1 157 15 10.00
-11O -07 -2/4 •xlv •• 34 <0.1. . .187 • • 15. 10.00 'A96-116-02-3/4 212 -26. <3.1 • -152 15 - 10.00 ,-,3'2. -116 -09 -3/4 71 .36. <0.1. .52 150 10.00 H3G -116 -10 -314 • 111 . 2 <C.: 52 0 • .550 - 4 .00 P06-113-11-314 .176 64 0.2 .. 520 240 10.00
n:.!2:2-116-12-311 136 GO 0.1 480 215 10.00 -:. 7:S-116-12-214 172 84 428 240 10.00
80 <0.1 .144 20 10.00 Fi96-11:i-1-2/4 131 50 <0.1 176 20 10.00 ':i3O-11G-17-2;4 270 88 <0.1 197 20 4.00
REPORT: 016-2900 K3HS 7ACE 2
SAMPLE ELEMENT Cu NUMBER UNITS PPM
%o PPM
A9 PPM
As PPM
Au TestUt
PPB gm
H96_117-01~3/4 ` ~ ~- 155 68 0.2472 215 ''.lO.00 H96-117-02-2/4 l40 40 <O.l ~IS'
-_335 10.00 n96_11/-03-3/4 123 42 <0.1 95 210 10.00
H96-117-04-3/4 103 28 <0.1 29 315 1800 H96 -11S 97 40 (0.1 384 . 185 10.00
H96-118-02-3/4 71 ` 30 0.1 240 ~~ ~-1075~ 8^00 K96-110-03_3/4 ' ~l3 16 <0.1 27 20'
10.00
n96-118-04_3/4 , 8 12 <O.l 8 65 10.00 H96-118-05-2/4 39 . 16 0L1 12^ '45 10.00 496-118-06-3/4 79 32 0.1 151 35 10.00
H96_1I8~07-3/4 ''' 82 28 <O.I 146 ` '195 ' '10.0O H96_118-08-3/4 99 46
' 0.4 134 160 10.00
H96_118_09-3/4 151 ' 42 0.3 292 390 .lû.OV H96-1I2-I0-3/4 ' ' '' 120 40 0.1 272 10 10.00
H96-118-12-3/4'_ 177 88 0.4 912 30 10.00 i 238 190 0.4 632 70`
10.00 H96-118-14-3/4~~ , ~ 189 156 0.6 712 165 10.00
'' 179 l6O 0.5 , 848 220 10.00 H86-118-16-3/4 180 164 0.3 496 85 10.00
896-118-17-374 237 148 0.2 648 450 13.00 H96-10-18-3/4 257 176 1.1 1216 15 0.00 S96-I19-01-2/4
` 246 120 0.2 248 15 10.00
h%-ll3-02 -3/4 97 26 (O.l 252 170 I0.00 H96-119-03-3/4 131 28 0.1 226 50 10.00
K96-1I9-84-2/4 1I9 30 <0.1 '276 ~' - 30~ ' 10.00 H96-119-05_3/4 93 31 0.2 386 80 IMO H96'I19-86-3/4 72 19 <C,I 162 85 10.00 6:7'6-119-07-27; 17.7 20 (0.I '09 1:0 10.00 ~S6-I2V'8l-3/4 123 36 >2000 65 10.33
iT-:6-120-02-2/4 32 26 <0.1 20 10 10.00 H96-120-03-3/4 126 520 O.A 276 30 10..00 H36-120-05-514 ~ 15 <0.1 22 35 l0.00
~9 13 <0.1 74 45 10.00 H36-1L-07-3/4
R's16-lZ:j-OC-3/4 87 32 0.3 7S 30 1C .00 H'3ü-120-09-2/4 32:9 Ic.)G 2 448 40 }0.00 E96-121-0I-3/4 64 ~.2 >2C00 lO5
10 CO
142 46 O.5 10.00 32 38 1)'4 75 10.0
olaus*=-Oeggmmwawaw'Lad.
5420 Canotek Rd., Ottawa, Ontario, Canada 8x5 Phone: 16131 749-2220 Telex: 053-3233
Geochemical Lab Report
Geochemical Lab Report
Booder-Oesi& Casp..y Lid.
5420 Canotek Rd., Ottawa, Ontario, Canada K1J 8X5 Phone: (613) 749-2220 Telex: 053-3233
REPORT: 016-2940 PRi~J'ECT+ ONE PAGE 3
;AMPLE ELEMENT NUMBER ; UNITS
Cu PP.'•i
Zn PPM
A9 PPM
As ?PM
Au PPE
SestW3Y
r:96-122-04-314 89 16 < 0,2 24 65 10.00 496'121-45-3f4 72 48 0.2 194 350 10.00 ;i96-1.21-06-314 237 156 0.2 316 85 10.00 H96-121-07-3/4 293 200 0.2 354 25 10.00 H96-121-08-314 359 360 0.6 464 . 50 10.04
E496-121-09-314 274 146 0..4 252 20 10.00 H96-121-10-314 205 104 0.4 304 20 10.40 a16.-1W.~-01-314 115 72 0.2 151 35 10.0v
Basider-asu & Conway led.
3420 Canotek Rd., Ottawa, 'Ontario, Canada K13 8X5 Phone: (613) 749-2220 Telex: 053-3233
Geochenncal Lab Report
REPORT: 016-2899 PRCJECT: NONE PAGE 1
SAMPLE ELEMENT NUMBER UNITS
Cu PPM
Zr!
PPM A9
PPM Au-150.
PPM A11+150
PPM Au .AV PPM
?esiWt 9ms
-150N1 9>Hs
+i5014t ç-4s
As- PPM
H86-113-02,03-3;4 H86-114-11-314 H86-115-03,04-314 H86-115-05,06-314 ii86-115-07-3,` 4
96 74 30 24 16
25 26 24 19 16
<0.1 <0.1 <0.1 <0.1 <0.1
0.64 0.41 0.08 0.27 0.16
262.00 :4.71 1i6.p5 28.76 0.10
3.52 1,09 0.81 0.88 0,1:6
14.00 14.00 20.00 18.00 ,V 15.00
16.18 18.17 22.37 2 r. Ÿi'v' s Sr..61
0.18 0.14 0.14 ..45 0.40
133 105 40 ., .L
H86-115-08-314 H86-=19-15-3i4 • .4 ~L~Ü~iiitJ~iF.~i-31~ ~
56
ilŸ ~ 210
22 52 LJ
0.1 <0.1 (~ ~.1/.1~
0.48 0.13 0.2~~
519.33 0.13
..24,,..63
3.16 . ~ 4 ..13 ~.~2
18.00 âJ.ry~V} ~ 1i„00
23.15 ' ~? ,: 9 15.69
0.12 ~ 0.7c
°J,iL
27 .2c, ,aÿY-.
Geochemical Lab Report
Boadar-Ckerg • Company La.
5420 Canotek Rd., Ottawa, Ontario, Canada KIJ 8X5 Phone: (613) 749-2220 Telex: 053-3231'
PROJECT: NONE PAGE 1
hb6-.64-07-3/4 ;-?S6-122-06-,/4 H26-122-09-3/4 H86-122-10-3/4 1486-123-01-3/4
H86-623-02-3/4 H86-124-02-3/4 H26-124-62-3/4 1426-124-03-3/4 H86-124-04-3/4
H86-124-05-314 1486-124-06-2/4 H86-124-07-3/4 ' H86-124-08-3/4 H86-124-09-2'4
. H86-124-16-214 i#8:7-124-17-214
53 160 220 250 420
21 112 202 40 38
270 35 112 34
80 37 1450 32 160 22
.90 66 60 20 60 37 116 24 176 28
.t,(r 56 148 90 164 78 210 156 112 146
• 370 114 . . ûG • 84
0.2 64 10 8.00 0.2 204 105 10.00 0.5, 360 30 10.00 1,2 600 70 10.00 0.2 220 45 6.00
0.5 1408 120 1.00 0.4 736 60 10.00 <0.1 204 30 10.00
0.2 113 25 4.00
0.2 97 45 . 6.00
0.1, 24 535 3.00
t0.1 10 20 9.00
0.1 33 60 3.00
0.3 27 <15 - 3.00
0.2 552 5 5.00
0.6 624 515 7.00 0.4 142 90 5..00 0.5 642 340 8.00 0.5 600 70 2.00
. 0.6 181 210 6.00 . ... ... , . ~.
0.3 • 164 20 • 7..00 i0.1 - 664" • • • 100 • 5.00
- SAMPLE ELEMENT Cu Zn NU .... UNITS PPM PP4
Ag As Au Tes ti#t
PPM ?Ph P?8
300 9.00
40 8,00 40 10.00
20 10.00
30 7.00
91
1486-122-02-3j4 ii,56-122-03-3i4 É181:-1.22-04-3%4 H36-:.22-05-3/4
R -4 6-lf.~. ?;6-3;'Ÿ
50. 0.^,`
50 <0.1
70 . 0.3
50 0.1 48 16 C0.1
317 152 188 386 39
REP2âi; 0i6-2932
Yordv-astre t Lanum7 Lad.
5420 Canotek Kd., Ottawa, Ontario, Canada Kll 8X3 Phone: 1613) 749-2220 Telex: 053-3233
Geochemuai Lab Report
REPORT: 016-2933
PROJECT: NONE PAtt 1
SAMPLE ELEMENT Cu Zn A3 As Au-150 Au+150 Au AV TestWt -1501it NUMRER LIMITS PPM PPM PPti PPM PPM PPii. PPM gms 9es sas
N86-124-11- /4 . 80 44 0.2 156 0.09 5,68 . 5.66 5.04 7.90 0,85
84.0 rOeg,&CeatepyLed.
5420 Canotek Rd., Ottawa, Ontario, Canada KIJ 8X5 Phone: 16131 749-2220 Telex: 053-3233
^Ft1A7"• PROJECT: NUS
Geocbemical Lab Report
: MPH CONSULTING LTD. ATTN: P. ROLLINCON 2406 - 120 ADELAIDE ST. WEST TORONTO. ONT. 81.15H }I1
kA CCRT. 0 : A':61517:-001-A I1IVOICE t : 170115125 DATE 1•3UL-36 P.O. t : WINE
Ni
f -)ro - 50 Sr If .. D . ➢ . .,. pV ope PP yel er •J Pe" Wm yet ot=
128 0.01 18 0.17
129 <0.01 15 0.02 l (0.01 11 <0.01 14 0.02 15 0.01 <I <0.0! 59 0.012
<D.O1 30 0.03 7 <0.01 31 0.04 48 0.02 45 0.04 444 0.02 69 0.21 10 0.02 72 0.06 1- <0.01 14 (0.01 4: '9.01 15 0.01 7 60.01 14 <0.01 69 0.0! 290 '0.01 115 <0.01 115 <0.01 262 <0.01 48 0.17
<10 <10 <10 <10 61) <10 CIO <10 <10 <10 <10 <10 <10 C10 <10 :.10 .1J <10 :10 :10 610 <10 <10 <10 <10 C10 610 .10 '.1')
1: :) [10 <10 <l0 <10 <10 <10 10
:1:' ;1: ") Cl•; <l0 <10
<10 ,,1.> <10 :I: 0 20
:IC
} !• ,: <1@
1] :10 :IO :14
20 'p; i2 41 10
52 :1 ,; 40
t] <1: ,2
55 C1•) 42 77 <10 69
119 <10 62 40 C10 58 42 <10 02 24 <10 5: 14 <11 56 41 <10 48 0 <10 3
108 <10 38
:14 54 15 ".' 'C 20 616 42 26 C1{' 72 57 n) 52 40 <10 80
1 :1: 11•: 92 :1 74
3° 92 1? 6b 34 5 ;1, 256 1 ;1 34
:)
'-5 :0 22 ;1..52 46 <1 70
74 :1 130
8 (10 8 (10 10 c10 6 S10 6 40 6 40 2 10 4 00 6 10 6 610 4 <10 8 <10 6 (10 6 (10 12 :10
:1C 16 :IO 14 <10 2 10 4 (10
6 10 6 10 4 61(' ▪ 50 6 <14 62 10 10 '.0 16 19 1: <10 12 <10
126 10
Chemex Labs Ltd. .AnNYrle.l Chemists •G.odamba •Re9iamM Ategara
212 Brooktbank Ave. North Vancouver. B.C. Canada Vii 2C1
Teleonma:48041 9844221 TNp.. 043.52597
Semi uuantitat:ve a..!41 elemen; OCT
i4iLric-Aqua-Re?ia di3e tio,. of C.7 material f:lIc.+ed .]1.403tion t> incomplete far .r.ar. mi:.er~la values reported for Al, 0f. Da. De. _a. Oa. La. M•3. 16, Ha. Sr. T1. Ti. W and V car. only be considered as semi-qu.9ntit.7::-:e.
COMMC'r4T5 : ATTN• P. 1O12.1150r1
CtBT 6r iCATC Or :.NGLYC IC I
0.01 0.13 0.06 0.05 0.06 0.11 0.04 0.11 0.0: 0.03 0.10 0.05 0.05 0.03 0.02 0:03 0.02 0.02 0.04 0.05 0.0: 0.05 0.09 0.07 0.03 0.07 0.01 0.01 0.03 0.02 0.04 0.04
mole ..1aiC2.tpt:we
H-86-01-248 µ-86-02-141 ' -:6-06-i38 "16-09-100 •-26-15-028 1-96-16-023 +-96-r.-031 H-86-25-NI 4-16-29-03! :i-5-35-169 '-36-36-061 4-86-37-021 •1-96-43-021 '-96-44-011
96-46-021 .-36-48-0 1 -6-50-0.0 •-86-52-021 +-36-59-041 :-86-75-101 4-96-76-120 -â~•-•~.06q 1-06-70-090 '4-06-79-068 `1-36-10-148 4-06-91-201 36-93-090
4-C6-91-101 :_.,. :?0..)21
H-96-91-041 4-26-91-051 H-86-100-041
Au pptr A1 f:4a6 -
c5 0.51 0.2 <5 1.12 0.2
0.2 <5 0.40 0.2 50 1.11 0.2 <5 1.19 0.6 45 2.96 0.2 C5 1.97 0.2 :5 2.47 0.2 <5 4.04 0.2 3 0.50 0.2 (5 1.67 0.2 •3 0.53 0.2 <5 1.63 0.2 3 2.26 0.: :5 0.50 0.'
1.10 0.2 C5 1.61 0.2 <5 2.01 0.2 cs 2.08 0.2 :5 0.38 0.2 65 3.35 5.2 :`, 0.43 0.2 C5 0.47 0.2 <5 0.11 0.2 5 0.29 0.2 65 0.03 0.2
:5 -.~ 0.- :5 1.96 0.2 'S 1.66 0.2 <5 2.62 1.4
10 30 5.5 C 3.59 <0.5 14 44 26 2.97 10 10 (0.5 C 0.61 <0.5 15 5/ 32 2.53 10 40 00.5 02 2.07 (0.5 9 31 15 2.08 10 10 <0.5 C. 0.68 (0.5 8 27 20 1.22
760 610 <0.5 .2 5.52 (0.5 0. 99 92 6.02 50 (10 (0.5 C 4.67 (0.5 31 76 89 7.21 <10 <10 (0.5 C 5.14 <0.5 27 115 76 6.12 <10 20 <0.5 (2 3.68 <0.5 16 47 4S 5.31 :10 10 <0.5 <2 6.27 0.5 30 187 42 9.81 630 30 <0.5 02 1.44 (0.5 14 43 :7 7.44 30 :0 <0.5 <2 3.72 <0.5 I? 23 40 5.41
(10 â (0.5 C 2.99 <0.5 15 46 33 3.42 (10 10 (0.5 (2 2.67 <0.5 6 31 4 2.06 410 20 <0.5 C. 2.80 (0.5 19 134 29 2.35 :10 10 60.5 : 1.01 <0.5 22 Ell 51 4.20 10 30 66.5 02 1.39 5.5 7 45 16 6.71 :0 60 <0.5 .2 3.02 <0.5 14 60 39 3.45 10 50 <0.5 C 1.64 <0.5 18 80 44 3.10 <10 (10 <0.5 <2 3.2, <0.5 107 43 4.24 C10 30 <0.5 C2 1.16 <0.5 • 125 43 32.81 10 20 <0.5 02 0M 5.5 - 36 5 4.I2 44 10 60.5 C2 4.90 <0.5 61 27 47 7.67 10 10 :0.5 4.5i <0.5 21 20 32 6.02 10 10 (0.5 .^. 1.74 (0.5 17 38 43 3.09
230 70 <0.5 <2 1.09 <0.5 44 56 87 6.75 <10 10 <0.5 <2 1.53 <0.5 1 29 7 1.13 30 10 <0.5 <2 1.19 :0.5 3 58 10 19.01 10 50 60.5 5 3.3? <0.5 19 79 42 3.55 10 .4 :0. 1.70 03.5 21 122 41 3.90 10 40 (0.5 C 1.66 5.5 30 111 41 3.48 10 30 <0.5 <2 2.21 <0.5 20 120 44 3.95 60 300 <0.5 <2 1.54 <0.5 17 127 80 1.16
64 R Li NI on 110 PP PP pp
10 0.10 CIO 1.16 472 1 10 0.04 20 0.67 32? 3
<10 0.12 20 0.70 3E1 61 (10 0.04 ::0 0.26 :'i 1 10 0.03 :10 2.16 989 1 10 0.03 <10 2.88 1009 <1 20 0.02 <10 1.00 1600 a 10 0.00 <10 • 632 1434 1 20 0.03 610 1.51 244E 1 <10 0.15 10 1.02 050 1 10 0.08 (10 1.11 1740 1 10 0.07 <10 1.36 732 Cl
<10 0.04 <10 0.95 214 (I 10 0.04 C10 1.35 486 <1 20 0.04 1) 1.59 1217 <10 0.09 10 0.33 414 1 10 0.15 10 1.11 430 1 10 0.10 20 1.12 348 1 10 0.03 <l0 2.20 542 C1 10 0.13 20 1.92 783 2
:10 0.21 1) 0.3E Y6 1 10 0.03 <10 1.63 •wc 1 10 0.05 :14 1.6' 1475 .1 <I0 0.05 <10 0.67 964 2 <10 0.01 (10 0.38 503 2 <10 0.05 10 0.34 367 <1 10 0.01 0.52 555 <1 10 0.20 610 1.47 591 5 10 0.11 20 1.44 570 1 10 0.09 :0 1.32 496 1 10 0.06 20 1.E9 55 (1 10 0.17 20 0.87 679 3
47 640 54 470 20 520 17 320 58 260 41 310 41 310 47 430
103 310 r 600 35 810 31 580 10 360 40 420 63 400 24 550 51 590 52 580 59 450 09 870 3 240
92 894 16 550 24 380
113 r..0 3 351• 9 700 49 580 56 650 52 610 56 610 73 730
Aq As Oa l.. Oi La Ed Ca Cr tu E. Ps PP PP PP PP ' PP pr PP OP =
Cerr.tfie•! by
ACME ANALYTICAL
DATE RECEIVED:
LABORATORIES LTD. 852 E.HASTINGS ST.VANCOUVER B.C. V6A 1R6 PHONE 253-3158
GEOCHEM I CAL ANABLYS I S
.500 6RAM SAMPLE IS D16ESTED WITH 3Ml 3-1-2 HCL-HNO3-H20 AT 95 DE6. C FOR ONE HOUR AND IS DILUTED TO 10 Ml WITH MATER. THIS LEACH IS PARTIAL FOR MN.FE.CA.P.CA.M6.BA.TI.B.AI.NA.K.W.SI.2R.CE.SN.Y.ND AND TA. AU DETECTION LIMIT IT ICP IS 3 PPM. - SAMPLE TYPE: CRUSHED AUIt ANALYSIS BY FA+AA FROM
/1 66RAM SAMPLE.
/~ j~~ JULY 23 1986 DATE REPORT MAILED: z6/ AESAYER. /C:C .DEAN TOYE. CERTIFIED
DATA LINE 251-1011
B.C. ASSAYER.
MPH CONSULTING PROJECT -- C-878 FILE # 86-1609 PAGE 1
SAMPLED Mo Cu Pb 211 Ag Ni Co Mn Fe As U Au Th Sr Cd Sb Bi V Ca P la Cr Mg Be Ii B AI Na K N Ault PPM PPM PPM PPM PPM PPM PPM PPM t PPM PPM PPM PPM PPM PPM PPM PPM PPM 1 1 PPM PPM 1 PPM 1 PPM 1 1 I PPM PPB
H-86 02-08 I 3 2 51 .1 14 7 498 2.03 4 16 ND 4 128 2 2 9 3.63 .046 15 4 .85 69 .01 5 .55 .12 .21 1 1 H-86 04-16 74 70 5 89 .2 47 12 1220 6.53 4 14 MD 1 50 2 4 21 2.92 .068 4 320 1.06 24 .01 2 .47 .12 .06 I 1 N-86 05-05 1 39 5 63 .1 19 10 700 3.68 2 5 ND 1 76 2 2 24 5.35 .070 4 3 .82 42 .01 3 .76 .26 .13 1 1 H-86 07-07 1 42 6 95 .2 20 12 1011 4.28 2 7 ND I 64 2 2 37 6.19 .090 2 3 1.21 17 .01 2 .39 .16 .06 I 1 H-86 09-IS 2 24 8 43 .1 31 11 804 11.63 26 5 ND 2 53 2 4 11 1.41 .063 5 7 .95 63 .01 2 .52 .08 .24 1 I
H-86 10-04 3 9 15 71 .3 15 5 932 12.85 16 12 ND I 91 2 2 7 6.89 .043 2 3 1.21 32 .01 2 .22 .09 .09 I 1 H-86 11-09 2 45 6 84 .2 47 20 2912 6.43 140 5 ND 1 32 3 2 12 5.55 .029 2 4 .83 22 .01 2 .69 .28 .00 1 1 H-86 12-09 I 44 9 74 .3 58 21 2042 8.10 4 5 ND 1 74 2 2 73 9.47 .033 2 108 1.74 16 .01 2 3.58 .13 .05 1 1 N-86 13-10 I 99 7 115 .3 59 27 1774 7.14 5 5 ND I 46 2 2 143 9.69 .024 2 127 2.69 26 .01 2 3.72 .10 .05 3 I 8-86 14-02 3 100 Il 104 .4 47 34 3159 10.79 13 5 ND 1 29 2 2 126 9.01 .018 3 41 2.02 7 .01 2 2.41 .14 .02 1 4
H-86 17-03 1 115 8 96 .3 60 31 1140 7.86 4 5 ND l 38 2 2 213 6.44 .023 2 146 3.23 18 .02 2 3.94 .09 .01 1 1 11-86 18-06 1 39 8 65 .3 51 16 700 3.24 50 5 NO S 99 20 2 18 2.85 .056 13 12 1.14 46 .01 3 .81 .15 .13 1 4 11-86 19-03 2 46 8 79 .5 500 56 1537 6.42 74 13 ND 1 53 12 4 104 7.01 .026 2 1024 8.30 3 .01 2 4.08 .07 .02 2 I H-86 20-03 1 145 10 103 .2 116 39 1588 5.91 2 7 ND 1 111 2 2 171 7.24 .020 2 234 2.69 45 .01 2 3.49 .14 .02 1 I H-86 21-06 2 95 9 99 .3 98 33 2024 9.15 31 5 MD 1 45 2 2 159 7.16 .022 2 195 3.22 24 .01 2 4.33 .09 .02 I I
H-86 23-04 I 55 4 66 .1 59 14 590 4.31 35 5 NO 1 39 27 2 36 3.71 .044 4 33 2.00 22 .02 2 1.98 .18 .09 1 1 N-86 24-01 5 83 8 140 .3 110 407 1143 7.81 59 7 ND 1 27 26 3 145 6.18 .033 2 124 3.88 6 .01 2 2.93 .15 .02 640 3 H-86 26-02 I 113 9 76 .3 139 34 1106 6.96 4 5 ND 1 19 2 2 164 5.99 .012 2 231 4.79 6 .02 2 4.51 .09 .01 4 1 H-86 27-04 1 131 11 86 .3 108 46 1253 6.91 4 5 ND I 17 2 2 213 6.23 .019 2 232 3.60 2 .03 2 4.07 .11 .01 94 2 H-86 28-02 I 70 4 77 .3 76 28 2410 7.32 36 5 ND 1 34 2 2 94 8.64 .014 2 79 2.74 9 .01 2 1.90 .20 .03 1 4
H-86 30-03 1 13 17 . 18 .2 13 8 518 23.11 5 5 ND 2 41 2 4 21 .51 .126 2 12 .86 24 .03 2 .35 .05 .05 30 1 H-86 31-01 I 78 13 113 .2 97 33 661 5.70 67 5 MD 3 53 4 2 55 .94 .053 9 69 1.15 51 .01 4 2.44 .10 .23 1 2 H-86 32-01 1 t0 15 24 .1 13 6 524 21.40 16 S ND 2 II 4 3 14 .23 .030 2 1 .42 14 .01 2 .18 .04 .06 22 1 H-86 33-05 3 27 23 78 .2 61 18 1641 9.49 51 14 ND 2 110 6 5 IS 3.12 .035 1 9 1.20 33 .01 3 .69 .17 .15 1 3 H-86 34-03 1 15 17 21 .1 15 6 787 21.21 9 5 ND 3 73 2 2 19 .71 .083 2 9 .67 25 .04 2 .21 .06 .11 11 1
11-86 38-03 1 38 2 55. .1 36 13 744 4.22 5 5 ND I 39 2 2 25 4.25 .051 I 17 .98 34 .01 2 1.24 .20 .17 1 1 H-86 39-07 1 10 11 42 .1 14 6 1087 19.80 34 5 ND 2 10 2 4 11 .28 .040 2 6 .95 10 .01 2 .53 AS .05 9 1 H-86 40-03 1 61 7 79 .3 52 23 981 4.93 7 5 ND I 62 2 2 55 7.01 .071 5 25 1.32 36 .01 2 1.80 .23 .13 I 1 H-86 41-01 1 13 3 60 .1 8 6 630 2.63 2 5 ND 1 29 2 2 8 3.00 .036 6 2 .52 24 .01 2 .56 .17 .07 4 1 H-86 43-04 I 106 6 84 .2 178 37 1138 5.27 3 5 ND 1 31 2 3 75 7.59 .041 2 121 1.75 14 .01 2 1.45 .23 .06 2 2
H-86 45-06 7 30 4 62 .3 25 9 597 3.51 4 18 ND I 37 2 2 23 4.00 .058 13 45 1.26 23 .01 4 1.20 .14 .09 3 1 N-86 47-02 I 37 2 67 .1 80 17 993 4.15 2 5 ND I 10 2 3 46 10.05 .040 4 66 1.60 19 .01 6 2.52 .18 .11 2 I H-86 49-03 1 67 12 89 .3 179 23 1175 4.67 8 13 ND 2 284 2 2 52 5.40 .041 9 218 2.44 36 .01 2 2.58 .09 .13 3 1 H-86 SI-02 1 42 6 60 .2 94 18 585 3.97 11 12 ND 4 70 2 2 52 2.35 .056 25 114 1.51 62 .20 3 2.04 .11 .26 2 3 H-86 53-05 1 58 16 77 .1 74 17 581 3.79 18 5 ND 4 138 9 2 43 1.65 .061 16 90 1.63 84 .01 4 1.96 .13 .21 1 3
H-86 54-03 1 53 17 89 .2 105 21 496 4.69 14 11 ND 5 116 5 2 43 1.74 .065 18 84 1.85 59 .01 3 2.39 .07 .18 3 2 SID C/rA-AU 21 61 4! 141 7.0 72 79 1147 3.97 41 16 1 35 49 19 17 21 70 .48 .109 37 59 .89 184 .08 35 1.73 .09 .13 14 52
MPH CONSUL CONSULTING i.i,1 L L i . L--N 7» F 1 L.[ # 96--1609 FAGF.. _-
SAMPLEI Mo Cu Pb In Aq Ni Cc Mn Fe As U Au 1h Sr Cd Sb Ai V Ca P la Cr Mg Pa Ti D AI Na F N Aull PPM PPM PPM PPM PPM PPM PPM PPM . PPM PPM PPM PPM PPM PPM PPM PPM PPM 1 1 PPM PPM 1 PPM 1 PPM 1 1 1 PPM PPM
H-86 55-06 27 15 5 38 .1 34 8 395 3.31 5 5 ND 2 13 1 4 5 IS .95 .040 1 141 .73 23 .09 4 1.23 .12 .04 3 2 H-86 56-06 1 50 2 75 .1 148 28 816 5.16 2 5 ND I 19 1 2 2 63 .80 .031 3 196 3.26 7 .26 5 2.89 .07 .01 1 1 14-86 57-11 1 32 8 62 .3 24 9 1725 5.98 61 II ND 2 78 I 2 3 14 11.08 .056 8 1 2.95 15 .01 4 .22 .13 .04 1 3 H-86 58-03 1 85 10 122 .1 105 49 2323 6.09 39 7 ND I 40 1 2 2 59 9.22 .048 5 22 1.48 13 .01 4 .41 .19 .05 1 2 H-86 60-02 1 30 2 130 .2 60 IS 2164 8.60 12 10 ND I 20 1 2 2 51 4.02 .084 6 52 1.10 6 .01 3 1.88 .12 .04 1 1
H-B6 61-03 I 54 6 112 .2 20 7 1811 5.24 13 11 ND 2 33 1 2 3 29 6.58 .054 7 5 1.37 12 .01 4 .87 .18 .07 2 1 H-B6 62-02 1 42 3 79 .2 51 24 1967 5.11 11 1 ND 1 41 I 2 2 59 7.19 .047 9 23 1.08 7 .01 3 1.88 .17 .04 1 1 14-86 63-01 I 46 6 77 .3 33 18 3360 B.76 7 lI ND 1 63 I 2 2 29 5.12 .068 10 2 1.69 25 .01 5 .37 .16 .08 1 1 H-86 64-03 1 30 6 115 .2 74 23 1140 5.94 5 14 ND 1• 153 1 2 . 2 49 7.10 .156 12 45 1.43 46 .01 3 2.49 .08 .21 2 I 8-86 65-02 1 20 6 41 .2 62 19 1204 5.92 3 9 ND 2 66 1 2 2 44 1.37 .107 11 26 1.34 37 .01 5 .58 .20 .10 1 I
H-86 66-04 1 45 12 172 .2 23 35 2237 10.56 17 II ND 1 72 1 2 2 21 4.07 .093 9 10 1.54 21 .01 2 .41 .11 .07 I 2 H-86 66-04A 1 54 14 147 .3 17 34 2179 10.08 18 II ND 2 11 I 2 2 22 4.78 .092 12 1 1.47 23 .01 4 .47 .20 .07 I 2 H-86 67-02 1 44 7 77 .1 53 20 997 5.68 3 10 ND 1 55 I 2 2 63 6.06 .102 • 13 36 1.72 83 .01 4 .89 .17 .05 1 1 H-86 68-02 1 48 4 81 .3 53 16 792 3.92 17 7 ND 3 121 1 2 2 26 2.66 .054 15 40 1.62 37 .01 4 1.63 .11 .12 1 2 N-86 69-02 1 43 11 134 .2 87 18 571 4.95 21 9 ND 7 61 1 3 2 33 .90 .057 23 57 1.46 46 .01 6 2.15 .05 .15 1 2
H-86 70-02 1 62 9 68 .1 88 16 1015 4.20 21 19 NO 3 384 1 6 2 19 6.20 .051 15 73 2.40 39 .01 6 1.05 .08 .14 1 I H-86 71-03 4 52 15 89 .3 85 18 502 4.42 10 10 ND 7 150 1 2 2 32 1.65 .057 22 72 1.73 41 .01 4 1.98 .07 .14 I 1 H-86 72-07 1 31 8 20 .2 40 10 728 3.39 40 16 ND 8 368 1 4 2 8 4.38 .086 16 12 1.78 31 .01 4 .33 .09 .11 1 26 H-86 14-04 1 50 6 56 .1 52 19 824 6.32 74 12 ND 2 146 1 2 5 11 3.06 .040 12 6 .90 35 .01 7 .53 .07 .19 1 1 H-86 83-01 I 36 5 71 .1 47 17 658 10.51 6 5 ND 3 68 1 -2 2 10 .85 .054 18 5 .80 41 .01 4 .39 .06 .18 1 1
H-86 83-02 I 37 10 68 .1 48 17 656 10.31 4 9 ND 3 68 I 2 2 10 .89 .050 18 6 .74 41 .01 5 .19 .06 .18 1 1 H-86 85-03 I 46 22 41 .1 16 7 594 18.59 0 5 ND 2 63 1 2 2 6 .74 .071 32 2 .64 18 .01 8 .19 .05 .11 1 1 H-86 86-06 I 43 26 303 .2 50 14 629 2.72 7 IS ND 4 209 1 2 2 1 4.59 .056 11 9 1.28 16 .01. 6 .39 .06 .20 1 21 H-86 87-07 2 14 10 38 .1 17 4 1396 13.97 3 12 ND 2 255 1 2 2 30 6.04 .052 22 18 2.01 6 .01 3 2.56 .07 .02 1 1 8-86 88-03 1 31 lI 78 .3 47 13 531 3.31 9 Il ND 4 169 1 5 2 30 2.44 .055 17 69 1.61 33 .01 4 1.24 .10 .08 1 3
H-86 90-03 1 46 11 78 .1 73 IS 650 3.75 8 10 ND 6 263 I 2 2 21 2.54 .058 22 47 1.58 53 .01 5 1.51 .07 .18 1 2 H-86 91-05 1 48 14 64 .1 61 17 633 4.16 12 5 ND 6 106 1 2 2 34 1.50 .058 16 140 1.48 46 .01 4 1.93 .09 .11 1 1 H-86 92-03 1 44 10 79 .1 61 15 563 4.25 17 9 ND S 150 1 2 2 15 1.37 .063 19 40 1.29 4B .01 5 1.01 .07 .15 1 1 H-86 93-03 1 32 7' 38 .1 59 14 745 3.16 10 15 ND 4 179 1 2 2 16 2.60 .055 17 55 1.33 44 .01 4 1.19 .08 .17 2 1 11-86 94-04 1 37 9 66 .1 51 13 691 3.34 12 11 ND 4 295 1 6 2 18 2.85 .049 18 30 1.54 43 .01 5 1.27 .08 .14 1 2
H-86 95-04 1 51 10 04 .1 84 18 642 3.74 21 12 ND 6 221 1 2 2 21 2.61 .065 23 61 1.55 44 .01 4 1.53 .07 .16 1 I 14-86 96-02 I 51 10 69 .1 72 17 544 3.85 6 5 ND 4 125 1 2 2 35 1.67 .063 16 97 1.74 61 .01 3 2.05 .09 .12 1 . 1 N-86 91-04 1 38 II 67 .1 56 14 532 I.32 10 16 ND 4 149 I 4 2 23 2.34 .052 16 58 1.50 45 .01 3 1.37 .09 .12 1 I 14-86 98-04 1 59 14 75 .1 62 15 642 3.80 16 15 ND 4 329 I 4 2 18 2.94 .052 IS 45 1.49 47 .01 5 1.31 .08 .17 1 1 H-86 99-03 1 40 8 55 .1 62 15 729 4.08 10 16 ND 5 334 1 3 4 19 3.42 .068 22 42 1.50 57 .01 5 1.24 .08 .20 l 1
H-86 101-01 1 49 10 80 .3 66 17 485 3.98 21 9 ND 6 109 1 2 2 35 1.14 .064 22 77 1.69 46 .01 3 1.93 .08 .12 1 I SID ClFA AU 21 60 36 139 7.0 71 29 1127 3.95 42 20 7 34 49 10 15 19 69 .48 .105 36 57 .88 185 .08 35 1.73 .08 .13 13 52
SAMPLED Mo PPM
Cu PPM
Pb PPM
!n
PPM Fig
PPM Ni
PPM Co
PPM Mn
PPM
MPH CONSULTING
Fe As U Au 2 PPM PPM PPM
PROJECT
Tb Sr Cd PPM PPM PPM
- C-878
Sb Bi
PPM PPM
FILE
V Ca
PPM 2
It 86-1609
P La Cr
2 PPM PPM Mo
2 Ba
PPM li 2
B
PPM AI 2
Na I
C I
PAGE
N Hull
PPM PHI
H-86 102-OS 2 41 8 71 .1. 59 U 895 4.11 18 5 ND 5 140 1 7 2 23 3.96 .054 ID 63 1.86 2° .01 5 1.52 .0? .12 2 2 H-86 103-02 1 41 4 61 .1 95 21 1398 4.97 21 5 ND 1 64 1 2 2 29 5.62 .034 0 40 2.12 30 .01 3 1.63 .18 .07 1 1 H-86 104-02 2 44 5 74 .1 55 16 599 3.52 31 5 ND 3 115 I 2 2 17 3.29 .04? 12 17 1.20 38 .01 5 1.18 .12 .14 1 1 H-86 105-05 2 49 4 84 .1 78 11 749 4.65 41 5 ND 5 89 1 2 2 26 3.75 .060 18 42 1.92 34 .01 3 1.85 .12 .15 1 1 H-86 106-04 1 48 IO 90 .1 55 17 621 4.00 IS 5 ND 3 75 I 2 2 27 2.49 .051 14 42 1.42 36 .01 5 1.62 .10 .14 2 2
H-86 107-06 2 48 13 79 .1 79 18 691 4.43 9 5 ND 6 134 l 2 2 35 2.30 .060 26 63 1.94 40 .01 5 2.09 .07 .16 1 1 H-86 108-01 2 61 7 103 .1 102 23 443 4.40 23 5 ND 7 150 1 2 2 31 1.38 .068 25 15 1.82 46 .01 4 2.05 .07 .17 2 I H-86 109-04 1 51 10 BI .1 76 19 624 4.48 2 5 ND 4 58 1 2 2 58 1.16 .063 16 110 2.01 59 .25 5 2.35 .09 .14 1 2 H-86 110-09 1 70 23 90 .1 87 20 882 5.19 13 6 ND 7 234 1 2 2 37 2.33 .064 26 DI 2.10 40 .01 4 2.20 .0? .15 1 I H-86 111-03 2 95 6 98 .3 378 40 1344 6.52 49 21 ND 2 185 1 30 3 145 3.05 .059 13 1497 8.48 6 .01 2 4.96 .06 .02 4 6
STD C/FA-AU 21 60 36 138 7.0 71 29 1123 3.97 37 20 7 35 49 IB 16 19 69 .48 .106 37 59 .89 182 .08 36 1.72 .09 .14 14 54
ACME ANALYTICAL LABORATORIES LTD. 852 E.HASTINGS ST.VANCOUVER B.C. V6A 1R6 PHONE 253-3158 DATA LINE 251-1011
6E OC HE M I C AL I C P AN AIL Y 8 Z S
.500 GRAM SAMPLE IS DIGESTED 81TM 31E 3-1-2 HCL-HNO3-H20 AT 95 DE6. C FOR OIE ROUI AND IS DILUTED 10 10 ML MIIN MATER. THIS LEACH IS PARTIAL FOR NN.FE.CA.P.CR.06.1A.11.1.AL.NA.K.M.51.IR.CE.SN.Y.ND AND TA. AU DETECTION LIMIT IY ICP IS 3 PPM.
/40'. ASSAYER./4r 4J..DEAN TOPE. CERTIFIED B.C. ASSAYER.
MPH CONSULTING PROJECT - C-878 FILE 41 86-21078 PAGE 1
SAMPLES Ma PPM
Cu PPM
Pb PPM
In PPM
A9 PPM
Mi PPM
Ca PPM
Mn Fe
PPM t A,
PPM U
PM Au
PPM Tb
PPM Sr
PPM Cd
PPM Sb
PPM Di
PPN V
PPM Ca I
P 1
la PPM
Cr PPM
My t
Da PPM
Ti I
1 PPM
Al I
Na t
E I
N Au$l PPM PPI
H-86-113-13 I 30 7 II .2 26 12 1637 4.44 49 5 NI 1 79 1 2 2 18 7.04 .093 2 1 1.30 9 .01 7 .19 .12 .04 1 1 H-86-114-15 2 73 14 1141 .2 100 3! 467 5.93 117 5 NI I 7 2 28 2 22 .37 .019 2 23 .51 9 .01 9 .12 .04 .02 I 4 H-86-115-11 3 72 15 162 .2 66 41 3621 14.82 60 S NI 2 21 1 23 2 20 5.72 .042 4 1 1.90 7 .01 2 .11 .14 .03 I 1 H-86-116-18 1 31 5 132 .2 60 22 1712 4.96 1 5 NO I 81 1 2 2 51 12.31 .035 2 24 2.60 5 .01 6 .14 .13 .02 1 1 H-86-117-05 2 42 12 152 .2 57 21 4415 12.08 61 5 N1 2 10 1 7 2 13 1.04 .018 2 I 1.01 5 .01 2 .10 .08 .02 I 1
H-86-I18-19 5 47 26 112 .5 125 27 2925 9.11 528 5 ND 2 20 1 35 2 1 2.63 .016 4 1 .56 16 .01 2 Al .01 .01 1 1 H-86-119-08 1 52 7 77 .1 92 18 607 4.34 51 3 NI 6 135 I 2 2 16 1.86 .077 21 IS 1.87 26 .01 7 .33 .11 .01 1 1 11-86-121-11 I 51 6 270 .1 22 20 1962 6.64 20 5 RI 1 22 I 2 2 33 1.90 .062 2 3 1.06 10 .01 6 .25 .12 .02 1 1 H-86-122-11 4 14 14 107 .1 82 33 6380 20.39 10 5 ND 2 23 1 2 2 16 3.62 .009 2 1 2.49 3 .01 2 .35 .10 .01 1 I N-86-123-03 1 27 8 205 .1 36 ll 4759 12.72 47 5 11 1 11 1 I 2 20 2.73 .030 6 1 2.05 4 .01 2 .07 .09 .01 1 I
N-86-124-18 1 11 8 175 .1 87 27 2496 1.22 129 5 NI 1 40 1 2 2 45 9.31 .022 3 21 . 1.89 6 .01 2 .48 .14 .02 1 I SID C/FA AU 21 62 39 142 7.0 73 30 1160 3.96 39 16 1 37 51 19 16 20 72 .48 .109 40 59 .58 189 .09 40 1.73 .10 .14 12 53
DATE RECEIVED: AS 1519114 DATE REPORT MAILED,
- SAMPLE TYPE. CRUSHED A011 ANALYSIS DY F46AA FROM 10 GRAM SAMPLE.
//%%
APPENDIX D
Reverse Circulation Drill Logs
Remarks ic h . } ipnrlVrÎDr .z
MPH MPH Consulting Limited
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OVERBURDEN DRILL LOG Hole *Sit)!
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OVERBURDEN DRILL LOG Hole I{-Z6=09
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OVERBURDEN DRILL LOG Hole t
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MPH Consulting Limited'
OVERBURDEN DRILL LOG
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SAMPLE No.
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Date(s)
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Remarks S v- 4 I. 4S
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole - S6 - 12-
M. Ft. GRAPHICL SAMPLE GRAINS DESCRIPTIVE LOG
ANALYTICAL
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 4 -se,- I?
Property/Area \ SÎi'~~E T~L
Township
Claim No.
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Sampler
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Depth to bedrock
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(o: o0
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
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Claim No
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Date(s) .JUNE 01- r 243
Drilling Co lie4 4, ShPrv,aocj
Bit No. CRtiszn 3(0 Location
Depth to bedrock
Total depth
a + 60 vv 31.0 3S'
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole ki - 26 - t17i
Remarks S~grfi - 3'00
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M. Ft. LOG Na All GRAPHICSAMPLEGRAINS
' ' ANALYTICAL DESCRIPTIVE' L06 ALAS) A 1
. 6A-E~ 41
-
-
s
-
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-
-
-
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so —
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we 11 -(•1 oc~lakd Îaccts F ,--.4,e. C~
30 _3 i r " qe k~,tr►eot~5 s.-.d~
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54âR.^L C 5 ti~4r ~O ro`4~ ~ v~7 S„-.dy
w = _
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- -
-
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- - -
J 1 - 3s- ' Begins (~.
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grc~ S.IiC eetd
j11~: }O J~ i5~ L vet ca.-.L 1 t p4.Rti>rr
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33' 4i
h~ lo 7, "`~7 (.,~1,
IA-55. p7 r' ~~ i-. ~,,,,,~ t,~.tiS
p/~rS 6 1.e-- ~1 - ~rri c; ~i Z"7n'r
- ..".".4116,-Car6owalc GSSoG'a~
V../ 1' fi-,1...,...,41 Je;~.:.~
Property/Area
Township
Claim No.
Location L. X 4-00 vJ
2 4-s-o .~ Logged by .07~ R.
Sampler
Date(s)
Drilling Co
Bit No.
Depth to bedrock
Total depth
Sample screening ~. k .
4.1-1 14- 7 ,
l o t\A, L-.
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole I-(- 26 - !s
Remarks S-14r-~ 4:0o
NEAL_ ~~ dr•,1~, waS1• ~eL~P' ~ ~roâ.~.~e ~4~-JcSI.~
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au
ANALYTICAL DESCRIPTIVE LO AS ' & L% Ay
- -
-
-
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-
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- 97 ' - ire.-, 1c .acte SŸc.;,.. ??
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.: r
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10
- 100 ""'.
-
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-
- -
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- -
c,,,,{40 _
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole
Property/Area
Township
bk. l J I Date(s) .,kiti1E oy- g(~
Claim No Drilling Co (-~eA~~•. d` S =^Qrvlvt4
Location L. 1 I +-OO v..1 Bit No C12, V3G
2t2st.i Depth to bedrock
S R. Total depth 21 1 Logged by
q.K. Sample screening fD 041aS, Sampler
Remarks 54ckei - - S:35"
M. Ft. GRAPHIC LOG
SAMPLE No. Au
GRAINS" ANALYTICAL
DESCRIPTIVE LOG 4,04)~~ - a.. 70,. ~
-
_ -
s _
-
-
-
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-
-
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23 - z~} _Sci`.ay ~r~tVCI F ~1-
p~~¢• • 11
i^N i• n ~ /L ✓oK.:7;~~
- 4 J ~y '~r
4 s,46,.,~,,, ~,,
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= • -
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole i4--ti
Property /Area .• r OJ Date(s) .~ .~ NJ E 5 1 sb
Township
Claim No. Drilling Co ~icq}C, a4 Sho► ._ ~~od
Location L !L{ roof Bit No. C3(o9,h3Co + OIJ Depth to bedrock 3l '
Logged by Total depth 43' Sampler q.K. Sample screening lo ►~~I-, Remarks Î ,S4- ~ CrPrk -
ha
M I_ I GRAPHIC LOG
SAMPLE No.Au
GRAINS ANALYTICAL DESCRIPTIVE LOG
Aub) ps C‘` 2••• AI -
- _
5
-
-
-
-
'
_ 15 ---I 50
-
-
- eo—
-
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' 20 =
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole ij- So- i
Property /Area Datels) JJr.3E S I 8L
Township
Claim No. Drilling Co i_CG1 Eke, w 004
Location L.— It t oot Bit No CSf.~o~~
~ + ~b~ Depth to bedrock
Total depth
ÎoS '
T f by Logged
Sampler P ~ Sample screening /0 4e4,
Remarks 9 :0/ ~ t..;
F - /o.•oS'
M. Ft. GRAPHICO
SAMPLE GRAINS DESCRIPTIVE LOG ANALYTICAL
Aa(MB) As ~ R+t ~r
_
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_
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-
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65 / wed i.-~du ♦ q~ !{~-~ -/ C~a.~
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f — .6 7 J new c. 5..1..c ee•~ - 5%~~ r P ed yE S - (c,~5) 9r,e1-,f,L Ce.-„amcfor btggtr.
*.tic,- Y r44$ I J1J .~ ar5 l~ Q J, t. . - 4r..i1"K,. "A~~ }~ 5 c t~ •~ ,~of♦ -695~
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H - S - ! 7'
Property /Area
Township
~•.-,e~~ke ~-JoK~e~ Date(s) jô(o
Claim No Drilling Co #1,"q11,, o -d _J ,r,)r
Location L (7 oo ~ Bit No Cel,gh 1p
r J r• a N~ Depth to bedrock
• Total depth 7-- , by Logged
. Sample screening to /✓(n tk Sampler
Remarks S-6,-,} - to:~9
M. Ft. GRAPHIC
LOG 8AMPLEGAAl1~5
No. Au
ANALYTICAL DESCRIPTIVE LOG A 4(W6y Al ' Ca 2„ Ac~
- -, -
5 _
-
- 10 —
i
-
-
-
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-
_
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c f' w~ ~
- we_ I f 4.* .l4 loc~ i tcl
60 - 68' {~e-~re~~. e►,eo ts sc,.-,di j r4L v I I-i )I
- s~7 L i`\1. TO -4-c_VOIfehC ~47.-...2....-..,E J~- " '
L - ~:•,o r
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..- S`1...4 4.1J4k r 7o Sup r044.14 0./
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;so
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.p=
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f0
--
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~
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1
7
;
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1-1- % 10
Property/Area J Date(s) ~ vrJE S ( ~â
Township
Claim No. Drilling Co j4A 0.vd Sherv,J0o4
Location L J2o 00 v•-) Bit No C g bso 3 (p
~ t n► Depth to bedrock 7I
Total depth 55 Logged by
Sampler A k. Sample screening lb tAP 5k
Remarks
M. GRAPHIC SAMPLE ~~ Ft.
DESCRIPTIVE ANALYTICAL
LOG Ak(H°Bi AS Cu Zn ~c
-
- -
_
s
-^
_
10--~
e—
-
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to—,
. -
.
25 —=
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7
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if 47 I.- S I 1 41e~ '~9er.eo~ls J
4-i 11
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S 1 -~.~ .R~pc,.~
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=
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77
—
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7. 1, p ~: 01 p i 60
9f~ $o~
lzsro 4`i MS- ab
ee 'D/~~ p o~s o H 240Oï
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4--.1. ; jC.
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7
7
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1
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole (4 - 86-zi
Property/Area Date(s) J lN,3E s I t>D Township
Claim No. Drilling Co ci Si-.or.. Noocl
Location L 12_ i -Ob Bit No G,gn ~~ 34-fso 1.3 Depth to bedrock 8
Logged by S~.R Total depth g5,
Sampler k Sample screening /0 N1n5IA
Remarks -5 12! 5Y
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL A,JUPo? A3 " GJ I-% Aq
-
- _
s -
- -
-
.o.-a _ -
_
.s_
-
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to-
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-
-
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n 4 /~ A
o - G(- . dtAi----.ts
_ 4 68' ~o+^~oyeheo~
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71 - 88 1 7e{ '►oreoms 4,- 11
— ver i
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(7 3.5- 7~>
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g ' I 3 ha-)e-)pCjt L T/ Ii
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-~ j: 00
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 5'
M. Ft. r'APHIC LOG
PlE Na Au DESCRIPTIVE LOG
ANALYTICAL
" 11.— _
.... _
,o—
-
-
,6—
L.—
66 --•
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s-
_
_
.,NO
1 q
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—to 6 S(- " Cr/ FjhQ(,j
4 css . (.1°.1) . !
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•
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole i - 56- . -
12. 0L K+ke kL&t° I Date(s) Property/Area
Township
No Drilling Co S b,or.400cJ Claim
Location L _1 too w Bit No. re Far? o 3?
.3+oor-~ Depth to bedrock
Total depth
ID6'
.5~. R. rtI ' Logged by
R k• Sample screening Sampler
Remarks
;6,14 51., - °O
~PNdC Ft. I`~
GRAINSM.
SAMPLE No. po
'ANALYTICAL DESCRIPTIVE LOG A,.01/5) %)S ' G. 2n
-
S —'
-
-
,o— -
_ -
a
_
_
25 —
-
30 —
20 —
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r~rlrl rlrf
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l ~ O^"to92nr`oct3 14c45),-•;nC
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/6 5L .- /°6.
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rO?mays 5..^.citJ gra✓Gj
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t ~5f ro
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--
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dm.,. k — ?? _
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Iy I rf1 CG 651 ) vG~.i Lai/ CiK pe fsasi
3 11°5'1) °7° ~~rl~ Ga r- 620,4t.
Eo 4 - III'
— { ---
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T-~_ ~•
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole tf - gb -~ a
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAMS
Au DESCRIPTIVE LOG ANALYTICAL
•Au. We) — A Ca Lm Al
,
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Township
Claim No
Location L ,2S? +00 W
3 too .-N Logged by -P R
Sampler
~}. K
Jk,oE .6- 18k,
tiga37 Depth to bedrock
Total depth
Sample screening
Date(s)
Drilling Co
Bit No.
/0 ngeçL,
77
sz~
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H-9(9-.11
Remarks Sfa„ f 4:2D
rinish
M. Ft. LOG No. Au GRAPHICSAMPLEGRAINS' ANALYTICAL
DESCRIPTIVE LOG Ak(M6u As . Cu2., p~
- : - _ ,` i1 ^ ,• A A
- ; 0 - 6 , - (-i, ...-...-s / 09A r.'- c-s
7
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✓r
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- =
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io— •
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-- - _ J ~J
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a— 1"i-S2' Bedrock °"+
J.
- . - 1;"31.4- qr~.rN grc.i kiSiG volt. - ~, = = U;+~J..i, ~ Si /~~~ _
20_i C ~~G~,
r~(i4e. _ '
_
:~ {{
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_ ~~ " - -51f ,..-\Pi'4ces oiWt h' - _ ,
a fi~e rq i-~~or. oo I`~
rv~ ~ 0 8 — y •'74.,,,' - 01 o
C . s~/A,JJ _ 02 0 7, O
23 —
-
_ ^ CSi- s,
t
_ 50 _3
~ - - J
70 -- - 100 ""' ! ' .. --
to Merl, Sample screening
Date(s)
Drilling Co
Bit No
oG, IRt.
~qih 4~â Sho r ,~ood
CAR I-,gb37
Property/Area
Township
Claim No.
Location ( ? / 4 (.36 w
Depth to bedrock
Total depth
3too ~
Logged by
Sampler
J
s. P R .
gk'
/00
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole IA-
Remarks
V or - Îo :SD
Q<-
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Ir k.
M. Ft. GRAPHIC SANPo LE o.
GRAIN DESCRIPTIVE LOG ANALYT ICAL
~ri~~ ) As ck Zn
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/locyl4%S - Pro~kw►S-
v 4t^N roals P l L+i~~ JJ
91 f.S- loo' Bedrock
t I~4•,f green Qrel Serre
~~. +D felsi c JG I~.4., i0
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l l'
i
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1y7l-1^11414(61Ld
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.. 01
J .• ta Property /Area
Township
Claim No.
Location
eqal.\ Sl-NprvJ004
cli, (0 53 032
Drilling Co
Bit No
Depth to bedrock
Total depth
Sample screening
uz' 1r4 ~
10 rAesl-,
31-5-01J T.t?R.
A k.
Date(s)
L 3 Z tnrn w
Logged by
Sampler
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole -
Remarks Sfcanf - S:/S iJ ok - A~•v+ 1~ rrt ~n h i +
f0/1r7 tint - .
~•~ iSl, - /0 :lIO
M. GRAPHIC LOG
SAMPLE No. so Ft. GRAINS ANALYT
DESCRIPTIVE LOG ANALYTICAL
Aa(A~) As Cr >;+.
—
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole F( - 26-25-
M. Ft. GRAPHIC S4MPLE GRAINS ANALYTICAL
LOG No. Au DESCRIPTIVE LOG Au (A°6) AS Cu. T„ At 100-7 ,b- ti,V. .: 02 ,03 D
`• = afr o 112'- 119.' Bedroc .2.1s- ?.4.0 156 90 o.,,- «
QS o - .245 32E alo 9~ o,Y
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MO-: : •
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole N -86--6
Property/Area Date(s) Jv►.lE o(o 18b
Township
No. Claim Drilling Co. S d
Location L 3 Lf t 0 W Bit No C $ (09,038 ?1so nl Depth to bedrock 7`f' S P ~. Total depth fS0 ~
Logged by K. Sample screening 10 NjeSl-,
Sampler
Remarks pu4_ ^ - 2civ4 4.~%e Z.00M VP~I~
-
M. Ft. LOG GRAPHIC~~~~
No.
' - ANALYTICAL
A0DESCRtPTIVE LOG ~(R°6~ AS 64 2"kt
- _ ^ : D-5` 1-1‘4.---...5 /Or3a..,.cs
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1
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ro
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25 -
J
=
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1
DO - - 100-
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1-1-
Property/Area
Township
Date(s) IviJE oL, 19L
Claim No Drilling Co
Location L 3 (, Bit No 0 R 6,50 zt 5-0 rJ Depth to bedrock 22'
Logged by • k • Total depth 53~ Sampler • k Sample screening ro M(4-, Remarks
M. GRAPHIC LOG
SAMPLE No. Au Ft. GRApiS •
DESCRIPTIVE LOG ANALYTICAL
44.0°13) kS Cu. 2, AR
-
-
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- — ''° ' 03 D _ $ ; ,2yo 37o I~Y "ii 0.4 %// _ 0~ 1,---1 c,„-- ~ ha~ '‘.2
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Remarks .5-ke-4- -5; ov
MPH Consulting Limited.
OVERBURDEN DRILL LOG Hole H - $ 6 -. Property/Area
Township
Claim No.
r 4-10 ¢-00
Datels)
Drilling Co
Bit No.
--eP I h SI-2r c.Jo oc Location
Depth to bedrock
Total depth
Sample screening
-79' gS' 10 Mo sl..\
Logged by
Sampler
M. Ft. ~' ' LOG
• ~ PLE Nc
o" ' ~ DESCRIPTIVE LOG • ANALYTICAL
14,41,4) AI (1. z~
io
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^^ 1 O — 4- - w •...,.~ / D rcpe% ics
it-76.S' .D ar k -6 lip grel _
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7 g ,s' 79 ` - s~,..if a.~►o~-.~ ~ ~~ ,--.4 ~,,~i
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= .~ 36b Spa kr7 1•k
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100
1
l
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2- -l- DO r`1 4). g,
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole t~-5(0--z-1
Property/Area tS 1K-' of T_L Date(s) .IJnJ6 OZ'V C~
Township Drilling Co. S~r tiiavd
Claim No
L 44- too Bit No. C3(c9g03R. Location
Depth to bedrock 9 9 I Totol depth 106 pR Logged by Sample screening Mes i,
Sampler
Remarks
M. Ft. GRAPHIC
LOG SAMPLE
Na GRAINS
Au
ANALYTICAL DESCRIPTIVE LOG /~~ ~y ~7(irp) AS a, 2. -,k
' -
s _
'
-
- w-
-
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-
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dep{k ;t . 10-CkS .1- -sL•
qwco
$7-9i' - c,~(e roqph~~ 54+.ôY q~0.~1 J J~J
4-iii
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Vo tCyr;L
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—
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//
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
Au DESCRIPTIVE LOG ANA,LYTICAL
- Itto
-L<, -: 03 ,-
__ 110 -.
_,
_ _ 7
Sil--...." .
~
. _ : IRO ~
_ ..7
2
..•
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NO- - 40 — -
. ~ . .... 7
_ NO -
i -~
- 7
48 ] -
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J
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. 60 — .
- 1 I
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-
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7 7
°0 ^ 7 7
zOD- -
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, ] ~ n
_ 210 :
ss .-1 t .
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— 2703
~ ~
_
- -
1
Qt re_o1/4 Remarks -
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H - 26 - 3o
M. Ft. GRAPHIC LOG
BIAAPLEGRAMiS No. Au
' - ANALYTICAL DESCRIPTIVE LOG Ai.iPP6Î As . C. .2- ~
_
- -
5 —
- _
-
io—
is J
-
-
_
' _
- 25—
., n^ .
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it - s4 ' #o«., o9e~+aoKs ~.1.1 f 1 ~I~kd IfCc.tSL~r itit Claj
Pt- 94 i UQr~ fi Sg..4 - 20-5vZ
9sSor-v4 'c~SfS q_„.4 ~~
p•Qa0--►~..{ ly
vo lL,4,,;4,
.- '1'75a.dY ----.4.....,---.4...--.4.....,-~o
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1 IrOr`~nE
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c 9,
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5o — -
03
—
Property/Area 110 ç c k /Joc
Township
Claim No.
Location L la too w l
Logged by
Sampler
Date(s) J thJE *7 rSb
Drilling Co. I /IN and Sherwood
Bit No C6 6$039
Depth to bedrock 94
Total depth 77 /0 i'(e;' Sample screening
.3 t- S ,1" i? R
k.
Date(s) 1JC OÎ g(p
TP R. A. k.
Remarks frIr-1- - 12:20 ~ f.10 -r'iL.~
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole - s6 - g,'
rAnue-d 2.5 M 4a1 /4..t.rcL5 [o.sel...rb,r 1b dr,'ll 32,
M. Ft. GRAPHIC LOG
SAMPLE Na
GRAINS Au DESCRIPTIVE LOG
' ANALYTICAL Aa(N6) As .a Al - n
' _ ~ - D s ' /4,4
1
..-..KS /rjqic,$
S-- be- Dck •-k h 1.q~} re
_ r
w-
- s
_ — - - wet( c10 cK{gJJkd, hyM o7eneoks
( Q c44 Si-eihe G%0. — - im- ~ j
_ N D T tL_ L_. _ .._
- - bD - b if a $CdrOC-k ao—
so= - (1,41-k9rei blqc,~, 9~~(~;kL
griiIliEe, - re.4,,4-;v(y soe-4-
= -
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~~~17
— ~ ~= _ i - QP~rs
-it. be_ pc,..-1-pc,..-1-4
~
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r I o~ S ~ 44..44 - (~e - r 12..-.`QiI~~
. _ $~ih
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~o - _ 0 ~ 5 ~-r~ ii ~or ..-~, 6r,..~(S
- `'~-~~ `~.`wilZ vw ~., -1G5 7 7o- _
_ -; :
b Z :S - -
J
_
D-7" ~
Property/Area
Township
Claim No.
Location L 40 +0 r.1 t 3oS
Logged by
Sampler
Drilling Co Ple_af. S~.Pr t
Bit No Cg b3n,?q Depth to bedrock (oat s.
Totol depth 61-1
10 MPsI~
~io.,-►Fcr~~l Joyr~c~
Sample screening
Remarks ti1 n T 1. 1-.L- k - 1P,•.s~ F 15L - 4S
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole N- 5 -32-
GRAPHIC SAMPLE GRAMS ANALYT II CAL • M. Ft. LOG No. Au DESCRIPTIVE LOG
Abaft) it. Ck 1"`
41
-
- —~ `~
- ~_ ~ N o -r i 1_4_
O—L} ' fit"•KS /OJ
..4-GS / /‘ :_
__
4 - 69 ` - D Qrklb!' ,f !
:_
L~ "'Wye ~5 ç~5f►-i
^e-
- a—
-
C'4J_
_ _ -
5- -
- we 1l TIoc(Ala fed 1.4f /CAS Sa w; f f,.~ c~ePlk
~' 7/ b - ,Bedrock
.. m _
~ ~
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+e
1
4~,
,
~,k Jed
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~Wy A:-.e 494 ycen
_=r
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,-=-
_ _c~~c4 s~d,.~.~.~6c17.1'~ -
_OCCY$io^W` '`i5 ~/~yCri~:- — _
F055i6li clv....-„; (4 eAlv,t;1e--
=_ - 5;1 iceokS QSR114Îf
_—~.o-_— _ _
:0- ~ ' (7 o~~ r~~ 1,,...4.-N~{'iiC. ~.
55--]
=
70— -
70 --////- ol ~-71` J ~6
~•~â•M
~ -
_ 3 :
p -. ~
40^ ~
_ ~ '`•
~7 ~
-
- _ -
''] -•
Property/Area
Township
Claim No
L— 4-15 1-cb (.1 ~ rcxLS
Logged by
Sampler
Date(s) J~ ►JE o-► 1 S%
I1€1;41-, 004
Depth to bedrock
Total depth
Sample screening
Location
Drilling Co.
Bit No
R. A.K-
i w,~sfa~e ~J~~.tel
7(
Logged by
Sampler
Property /Area
Township
Claim No.
Location L. 32 t-00 vl
t-303 S R.
Drilling Co
Bit No.
14P..c01.-\ et S (Ner,..1'oo4
CA h gr-) 3~
Remarks 54-INr - l'S(.
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole F4- g6- 33
F~~ç►~ - z- "
M. GRAPHIC SAMPLEN GRAINS Ft. DESCRIPTIVE LOG
ANA LYT OCAL i~iF1~ AS C~ ~+. 19Y
:
-
s— -
-
-
lo— _
-
~_
_ -
_
Ys —
10 —
_
:~~ n^
n .
.
_
_
d -'✓r, ~Lt«-~..LS I Or~ ti~ GS
S1- 1 Dc~rk Iv I, ~1-4- 3r1 well 1oCyat~q
J_
I
~^'b9lneous ~4C~t,$~1~►e
clay J
.
Î~- 9/r L1J
i~e.tCrop.trleo tS 5,4-,(Li J1 ~Jf
Jr~tJ`~ 4111 _
` 4r" ...loir ClRSS 4 royk,ried
Pe-We-5 9 ~
/
'"- g°/, C - /hf . i/o ' Car► iCs
- ~al~'ra-•; fic. 4^~ /o y /o
~_ sed.,-,er~.-7 der;,~
- 75-' Jeâroc.1‘
.....
-
-
-
_
_ :
a_
- Yo-
_
^
_. — —
- _ _
- _
—
_
_
_
Yo=_
YO—
so - _ =
— ~r !< j!~
bl~c k. 5; f; ~,~;~ - s1 ,9~.1ty .~h
~ ailL irp.,S Foote. Ohc
t+-`. /-
~ 144.~„I•~C~~
r~1~4;vi ,1 ~w ►rd
- ~^ i hDf ~t.4.c.r ft. VG.r^~,e~q
- S'w-i(~,r J
h bedro~k ; .., ~~e.31
— J
_
~
-
.7,'9s ~
✓ ~ ' ►.=
o.Q" v
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cj
- OZ
p âo 172 2aa &o a8'
~
~o .Q'~ ;. :: ; Q _
= 03 0 l ~S 3F6 /oF ►oY a6
o 1{- 230 ssz (08 lao 0.6 ~~ =
Ds'
: -
100 _
Depth to bedrock
Total depth
Sample screening )1. K. p r l•S
%4 Om FSTr}r C 1 J O V TE L_ _
IO Mnsi,
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 4{ - b -311-
- 3'. SO
M. Ft. - - • LOG
•- PLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
A.( NB) Rs - Ck 2.‘ A3
_
-
° —
- -
,o _
-
~_
_
so—
- zs —
so —
". ~ /~ A. n
uis
~ ~
~.~ `k`r+...1/45 I Q rg4..,Cs
3 - 60 ' D4rk .6 I JI...i- ore.) 1).-.7,,rz,.-,5 I9o.5fr,•.-te
Cl° .7 (~-11. ffocu.li4kd}
' ~ _ 82: 1-1.644130 ~vaJc•~e,o,L5 Sa-,dy 9r,, ,.1
~ ll .1 .J! '` 1
a ~Miar ~ ro~..~4 ~,~,
~ ...,~-c_ „a I C.r~..~~ $oj e
-- w% irlar g~
p~s C 44n1T i [S
a~ 9e".NC-45
,s 107,
82.- 8S ' Bedrac..}~
1
-
•
-
- p
1
m
~
I
---
-
_
—_—
- r %~~ re-G1a~ 61„,,k,
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— r Sr lrCPo4s
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~0~ _ 8S ~
so --_
~}^~•r• le r: G:•. SiI1~Siro~e
It - ~~tqrr~
~ • • p•: v.o ... . Ol,oy p IW 130 160 yo <D.i
c...3
so
1
1
Remarks
Property/Area Dote(s) Jvr.1E 0-7 (" Township
Claim No
L ?i, 1-00 t5J
~Podt, S:.rrt..)00~
Bit No CI. Q 3 ~ Location
Drilling Co
Depth to bedrock
Total depth
Sample screening
$2'
$s' JO 042.51\
.3 f--go 5 .S. P R
A. K. Logged by
Sampler
MPH Consulting Limited`
_ 6 :on
M. Ft. GRAPHIC GRAPHIC LOG
SAMPLE No. Au
OWNS ANALYTICAL DESCRIPTIVE LOG
AL(M) As G. gen. A$
.
:
_
-
a—
~
_
ü
,
_
- 20-
_
-
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_
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i~u~S IDriar.,çs
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Îlo...NOc,pheo 4.5 Wer'I r
JJ t'l e~ `'~(r..~ed k C`v`r f ~ C1Ay
gD $9' vQ~Î
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gq _ ~2z, ~ 51 ~ ayy,~ b o` 4dP 2 Yio—
4'(I
` R1~~01^ 54k 'NCI %V 41•N
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7
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0. :.'
- Of I A6R. .40P4 3y( 131 n O~1 ;
w — 70.-'
'p` 17 a.'
- 03 -
IAtR. .3(.~ 2W 90 3G 0.1..
OVERBURDEN DRILL LOG Hole
Property/Area 0 c 1141(E 1 SC t) TEL Date(s) , 1 ~► ~J E
Township
Claim No. Drilling Co.
Location L 3 4+ +- 00 Bit No Cis ( 4- 1-5o S Depth to bedrock
Logged by Total depth R Sampler A lc. Sample screening
Remarks
FI -86-3 E-
a-i. ~ ~~~
S hQ.tvJcinCi
cf 12. S I 132'
~
Io vAD5 1.-.
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 4-$6- 35-
M. Ft. r GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
~ik(PP(i S A5 G,. ~w Ag
- ; Rio
y7
• : ' . -~ 4' : it I ZZ -132_ • Be _;...41-121.1._ _ ~ . k.
v:.~ _ - _
~6) ~
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~ 9 ~ gr4( Its 132 ly7 `l9 I.2 - _ 9 . ~ : 6 ~ ,, .• 4 (. ~.. ~ ~ ►- ~ _ oti5 —
,6 _ • ~ 9~5+lI ►' E~ _
~ i 7 U
Ito - r:',• — g• w(-C.. S~ l.[ eo.iS ;,~
!co la la~ 3G D6
— - . 9. '
r g i 14614 _
f ~S 3Bo AL', !ny 91 0.8
- - . /
1//~
: ''
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- 110 - ////1-± D I - i~ 1 zq'_ ti-,~,r~ ~ K i _~ . .
,~-= 5 ~
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_ ~ ~ ( 6SS161,~.
~(4cce4s = 7
_ ;
M0_
-- ~
7
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- E : - 4c1.-11 .1-4. - au! ,,s ,
-
46— ; _.: ~
J e9ti - (.32.:
-
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:
-
7
j
:
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so — : :
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3 . - _r :
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- :
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:
- 210 . 7
i6 -0 : :
_? ]
_ :
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71 7 - -1 -
Property/Area i•\o,AEST►tKG 13001EL.-
Township
Cloim No.
Location
.Jvi.1E c-( l Sb
Drilling Co L Skerv.,004
Bit No CA (,"7 I O12_
Date(s)
Logged by
Sampler
N, o. k,J. ~k.l,y Depth to bedrock
Total depth
Sample screening ID McSi.
11,3'
(23 '
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 4 - S6 -3&
Remarks
M. Ft. GRAPFAC
LOG SAMPLE
No GRAINS Au DESCRIPTIVE LOG
N A LYT II CA L Aitilta) As C. +Z~. Ag
- -
-
5 _
-
-
- -
l0—
_
is—
_
- 20—
-
J
35 —
-
—~
70 —
..b
-
$
~ S
S S
E >s
g a
~I
►i►
t lu
i tin
ul
►iii L
i►ul
►i►i
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i1i1
Ii
1ii1
il m
i l t
in~.
~u
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_►ti
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►IIIL
LI _►
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ili►
i~~ A
A^ n 1
A r
^ ;
• - -
a - ID ' - 1440,-0.4.5 /D c7aiN..,iGS
!o - 83 . - La e ..c5 i-- ; -•. e. e. _[4.y
83 - g`t• S - s ~~ .~r4~ I-;( I
(11-6-- 87)" Ijew .
•~ 9're~.! J. - I,,~.f - ire-~ VJ (x+lt-
9~J/re`j grGe..1
-i.` I
t-
vo k,,,~,/
' ............-..,Dr pi, i. k ti ~nsr 1.....,+1 .,-60.......1-,- ✓cr^``1-5
(t !0 - 1 ! 2 ) Oil
(`
~~1 5..-.4./ L 6, I ~ 1-1. ii
I13 -123' gedrock
'
.
=
_
r .
- - _
_
I:
_
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lxlls y.,; 1-1-, ~~..~ cl~j's t
- --t-I L e -.. e ►,.1.. :1-ri- 640.4_ Sc--.fic_ 7%
- re-4-1 S,vyi ar'.1\;`•J
- G•P132ars }n ).e ..-..sF11
'g~`} J`r~ (`e ls~c " ~ - i-tiL ~
k•,4 C Iks }5
- 4.• le V.. 6L-• 4c. 1u' ; -, CA 1,
--~k ~ obk~.:.,
(..--•‘.5e c~.'ps
6,i1 — 12_3'
- ~
r
-
-
_
_
r
- .. o
- —
> . ..., ' 0 60 3of' 130 SG 0.4
4• - ,' p ~ p ~..
~ DZ _ -
fluc. Ho ~61s no PI a6
9.0
9 4: Q3 0?z;) &96 90 y3 o•B
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole
M. Ft. GRAPHIC LAG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL /~(y6) hS Cu .t+A Ay
—
-
-
se—
40 —
_
_
,e—
SO—
-_
-
_ ~_wo
_
_
__
_
a—
IC ~
..a
-
qp~
- '-Y'• .•
:v : r.
.. O
_ o3 . al
= 220 &96 90 '!1
too —
-
_V _•
r - fz' - I ~ ~ '
• d 99
Of .
_ 7i7T ////
'/// r/ /
os
—
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— —
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ao - ...
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... ~
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:
wo-
-
~_
-
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~
-.1
--1
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=
200--.
~
!10
' -
]
_,
ro --=E
!2D -:
]
1
1
E
~
I
1
1
E
i
~i G
~
~
~
Logged by
Sampler k.
Property/Area_qDME.S fA is j J OJ 7C (-
Township
Claim No.
Location
...Woe o-( (2,6
Ile9fi. Sfter,~101,4
CQ L -t 9 0 -1P-
Depth to bedrock
Total depth
Sample screening IO At'bSk
/ 03
log'
Date(s)
Drilling Co.
Bit No
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 1{-56-31
Remarks
M. Fr. GRAPHIC
LOG SAMPLE
No GRANS
Au DESCRIPTIVE LOG ANALYT ICAL
Ar(As) As CAA En p~
_
-
_ s—
_
io—
-
_
T
_
20—
-
-
~
2S—
- _ J
_
00—
iiiii~
rrr
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i~~
rri~
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~~
ii i Iisii
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riji1
tn
im
1riiiii
•
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8
2
2
^ ~` . ^
^ r
-
-
-
-
O - 9 ' - Ei •...-.•,.s 1 o rqa ,i GS
p
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f -SS ' LgC~tSÎr~~1L C Loy
J
. ~
s; 15 sa..d
ss- 7o ' -F1•1.N.e. Jr
r
b..,i,~d S, 1+
q~ ~-~a5
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- tt' -âr wr.
- Î% '- Si• I~ ~ y J oCcA5f~~^,E. C14~
- q re,/ hg re/ 3,—ten
4~ 5reehl,S~. 11".."--**
1 3' g-rtt 9r4ir►eÿ +~ Si-S ~
- /RC E./611'1.4e -
1J14"~ ârom‘ ,
93 ' ~ . 1
—Io3 c`•-~~ ~~0.~~ I ~r 1
.
l°3' 1a8. SedroC.F-
—1111-1.1.-- 31(47o
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-
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:
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c61.1~'
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- :
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` 4 .] c G ' Q • . 0 .D
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":
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 14- 516 -37
M. Ft. GRAPHIC SAMPLE
O. GRANS.
DESCRIPTIVE LOG ANALYTICAL
Ak(~f,l RS at. Yx t - w0 -
- 4a
0. ~. ~ - b 1 AbR.
- ~.✓ ~ . °2- Ip - -
-
35 —
120 ... 7
~: "• - —
'.
RO— ..: 40 — - "
- ] - = 7 - = ]
- NO —
- .]-
- ~ ''] 45 — ~ ._
..RO — ] .i , " y
- — .. -
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50 " '
I10 — ~
- - ti
• 11111
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as — ..i
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;
TI
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D
MIO - - 0.
- -
-
ml
IMi
Go — - - zoo- -
- .
- Lw - '
55 — - -
_ 220.. - —
Property/Area I4 'f S~°l~GC (ao•~k~
Township
Claim No
Location
Logged by
Sampler
N.O.vJ.
A.
J ..1 ►,► E 01 `4 6
Drilling Co. ~4 d SkGr-...IDoct
Bit No. C3 618 o12
Sample screening
/0 IA 42..ç
Date(s)
Depth to bedrock
Total depth
IID (
I l,S t
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole
Remarks
M. Ft. GRL~ SAMPLE GRANS ANALYTICAL DESCRIPTIVE LOG 1100.6) Rs Ca ~. A~
_
-
°
-
io—
-
Y5-+
tb —
_
_/~
_
~
^
: .
. - n,~
o _ ID ' _ ~( ,^^`iS jOrjcts...,-cs
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- Lt.S 'gC451rinC. CAa.j
-'J "- Sgi laICKSkrf..5Q Si i'}
.70 - %if igCK$ki1G C '/
~ .-•di , ~K ~~ I ~ ~~ 91' ' 11 v - Sq
W 41,-... 6+r.i^or ctOj
pe lle-15
r
lio'- le ' Bedro c!L
•
-
-
-
_
—~
-
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so
=
-+
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.....
:
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LL 1 tr r
- / ~00 T
~ 1..,}. / .A t~~ ~1E{q ~
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/
^ P~
,........."..t.,+ +1igp~ l.sr.~~n.('de .4..1-,
- s..Q---s iv L. 1nie,4,tce iF
%nt. I-4-f 4..d ho4ti.(. a r,; IIi k
tOhG —
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1 1✓D ~} - 1~5
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-
- --
-
_ ao—
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a' D,. , a •
_ p~
. p .29U 3,34, 132 58 04
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H -v, -3
M. Ft. GRAPHIC HIC SAN0.l.E GRAM ANALYTICAL LOG
ANALYTICAL Au Ault/R) As G. L., (13
45-
100-• .r _ _ • P D
o I
1q
_ — —, 0 —
- - ,; P, . — Il ..c. ; 0 2 O W6. .24P I it.) 44 0,7
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15
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7.
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_ : :
- : .
J -
200~ -
_ . ••
-
-,220 - -
-
~
~
_, 710 -: ~ • .
EL ES Date(s) Property/Area
Township
Claim No.
Location
J00E o7 iqL.
Drilling Co
Bit No
a-.â Sk.cru..looc)
Ce Depth to bedrock
Total depth nl . o. %Al ID Njes L, Sample screening • K
Logged by
Sampler
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1-1
Remarks
M. Ft. GRA WIC LOG
A S MPLE GRAINS No. Au
ANALYTICAI DESCRIPTIVE LOG
, Ac~iPPô) A, G. Z."'
-
5
-
-
-
io —
_
20 —
-
-
10 —
_ -
^ .•1
n
^
: _
:
8 4, kg IIRE . 1ûtL
0- l0 ' - 114-•...15 i
G r,Q-" 45
I /0-!fS' L4C ur i~e c I a-{ ,J / ~J '.~.~ / ' L CZ C ~-t 5 ~~ ; ^ ~ s;11-
ss~ / q or LQc4$he C C / 1-,- c. /
ei fe w pc.6bles
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02.0) ,+„hor a.._•f. e ,~l7J F q
<<~ ✓
t(/23> irons c06,6c06,61/...~,
red a•~ ,..11-,;k 6crciuI
(! 1w' ) No re1,,,-r, - 1L;k- pl~.giel
rZS- iZg ' _ 4 ver~/ he Obi s4-.C~ /
~°~,k cl,; 11%~ 2-0Z co15las - Ce55or f ed,
I Zô - 13 3 ' •geriroc k-
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-
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-
;
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_
-
,o -
_
_.
so —
_ -
o ~ _
.. :
~ co - - —
-
- ~_
_ —
-~~_ _ ,--
- c Ler~-I WI-~.;}e 4.4 browrN
Io.,,..;J~s 6.4 - "46111:41v4:15
— Pc6S;~~y Qu~~ 4 ,~or~s~h~ u~;~ - c ~.,,_; c41 sad: -,.`.~
a` Ii -
133 i
-
~— ►~ 90 yB8 too .~1 0.~ .
T = ~ ,
a ~~
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N- %,? -37
M. Ft. GRAPHIC SAMPLE GRAINS ANALYTICAL
LOG No. Au DESCRIPTIVE LOG 461,1h1 AS Ck Z4. h3
_
Iü0
_
_ _?`' o - i .
_ _ -,,_, — OZ _ v-=, .
O—
ix, N •Ç'-
_ • ® . ~ 03 o 60 38Z 190 bs 04
Ito =
_ 3 A®c. _ _ olf IkL o.i(mi .2qo GL Y2 o.y
_`, , _~y,
o~ 3Rde ai~Uni) WU. Go 37 0.3
.... o U JD S42l,? ~ y0 1).4 no =
7 •o— " , /// O
Iso— ~
Iso — ..4.
— .
~ _ '
200— -
16— - ~
ow so— —
•6 —.•0 ..- ..
IC - - -
— ;
Is — _
MO — —
- •
IID— —
... 11.0 -
210 -
_ ~ o
— 220 —. —
.
71.
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole /to
Property/Area T 6,414'
Township
Claim No.
Location
Depth to bedrock
Total depth
Sample screening Io rAe_s k
Remarks
M. Ft. GRAPHIC GRAP LOG No. Au
GRAINSANALYT ICAL
DESCRIPTIVE LOG ALLOW AS Cv l'A As
-
- s —
-
-
io—
~ —
-
u
-
-
H _
_
~ ~ i.
A ~
:
- - 10
0 "" ''0 1 ~y t..-,....,,S r 0 r,ctr.t.CS
/a 45 t I et C k5 Fr r ~,e C ici./ /
4,~ - 6/ Iact4S 1-1-i-►~ .S i if
/ 6 ( - 6~ _ ~ 4~~5 ~r1~ CLni
6S' 7é 5~.-dy qr,.►~ ~ 1 ; l I
~ `-~.i..or I.3 dots
7$ _ g3 •.~droct
w
= ' _ -
_
~
_
_ - ~
m-
—
—
- :
-
so=
_, ~
_
: -
_ : -
~ - ~s; ~ 4-,..“- - k5.,..d.,.,+ S~rr~ c..;}~
- a,~tior` /0-a .11- ~ I - ~;.,-;k 72 t«.~p•.:~a:.#f
~Î ° 9 ~ is,--e. L..wr 6. ve ~ h
- .se.r, c <L.s.- 1- j P.m.. 6,.....1; k'
rr ? }a`J. ✓-0(5 6,St.
_ -_
_
-'-
s0— •
— ';
. "; , :
2 8v 711 130 (.& 0.6 -- 70 - d ; .,Q
~~ p' '~ =~ CI
~ 01 ~
0
390 3~1 ►:. 8Z ay _ ''t G' : Oz zptt
•
irr 1007 —
Drilling Co
Bit No Cgt^-1,3D3
Date(s) .‘ t.r ..I C 08 I g‘,
Logged by
Sampler A is
Property/Area
Township
Claim No
Location
Logged by
Sampler
A.
Date(s) ~ ss~~ C)5 I Vo
Drilling Co
41'e-tct r- tool
Bit No cRL-cg 0H-
Depth to bedrock
Total depth
Sample screening
i{bwAESTq Î.!oJTE
Ltn.3 ~.S
10 Mcsi,
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole - R (, -
Remarks
M. Ft. ~LO SIMPLE ~GRANSN
Au DESCRIPTIVE LOG AMALYTIGAL
Au(/RS) As G. 2,
_ - n n - 0 - Lt ' - 14.4 ....,..,5 i O ri a •-,<<5
- ei _ if., !'Q
C k5 1-r i Ke. C 1::j w =
— s —
— -
' (319 6.,, it Pecs
- - 440 - 40.3' - 5.••-.d 41.0.1ireAuc,1 >m--=
40'3 ' 46- beârock m - -- i, ~
io—
_
_ i J + a 't'-,1-• 4 4 .154 4-.-e
- ~ .+ + o r 1467 ENOU6H /AA74)1'1tL
ai
Is- = ~— - -
_ so
_
Yo - - ~
- 70 =
b - r .
25 -
90 -4
50 - - - 100-
MPH Consulting Limited'
OVERBURDEN DRILL LOG
Property /Area
Township
Claim No
Location
Hole I-t - S(c)_ Lt
Date(s)
14e a 441 d S-.er,,,iooci
Bit No CRts -7 014-
Drilling Co
Depth to bedrock
Total depth
Sample screening (o Mes k Logged by
Sampler
N. O• ~.1. q K.
%0
Remarks
M. Ft. ~~ SAMPLE GRAINS DESCRIPTIVE LOG
ANALYTICAL Aa( v6) As C~ k~ AÏ
-
s
_
-
io—
~
20 —
-
30 —
- ~ n ~ n - .
~
:
. _
~ o - 3 1}k~~5 1
Droa•..Cs
3 -7$' Laetks-kr.e, c 1scti _
—SI:~1y gr~ay q ~ 1 J ~o,~~d ~IS~
CI (.6‘-‘0",-C1 6°' k..d"` i-b beco.,-.e . s;j }~ Cla
7si'- Sa' . 5 I • 4r`~% qra✓e,l T~~
- Sc~1{freck c_ V.,1 ~1,e_{.5
$0 - 85' pj¢ckroc k_
=
_
_
r
_ —_ t0 -_
—_
-~=
>b-, - _
~
_
_
-
—
_
~
!
- ~/cr.l 1 ~q~} 3,-ci grerv.
11V- V o ICJE --,...c.. a1 r CJ,.4s -lb S w~ 4e
jr,--45
,
_
•° _ —
w _
~
=A~ A ° - o! d So 31z rio V0.5"
2S—
-
/ ~ / _
~ OL
•0 —
_ —
~
-
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 1-1- 76- 43
Property/Area 0 5 -TAKE IJ OJTE_ Date(s) ( s (. Township
Claim No Drilling Co Sker,Joocl
Location Bit No (p, Depth to bedrock
Logged by 0. W. Total depth 43 ' Sampler K Sample screening (U McsLN
Remarks -
M. Ft. a~~ SAMPLE PLE GRAINS DESCRIPTIVE LOG ANALYTICAL
FL(") AS G,, R~
_ _ _
^ A n n _ ' 4_...„
O — S' "'"',„S
- -. ~ . S'_ Î2 1 14 C. 1-4. .5 1-r- i KG C. la
J - ~r J w- 4-o b1.-\.i5h ire -i
' Z 'iJLi bS -s;
kV7J c l°`j
- - ' Î2
1
- IS '
54.,.,dy Srque.( 44 ( I ?
- >o--
10- =- = 9 g - 73' BedroLE.
- ,-,1--; i< ,,..„..4 —
~o _ - k-;-%1 GL...eS < 5 ,h (10ie
_ _ —= 42 "
_ - ~ a; -.~ ~ Lc Go~...e ~ _ ao - I r r ~. e.. qce —
J -j t~.t+gcew5~ J '
Ioek,,,,..,~
_ sa _----
20-
=-
- _'6V .' : 01 f eea.
r e ~ 9' ~oS 37.1 Wo S3 D•B
-_ .p - ` 2 DZ 25- - 9
` -
_ _ r v - p3 IRb[. ,jpp 720 13io Sc) o.i
t { c r
!0 — 1
~ l =
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole - ~9-
Property /Area C V ~ Date(s) ~ .l+JE cyA f Rb
Township
Claim No. Drilling Co 1-611, SL.ev„o.cp Location Bit No CB 6ZA Q4
Depth to bedrock S'-t- ' Logged by NJ- 0.vJ. Total depth 59' Sampler k . Sample screening 10 n>teS L.
Remarks tJ o
M. Ft. GRAPHIC SAOG
MPLE GRAA~IIâ DESCRIPTIVE LOG
ANALYT ICAL
A.(M6) A~ " C. 2. q~
~ - - ^^ - n ' ~~a, ' --w.s
- -
= .r ~ . 8'- Sif - Îgc.4.5+rih.e cic4:i
- 5 ; t k--1 6 ,,,ar d5 h..sc. ~
w; Ft. .~...,,,_ ~ S— 5c•..VVCred ,pe_bb(eS _
- >eo=
- - ' Si- S9 ' b tzc4 roc. l-
- ; - ;....~. ~o,~.f d~o~:,~. ~ __- ~
_- _ ~—
io— _ . - .4Co.--- ;-..1 ~err- •+qPC
- - ~ 4 51,
- • ~
— I..... ;.,or dss. (A--1)
tcµ - 5-.9,
„~_ -
ü— _
_
•
20— - _
,0_ ~ ~ =
~ - _ .
25 — - ~
-
30— _ ~—
_ -
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole \k-g‘ - 4s
J 04.4 Date(s) ( 8 6 Property/Area
Township
No. Claim Drilling Co.
Location Bit No C- j2 1 (7 0 I-f- Depth to bedrock ►► l'
f.1i 0.vJ. Total depth /22 Logged by
A.k Sample screening /0 *51-s Sampler
Remarks
M. Ft. LOG No. Au GRAPHICSAMPLEGRAINS
ANALYTICAL DESCRIPTIVE LOG da(AP6) AS " Cu. 2,
_
_
5 _.
-
- io—
-
~—
80—
_
25 --
-
ao—
: _
..\ A
n^
-
:
=
-
~ 0 --$ - 144.4,.....5Of~10.~.t-S
3 - 40 ' l4cK5i-rir►e clay L ~!
S` '~i q,-0,4".01 16-I -.5;
- ~-`"rlo ► ?ell')k S
iji4 ^ 4- ~~, - [C‘tS 41"+rLC 5; if
SS- g5' -
l u CKs E, ;.►.e, ct.) - (is)- 5: ‘V~ c~ j
pabbles ar•oyv~ $6 ,
itr-- I 1 sy,►.,4af •Jqrgye.`
( -(1°S-- Hi) 1--, II ere
- hice 9~au.l r Glg$FS o 1/41e✓ 1.,51- S ~ f e
11 -7 - 122 ' 6 eeko c. ti
w — ~ '
_
so_
-,-
m _ _
-_
-_-: —
—
_
w =
-
s0 ~
_ '
,.,re..-1ck~ ,,Ik' 'i'C.
T 1 ~r ►•~ G~C, iV~
`
~)
Ptv.
J4J q~ii...5 Cp /p./j
1J V
--
To — _
_
~_ _
-
yiF I2& 66 a~ =:ô' -.'
D:-
I~ ;' ~i b
546t. 2So
„ ~ 01.
Ire'
~ ~_f
.. ~_
~ .23 S) at) E~ sl
_ G.d
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 14- A6- 4-5-7
N. Ft. GRAPHIC LOG
SAMPLE Na
GRAINS Au DESCRIPTIVE LOG
• ANALYTICAL
A4(PPE) AS Ck 2,. A9
-
_ a6 —
-
_
-
.o- -
_
.5-
_ -'
_
_
eo —
as—
-
_
too — =
f'-'- vo : 0:3 C3
-ip
_•
_.
- _
v,~ -
._~ .: l' - " (
: pi~ - 1
0 19S 568 10e It 0.`I
_. r -
. :, ' 7 03,,- d 24I S 3,3.2 110 410 0.`if -1 ~
-' / ~ ~
06 .
_ ~
._
~
'
-,_
_
50 -
ss —
_ _
~~ - - _ _
_ No —
_ - ■0~
......
~=
...
- ~o :
-
-
SO —
~ ^
]
soo—
r
+ ..
=
520 —
-
-
"' -
_
210
~ -]
~
7 , ~ ~
..]
] .
:
ï
~
~
:
J
; _
-
:
;
-
.J
-
5.5 . (o Mel!,
Depth to bedrock
Total depth
Sample screening
Date(s)
Drilling Co.
Bit No
.~~IJE 1531-D
kl ect {4, 4 Sb.Pr,,,loocâ
CR h-7 g o s'
Property/Area—~1~t~S~KE
Township
Claim No
L(flOt-oovJ Location 2fiSos
Logged by
Sampler
SP. R. A.K.
if jr MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole u- 86- 4-G,
Remarks r ; :,..;-51-. Î : O o
Ft. GRAPHIC
LOG SAMPLE
No. GRAINS M.
ANALYT ICAL
Au DESCRIPTIVE LOG kW A; " Cu 2~
-
-
-
_
~—
- zo —
~
_
-
25—
m—
_ - /1 /4n A
Z
J
, ~ -3 I1-,..,«-•6,,5 O,-jq•ti.t.cs
bark, .1-. 1~1~~ J°rG~1
(gc,t5 ~ri+ te C IA~
WC-1 ÇIoC%AIgk-d
SD ..- SZ ' I~ ~{tE rogenCo ks 5.4 41
Sro.J~c 1 -1-i 11 ! -`Sy,~Q
.
~~ 4. Yo~ 1
Ciec~(IS ~. - P~ ~ ,......k. .1.., ..-.~. i-
vo IC av~iC.
5-2,- SS ' g edroLk
_
-
3-SQ, _-
°—
10—
=
_
- —
_ -
—
so-
>f0—
-
_._.
.
- 1
—1-
- so , v ~ b _ oZ ~ i~k gyyree
-r}. d w~i ~G
Str r - kg. L ►~.;Jti2~1 ~-.~. Vo ~BU Strt 330 Ti l.a
-% : 03
.
so- _
-_
~
~ ~ -
,0 _
~0—
_ i° ~
-1'
- ~
-
` : `
_
_ '
-
- ~
-- +c~ pi
— re - ► 0 ly so~k 'd ,,.>:
4 I r bh ~kT
— 4,4(4_ / Upy) I r LO j L . row's.- ,
1) T c
~~ c ~rt -C; 11
I9 - +'~j S,,L~t.sdra I ir..~..„5
- L
....:~..a^' CA/
Z bo~wk ~~,rs
- SS ~
; %n 6,251d0
//Tari< ovulez -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 1- t - 47
Date(s)
Drilling Co
Bit No
~urJE Il tg.‘,
!-eaft, ¢ Si.ervJood CE 4, 7R 0<-
Property /Area
Township
Claim No.
Location
oJT
Depth to bedrock
Total depth
Sample screening
57' /Q ~/lesh
Logged by
Sampler
.SP R. A. K.
M. Ft. GRAPHE
LOG SAAIPLE
No. GRAINS
Au
ANALYTICAL DESCRIPTIVE LOG /I.(") AS C.
-
~
s —
-
E
ici—
°—
_
20 —
- —
- 25—
_ _
50 —
_^ _
^ ^ ^
~~
o
D - 4 ' r1 `~ /0(7?""- 5t /0(7?""- 5
it--~ - ~Ir k ><a l,~l,E,r~
(k►<-iI f toC IA fc( fed ho ftylea415
,9«J `iai
lit so , ~4Ck5i~;,~ 5~'~ Sa-.d
50- 3-2' ~e.~Cra9ehtALtS Sa~J J`"~
y q 1 hi/
— 907. volca~~'c - —4z. -4.
r. ~r.~.h~c, I. F.
SZ -57' ~r0c k .
a _—
m
_
- =
~ afi
-
so=
_ —^
~ -
_
` - W — ~ 4 1, ~ten Serr i c,~i 2ed
andes.le 1h.q54,,If — r oss'1b~ ff [[``~~
55 .332 .~.~ 0 d !S S94 36o iL 0.8
.
60 - p ~m - o!
~ = GZ
~
--
~ b -
_
- —
_
_ _
-
_
= om
_
-
~
:
- -
~ d
~ ~ `*TI~ICEoys
r-1~~,, 1,.1 sc.“t~.~F d 6 7
` ;~ 6.4- i~I° y Pg.sle
."- yQpcC.~S 4-t. 6.e_ ck,lo,:E-i~
%(~wsfase~
(S~ / ° ~~e~ ~~Qrf~ Je,' ......6(-5 (! -z w. _, ,~ i 4
ENI -511
i~ - ha~ r r die jc w4s~ 11c, je
4-1:, p-ody ce. b!q wy5l%
.s/p,--I
- g .q-Q Remarks
112 .5 // 7'
Depth to bedrock
Total depth
Sample screening
Property/Area 14)hEILL/23.
Township
Claim No.
t- 60 -loo r.I Location
Remarks .Slar - 9: IS-
/ foo iJ
Logged by
Sampler
S ~ R.
01. K.
JkJtJE ll /84
ijecdt, d. sivrwood rgt,7Ras
Date(s)
Drilling Co
Bit No.
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole g- R6 - 48
1:0 2
M. Ft. GRAPHIC SAMPLE GRAINS ANALYTiCAL DESCRIPTIVE LOG A.(~? Ph Cu. R., 149
_ _
_
-
- io —
_
~ -
r
_
!0— -
- 25—
'
"•-
= ..
n 1 ..
n ~ - ~
- - _
D -s ' F/,A.,..,t5 /07...4(6-
`S 914
Zar-k 6l, 1.,} 3rey
. 9
r q~
i
1
'~o ~~IJ
ChtD~{S - kle, ii t IOCMt
1Q-~S b.l~ * ~l 'oC~1.T~ 1R1 kJ • {ti de~
9/- 112 Ve,y ~~ 9r c.wei I i- II /. — Pre+•i. N1 f ~a .-ut pc... G +m ÎC .
go- 47D2 - 5-z ....~~d
J
q„~,,~wgC(ces
' ^'....+hAP ifd1 ...il-iGs
- c Iys4S .s 4.61;11kigr• 4D ~,,1 r~,~
bI a - C96- 7(0- dq.~. iC~ ~1"5,,i11
~ .,.iâer
103
'1
) -we.il 1 'hdyrq~ Or:~j C~~
- (%1! /
s
SI~ ~{`,~ rK
J S~ or., n:iGle . ~+S~~
J /Z '}l2 .s ~ - VG.i g 1G ' Ce5 P3e 54.4
/12.1- 117 3e.d ro c k.
;
'
.. p-
S
- =
m_,
_
~ - -
40 ...
=
-
~
-
_
~
,- _
•
- - _ _
_
to _
~.
- =
~ _ _ _ _
•~ _
_ ~
—
- _
—
- dg. ~ 3.,.7 b(~k , 4re,i I(.~k - 4044 — —
ylc,..:c l
- z-3,,-- tz veil.-..S-
: O' -
- 3 ` ~~: d~ q~4
e
014•2 Z 7 ()i)feiak{ 1-. e~ktr fl v ei ~ -C â a (far5 h ¢ IhrcJcf I 0P• l i
Q.II.
336 3i'13 D.
-
~.~ S.{:Clow$ —
(~
~
~. g°
2„,- k4 u é ,.~~a. ~ 5,~~1 110,,..3.s.---P(e30
.e ' Eoi/ f!70
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 4- 9k9 -fit
M. GRAPHIC
C SAINa1.E ~NS
Fi.
DESCRIPTIVE LOG ANALYTICAL
AfMS) 14S (,. R.,., 43
_ lm -:
_ . y. 't.' 45—g.:
`" -:: °'. 3 ô gs 386 /.2c, .2y 1.0
_ _ _ ~ O
1
L. p ,U,5",U,5".Zî`{ 136 3[. Oh
_ - T.° D
- 0$ O 6s l000 44.0 l9 Go !fo
: ~.:A. P' - Ot5, D AS. 350 HO • ?I ab _
18- / 1
07
1i0~ -
ISO ~ a, .
-
40.a.
;
w0 - ~-
se — ~ ~
1110 a _. _
,
-
-
- _-
,
1.0—
SO ...a =
RO ... -
66 —
_
N0 a ~
,
_ 1
-
_ a ,
_
_
ISO -= » -
.0 - = 200— -
,
~
_
a.~ -
-:a ..: :
• O -a. -
= :
-
- -
- ~ ~ = ~
J - -
57
ID tYs I-,
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H-$6-47
Ft. GRAPHIC LaG
SAMPLE No. Au
GRAINS ~ ? ANALYT ICAL DESCRIPTIVE LOG AtaUIôL As CL` 2
- - il
~ n
_
_
- r
_
0-5' ~y--•Ks I Orzq '"cs
5-Sb i bark 1-4) I iJkir ,Drej
b:3 bev3en.tou,S ‘qCWsrir.G
CkJ - .,Je. II I l oc.,~tkle,~ 1.4 le ss
so~:F~,.d~
5` - 5 / . I 5.,..-41 i re..„el h (( ~~.
~4. . la .......rit_ YOiCgr.iL
- s 4.scto-v34.4.4r 4D 41r•y4...tgr
.5-7 - 6 2.' BedroC.h ----.---_
~
'.
0—
--
_ . ~—-
_ —:
- - 10-
_ _ ~
am
- =
-
—
- ~sà l ( ~ Ardesil>` 1- 2 c._._ UCdt T,.ariE
Car~p„~~ dG_...~
— +rgCE. C~) V. ç J 9 . 5g-~6~~ (
C 6+r6es
... C klOr i ~i{C,d
EN - (02'
_
oi3OL 1 A&. ~ ~1(1P+~11 3F ► 2m GS
_ w J ~~ 03
• ^
,O ~
SO~
_ 100'".:
_ .
_ :
•O_
a
-
-
s
10
iti
20
25
30
Property/Area rr:L- Date(s)
Township
No. Claim Drilling Co.
Location L. (4 + on ~^ ) Bit No.
y + tJ Depth to bedrock
•? R. Total depth Logged by
Sampler Sample screening
Remarks
('TOs
M.
Jr/E. $(:'
1le4--1-. d S►•,e..r.,.,,oQ.d
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-36-.c
Property /Area
Township
~aM~S?fj KE /~IOJ7EL Date(s) Jyr.1E II~86
Claim No. Drilling Co H cs1 tt. G' .S ker,,, l ooci Location L ,6 o too I.J Bit No cRti? Ao~
447A" ^) Depth to bedrock 4,0 ' Logged by
Sampler
P. R. Total depth 6s' A. K. Sample screening 10 Nle.s k
Remarks Sf of 3:117 ~ ttIc.,..itylir.q is Q- [o..d.v,cfor F/iN5~• S,bo
M. Ft. GRAPHIC SAMPLE No.
GRAINS Ay DESCRIPTIVE LOG
ANALYTICAL ;UPC AI - Ca „
~
_ _
T
—
io —
-
-
to —
:>s—
30 .--
-
'
/. n t‘
-
—
- -
0' if' kill s'-'14.5 /O,1:7r‘lcs
4-,51.' Dark #0 I~•L/ qk) ,5,- Lei
~ i~ .J
- k° , b~e~~s W ~il eI°``~~ 5(..-5S' - v2r.{ T h~ Sq~
59 60 ' - ~k,.o 9e"""'ç5 S..►` ~
9~v~ }; 11 — Jery Sa-~si•
.J - / s~bq ~ yiqr io S,+ 51-0y....1124 c kS{S
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1:546--I Property/Area ~a ME57~Fkr✓ f ( I Date(s) ~tI t.IE lt 0 Township
Claim No. Drilling Co ~-ea t S er wce c~
Location L r,O 4-oc 4 Bit No C.138 o e -E-1 6 f-S-0 Depth to bedrock 8I '
Logged by Total depth g
Sampler q•~. Sample screening /0 Mezl \
Remarks 5fttri. F,.;t3►, - (= f-c.
M. Ft. GRAPHIC SAMPLE GRAINS ANALYTICAL DESCRIPTIVE LOG fli.L(iva AS ' Ca >;,n AS
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole Ii-$6-3-.
Remarks
M. Ft. GRAPHE LoG SAMPLE GRANS
DESCRIPTIVE LOG ANALYT ICAL
LOPS) As Cu ~_
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Township
Claim No.
Location L too 4-00 vJ
SfiSO ti1
Logged by
Sampler
Date(s) JJ IJE 12 t86
Bit No. C6(,-ig01. Depth to bedrock
Total depth 75 1
71'
10 tvlo_sk
Depth to bedrock
Total depth
Sample screening
Remarks - 2:30
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole 4-1-5i6 -53
M. Ft. GRAPHE LOG
SAMPLE No. !w
GRAINS ANALYT DESCRIPTIVE LOG
ICAL
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Claim No.
Location L.. (a O 4-oow
~J r.lE i2 IBb
Drilling Co 11e.A{t 4 .Sker~ooc+
Bit No. C.S6 Ofo
Date(s)
/o tSo 'NI
Logged by
Sampler
.TP Q.
~.k
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole - -5
Property/Area HOr ESTiiKè= /JOJTEL_ Date(s) . ) cJNM. ►a, '$(~
Township
Claim No Drilling Co S%1Crh1coci
Location r 58 f-oa v,J Bit No CAf.'Î$nh 4 1-2-5 rJ Depth to bedrock
Total depth
(ea' Logged by .37 k .
/ ,r Sampler R. k . Sample screening /0 4Sl-,
Remarks
M. Ft. GRAPHIC LOG
SAMPLE Na
GRAINS Au DESCRIPTIVE LOG ANALYTICAL (~ ~
O QS - Cu. 2.‘
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole q- S(0 - 5-5
Property/Area ~/✓IFST1}KE /JoUTEL Date(s) f..1 E. ► Z lSb Township
Claim No. Drilling Co e SI1ert..looci Location L C) 4-Do ►J Bit No. C 5Z 07
4- +-SOS Depth to bedrock
Total depth
93 Logged by s. P, ~. 97 Sampler A. k Sample screening to Ai1e51,
Remarks
M. ft. GRAPHIC LOG
SAMPLE Au Na DESCRIPTIVE
GRAINS W DESCRIPTIVE LOG
ANALYTICAL l~a(/•Q/ As _ C. .a.,
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-q~ ~.Ie Îi ;«.s~rq~d Jr1~ C~
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole FI-2 -S'
Property /Area ~r Ti✓C~ Date(s) tJF IZ 1R~
Township
Claim No. Drilling Co Heck(- St--err,oco
Location 0 +00 u1 Bit No. C.g 6-r8 b7
(fl 4-SOS Depth to bedrock
Logged by ~~ ~. Total depth 12_0 ' Sampler A. k . Sample screening /0 Met% Remarks r} 3: 3t }t5111._ 20 ►k .r_,Nesi- ~~ ri rçH,q
4.50 ~
M. Ft. GRAPHIC L06
SAMPLE No.
GRAINS Au DESCRIPTIVE 106
ANALYT ICAL /4.4.04,6) AS C44. ~-
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144812 . fIk¢.
130 !$ 2S 23
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole -86 - cc,
M. Ft. GRARAC
LOG SAMPLE
Na DRAINS
Au DESCRIPTIVE LOG ANALYTICAL
p„ (ppg) AS G. EA. Aj Km
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1--56 -37 Property /Area ~1-tc J E5TgK.E i~ J Tt, Datels) JutJE ~R(r
Township
Claim No. Drilling Co. dectf(-: é •Sker,,,l0a4
Location L- .36 4-o0 Bit No c~6 G, —1 +-50.5 Depth to bedrock ize
Logged by 0- P. Total depth 12s '
Sampler ~}.k. Sample screening ID Most-,
Remarks Ska•~ . Il'lo Co nôa.i r fh r L4uVel-.
M. Fr. GRAPHIC S~~LEG~tNS DESCRIPTIVE LOG •NALYTtCML
A..(A9S) As • ~• .e.%
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 1i- g6 's7
M. ft. GRAPHIC LAG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL 44.4.0P6) A} at. 4-, t
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole
Property /Area
Township
o t/ Datels) J J NE 13 1 g6
Claim No. Drilling Co ikci7r` ar0( .)Î'brh/Ood
Location L. f-rl n ~ I Bit No. C!3 (.77 90
gfnnS Depth to bedrock
Logged by Total depth 1It0
Sampler A. K. Sample screening IC' W1# Sk
Remarks s {titri - 2:So if J 2r~ Poor-1y dCJ¢-%peel Ft-4,5k 11-..q.0 no %'I(- CIcw 6~2dre,r• k
M. Ft. GRAPHICSAOG
N t.E~~ DESCRIPTIVF LOG ANALYTICAI
A~.1/~a~ Az a. ,E.„ AS
-
-
s~
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io—
-
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,
28 —
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PS-- IM' 1-g".-‘ery ~+~ S:Ir s....-.4 (l4ta ►-►e~ sf+-
~s....-.4
107o Isoit({a Pf-uies
S4brOH..,Aittl
• r3S-ly,o' _ Bedrock
- 1~q1,1 Qrey ✓fejwv.ciCe-/Sil~
_ ve-r.l 5`4 ~~.~~ .c s , !
- 1,4 C ~‘ -`•; , rotk i•'‘ r prs ~
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N — g4-SA
M. FI. GRAPHIC
LOG SAMPLE
No GRAII~
Au DESCRIPTIVE LOG ANALYTICAL
Am (it) AS Cc. Xm
—
1
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56 — — —
KO ... ' • ,
_ .
_ 1710 — o r D No 41~ 200 6Y o.r .°_ —0). -
_ ,. = eZ - . . -
J/~ 03
No _ , -
48— ~ ] `
_ ~° ~ ]
~
ao—
610-
~
~ -+ ~ . • ,k
]
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r _ _
6a fi°~ i
_ _0.0 —
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60 —- zoo—
_ - , y
'7 7
it —
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_ : ~
Remarks S{ar} - 8:30 F - Iota°
f lo :00 Ft-d~4..1:~ l.ne sft :}
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 14-0- S7
M. F t. GRAPHIC LOG
SAMPLE No.
GRAINS Au
ANALYTICAL DESCRIPTIVE LOG ;.. ;l. A 4..
-
-
-
io—
~—
~
20 —
_
25 --
30 --"`
_,‘ -
^f ~ „ •
U q
0 - if» 4.t....•. D rytr.ics
I{.- (/o ' Dçrk •~-0 Ir9t.~ G rey
./ ~J ~,0.,..05eirve.04-‘5 I4C-45 k chc.
C 10
- well t' (0 C MA,~Kf , ~ lG53 Sc. w i{(., de p111
~ b0 -63 - ~r~-1 ~~G Sq-~4
b3 - (oq.s d-eieroe►.►to~►s sa-.ci Qwwel Jd J J 1-iii
P~~~
C.
-.~cy 4. it ~~,
— -5...6" .."......tar- 61 r o y r,p~ C ~ 6 - h.,,......- JS.abro,...i.d,d jr4r,; I•ic.,s -
~ ( /o ! i-IN.-Ne .Fr ~+c e.~s ? ?
I _
09 ~ / ~ s °l1 7
l (oâ.~f (t,
69•S - 75"' 13edrock
2W- f •24 lb 66 O•$
a =
b—
•
=
=
- ol _
-
_ --
-
~,
_-
bo=
.
— ~ ~
!
u
~
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- -
=
i
_ ~'!
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L~l o 421 192 `19 1..2 ~7~. Y~ - Oz ,d~ 3aE2.
• _ so —
~
~
~
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~
-
~
-
-
-
J
-- Jr!"1'jilt 9rcer, ~~ serriu A-zed
felt. Va ( reç..« F05511211 ~~TRCt!o5j
ZO-
l%> ~7 44F+r-~ Cc.rOowR K►^S
` l/ ~~rs 1E ~Je(. ~5drCi~7'eq
(7T. S) ir•, i✓1or 7...... a .-1-7 Ca r~ ~joh g{C.. L~
Property/Area
Township
Claim No
L S t-o o us-1
13 -tpo5 S R.
-
-..1%1NiE It+ `aL
l-eafk fi 51•-.e-10.1004
cB 6-119(r Depth to bedrock
Total depth
Sample screening
Location
Logged by
Sampler
Drilling Co
Bit No
Date(s)
/0 t4k
_~on~►E5T.4KE i.SOJTEi=
â4 .S' i
Drilling Co. 4e4ikd 5herb.3oo4
tü MesL, Sample screening
Claim No
Location L 2J Wo Ns-) t3roo
Logged by R .
Sampler P . k •
Date(s) Property/Area
Township
c 7-191
Depth to bedrock
Total depth
~o~frSTA- -~~_TEL
Bit No 5I ,
51'
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 14- g' - (DO
s{nr - 10•44.
Fi-,.;5L- 11:33 Remarks
M. F GRAPHIC ANALYTICAL
DESCRIPTIVE LOG Au( s Cu Es'
- -
-
-
- _
^
20—
,
_
-
ao-
- - : -
^ " n n :
_ a -~,
........./ S j )O rjo.k.îcS
~^~ I D ark, 10 1. - qrej
i1o~o9tneo~
(~►
ia.çcasfrihe t ID
- L.se-11 Floc.,.~eo~ ba.E IeSS../
.S. w , N.` dépi1,
7° -Sr Ikkrcge+tieoWs s+~ grq~
14 J J
+ ed. ;1.f. lb.ltit'1t VolC47i;rs 70 -.907.
`"i b 262 3,~y, ,~~'s,(4sf~ll~ ~r gi s .
cI9S~ 9ene~.!(~ -54,".b,,~. it. q ,~/ar.
~
SI-57' Bedrock_
= ~ " -
5—
= _--,-
=
— io—
>D-,
•~ _ _
_-
— '.~,p A-r4~ _r~r of F~se, 5 S 51oa !Go 60 02
-//
-~~ oZ
28 —-
_ ~
_
_
_
~ so _
b _
_
_ .. - ...
7 .
re- -
_ _
~
'
-
— ~arL tr~, biq~ ~~{
- .5 tar+~.
s; 11- sbl•.e - (
5 1 '1 {{
1-44541 9
1
„kar7t JC.Ih
1,4 c~`'"+rhe~d ~eÂrOC% i.~p .1,55k
(S3 ) a6 `~`~4r~ç a
- . ~.i►~:.
(1b~o~tr.GoyS dkr(c. ' ~
s~L.:s 6x f~,.F~~ 15-it S)- r(-1.51,iIR~7! .0~
6.1.- ~ ICM 1-6'(..k...
-(S6 9 4.1.`"•• blade ~-,a.e ar3,.1t,i,'c s I,y~.l (y »~~~~;c
.eoj1 -57'
qtie,_,pkrj ib ~~t' rC✓~d~.r~f skirl - I!'te - Iz- y~
Remarks
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 11-26- 61
HoME5T4ks 1Jo0 TEL
L foo ~l
„Li 13c_-- IL{- (st,,
1-t ¢ltti-, -,er ,1ooC1
Property /Area
Township
Location
Date(s)
Claim No.
Logged by
Sampler
1~ t z,s S S.Q. R.
K •
Depth to bedrock
Total depth
Sample screening
7b'
/0 Mete,
M. Ft. GRAPHIC S4IAPLE LOG No.
GRAINS Au
ANALYTICAL DESCRIPTIVE LOG d..iPR6) t`~ As Ck Z.. AJ ;
_
I
,o—
-
,5— _
- _
-
to—
-
-
26 —'
70 —
A ^ .
-
0 -3' ~~,,A.4s t or~1.,Fcs
3 - $6 ~ -Day"-Day"k Ta i .-314T q re-i_ ✓ J J
;7o^no'e.,co~ la c(45 J
frire cJ4q
S6- b+~ d~~ h1~ S!
j L ~r
'I- ~
1.L
9 ✓ `4Ly51ri
644. /(!(~ asSer l~ ~bâitj
it -66' ltcielo9e.►tovs 5^~' cwe.! J ~il
- ~es ~ p~s,~ ~°~~i: ~~~
„4.,,„..,,,.....4.~o~
lob_ 70' Bedrock.
~^ L
:
_ a-
'— — -
_ -
>D=
=
_ ~-
- so~
- ;
,
- z-----
_
- Ôgrk.. grty Soir - 4rgrl~i><C. •J ~J `",c4gfptiG
- ~ ver•, So~ - eaSJ " {z, drill
- 41 i ~./ S~
9►~ f (^+S~SE Cr+.4w~les /, i1 }7~~5
- Carbo•NAu04-5 -,..4.4sfahe.- po553k eYPV.., 411'001 eF 0,-4,6°r
- -ihor- a.-.4 of ro ck ~ k ~
pro J1,t~.
F..d~ - 70'
--
.1z - •Z52 124 ~ISr al _
so =
:
:••,. - s•
' . E:p D ; ~ '
• ~ _ - p~
: °Z _ .,
C)
~/ °3 :
~ so 4
]
1
:
-]
~
—
1
-
r r
-
L
'
Drilling Co.
Bit No
Sample screening +k, MGTH
Property /Area
Township
Claim No
1. ~l•caLJ /.SiOC~i
Date(s) Jo,;—
kc~lA1 fSrrr+.'c.rzrS
Cr; 6TO7 Location
Drilling Co
Bit No
Remarks
Depth to bedrock
Total depth • Logged by
Sampler
lIL+•k snit(' /34,a Z
31`
~• ilk
fi.4)16,,
f/I\\ MPH.
MPH Consulting Limited
OVERBU RDEN DRILL LOG Hole fl- R
fm:,s,r l ;s
Ft. IGRAPtiic
LOG SRAM ~w+T
Mani M0.
DESCRIPTIVE LOG ANALYTICAL
A.( PP6) AS Ca in ~
_ _
[~ ), ,k -
:
oiA
Q - s" - MAO
.5-' - .a ' - Gr~y-62~.,. ►144 a)-449cT cRcusnE,ti atiy -oak/ SorarE cJ. al lime.
,t j`• 3[ .- CClbtity 7lcC L, »H h1414.0X !r- f s~ y â[e i
- CLAUS A~6wk tv i 5.,..S-A,6t,e~ Am.. ~c'-
I+I. LaG6wC5 ,160.+44-+u, Sais
1J,T4 Pti,46.. eü.447K5, 1. prxcrluCS L.5. 31 IC7kOCr(:
l4 ,?uSry 122 C(cy S2 M[Srasé S1LTS~ w~
ueNs *Mfg as-i.v CGR. 1.0 TIGaz,uzSS 41%6
CS-- se,r~
ole(wksr
2 Sop.k ,liai ( /....4.) AûSKCMtiluS LRyc+QS A.b...+ A
/
NUNo; 41.4410.i4.4. Or ilirA~
~ 3S / 4 Gj W .
(, 3Ar+L'cE co -4 IS 1.49I-do,n neo,•r tr' lb 3s' .
- ~iLy
-
-
1Sa 35. !9Y 40 0.
,t
_ so—
-
~
-
;
_
-
_ - 1A8(•
-
so—
_ _ ~
~= Go ' ~4 ~ = o or zrn 34.1. Soo 34_ a2
-~1//~ . 6,Z _
., =
— ~ ..
so =
— GO - 0
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:
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90 -E
1
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=
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-
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=
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.
^
.
- -
Property/Area l/uni_sm/ Township
Claim No.
Location L F+2Ss
Dote(s)
Drilling Co.
Bit No
%,. ti/K.,
Depth to bedrock 15'7 '
Total depth kl••S Sample screening a /U
Remorks
C7611 .7:00
Logged by
Sampler
bulk_-~ tt•l»ty
&s/
ll:771W 4- 5N441kÀ
C6 4R97
!!ï\\
MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 11-é'6 43
1;/..4V( .
Ft. GRL~ K GRAIN str~ 6 DESCRIPTIVE LOG ANALYTICAL
Af4~ ~'
AS cut y..71A 5
- it
: / n = ' G -5 hi,MuS
- to—
1 _
— 20 a
J _ .
!C— —
: S `- 52 ' -Cu(t Y-c"sKti,a,cl Hqoit, tt,»VI1tI LACogiZotc- CalLY
—
—
- hiuUd ebit (tA GJ t r?( A'l'ly ,p
ao —
so—
w —
.
? p
-
~
~ -
cil '" 120' - /1".•.: d,ir=dY fiuve-) 61.4 (44 CuT441►( wait
-< ,C • - ,/0.14- iii,t4Se6 k?zcc S (GLhvv ( CS , t[.rfimwc4/
. •• - Fi,C Fi4ST SC (rer tk,T <xîhL•u; 4.:v
"iv.— ~TIîi.CLY f .0.43
MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-s/-63(2)
Ft. GRAPHIC
LOG SRAM COUNT
SAMPLE Ro. DESCRIPTIVE LOG
ANALYTICAL
11u(ARS) /15 Cu ~~ Ad
Ip - -
120
-... --.
. -.
~ .
. -
-
-
.
!z0 " 153" / -!"C~LY 71LC 4/iT11 /shoo( 0F ~4,~$PpCLNkT(ty
901„ F .Yv~.IU KJiI% 4.4/o7n (my
- OASTS S.)a-4A6wtx 4..1 ,'1t7Z`‘o6cxcaiS
L/A.IiL i4-1' l,,r~c 40LLga.jC 5 lbï~t a/f ~ . r 5 O,~tv.,.~`
N5-L55 ' Mal 01- '-10 MRJ~irRt
15S'15q ' 6ca) C[.f/-(fCH 643AL Pa ran! 4.6c0.01?6
b$ IOS
S E~~
- _ _ o
_
lao —
= -
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_. 7
RO-,
-
_ ,
L L ,
a ~
;
1 ~ --
. ,
n
~ ~ - 6
° _
- - : 0 0 ~
~ NC 2S-) Ci oS
_ 0 z
- O
-
371 21.o 9C 0:7 :
- O
: _
ay I15 224 .ZNo Sy or
ILS" 11.1 132 Cy a3 .
-,
~
6 ~
-
- - n ~
OS
-1cé \r,/,,` -1 O hC: ŸS IGy C2 0.z.
-~
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no ...
~
~
:
05 -=
~
: ~ eoo— : :
—1
!10 ~ -
; --:.1
-.1
o-
so i 0 7- atilié #7460Z-75 kc26404,,t7aY 4 eic'Y
` .
'>_
..
-
SC !` //'tuD,Ç/ZMC
,
l57 &diiLUl. Gêry, &ro+eY r. Gei,.I4 lAxrikllc 014
19:r,rc.4-tr sâ-r -1 Cary etzcs raeoict .11,;( TC' Q/ r Ataiuie
161' - rleaestt PIuc~t hr,tlacP -', tiPArinlaurS
I/. /4461.1•Ere 4./b dlovlOGduectis- ,
(6(.5 ' C 0
H. - Mow Ta rl f. 10r.cl.su do- Wt.(
l/i%c-" MMrlURL ic~CZS
=
.: .
■o L-:J
:z -
-
~ - 7 -
j
~
~
.:
~
7
: ~
7
~
] 1 : , -
_
---
Property/Area /F6,riF5 575-ICE /.1bUTEL
Township
Claim No.
L 2o foo„ J
Date(s) _,Oae. 141 S6
{~CLITh ~ SLarW ooq
CB1,77 47 Location
Drilling Co.
Bit No
Depth to bedrock
Total depth
Sample screening 10 MpsL, Logged by
Sampler
.T.P R•
9rzss 76 '
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 11-5& - 6*-
Remarks Skrr1- - µ: o 4.
M. GRAPHE
LOG SAMPLE
No. GRAM
Ft.
Av DESCRIPTIVE LOG 6- 2"'_
ANALYTICAL
A~.(PPa~ AS
_ -
_
_
- -
- io—
~
-
m —
25—
= n q
n 1% ;
-
b' µ ,,LL ~1`"`"-~3 GiiA•,.IGs
4- 4.5' Dwrlc 11,11)14jr ~o ~ J •1o4lwr.
Cgy Jy
- L.-re ll çle cw lnkâ L.,1-less so
wi ~ ôeP}~,
LIS---10' . utry 1-i ,e • S ;( 1-1 Sg,A
70 - 7b • ~r
~f~
,~ 5o
Î1 g. r~.rc-i 1411
- . ~. 7 ~ r ~tt1G.• volc. clas~
u--:-.0, a• r q r. : tiCS q..~ ~;~~•J
76 - g7' SeslrpGk
- jar 9feer. 5. fi „1_ !~. G,
Vol'cAHiG,. .
— c,~~
~.14 - s.Fi ,~~~.: FlQke3
1-10 ,..1e51.,
-(4704-‘ r'rye r n ~o..r(Z vC~i.w' l- 2 C•...
- ~r4u (P%
~ ~
"0-% •••10f. Car~atf_ 45Soc.'a ~ ~w1{L+ Pe (, _ /~
4G•-,/Q Sti rl-olccs
Ea4! - Sa'
100-
r r
zD=
-ti=
1 ,3 _
-
_ --
=
so ~
-
_
—
_
—'
40 ~
-: = -
-
..
_ fD—•.
•
;•.
u - : al ~ ~âo 5N4 14% L6 p~ : o~. n 9S t.722 3i~ 94 Oa 03
10 —
-
....
~^
]
= -
_
Location L /8 {-D o v.J
Property/Area qo ESTAkF /JouTEL
Township
Claim No.
J~ eJE 04- I86
Drilling Co. 14eaf(-.4 Sker.ticioc1
Date(s)
Depth to bedrock
Total depth
Sample screening
g9' /0 Most-.
P E A. k
(-6477 q7 /0 f S
Bit No.
Logged by
Sampler
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole Fl- 'é - 6s—
Remarks S¢rri - 5":1~
M. Ft. LOG GRAPHICS~LE
No. Au GRAINS ANALYT
DESCRIPTIVE LOG ICAL
A,4(~) AS C ii
-
-
6 ~
-
-
-
,o — -
q—
-
-
~
s—
-
D—
^ 1
-
i ~ra.
rc-so
0 - 3' i-k& /Dirt 4-...c.5
3"s6' Dar~ le.( ‘71.1- ,
1a~ i
~ ~~~. Ksh i.v.._ c [:j
Jli-Si' Jery (-1--te 3; 15 t4CKSi :.,~
5--.d
i2-83. JIc kro9e~uo~c5 s~ 1~9•e1 OLL$, t.%5i
30554.,0 .~ ~r1 s 4 ~~
P'"1- is-%1-
13-811 8 ad rock
i
41. ~c. ~Ica•. L
.me 7 34 ra-+ .7+10 ..
o.y
_
- b—
•• _~
_ ao _
,_ -
— —
-
_
1 —
~~ _= _ --_-
-~
_- _
~ z. -
- _
—
_ _ -
L/
1,,,i1 SerliLrt-i Zed g.1.514.. -'7
1'
~ oQ~(
~~SS : ` ~ ~~4 a+ ~c 70
~o— 7 4 '~^°d tar, A: 74ff ^ (Q`t.s" r r i.)
~ro' g5 w. o-y4. r ~ ~t3 ! ✓ct
rr<<i+,.ro. J
- 025-025-1 '►, .`k' `L~ ~ - ~ Idsp. li,~c r'
~~+'r.le }S ' çol(o~cd,SiZo_3oyo ~
-
_
.
dA3A^
- I
_ = -
"
- "
; , -
. " ~
- ~
4 + /
" 2! l I AU Ho &bE tSt, i&b ay .
= D ~- -✓ !
.-1,151,-1,0"13 - r
~â ~st~ b r.,~,n Pss 1~ P~~~
EMI - g91
4r."1 ar; 11a.4" wKsL. kak ko pra51..ce NA ,..~Sk.
4
_
.... _
__ :
.
Drilling Co.
Bit No
ac.af k rt ,S1-nr,,.io6d
rfqE,779R
/ ob ' 10 1' Depth to bedrock
Total depth
10 Sample screening
Logged by
Sampler
V• -P. Q. A. k.
Remarks aik..,,f,E," 16 1,4 r6.,4..,fer.
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole II- 9&-66
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYT Au ( K.g) AS C. 'in
-
_
-
-
- .o —
— ~—
-
-
25—
so —
: nn ;
5
~'3 , ~
1~+.. .r~ or3o.,:Cs
3-6°' Dar k 4-o 1,9i.t ~e ~ Jrcy G
((
ki
MJ C1I i~oC~ ~d
60— 951 1/er y FI'-,,e 5;15 1ac,,,~s fr-,;c 64.-v:1
95 - 98 ' - ve, f s A....7~ 1
-/ r hale re1e„e Ces
9 %QV~i ~9 1'f 77 -
P r ~ ¢~ Jo ICp ".--c. G i4,S
98- /0/ ' ver y ,~+►,e S ' y 5•I , f ~
lol l°6 Bd cc!
— '
-
.
—__T
.... -
-
_
_
_.
—~
= _ —
-•
40 ~
_—. _
- -- _____
_ J
w _ ~ _
_
_
~ ~
~
„ -
-I
_— = - "____,
' rk s 1 y r,'.~ r de e(eP~( o~
- v4...k fo ~/tso— çey Sere/ k..81{14
/0 FI- S,~ ~~k~,~,~y~~ro
EbN - /DI'
~:
-,,
-'•
. e •
'
, ,•
,
, ; ' • ,
-
~
- :
-.
- _ - :
'
f A,.
° e
Of
; °Z f`r5 t,32 MC 12k 0~
Property /Area
Township
Claim No
Location I— 15? t D o I,J
9 tbo s
~o~~TM1~C ~.~duTLL Date(s) -'Iv ►JE l* ~ 86
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 14-86. - (~
M. Ft. GRAPHIC
LAG SAMPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
AR (PAS) AS Cu. 7.+1 %q
I ~ u
1
1 I 1
l
1 I
I I
-1--1
I-- I
-I
I I
1
~ g ~
2
~ s
.
' r _ 03 0 110 In IGo ?4, 0.3 wo J ♦♦
17:2'_.4 Dy oyn .
~ _
a y
— _
.,110 ~ ;
: ...
i
_
It0 — 7 ' .... -...a -1
] -1 ~
110 — — = ~
... a
~.:
140 —, y
...: ~
7 3
..0
NO -
: -: 2
,
MO 1 e
_ ~ _
, Fro— - _, r
- ~ , ,
no -: :
7
- -, ~ .d
I10 -Z. ..:
: 7
_ ÿ
200— ..
'
-,
LIO ..:
H
_
:
~ !!o — .-
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 14- 516 -
Remarks
M. ft. GRAPHIC~ ~~ MAINS
ANALYT ICAL DESCRIPTIVE LOG
/7A V AO As ~ CK .E.n
_
T
-
-
Io—
-
_
20 —
_
zs—
_
30 —
~ ^, A :
- -
_
: ,--
=
-
~
- _
=o
- • Iq
• 0
o
0-3' t-1..........45 f drga..:C,j
3 - it6 ' Dark ja l i 9q- 41.-n474443 jrcy c(4j
7i,- gif' Veri •C-.e S. Iti
sa-~
4't- sits Z0 ,6 Gig5t5 %-. s...AI .-14/,-,x
84.5- g9 ' gedrock—
4S. l06 IG'i 72
,
0.2
= —
_ m—
__ _ _ _ _
~o —
b-^
_
_
_
_
! - `
so q
- Serf- iGii-i-Lee1 etikG.,It
— 1114 ~.~..~ wkte
— j°p3s;iv~ ~~Ge.o..s ~~ 7 - SS` ii,I
` ~ /° d
L
.~1E ~:..•~_ - ~ I. sro ~5 ~ ~0_13^
Et) 14-891
flocl el il~er v4..51., kde j,
I_ +aroc~rCC. 8/ A "44S L.
_
,
ti
- •
_ •
.' :
.. :
•o. 4Sb 3of.( ll.~ 1.1k. AL
±~- p
o~ »o —
: =
Property/Area ou TEL
Township
Claim No.
Location L. /6 #O J
tl 42s s
Logged by
Sampler
Datels) Jo,JE IS /Si,.
Drilling Co tia d Sc,a.r,.uoeel
Bit No re b779A Depth to bedrock
Total depth
10 r/bs L, Sample screening
R L.j 5
89'
f/INN
MPH. MPH Consulting Limited
OVERBURDEN DRILL LOG Hole ,g- 1 ck
Property/Area
Township
Nrr1'- CPliLE /JLk.:rt2 Date(s)
Claim No. Drilling Co. /Itgti . 01"NN
Location L k+ r 4i' 7S/11 Bit No Cis tell
Depth to bedrock
Total depth
6b
dh,z 71. Logged by
kelw1U Sample screening +I(, Adel Sampler
Remarks $n)fr Fi,t ,.5rl toc
Ft. GRAPHICA
LOG GRAINppy~ SAMPLE
11D DESCRIPTIV E LOG ANALYTICAL
~(PP6) ti S Ca Xr.
= n :
01>i
' HidniuS
4(--65' GzeY Qcû 1.4a4144z CLAY &rr~,C> Sae(
Ual/ b"
eS ~~b -~7oc~ l~.kY-QCy IhltTK+K StaOk,~>t~ T1CC
- A>~.6c k~,=i/c~s Prir~wr~zy pr a(wnu!)
M'4;,ulCc~tx~S Sr>SS 9..¢1 1. h!r_C~CS c,rn/ M4cti< ('~RM„ 71CS
(E i t (ctéCfKl â4WSr{ -âüKic 6441127C/bi6¢ta2 regair '
i,,t rH Scg n.zy CcFm.>Ir,r'
7c>'- Fa) ~r,~,as 4-,7111 =.~~ Py RS 1~S-
1. 640,44 ku146on CcotS - riaix,, Nv.,,,n7 Acrt7,ir•7tx
-12' -kocx ntUtc SruCr.t~S (yct[a.~-6k.)
33 r- CS -F,wh,.tb Cvq 44n, = 1c..., THrcrc (/irriar:AitY 6,,z.:,,, r~ /+ra~uc hâti~...~
}.3S - 51~1CetuS 66,./..
• ' E ~ k(. ?•1' H[rtac,c, ax3 ~ /~ ~~
_
—ehux-àr2$
1 ?L) 1352 Acx) Jo 1.(
- so --
zu-
-
so-
:
-
_
,0 _. -
~ _
~
=
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-
: (>
GO _
- `: :. h~
, 0 01 35- 0.1 10l LIE 02
~
~' - Gt
_
.o -
_
-
so ~ ~
_
_
,,,, _
- -
i 1
Property/Area C /:k p.L
Township
Claim No
.Ç ICc, c/, /; /v
47.4.
/tkhxa.+ /kiwi()
J Lc/
Drilling Co. 1-01m +.It/c1G.rcv\
Bit No
Depth to bedrock
Total depth
Sample screening +1u I4 SH
Location
Logged by
Sampler
Date(s)
(4 i/k
.31'
Remarks
~nb:T l: /s
fir.\ MPH . MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole
Fl i.r.S/1 / 5v
Ft. GRAPHICaRAliAt~E ~T NO. DESCRIPTIVE LOG 43LOG
ANALYTICAL
Au(A>8) as G~ 4 =n^ ~, : -. „ - c- y i Nc..tv5
m-- -
—
1
y 33” -air GKcY LAcL,smfit a/W
=
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~4.A.)
145-- — 35 -3'1' . NcüSreycY t? 111w Nüir&K.~ O~ Si+.AY-6~etY —
y /2a 4-: ,—~ a ei
,~ ~~/ _
~
o1 ' Cc~515 /iwta57 ~Tr~zY ~b0G. &w~" A,,n!
n,,,~,. ~,.4kà ~ars
_ - `.~i ' 64'21"[C(~C: - Ll6Hi ~Y ,k5f ~ GL.~sC 0101 t~tK.,r~
— — fit- 10141 fl,RcS t!~G.1 6.1.7ilruc'
5o- = tS :COnh_S ScibrJrZY /i?(IcC[(Sy,,S cJtrt/
— - tanH
— : # SA~Iu 01 (100-47.1 V L 07 41 MAttrt„ ~~h3cY so _ = 1'IvuLY (S~lbiccK
70 —,
SO —, —
-
!0 - ^
.,,, _
//l\\ p~ MPH Consulting
OVERBURDEN DRILL LOG
Limited
Hole N-cc-°
Property/Area -1)4 P}A / 2Z Date (s) .~.,1‘,/:
Township
Claim No Drilling Co li3i11( a S/lo.a 1.<-))
Location l F+CC[_ Bit No Ci; 499' 91
Depth to bedrock
Total depth •
13
Logged by Phu , k6L: .76'
ro-„ 11ti k~b Sample screening 4/0460 Sampler
Remarks Snti:r .?:of;
GRAPHIC LOG
SRAM co~T SAMPLE MO DESCRIPTIVE LOG 11Ft.
ANALYTICAL
Ru Rs 6,(PPb~ ?n
_ n : ^ l ~
a A
DI
-
G I A ( wri$KJ
~
.
p • y' uwrws y'- g` GRi Y Cro1PA4' HA(zi) LAw.L~emr Ceo
9'-)3 ` - 6^r-) ~ >la 4J~ n~ nl~gc 6.1"; F.SA~br.Sr4r
- G~s /k~S yrua,w,~s: ~~ , $ tK tc.oa+cs, ~rSr~S
13' 6.,~ : INK Gen F 64.4..t,6 6~ kb-
1`h5 AKIN Qz, i~w L;y7i/ Md5stcr
i -6wt4A4 py M«cX (c..,. lNtC!(
K ' NfOkâ 44' pi 4c7aS !g); 7h...Aa1 6V640,1 0.5 c- Ma)
IC.S' 2~Ckc ~ RuNY âlOKc+~i-u0 &~c 44 a. Qz . -, pnAs4 y +f 1.46:2e FkAc7talc
13-6' rYxi 71lw Cv-/y whos /.4, ilatoGèu'iYg 64..lc
AL)! côK
U
_
27c) at. ! }t: 12a pq
-
_
-
, ,2 A6e • io _ -
A
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— 0
- 110 386 !Y~ W. aY
VI_III/7
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so _
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- w
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4o — -
—:
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. - -
- :
—
-
-
- _
_
-
-
-
—
- —
.
Township
Claim No
Location / I <<c, ,1, 16A.;
MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H 71
GRAPHIC ~~
MIME Ft.
DESCRIPTIVE LOG + ~(P~
ANALYTICAL
(}5 ~ ~,n ~5
_A A . _ A . 0-41' lltiMWS
_ r .4 4-1(,' —C,i1r`! CnMc,' or~ La# cunP~ s Gay t0 — -I•••••
_ .
~ 1‘,-.?Ss r 6 - ~iCb6 A+u'~u-A~ C~FAv~ttY Tau [.,,~N ~rkrx,K
—',. /J.d _-
Of Flnt Sii.~d~.Srcf 45b Z32 ~C.G 141 6-
„_ .a - . 6 - ° _,. °f C~/tSn O~aehc~t,~zy /xrc~, cs ~1 /~~ard us
- -` ~ -" ,.1 • ow 0.? 5i-10.404s [,,,t7t . M.n.~ GwbulRcs 3-b- 44.1 l2ti 3~ Q3
J{
n///
= ~.~ / &cû` : "n. ( Fut.:- i]NnRCi, i7,+ISC
30
/ /0:
03 .t3 s -A.I. s ' -1201-y , ih~il st~; ~x ,~xx
Rys-~s ,
CO t. '),) ( (r,7,nril 4-4 Maack) _
— -
~ _ .15-„Z7' - /Ia.+aSrnssx3 6~
_ . :2a .t ZS - Q? 1,&)4, 4,714 r7uGy Rus/ - . %z; -.3(f - N6,406,ka,,,1- `+k.KC .
,o= J t." k~k
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-
60 — -
_
_ ti
— - 1
70 — -
~ -
w - ~
- -
30 -= _,
_ - __,
... -
-
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Property/AreaM 'L P? /1Z.a
Sampler
Date(s)
Drilling Co 'KW(rtSrfc aar. )
Bit No CA C74
Depth to bedrock .2.5.S1
Total depth •
Sample screening la t46/1
Dito 3:6"
I ~MS~I
Remarks
Logged by An.c &it
MPH Consulting Limited
Date(s) k,. IS*
Remarks Srw r
OVERBURDEN DRILL LOG Hole '1-16 `.?
f",..$•1 6 'lu
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
Au ANALYTICAL
DESCRIPTIVE LOG /24110131 ti5 - CLI. 21% ~
_
-,
-
5 —
-
-
-
-
rs --
_~
_
-
zo — _
_
-
- o—
_
a —
—
so—
Io-,'
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A AAA il
: -
:
-
- -
:
. - -
~
-
0 -5' Hu»~wS
,5 '-a; -Gi C-Y-6L4x Hkïd Caviar LiPLcJI+(ru= Cup/
-Plow.Sex'xx Ito" i°7711
V 0 -FiuJ ro fL.¢(i,(Z 0~n.,~r N e C~. 511~à 44/_ s -~' -
c~xt,k~i ow (;),66,:.t As team Ia.rrvx.~ • - Cuits-r5 -Sv~.u,,.1 40 .~r~+naeA kxc,~,cS
(.0` - Sc,' - CL),:, 04e7.1496o+ilor 44.4c+,nt Ircc
%0 -To"- NAMK ot r.uy:S44,11 , SILT ,64.4,-.4-s
A~.b aC~s Fr;zs~ ~ ~~ ~r.ca~,~Csr Stt>~~ , GFAwncs LS.
- M.I,aC~CS Ctn.%H~.o CS. k~usw,a>'y
40 - iU' - KxCr•ïtx,r CLAY-RICH QwdLY nLc
/~4)a->..rl>Li 6y Pi- txxGi».vCS 11)4IIS-5
Gr- ~cY M~.JSrüt.é:e—
6-~►4ar~: Zr. Cie/ 44-1109(4005~rur~ ~irrr
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iG >; a~ fi
.
_
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-
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40 -~ - _
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1—
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00 512 lit 9C 43
-
• —~~_•~
:I -
~° .
_ - ••
•.C'.G~
: D f -
p
1'75" 3` 6 y ~2 Q 2 02 : O
u5 3by ICo 9C 1.3 .o
-
70 -~
_r, :_o.
:7''
-°~h,
A c., , - u
:; '
L ,.Q. ) f'_d
_ = 03 0
3c) 52 IOy S2 co-( °l
_
_ ~o
?v 127 9Z g• 43 : 0S -
o
1C7
120 yl: C~.3 -,; ~g ~
° ,..4-, :
06 0 ...o -
0:- v~ o
Sv '
r
_ -
90 ;
.
--] 1 .
— -
too --d - ~;
Property/Area Ik . _; 57AKr !Jain.
Township
Claim No.
Location L a t( r. /i' + 75ti
I;n &,ie= if bLrti ItpP•ib
Drilling Co kt-)?Q +.Srl•,fz xri\
Bit No. Cci G7Wil-1 cf
Depth to bedrock fit` Total depth ~` f Sample screening
Logged by
Sampler to M6f
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 1146 93 (I,czcgrc-)
Property/Area 1/•4 Date(s) 14tit
Township
Claim No. Drilling Co. 4,S/ci.4Ct/\
Location f rh, Bit No. C6 OM Depth to bedrock
Logged by Total depth y5 ~
lii.h tk ivoprG Sample screening *IC r?GiK Sampler
Remarks STNKÎ (f:3'i ‘S-mir /Lc k'H1S FI.•Gwi H-SG'Ÿz /•, 11iri., 711i.S lQ'.iiJw,i
6r.vSH - hFv.ré l'x6a) JuCw+IDi.rt: DcÉ 7b ~x7xenfe1Y 60u.AeR kol5acé -"leg 6beawu AcsitPa•n+><, 6,i
M. Ft. ~iR APFNC
LOG SAMPLE
No. GRAINSA1N5
4u DESCRIPTIVE LOG ANALYTICAL
14,..&06S, AS CK 2n +~
~
- _
5 —
-
-
'cl---
-
- ii —
_
-
_
25 1
-
_
10 —
„
'
(, - i' Noolo5
r '- 7 ' Û4o.,ti C[iwMâKT LAG.JSIt,~ Ce~7
7' g' Pass,(~r-y Cc~tY-RICr-P Tat.
y`- !ci' rikr,c U,xfA..( 60.4-4.),
le - Jl.,s ' -G00)j CCRY-,}rin.b envy McukpCx~sxdS Ave 1.
n Lc
- mMt,x ltCv(o,c 6o7.G.,r~Y .vo?. t• 34.46 - Cu15rS : l~Gw,cS, lrktn.btC~vS .&11S C,~+ncS
CS CS -<,,,m,c.ct 4)i` .to - roam ,Iw ~! +~, ~~ Cuiy /1,6 ClASTS fer-
li,wiu.+ip?Y 11Mot 1 !n<(jicL/lt
3r 3 -y5 - Cs S/66-ce n,.~z cod6cé Jlatr?cw wirf! / C` ~n Gr QJf" , biUe2 , CèvMY SkiSAnti
61.4.kE AL S06-.a»Z ro delj,,J
- SrCuwrJcitrur en - pi rta06,u s J. 1ü = , 44,5'laou 4A. • 8rr r5 Fi.w5rk21 / flou k4ud~i âtGk,te
1Nr5 7YPz- or- ruivertt 4N42. Del
/4.-10111.Y Ikà7xoy AMC 8/7-1
ka) i/044.- 4-7-o 4-7- .t 453 11-SC-SC
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I
Drilling Co f(cji-1H r-SN-x4<z 1~
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-4 'H
M. Ft. ~
LOG SAMPLE
No. Au GRAINS
AMALYTICAL DESCRIPTIVE LOG kaki
~. Cu 2n g,
-
,
-
s—
-
-
—
to — _
-
15 — _
_
_
-
Y0.—
-
-
zs —
_
30—
II I IIÎi
111
' 1111
I11
11
~iin'
11
11~
1Il
rll[
l~l l l
l' I
lfi$I
IiT
~il
l Is1
11
1'1
11
1'
111 l '1
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11
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• .1
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e.
e:
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g
i i
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I
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:
•
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G 5 ' -MAWS
S '.ts '- IJ<l,c- -ucY G;Af41,16 1A:R., C>.acY -dTc.,,,u
CùwaaAcr vttvs7RMr Cu?Y (,1,7ï1 .4041/
- 1.>0-RcNk.'lY rim.d /1n.11 CeMier (kd deuAaci
$W(21 I„!1S( tag/
,
aa -~' - 6036 Ht~o~s ~~~ Sl~.1Y-G~ Va
- /14i-Ra *PAM( Sb 7„ cuw, s 7 F- s~.J
- ca~s, ~s Pe~~ ~LY r. ~~,~ ,cs 4-6642.4-acs
2-5'- 714i M6(21.- Cut3r-S~il'o4?rtD wall elucrl iw~ . CAilx.wtTt (4%4(41'11E?) N>uJ io:c.aacs
.3Ù' (Ék'1~KGCK ?) -_ QuSTY CA~(x.RR l.11l7~1 dniDS oi 4.1144" 1A4.io1/7E7e4 C4,40,0m:
- PwK ia.yeuk 01 a,u (wad (wrlN 4.,Q 771aK cAâ/~i2c~ 402k
' Pl'IR31r7[ 4X 7AclaclY Soil- (6îoixS 6s) ou f.~.+6tKd !
- S7rcG Sor✓rr SR+.il A,Lp GRAia A4c.F~ +~ ~taACR,,i'cd ?
315 `- nxu.) ia;v A 1..r1l,e -c;icy Sk rStt..u:
POT /Mjcnes c «a...eviuile4-6 /c.e.lzreQ
35 - 3S.3-' . /1,w711ek 2EA.4-. Li C.Albr12d wrz'kviz <I I rH /1 7y4v !Y! 64:.-i.t
SS 5 •,SE ' - Hb►ldelc'>lrV(iS SicTSA,n,t
3,S E ,N
o.FU~lI 31 Z2<, ,cz ~o , °. ; : e.' _
- B-
3
DI z Rk.
ycx~ 7 Gs' .31 0.3 - Oz 2 A6P.
,u, 31 y°/ 12 <al ~
`"`-z t;,-,----' i~, ~/~ ~
. - 05 _ 0
~ . af
•
_
- -
_
_ ~
-
-
" " -
-
'
r
Property/Area I(iw iiilcl / JLv,2t
Township
Claim No
Location ~K cx- S+1s S
Logged by
Sampler
Date(s) /Ad.: lC i 1G
Bit No C!G`l,Oci
Depth to bedrock 33 Sresso.
Total depth 37
Sample screening */U e1tV1
J1-o<,
i'pxSH l2/ti Remarks
f 1fZL J(aliL-
1~u1;rw Kii•.tG
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 73-
Hu,1L,î71ru dada( Date(s) ~ Îoti icISG Property/Area !
Township
Drilling Co HrS Claim No.
l 'r•:5 S Bit No Cr i 1c Location
Depth to bedrock E}'
Total depth ~ii'.c LLVÿc Logged by
Sample screening 4 Ic; rick( Sampler
Remarks
b„ Sir â~y5
M. Ft. LOG • No. Au
ANALYTICAL. DESCRIPTIVE LOG 7$,~(lP(j) /}S " C4 2A.
s
15
'0
:S
o
Al ~
11 4 C -S ' !ltr.7uS
Sl-
3x r - GKy Ca.+r3iCF r-.icuJtk rA.0 Cc,tY
- l'kXri SLu"R-It. i-orTH Q:'+$H
,3C =93 ` ( l4c 5.a ~d
y3'-~ - Fl,k S►xÛ ~ CŸ1C2 4rr1Fl Kti~k ) Pd(F
6066_,S br niAl..uY 07. UawixiCS t✓IIN 07A40r,
6449,4., n3~ , rt S'klClouS .Scl~S /ic[vïCiflfJ3 Sc11S
$C.,/- i3. - fioot) a4-1-2104 AtiGwii I,74rTkrx Z.;404t1
aCÙLY nu-
- Ccrlsn P~k~,~r wrszzy r~~s S-21.3 a rrH
P1wori 6~rTicS r uxc.e~rcS
60' • 7v7lrtC (dtUtnxcS T. 1Kx1ii,,.rCS rfPicft:
5~r<ru limbrlimbh.,c C„r Qy o.~o., Qz t/r;,a,S
~0` H Oz -~ %zrp t, to, n" èdc:►k:.7S rvYRE 611:
'71' - iCcri7AT rITt ~(Yi
7S - ii 3' - Mc v7orc (.1.4Y- r1rCA-I AFx.Û Cut37S
44G~.
%ow(
IN
--~
,o
so _
I
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; . .
/.5 g~ 9i 51 a2 • .
• - _ ~---:
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az
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3nec .
i It1.
'
I1 2$ CP 2y
.
41'14
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r- ,e F ~ .
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A. t.
A'
-0 _.-e.~
....- ~~. / 15~
z, - fl
ti ~,
03
06 I
SAee
1 MR.
18S SL 1C2 '4 o -i
( ~ 5 4-(4. 91 2F .
co.(
&..) sly 25ü 4k> Dy Oi
O~ ~
~• ~~
O IC) i.S I j() 34 ~0'1 Q,
o ~ q
!SS WS .34. 2F b( Oct IAeR
Am-ta).) 6y IF.
i.3 - CL-1 GtC : -TRSPIrk i n1riC,~.c71 Z ~. ~. C2.4rknCr n.-iv/
3` 0j SkKiviS Cx/ti,.) m.:b ér7ca
)//
1L)
~ ln-lo y7sr'r1). /r•i.Ki
- rt<LJI,..artblY kCrAc .1C..TS AtZL iiK,é.1 • Mucci CS. rZ F - <;On„ol tûr7,.:64L i'y4•u]I4c
Siuclou5 aa:,k.Y..S
a ' 7; C1 H.
Date(s) J~- It—i?/S6 Property/Area H PP:STk I32..4t.L
Drilling Co
Bit No.
1k'+r'ik 540.4cc,t)
~n 4716t jc04,7c4.l
Logged by
Sampler
beck_ K.i,.i(
Township
Claim No.
Location L A to( /if25 S
Depth to bedrock /16
Total depth Its
Sample screening IC NrSE1
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole
Remarks
3i?
Ïrn,,Sj! b:-1, (17 m)
M. Ft. GRAPHIC OG
N~ SAAIPLE GRAINS DESCRIPTIVE LOG ANALYTICAL
kw(PPb) /is G. ,2+. At .
H
-/i it 4 - 0-3' 'HcMuS
. 3'15' ' 6ÆrY (1oiOiQCt LACuST11144: CLAY
s — _ - I*IoCaJ .►ü&-1112 1...s ni k'ffli
' ,
-9: •
_ : `6 -65• - Fik,t- SAvd 4)in1 t /2) C,K.iuAA.1(r),44/..y
- EA:IiWi/CS, ..
'-0 —' ~ a. • ~ ` (o S -45 ' '- 6C06Nt7t1'dC-,ru-~u S ~.whï Pr6di y lia.
- - :..sp : or a `S- 7U' - FfAwb *S/Lï MitïT"IJC, C4î475 0/044y i(-) ($9 Ir! CC aq
70 Pl. UczGn,K lir:ck~
~ ÿ h • S iC,irS $ D,wtwi$ 30 3Z.1 110 00 0•3
_ - a2,oj IRK 'it,'- u.M. tKxu~.c {y,..6,,
_ , ~ : ?û'-45'- r•~KizJx Lb.•l,ti.o.icy Amy (,rrit d`:~
_ , . oy 1 q~. Ic~ &4i: 12o rU 40-1
- - ° \' - s~c• 71- [a•i. IwxC.~.0 Or~,Cs~t
1D — ~ s ' âG'-Zr. eoL+&lZ
:6— 1a . : b5 5•,......6 q,..; - CoMre>rk i C4}Y fiii2l?a.: ~~~
- ~ ~— ~ _--al' o 9 " sou 7iYcK.teZ
- so -1 .. ~,
^ 09 bL -Ys 'C~as%S (,~),+,,,,tiLll üY PI- wtcro,.cS 5S
- = ,` - v$ z~.
~-~ Li- Hy I~sc 8y 31r aq
- - ... • . - S 45 ~ l02' - Lta,,S o; Î ,6, Sem-,4 1,,;r4 V. trrILC üv
_ o l~• M~k, MS 23,1 . G`1 3o0.2
io— .
- g-- -
--, -
- m— -
- .-, ~-- -
- tD= ;
-- ~
- 4o— -,
~s
— - > !0 —-
- ~= . . .
_~- 4
304 go 14)a I -
= h , -
-, 9 2 ree . _ 100 . ' .t hd..
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole Xbe-7(,12 )
Ft. GRAPHIC LAG
GRAIN >N ~LE ANALYTICAL
CO DESCRIPTIVE LOG
.
44(P:K) Ai C.. 2+. - 4 - : : :: - o`t - a'•- ;- , )4.., lo.:- no' (3N(n /.:z boob anY-k1U! 7/LC S1J 572 9C 92 40.1 - .. L —
~ -
n O
I)
-
1v`!' fuCwC Cos1 62 J' 36 TG (Hi~ ûrT
S }f 7 y ti- i b :?} 4:11- ~
471 92 .30
I10 // ('
',
- '
J),I I ! ' ;'
lL('
- !z -(LASTS P82c11urUk.iYR.aY /r+161(..cc(rw6 L-StrYka,n,c?
le n_Ûko(k: NUIaa,ukpo5 lxnCK AcC,JulTt
- - I15' E0~~. 170 _ — U
r
110 - -
_ ~ ~ 140 — -
150 — -
lso— -
170 — -
NO --; - -, -1 -
1110 - -
700— -
210 - -
220 - -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 8I46 - 91
/k..ql S7hxr /JJ.tv2/ Date(s) 1711C Property/Area
Township
Drilling Co. WOO .4N CA: 4e.r~ Claim No
•~ +CC..~,
P-1+SS Bit No Cf, d >zk , I Location
Depth to bedrock S`I ` Total depth ES' I HL: ,4'ti/C Logged by
Sample screening } /C' MOH Sampler
Remarks Snh-r 9 a rrM~~
it. ss
M. Ft. GRAPHIC G LOG
SAMPLE No.
I Au
ANALYTICAL DESCRIPTIVE LOG ~(~ its 6.4. 2n ~
_
-
5—
-
IO---
-
-
IS —, -
—
1 to—
_
1
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:s—
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0—
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ri ,; - - y ' G . Nc mcs
'I' -39 ' C~rcYlSH-ÔLu: Co.**r t.filuSrKM,r 0.01-y - i~cCGr•k-S 60' jig 2.,1T?i lk~A/
3-1 •`i ~u ~ - ~ J ü s a • /() r,]N1il•kNr! i,`uvi....«,1
• 4,,,b /rb.4ç5 of /ifzrt7(cYx,aoos (üwaJ/Jlk+,)
HS - Sy' - Gc~,, C[NY-CrcH nA74,K suAb„a7) ~c,ëxiLY Tf~
- in97rF, x A~AKox . ~S/o LT. 6Fnu,u GCAY, 25 Z5p Éwc 54%,6
- ii~whc~m. Td Srxi-~uGr.r..rn CC.iSis ~,.m,,~
8Y C%✓( agzihwcS j rY/raloQ ÛRihw lY$
-
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-
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•
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l0005 G{ /cit,b 11 1,14.0-3 - 2.)e*rKLY Sclùcrnc
57Sÿ '-T1cC ivy—, CtRST Sc.vïvîltù 4r7N I.r / Grr.n;,ACS C C,z I irre.i..,cs '/wo+are!
- I,cx.c,r..;,Cs, SryS Cur àY Gik,h,o 6PAtc7v
nt` ' c 54 Ôcii~(iK r C'cr7 , r.,yik f `F~G~fifi„e>j rrt Si( tExcih,•K
4f ' - fcvSTY Ook•7kou 0( S.+. ii, AM( 41rnf ~jQri•rN 17 c hCvCIâ1uS = 1,....,,
- Sctrvs R) GC Crh,ê>a mr' ika,n.6
^~+- I~~~r3
G^ r2
63 I ~i fibti>~ LLrlcp.iR Py _ aQF FCCK
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-
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so_ -
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10~
y
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-
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- ~
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- •
-
-,GS'
Property/Area / laze_
Township
Claim No.
Location F+CCC; /7i..5S
Date(s) l?
Drilling Co. MAN S44....C2->t)
Bit No (6 C?161
Depth to bedrock
Total depth /OS
Sample screening
Remarks Snh; t 17 sir
Logged by
Sampler
P~c- ~evc
/}nckcki btrtI
"kJ Alai
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole '/-r(- 7~
0
M. Ft. GRAPHIC SAMPLEo
No. GRAINS DESCRIPTIVE LOG
ANALYT ICAL lL iPfb) Rs Ci,•. 2"
A n ,. G • I •N(0.403
s = ~'-yp' -ciiry'ûwi cricus7~UtiZ liAv
- !PM b 454 Ce,r•t/ixT ,dur 6:eo•t,n.4 SoF1rK - ~
--N. 4,e rN 40V?
~ YU Ye ' - Pa36-Y (iexs,a4)) Exedur:2 4- rm., é s>tiw1
— _• •t• •~• - oc Z~. Cc4sn HerrcoGca~o~1 m-5 Cu~.tF~u7,►c) 3iU 24.'4 9~ ?c 0 3
50a f~~i : 02 D K~-5s' - CtociS Cc.tY•KrCt{ !►u'xuh: ~ti8cy IL 46-16c.)GL ~îG. O.y
_ = o : - CcR57S Ù>M~cY UGrC.h„t5
_ 03 o Nq'- M• kx.c,f.:~C ~~
so — •• ~• _ 3ti âC 24 & <0.1
,o ,— :: - 55 - S ' - F~ .sa,..a we,tt <54,.a
c~,.~Cs A..4 /adz~:,... _
_ _ •.: ` ; - l,'cc...Da.) x .k.o-uicx,n.À ~ GGuars~+wrt67i
IC. 9 3C 4.6470 — , • • - QJ ~ 6Y fn~i~iCtDvS r$'[?),rkU.%S, in. GCYC/4ifC.S ZU
_ . . . _ U6 ~ ~2p 33 t4. 4v <al
- _ fi5 ~ll'' A,.,6r,u't~i CLtjpr_Y 7/u 1...:01M/ti:i ~x o` rSi~, -' §=-:4, - ~ Sic 36w G`{ sz 5Y 0.1_ -:c!,. - 0~ p
so .:.-14-•<' - - Mck oKiJeri_vt o,: Cuts 75, S4„.6
- .c, - 06 14*. Ÿl -ÿ~.j - C~Ocb (14-rd r~
-
...6-(--t ,c, au - . ÎcN)LcS k/41.1.,--S Pii.,,ii,H,AdtTtLi S,24.2„,:71.
0 JI I ~
9b5'~ûfG(K:I:KïRei~kcY SGriiGkcY (c'tSK Utie.tihwC los' L op.( - hlu.t{ C(4-7-glus Aµi U c r ïKt7 -IU Puoa,At
-
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_ , , ~ . c - - •
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- - ti`,,b\ _ N .tirx S~>'iciizt! riL( c,irN } ~ 7-12 ,-H1~1y ~• 1•7-
~ ~+ ;ill/
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole h iti l
a pit_ J//-irr l:hIL'l Date(s) Property/Area
Township
No. Drilling Co 11,11r7t ~ Srrrsc.cr.t) Claim
Location /.r5US Bit No Cn 67501 / (l 6 ~dJZ ((h 7E5I
Depth to bedrock
Total depth i }riL, 1'IYC Logged by
Iir.e~o~ ' b~ln,U Sample screening 416 i16:1W Sampler
Remarks çDi);T y'li
/r 4.4Sir •6: c—
M. Ft. GRAPHIC LOG
SAMPLE Na
GRAINS Au
ANALYTICAL DESCRIPTIVE LOG }}u.(pP$) Jk ci, 2n r%
~
-
_
p —
—
-
10 —
1S —
~
—11
-
'D —
_
-
:5 —
-
o_-
- i\ rL ' G- ,?` yc.+wS
2 • 3y' CNït^/'61,ktc CcPtr►tc-r Cil1Y
31.11' - rot, 5,1,,,d w in( < <I 4va~.~ Ikwilftutui
PCbNLrS -, %LU00 -6ut••tL
~~-:~' - HeleIdwa-005 ktidcY ls. 5/+.(/ w ~ I
/^`'!1/hZ=.Cr.}t Mk ,1GPALS Fcku,.t~'Gc•k},,tc .tS
(.L fiz ,~11C dam-bat
t9 TD SW- ~, Aw~ ~
(trtY ox Sua ill - Muft{ OF 7Fit 71.tf6~&rES 14-4(xx.uA,v,cs
C(.7 6Y û?z cE,.4rT~ /b••J S44,--' Sd(,t,.2= ALT - kraR r}cw
%5 - ~ ' ~S]`r (SîGax: (OlcrdlZr~~ Cu}Y-4Kli Tlec
- (b.Gcc,hz (o~;w ~S/ÎcB~xis â~+µ.t,ati 6Y ~c:2SrC 70 ÎN,2i.IiJtM?E lxrtC.~„ cS , rl,:~.ictw, 5c111niu.7S
6Y' to f„uSl-r~,~ ~ y~3o A.,2,_. "ca [7fsl` 5v+.:
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1-75' Tic( A),-u,..lrttj dy 6,rY Gi'tÙ.riat FrcSl< ksC.t...( l.,,TN t2 Aiu,,L, 4 e 1664) 1,0A-1.4:1
75 L't~RGCIf _ GcrY Citi,~ .tit >) FT I.ctc.lx K c~,.rN Fbé 11wis 1‘.., /ru -1-1-llcn,.rsS S,ta,,,,~Ci
~b` I.: cÿ~ ~- cos i'
Property/Area f/'111(Z MAL: /-.ra,Yz
Township
Claim No.
Location /
Dote(s) .T~r- If jd'c-
Drilling Co k 1 I +SI11+ctXcsk
Bit No Ç6 475//6;471S--.)
Sample screening o- lo
57-ii r %S.s
Fti15r( 1-~,. Remarks
Depth to bedrock
Total depth
âC.s ,
bb~ Logged by
Sampler
//}LL &1]1c"
/b L,~c..
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 11- i4-4c
Ft. IGRAPFNC LOG
SAMPLE No.
GRAINS Au
ANALYT ICAL DESCRIPTIVE LOGM. Au, (#4)41 RS û-: r`t'n. 47
-
,
-
3—
- y
-
to --
_
- -
_
-a --
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~
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0-1' Hu~tvS
‘/'•301 ~Y - (jc t644u. t644 QrtAAcr LrJ4.6rz1a~ cup?,
-14 t.i~A{ ~~
-
3(~-N3` 'tt~o6a:~ Cou,.>„-i1 htJva-GAOL
- Rad a. sa,d
.
i./3-57' -~oc~il ~fx1Gu~M-.iubat+4.~~ C1tY•ArcH nil. 93-yd ' ~ ntaneltr e~f-sl~r urTH CutsrS fee, 7
Prisctes a *41<.t(cikJs SK-tv+.,us
y6 57' - m~x Cuty-~,,~ OW ~l~r.ra ~
albdcc5 or 66I14 , UucG(n+ici Ct.T BY CA-4.1,47z: U~durTS , 'Iwo( T. Pk., -
Jncs , S~iUURc wu. S?.S' -Gt.nR bDw62Y
5?" 4i.5' • Svb-Rog w~~) 64.4,-1.-, Aa5s18cC Acc kid-V/444—
-61A et- M-uutCA„JCs u1>H
Cii+c6 LA'ie.,.,7s SN2K,nc (z2sec 0:IG,h-cS,RusTY IhxLC.lru[S , Mug( Sc1~/AFh±S
6.2' - $GyrSPSr SckCrnC Scaw,b..r cur 6Y FKeec~u (4£6. LE-‘44.01 1id.xGuxç 0,-, ~ ardtFi (rapt at -2o r-1.
- UO ro /IA Ass /y 1•C SG1Gs1KLCK" laic
- 41• - 0140.-c If: e>,I,~:ti Rldfif9t Aboies
1-1' - ri. I,aan,,, hwc
c ee)(1J1TH c$. kLgc,tk,jc iy it.•-.b r. c,do,.,_ iuwxc.t;lo..ay iy br-ta A...Jj ShbA6.,
78 ' 6i7 6.4.4,..d..,-. IL, 1bbS ,b4,..4 4. /; 7tSi - civil cxib,2zil ncxitk,..
64:01(.4 x 3er~c ,rrC QuSrY tnis,( tKr.c.ir+L+c , sa.xà+tli CAr.(c 00 9s FS'
k ~ !. 04
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.
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15 —7 ..
-
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w- - 03 J - f FC .?o `~z 24
: 4Y40- qÎD °15 "ii` 6 `ii 401
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o
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13 Ipy Sc.) ~~ ! .:: 13 p.a(A0.4 ?(.) c1o• Go (a!
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- ,
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-
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- ~ 'S'
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole lî'86 11
flcr•~ Vxzr `~ctte't Date(s) Jl.ri lh/iG loti. HIdG Property/Area
Township
No Drilling Co flc-+t t7l f SNck[.r.c.~ Claim
Location 9d lltcrS Bit No. Cr; 67851 / in
Depth to bedrock 1174'
rK~. kit;(t Total depth l S Logged by
Arndt') Sample screening +/O 01E,1r/ Sampler
Remarks Smr 1:►S Attt»sDlaafi tc HtT S~= FctAxt- an,; C61a.41(xra2-+ Rsssrtiy QY
Fwt.(ti l9) AY,C/riC 41.6rc/tz
M. Ft. GRAPHIC L0G
SAMPLE No. As
GRANSANALYTICAL
DESCRIPTIVE LOG 'kW AS Ct..
-
5—
_
-
-
io —
-
-
-
15 --
-
-
o—
-
_
-
-
-
~ —
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-
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;
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:
0 3'
3Y `às '%
7Kc
- I I
-1, t-4,-
37 YS
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fyu4 N.Ixb Ccraktcf cACaretk [ay
- SDI"trK kiwi1~:►~ri:{
• r 31-Yû -Ski)), Pr6tky 44(.4.11i P41f1klx-S.kw1tÙ
rut t.1/rr( CtASrS Pkc6wtw,rs~Y Cw't"+rltS
`%40'-59.5 =6~ootj Qtry-drC11 Pr~ ,tA Ly nr~ tt Ccdmj
P/icd,nr•dE~Y /i't;ll✓Kt~03 St.~lUNdtir$ (h.xt.
6° 6uluc,cow~/Kr curl trla *•7 55'
56;1'6 6::(6::(604444l C04,60/ UtrN 6.136 or ;IT T8 rrlltflC IkYUurcS t5wwu44-
Stt:5 - dC' - Fi2hwILy l Go68tY T111 (/yry 5)0 tt/iY
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1stt,lnM 6015r5 or (*Inc 5i45.4.12-,- Aak+•+lt0003 &t1640.aS,wtctt.,Ics ,I.F.
71. h' - S*A0•6R44r1Ly rotAtro (I50 Gm IU MRTCIK,
• 75's" 'Gtx6 Crfry - I:aH Ct,ti6cH trldyclx-Suiroie4 nu wtm C'irlsrs 110.4N-514 Iy Cïlt>,r.//t rt . l.uzR+wtS 5K:S SC* S1IISZ F+.>t(c
}b'- t'luW 6460utrt ,7kt Bdonr.wri I+k7îr
b 3' - Cs rG[mncb kLne$C/(t Py ra frls< IRxfA.,,,t 6arbck
7.5 ' - Jltu6utrC Stê~ +Y~I -Gwit.rtt Y TkL t,-~rrH AX) fifty /u n/ygrlt , MuCH 1066.rs /60aa1JE's
- casts `XAïrnUY NEJt~.S
3' BrrrK,+s. , 1...:,, g c6cii53 y r~,1
1./i[t~c Coaxes of 6uKC- r` W[C.i+:..t ('valait7
3/AIL' CS. (0.5c.,.) Py hlaarta,Qj
45 k s ~- Maz(1 Py rti F+..rtL F t.aat.,..K ~6 115
blx~~ ~4 •
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1N M/MX
2.5b- 129
~
âo 38 CC). I - 05 -
1 A6>;.
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5 — rr.
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! = ç, :
;
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- _ O6 _
6
:
-
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0.2SI(iiit) 320 240 4,i b.7
- l b 6 Au.
,o J
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.
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-
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26- t9S 142 ŸY 0•2 t,„ + r3 0
: H l SLo
- tb3 152 S2 0.2 .
lS -
2ABR. 2Wt•
-- - ~
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole {r SG SI (2)
Ft. GRAPHIC SRAM
ANALYTICAL DESCRIPTIVE LOG ti.t(leti) As G. Z,.
I00 .... ..._-,>- 6-
- ~ 5.-,...
~ . - O _ Al .2S ~ li~l 131 5-E- 0.2 ~
• -• - lu$-tru' F Sitk., &uc16 Or ik.> rirt21400-
- . ï -• . . : lA(i4• 17 lid - I(7.5 ' CS .ï,in6:G:~tt<t t1~i>,..,rtL11~ 6'1 COSTS
93 by 3`Î O.
Ip
04-
r ~~ 390 7i 56 ‘i`l car - '4-, '1 ri
'
_f
_•,- 0 L
- -
d 14 '-10
~ ~ 13 ► 220 320 0.q
f )17.5 tîrDkorrc : r{~Intir tn,nk2Y Sorr tNirt r'As2 ti~5
In _ üui k7 t2o1. H 612;77C1z5.3~ ~1612;77C Aki-
_ .2.c., lutrÉ a:n7f R SracC4lolIlCj Or Q2 UG~AfL7S
- -Py CXcus As F-61.4„1 /4.a C.Ac.~~r.risA.4
ISO : As tt~~ Cc~S _
r
- /iFtz~c t2s.5 ' (y4CK 1,4-0SriFr Mlle
_ 12G•5 • I:: of 11 4e i~lElkcx ~"vxK ~i~itiLY /~Qrcsn:[Y Sa-7 Cu?e /
- 6 FciSI< WOW( lGbwC
. 1
MO -
1601 -
J - ~
: -
I60 -: ~
]
RO - ^ -~ ~ - -
.-. -
1110 -.. .-
:~ -' ..
6f0—
200-1
210 ~ ~
220 -- -.
..
Property/Area 1Lni.51kki= Ian1
Township
Claim No.,
Location L ,k ,Q cl
Logged by
Sampler
YrCc
lb.rL,c1 krir.lb
Date(s) Joti~ ryl(G
Drilling Co i1' ifr :ei t ck
Bit No Co 47b 31
4 k , t /i Sample screening
Depth to bedrock
Total depth
96.5 ' lCd '
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole • fr a~ az
fiTrkrlPêu; ro IfrT rnwd,XrZX: AS 11-4-79.k>,Si a 4Pko3ct Tc 6t SCxafivafc,/
0AIcz
M. Ft. GRAPHIC
No. SAMPLE GRAINS DESCRIPTIVE LOG
ANALYT ICAL /IA (PO 43 64 ga tF~
-An
-1 —/l - - _ ~ r, 0-9' 1f~S
.;
- ao - - - $critk 4.4 14 ÀtroiN
5 r _ : ç' .y1' -buw 'Cuîcy N40C›,,iAEg Lrt(u9gr5F CtiFy
_ - e • - - jH'-93' 'FIiucSA+‘„t1J7T1( [ ILA, Nks2PC+Gà1.ta$ etluiudcii
—.•. 2~ 4g 96 () S co. I
_ - ~ - Y3'- â2' - Gcnû Cuit-ow /$uEiu.~c Cs6&~I nu
_ `13--11' - f:UWci`S Qmi wttiRy um Uor.(MwCs 4+1fl{
G~ ~ N55 • Py 10 14âi 34'<O.1
R —' ~ _ ,C~, ~ . 412~ `141-3- '01(.<1•1 •Mc,Ci{ Ci,2ifn.a71C5
_ G - : 55JZ-' -F SitxJ - t~ S ' 36'- 12' -CCdST S J%wU.,i i1b 6y YxQt,ucS ïcdS.
.o _~ &_ 663 10 0 loi 40 6,k <0.i
_ .. 1.-~ = 5o Yo 132 « 40• 1
- . i--.~ ~ C6
~,• - . .
5 - il' - 51
r
~- 43 - Nun -Cid•k=uy /?u6oL4t oh* trek w k ITN : ' 6'11: . Cac (~ STkL MuCH tü64r5 7() 16 I 9.0 cf > '<O. I
- Gitws :Â^i„aRl7J 6y SEXiCITiC F-McxCA+KS,
~~s" bi iItBR• iuSTY 6vKé ' MtM„C G~,i,,..nc5,n.i~.cch.,cs 0.1.0,40.1.0,41$8 to Go 10.I so
_ ~ '3 "_' : 93-'-)4-5' - ÂUSfY CoH4ICFi Co6ot.Y -lia. ldini ObticCï
.: , _ CS 0
1à0064.,riv,S00 bpi kXGn.,CS $tkKfrY F. tr.i(.i,ucs 30 A6 3.Zo lyy O,Z ...~Ji ~• . ~
/ // J oY c14.5' fig,l~ra: ~l,WitF-C,~`f , So.-7- P4srz urry v u2r"
rob' k Fwx w,trs~.r~
~ H /ii"Vari+:S Tv 4,- S/t,.,C r-. Vü.CAA,IC
- b— -
io —
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~
o _ - oYa -
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•
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-
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Remarks
3.1"
Property/Area Ifùn>L,SPMM, /J -?ti
Township
Claim No.
Location I. k#cf,A-' y'/JS
Logged by
Sampler
Date(s) 19/1'6
f10lli-1 <S%kAL Ct ü
Cà
Depth to bedrock
Total depth
Sample screening
Drilling Co
Bit No
.3
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole k-46 .63
Remarks
.îTK7 /1:Ç
/t7&r]D7i,:G 70 N/T Caluécx77.x klo7lféu. . 4rïluvy kS.r2.446n+:1i
bY /YR171C Na:+PcwS 4.5I7Nw fiVi48oiJ
M. GRAPHIC SAMPLE GRANS Ft.
DESCRIPTIVE LOG
ANALYTICAL Ac. WS) A5 G,.~ .{T
- A A il - Ci -.2 ' NOMUS .2 =3` lficr Lla.w C1dY 4.u7x M„uor AriGcd,fr; Fit&Az
- w— 3' ~-~: TA.io~,, /~r~ri AA:r~;~e,na-n~,~, 6-uni
- _ - 7N7ill (i.e,;)- f'y Ye 4./S
y — -V-9' C,QrYrSM•YrZGa4; Ck03.0 S icTSxx,ë t
- - Millir).-MY 6kRék,
9,
~~.
— I l G F4Cii or I.F. 17üL
io— - -
IS —
• t0 —
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0 — v -
- >n—_ -
- so=
~_ ..
!
f0 — ~
~ - -
70 -- —
~ — ~
-~ .J ~ -
......
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole use s'I
Property/Area
Township
1ŸunrcS?s — J~ic; Date(s) 7Ld.- 19/rU
Claim No Drilling Co r7t/iTÎr gif"14 C YlÂ
Location L ec& ,iriC S , Bit No Cc L~âsy
Depth to bedrock 72'
Logged by ~)ILL 'ZrYC Total depth
Sampler 4,1\4,- Kmlko Sample screening to rug
Remarks Stl}r;T I~HS kKPCRra.rl 6'2 14,6:147e"1,
11.r 3ti 3-oc., rti R<< rw. 2 ïd:40121%
M. Ft. GRAPHIC
LOG SAMPLE
No. Au GRAMJS A
DESCRIPTIVE LOG N A LYT I CA IL
a4,61 AS & Z4t ,
-
-
-
5 —
-
-
-
-
_
Is—
-
- -
-
Zo— _
- -
25 -•••
-
•-•"'"
: - n /1 q n
: • L'(. ' Hu»tuS
C~ 2J ( Ittit -G Rrl+ tld26 CuNIPRcT LA[uSfl2wr Coy
.
L3 35 - ~owu, Tü Su6Ruu~ CLQttY C
- Hc7aa, CAA-2,r éuu 5 CAA-2,rCe.P.1 poSlnohl
n«/►a 7U A 36 1- 91 '- 6006 Ri7 S~6-ryC~.,M CG6pcY
TILL 1.-11171 CLAY -Sil Mbtll(IX
CLAJ TS 1~irn KnTLY 7t5s I.lxG9><.C5 4,0?
Mr.wd Si1i!»ic'A.I5 CiRkrw7f[S !
r},2' ikUbGC ~/6t'R,; IYrLievtern7r lk.+. io{r>awu 4lrTl-1
r iA,.. -6-)44.4,A4-.16 ?rim 4t.64;4 itiu -
L~i7c~S 6r~rn, 9cia7Z IAuO pLt~Lc7lR~/
JhSpéX NaKI~}wS
3-3-5 ' Ktraat,c1 /40.6 ITC. ( fix) Crz,Pyj
-35' r ci 1-I
'0' 100 Ike
w ~~ 4,0.1-
-
10 ~
-
-
..
•
-
'i o;) —
-
io — -
-
:,.
—'~.0
~ ~ C.)
, .
so ~
-
- GI . .
0 130 33t o 3 o. I
-
40 _
-
— _
_ m = _
so _
=
- = -
eo-'.I~C:
-(
~ ~~
,~ "- 1.1
a\22,
\ L.: 6_
p c
~` o '
: ~ L~
e~ ,\ -.
e=; _ d~,;
1 ~-
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. . ~'
. : CY / r16C. QJ &5 9I0 Q2
- 03 I R6C • ‘15 ~ S6
12a) 'i W .:y a I _
- &I IA61'.
- - C6 . p zS 129 lo-1 ° I2 4C,(
- (X.0 I2o 12s" I2o L12 `a(
= a 0 10 23 Sr ?c. 32 co. (
_ os o 25 54-1 il ‘P4 0.1
- ~ l M~2. 16o bo C.3
:711/II: lu
.
-
_
~ ~~
~
:
~ 100—
:.1>o
7
:
-
...
: ....
-
:
: -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 11-Se-as
Property/Area HCM1. ]Pi lfCwvz2 Date(s) ,/114,
Township
No. Claim Drilling Co haHAt *SM~dr.,tr1)
Location ~ ~1czti ,111.9S Bit No CI; CAS"
Depth to bedrock
Ji.1]IL- . Total depth by Logged
/{,_r1;tk Kn,.10 Sample screening 4 !u MrJH Sampler
Remarks -17 krulU.d, N k 93 4J17j1kJ N-S PRnFicé
llvi SH• 9:JS
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au
ANA LYT!CAL DESCRIPTIVE LOG ~(~~ AS . GA- r~A
-I
-
° —
"I
-
is—
-
- - _
_
20 -- _
-«
_
- /I /1 /1 -
-
-
G•.2` N(;Aio$
,Z % q I QRG~i.wc ( s.Aci(-6Ed,,,u ail-.
q' -16' LT. 620L,~: N/h:11 Ca-i~il4` L•7LuSTLi•~,é 6.01
4-11' fiw'wlt 11ùxeZli ,i't(lüliS
_ -
b--`~`_ -<<
-
fl`-I(' _Nc7tvzacv.,,i,s cs.s&AS Asti C~ai4.r.L.Ly nc~ - A.15..uec ID Su6-rlwGut..l17. GAM OF 64,,K,:: LAN
Py Co ~riiul,s ~ Iy3s~nr1....A7t) Ci.ki>wk FAke.' I
GoJi,~ D Cc;(ts • ! ~ ' as.s " - (-;',6c~Y-a,w ~ ~~l nLL e~t~+
tri 3k73Tan.a< FiEat,awS
az.s bcZ%o(K: hay /. 64A.4:-IS peMniy Sirs,oA.z
29' Ulu oc.1AitÙ 2.S' ~n.To R Awc ~(~rn:Jtvin1
K~•rs 01 F~-6•~c31 Pi 2.E ' r.ugY Inoi$E-r,t A;.rLa
3,.; PAuc enAi. 36 R iN
-36q_
sop AN 12,4 SG 63 ?;,; at Cv - 20 -'
J
4 : ~ 4
~4 .--.
- -
02 0 ~ r1°1 1`) <Q. ►
-
-
- a 3
IS -- -
25 —. -
30 ---
- -
~
-
-
SO•-•
.o—
-
- zro
+o _
~ -
wo-
40 - -
4 ....
-• -
-
-
r
:
- ~
- -
"
_
= -
- -
-
: -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole W-g-S[
Property/Area Nom Sl*ISé /T01-fa Date(s) ~~„;
Township
Claim No. Drilling Co I104714 +Slicx'i.u7À
Location Bit No 4.7i-53-
Depth to bedrock SI,
Logged by Fitt $4,64t Total depth SC'
Sampler /hrbcc.0 44,•co Sample screening 4 10 matt
Remarks r /(;.00 141ftmaNE, 7Z> HIT Co1u]1ocz1( lbt~cr'c rgISSc'6
rm+SN 11:3u
M. GRAPHIC SAMPLE G~Olâ Ft.
DESCRIPTIVE LOG ANALYTICAL
1~(rgSl ris 64 2~, 7 - n
Ari - 0-3' )41..41.)S
4 — .
5 — -
_ _
_ = 3'-5.2' -C,Qef /ARA C'omAtü utos,~ Cull _
- - Stuc 4,r A-1 6_41}( - so-
is — — -
_ ~_
15 — 60 ~
^ 62 ~ ii ~ -Tlci. _ •~~ : • ~ - ',~ , • a' - O( I ABe 52 =r. ~' - I~A>t G~i<Y 7
~
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(
c o,' 0
u.
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~,
•
,
(
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M(
nr SIS `Î I `lO 31 4O• ( - - . . ~, _ - ~'t. soi-6 f J~~r, W Sr J /~~N 1~M1ICly
`° _ `J} _~~ 6446,.,rrcs rkIcé , ,gw.olt ,10e.tweS
20-~ -;
Q'..~,
~-' tl= — - Dz )~• 47 -32 '- INfiiYCly r~S,ah,J1 St7 ,CU~Srs M1Rr,1tY
M.~e+tcd,.,s Scil/r~,„ 1-S ,Z. r vcic,t..,cS US- ' Iz S b 3 6 gat
- ro ~'~~y: .â : _ Gj ~
- •~; ~ - Sr - COlY-41cH /f>`+cu.fie lice 64-Yel4,.4 _-~<<q, ~ m ~ Cc,tsr S~/~Rt U17~ t~i l
zc.S 3~r 144 4b oS _ — ~, >
~ - oY 0
-OASTS J,.n....ln-g Sy ~,- v«.c.n.jcs
~- (~ 0 JJZ, 7i 4 SI IoYO D{
25~ r ~
71/r'
LL
I~mocK:-('j(em•4fic1/ t. 4i.47,0 Î.4i. 4~C~►Lrc
4.N771 Ck I16A.:Lk7S - — / %- j;~~ [.,~ p _ _ _
- - - /114"~~IIZ/~lrL: /j'2.1 L`A.{I1~4N Kl~ i, 5e.V.1. 01t;
^ ,p =. k~~krcSiJY.• of. ,5"..-4 64 ik>~.7s _ _ . - Lill-k3kdt F.C„A1,1Ct ti At 4,41H4u itu.:.nf"44-
- - 2xxS
- - w?cx.e,,13c- &z,< AA°cn,cs FLc.W 30—
100= Cott(
_ ~ _
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole ti-SG - 4 9
Property/Area //0.1c S7HAf I TcLzt Date(s) ,1un~ .21 1,14
Township
Claim No. Drilling Co 4 cr+LIa01)D
Location L .2tcY'~ /?r.251; Bit No C6 6 iiSS"
Depth to bedrock S 2'
Logged by Scxi+c Total depth S?~
Sampler 1ti~Arta Kib~lG Sample screening tlOpikS(
Remarks Si7t~ >" rl~`f5 RT&M011.uG ID HIT Srlwtc ('L+x:.6.xi3A ft5 60-1646-+ 1145516cv RY
`tn,sH 12:qS km( sari Oz-CAab Lt'7.uS k, 01+4-rrc lkxt,hwc
M. Ft. GRAPHIC
LOG SAMPLE
No. GI>A~
Au DESCRIPTIVE LOG ANALYTICAL
AVM AS (1A ZA.
_
-
5
-
-
10—
is
-
~
_
20 —~
_
_
-
d5 —
-
_
A _
. _
_ -n
-n /i ~
-
_ -
0-6' -HuNuS
C-16' -C,vrY-6Lté HAad QswMcT tllcuS/Ca.l (ay
- Muu1 cSDPIM win! &P?(
V-?-1' -AtIG Wb2 CtrtSi3t1 Ci1 ii.g1 74 c.11 fï( rul Sh,6 A71i•Ft:iX
- CutSTS ikracG2wccvS (LT D604«ulkt .8y
GArbc~+TxÇ, UUL.itwlC$
?-1 '--1.1: - CLkY-!1Q j A,uGtaA,Z Qo6tbtY 71LC t ryiQ'1KW - SuA ~
- Ct~ts Donit~ 6l hN?K 6cKLbwCS ~/ - 64 0-4-1touS
' 6r~20CK :. C1Qc~~ -GQrY Sklc IooS F 61kMcb ïocK 4.vnl ka
PYe in( AKItkY oz-CAD w4: S Ar â9 - S5 '
- t~lei/r ocC.)es As bssrwr~.hïkk:S c-~,nlw+
$1c1Gou6 AOcic An.b AS e,ric'b:dt C.44 A...6
Ç. Ewhm-~-+) lu;c.teTa~ R+R s cxn1,.~ /kt~ /
Or folly. ~ /t~w7 n., C~tiS
U - Î106K A91t1FfS RJ te /1 /o.t►C IkAGMrG
--
—
-
- so--
_ —
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:
- -
q~
—
m-~--- —
.
- —r
-
-
ao •^ -r
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w-
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_;
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~
:t;.-1.5, 3 ~
. ~S o; •
.
- p U f ' -6
,5 _~ 41 cK
: of
- 4 no o .2icG 112 94 b• Z
„ ~=0Z _
: -
30 17.f ‘11- if, o.1
= 03 -
0 % .21 2 9i c:Y zo• i
- _ ~
_zz/t
-~,4.,.
'b -: \ r,o
\1 SG
- _ Uy
~S" Zli`i i j0 S0 0.: -
- b5. -
so--C ~c r - 06 0 z5a 312 12oa Pi p•
~// /~ 1 ~ " ~ }
_
_-
—
.3
so -
IOP-- __.
:
_ _ _ .. .. . _.
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole d-'6-b&
STXhc71-oc,
~nv~K .Z:a0 01-044 tli 76 H!r Srtr4: CcwackiTiE M MfrrleS H,lvr
M(Ssel.) OP-Jet:
Remarks
M. Ft. GRAPHIC SAMPLE ~~ DESCRIPTIVE LOG ~~
AS ANA~ ICM~
_
_ : n A : 0-9' Hu>rws
— y' -SD' -Gic`I-&,0 LA(.utiwui CLAY fkAty„r
— . Tv N►hccl ,CwaDAcr 4FcY CYA7 40 1111 — ap— ---,- K 12,, Cdzii..xcS iHé'7beoGrw,rbo5 luisoiaSrags3
•-. a ~ - So `• ~o' - N~6u~c Co~ EJtA Y urt rlu a11n4 P~.~yap
A = : é _ - rlrEnux Ifis 32,1 ?G '73 4p.1
— = e> : UI -C1AST5 Pec]bmnw4w•iCY Fr.ilcr 19165111.114" — `~ 4;. t~ tfN M~:Z CvP.t•Jlncs
_ -~:~ d- 65' - ric,nE Tu'. 11a.tnw.cs 7.8..+ CLAM _`et: - QZ p G° 19`1 6)r iZ 4•Z
- _ a'9 : f'CJ' 6et•lOcK~• Met 6Rrx).1-6RcY F.c,/A•et Fax/Swc*2,s
- ~o -1
Co pimp( T~ubsc~,~F rl.slaYtic
~~ - 63 r Ga~,~,~~ Py
— • rgrrisnts TO Eire. rLlree LntC.b„K ,MtAu7K
~ -
- to—
s —. — -
10——
—
- ao— —
— -
15 -... ~ 1
so - `h t;
'o— _ ~- 1s ~-`
S~
J
o _ ; _
-, -
=
Property/Area 1-16p1tSTI' /31)fl'L
Township
Claim No.
Location L t oL) I2tis-
Logged by
Sampler
Date(s) ,Ta.Jc 41&6
Drilling Co. 1 1t1H ~.S1kPn►x
Bit No CR 6.715.S-
Depth to bedrock 7e)'
Total depth
Sample screening XMto +-lo M3N
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole ii-b6 b9
'Property/Area
Township
IL'kS%h.c tJcur2( Date(s) 3-64.L ,e/ /j(.
Claim No. Drilling Co fJA447N 4 49rrY4rzJ
Location L G +cam ti; Bit No C4 E:76 â5
Depth to bedrock
Logged by ALL SAiic Total depth ,
Sampler mirk) Sample screening 'br'lc.1H
Remarks Simi .'--.3o Lék.•r,; (Ow4.1.1 i3,{
Ip,.,gti . ,3'i
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
Oic.(k3), AS ~ >?n !% l, /, >L
. U -1' /icmWS
-{ - .
- po — 7.
- _ ' I '-'1`i' -(414 t,(tEY Hfl+ed 4)43i(7 LACcita„~c' Cal
' - ".$?)YR-K 4J , ni /WM
- s0—
- i- 30—
10 — -
- . A`
" 40 - _ 4H-1(.' "1~+~ kCiiLY 60,8. w,rFl CulsrS
- - : 0141 C ol A(G.~Sti) bF Fu,xcr I,tx[•>w,cs Cu'.i.wecs, u 5Z:0 2.5,i 76 52 0.1 i '".':O.. -O.:''''' a► o 4.-4S CS ~GGF+Airt 02. Y.3) 25^i 1,70 'FF OS
1a — so
/// - 02 r l6 ' (~Z1?ocx ' -6e400(AN(7c,rrMdt,$ (LexlA,rc
- . F. 6cAuri} &rn calm dtvK How-
A 1 - /7.41.6 1 %4/ëCY Tui . 7u7-
- ~ - - Py _Tu(YSc~c,~+M.(Tc: 45 ~
-1_ _ . f. cy2~h ~b 4& S
_ w - -, - - a.; k 0-1 H
20 — - .. •Se $fbalki: OA is 6-434-e04u rîfca2 35' R, .Y_)'
rot _
- n - _ w~ _ 1 '
'S — - J :
_ -: 7
9°1 : _ . ~
-
9— — . 100-" -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-sc ao
Property/Area
Township
tiOiCS7nKc- /J01..IP4 Date(s) .21/k
Claim No. Drilling Co W - qiu t- icxaxxrl
Location t 2*Gc)é E-4-1Ç Bit No C6 (53
Depth to bedrock 37'
Logged by p~r Sogi<< Total depth 13'
Sampler I11-bra, 4k9.00 Sample screening ~ IO lhits►i
Remarks S74i 3:r~ Ii rr'emP0A,< 70 1/l7 Cauti.r13a -ir tO5S76(Y e)csot„tirA 6Y c'euLx.-icTlw.ic i i)Yr 6A43.4 Y-ov (>,c 6Y r4 Sl+vtcr FtAG"Zr'lC
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYT ICAL
/066) A5 CLc Zn
_ ~ _ A A
n . 0-1 4 Hu*w s
1 — .
- lo— - ~ -
- l'-30 4 -br.d= -cifc'Y N44.6 0.*040- LitcaSilCKe.` GAY - 5 ^
- ,
20 — — — SOF 7t1i 4,1 fi ,k,P'y
30 37' ' iluZu.AI( " HomaGct.rikJS G'ûA.ac2c Y
_ ^ ?lcc win/ td'!-i-:IK, ai- n1r11571.oi
- - o1a - C trs PA~>~zy r4,-,- rca~ tzo 3G loz 4,6 a so
~
lo— _' ..4:' . '‘ ,'~ =
- U ( D
C•Iw+:r , t<,rna Ml..pt Mmfic uoi.ce,vcs ~ ZSU i><5 Q~ 34 a Q . C~incs
- _ .,d ~ - Oz 0
01-1160x94 65 33Y vs OD 0.4
37' &AetcK:- R>çv>Ws TZ) tE. A folly pnti>tic J ' - +o -~ 03 /~- uc iC~e„rc t..+IrH Gp c..,. 71,10K
/!~ PyRr7<: Sæ.u6czS - _ - PY fiA.c61,t.j 4.4. dia/tu.-
15 — _ AQY
_
-
.
' 4' /'+4fUZïtYMcza0CeLcv)S 56.4,#
q ( ~IU,
_ _ y3 r ~ H
_ .o__ _ - _ - '7t)Y3 Ye grirlhc 61-14 IS 4✓tSN - 4.w4-1 AK RS.
_ 20 — -
TO — —
1 -
25 — — —
~ — 30 :
:
70 — — - 100~ —
Property/Area HW. liknr f :k moi
Township
Claim No
L C.cr>c , y, cb ti
Date(s)
Drilling Co
Bit No Location
k',t ry! . Slkna r nt)
G5 67d51
Depth to bedrock •
Total depth 4k3
Sample screening
Logged by
Sampler
AO: L!C + r?cSK
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-s6 91
Remarks S?h°T `1 h i'r.wiH S i`
liTIP'i4101 lt , du .ÇPr?c CekhxP/: RS H-Ç< 9cl ~ l'a~S)ntv ~'Xdcfl,nc~ By
~2 i✓ )N Ltti ,)3v $t'uiLC IKitC,ZRé
M. Ft. GRAPHIC SAMPLE GRAINS DESCRIPTIVE LOG , ANALYTICAL
4.,.(rYô, ►(S L. dA >}
: ~~ ~
_ : - Saint W)Td 60-1
- 0-`f ` %i~1113
- mo- - g'-`1`i' - 41.(4: -Ck'cY tHtilih Ci,hiiiicT i-AcoSTxt4 Cuff
- ~----
- - -~ • • y'-( -59' ' S1iR,l`/ 6ï,n+i:1 4o17H Gai.+.trS,Sauiu Pïxi'.cS 3p 36f; b3 . 0.3 ti re S~6-4.4.4.A
Su6-aou J .
- M,ITgoy Al $4,.6 _<< d, : 3A(C. - culS75 Nt&L[~GausvS fw~ Ac~71a'i.wi.icy (-.~,,iCC 11~5 99 lp sy O~z
n — ~
— - . ° - as ?hi. • LAni F>,.E. C,;,i„4 rwSç,i- P4,?,t &O.Z Po.,l 135 47 3z •ki 0.2 -
s0 J !~ ~ 53' k))ccUc; Sktctous "tut.. . ,~ CS -04,40) Ci2
- -~ i , ir - " I uk),u 6,,a ro., i'y SU, .(16(5
20— - ôG' -i.' r7CACll...c (HL)LskoGdtd.LX sn.ay
_ wurtn,rtc)
— - ,éGiJC ~•iruxur c,i~e,~c RFRsc g~'
- - ~-
a- -
- >to- -
10 —
-•
=
.~
- .° . : (-)i
/ --1 // STR,Aracki
2â— —
-~ 4— _
,0 - —
7 ~0 —• —
~ -
fo =
— — .n
.y
100— —
.-
_ ; C3` C o~H
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole W A 92
Property/Area
Township
/O"k Thrsc /3Q'nz Datels) SY 41;" ai l(6
Claim No Drilling Co Jiar/+ Rlc xn1
Location I G' c J Paw Bit No its 67153
Depth to bedrock
Total depth
yd
Logged by PAL,, 53
Sampler R•wtr.i k~ Sample screening +/v McSy
Remarks SpntT S1S Ùuwe•ICi- Or C'a+doc:a2 Audit 6:2G
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
AO DESCRIPTIVE LOG ANALYTICAL
_64041 /b " Cu. 2,,
-A A n - p-3' NurwS
- a --
-- 5— -
- 20 ---- -
- - 13' -LW ikA.it, son- Cal atlo4 frlc'y • 3'- .Iurc)
- - - 6wc Alfd apt/Act aca,trx,44 cuPy * Y '
- 7 - SoFrzac ow kiwi~__
10 — _. --- . .
,--
- _ ,0 ,_
_ - 4M =`IB t -S'f•+t1Y !R`Bbey C~ih+~t vine As. .À` " - ex I1tP. I{OI,,.M Cu4y5, *mg : or /..S4 $20 /44 io y6 04 ~
- •ra. - . : oz c Di 414011) -CLlsrs !/cRzrbGcwatbs ior Pk • yo ►'k1 Irz kg 0.3 Is — _ f~1e.~.4b~l,~ N,the LtYGI~xs G~iICc .
w ///// / - 03
-
- / , : 4, y5 ~ &~x: i%1oFx~s MkFiC Kxc,iogr
-1Oo or faCi+kwS k•r Wick-vi - -
- - : . ,Atlawl~ SAvkL % ~~) 1~.10 s 40 _ ~ -
TiZAZ 1b4s. oy.
><o — — = 53 ~ ta~N
70 -4( S+ti+o4 aA i5 4.1/1.2?-451,71.1 /LO►r 3s '
— - : Z'
- . _ ~ _ . YS—. - -
- -~ -
- 110 J ~
~ ~ :
70 — - - 100 — -
Property/Area
Township
Claim No
t b )4.), +2,1 A.)
Logged by
Sampler
~+fut û~6lL
lic,uLfes., k.f»tn
Date(s) T(ur ,22IFG
447/7 4 J./rgGn:J
C6 6ïtS1
Depth to bedrock SF
Total depth 60
Sample screening
Location
Drilling Co
Bit No
4/0 /McSo.(
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole II-CG-q3
Remarks
SAC $:,3v
r)415H /0:0(,
RTiL'afOfiruG A HIT SAy4E ks 044-It ,96 1.167 exPun,x-il 13y
Wits H<xe
M. Fr. `.
II.
GRAPHIC SAMPLE GRAINS DESCRIPTIVE LOG ANALYT ICAL
~ A~(RB) As . G. ~-n ~
1.,: d-l' HuvituS
_ - : r-yq " -471 610.yu SoFT. Cuff Cruâm►4 Alb
= - 60 -beuez aARd , Z4iMci LRCutsfl4+tr (by(
_ Ai 7'
- so- - - 35FRifc Uln/ OM
~ — 1 = ol AD ~ 19'• Sb f - Su6-406(4•f7 (>7tAuacy TN.L. l ~ ,34? ,!o c~ 6.y
- :.'2,..(`'~ - Di C '~i• iz= = ?~. ~„ : 1'44: S7h-4
- lo -r-
s- - "
io- - ~
- _ 1 =
- m-
40 - -
~ ~ - 1 -
so_t •a - s5`~►7k7tToLCufy,S'o2 45 143 117 .51 64
~~~4_ _ OZ U OtA(c.AS►4 •G,tSis P410,40w.rZY'1 • .b 24 WS ,S( 02 *tributs (,flr7/ F. C,l?Awai kilt biza A4,6 sT4Q0
- ~ - 03
~ S5-51 '- rr16QE Coty-Rttt{ Ai4 &C-
YO - - • Wt~
- _ - -al+srs PR~~azy kilt. -ri C45,.:_
_ ,
- _ - 56 / bC~ouc: 9ucaus ,'?Al( lkxCibwC [Jail 1-27,
_ + : Qyk l z Si►•wroE S
ie- - - -((7AP~~l~~u
~~CF{ R°5) , cï~~R A ,t.~I7- CZ '6rnr
~ rlr~ A~TqCdw 7a CAd6ou~
- - _ 3c yi„7pi pl A IS U►95N-Ixtwa 14.1 in' 7) LS
'
30- _
70 -
—
.0-
100- -
- -
t~N
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 1-i` -`t1
Property/Area
Township
No ,Sît /kcal. Date(s) ~~ azldl,
Claim No. Drilling Co l%i 111 . S44,14WOci
Location 1 Wt 41.2561 Bit No Ch 67 5C
Depth to bedrock
Logged by Da. Total depth (do'
Sampler kAfto IOMrl+{ Sample screening
Remarks STt?, T 1U:3c) ïiTiNMPAACI lb Nei CtwJouZar,
fhoiSN 1.Z:oo
M. Ft. c -. -
LOG • . - E
Na c", r
Au DESCRIPTIVE LOG ANALYTICAL
fitt#6) AS C4 rZ„
lo
IS
20
25
lo
A
OI A I ffR.
0-3' HurloS
,•y,2' - Lr6Hr bRo.;ru SorT CufY oruid.< i,fr0 Y-12' -
bcik-c1er 14.63 12.44cr eaca.tsnem4*
CcAti @ IC'
- SvruA c.uT:t ilea(
RJf -3y ~ - Auraucrtit 62Act;U.Y TkL t,rrTN
144-i¢1K oÉ f.SANJA
'-imabacY ucr.ximicS 9295~~r~ - ~tt.é Cu. lIIS M• urx
a-q(wAM) KirAcxis
4?gmS-Sa'?gmG4x~ I Fr1Sc rvri~
~ WI-A.46
~ Sil - Lip CuIS7S GARb~.~714fv
/e14 . r. s~~
DrNH[..4441Y M• Wtlta+lci,
5`I' ~j~txK c !lace-0S 61tARA) n- uoc .-L,ülil
ilw<stFc.f,..T G(!(I jpu,~4T1?iF11tw7
bo' ~~N•
-* SotAL a-R 15 1,11-StF&i3OJ
0.
E Sil~.uxt=1,
E -
10lead5b //6 ab
, lo
~
1
I
m
~
°
00
b • • a
••- ~
6-
G( b yS WI 117 kt 04
02 0 73C 256-256- ~ Cf So
03 o 110 512 95 'hl 04
so
l
I
(~ ~
ii1~AiACGbJS SAS
.
„
I00
1
i
1
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole it & -'s
Property/Area 1-16hkSn1KF Noun-? Date(s) .iUAé .7Z~dC-
Township
Claim No. Drilling Co 1-1r471-1 ¢3HekLcxA
Location L Ç*oo Bit No a 6?i;S1,
Depth to bedrock
Total depth
S2 Logged by SS
Sampler /Lôe.) 44n7C Sample screening ' IG ACV/
Remarks 9.,KT /2:10 ~k~i-TCL' or Cc..,t1~-~Z,12
F~+SN !'lo
M. f t. LOG GRAPHICSA~IPLE
No. GRAINS
Au DESCRIPTIVE LOG 2..t,,
ANALYTICAL
AdAod~ AS C.. n ~~ p- 1 ` NwduS -
-
t`- II ' -46,-IT 13/.0‘1W ecAY C,itAti,uG iNrU GzeY
b _
— eo - — wit, [ârlPbtT LACuS7K'hve; CLAY 47 ? '
— - -So0241 1.-0771 0714 -
- a~-=
_
-- —•_
10- ~
-1 -
- ~o r -
- -.11~ 01 `ii -S2' - /is16wb2 fi"R.4w.'b[Y TJtt 4474 M47KIK Oi. a. SAK4
Iw la los 92 04
- ~ -s - G 2 ~ ~• - Ca- S7 (U?w S~►~ Ru P~ôt~S ~ ~" 45 3(.v % 36 p,5 N _
~~ ~; 1~5 Qn ~cb~W/wi,vZy NyffK ttXCoh.rC$ _ 0 3 0 /0* /so 36 col - . tl ._ ~ b 6,,e.,
.f4o
y1s16' - n,A17uc- Cu. 1•s rv.ie tk.r_ehwee Crl
_ fr.ASrk+a S
_ `o - - 52 f &tga.1s . • ltoo&D...irvos nEhc bnLcA.,ic wnf
_ - 3`` FfAuv4: !f'e 3,1 ( . 20-- - ~
- - 00 S/GAwrrc4,7 1ttTggiffk`"
70= ~ ~M
~0 - ' 2b— -'
!0 -- ~
!0 — - 100 —
MPH) MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole ll- -(16
Property/Area dank3flM JJi llzL Date(s) ,22
Township
Claim No. Drilling Co /%r?r7/ +SHrX'(06),1
Location Bit No C6 67-5SZ.
Depth to bedrock '/3
Logged by Phz SiArc- Total depth yF
Sampler I~.aM ntb4) Sample screening F to
Remarks At►.r1ail.u4 1v (imuadcrLo2 AS 1.1-1t44SI Adr4cnrL'! `! L;?42am.t.1 fiw soi 2:30
M. Ft. GRA LOG
' ,-PLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
AL(013) As .
(1, X~
- A n - - n 4y I Hur+tuS
- ~ w -
5 — o
- 41-31
,-LI6+T 6(4:3 ,0v Sa-7 r CLAY GRA)bSC, Aux)
_ 6ux-6nrY NAa (oNtFiecT LACra57744c
Curl AT 6 '
- - Sotrt( Wdu lei°M - ao
w—
- 0111 1 Aek. N I-13 i - 4,...6afx t.îFAuttcy na 4yNlmiGX lylp g*/ Jbu Sâ 0.‘ .a: : Or M~A CS • .• o. :a: . , 0 f ~ O o+A& .>9w' - CcAsrs hitz+wdekeaos kb egu,06I76.)
,~j p lala kV.) 0A6
- lll l
AI,a ai &sea. st2 a,.S sern414
- ,tlkot ii,qa.b.os oi Limti 0.,_ is — A>07t6 IN MArK YOLCAm,K f~ -
0E-FurS .
_ '13' Ôtii7dxK -,Stl2iClnc SruCrods nY(-f( {,t)L. /.01/
Fi,., Liii.o) Pybrc As &ass, sTe4,6-
~ 1.9k3 (c/% )
- ~ - çcok G4Z60*i iri`il Aa,f ,
20 -- 41d 1 4-:01 14
7O V sri.J.'LE Pi-4 IS LirtSNbaklioabiq As' Rb`!fi '
. 25--
— ~
10— ~ ~
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H-E6 -91
Property/Area flenI 17 (t /.T& n2 Date(s) Tu. .a/i6
Township
Claim No Drilling Co ~°Nk! 4, k',txti)
Location L lU+c.eXJ l/foo10 Bit No C6 L 7d Sb
Depth to bedrock Il '
Logged by P,h4 Total depth y6
Sampler Acad...) k/Prqi ~ Sample screening flùive-Sii
Remarks 07Jxl 3:o0 AflI:Ir1P?a6 lr SAIL- CDn:i1JC7[y: 115 N4(,- 94 ALLb H•dc •?C-'P arT Cs • 624.4.3 L~SK Y~oo a2 4rJti i
M. Ft. GRAPHIC
LOG SAMPLE
N0. GRAINS
DESCRIPTIVE LOG ANALYTICAL
i(v (l~ip) l45 Cü gn ~ n n
a.;-
. D-t ' M.wtUS
- -,
5 — - -_
= I e-32 ' -Ll6flÎ 6B4.yu S,FT Cufy •CAtbuc wuly
- m 1-- - gu,c -6iey imieD CaMa eAeammy: CaY - h7 S' =—
- - _ - Salo2 caw )>g95771
io `~
"'Il '-/~J(uUFQ Nc~pGAsYhJ3 ~YtY MI- .
• - :4-
. ~ Q~ Mi. iv i11 lfs 11 0.1
• a o -~ e. - -,Ir~r,ec C~ ac,~ t4-At v~~ hu A
-~o
:.6:
~ ~`
~ 6
- - a2 J
b STbuu b2Ks ~~ o lu ratirc tkY.cAw c fka5r>WwS
135 6?6 5b Go Ad
03 - me. HL SA- uo Si G~3 ~ /
es - -
-, ~ //^
` L[[ Cl yl bcS►?cxK r30,c 4 nc ►t.t~ Lid pi .-61.6.t.40)
~* t~J~S k7 13' AA) 43.5 '( ~?y _ _ MS— 5o ~ - IVLK KoS7y R..d Slucioos IN vrc[AKy
_ : (n' oc-1.‘-S
_ - (: fc;wtcôtikc-W t A-rR`k y`l'
_ _ so
_ `f~ C fi.
20 — -
10 ~
.
25— - -
-~ -
-1 20— - - p0— -
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole N-si, t
Property/Area Nor16-S1NKE ~TouTEZ Date(s) /k.
Township
Claim No. Drilling Co iientr
Location L d {rn LJ ,1It251J Bit No a ofs~ Depth to bedrock 37
Logged by P&L Sale Total depth y2
Sampler kMQv Sample screening 4Io 4Si(
Remarks S17lkT y-.io ~2l~Lc~ a-1cr' hfow( Caon►viNG IuifTL.ar-" G._ 4v1Nmi Tit
f ~cNSFi 6,3e SrC71(Ai
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
A n n
ANALYTICAL
PA OM AS - Cu PA
- - 0-1 ' ll4Ot(u -, '
- 10—
_ - i'-26.-1 -LK,NT 840,.K, Sàr7 C(AY CIGfÀwÿ mra) 6uF-
s _ _ : CxrY N~fïc~ ()raffiaGiPw57iû~.,é C~YC 3'
: -3orrtnt urni DePik - xo -- -
- -- .26 :-3? ' -13+4444. HatsaeoGr44.xX 60644.Y Tact _4
..; _ ..
<~ 0r • p tRrx 5/1 ca rs v7o La(
e 1 8ao ?v ~ •
b P~s- m=.~.
io— _ A. : - Q[ 0 35 3~' - MAiZlkrAt 5u6-~C,4.ubc 1?..., SS06404.4.41j145- S42 US" 54 oL g
^ IOSCItlIt !Lea: CL /M rf_ WrGAmc - 03 0 los CtDF u3 la o.- - - 66'- ,--
~0 ~~//~/
~
-t.(.tSfS PŸci)~iw+~b..<Zy sCH(SR.üc rt-Ux
/(*,b i~ii4JlCE
-- - 37' - Srilcl714 , $GirS1US. /9ffIctoccoWlc wllt{ f-27
_ ~ 1:iA'c -0-AKcb 114 a' dYR•Arlers is— - -
°0 - : • S1YNoGcS:S Saicv•-‘111 6y eusTy /bsi4rit
— _ = 42' E~H.
so——
so— — -
_ to — ~
— : - _
-] -
_ :
- .3 -: _ • as — ] -
: - - -: ~
. SO
=
: _
: 90 — _ -
100— -
Property/Area Ncv1tiSTitki. la ra
Township
Claim No
Location L
BILL LtSic.i.
1‘.bic4J K,b•to
Date(s) Jv,~ .23 iFC
Drilling Co. l-Icl4A(
Bit No Cb 69F5~
Depth to bedrock 4.1(
Total depth 6
Sample screening
Logged by
Sampler 4- Iork-SH
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H-&6-q
Remarks 5/71):r aor✓ UP l4: CAC Aullk.i Cu "fr( CrCuî.tlacrS
F/lilst( & :~c,
M. Ft.
GRAPHIC SAMPLE GRANS ANALYTICAL DESCRIPTIVE LOG No. Au Rrk(rr6) AS G:L 2n
- n A 0-Y1 'Amos- ~ n n .
5 ~ - - •
_ _ @ e,
- ~( ~~~ t 6464x) &v-r r dr~w &rtY Ge.ferNr, . ~ ~ SI r
- __ ' %x.ul: - C,2rY H.f4iY Coy4AtcT tACoS74,4,6. att.(
,~,6 R - -_ vi 51'-`(' - 140-ezocavitbs AwGu-AyC Gt.ketcY TILL ly5 420 ,Kg 12 0,9
~ Lida M• Soh~.~ #.1#.1470(~ •,.. tg7
- - I.,rrN
— P~ùO~te.11~ll ~~ IE7eL.fwYiS (SOMEG1,Ies Ci Us' 3,14/ lï ,3ti '.a. i
_ so .—
Mo.r.0( 71 irx. , Cr,.xi. , 6e.MnncS
-,/// = 03
1 a~ Sor~ , Sdücrnc C~BGM r l7zij GrECu ~ 20 --, / / lil.TCwa51E( k->LG(n+rC ,
_ _ _ - ii)DPrlffiS 6riîFlwiOt= 0144.02AuZiilo.v
7 - Sp+du GR -C646 . ueirurri AT 64,'
4,1`t01H-
_ p _: - o
- w—
- -
- so-
to —
J
-I
-, _
-. .~ ---~ ~
-
~
O .
_ .
o` `
70
25 --• _ -
30 — -
-:
~ ~ ~ - J
= _
-] IOC) ~
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-ï6-w
Property/Area
Township
3MAL /50-121 Date(s) A4-
Claim No Drilling Co Neilm' #Sika.tiscX
Location L kr`c; (24 7Sa1 Bit No
Depth to bedrock '1L5'
Logged by ALL 161/.1- Total depth y}~
Sampler IL/IV ~ • KING Sample screening 4 k) McSI(
Remarks SnnIzT F:~z UPIOE OF Wick CLI 7(cc GC'Cokr•wtl-Z
rM,;Si-( 9:3o
M. Ft GRAPHIC
LOG SAMPLE
No. Au GRAINS ANALYTICAL
DESCRIPTIVE LOG 1 ~A fYA(~rn~ ~~]]~ ~7S C4 2..1 >~
-
-
S _
-
• to--,
-
-
ly —
!
Iro- -
25 —
-
-
30 -•-•
- ~l n P.
p-~ ~ Ht.~~,s
t f- 3+' -LIGHT BRa.yU cSbt=r Cu4y Gotclmr, imiz)
C7it1/ , m1/44CrsMAfG WasT7ttaE Ct.,t•Y I}T y'
-Soi-At um( ttionN
SI = ( ~•5~ Nc~S Ar.~446,.-4A GFAuecY T(cL rJlnl 114-n2iK or M- S•4164, Co681.1
N(`- .~ui. I,cr. Cc:d6t~ yz' wsFFtc wx. r~1!kc
,
`1? 5' 4cû/xOClr: -G~, CAC-Y rGea,.r1y Tui-L-tiukime
Uowt*ac 7L~r11t<~u5
- AtleriCS 641Z1 ~ 4 or Muzk.tL12dikrJ
ri,,l~c Py
.. Po55t(XY
-
--
io_
-
- so
. -
- - -
,
-
_ -' 1t0-
-.o
-
_ —
-
-•
- A
-.~~,
n 'c ~ b
~ • ' {~~
- :
01 llki. /HS â37 .290 Sv to.l
1?s ?YY los 49 0.1 02 -
D
Ibo 3r1 ?s 3C 10.r os ~
_
Illl/
. - ~ _
_ so —
-
_
b-
-
_
;
~ - :
_..i -
Ib --:
- 100—
:
-I -
,0
- -
_
_
-
_
- - - - - _ -
~
- -
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 11-S6 -161
Property/Area
Township
Hal\Talc( Date(s) ~GtJ 2i/S,
Claim No. Drilling Co. 114.47H . ,roky(.Yx
Location 1. /O+ObU t4 26- A-) Bit No CA (iç?
Depth to bedrock St`
Logged by hut JC161C' Sr
Total depth
Sampler /iIuuvraJ bf„2C> Sample screening + lo MrSN
Remarks .C1711CT I=05 6r0,40,66 n N/T Con; CItsC -'> PoSsiaY CYôtriiar}\ 6Y rLirrc iictiC,f, yc/
Frrwsf/ 14:61/tor lloxo?ci ,c/ üY fh+BUüCr L} /R( .ŸGarr/vh.,i /ÎtTz-KM40
M. F t. GRAPHIC LOG
SAMPLE No.
GRANS Au DESCRIPTIVE LOG
A N A LYT I CA L lû(Fr'd r}s Ca 2;, +~
0- i ' No4ui
- 1--- . _
lo,
~ 5 — -
- YO — '
~^
- 1 =S1 ' -1.1641T 61104.w SoFT ally 64114.4 GuTO — ao t - aey &...00,40- biconzwl; erAY AT 8'
lo — ~ • '-cS0FkYC L31ilf &V71{
- - r _ _ Si 6ctROUK ' -ilia i • 6LA(.4 t, MifFK UAc.c m6,r(
_~ ' - ('iii'tÔrNÿ /,dT1) Ax(,ku~uS ,i7~+'1~i
1 49z'+: sr-, G,ihPrl rZc ? -
- -' - - C FiCAciuc6 AT 55-•6 ' SHaaS -i-
is— - _ /}L IAA T/a,, CSesc *C/ilîQ' oru dor~/ 00 1
14 4.4 rK6 144tmît,~t~ Sr ~3 Fbe
_ J// !.
_ ~, fi;ikr*. L''
_
.o - _ S 6.1+1.
20 — 7.... -
~- _ H -
b ~ ~
25 — •- -
110 --I
10 — - - 100 .— -
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H- s4 raz
Property/Area
Township
f lama Date(s) 1.3I bG
Claim No. Drilling Co. MAN +Sr~ltckxv~
Location L 12t 1+d5 ry Bit No ('8 695.5b
Depth to bedrock 53
Logged by Total depth
Sampler kfi4c, -1- /uMcSN Sample screening
Remarks 5n}7-;T I-b R7r3vonA+c; lb Shedz (.twducrl>C rrs H-f(•lol !17'4-4141 "ib 6t Cl
1 4514 3:3o
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au
ANALYTICAL DESCRIPTIVE LOG
/44045) IS -
64 2~ ~y
_ n ^ . : n A ; 0-'1' NurtuS
~ _
- p-- -
a - -
- - >eo - ~ _
- ~- - `l~Gi ' •LIGHT tY~-at1 $orT Ci-el G¢fs3~G Mi.)- so— _._
io — - ' C2Acy HhM Cc~P~4cf /.40.102•4.4" a4-‘f@ S
.r ' - MucFI 36:41. LJ)TIj drri%d _ J
`1 40
~ IS —, — w —
so _
:o 7.1 _
`i`_ ~' • IÎCiL1t0(~cwcùuS AtiGu.1.L C1.Q/Ii.ttCY TILL (OHSl~ al
" CM
' % GL
. . —
_ _ ~ 6~.
'~ ,.e
: 01 C MA TRtx Or- F- SR74 , Cosa,' - CLR3TS P.OoMu.hr-,TL y FttSK-'•I.w. la .
- - .1 _ Q2 U
7-S -k2 ' - SI+wL' (LM w AN-mix rMlL~tatL Si" 912 1(4 3t 0.3
- z.5-7.
CuttT-éielPo[7t]j ~ IS •
as— ~ — ~~~‘ ~ ~ " _ 03 O 34' - MkNc (kiLfi. C,ic ~+.A~( c.rrt{
N-”v4nrr- rr1"..rtI OS- $35 1112 BD 5-?
- ~
~t",_ Se - ~10 I 7àutürt &A las 115 19 1.26 .52 Ob - Cy•J t)
K, a//////-:" 65 ~ Air'ss' Air' ~WG P1411.4611.;P1411.4611.;P1411.4611.;I
j7i>~ DF Du.
: g} 6r bRCXJC : 5(11(51211 -t- 14.1.61. c.,+7H f 4 Coi. a.), _ — ,1-7 41' b1o,,....6 &minit
30 _ if Eel H.
Logged by
Sampler /4441,1
PAUL 4:19C
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole ii-g"
Property/Area /Tairr7
Township
Claim No.
Location L wf•txxi 9.7510
Date(s) ~eft .Z315t
Drilling Co WOW #510cLioct\
Bit No Cb 015t
Depth to bedrock CS
Total depth 93
Sample screening f !o rial
Remarks Sig,tr 3K5
&Ali 9: Zo
471:#70 7ni6 t Ht i ôr!4t lovolucRa RS H-F6 -io l e !o Z y Arr13•fics 7D & /JP- I c~
M. Ft. LOG GRAPHICSANPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYT ICAL
WA/ As,
Cu. 2.,
_
~
s-
-
- io
~
~ so—
-
-
Es —
_ -nn n :
-
0-'4' /4040S
4'-62.'- bl.ck •6k-1 H446 Co+IMCT tAcuilgtit' It/P/
-MuC[{ Salet a.u7H bial
42'-4i' -NclTrato (ick.a)4 Cst414-Lt.Y 71u. -PcBB~i s S06-4wn.d ~ü /}uGwtrf - SCiMr CS. Cy2Rtnt1) ~2 .
G b 6c7ytacK' F+?r.W /crwtu~il Miff"(ltxc~qc SieitirEY
' RoitRf( jA C•kia.aldauÇ , C 10ikwaN SOFr - Hcseczd r+,oS Fee S'
9-3' ketH. 7
7
-,
- -
-
---- -_.~
-
--_,-
D0
—
-1 -
-
-,
is- ao -
.
~ ~
-
- -A ~ t Q •
1 CI I 1 ABR. +
2.a~(Pr>'U 4k~ Io5 'il cD. I
I J T0 / 1 1 7 02
// / !
•
.
4:11
~ -:
.] ; -
-:
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole
Property/Area H..31>}Kr n Date(s) IsG
Township
Claim No. Drilling Co +SNrraux,,
Location )- WKr, t3 916:),J Bit No Cb 6715i-
Depth to bedrock VD'
Logged by 16Ic::: Total depth
Sampler /1).;kici,., ICihdÙ Sample screening 4.lu ril. f
Remarks T `130 hDiuk ) -Jcc oF CrA.ACok
Fi~uSr{ S:►~>
M. Ft. LOG GRAPHIC SAMPLE No. GRAINS
Au DESCRIPTIVE LOG ANALYT ICAL
AK(PDdi AS CG. In A3 _ 1 n ^ 'l : - v-y' Hcrwlu.5
4 —
- ,o— -
S —
-
-
-
=
-
y 4-61 -G¢cV 114ù &Oka tAwar164. CLAY
m-
- >a - : — Mlxrf ~Sol-~c u~ i~i t1~ ,o— -
- . 40
rs — - - sD — -
11 — -
- Go ^
_, : 0141 0 4,5- SW 2Cc Plo 1.41
to — -.' d-i,' 7 4y131,' . NcilitGd+dUs 6iAu?a Y tü.L cor ni pl•fillK -!Z.: - : O► 0 of F. 5~ sow CaSaceS ~ SU G.* WS lu 46
- - ' ~• ' 0i A(4rbN) - QAS1S Su6-Gx,A.D zA..C,~..A~C 11..6 kc l~r+i m -l'
///:.' oz - ~~ m~y ra~F~c RIFF
-/~ ' 701 Ôt ii?c)U(: NoM0G:9,442,5 MILK GeV PYlFrC 1Nx17.4F - : L,irTH VWa, uc~ AT 72.5 `
- _ : - ►wcH F. 46h4.0 PV A~ GP ~
za—
w
- - V- 3rwjl[ ~2Mc (~ITif Cal,(fc7NIUGd•ciwS ~ _ r+r~Ykr4L
— J
so -
-
-
~ k~H.
-I _ : * yi,,ir'ct OIA t3 LASH-14:44%) tLL,nl SS ' Tv 9s"
!o — - -
loe —
,
1 -
Property/Area Né~ir arkk'e ~TcvrZ
Township
Claim No
Location L 16#o0,..3, 5.svu
Logged by
Sampler
PAL
1t,b;60 AA,.an
Date(s) ~in.: m2311!,
llLRp{ Srfc1.4xY41
a C7-isir
Depth to bedrock
Total depth GS
Sample screening
Drilling Co
Bit No
4 A.) MCSH
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole ,HA- dos
Remarks
Smr
farSs! 6:ti3-
Ft. LOG No. M. ANALYTICAL
DESCRIPTIVE LOG r (itt
, Ren AS
s
io
is
25
~
^~
0 S r MAWS
3'-o‘ -GRcr , 444 CaMRtcT acctvc.+t CcAY
- 140a1 Scow c.rrni &4,711
r - r `( SO 'Ikla206:ke-6,1S G1.4uOtY 7kL r yp2YM~br.wK
4,17), MARIA- dI~ F. Stud)
W -CHcaunc I401-Fu tti.u4.4( d).aerc - -muck/ Gf~+:6- C~ ~~a
3t it) ~- CLAMD~I~t N C~wcE,
'
~
I
1
~
w
~
--
+o
ao
so
}
.~ ~ ~
16- 2- ' t:`
16 •
Ii 0
.~r2.S
~~MMEiTâ
3zY sc u
~ 0•6 r
'if - as 02
03
i' AdR.
„ • \~,
0 95 04 S ri e6.1
Ari,, riux.
- 146142_"..A146142_"..A72) 406.41440;
" SD+a.: (t f cNj cut,/ IN m o k A7~CrK
SV r ' MACK /42Arct I/L' i OChcwct7 Sor7 f 6,46,cl1 (Whit
nit 430 llo •730 0.6 W U
ra 11111
~ ~ ?
,o
~
"Iili'dh2s lb Gc A SDckracFS Dr 4e-Ujfd
uGti.ers AT fi?.s ' r3 '
- tiC,wxdz 04 -U.e Gn rti,J,09/
S' C Q/ N.
Property/Area
Township
Claim No.
Location 1 kflX c-! qt)&
Logged by
Sampler
Date(s) +I i!
Drilling Co
H t?A! t-Sllexc,00A
Bit No
Cé G7-5 i9
Depth to bedrock ô`1.
Total depth 96
Sample screening , 1h-10 4 ry
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole /i- rr--ivb
Remarks Srer f u~
IIa SN 9:15
M. Ft. GRAPHIC
LOG oLE GINS DESCRIPTIVE LOG
ANALYTICAL /}k(t3'û) /iS Cu ~n ~
_n n - - - n p l N1 »w5
- : l.A.tT .20')
5 — — - -
10— — : `~i ~3 -Grey 1Httx6 ,cc,alMcr cACuS7Kue CIhY
- - h1ucH gdlbz wlrli dcilN% ié7u4t41 iciR
_ —= _ 0I01 73 =ry.,' - Cow1 a.x~.~.~ N~ruc,c„~a:s c,a~a t€o t i2 . ki s~ ac
- e •-•IGJs Ci) 5`l 0 ,; ~
_ --_ ~. - of ~ n• Va WrrH mdn;nr D! !Mc Si~4 RoO
~`.- s ?3-7b'- CtApS Pi1dtalArotiLY r Dai- - 7 ~
~ -~~
' p z t,nr ri,,,rrc II1rr,16,.,1c~ le (d~{ 9S • 'H 0./
zs— ,`ë~`^ 01'A(wAbM) ;S 'i~.s' - Malx1}~ ,Z1. CttgY, ct.ls~s t, .2992 9c 52 C•~ _ 7//1~ _ P42br)w~:LY Aa~ikc,Tz-,
_ C / ruxrl 4,1 tel F GFa,.ils el'
:,/ ~ I - V CtxairAa,S
_ : Ei•J &t'ex' ItwoEx.*eous lÿr-rtu< >1~tlifLzlÉ LLM•l
: - r'hwn CU.ucliL7k..44y Nia= @ El'
ici E ot H . 30 — MO ~ _ 4' ,94,-iPc<= 01 A 15 4AtsH-te.rù çie.).1 7i 'ro go'
~ - -
- q— -
J
— m- -
——
15 --+
20 — ~
!0 --- J — 11 — 1 '
y {o ~ —
10 — --
441- Q.o'., - _ G
- ~ vs u
Property/Area HO/alar J3i'12L
Township
Claim No.
Location L ^L.! 1125111
PAIL SOMr
4401.0 k/in7tJ
Date(s) .806
Drilling Co L-*mfS1'ô. til
Bit No C6 61159
Depth to bedrock h; i
Total depth /0
Sample screening •»/D FkZYI
Logged by
Sampler
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H-11v !07
Remarks S7NtT 9 dc,
Cicv SFf lo
M. Ft. LOG GRAPHIC SAMPLE
No. GRAINS
A~ DESCRIPTIVE LOG ANALYTICAL
flu. 09 lb . C4
R~
_ - _ nn
n 4 n
• If~1wS 0-4' ,
-
. ..-- a _ _,—
- — --
5 --
- m—
-
— !p—
10 —
L1'.- 7`1' . 1i6rlr aky NA4 Ctr+iAlcr GKutX•ui coy
-
rs — w _
~ • Mucrt Sai ,i i rd IOW
-
~ -_ 4
so =
--- -
.
so —
-y
io- -
_ 1 -
_
~ b?~~f:,
314 a U.,S --I~ - 0 i 7q:--114.0.4K--114.0.4K--114.0.4K2S U ' !{Û' ~c , ►~k~Eti.dk~S 6Eek.G3Lr 7k1 L.),41 ^' 7 V : . . ~ - Vt~Les
- 3yv ab CI :SI o. i -EL. dl - ry~pSlK or F 5/i,+d 7t.L Cursr Su/vacrrJj ,
_ - 4,ro ~• - 02 Me. -_-_.al-; rao ~
-CLAsn P~r2rA,.~•i,~.ay I}~6., didFK iKt. uttN
- - ~ -^ : =
> v 3 0
ruxa C,;,t..,ncs , LS. 1-i . 19J Soc. SS• ? f; o•y
,~ ~. ~j5- ios SUa:j,~rd n~ti ~c kt[~wc C,.~isrs .~t '
~ - 0`1 116Q. D CD"'~~ ~., G. ,~ b c-tixdt:k Zia- 3g,~ st I• o ao—
too~ ` --,
TPr.
_-..-. ‘k - os- i tk~ .
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-s6-1o7(2)
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
Jh (riiij !k (4 {n !~ ~~ OQe s -
- _ e e,a, - OS 103 ' 6rû,:aK= ÔLdCK-G',îry F.6~-c-riitwc~~:d►,cs
R' &: n~ fK ~xr.f>vac ,zsc (14& 130 -10 o.y
_ ~~
-
///~ - 64. '~~~ "! 7 Stv
- 110 - - OrP7rfSSl. - r~ (ie,ba.c ►~Y S~r~2S
/twA lrnuc.ic.~&,K.S i f~SSleir" hf~i7~u - ~ _ %,
38- - - lus- ' - 404-0 la Bt ac.n., A,orcrGiJus
- 7 5g4W1cti7 /Law
- = ~ - u~ r G4hvN, rk
_
Izo -*
Z :
- -
:
~GL ' - l'YKr7tc ( 17 ) ARs~ ~r~
f0 5' cau ~ H.
ISO -. ~
Io— _ -I _
:
-
-
140 -E
,
]
- 7 aa— 7 -
_ lso ~ ..
- 1 :
so —
-160
~
I '7 ] -
7 - ao - -
ss —
~
M0 -
~
;
. ,
MO - -
so-- - -
200- -
210 - - •
115 -,
_zso
-
-
:
-
.
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole I/ io e
Property/Area f10hi .Sft-,: J3Y TL Date(s) ,Z'iliG
Township
Claim No. Drilling Co +$ie flock
Location 1. X ,00,J, 10î5U Ai Bit No a 67459
Depth to bedrock ~Y
Logged by /141.4- S,rk[ Totol depth 1-9 Sampler iA 4~icll KM1D Sample screening 110 a+tC~k1'
Remarks SnI)Z r- lC-`IS- f411.)yik6 Ja HIT CukAamk pacSkScy k°K/lAmc).1 LSy 6? <net;
LraiSN /1:10 (.0440.5 rlvCif ,ÀiSfcwt,k.n3ki ~Y
M. Ft. LOG GRAPHICS+WPLE
No. Au GRAINS
DESCRIPTIVE LOG ~ , ) Q.A
- ~
-
6 —
-
10 —
_
10 —
-
zo—
-
_
cs —
_
o—
_
_ -
p-
9D
:
-
- ~—
.~ ~ so —
/1 A n
: -
l tt6~.
C} 5 ' Ku»tuS
•
g= g`1 ' 6cGE - GtrY H603 ,C6,4)4ci
I 61-4 (4,~ri,ti
$`I 8-t d x: 1iF/CAfS 7o r~ A StJ6HRy
Sck,cr7u Ant ~G- 1416604.l v
W6' ' .S&-, CR laëtu ffiva.r6 6Y
tutu< , i.G4h.4Ù , Mo*ko6û.da: s LocK
?G ' - Ca kic6 lxa.t.es i.,rnr ~if 4+46c•:sTlarnav, ti,-Z /1.7ki7„bS-S.->4,-.tat py
~1•' kG*106ia.coJ$ tax
79 . L.-7 11-1
}c sAY.trler 6141S 4tt5lzdoi.~ h~ii►+i 65 7b n (tfi:mQSr oh rbt1L-lCw4L)
,1LY, i: . iLy Lto k, 2
—
-
—
.
•-
-
-
~---
_
-
_
- - :
to — - _ =
- ~
to ~ _ -
pp. -
~~~~~/~ GI
. =
-- -
_ ., : :
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole 11-54-101
Property/Area /2c22 Date(s) 1-44:, 2•1/S4
Township
Claim No. Drilling Co 14u17N +,91Ei,.xxV~
Location .Zy II +Eù N Bit No. C6 C7i0
Depth to bedrock 8'1a
Logged by Total depth 91
Sampler fraao Sample screening
Remarks 57)}îT = Ii-SS iiTZ+Nlk16 ir HIT Seimk Ccv,:Jl.canî .b H- f6 - I0i ► iffir*:S TG f,t A CoknKi
r r~,SH JZ 3C) h7.,c<~ dyd,nc ~dw~cti.S
M. Ft. GRAPHIC LOG
SAMPLE GRAINS Na Au DESCRIPTIVE LOG ANALYTICAL
1vx(rro) HS Ck ~`
~
_
a —
-
-
io—r
~
IS ---I
20 —
-
28 —,
^
-
!o —
- -
tp
_ _n n
/\ i\ /1
: - p-(, ' tonus
L ~ -i1+KK 6itY N.t-K6 ,CGwlîe4t: G,tt4.)57Y'wr Cut'-(
-SaYfk ion-ti Delel1f
icy < (OW 1.5'-g7-6 ' - ~~+t ,44c~.ro6a~~7u3 Cut.i~ TI<
h7~47Tn OF F. 3✓4. >,, /Iwor /r~iS
?5-l; - K►tn,.w Cw Sa -iv w i'1 • ua. fih6ftc+w S
Ÿv- b4é~- a~Jif,tt. ly 1N ,'I• tia. , CA iŸ,zrts twrt. t,cxtwu<5 11N.,tn_~ +,~ nk
1b~c ~< ,0ï b76 :Sur , ' , C,'.'rY r :6,~t..ic11 iv/. ~ ,%~,w1
C, nc 6,7 6M4450 CŸ 04.4.14c 12630%.!
~v 1wZ+ k %Vl,nc $CA7r•'I lcÛa•h~.i v,',7d 4 r (.44,..1) CCaw4cTl,ws, 4k+K,2auS
0.i._
- - Ci.7yu
- CZ
.
_
__~-
m-
-
- - -
-
—~ -.
so—
-
--- - •
so-
J
-
i0 -
~
_
~
•
.
-
/p —
63C Hu bi
- -
-'
~
b ~. .
aA.~
-ra
lb. ' •
t r._
g¢ .' : a '
`` '0` ~
:
-
- O 3SG 13p I `I 0•6
0S 4.10tu 34E& vu yd • o.s
//1,1:'
f0 Sty( ~
- roo —
- -
- -
. = 1 tS
MPH Consulting Limited`
OVERBURDEN DRILL LOG Hole H-3e I'o
Property/Area
Township
{46ve13iNkr /Ja ra Date(s) •NlJ6
Claim No. Drilling Co kc*TH *Siidu.xx.~
Location L 1Y+rx• u ~*LGA Bit No C6 6C t 4ic"7d 37i•,$rioJS LnSï
Depth to bedrock /26'..5"
Logged by 14,.c JLW L Total depth l •
Sampler ii*=die-L.2 Moo Sample screening # lc flag
Remarks Nzr roc, /irk+•7PTMA 73 HIT 6.44.iCib/{ -•'i HIT $71:(KariGKS br 62 -(4.--6 U4.- eier6 .0
Ç4.),5./ -H 6
!'>'t „x HüG lcQ
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS AU DESCRIPTIVE LOG
ANALYTICAL
~(ii~ /7S (it X.,,~
_ "" -
11 r1 A
L,-y ` Hu+alos
~
- w—
s — -
- 20 ,
- - so-
a— ~-- _
_ .446' -C4-Y NlhcD CowlA4cr C1tccw-new.,- coty =
- ' - &Pak tJRN rhmN nail
15 — - - !0 —i
! _
.y .
_ -
20 — .'"-Z
~=
70 — -
- ~ -
-t - ~
_-
- ---~ p — .
25 — - -
-_ 85'-I25. ' T~eC
o°
~
:'°r : of 246e. .t45 Szb 11c vz &J-
• fS= 95 - ~u.,d: , rrcTrl~,..:wS, CobAcY
~~ - '•
, ,. : *,..•~' - QZ _ p C7ihL`c Q.477-( mdilpK Oe- r . S~ .
_ : ~ ' - Cc.+sn R~ tbh~M,M,,Zy F. c~.~~c.c~.►(
~ ~ ~~ 0. y
so — _ ~'~ a ~,
t : os G
ütiN ,SGw1r AA-A.À.- ~e.~ NCAiee~
l++ r,u.~n~il M wu.tti,c5 ~ - ~
U roo- ! .:~ 95-99 - CLAY-kIUi mienztX
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole 11-h-110
M. Ft. G GRAPHIC SAMPLE
, GRAINS ANALYTICAL
DESCRIPTIVE LOG Ar,Gi1;i As Cx; ~.n
-
-
-
„—
_
-
.r
~
! —
_
-
-
-
50 _
-
-
_
- 40 --
_
po -: , ~
- 1 ia —`(;.
: • - ~,
~'
120 -~~ ~ .,,
..-
_.•:4.-
~~<, . ~~,~. 1114 A.
• ~ '_ ~
7-ls' ;6 /•,' -
b:. ~ . -
x~ ',
_~9~t ~-` it'i , r,..e; -,, , 131
- 0'1 0 -
-: -
CL,tSi 5 /tc1bHU.ufn:RY Uri Lzx[sf~uCS, C.,,~,s,.<n C5
411. loci ' •aACt< JAR.) Nc701060.e0.,S 664,x7cy
&) V) li~ yj ai
- 06 .'
U Nrtxnhum(lr u tit C,..Ry nu ,+Yi~X,y /ES dCL' 5î 3S 0.2
-
o~ -
wiz
- PcasidLY CdvdrtY 5X,2~i &Is Co+kst[
oint ban.?134,-) 33`I jog ("125-5 '- ~.~xcrt141,7 ccA•Y-k,w m144•1 nLc
l6v So o1
- 07
- G
Om( HcX-+?alx.4.t3N5 CLd3T CctiaP-
651770%1 Rsr.ilwMrA Sr ~mcS
Nb'- C',F.A1.', rÉ $y y-.1c14
125 / 5 6c:644u<: D1t. C,atY 6ottkiS CxJKe//faiKcgt
4.0714 Srarwx~c~ or 2,40‘o.
Q? 121.QS
- grQ i >i S3te,osers Az teSsefMNAell
Cosvs tb Ala- iiirek assecktiri)
I,A rH ,2tb4CL►:aW<s
f2k•f3c' Afi$11064.4.05 G+-Rft
130 l, 01H .
7
Qp yav 12s by CY
J - 0 ir
..1 () l,U .Z3a rib 7b al
/
1
,' C4
'
45--
-
66-1OOi
-n_ sa •... ;
,,, _ ]
]
1
no— .~
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:
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-:
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: :oo-:
, +~
^
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Hi
-~~
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Mo
~
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- j ~
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: :1 _ ~ 7
:
7 - ~ ,
~ -
3 ~
~
. -I
-1
: - 7 ~
1
Property/Area /lOn1457/i /~kiir2
Township
Claim No
Location j c) 4+q3 N
Logged by
Sampler Iri4.ric>
Date(s) Siitti 414/ Re
Drilling Co f/c417/ t,(idtxj
Bit No C4 67i co
j l0 Mc~N Sample screening
Depth to bedrock
Total depth
'13
MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole )146-/i/
Remarks SPh"7 N 33
f•w.v~ S'.Zv
477-klvio1/44 7U or fltrit C'dwiLXrtx fis 11-f6-110 4-WrfiïS fr N444c Mai)
M. Ft. GRAPHIC LOG
SAMPLE No. GRAINS ~ DESCRIPTIVE LOG
ANALYTICAL
A;Wl As Cu 2 -n A -
_ _ A n : 0-41` humus
—
1 W _
5 — __
: - so— —
z •
->a~- - i0 --1
-
J - ; g'-f I . -Co i_Awsneo...k- cut-f - 40 — - -NA.acl,CtmtoNc ï 607 SoFlec c.u71f barN
_ !S — 1
6D ~ •
1
-
—
s0 -:
-I 1 YO — -=
70 —
~ 1
zs— Ci 4i '' Ri6cutx, Na~oCa>,ctNS ~:rtcn:2ty 7/Q. 4,001
MA7~2r>< oF r S~J
als:e,`
.. too y4C Irk d12
_
~4.`e
à ,•
,.: o6s. 01 0
: oh..:: . 02 lA6Q. - AJA-Tlué fi. c5et0u I,,, r1. tutitwi2C FitirviA .iS .2`IC IOC 7? S(. Q Z
- " 12/1////7 03 I~ - (LASTS P.rabwu•.w1.+Z Y All f,tY r.t..~c S
~b ~jc~litoCK: Sg)CcCIi7C, RoSÎY T~;Zxrkü.tiZ (kxC.h+'c itolaeL~ 3S K,0: 5 1
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MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole >(- h4
Property/Area
Township
l .-YNKr /JCtvT-2 Date(s) SitG
Claim No Drilling Co 1k*i,( ....NA-4(4S
Location L .3 400 r,'; 6FSDru Bit No CA G 7t40
Depth to bedrock
Logged by ►"&L 16 Total depth r
Sampler 14,, 10 4-10 rr14:91 Sample screening
Remarks 571i>`r -Y-.13 Aixr abT :•1w10ir7tJ) AS 8/T 14,24: 1kr7H /hub Mavaoei lb ~ ~/w:1 54id j :Uo ( tSrhi 714.: 4fc ~VLr A~ Q+HC Eiuoo Pkico2,7y
M. Ft. GRAPHIC LOG
SIMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL ~'~
L.(1L.(1)6) /Ij ~ c.,
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15 —
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40 .- 131 ' - CcAy'k I W ~l/f7'Waryc.frrH Cu1STS
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OVERBURDEN DRILL LOG Hole If )4 x,2(2)
M. N. GRAPHIC
LOG SAMpLEGRAINS
No. Au DESCRIPTIVE LOG ANALYTICAL
k(rio) NS (. ?,i !(
-
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530 azb kb i( I. t.) -
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,~~,;~ 9S0 9S! 95 Y
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11,5-120' tiz,wesT tnunncZ`/ T.ui. ui.r.. Ca544,.: S
121' Ci.r r Kchc r&M, (L`1
153 ` 6i.ur , dCFkcwkLY NfiCr~' Cch~(
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01...6 ~ '~ of i. -Cc rÎoWaC, 21C1 TZ~
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_
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OVERBURDEN DRILL LOG Hole H N7 /13
Property/Area NoMe3MKE /SooTLt Fnucu-& P Date(s) ~uLY .73 I K.
Township
Claim No. Drilling Co. Ilero41N + 90clxnIS
Location L ?6roo4J loroo S Bit No Cocain C6.00179
Depth to bedrock
Total depth
to 5.s '
Logged by P&L S&r lOry•5
Sampler SALcY AcgiaS0,0 Sample screening + 10 MCSN
Remarks S14+CT R.,io @Z,Li d,?Î SPo7-iki 70 HIT CdudUda,( H -9 Ai/d41cS TD 6é SUGHTcY bw,u-
F u~5r( h:3o (focY 4.i )
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M. Ft. GRAPHIC LOG
SAMPLE No.
GRAMS Au DESCRIPTIVE LOG
ANALYT ICAL
/i0.CA'65 AS Cu 2-,
-
a —
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10 —,
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so—
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_
a—
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.
0 -2' HuMuS
.2 '- 39 ' -Alue: -64eY H,t(J rnAA4u LAeu$i1C,wt C~itY
6143644 NM ($pF1tX,GRey Cosy LO IS '
- MwOK CuLi7S a te€26z$, 6IA.x4e3 of AQ4.,
Gott'
39-96 - /OW pa66y Aldi -SA.,J *Caw
- cows Actwi2t1 a.1J Nr~tRo~i>r~c w
, 4/S.-CZ FioOJ CLAY-AICI•1 A*YuLArt (is64cY TUL
15GCt~ti+1c~ rRbxr GAY-kith [J,%H 20TH f
- CLAM C-11/1D OE FRo>~l lG~S.t A Tu7.,a4Fec vou.t.xcs /'M*. s AS SEcTlo„1 àe2It,u
- M Wa( AAA., ~9dbR0, 6RAnx TILS 59' CO.Co68LE 4.3' 4H -CAAh fAAC,.muTS
CLAY -tei+1wt.T LoaS
65'- q I ' RxK,t t.t>< HaTtxo Gdurbo S 6P.tLrZ , in(9K1 K bF Mct +CS. SANI)
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Ter lkxuwcs û M,,,oY 614wncs,64.rC, MA-F(c l+u.kycs
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- CLksrs P(AyA,.00.7Z`T Fe1SeC va.cA,.ues IF (rtt.t i~lu,zs) W1Th M, ~x uM,GrA.,r,xs
Mbkurt 71' Qc,J,ic1) coo Tr FRA6,0.75 73' zu7 voL. (tali" 2o i$' SICICC-Cus Th FXA~.~ G i6' ~~ 1N+ACi. I► ?g' 1 fi voL Coe6eLx Si' MkFIc. (RR._ Ca66cc
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- 0 9 230 166 15 0 74
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-SL-tr3 (2)
M. Ft. GRAPHIC
LOG PLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
41...ill0% 45 Cc. Rw )4~
ao W~ 2:56 I Ht., Is r1w, Dr241 TO CHA..tCié tri
- tz Ia,~ ~45 !76 Po
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- ~ ~, - / 106.s. -OxrDr~ CC0660( GRAut;l L ~t7~X,fni gy `- 1AS.
- no
:--
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; 13
of fAcil.-► Cs. SrIn,J,Af~c~cS cR~.~~v~
• CtitS1$ R►IG 34-64. AwI P¢e- :•. -
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in -:
Ei ~ - Nam( /I. I/OL. COBBté
- 90` ?fuT t+tA, C6ddL~
- A~RlitLf.►>E RAGSUf171 R~Y
: : lYIGR` (,r,egS
: 41' - SrHtS103e lui GaxCc /lzov - Felrolov75
.C_, 'so -:
- ..] , 45' -C1«rDfirt NOtfâ6oz i,v (ir.l►cE
: : - Cum (ici1bmMn•aLY 341S. _ = loo` Ff2SrC To* Cbtidce
- : 7 103i 64ttcr ,8fbser,,fc 61)E6t,6
- mg) 7 fo5` CS. -(yPi404 R0Sr! Oa
- -] ,.ÿ 6.45 bfT 6r4u1J4 -+ SIA~u A5414 AT 4,1)00
+D _ _
?
ac --1
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- ~ IG9 C KYi.s` - 42-Cet6 u~u5 ‘u~~tS - 7
No -
: Ü MkVfsc Ffaué -61tAiaeÿ
t;~+►Ic'bRéL PY
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ao _ : : hçkocr,tfia) 43)iit t>!!aS ,
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55 — 7: .
-
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole R-R.-/H
Property/Area 1>'tot SPfKé 1Sou'rkz. Focwc.)-oP Date(s) ~txY .23/;rG
Township
Claim No. Drilling Co 110401 •r SK .2ror5
Location 4-00 11+546 Bit No CO= t 7t
Depth to bedrock 89
Logged by A)L Sodrt Total depth loo'
Sampler tiS4e..cY Rob.JSoti1 Sample screening 4 10 MCS+,'
Remarks SAL47 4:00 SAS170\ 7D NIT CG~c1fraCAk; /{ -+ AA/axK.S Holft.E ti@2+U ScYLCSL~x gasti .2:oo
M. LOG Ft. • No. Aa DESCRIPTIVE LOG
ANALYTICAL
io
Is
ts
O
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A A A it
-•1' • Homo S
1-1'-2•1' •BLt.t;-Gec`! H+Kôi Caw+tAci tAGuara,Nc CufY
- SpftiB( tJthl h:TH
z`1 i- N:: -~
, A:t~t,y 6~t c..11-pi » Ih7R+x OF Flak
• - CAM sue,- Rouwù 76 SA-415(-4-44 1 Pltr.1:r+1 -
)WW1"( lbtcrt~n[s, Gbb~++7lcS 4.3101s17K MraoR
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' Pq~F7Kix SufYaC7ët (La?a7, Ca.+ly Jo •!da F. f
- OASIS ~Rt-ISoHrw~2y ?lu 1. +s MAftc vet.,
OM S} i.51714Mtooe 1~16'GM+17tcs 3€'-2rur IbL. Ce66ch C.)gz •CA~R6 vtd~ceE
bk'M+FfiE WIG 'kb( TAIT • te.v.. Cabbt.r qi! a#11-16.4,010.17 Lela Uj>}1 mum(
'7 Curas ra(. fil. va..) /414./ . : •, IF I GIt 6 1'F
.{q'.4y ' Sod-A►Y,u+h( Hc7tY0Grueoo5 ?t66+.Y riRArlL Wt7H +`'iA•TfIK OF P7. .5.9i41
52' D+oi(+nc CAM6`~ 35 =W `- ttittbrèrD 5~1.ia1Y t~1ll7itl Dawn)
ac Co8bc6 /1 - MuU1 PtoKr rm.. ,Grat.nna
4Y-43S' - dCt~l~ Ct+IY•R+a1 R+runc~ 7tL.t. ?co. bY Cnt,a TF) trcrS7Tr, F.ueL.
bc' -CHL. ri. tbl-. Ca►bLc
6a'— 7Cu»uTl~ <AtShi~ i AuCH SuICa~lI
CAIN'S
Va >1 i ' _~stt; ot. cc6&.c
4.2' - GAGblztc Ca66L
73.5-841' C9t+l)iA CrbBLY Ga.tlwlTH Mb71Ux t>F
MrL-+a• St.--+>) (kr.xye,c471L(.?)
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- APAA& Ciau+182.Y So+:na
zo ~
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12
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13 ZD JIS 24 40 0.1 1s( 39 litô., ?=--'• 800 22i, t, 0•2 so
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15
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N-t6 Jr'( (2)
M. Ft. GRAPHIC I N~ GRAINS LOG
ANALYTICAL
-
-
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38—
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-
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:
,
Property/Area HOWYAKE /.7GoltZ kW :Q-0P
Township
Claim No.
L Si +Oo.-.i 1.2+203
Logged by
Sampler
19vL So61é
541.7 1.06.45as
Date(s) ScxY •23A4
Drilling Co.
Bit No
Depth to bedrock 4.5 '
Total depth
Sample screening 4 /017C.SH
Location
9/tR1.t7D~
cocoa
/ /1\♦ MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole ii-ac-us-
Remarks Sti4RT .2:Uo Fwr&1' S`fS
36774 2) CD„i,c>1xc H-+ JcxCZ.SkxcY Mg: Cca'srh,cnLt
e.PJnizi.1Nr>S Ikobldr.Y cSu6NT(Y cru 7111é roOT- . kL d
M. Ft. GRA PN~ LOG No.
GRAINSSAMPLE Au DESCRIPTIVE LOG
A N ALYT I CA L
4.(M' iiS 6. krk
-
e-
-
- -
-
i0-
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~ —
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RS Cd++AtcT AS ,tnc~ArcY <MI) - vast L/TJtt Rc?uC~
. ,
y y :~' - Sub-Ro~ ,b 34)41,..4.1.4.*34)41,..4.1.4.* l.aosE la3 ,,c/X r e~~s I!'~6.~( G1(A ~
. or Fl.,é To elot S44•1i - - -r~.,~r~y ,. ~~ ~ f
- Cutsts Acclbr4IM+6ri.y Gftulirci, Casr♦ Far uolr.t,at5 r.Ir01 Swell r~J~ w~ I~,
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117 80 68 : OZ
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alt ~a
-
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SG' •T+tf7b Werb~ 6RAuiL -4i6846 Cc66tE
44' - SfK1cr7K F-txx. Co6b+.r CA' - i(a1•rY ClntQs)411 3t C6del,r
W -GEAwli2 Cbb6+.L:
Pl F6'.9 ( ~- Fw4 nK~~l~,s~I.0d u M155o5c bo,*rl
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ÿ l -9 .3' Jâ~üwlte ~L7 ()Me. kp,,,4p~ fir Sttlurt F. UN. F„~ r~ba~ $t,.l~
q3' (,d2YlocX: So('ï c• ,ik17 Atli QM FkLSIC VOL ACKt+Mt5
47.5. 9b i- Se7{1C1TK kZSrc z 7ur. Ud.CA..< urTt-1
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MPH MPH Consulting Limited
OVERBURDEN DRILL LOG
Hole (2)
M. Ff LOG p~ CI~~~ NS DESCRIPTIVE LOG
ANALYTICAL
-
-
-
26 _
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_
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40—
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.
48.---
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Nlt)CFR Ckt6cu4ï ~2+09.t KuHc`DtgZ
ei,tss,ul Py , r714101( .ViQiciX hti~C93kLJ
193.5'-IoS' Sori"c,Rst7( brne
105' k"ql•{ .
F
Property/Area Nar74:.5114KL iSct.at /acc.a,3- tao
Township
Claim No.
Location L 1 t: Ht 375
Date(s) JucY 2-th a.
HORN +SHltt.>za)
C0001~'t 64.74i2o
Drilling Co.
Bit No
Depth to bedrock
Total depth
Sample screening
120'
12C.S'
+10 016.1
Logged by
Sampler
P4tt ,S6t~ cSAtLY RoG.uSov
/%/I~\
MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N-se , t16
Remarks .iT>4+CT il:Ot) SPeTR-1) 15 HIT Cbmkat)R N -• fiff&»RS InmRccUM C,wiocrtu:
F/IufSH Ia.SS (Ro83lata+b Atrt. 25 14 ) éivurrW.ayto,sr ,SuGNT(Y Gu 7-1i; HArJC,1aG 4:X1-L ârd~
M. Ft. ~~ SAMPLE E (>~ DESCRIPTIVE LOG ANALYTICAL
/1,4(1,) As 6, .En
-
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OVERBURDEN DRILL LOG Hole H•F6 !I6
M. Ft. GRAPHIC
C SAMPLE G~ ANALYTICAL 16 DESCRIPTIVE LOG 4c.. (FM) 4s Ci. R~ 44
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Claim No.
C 1o•oot; 1;+ 2~5
Logged by
Sampler
PAtt &Str'
SAccv Ro6,n,sonl
Date(s) JuCY .15 EC
Drilling Co
Bit No
NrA7N + SKC7tr.rdD
1S G 742 i
Depth to bedrock
Total depth
E.i•S'
45 '
Sample screening
4 /o MéSH
Location
MPH) MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-c4-I1?
Remarks 5774,C7 8:3o ( 7todS)
Av13N %Z:oo
SPo77d5 7D N,7 Coxr&upDR K$06MTCY j>«-w ScCctcSSn.ccv
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M. Ft. GRAPHIC SAMPLE GRAINS ANALYTICAL
LOG No. Au DESCRIPTIVE LOG
~ i4i t an i.
- to --:t
;A n ~.2' iyuMuS
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2'-'16 ' - 611,>; -Grtc^l N►l+tJ Caw►IAcr LACuSTItwÈ
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- _'~=~ Y _ - Cotas ( freias, cowes Ptcateiµtwuv aft.' - 2) 5" 472 is og n.
_ „2ilis' Uiai Mtaoe n1AfrC VtxcMeS 2,
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OVERBURDEN DRILL LOG Hole ►14-1/7(z)
M. Ft. GRAPHIC SAMPLE GRAINS ANALYTICAL
LOG No. Au DESCRIPTIVE LOG
,:`— :
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OVERBURDEN DRILL LOG Hole H-K-IIe3
Property/Area
Township
Hook-S7**" ITouret. Fol.690.0p Dote(s) TOLY ..t4 I 14,
Claim No. Drilling Co. Flea/ .4 Stiett.bo3
Location Laftok 14#374 BR No. 6 47i.0 6 OM, 601.2. C000lf4 -
Depth to bedrock 124
Logged by AA. Spew Total depth 1.54"
Sampler S4LLY Robas Sample screening 410 ofiSti
Remarks STRRT R:.3o (MAY 2517 ) Sort-' 7e4 HIT ect4gLict1f SixaSivaY L'AZZAki CopuboorivE &um— rSH .R:oo e7uLY4 ameadr
M. Ft. LOG E
No. DESCRIPTIVE LOG A NA LYT CA L
Au(PIC I 4 I 2,4‘
io
15
to
:
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Fmk it50
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CibtwInCS , 61•60.0S - Co6Siz3 itU. t44Fic itx.choics
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vccos.mcs 6 pliA304 sr Atisluili '.Jr,
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: a I Ar,„ ,".
lb 3:1 0 Pou.k.Al.t.Os-, isir Ft.oisticoS
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OVERBURDEN DRILL LOG Hole x--llrr62)
M. Ft. GRAPHIC
LOG SAMPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
-
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36-+
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ur~ 113'• Jh4F►C UocCA,~C 6o1.cd,~c wail Qt-Ut6,
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44 A$ c., i..,. t13
0.(17
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, - I u *So 911. l i 1 18 0. i}
: 15
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-
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1(4- 712 fil !
s
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al , -ftuuuAc FicA6/46.7S, Itu3YY F obc. ► pe
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31,k7 Au.)9: 00 + Iwo de rm001i''1 451.4)
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sr+ecr,GAK1 *7 12:34) NM) 6Tl6674222
1 z~f-121.'- 4061.4.0 PP460/~u 1b*~M•~►~t BY lMNtc
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CAd6o1.147)k]~ Te.GYGbuK Gi171{ SLAW
1glx+e~, MMIOC Or•r~%py bt9wxrf?
12f' 64.1E of IkthtArt 1k.Tt'tA'lau 44 I~fSLuc IY ~S/k9w5 ION
U•c11~i.é 041#1,7( 131' 37ux owl F6a41.a1 rUKSu.é
py
1,52' STcaxcnKlcS OF Q+•Gh(6 W>•++'r.û, MICAp-Ix9w42S 111.1 LeSS-RtiL+1tp, 1)11. !><. Y
ISt•J ' kw( MIIkSU14: 1 •CJd Lela • Pr
1335 ' INONcrit 1y1G71C max) MI G9t,-
. 6,4“724 utcctaClc
31' - h9►aal ~SSt'1iM•1.MRÙ A/ )4
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9- Nor_E SAW 7b 1.144 . ~sr M/SScb 7ifc m4.43
aHK►?c 6.,t: ci: 7lé Co,uà,c7be ou Ili FOOT-
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GpKS Cr Ce -6106 -Oy ~u+fl$, MIUcll~Mxr13
, l'tA6n4#7S
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a,. - IQ t' 12A1 7 Sl 176 1-1
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~~P MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-K-r/q
Property/Area HA'1ESr4ri bora trXtex.1-u0 Date(s) SW/ 2c iêG
Township
Claim No. Drilling Co HeKni + 5Ne4.kn1.1
Location 1 4t00r t2+7S1 , Bit No 64 9422
Depth to bedrock 601
Logged by A4uc,s4yc Total depth b?
Sampler .SFktY itAdµtSaJ Sample screening ;lo A1ESd
Remarks ACT .2110 9brtd llkiCç or Couhocnt H -+ AoSS,ec Y kurfakb A !maxi (AIN 1.057YGK6.)
body 3:5b
M. Ft. LOG GRAPHICTS4MPLE
No. GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
AuUlt * Co, 2n ~
-
_
-
_
-
io -r
-
_
20 —
-
-
2S—
30—
-A n ^ -
-
0-2' HuswS
2'44/.6 ' LT. âfc1..0 Ctllly (MI" ]Ar7o Etu1: -(VIeY hik;, Combla yAC.ut7Ami GaY 47 /h'
.2'i S 1 Î9D' - Low Nr~t S.6-~l+.Yw/+c Para Crt9tk+. ùMfb+rtrt2l 6Y 6t~w+nrs, ;kart 7D Tu7c+Q~►Qs£ kx4fw oak JdWD( , SaDS ZF - ,497eIK .><à. /0 Cs. So1"4
.2s-S`. •275'- ChcoRlnc MOIL yxxuac t+~x Î~ Sio7o oa./y 3rltw.Gacs y MdsLw 1d>~, F►~Jc -6
31' - G" ecAur tun yeas 3/. Fr7src t,<k c,hurc coo~, SL1wIerA[, u,al uorc,
S~ Fwt,ltJNb1 bssa~ttaD C.,r,dIOA~ >5y 31' <gYotrAc Aufa uoww C Gatti y`!'•64teoD mtaa 45'• nncrac ccdeli psout n~.rv-.Eso4 Y?'•S~+ rrc feu( tkxcAmc rrds.~ 3c')'-6cllCe; ~‘ 6aos+w4 PtAbI( eoiucnR+e►sOF
'?S ~C ILiC.lc C alai SS '- M rvei( ysAY W A1N7L1X, MuCN dA'ZLew►T6
IF Ili 7114 -
110' AIWA: kWIIAuEtY SdticrTlC kLSiC (aDlGf+wC i)17t1 1!
1ju,.t.
~Qt• .10* Py ' 00 e 42' i I-31, Fie( •
u~^..cD EwIr7lt~IL FYI
4.5•6' -.1$00 A RostY A~ .. Git~m,.clrE Ito?
balk 143-'UIre%!c Sluteaos, SrtgaK Fe35r VotCA0C të7lxukis
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" 30 27b I f 3 ° Loa :
: OS $0 3 86 13 31 0-3
: Oi~ . g5 1C,2. 12 l9
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110 =
- 100'7
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=
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Property/Area NeMr5771KE Po/AZ i-oP
Township
Claim No
Location HfbâS
Logged by
Sampler
ATASioi
S+ltcY /labstio
Datels} -SLY .tG 2q/S,
Drilling Co E/aVPSNdWkaÛ
Bit No d63rix r d ïriz3
Sample screening +[o AIM
Depth to bedrock
Total depth
111
MPH Consulting Limited
OVERBURDEN DRILL LOG Hole x k -i
Remarks S/1hfT 1:2n (SkxyA}
4015;1 /4:00 (:,ac y zf)
SlonA Ta 11,7 LAW C044234 &a77/ Oi H' + Kali Aisub,Jol cXrN ags; (aveS
litchi ha? 6iT 4Ati hcric.td HGtr 4u11 lkIA4e,4 SelpA Air
M. Ft. GRAPHIC LOG
SAMPLE Na
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
A4(feS) AS
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3G~•FtlSic WüAwc Co6iiz c.AÎrs 1r0w4 6y.(~Ls'Ic-+Iti; IkCCA,.t( 5,446
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MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N-54'126 4)
M. Ft. GRAPHIC SAMPLE GRAINS
NO. Au DESCRIPTIVE LOG ANALYTICAL
&A) As G. .g., 100 -:44 •} _ 9'~ • W. U+~n1r24 Su6-Itouwkil Pz6&Y 0-41011.
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- ~• 09 112'-g,, tckY Logs
vs— - crkolr3k P>:Irrc uScc.M.vc Ca64rr
_ : : 11.31 - Sc'r<10714, , SarceDuS hcs+c va • 120 -:~ &DOLc
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Property/Area NO>'gn ti / J7ZL hX.OJ-c
Township
Claim No.
Location 1 rb+cnr), /9+61,51
Logged by
Sampler
Octets) -TUN ?? jâL
Drilling Co. Nc'91N 4 Sile.a.1013
Bit No S67924
Depth to bedrock /2f
Total depth 1.53
Sample screening 4 ID mail
&& SRccY Ro61wso4
MPH MPH Consulting Limited'
OVERBURDEN DRILL LOG Hole H -I?1
Remarks S7'bc1 Ib:30
h4WSK 3:So
90774 1) N/7 ketc CauDtriIt .SaI,Ar or X 1Sn. kr,•t K•16•/20 fi46+44o4) -s faS1601 J71ttSRAt (*45E Gk GtuS (0frhtetx.v
M. Ft. CiRAPFqC LOG
SAMPLE No,
GRANS Au DESCRIPTIVE LOG
ANALYTICAL
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OVERBURDEN DRILL LOG Hole RA-1,2 (1')
M. Ft. GRAPHIC
LAG SAMPLE
No. GRAINS
Au ANALYTICAL
DESCRIPTIVE LOG 4.(w61
SS Ca t., , t 100 ..:.!6 d.- 1!. - Pi,Hkl[ IHa~IuM nCS. SA..~
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- no. ~ - R0.96Ie0.v aaSESoZ LSO; 4r 11605 ..
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Property/Area He&37t?KE I.70u1k2 &Leo-OP
Township
Claim No.
Location Z ?ktoo4 ) 1Y+.SYS
356tc
914,1 gelyacA,1
Date(s) Jur.Y .17 .?F JiG
Drilling Co RAN +.Ÿlr'KcbtA
Bit No 6474
Depth to bedrock 102 '
Total depth 109
Sample screening
Logged by
Sampler a la Mt'SH
MPH) MPH Consulting Limited
OVERBURDEN DRILL LOG Hole
Remarks S7M027 .P30 (7atY.27)
FturSH 9:ov (0ii+ty J. S)
3,074 70 167 L.iH4K CauALzrert SotlPf ctic H -+ ciuScicusFuc lat ASS/SLY
raki 3F CAt A AWL&
M. F t. GRAPHIC~SAMPLE PL.E GRAINS DESCRIPTIVE LOG ANALYTICAL
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MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H rc -'f.2'
M. Ft. GRAPHIC
LOG SAMPLE
Na GRAINS
Au DESCRIPTIVE LOG ANALYTICAL
VP9S) As Ck L 43
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MPH MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H-S /.23
Property/Area i 1EÇi*i JAL 1bcl.ou-OP Date(s) ~cxi .2d~dG
Township
Claim No. Drilling Co Hem ' 94dittroU6
Location L .2400: H..26 - Bit No d 479ô
Depth to bedrock
Total depth
735'
Logged by P4.,L Smite
Sampler Skit I(5ba15oU Sample screening ,HoPttall
Remarks 571UfT ID:oo 91:01t% 3u64rnY 2bil4-/cr" o< K 7a lvuanail% HtEr► fli -PHASw
i aNCH Avows/ iba7Ktaft, ',Tam .StlNST /1dU3xJ
M. Ft. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYT ICAL
&l/P6 >tS G, R.,
-
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Township
Claim No.
Location L 41#6d0 . 13+25 S
Logged by
Sampler
P4.4 ,~~
Stilt Y Aaawsaa
Date(s) JU(Y .?f ~âC
lueti11' SHe1lc,bpt~
66?4DG
*Io /
Drilling Co
Bit No
Sample screening
Depth to bedrock
Total depth
ISZ ~
ts~ '
~MPH~ MPH Consulting Limited
OVERBURDEN DRILL LOG Hole H &,-/2'
Remarks
,SPfi(Tf'YS
Fi,uürl 620
S$a A H ,î ifrouhuc7pQ tl ^')So4afixcY Ptk,rP>Ag XoMcrlakibtzS
6/./901 7?.
M. F. GRAPHIC LOG
SAMPLE No.
GRAINS Au DESCRIPTIVE LOG
ANALYTICAL
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M H MPH Consulting Limited
OVERBURDEN DRILL LOG Hole N•6612v(2 )
M. Ft. ~~ ~ ~~ .
~~ DESCRIPTIVE LOG ANALYTICAL
A~(~I /Is G1 /4 ~ ~
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APPENDIX E
Overburden and Bedrock Geology Results
Upper Clastics Lower Clastics Depth Total Hole Organics Clay Silt/Sand (Mainly Till) (Mainly Till) to Bedrock Depth Bedrock
felsic-int. tuff felsic tuff int. tuff chemical sed. felsic tuff int. to felsic tuff int. volcanic white rock paste int. vole./diorite felsic tuff int. volcanic mafic volcanic argillite mafic volcanic int. to mafic vole. mafic volcanic argillite argillite/mudstone argillite int. tuff/diorite int. to mafic volcanic chemical sediments greywacke/siltstone int. volcanic mudstone/siltstone argillite/mudstone argillite/mudstone felsic volcanic mafic volcanic felsic to int. volcanic felsic to int. volcanic dacite argillite greywacke greywacke
H-86-36 10 73 30 113 123.0 H-86-37 9 52 20 103 108.0 H-86-38 10 71 13 16 110 115.0 H-86-39 10 70 10 38 128 133.0 H-86-40 10 39 16 13 78 83.0 H-86-41 4 36 0.3 40.3 45.0 H-86-42 3 75 2 80 85.0 H-86-43 5 67 16? 88 93.0 H-86-44 8 46 54 59.0 H-86-45 5 65 15 32 117 122.0 H-86-46 3 47 2 52 55.0 H-86-47 4 42 4 2 52 57.0 H-86-48 5 86 21.5 112.5 117.0 H-86-49 5 51 1 57 62.0 H-86-50 4 52 2 2 60 65.0 H-86-51 3 70 7 1 81 85.0 H-86-52 4 62 4 2 72 75.0 H-86-53 5 55 12 5 H-86-54 4 53 5 62 66.0 H-86-55 4 61 21 7 93 97.0 H-86-56 4 72 11 18 10 115 120.0 H-86-57 10 60 11 19 20? 120 125.0 H-86-58 6 99 30 135 140.0 H-86-59 4 54 3 6.5 69.5 75.0 H-86-60 4 42 5 51 57.0 H-86-61 3 53 8 2 66 70.0 H-86-62 5 25 3 31 35.0 H-86-63 5 87 28 37 157 161.5 H-86-64 4 41 25 6 76 82.0 H-86-65 3 53 26 1 83 89.0 H-86-66 3 57 35 3.4 1? 101 106.0 H-86-67 3 43 38 0.5 84.5 89.0 H-86-68 4 61 - 3 68 75.0 H-86-69 4 29 - 1 34 40.0 îl-86-70 4 5 - 4 13 n 20.0
Upper Clastics Lower Clastics Hole Organics Clay Silt/Sand (Mainly Till) (Mainly Till)
Depth Total to Bedrock Depth Bedrock
H-86-71 4 12 7.5 23.5 30.0 H-86-72 5 45 10 20 80 86.0 H-86-73 1 9 21.5 13.5 45.0 H-86-74 05 17 8 30 37.0 H-86-75 5 31 7 40 83 88.0 H-86-76 3 42 20 30 7 sand/ 8 till 110 115.0 H-86-77 4 35 6 14 59 65.0 H-86-78 1 39 6 9 30 sand/11.5 till 96.5 105.0 H-86-79 2 32 31 10 75 80.0 H-86-80 4 26 13 14 34.5 gravel 80.5 86.0 H-86-81 3 31 6 45 32.5 sand/gravel 117.5 126.5 H-86-82 9 25 9 39 9 gravel/3.5' till 96.5 108.0 H-86-83 2 - 1 3 9.0 H-86-84 6 17 12 37 72 75.0 H-86-85 2 .14 2 45 22.5 30.0 H-86-86 3 49 20 9 81 86.0 H-86-87 6 40 35 11 82 87.0 H-86-88 4 46 20 70 75.0 H-86-89 1 43 2 46 50.0 H-86-90 4 26 7 37 43.0 H-86-91 4 40 13 57 63.0 H-86-92 3 40 5 48 53.0 H-86-93 1 48 6 3 58 65.0 H-86-94 3 39 12 54 60.0 H-86-95 1 40 11 52 58.0 H-86-96 4 35 4 43 48.0 H-86-97 1 31 9 41 46.0 H-86-98 1 24 12 37 42.0 H-86-99 4 47 10 61 67.0 H-86-100 1 30 11.5 42.5 47.0 H-86-101 1 50 51 57.0 H-86-102 4 64 7 12 87 92.0 H-86-103 4 58 6 68 73.0 H-86-104 4 60 6 70 75.0 H-86-105 3 61 8 8 80 85.0
greywacke argillite/mudstone
carbonate IF oxide IF argillite felsic volcanic felsic volcanic felsic volcanic felsic volcanic felsic volcanic felsic volcanic oxide IF oxide IF carbonate IF int. volcanic mafic volcanic mafic volcanic int. to mafic volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic int. volcanic int. volcanic mafic volcanic mafic volcanic mafic volcanic mafic volcanic argillite argillite
Hole Organics Clay Silt/Sand
-4 -
Upper Clastics Lower Clastics (Mainly Till) (Mainly Till)
Depth to Bedrock
Total Depth Bedrock
H-86-106 4 69 5 6.5 84.5 90.0 argillite H-86-107 4 75 - 24 103 108.0 mafic volcanic H-86-108 5 69 - 74 79.0 mafic volcanic H-86-109 6 69 - 12.5 87.5 91.0 int. vol. H-86-110 4 81 10 30.5 125.5 130.0 greywake/argillite H-86-111 4 77 - 7 88 93.0 int. volcanic H-86-112 4 79 - 38 10 133.0 graphitic H-86-113 2 37 6 20 6 gravel/34.5 till 105.5 109.5 H-86-114 4 20 12 13 24.5 gravel/9.5 till 89 100.0
15.5 gravel H-86-115 2 42 6 38 7 sand/gravel 93 105.0 H-86-116 4 14 45.5 24.5 10 gravel/30 till 120 126.5 H-86-117 2 44 4 15.5 20 gravel 85.5 95.0 vol., argillite H-86-118 3 40 - 16 126 135.0 int. volcanic H-86-119 2 22.5 - 35.5 60 67.0 felsic volcanic H-86-120 4 60 10 38 2 till? - 114.0 H-86-121 4 59 26 39 128 133.0 int. tuff H-86-122 ` 5 52 - 21.5 15 gravel/8.5 till 102 107.0 dacite H-86-123 4 60.5 8.9 73.5 78.0 pyrite schist H-86-124 2 42.5 14.5 73 132 137.0 graphite
APPENDIX I
IP/Resistivity Pseudosections
Grid A: Line 82+00N Pole-Dipole A-1
86+00N Pole-Dipole A-2
Grid AA: Line 8+00E Pole-Dipole AA-1
Grid D: Line 66+00W Pole-Dipole D-1
68+00W Pole-Dipole D-2
70+00W Pole-Dipole D-3
72+00W Pole-Dipole D-4
74+00W Pole-Dipole D-5
74+00W Dipole-Dipole D-5a
76+00W Pole-Dipole D-6
78+00W Pole-Dipole D-7
APPENDIX F
Statistical Analyses
Mlnlottrl; do i'~r ~~~rgiw et d7,w Noacurees Service de la Géoinformation
Date: 2 7 171R. 19B1
No G.M. 414.377
'1? ROUMI( !
H-86-01
DEPARTURE tX) LATITUDE CT) ELEVATIONCZ) 0 0 0
3-4A
FROM TO TYPE SS BEDROCK 60 76 80 10 180
IS PYRITE
PPM NON MAG PPM MAG VG 2637 1922 4.8 0
Au: 1800 eAu: 4746 Ag: .05 eAg: .1 As: 89 eAs: 235 Cu: 64 eCu: 169 Zn: 20 eZn: 53 Sb: 0 eSb: 0 Ba: 0 esa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: O eW:
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * 9889 Ag * 8888 eAa * 9993 As * EEEE eAs ?E EEEE Cu * EçEE eCu * EEEE ~r ~ FEE EEEE ç_ `! EFFF N EEEE Fa N EEEE eEa N EEEE Cr N EEEE Cr= n, EcEE Co N `!YX% eCc N vvvy Mo N
zMa N Ni N
e N : P) N
eW ")
MAX
Au: 395 Ag: .05 As: 114 Cu: 120 Zn: 23 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
eAu: 568 eAg: .1 eAs: 164 eCu: 173 eZn : 33 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
ro gnTrg7A.(f 1
H-86-01
DEPARTUoEfXJ LATITUEEtYI ELENATIOJiIZI 0 0 0
5-6
FROM TO TYPE SS BEDROCK 76 90 80 10 180
PPM NON MAG PPM MAO VG 1438 1414 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * 0000 As * 0000 eAs * 0000 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 450 Ag: .05 As: 101 Cu: 79 Zn: 24 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 788 eAg: .1 eAs: 177 eCu: 137 eZn: 42 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Old dORfSTAIE I
H-86-01
)IEPARTIIREtX) LATITIiBE(Y) ELEVATIOBtZ1 0 0 0
7-8A
FROM TO TYPE SS BEDROCK 90 105 80 10 180
PPM NON MAG PPM MAG VG 1751 1383 .8 O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * 1111 Cu * 1111 e C u * EEEE Zn -)E EEEE eZn * ECCE jlr,, N EEEE eSb hi
EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XX.'y eCo N X?CXX. Mo N
pMo N Ni N
e N i N W N eW N
MAX
Au: 100 Ag: .05 As: 8 Cu: 40 Zn: 13 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
eAu: 194 eAg: .1 eAs: 16 eCu: 78 eZn: 25 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: C eNi: 0 eW: 0
0r3 pQ3rçTRIF :
H-86-01
DEPARTUREIXI LATITUDEIT) ELE4ATIONIZ) 0 0 0
9-10
FROM TO TYPE SS BEDROCK 105 120 80 10 180
PPM NON MAG PPM MAG VG 1939 1261 .5 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 1111 eCu * 1111 Zn * 1111 e=n * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
11d NOMME I
H-86-01
BEPARTUIEtB) LATITUAE(Y) ELEVATIONtZ) 0 0 0
1112
FROM TO TYPE SS BEDROCK 120 130 70 10 180
Yi rTl17E
PPM NON MAO PPM MAG VO 1621 1664 4.2 0
Au: '490 eAu: 794 Ag: .6 eAg: 1 As: 120 eAs: 195 Cu: 48 eCu: 78 Zn: 25 eZn: 41 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: O Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 6666 eZn * 6666 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 12.5 Ag: .05 As: 27 Cu: 48 Zn: 20 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 34 eAg: .1 eAs : 74 eCu: 132 eZn: 55 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Old MOlESTAIE I
H-86-01
DEPARTUREIXf LATITUDEtT) ELEVATIONtZ) 0 0 0
11A
FROM TO TYPE SS BEDROCK 120 125 70 10 180
PPM NON MAG PPM MAO VG 2747 2343 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW lV
MAX
O/B 008ESTRIE I
H-86-01
OEaARTUREIXI LATITOEEIYI ELEVATIOMIZJ 0 0 0
1314
FROM TO TYPE SS BEDROCK 130 139 80 10 180
PPM NON MAG PPM MAG VG 1375 1291 .8 0
Au: 10 eAu: 14 Ag: .05 eAg: .1 As: 164 eAs: 226 Cu: 95 eCu: 131 Zn: 36 eZn: 50 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu '1P EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE e8a N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 535 Ag: .05 As: 148 Cu: 66 Zn: 30 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 482 eAg: 0 eAs: 133 eCu: 59 eZn: 27 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
011 NOMMAI! I
H-86-01
DEPARTUREDO LATITUDEIY) ELEVATIONIZ) 0 0 0
1516
FROM TO TYPE SS BEDROCK 139 150 80 10 180
PPM NON MAO PPM MAG VG 901 947 O 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 145 Ag: .2 As: 36 Cu: 82 Zn: 30 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 266 eAg: .4 eAs: 66 eCu: 150 eZn: 55 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
0/1 BOOESTIülE I
H-86-01 IEPARTURfifX) LATITUI)E(Yl ELEVATION(Z)
D 0 0
1718
FROM TO TYPE SS BEDROCK 150 160 80 10 180
PPM NON MAG PPM MAG VG 1833 1990 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N O000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01B NOMISMAME I
H-86-01
DEPARTINtEIXI LATITUDEfY) ELEVATIOMIZI O 0 O
19
FROM TO TYPE SS BEDROCK 160 165 80 10 180
PPM NON MAO PPM MAO VG 1962 1711 0 0
Au: 15 eAu: 29 Ag: .05 eAg: .1 As: 10 eAs: 20 Cu: 33 eCu: 65 Zn: 16 eZn: 31 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N O000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 35 Ag: .05 As: 48 Cu: 108 Zn: 27 Sb: 0 Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: ~5 eAg: .1 eAs: 103 eCu: 233 eZn : 58 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: C
OIE EO!1fST4(f I
H-86-01
IEPARTUREIX) LATITUDEIY) ELEVATIONIZ) 0 0 0
20
FROM TO TYPE SS BEDROCK 165 170 80 10 180
PPM NON MAG PPM MAG VG 2156 1911 0 0
Surface EEEE MIN EEEE NM * EEEE MAG '.E EEEE Au ?E EEEE eAu * EEEE Ag * EEEE eAg 4 EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE e_n * EEEE Sb rJ EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N EEEE eCr N EEEE Co N xXXY. eCo N XX`CX Mo N
eMo N Ni N
eNi W N eW N
MAX
Au: 15 Ag: .05 As: 105 Cu: 90 Zn: 38 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
eAu: 52 eA9: .2 eAs: 363 eCu: 311 eZn: 131 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
o!d A^RfA?RdI I
H-86-01
DEPARTURE(X) LATITUDE(T1 ELEVATIDNtZ) 0 0 a
21
FROM TO TYPE SS BEDROCK 170 175 80 20 180
PPM NON MAO PPM MAO VG 3458 2531 0 0
Surface EEEE MIN EEEE NM * EEEE NAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn Y EEEE St, M EEEE eSt N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 20 Ag: .4 As: 152 Cu: 96 Zn: 60 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: O
eAu: 63 eAg: 1.3 eAs: 476 eCu: 301 eZn: 188 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi .: 0 eNi: 0 eW: 0
ara1MET4PcI
H-86-01
BEPARTUiIEt%1 LATITUBEtT) ELE4ATIDMtZ) 0 0 o
22
FROM TO TYPE SS BEDROCK 175 180 80 20 180
PPM NON MAG PPM - MAG VG 3131 2141 0 0
Surface EEEE MIN EEEE NM * EEEE MAG -)P EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 42.5 Ag: .6 As: 616 Cu: 350 Zn: 580 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 74 eAg: 1 eAs: 1068 eCu: 607 eZn: 1005 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0!P .40!lES7ARf I
H-86-01
DEPARTURE(XI LATITUDE(T1 E1.EYATIONiZ1 0 0 0
23
FROM TO TYPE SS BEDROCK 180 181 90 30 180
PROCESSED DTDROCI
PPM NON MAG PPM MAG VG 1733 933 0 0
Sur-face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E . EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi p}
W Al eW N
MAX
Au: 45 Ag: .05 As: 115 Cu: 100 Zn: 42 Sb: O Ba: O Cr: 0 Co: O Mo: 0 Ni: 0 W: O
eAu: 117 eAg: .1 eAs: 299 eCu: 260 eZn: 109 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Dlè s0llfSTAIf I
H-86-02
DEPARTUREIX) LATITUDE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 54 60 80 10 101
PPM NON MAG PPM MAG VG 2603 2815 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba iV EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
0/P d^IlES?ASE 1
H-86-02
1EPARTUREtX1 LATITUBEtYI ELEVATIONlZI 0 0 0
02
FROM TO TYPE SS BEDROCK 60 65 80 10 101
PPM NON MAG PPM MAG VG 3419 2280 0 0
Au: 55 eAu: 188 Ag: .05 eAg: .2 As: 175 eAs: 598 Cu: 72 eCu: 246 Zn: 36 eZn: 123 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * O000 Zn * EEEE eZn x. EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N éW N
MAX
Au: 35 Ag: .05 As: 13 Cu: 23 Zn: 16 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
eAu: 162 eAg: .2 eAs: 60 eCu: 107 eZn: 74 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
011 90;lES?Adf I
H-66-02
DEPARTUREIXI LATITUDE(Y) ELNATIONt2l 0 0 0
03
FROM TO TYPE SS BEDROCK 65 75 60 10 101
PPM NON MAG PPM MAG VG 4632 1731 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * O000 . Zn * 0000 eZn * O000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 55 Ag: .05 As: 24 Cu: 42 Z n : 25 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 136 eAg: .1 eAs: 59 eCu: 104 eZn: 62 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
011 aORESTAIE I
H-86-02
HEEPARTUREIXI LATITUDEIf1 ELEVATIOMfZ1 0 0 0
04
FROM TO TYPE SS BEDROCK 75 85 60 10 101
PPM NON MAG PPM MAG VG 2471 1451 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 . Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 15 Ag: .05 As: 15 Cu: 49 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 34 eAg: .1 eAs: 34 eCu: 111 e2n: 55 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE EOAfS7AdE I
H-86-02
DEPARTURE(X) LATITUDE(Y) ELÊS)ATIDMIZI O 0 0
05
FROM TO TYPE SS BEDROCK 85 90 60 10 101
PPM NON MAG PPM MAG VG 2275 1196 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE e2n' 9E EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX, eCo N XXXX Mn N
eMo N Ni N eNi N W N
eW N
MAX
Au: 45 Ag: .05 As: 16 Cu: 44 Zn: 25 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 124 eAg: .1 eAs: 44 eCu: 121 eZn: 69 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE 909ESTME I
H-86-02
9EPARTURE(Xi LATITUBEtYI ELEUATIOR(Z) 0 0 0
06
FROM TO TYPE SS BEDROCK 90 98 80 10 101
PPM NON MAG PPM MAG VO 2756 1778 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XX;!X Mo N
eMo N Ni N
eNi N W N eW N
MAX
OId °O!lESTRIE I
H-86-02
DEPARTURE(XI LATITUDE(T) ELEV1{TIQI((Z) 0 0 0
7-7A
FROM TO TYPE SS BEDROCK 98 101 80 20 101
PPM NON MAG PPM MAG VG 1758 1215 0 0
Au: 40 eAu: 70 Ag: .05 eAg: .1 As: 76 eAs: 134 Cu: 58 eCu: 102 Zn: 530 eZn: 932 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi ': 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 30 Ag: .05 As: 300 Cu: 76 Zn: 30 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: Si eAg: .1 eAs: BvC, eCu: 204 eZn: 81 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/3 BO!lfSTA([ 1
H-86-03
BEPARTURE1X1 LATITU9E)Y1 ELEi)ATIORtt1 0 ' 0 0
01-2
FROM TO TYPE SS BEDROCK 50 65 80 10 134
PPM NON MAG PPM MAG VG 2688 2116 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * 0000 eAg * 0000 As 9E* 0000 eAs * EEEE Cu *- EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 5 Ag: .05 As: 32 Cu: 46 Zn: 26 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 6 eAg: .1 eAs: 38 eCu: 55 eZr.: 31 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Olé BOIlESTAtf I
H-86-03
DEPARTUREI%) LATITUDE(Y) ELEVATION(Z) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 65 75 80 10 134
PPM NON MAG PPM MAG VG 1194 1493 1.6 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -)F EEEE As * 1111 eAs * 1111 Cu * 1111 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo A.
eMo N Ni N
eNi N W N
eW ri
MAX
Au: 110 Ag: .05 As: 19 Cu: 32 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Ma: O Ni: 0
W: O
eAu: 182 eAg: .1 eAs: 31 eCu: 53 eZn: 40 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
d!I 8O8fSTAdI I
H-86-03
DEPARTURE(X) LATITUOE(Y1 ELEVATION(Zl 0 0' 0
05-6
FROM TO TYPE SS BEDROCK 75 95 60 10 134
PPM NON MAG PPM MAG VG 1655 770 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 1011117 011 I
H-86-03
UEPARTUREtX1 LATITUDE(Y1 ELEUATIUN(Z) 0 0 0
07-8
FROM TO TYPE SS BEDROCK 95 109 70 10 134
3% PYRITE
PPM NON MAG PPM MAG VG 2144 1785 5.7 0
Au: 1050 eAu: 2251 Ag: .05 eAg: .1 As: 48 eAs: 103 Cu: 85 eCu: 182 Zn: 30 eZn: 64 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag . * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 7777 Sb N 7777 eSb N 7777 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo ^: Ni N
e N i 1`1 W N ew N
MAX
Au: 95 Ag: .3 As: 145 Cu: 160 Zn: 58 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: O
W: O
eAu: 243 eAg: .8 eAs: 371 eCu: 409 eZn: 148 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: C eW: 0
O/d 1101ESIA6E :
H-86-03
DEPARTJRE(XI LATITUDE(TI ELE9AIIDN(ZI 0 a 0
9-10
FROM TO TYPE SS BEDROCK 109 119 80 10 134
PPM NON MAG PPM MAO VG 2559 1670 1.1 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Pa N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIE RO!lESTALt 1
H-86-03
DEPARTINtEtX) LATITUlIEfTI ELE4ATIONiZ1 0 0 0
11-A
FROM TO TYPE SS BEDROCK 119 122 60 10 134
PPM NON MAG PPM MAG VG 1674 2504 0 0
Au: 25 eAu: 42 A9: .2 eAg: .3 As: 16 eAs: 2? Cu: 130 eCu: 218 Zn: 40 eZn: 67 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 .eCr: 0 Co: O eCo: 0 Mo: 0 eN i•: 0 Ni: 0 eNi: 0
W: O eW: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 5 Ag: .05 As: 7.5 Cu: 350 Zn: 69 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 14 eAg: .1 eAs: 21 eCu: 972 eZn: 192 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
011 101lE57ALE 1
H-86-03
DEPARTUREIXI LATITUIEIY) ELEVATIDMIZ) O 0 0
12-A
FROM TO TYPE SS BEDROCK 122 125 80 20 134
PPM NON MAG PPM MAG VG 2778 5042 1.1 0
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * -EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 AO!lfS7Axf I
H-86-03
DEPARTURE(X) LATITUDE(Y1 ELEYATI09(Z) 0 0 0
13-A
FROM TO TYPE SS BEDROCK 125 134 80 20 134
PPM NON MAG PPM MAG VG 1680 1626 0 0
eAu: 1495 eAg: .1 eAs: 227 eCu: 386 eZn: 689 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: O eNi: 0
eW: 0
Au: 890 Ag: .05 As: 135 Cu: 230 Zn: 410 Sb: O Ba: O Cr: 0 Co: O Mo: O Ni: O W: O
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 1125 Ag: .05 As: 388 Cu: 132 Zn: 50 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
eAu: 1397 eAg: .1 eAs: 482 eCu: 164 eZn: 62 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
B!d IOI1fSTfütf I
H-86-04
DEPARTIMtEIXI LATITUDEtYI ELEUATIUt)tZl 0 0 O
01-2
FROM TO TYPE SS BEDROCK 45 65 80 10 115
PPM NON MAG PPM MAG VG 1242, 1388 .7 C
Surface EEEE MIN EEEE NM. * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F 1111 eAg * 1111 As *3E* 1111 e A s * 1111 Cu 9E 1111 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE éCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 30 Ag: .05 As: 73 Cu: 48 Zn: 26 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: O W: 0
eAu: 74 eAg: .1 eAs: 181 eCu: 119 eZn: 64 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE BORES7ARE I
H-86-04
DEP6RTUREIX) LATITUDECY) ELE9ATIOIiIZ) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 65 75 80 10 115
PPM NON MAG PPM MAO VG 2476 1805 O 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu 9E O000 Zn * 0000 eZn 3E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 1580 Ag: .05 As: 101 Cu: 200 Zn: 30 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: 0
W: 0
eAu: 3720 eAg: .1 eAs: 238 eCu: 471 eZn: 71 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 80107A1E I
H-86-04
DEPARTURE(X1 LATITUDE(Y1 ELEVATI011IZ) 0 0 • 0
05-6
FROM TO TYPE SS BEDROCK 75 90 80 10 115
PPM NON MAG PPM MAG VG 2355 2156 .8 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 1111 eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIE 9O10741f I
H-86-04
DEPABTUDEIXI LATITUDEIYI ELEVATIOMIZI Q O O
07-8
FROM TO TYPE SS BEDROCK 90 95 80 10 115
PPM NON MAO PPM MAO VO 5071 6452 0 0
Au: 105 eAu: 533 Ag: .05 eAg: .3 As: 55 eAs: 279 Cu: 114 eCu: 578 Zn: 36 eZn: 133 Sb: O eSb: O Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO *HE EEEE Au * EEEE eAu * EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N _ eNi N W N
eW N
MAX
Au: 85 Ag: .05 As: 280 Cu: 110 Z n : 38 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
eAu: 218 eAg: .1 eAs: 719 eCu: 283 eZn: 98 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Ora ROBESTAIE I
H-86-04
DEPARTifREIRI U1TIfllDEIYI E1.EYATIONtI) O O O
9-10
FROM TO TYPE SS BEDROCK 95 105 80 10 115
PPM NON MAO PPM MAO VG 2568 1770 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0l1 90MES70,(E I
H-86-04
OEPARTURE(XI UTITU'}E)Y) ELEVATIONtZ) O 0 0
1112
FROM TO TYPE SS BEDROCK 105 115 80 20 115
In M'Rl7E
PPM NON MAO PPM MAO VG 4746 2508 5.9 0
Au: 1030 eAu: 4889 Ag: .6 eAg: 2.8 As: 163 eAs: 774 Cu: 134 eCu: 656 2n: 80 eZn: Z8ïi Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi.: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu 9E EEEE Ag * EEEE eAg #* EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE 2n ~ EEEE e2n * Er=r. Sh N EEEE aS5 N EEEE Ba N EEEE eBa N 6666 Cr N 6666 eCr N 6666 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
e N i N W N eW N
MA><
01? PnPtç?A.S£ 1
H-86-04
DEPART9RE IV LATITUDE (Yl U.'rVATID)I tZ) 0 0 0
13
FROM TO TYPE SS BEDROCK 115 116 80 20 115
PROCESSED MEDP0CI?
PPM NON MAG PPM MAG VG 6154 4103 0 0
Au: 55 eAu: 338 Ag: 2.8 eA9: 17.2 As: 270 eAs: 1662 Cu: 2600 eCu: 16000 Zn: 2500 eZn: 15385 Sb: 0 eSb: O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: v
Sur-Face EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ******** EEEE eA9 *HE***#*-)E# :**~ xx EEEE As *# EEEE eAs -)F EEEE Cu ******?FIE EEEE eCu *a;**.fE.K=**aE#**#*?HE-)4-# EEEE Zn *#x*** EEEE e Z n *?E*aE?HE #* x**** iE*HHHE EEEE Sb N EEEE eSb N EEEE Ba N EEEE.... - eBa N EEEE Cr N EE= eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
n.►d P.OKES7.4dE I
H-86-04
DEPARTUREtX) LATITUDEfY) ELEUATIOM(Z) D 0 0
14
FROM TO TYPE SS BEDROCK 116 127 90 30 115
80% PY PROCESSED BfDROCI
PPM NON MAG PPM MAG 1103 . 23 0 0
Au: 12.5 eAu: 14 Ag: 6.4 eAg: 7.1 As: 350 eAs: 3S6 Cu: 5800 eCu: 6400 Zn: 8000 eZn: 8828 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: C eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: C W: 0 eW: 0
Surface EEEE MIN MAX EEEE NM * EEEE MAG -)E EEEE Au 4E EEEE eAu * EEEE Aç 4•)E*HE***#*-xiE** aHE )F )E* EEEE eAg ****** EEEE As *** EEEE eAs * EEEE Cu ******************* EE-EE eCu ******* EEEE Zn #*iF**Ht-*$?HE:4?(**XXX*** EEEE eZn *********** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N 0000 Co N 0000 eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
018 PO!!: S?R.{£ 1
H-86-05
DEPARTUREfX) iATITUDEtY) E.EUATIONfZ) 0 0 0
01-2
FROM TO TYPE SS BEEROC}; 50 60 80 10 65
PPM NON MAO PPM MAG VG 3315 2414 0 0
Au: 200 eAu: 563 Ag: .05 eA9: 2 As: 107 eAs: Z55 Cu: 93 eCu: 325 Zn: 46 eZn: 15: Sb: 0 eSb: C Ba: 0 eBa: 0 Cr: 0 eCr: C Co: 0 eCo: C Mo: O eNi: C Ni 0 eNi: W: 0 ek:: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu ?E EEEE A,3 x" EEEE eA9 ;x EEEE As * EEEE eAs :k EEEE Cu * EEEE .eCu *
7n * EEEE eZr * EEEE 0000 eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMa N Ni N eNi N W N eW N
MAX
O(* 9"!lES7A.{E I
H-86-05
DEPARTUREiXI LATITUDEIYI ELEVATIQMiZ1 0 n 0
03
FROM TO TYPE SS BEDROCK 60 65 60 20 65
PPM NON MAG PPM MAG VG 3169 329 1.5 0
eAu: 1981 eAg: .2 eAs: 105 eCu: 254 eZn: 146 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: .625 Ag: .05 As: 33 Cu: 80 Zn: 46 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0IS N0MESIAIE I
H-86-05
DEPARTURE!%) LATITUDE(Y) ELEVATIOXID 0 0 0
04
FROM TO TYPE SS BEDROCK 65 66 90 30 65
PROCESSED BI IOCI
PPM NON MAG PPM MAG VG 2902 1294 0 0
Au: 15 eAu: 44 Ag: .2 eAg: .6 As: 238 eAs: 691 Cu: 1600 eCu: 4643 Zn: 1500 eZn: 4353 Sb: 0 eSb: v Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: O Mo: 0 eNi: 0 Ni: 0 eNi: C W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *r EEEE FAs * EEEE Cu ***** EEEE eCu ***** EEEE Zn *** EEEE eZn ***** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi. N W N eW N
MAX
C!F 9?dE.7A,tE 1
H-96-07
BEPARTURE(X) LATITUBE(T) ELEUATIOMIZ) O O 0
01-2
FROM TO TYPE SS BEDROCK 44 55 80 10 73
PPM NON MAG PPM MAS VG 1920 1721 .8 0
Au: 180 eAu: 346 Ag: .05 eAg: .1 As: 78 eAs: 150 Cu: 62 eCu: 119 Zn: 24 eZn: 46 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: C Co: 0 eCo: O Mo: O eNi: 0 Ni: C eNi: 0 W: O eW: O
Surface EEEE MIN
MAK EEEE NM * EEEE MAG -)E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 1111 Zn * 1111 eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
Au: 210 Ag: .05 As: 50 Cu: 144 Zn: 28 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
eAu: 405 eAg: .1 eAs : 96 eCu: 278 eZn: 54 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Ols 000fSTAdF 1
H-86-07
DEPARTUREtX; LATITUDE{Tl ELEV8TI9UtZl 0 0 0
03-4
FROM TO TYPE SS BEDROCK 55 65 80 10 73
PPM NON MAG PPM MAG VG 1929 1556 .8 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9P EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9F EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 11.11 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIS SOAESTAfE I
H-86-07
DEPARTUREIX) LATITUDEIY) ELEYATIOMIZ) 0 O O
05-6
FROM TO TYPE SS BEDROCK 65 73 80 20 73
PPM NON MAG PPM MAO VO 2785 2533 0 0
Au: 50 eAu: 139 Ag: .05 eAg: .1 As: 106 eAs: 295 Cu: 184 eCu: 512 Zn: 100 e2n: 279 Sb: 0 eSb: O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 RO/UTAH 1
H-86-08
lEPARTUREIXI LATITUpEtYI ELEIMTION(Zl 0 0 0
01-2
FROM TO TYPE SS BEDROCK 41 50 80 10 83
PPM NON MAG PPM MAG VG 2667 1786 0 0
Au: 115 eAu: 307 Ag: .05 eAg: .1 As: 49 eAs: 131 Cu: 60 eCu: 160 Zn: 28 eZn: 75 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eA9 * EEEE As * 0000 eAs * 0000 Cu * 0000 eCu * 0000 Zr: 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIE AORFS1Aff I
H-86-08
DEPARTUREtX! LATITUDEfY) ELEUATIDlIt2) O 0 O
03-4
FROM TO TYPE SS BEDROCK 50 60 SO 10 83
PPM NON MAG PPM MAG VG 2184 1411 0 0
Au: 65 eAu: 142 Ag: .05 eAg: .1 As: 130 eAs: 284 Cu: 64 eCu: 140 Zn: 30 eZn: 66 Sb: O eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -)E EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
e!3 ROME.T ME I
H-86-08
DEPARTUREIX) LATITUyEtYt ELEVATIOlIIZ1 0 0 0
05-6
FROM TO TYPE SS BEDROCK 60 70 80 10 83
PPM NON MAG PPM MAO VG 1656 1645 0 0
Au: 345 eAu: 571 Ag: .05 eAg: .1 As: 7 eAs: 12 Cu: 40 eCu: 66 Zn: 30 eZn: 50 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: D
W: C eW: 0
Surface EEEE MIN EEEE NM R: EEEE MAG * EEEE Au * EEEE eAu -JP EEEE Ag * EEEE eAg * EEEE As .x EEEE eAs * EEEE Cu * çEEE eCu * EEEE Zn *. EEEE eZn * COOO Sb N 0000 eSb N O000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 70 Ag: .05 As: 139 Cu: 94 Zn: 120 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: 0
W: O
eAu: 174 eAg: .1 eAs: 346 eCu: 234 eZn: 299 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/1 10107A(E I
H-86-08
lfPARTURE(X) UITITUSE(T) ELEVATION(Z) 0 O O
07
FROM TO TYPE SS BEDROCK 70 75 80 10 83
PPM NON MAO PPM MAG VG 2489 1547 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * ELLE eCu * EEEE Zn * E_EE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N O000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Olà BOAESTA,tE I
H-86-08
DEPBRTURfIX) LATITUDE(Y) ELEVATION(Z) O O O
08
FROM TO TYPE SS BEDROCK 75 80 80 20 83
PPM NON MAG PPM MAG VG 4025 2148 2 0
eAu: 1529 eAg: 2 eAs: 676 eCu: 728 eZn: 439 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 380 Ag: .5 As: 168 Cu: 181 Zn: 109 Sb: O Ba: O Cr: O Co: O Mo: O Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu -)E EEEE _Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0 r3 30107Adf 1
H-86-08
DEPARTURE(X) LATITUDE(Y) ELEVATION(21 0 O 0
09
FROM TO TYPE SS BEDROCK 80 83 80 20 83
PPM NON MAG PPM MAG VG 5204 1548 0 0
Au: 15 eAu: 78 Ag: .05 eAg: .3 As: 312 eAs: 1624 Cu: 450 eCu: 2342 Zn: 940 eZn: 4892 Sb: O eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: C
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **HF EEEE eAs * EEEE Cu * EEEE eCu ** EEEE Zn ** EEEE eZn *****HE EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
POMESTME I
H-86-09
DEPARTURE(%1 LATITUDECT) ELEVATION(Z) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 41 50 80 IO 99
PPM NON MAG PPM MAG VG 2667 2210 .8 0
Au: 55 eAu: 147 Ag: .05 eAg: .1 As: 274 eAs : 731 Cu: 90 eCu: 240 Zn: 34 eZn: 91 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: C Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * 1111 As *HE 1111 eAs * 1111 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 95 Ag: .05 As: 322 Cu: 144 Zn: 38 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 187 eAg: .1 eAs: 634 eCu: 283 e'n: 75 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Old MSTAdL 1
H-86-09
DEpARTUREIXI LATITUDElYI ELEYATIDIItZ) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 50 60 80 10 99
PPM NON MAG PPM MAG VG 1968 1839 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE AS * EEEE eAg * EEEE As **# EEEE eAs -?E 0000 Cu * 0000 eCu * 0000 Zn * EEEE eZn .x EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 85 Ag: .05 As: 236 Cu: 72 Zn: 34 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 103 eAg: .1 eAs: 286 eCu: 87 eZn: 41 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIS AOAfSTRRf 1
H-86-09
9EPARTUREIXI LATITUnEIYI ELEVATION(Z) 0 0 0
05-7
FROM TO TYPE SS BEDROCK 60 70 80 10 99
PPM NON MAG PPM MAG VG 1212 1266 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *HE EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn ?rr 0000 eZn * 000C Sb N EEEE eSt N EEEE Ba N EEEE eEa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
e N i N W N
eW N
MAX
Au: 360 Ag: .05 As: 198 Cu: 89 Zn: 30 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 920 eAg: .1 eAs: 506 eCu: 227 eZn: 77 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
cia 908ESTB!!1 1
H-86-09
DEPARTUREtXI LATITUDEIYI ELEYATIOMfZi 0 O 0
8-9A
FROM TO TYPE SS BEDROCK 70 77 80 10 99
5% PYRITE
PPM NON MAG PPM MAG VG GALENA 2555 1904 3 2
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu ?E EEEE Ag •3(- EEEE eAg * EEEE As * EEEE eAs 9E EEEE Cu * EEEE eCu !E EEEE Zn * EEEE eZn •3F• 6666 Sb N 6666 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 260 Ag: .05 As: 284 Cu: 120 Zn: 32 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O
W: O
eAu: 421 eAg: .1 eAs: 460 eCu: 194 eZn: 52 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
01! IOHESTAff I
H-86-09
DEPARTURE IX) LATITUDE Y) ELEVATION (Z) 0 0 O
1011
FROM TO TYPE SS BEDROCK 77 90 80 10 99
PPM NON MAG PPM MAG VG 1619 1407 .8 0
Surface EEEE MIN EEEE NM *
. EEEE MAG * EEEE Au ')E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 1111 eBa N 1111 Cr N EEEE eCr N` EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 3580 Ag: .05 As: 113 Cu: 116 Zn: 42 Sb: 0 Ba: O Cr: O Co: O Mo: O Ni: O W: 0
eAu: 6879 eAg: .1 eAs: 217 eCu: 223 eZn: 81 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE 94RfSTAdf I
H-86-09
11EPARTUREIXI LATITUIIEITI ELE9ATIONIZI 0 0 0
12
FROM TO TYPE SS BEDROCK 90 95 80 20 99
PPM NON MAG PPM MAG VG 1922 1765 1.6 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au ** EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE e2n * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N.
eW N
MAX
OIE ROAESTAdE I
H-86-09
DEPARTURE(XI LATITUBE(T1 E1.EYATI0NIZI 0 0 0
13
FROM TO TYPE SS BEDROCK 95 99 80 20 99
PPM NON MAO PPM MAO VO 2529 1241 0 0
Au: 50 Ag: .05 As: 480 Cu: 198 Zn: 250 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: O Ni: 0
W: .0
Surf ace EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 126 eAg: .1 eAs: 1214 eCu: 501 eZn: 632 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
OU ROAESTA(E I
H-86-09
6EPARTUREIX) LATITU➢EIY) ELEYATIOIIIZ) 0 0 0
14
FROM TO TYPE SS BEDROCK 98 99 80 20 99
30% PYRITE
PPM NON MAG PPM MAG VG 23818 606 0 0
eAu: 238 eAg:. 1.2 eAs: 8051 eCu: 857 eZn: 1572 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: C eW: 0
Au: 10 Ag: .05 As: 33S Cu: 36 Zn: 66 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE N M ******* EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs *** EEEE Cu * EEEE eCu -)E EEEE Zn * E~EE e?n ** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 000C eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
013 I0!!ESTAd( 1
H-86-10
DEPARTUREtX} LATITUDEIYI ELEVATIDAiZf 0 0 0
1-2A
FROM TO TYPE SS BEDROCK 53 65 80 10 68
PPM NON MAG PPM MAG VG 2093 1582 .5 0
Au: 650 eAu: 1360 Ag: .8 eAg: 1.7 As: 134 eAs: 280 Cu: 153 eCu: 320 Zn: 30 eZn: 63 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: C eCr: C Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *-JE EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 1111 eBa N 1111 Cr N 1111 eCr N EEEE Co. N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 25 Ag: .05 As: 171 Cu: 60 Zn: 74 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 65 eAg: .1 eAs: 446 eCu: 156 eZn: 193 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 RORESTARE I
H-86-10
DEPARTURE(XI LATITUDE(Y) ELEVATION{2l 0 0 0
03
FROM TO TYPE SS BEDROCK 65 68 80 20 68
PPM NON MAG PPM MAO VG 2607 1254 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag l6 EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 65 Ag: .05 As: 330 Cu: 184 Zn: 40 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 131 eAg: .1 eAs: 663 eCu: 370 eZn: 80 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: O eNi: 0 eW: 0
OIF AORf9TARE 1
H-86-11
DEPARTURE(%1 LATITUDEITI ELEYATIONIZI O O O
01-2
FROM TO TYPE SS BEDROCK 50 65 80 10 89
PPM NON MAG PPM MAG VG 2009 1793 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIS BONESTAI£ I
H-86-11
DEPARTUREIXI LATITUDE(Y) ELEVATION(Z) D 0 0
03-4
FROM TO TYPE SS BEDROCK 65 74 80 10 89
PPM NON MAG PPM MAG VG 2034 1995 .8 0
Au: 760 Ag: .05 As: 468 Cu: 157 Z n : 22 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 1546 eAg: .1 eAs: 952 eCu: 319 eZn: 45 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi': 0 eNi: 0 eW: 0
MAX
O/I 1O0ESTA1E 1
H-86-11
1EP)1RTURE(X) LATITO9E(Y1 ELEUBTION(2) 0 0 O
05-6
FROM TO TYPE SS BEDROCK 74 80 80 10 89
PPM NON MAG PPM MAG VG 1500 1657 .8 0
Au: 420 eAu: 630 Ag: .05 eAg: .1 As: 346 eAs: 519 Cu: 70 eCu: 105 Zn: 24 eZn: 36 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: O Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 100 Ag: .05 As: 159 Cu: 198 Zn: 46 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: 0
eAu: 375 eAg: .2 eAs: 597 eCu: 743 eZn: 173 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi. : 0 eW: 0
OIS 000ESTAIE I
H-86-11
lEPARTU(E(X) LATITttDE(YI ELEVATI01((Z) a o • o
07
FROM TO TYPE SS BEDROCK 80 85 80 20 89
PPM NON MAO PPM MAO VG 3752 5619 0 0
Surface EEEE MIN EEEE NM * EEEE MAO ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eRa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Ol d AOnESrarrE I
H-86-11
➢EPARTURE01 LATITBLEIYI ELEVATION(Z) 0 0 0
08
FROM TO TYPE SS BEDROCK 85 89 80 20 89
PPM NON MAG PPM MAG VG 3894 1884 0 0
eAu: 78 eAg: .2 eAs: 3583 eCu: 366 eZn: 389 eSb: 0 eBa: C eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 20 Ag: .05 As: 920 Cu: 94 Zn: 100 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As iE*1F*lEiFIFdF* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMô N Ni N eNi N W N eW N
MAX
Au: 2690 Ag: .05 As: 480 Cu: 125 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: O Ni: O
W: O
eAu: 3478 eAg: .1 eAs: 621 eCu: 162 eZn: 57 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Old R07ESTAUE 1
H-86-12
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
01-3
FROM TO TYPE SS BEDROCK 47 65 80 10 90
10S PYRITE
PPM NON MAG PPM MAG VG 1293 1406 1.3 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE . eAs * 2222 Cu * 2222 eCu * 2222 Zn * 2222 eZn * 2222 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 210 Ag: .05 As: 232 Cu: 74 Zn: 26 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
eAu: 298 eAg: :1 eAs: 329 *Cu: 105 eZn: 37 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
0/1 d0AfS7Ai[f I
H-86-12
IEPARiURE1X) LATITUDEIT) ELEVATIONIZ) O O O
04-5
FROM TO TYPE 3s BEDROCK 65 75 80 10 90
PPM - NON MAG PPm MAG VG 1413 1447 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE eZn * O000 Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 155 Ag: .3 As: 315 Cu: 93 Zn: 111 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0
W: 0
eAu: 254 eAg: .5 eAs: 516 eCu: 152 eZn: 182 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O
eW : 0
Olt 9o!lESTArTÉ 7
H-86-12
DEPARTUREIX) LATITUDE11f1 ELEYATIDNIZ) 0 0 0
06-7
FROM TO TYPE SS BEDROCK 75 85 80 10 90
PPM NON MAG PPM MAG VG 1639 1174 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *at-* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 285 A9: .8 As: 314 Cu: 57 Zn: 96 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 1129 eAg: 3.2 eAs: 1244 eCu: 226 eZn: 380 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIS 801lES1A,lE I
H-86-12
DEPARTURE(X) LATITUDEtYI ELEUATION(ZI 0 0 0
08
FROM TO TYPE SS BEDROCK 85 90 80 20 90
PPM NON MAG PPM MAG VG 3961 2196 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 ** EEEE eAg ## EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
• MAX
Old IOMESTAlI 1
H-86-13
iEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 40 45 80 10 71
PPM NON MAG PPM MAG VG 2186 2216 0 0
Au: 90 eAu: 197 Ag: .6 eAg: 1.3 As: 520 eAs: 1137 Cu: 44 eCu: 96 Zn: 112 eZn: 245 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As **9E** EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 145 Ag: .5 As: 262 Cut 40 Zn-: 88 Sb: 0 Ba: 0 Cr: O Co: C Mo: 0 Ni: 0
W: O
eAu: 293 eAg: 1 eAs: 529 eCu: 81 eZn: 178 eSb: 0 eBa: 0 eCr 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 I0107A,tF I
H-86-13
DEPARTUREIXI LATITUDEITI ELEVATIONIZI 0 O 0
03-5
FROM TO TYPE SS BEDROCK 45 55 80 10 71
PPM NON MAG PPM MAG VG 2017 1857 0 0
1J
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Olt AOMfSTAr£ r
H-86-13
DEpAATU2ElXI UTITU:EtYI flEUATIDMIZI 0 0 0
06-7
FROM TO TYPE SS BEDROCK 55 65 80 10 71
PPM NON MAG PPM MAG VG 1096 2237 0 0
Au: 240 eAu: 263 Ag: .6 eAg: .7 As: 165 eAs: 181 Cu: 30 eCu: 33 Zn: 64 eZn: 70 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu '1P EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
dld ®OAES7ALE I
H-86-13
GEPARTIR2E(X1 LATITll9E(Y1 ELEVATION(Z) 0 0 0
08
FROM TO TYPE SS BEDROCK 65 70 80 20 71
PPM NON MAO PPM MAG VG 3467 2076 0 0
Au: 140 eAu: 485 Ag: .4 eAg: 1.4 As: 153 eAs: 530 Cu: 35 eCu: 121 Zn: 240 eZn: 8~2 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: O Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM °1F EEEE MAG i6 EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn *_ EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 90 Ag: .7 As: 378 Cu: 95 Zn: 1375 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 136 eAg: 1.1 eAs: 572 eCu: 144 eZn: 2080 eSb: 0 eBa: 0 eCr: C eCo: 0 eNi: 0 eNi: 0 eW: 0
011 90MESI9df I
H-86-13
DEPARTURE(X) UTITUDE (Y) ELEVATION (2) 0 0 0
09
FROM TO TYPE SS BEDROCK 70 71 80 20 71
PPM NON MAG PPM MAG VG 1513 1179 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn *** EEEE eZn *HE EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Ora ROMESTA[f 1
H-86-14
DEPARTUREIX) LATITUDEfY) ELEVATIONII) 0 0 0
1-1A
FROM TO TYPE SS BEDROCK 30 31 80 20 31
PPM NON MAG PPM MAG VG 2503 1825 0 0
Au: 170 eAu: 425 Ag: .6 eAg: 1.5 As: 366 eAs: 916 Cu: 41 eCu: 103 Zn: 290 eZn: 725 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu *-EEEE Zn 9E EEEE e Z n * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 870 A9: 2.5 As: 2000 Cu: 63 Zn: 445 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 1604 eAg: 4.6 eAs: 3688 eCu: 116 eZn: 821 eSb: 0 eBa: 0 eCr 0 eCo: 0 eNi: C eNi: 0 eW: O
O!d BONESTAIf I
H-86-15
!lEPARTURE(X) LATITUnE(Y) ELEVATIOM(Z) O O O
1-lA
FROM TO TYPE SS BEDROCK 40 42 80 20 42
40% PY AMI MS PO
PPM NON MAG PPM MAG VG ASPY 1844 2823 0 3
Sur-face EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EE EE Ag ******* EEEE eAg **(-* EEEE As ******************* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX' Mo N
eMo N Ni N eNi N W N eW N
OJS .90AESIAdE I
H-86-16 BEPIAlTURERXI UTITUnE{Y) ElE4ATI8i(Z)
0 0 0
1-1A
FROM TO TYPE SS BEDROCK 23 24 80 20 24
PPM NON MAO PPM MAO VO 2446 1969 0 0
Au: 300 eAu: 734 Ag: .8 eAg: ~ As: 704 eAs: 1?22 Cu: 59 eCu: 144 Zn: 139 eZn: 340 Sb: 0 eS+^: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag *9E EEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu TE EEEE eCu * EEEE Zn * SEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 240 Ag: .6 As: 504 Cu: 47 Zn: 280 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: O
eAu: 376 eAg: .9 eAs: 789 eCu: 74 eZn: 43S eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 b'0!lfS7Alf I
H-86-17
DEPARTUREIXI LATITUDEIT) ELEVATIONLIL D O D
lA-2
FROM TO TYPE SS BEDROCK 35 37 80 20 37
PPM NON MAG PPM MAO VG 1566 1646 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Ole AMBUST4fl 1
H-96-18
DEPARTURE(X) LATITOHE(Y) ELEVATIDRII) 0 0 0
01
FROM TO TYPE SS BEDROCK 37 45 80 10 65
PPM NON MAG PPM MAG VG 2234 2054 0
Au: 445 eAu: 994 Ag: .5 eAg: 1.1 As: 528 eAs : 11E0 Cu: 60 eCu: 1Z4 Zn: 108 eZn: ":41 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: C eCo: 0 Mo: 0 eNi: 0 Ni: C eNi: 0
W: O eW: C
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * 0000 eCu * OOCO Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
éMo N Ni N
eNi N W N
eW N
MAX
0l )t 901lESTAIE I
H-86-18
)EPARTUREIX) LATITUDEIYI ELEUATIOMIZ) 0 O 0
2-2A
FROM TO TYPE SS BEDROCK 45 55 80 10 65
PPM NON MAG PPM MAG VG 1418 1466 .8 0
eAu: 1135 eAg: .9 eAs: 1078 eCu: 54 eZn: 139 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 800 Ag: .6 As: 760 Cu: 33 Zn: 98 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 1111 eZn * 1111 Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 25 Ag: .7 As: 380 Cu: 61 Zn: 180 Sb: 0 Ba: O Cr: 0 Co: O Mo: O Ni: 0 W: 0
eAu: 57 eAg: 1.6 eAs: 859 eCu: 138 eZn: 407 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
OIE IOMESTAKE I
H-86-18 1EPARTUREIXI LATITUDEIY1 ELEYATIOlf121
0 0 0
03
FROM TO TYPE SS BEDROCK 55 60 80 20 65
PPM NON MAG PPM MAG VG 2261 2106 1.5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/11 IORESTRIE I
H-86-18
DEPARTUREtX) LATITUREiYI ELEVATIQIi1Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 60 62 80 20 65
PPM NON MAG PPM MAG VG 2803 2204 0 0
Au: 40 eAu: 112 Ag: .5 eAg: 1.4 As: 238 eAs: 667 Cu: 60 eCu: 168 Zn: 142 eZn: 398 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *9E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 30 Ag: .4 As: 177 Cu: 103 Zn: 165 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 82 eAg: 1.1 eAs: 482 eCu: 281 eZn: 449 eSb: 0 eBa: O eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
011 101fS7AI(I I ~
H-86-18
BEPARTURE{X) LATITUDE{Y) ELEVATION{Z) 0 0 0
05
FROM TO TYPE SS BEDROCK 62 65 80 20 65
WELL IIIDVRA71 SRI77Y CLAY
PPM NON MAG PPM MAG VG 2723 1418 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eN1 N W N eW N
MAX
011 BOlIESTAdE I
H-86-19
1EPARTUREDO LATITUIEIYI ELEVATIIO)IZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 60 65 80 20 68
YI PYRITE
PPM NON MAG PPM MAG VG 3718 2205 4.1 0
eAu: 1673 eAg: 1.5 eAs: 2469 eCu: 119 eZn: 335 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 450 Ag: .4 As: 664 Cu: 32 Zn: 90 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O
W: O
Surface EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *****HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE e8b N EEEE Ba N 2222 eBa N 2222 Cr N 2222 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
0/1 101ESTAIE I
H-86-19
DEPARTURE(X) LATIT(OfE(Yt ELEVATIOX(Z1 D O O
02
FROM TO TYPE SS BEDROCK 65 68 80 20 68
PPM NON MAG PPM MAG VG 3024 2048 0 0
Au: 305 Ag: 1.8 As: 379 Cu: 75 Zn: 265 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag ***** EEEE eAg *XXXX EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 922 eAg: 5.4 eAs: 1146 eCu: 227 eZn: 801 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Old IORESTAIE I
H-86-20
IEPARTUREIXt LATITUDEIYI ELEVATIORIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 46 50 80 20 51
PPM NON MAO PPM MAG VG 2645 2842 0 0
eAu: 476 eAg: 1.6 eAs: 2137 eCu: 169 eZn: 489 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: 180 Ag: .6 As: 808 Cu: 64 Zn: 185 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * ESSE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N ESSE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
g ►! ,49NESTRIE I
H-86-20
IEPARTURE(XI LATITUEE(Y1 ELEVATIOR(Z) O 0 0
02
FROM TO TYPE SS BEDROCK 50 51 SO 20 51
PPM NON MAG PPM MAG VG 2216 1647 0 0
Au: 485 eAu: 1075 Ag: .7 eA9: 1.6 As: 1250 eAs: 2836 Cu: 114 eCu: 25= Zn: 260 eZn: 576 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Sur-Face EEEE .MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ************ EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01d PO1!(S7Ad( I
H-86-21
DEPARTURE(X) LATITUBE(Y) ELEVATIO!((Z) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 71 80 80 10 88
PPM NON MAG PPM MAG VG 1878 1117 0 0
eAu: 911 eAg: 2.3 eAs: 1232 eCu: 223 eZn: 845 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 485 Ag: 1.2 As: 656 Cu: 119 Zn: 450 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg ** EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
0!8 IORESTAIE I
H-86-21
9EPAR11XtE(XI LATITtiDEtY) ELEVATION(Z) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 80 88 80 20 88
PPM NON MAG PPM MAG VG 1527 1355 .9 0
Au: 250 Ag: .8 As: 942 Cu: 160 Zn: 38 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *-)P EEEE eAg * EEEE As 9E******E* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 382 eAg: 1.2 eAs: 1438 eCu: 244 eZn: 58 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
0/8 BONES1AdE I
H-86-21
OEP11RTlNIEIX) UTITUDEIY) ELE(t#TIONIZI O 0 O
05
FROM TO TYPE SS BEDROCK 88 91 80 20 88
201, PYRITE
PPM NON MAG PPM MAG VG 3171 1189 5.8 0
Au: 60 eAu: 190 Ag: 3.1 eAg: 9.8 As: 920 eAs: 2917 Cu: 37 eCu: 117 Zn: 475 eZn: 1506 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ********* EEEE eAg *****HE*** EEEE As ********* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * ESEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 2222 eCr N 2222 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 75 Ag: .8 As: 314 Cu: 81 Zn: 156 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: 0
W: 0
eAu: 123 eAg: 1.3 eAs: 513 eCu: 132 eZn: 255 eSb: 0 eBa: 0 eCr: O eCo: O eNi: 0 eNi: O
eW: 0
OIS 9OAESTAXE I
H-96-22
DEPARTURE(X) LATITüûE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 93 104 60 10 106
PPM NON MAG PPM MAO VG 1634 1408 1.5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 70 Ag: .8 As: 570 Cu: 230 Zn: 79 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 113 eAg: 1.3 eAs: 921 eCu: 372 eZn: eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0!! BO1lEST/IdF 1
H-86-22 BEPARTUREtXI LATITUBEtYI ELEVATIOMIZI
0 0 0
02
FROM TO TYPE SS BEDROCK 104 106 80 20 106
PPM NON MAG PPM MAG VG 1616 869 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 75 Ag: .8 As: 1120 Cu: 230 Zn: 79 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 2C6 eAg: 2 2 eAs: 3071 eCu: 631 eZn: 217 eSb: a eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/1 80dE5TAlE 1 .
H-86-23
DEPARTURE(X1 LATITUDE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 74 76 80 20 77
15% PURE
PPM NON MAG PPM MAG VG 2742 3396 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -3E EEEE Ag *E EEEE eAg ** EEEE As *-iHE**jF*9HE** EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
018 BOdESTARE I
H-86-23 DEPARTURE(X1 LATITUDE(Y1 ELEYATIO((Z1
0 0 0
02-3
FROM TO TYPE SS BEDROCK 76 77 80 20 77
20% PYRITE
PPM NON MAO PPM MAO VG 2355 1825 0 0
eAu: 259 eAg: 1.9 eAs: 1639 eCu: 452 eZn: 170 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 110 Ag: .8 As: 696 Cu: 192 Zn: 72 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0IB BOBESTplf r
H-86-25
DEPARTUREIXI LATITUDEIY) ELE4ATIONIZl 0 0 0
01
FROM TO TYPE SS BEDROCK 94 95 SO 10 112
PPM NON MAG PPM MAG VG 2000 1137 0 0
Au: 160 eAu: 320 Ag: .6 eAg: 1.2 As: 173 eAs: 346 Cu: 170 eCu: 340 Zn: 68 eZn: 136 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo.: 0 Mo: O eNi,: O Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -)F EEEE As * EEEE eAs -)E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEE~ eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Ma N
eMo N Ni N eNi N W N eW N
MAX
Au: 230 Ag: 1 As: 306 Cu: 200 Zn: 46 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 333 eAg: 1.4 eAs: 443 eCu: 290 e2n : 67 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi.: 0 eNi: 0 eW: 0
OIE pnAreTAIf I
H-86-25
DEPARTUREIX) LATITUDEIYI ELEVRTIONIZI 0 0 0
02-3
FROM TO TYPE SS BEDROCK 95 101 80 10 112
PPM NON MAG PPM MAG VG 1448 2844 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OI A SORfS7Alf I
H-86-25
DEPARTURE(%) LATITURE(Y) ELEYATIOM(Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 101 105 80 20 112
PPM NON MAO PPM MAO VO 3333 2049 0 0
eAu: 817 eAg : 2 eAs: 1200 eCu: 520 eZn: 320 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 245 Ag: .6 As: 360 Cu: 156 Zn: 96 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Nd 904fSTAdf I
H-86-25
DEPARTURE(X) LATITUDE(Y) ELEVATIOM(Z) 0 0 0
05
FROM TO TYPE SS BEDROCK 105 110 80 20 112
PPM NON MAG PPM MAO VG 3178 2200 0 0
Au: 205 eAu: 651 Ag: .8 eAg: 2.5 As: 328 eAs: 1042 Cu: 210 eCu: 667 Zn: 90 eZn: 286 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi.: 0 Ni: 0 eNi: 0
W: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 R0RÊ57AR£ 1
H-86-25
DEPARTURE(X) LATITUDE(Y1 EiEVATI011i1) 0 0 O
06
FROM TO TYPE SS BEDROCK 110 112 80 20 112
PPM NON MAG PPM MAG VG 2909 970 0 0
Au: 135 eAu: 393 Ag: .3 eAg: .9 As: 61 eAs: 177 Cu: 49 eCu: 143 Zn: 56 eZn: 163 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIB BOBfSTAXf I
H-86-25
lEPARTURE(X) IATITUDE(Y) E.EUATION(Z1 0 0 0
• 07
FROM TO TYPE SS BEDROCK 112 117 90 30 112
An Pr PROCESSED lEDROCI
PPM NON MAG PPM MAG VG 13662 472 0 0
Au: 2.5 Ag: .6 As: 129 Cu: 104 Zn: 20 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM **F* EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE e A g ******* EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn *
- EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 34 eAg: 8.2 eAs: 1762 eCu: 1421 eZn: 273 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: O
MAX
OIE EORESTAKf I
H-86-26
DEPARTIIREIX) LATITIlDEIYI ELEVATIONIZI a o 0
1-1A
FROM TO TYPE SS BEDROCK 73 74 80 20 74
PPM NON MAO PPM MAG VO 1933 1333 0 0
Au: 90 Ag: 6.8 As: 351 Cu: 820 Zn: 48 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
eAu: 174 eAg: 13.1 eAs: 679 eCu: 1585 eZn: 93 eSb: 0 eBa: 0 eCr: 0 *Co: o eNi: 0 eNi: O eW: 0
Surface EEEE MIN MAX EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag *******X X X Xif X X X X X** EEEE eAg ************ EEEE As *** EEEE eAs * EEEE Cu ** EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
011 BOAESTRIE I
H-86-27
IEPARTUREIX) LATITUDEIT) ELEVATIONIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 71 75 80 10 82
PPM NON MAG PPM MAG VG 3034 2759 0 0
eAu: 1366 eAg: 2.4 eAs: 1135 eCu: 346 eZn: 97 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 450 Ag: .8 As: 374 Cu: 114 Zn: 32 Sb: O Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 *9F EEEE eAg *# EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE . Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N O000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Old RONESIAKE I
H-86-27
BEPARTUREtXf LATITUDE(T) ELEVATIDii(Z1 O 0 O
02
FROM TO TYPE SS BEDROCK 75 80 80 20 82
PPM NON MAG PPM MAO VG 3176 2941 1.6 0
eAu: 1048 eAg: 1.9 eAs: 788 eCu: 426 eZn; 108 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi,: 0 eNi: 0 eW: 0
Au: 330 Ag: .6 As: 248 Cu: 134 Zn: 34 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
019 AOAESYAfE 1
H-86-27
IEPARTIIREIX) LATITUIE(Y) ELEUATIO?II?) a o 0
03
FROM TO TYPE SS BEDROCK 80 82 80 20 82
PPM NON MAG PPM MAG VG 4806 2444 0 0
eAu: 1153 eAg: 2.9 eAs: 1778 eCu: 615 eZn: 221 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 240 Ag: .6 As: 370 Cu: 128 Zn: 46 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu 9E EEEE Ag * EEEE eAg ** EEEE As **HF EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 96 EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo' N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 20 Ag: 1.4 As: 380 Cu: 1500 Zn: 80 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: O W: 0
eAu: 67 eAg: 4.7 eAs: 1277 eCu: 5040 eZn: 269 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 BOpESTAKE I
H-86-28
9EPARTIRZElX) LATIi11DE(Y) ELE9ATI0111Z) 0 0 0
1-1A
FROM TO TYPE SS BEDROCK 78 79 80 20 79
30S IYRITE
PPM NON MAG PPM MAG VG 3360 1653 0. 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag **** EEEE eAg ***HE EEEE As *** EEEE eAs * EEEE Cu ***** EEEE eCu *iHE*HE* EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Old OOAESTAff I
H-86-29
DEPARTUREIX) LATITUOE(Y) ELEVATIONIZ) O a o
01
FROM TO TYPE SS BEDROCK 87 92 80 20 99
PPM NON MAG PPM MAO VG 3881 3000 0 0
eAu: 427 eAg: 2.3 eAs: 1987 eCu: 582 eZn: 144 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 110
As: 512 Cu: 150 Zn: 37 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ****HF EEEE eAs 9E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 12.5 Ag: .6 As: 334 Cu: 80 Zn: 35 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: 0
W: O
eAu: 51 eAg: 2.4 eAs: 1357 eCu: 325 eZn: 142 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: O eNi: 0 eW: O
011 ROMESTARE I
H-86-29
DEPARTUREtX) LATITUDEtYI ELEVATIONtZ) 0 O 0
02
FROM TO TYPE SS BEDROCK 95 99 80 20 99
PPM NON MAG PPM MAG VG 4063 2730 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag •)E EEEE eAg *•1E EEEE As *** EEEE eAs * _ EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn •)E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 90A(STA,lf I
H-86-29
IEPARTUREIX) LATITUDE(T) ELEYAIIONIZ) 0 O 0
O1A
FROM TO TYPE SS BEDROCK 92 95 80 20 99
PPM NON MAO PPM MAO VG 2743 2743 0 0
Au: 165 Ag: .4 As: 392 Cu: 68 Zn: 43 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -)E EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
eAu: 453 eAg: 1.1 eAs: 1075 eCu: 187 eZn: 118 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
018 80RESTARE I
H-86-30
9EPARTI1REiX1 LATITUHEfY1 ELFUATIOMtZI 0 0' O
01-2
FROM TO TYPE SS BEDROCK 84 94 80 20 94
PPM NON MAG PPM MAG VG 4904 1925 0 0
Au: 230 Ag: .05 As: 141 Cu: 42 Z n : 32 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: O
Surf ace EEEE MIN EEEE NM * 'EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 1128 eAg: .2 eAÇ: 692 eCu: 206 eZn: 157 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 80 Ag: .8 As: 472 Cu: 200 Zn: 80 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 44: 0
eAu: 102 eAg: 1 eAs: 599 eCu: 254 eZn: 102 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: O eNi: 0 eW : 0
0/8 BORESTAXE I
H-86-33
DEPARTNREIX) LATITUDEITI ELEVATIONII) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 74 85 80 10 91
PPM NON MAG PPM MAG VG 1270 910 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
NI NOMME I
H-86-33 DEPAP.TU4EIX1 LATITUDEIYI ELEVATIOliIZI
0. 0 0
03
FROM TO TYPE 8S BEDROCK 85 88 80 20 91
PPM NON MAO PPM MAG VG 4314 2510 0 C
Au: 175 eAu: 755 Ag: .6 eAg: 2.6 As: 386 eAs: 1665 Cu: 108 eCu: 466 Zn: 104 eZn: 449 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
013 BO!lESlAdE I
H-86-33
DEPARTUREtXI LATITuDEtTI EiE1iA:*:01112) 0 0 0
04
FROM TO TYPE SS BEDROCK 88 91 80 20 91
PPM NON MAG PPM MAG VG 3804 2353 0 0
Au: 230 eAu: 875 Ag: .6 eAg: 2.3 As: 552 eAs: 2100 Cu: 108 eCu: 411 Zn: 100 eZn: 380 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 180 Ag: .05 As: 130 Cu: 100 Zn: 40 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
eAu: 442 eAg: .1 eAs: 319 eCu: 246 eZn: 96 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
P!à 90AES?AdE I
H-86-34
DEPARTURE IXI LATITUDE{Y) ELEVATIOM (Z1 0 O 0
01-2
FROM TO TYPE SS BEDROCK 80 82 80 20 82
PPM NON MAO PPM MAO VO 2456 2152 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg 9F EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 !OESTRE I
H-86-35
BEPARTUREIX) LATITUBEtY) EiE+fATIOIIiZ) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 89 95 80 10 125
PPM NON MAG PPM MAO VG 2033 1650 .9 0
Au: 450 eAu: 915 Ag: .1 eAg: .2 As: 346 eAs: 703 Cu: 134 eCu: 272 Zn: 37 eZn: 75 - Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1 1 1 1 e S b N EEEE Ba N EEEE eRa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01B BOAfS'AKf I
H-86-35
DEPARTUREIX) LATITUDE(Y) ELEYATIONIZ) O 0 O
03-4
FROM TO TYPE SS BEDROCK 95 105 80 10 125
PPM NON MAG PPM MAG VG 2459 1928 .7 0
Au: 760 eAu: 1869 Ag: .6 eAg: 1.5 As: 284 eAs: 698 Cu: 90 eCu: 221 Zn: 36 eZn: 89 Sb: 0 eSb: 0 Ba: 0 eBa: O Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 115 Ag: 1.2 As: 1~'" Cu: 198 Zn: 49 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
eAu: 241 eAg: 2.5 eAs: 277 eCu: 415 eZn: 103 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OM BOIlEJAXE I
H-86-35
DEPARTURE(X) LATITUDEIY) ELEYATIOiI:Z) O O O
05-6
FROM TO TYPE SS EEDROC:< 105 115 80 10 125
PPM NON MAG PPM MAO VO 209S 203 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg ** EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0!d AOAES7A,fE I
H-86-35
DEPARTUREIX! LATITUDEtY? ELEUATION121 0 o a
07
FROM TO TYPE SS BEDROCK 115 120 80 20 125
PPM NON MAO PPM MAG VG 1856 1550 0 0
Au: 150 eAu: 278 Ag: .6 eAg: 1.1 As: 155 eAs: 288 Cu: 100 eCu: 186 Zn: 36 eZn: 67 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Old RORfSTARf I
H-86-35
DEPARTUREIX) LATITUDEIY) ELEyATIONIZi O 0 0•
08-9
FROM TO TYPE SS BEDROCK 120 122 80 20 125
SS PYRITE
PPM NON MAG PPM MAG VG 2813 1725 2.9 O
eAu: 1069 eAg: 2.3 BAs: 743 eCu: 293 eZn: 200 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: C eNi: 0 eW: 0
Au: 380 Ag: .8 As: 264 Cu: 104 Zn: 71 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *IF EEEE eAg ** EEEE As *IF EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 3333 eCr N EEEE Co N XXXX eCo N XXXX Ma N
eMo N Ni N
eNi N W N
eW N
MAX
0!D 90RfSTA[f I
H-86-36
DEPARTUREIXI LATITUDEITI ELEvATI01iIZ1 0 0 0
01
FROM TO TYPE SS BEDROCK 82 85 80 10 113
PPM NON MAO PPM MAO VG 3570 2581 0 0
eAu: 107 eAg: 2.1 eAs: 1100 eCu: 464 eZn: 200 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 30 Ag: .6 As: 308 Cu: 130 Z n : 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 170 Ag: .6 As: 268 Cu: 220 Zn: 49 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: 0
W: O
eAu: 551 eAg: 1.9 eAs: 869 eCu: 713 eZn: 159 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 ROAfSIARE 1
H-86-36
DEPARTUREiXI LATITUDEfT) ELEYATIDNIZ) D 0 0
02
FROM TO TYPE SS BEDROCK 85 95 80 10 113
PPM NON MAG PPM MAG VG 3241 2154 1.6 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -)E EEEE As *-lE EEEE *As * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
OJ! BC!lESTIülE 1
H-86-36
BEPARTIIREfXI LATITL'DEtT) ELEVATIORlZI 0 0 0
03-4
FROM TO TYPE SS BEDROCK 95 113 80 20 113
PPM NON MAG PPM MAG VG 2291 1781 0 0
Au: 220 Ag: .8 As: 896 Cu: 90 Zn: 43 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg *. EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N O000 Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 504 eAg: 1.8 eAs: 2053 eCu: 206 eZn: 99 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
OIS ROAESTAKE 7
H-86-36
IEPARTUREtX) LATITUaEtY1 ELEVATIBNtZi 0 O 0
05
FROM TO TYPE SS BEDROCK 113 118 90 30 113
PROCESSED BEDROCK
PPM NON MAG PPM MAG VG 1146 421 1.9 0
Au: 265 eAu: 304 Ag: 5.6 eAg: 6.4 As: 2000 eAs: 2292 Cu: 3100 eCu: 3553 Zn: 1280 eZn: 1467 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: O Co: O eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 . eW: 0
Surface EEEE MIN MAX EEEE NM * EEEE MAG *
• EEEE Au * EEEE eAu * EEEE Ag **************** EEEE eAg ***** EEEE As ******************* ESEE eAs * EEEE Cu ********** EEEE eCu ##** EEEE Zr: *** EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N . 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
Au: 100 Ag: .6 As: 352 Cu: 160 Zn: 53 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 w: O
eAu: 283 eAg: 1.7 eAs: 997 eCu: 453 eZn: 150 eSb: O eBa: 0 eCr: O eCo: O eNi: 0 eNi: 0 eW: 0
013 100ESTAXf 1
H-86-37
IEPARTtptEtX1 LATITUIEITI ELEVATIONIZI 0 Q O
01
FROM TO TYPE SS BEDROCK 93 103 80 20 103
PPM NON MAS PPM MAG VG 2831 2119 1.5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Old 0010741f I
H-86-38
DEPARTOREIX) LATITUDEfY) ELENATIODIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 94 104 80 10 110
PPM NON MAO PPM MAS VG 4000 2804 0 0
eAu: 1160 eAg: 3.2 eAs: 1344 eCu: 528 eZn: 232 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: 290 Ag: .8 As: 336 Cu: 132 Zn: 58 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE' eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 BOIIESTRlE I
H-86-38
DEPARTURE(X) LATITIlDE1T1 ELEVATION(Z) O O 0
02
FROM TO TYPE SS BEDROCK 104 110 80 20 110
PPM NON MAS PPM MAO VG 3164 2149 0 0
Au: 145 eAu: 459 Ag: .7 eAg: 2.2 As: 268 eAs: 848 Cu: 180 eCu: 570 Zn: 64 eZn: 203 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *NE EEEE As 9F# ELLE eAs * EEEE Cu * EEEE eCu * EEEE. .Zn 9(- EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 1090 Ag: .4 As: 488 Cu: 100 Zn: 34 Sb: 0 Ba: 0 Cr. 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 2731 eAg: 1 eAs: 1223 eCu: 251 eZn: 85 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
da BOAESIAfE I
H-86-39 -
BEPARTUREIRI LATITUBEIYI ELEVATIONIZI 0 0 0
01-2
FROM TO TYPE SS BEDROCK 90 110 80 10 128
15% PYRIIE
PPM NON MAG PPM MAG VG 2506 2553 6.1 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***9E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 8883 Sb N 8888 eSb N 8888 Ba N 8888 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Old OMM I
H-86-39
DEPARTURE(X} LATITUDE(T1 ELEVATIOMtZI 0 0 O
03
FROM TO TYPE SS BEDROCK 110 115 80 10 128
PPM NON MAG PPM MAG VG 4370 3759 0 0
eAu: 262 eAg: 2.6 eAs: 1669 eCu: 830 eZn: 284 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Au: 60 Ag: .6 As: 382 Cu: 190 Z n : 65 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N. EEEE Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 100 Ag: .4 As: 290 Cu: 66 Zn: 42 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 325 eAg: 1.3 eAs: 943 eCu: 215 eZn: 137 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
01! PO!lESTALE I
H-86-39
DEPARTUREiX1 LATITUDEtYI ELE'dATIlUi1Z1 D D o
04
FROM TO TYPE SS BEDROCK 115 120 80 20 128
!SS PYRITE
PPM NON MAO PPM MAG VG 3251 3781 5.2 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au i(- EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zh * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 4444 eBa N 4444 Cr N ELLE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/8 R08ES7ALE I
H-86-39
DEPARTURE(X) LATITUDE(Y1 ELEVATIDi((Z1 0 0 0
05
FROM TO TYPE SS BEDROCK 120 125 SO 20 128
20% PYRITE
PPM NON MAG PPM MAG VG 11111 3150 4.6 0
Au: 170 eAu: 1889 Ag: .3 eAg: 3.3 As: 1072 eAs: 11911 Cu: 60 eCu: 667 Zn: 37 eZn: 411 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM *** EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *** EEEE As ******?E**E EEEE eAs xxxx* EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 3333 Cr N 3333 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 10 Ag: .6 As: 512 Cu: 62 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O
W: 0
eAu: 214 eAg: 12.9 eAs: 10968 eCu: 1328 eZn: 85? eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
d!E EOAESTAAE I
H-86-39
DEPARTURE(X) LATITUDEiYl ELEUATIOI)tZl 0 0 0
06.
FROM TO TYPE SS BEDROCK 125 128 60 20 128
25% PYRITE
PPM NON MAG PPM MAG VG 21422 4018 0 0
Surface EEEE MIN EEEE NM **HEdHE* EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ***iF**IEaE?HE** EEEE As xxxx* EEEE e A s **** EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 8011ESTAIE I
H-86-40
DEPART10tE(X) LATITUDE(T1 ELEVBTIONIZl 0 0 0
01
FROM TO TYPE SS BEDROCK 65 75 80 20 78
PPM NON MAG PPM MAG VG 3111 2512 0 0
Au: 280 eAu: 871 Ag: .8 eAg: 2.5 As: 714 eAs: 2221 Cu: 130 eCu: 404 Zn: 68 eZn: 212 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: O Co: 0 eCo: O Mo: O eNi: 0 Ni: O eNi: O
W: 0 eW: 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg *HE EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O13 !OMETTRE I
H-86-40
DEPARTUREIXI LATITUDEIYI ELEVATIOMIZI 0 0 0
02
FROM TO TYPE SS BEDROCK 75 78 80 20 78
15% MYRTE
PPM NON MAG PPM MAG VG 3080 2629 3 0
Au: 390 eAu: 1201 Ag: .4 eAg: 1.2 As: 344 eAs: 1059 Cu: 188 eCu: 579 Zn: 82 eZn: 253 Sb: 0 eSb : O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Su rf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *IE# EEEE eAs * EEEE Cu * EEEE eCu * •EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 2222 eCr N 2222 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
JIB NOMME I
H-86-42
DEPARTUREIX) LATITUDEtY) ELE4ATIONIZ) O O O
01
FROM TO TYPE SS BEDROCK 78 80 80 20 80
PPM NON MAG PPM MAG VG 5075 3545 0 0
eAu: 254 eAg: 2.5 eAs: 1583 eCu: 913 eZn: 274 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 50 Ag: .5 As: 312 Cu: 180 Zn: 54 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9E EEEE Ag 9E EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 9oAESrA,ff I
H-86-43
9EPARTIOIE(X) LATITIlOEtT) ELEYATIWttZ) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 72 83 80 10 88
PPM NON MAO PPM MAG VG 3183 2845 .8 0
Au: 205 eAu: 653 Ag: .8 eA9: 2.5 As: 372 eAs: 1184 Cu: 140 eCu: 446 Zn: 57 eZn: 181 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: O
W: O eW: 0
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N _- W N eW N
MAX
Of! AOAESTAdE I
H-86-43
DEPARTURE(X) LATITUDEITI ELEYATION(Z1 0 O O
03
FROM TO TYPE SS BEDROCK 83 88 80 20 88
PPM NON MAO PPM MAG VG 3741 2796 1.5 0
Au: 300 Ag: .1 As: 720 Cu: 136 Zn: 50 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 1122 eAg: .4 eAs: 2693 eCu: 509 eZn: 187 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
0!3 4DAfST14RF I
H-86-45 DEoARTUREIXI LATITUDE(Y) ELEIfATIDN(ZI
0 0 0
01-2
FROM TO TYPE SS BEDROCK 85 95 80 10 117
10% PYRITE
PPM NON MAG PPM MAG VG 2247 2012 5.9 0
eAu: 562 eAg: .9 eAs: 1096 eCu: 288 eZn: 143 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 250 Ag: .4 As: 488 Cu: 128 Zn: 66 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 6666 Sb N 6666 eSb N 6666 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 50 Ag: .6 As: 280 Cu: 80 Zn: 54 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 159 eAg: 1.9 eAs: 890 eCu: 254 eZn: 172 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
90!lESTAdE .►
H-86-45
lEPARTUREIXI LATITU);EIY1 ELEVATION(ZI 0 0 O
03
FROM TO TYPE SS BEDROCK 95 105 80 10 117
PPM NON MAO PPM MAG VG 3179 2092 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *9E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE .eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Old RORESTARE I
H-86-45
DEPARTUREIX) LATITUDE(Y) ELEVATIIa(IZ) 0 0 0
04
FROM TO TYPE SS BEDROCK 105 113 80 20 117
PPM NON MAG PPM MAG VG 4121 2828 0 0
Au: 195 eAu: 804 Ag: .4 eAg: 1.6 As: 568 eAs: 2341 Cu: 108 eCu: 445 Zn: 48 eZn: 198 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: O eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 'E EEEE Sb N EEEE eSb N EEEE Ba N O000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni .N
eNi N W N
eW N
MAX
OIS MOMhSTAIE I
H-86-45
IEPARTUREtX) LATITUDEIY) ELEVATION{Z) 0 O 0
05
FROM TO TYPE SS BEDROCK 113 117 80 20 117
PPM NON MAG PPM MAG VG 3099 2385 0 0
eAu: 759 eAg: 1.2 eAs: 1029 eCu: 341 eZn: 124 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: 245 Ag: .4 As: 332 Cu: 110 Zn: 40 Sb: O Ba: 0 Cr: O Co: O Mo: O Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
4!d B^1lf8TAIf :
H-86-46
DEPARTUREIX! LATITUDEIY} ELEUATIONIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 50 52 80 20 52
PPM NON MAG PPM MAG VG 2995 3169 0 0
eAu: 1138 eAg: 3.6 eAs: 1761 eCu: 988 eZn: 282 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 380 Ag: 1.2 As: 588 Cu: 330 Zn: 94 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag **# EEEE eAg *** EEEE As ***** EEEE eAs -DE EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
91F 9M. ES7AlE 1
H-86-47
OEPARTURE(X) LATITUDE (Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 50 52 80 20 52
PPM NON MAG PPM MAG VG 3947 2400 0 0
Au: 55 Ag: .6 As: 332 Cu: 260 Zn: 64 Sb: 0 Ba: U Cr: O Co: 0 ho: O Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: <^i7 eAg: 2,4 eAs: 1310 eCu 1026 eZn: 253 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: O eNi: 0 eW: 0
MAX
013 NORESTAIE I
H-86-47
1EPARTDREI%) LATITIIDEfY) ELEVATIDNIZI 0 0 0
O1A
FROM TO TYPE SS BEDROCK 50 52 80 20 52
DIA 01 MASO
PPM NON MAG PPM MAG VG 4288 2468 0 0
eAu: 64 eAg: 1.3 eAs: 2539 eCu: 1544 eZn: 326 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 15 Ag: .3 As: 592 Cu: 360 Zn: 76 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **#** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/1 d0A1STAR1 1
H-86-48
DEPARTURE(X) LATITUDE(Y) ELEVATION(:) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 91 100 80 10 112
PPM NON MAO PPM MAG VG 3102 2542 0 0
eAu: 651 eAg: 1.2 eAs: 1042 eCu: 416 eZn: 133 eSb: O eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: O eW: 0
Au: 210 Ag: .4 As: 336 Cu: 134 Zn: 43 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
011 10RÊST4dÉ I
H-86-48
DEPARTUREtXI LATITUIE(T1 ELEVATION(Zl 0 0 0
03
FROM TO TYPE SS BEDROCK 100 103 80 10 112
PPM NON MAG PPM MAG VG 3200 2809 0 0
eAu: 304 eAg: 3.2 eAs: 1235 eCu: 384 eZn: 93 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eN i : 0 eW: O
Au: 95 Ag: 1 As: 386 Cu: 120 Zn: 29 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg #* EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9P EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N O000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Olt é0llESTAZE I
H-86-48
IEPARTUREIXI LATITUIEtYI ELEVATIGNlZI 0 0 0
04
FROM TO TYPE SS BEDROCK 103 106 80 10 112
PPM NON MAG PPM MAG VO 4095 2724 0 0
eAu: 1044 eAg: 2.5 eAs: 1122 eCu: 557• eZn: 147 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
Au: 255 Ag: .6 As: 274 Cu: 136 Zn: 36 Sb: O Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *HE EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 65 Ag: 1 As: 1000 Cu: 250 Zn: 49 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
eAu: 198 eAg: 3 eAs: 3039 eCu: 760 eZn: 149 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0
eW: O
013 BPMES7ARE 1
H-86-48 BEPARTUREtX1 LATITUBEtT1 ELEUATIOliIZ1
0 0 0
05
FROM TO TYPE SS BEDROCK 106 110 80 20 112
PPM NON MAG PPM MAG VG 3039 2902 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As ********* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O!! POAESTAdF I
H-86-48
IiEPARTUREI%) LATITU>tE1Yl ELEYAT ION (II 0 0 0
06
FROM TO TYPE SS BEDROCK .110 112 80 20 112
lR PYRITE
PPM NON MAG PPM MAG VG 6426 1593 0 0
eAu: 161 eAg: 3.9 eAs: 1928 eCu: 900 eZn: 456 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 25 Ag: .6 As: 300 Cu: 140 Zn: 71 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *** EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu 9F EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
? I B IIONESTAdE I
H-86-49
DEPARTUREIXI LATITUDEITI ELEUATIO11IZ1 0 0 0
01-2
FROM TO TYPE SS BEDROCK 56 57 80 20 57
PPM NON MAG PPM MAG VG 2500 1833 1.3 0
Au: 2930 eAu: 7325 Ag: .5 eAg: 1.3 As: 384 eAs: 960 Cu: 200 eCu: 500 Zn: 52 eZn: 130 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn- * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 240 Ag: .8 As: 373 Cu: 200 Zn: 62 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni : 0 W: 0
eAu: 483 eAg: 1.6 eAs: 750 eCu: 402 eZn: 125 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0l3 AORESTAdE I
H-86-50
DEPARTUREIXI LATITUDESYI ELEVATION IV O O O
01-2
FROM TO TYPE SS BEDROCK 58 60 80 20 60
PPM NON MAO PPM MAO VO 2012 1848 .9 0
Sur-Face EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EÇEE Ag ** EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * ELLE 211 * EÇEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Olè !MESURE I
H-86-51
IE'ARTURE(XI LATITUIE(Y) ELEATION(Z) 0 O O
O1A
FROM TO TYPE SS BEDROCK 80 81 80 20 81
MP 01 WASP
PPM NON MAG PPM MAG VG 3077 923 0 0
Au: 200 eAu: 615 Ag: .8 eAg: 2.5 As: 282 eAs: 868 Cu: 320 eCu: 985 Zn: 64 eZn: 197 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As *9F EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
ara MAMIE I
H-86-51
DEPARTUREIXI LATITU9EIT) ELEVATIOIIIZ) o a o
01
FROM TO TYPE SS BEDROCK 80 81 80 20 81
PPM NON MAG PPM MAG VG 3619 2667 0 0
Au: 250 eAu: 905 Ag: .6 eAg: 2.2 As: 132 eAs: 47e Cu: 260 eCu: 941 Zn: 68 eZn: 246 Sb: O eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As * EEEE eAs ?E EEEE Cu * EEEE eCu * EEEE Zn * EEEt eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
• Mr"►:<
Au: 330 Ag: .8 As: 177 Cu: 158 Zn: 68 Sb: 0 Be: 0 Cr: 0 Co: 0 Mo: 0 Ni: O W: 0
eAu: 698 eAg: 1.7 eAs: 375 eCu: 334 eZn: 144 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/D PORFS7ALF I
H-86-52
DEPARTUREIXI LATITUDEITD ELEVATI011Q1 0 0 0
OlA
FROM TO TYPE SS BEDROCK 70 72 80 20 72
119P 01 YASS
PPM NON MAG PPM MAG VG 2116 1989 1.7 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu -1F EEEE Ag *E EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Ma N
eMo N Ni N eNi N W N eW N
MAX
013 901lE3TAtE I
H-86-52
DEPARTUREiX) LATITUDEIY) ELESIATIOAII) 0 0 0
01
FROM TO TYPE SS BEDROCK 70 72 80 20 72
PPM NON MAG PPM MAS VG 4215 3484 0 0
Au: 135 eAu: 569 A9: .6 eAg: 2.5 As: 318 eAs: 1340 Cu: 184 eCu: 776 Zn: 80 eZn: 337 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 12.5 Ag: .6 As: 134 C u : 340 Zn: 66 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 44 eAg: 2.1 eAs: 468 eCu: 1187 eZn: 230 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
el! AOl!IS7ARf 1
-94 -53
DEPARTUREIX) LATITUDEIY) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 60 61 80 10 72
PPM NON MAG PPM MAG VG 3492 2095 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 320 Ag: 1.4 As: 356 Cu: 2200 Zn: 43 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O
W: 0
eAu: 853 eAg: 3.7 eAs: 949 eCu: 5867 eZn: 115 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Oit 9ODESTAIE 1
H-86-53
1#PARTUREIX) LATITI)➢EIT1 ELEVATION(Z1 0 0 0
02
FROM TO TYPE SS BEDROCK 61 65 80 10 72
201 PT AIDE DODLDEdS
PPM NON MAG PPM MAG VG 2667 1258 1.5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ***dF EEEE eAg *** EEEE As *** EEEE eAs * EEEE Cu ***E*** EEEE eCu ******* EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Ca BOAfSTpLF 1
H-86-53
DEPARTURE(x) LATITUIE(Y) ELEVATION(Zl 0 0 0
03
FROM TO TYPE SS BEDROCK 65 70 80 20 72
15% P1117E
PPM NON MAG PPM MAG VG 3762 2524 5.7 0
eAu: 451 eAg: 3.8 eAs: 1264 eCu: 647 eZn: 177 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Au: 120 Ag: 1 As: 336 Cu: 172 Zn: 47 Sb: 0 Ba: O Cr: O Co: 0 Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *HE EEEE eAg **HE EEEE As *)F* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 3333 Cr N 3333 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Ola 9ONESTARE I
H-86-53
OEPARTIIREtX3 LATITUàElY1 ELEYBTIOMIZI 0 0 0
04
FROM TO TYPE SS BEDROCK 70 72 80 20 72
IR PYRITE
PPM NON MAG PPM MAG VG 6182 1939 9.7 0
eAu: 3462 eAg: 7.4 eAs: 2967 eCu: 1088 eZn: 371 eSb: 0 eBa: O eCr: 0 eCo: O eNi: 0 eNi: 0 eW : 0
Au: 560 Ag: 1.2 As: 480 Cu: 176 Zn: 60 Sb: 0 Ba: O Cr: 0 Co: O Mo: O Ni: O W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg *****HE EEEE As ***-IE EEEE eAs 9E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Old IOMESTALE 1
H-86-54
1EPARTUREIXI LATITUBEtY) ELEVATIONIZI O O O
01-2
FROM TO TYPE SS BEDROCK 57 62 80 20 62
15% PYRITE
PPM NON MAG PPM MAG VG 2380
Au: 135 Ag: 1 As: 504 Cu: 200 Zn: 63 Sb: 0 Ba: O Cr: 0 Co: O Mo: O Ni: 0
W: O
2505 6 0
eAu: 321 eAg: 2.4 eAs: 1200 eCu: 476 eZn: 150 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 6666 Cr N 6666 eCr N 6666 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 365 Ag: .8 As: 386 Cu: 160 Zn: 48 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O
W: 0
eAu: 941 eAg: 2.1 eAs: 995 eCu: 412 eZn: 124 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/d NDI)E57AL( I
H-86-55
DEPARTUREIX) LATITUDEIT) ELEVATIB)IZ) D 0 0
01
FROM TO TYPE SS BEDROCK 65 72 80 10 93
15% PYRITE
PPM NON MAG PPM MAG VG 2578 2222 8.5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 6666 eZn * 6666 Sb N 6666 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
4/d R?RFSTARf 1
H-86-55
lEP#RTIOtE(X) 1.ATITODE(T1 ELEVIITIlItIIZI 0 0 0
02-3
FROM TO TYPE SS BEDROCK 72 80 80 10 93
PPM NON MAG PPM MAO VG 2106 2032 .8 0
eAu: 284 eAg: 1.3 eAs: 1146 eCu: 312 eZn: 99 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 135 Ag: .6 As: 544 Cu: 148 Zn: 47 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg -IF EEEE As ***** EEEE eAs ?E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Old AOIlESTAiit I
H-86-55
SEPARTUREIXI LATITUpEITI ELE9ATIOAIZI O O O
04
FROM TO TYPE SS BEDROCK 80 85 80 10 93
PPM NON MAG PPM MAG VG 3316 4421 C 0
eAu: 182 eAg: .2 eAs: 1220 eCu: 484 eZn: 126 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
Au: 55 Ag: .05 As: ?68 Cu: 146 Zn: 38 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu -IF EEEE ?n * EEEE eZn * EEEE Sb -N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N N
eNi N W N eW N
MAX
Old 8ONZS7111E I
H-86-55
DEPARTURE(Xl LATITUDE(Y) ELEUATIDBIZ) 0 O 0
05
FROM TO TYPE SS BEDROCK 85 89 80 20 93
PPM NON MAG PPM MAG VO 2617 1883 1.3 0
Au: 540 Ag: .05 As: 696 Cu: 88 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: O W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
eAu: 1413 eAg: .1 eAs: 1821 eCu: 230 eZn: 115 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
MAX
O/D OOAfSTA,tf I
H-86-55
BEPARTURElX1 LATITUBElY1 ELEYATIONlZ1 0 0 0
OSA
FROM TO TYPE SS BEDROCK 89 93 80 20 93
PPM NON MAO PPM MAG VG 3086 1962 0 0
eAu: 1111 eAg: .2 eAs: 1086 eCu: 265 eZn: 148 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 360 Ag: .05 As: 352 Cu: 86 Zn: 48 Sb: O Ba: 0 Cr: 0 -
Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 8010TA,(E I
H-86-56
DEPARTURE(X1 LATITUDE(Y1 ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 87 95 80 10 115
101 PYRITE
PPM NON MAG PPM MAG VG 4271 2725 6.2 0
eAu: 3459 eAg: 2.6 eAs: 2870 eCu: 675 eZn: 158 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 810 Ag: .6 As: 672 Cu: 158 Zn: 37 Sb: 0 Ba: O Cr: 0 Co: O Mo: O Ni: O W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *E**** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 4444 eSb N 4444 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OC ROIFSTArtF I
H-86-56
IEPARTUREIII! LATITUDEITI ELEVATIONIZI 0 0 0
02-3
FROM TO TYPE SS BEDROCK 95 105 80 10 115
11?S PMU
PPM NON MAG PPM MAG VG 2058 1932 3.9 0
Au: 130
eAu: 268 Ag: .05
eAg: .1 As: 15
eAs: 31 Cu: 28
eCu: 58 Zn: 23
eZn: 47 Sb: 0
eSb: 0 Ba: O
eBa: 0 Cr: 0
eCr: 0 Co: O
eCo: 0 Mo: 0
eN i' : 0 Ni: O
eNi: 0
W: O
eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 1F EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 5555 Ba N 5555 eBa N 5555 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi tJ W N eW N
MAX
Au: 1670 Ag: .6 As: 536 Cu: 160 Zn: 36 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: O
W: 0
eAu: 4652 eAg: 1.7 eAs: 1493 eCu: 446 eZn: 100 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/l AOAESTA[E I
H-86-56
DEPARTUREl:) UTITUDEIY) ELEYATIWNIZ) W W W
04-5
FROM TO TYPE SS BEDROCK 105 115 80 20 115
In PYAITE
PPM NON MAG PPM MAG VG 2786 2114 6.9 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9F EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 8888 Cr N 8888 eCr N 8888 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 B011fSTlUE I
H-86-57
DEPARTURE(X) LATITUIE)Y) ELEVATION Q) 0 0 0
01
FROM TO TYPE SS BEDROCK 70 80 80 10 120
15% PYRITE
PPM NON MAG PPM MAG VG 5108 4246 9.8 0
Au: 120 Ag: .8 As: 370 Cu: 156 Zn: 56 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag 9E* EEEE eAg *** EEEE As *** EEEE eAs * EEEE Cu * 6666 eCu * 6666 Zn * 6666 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 613 eAg: 4.1 eAs: 1890 eCu: 797 eZn: 286 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
MAX
DII BOdES7A[E I
H-86-57
REPARTURE(XI LATITUIE(T) ELEVATION(I) 0 0 0
02-3
FROM TO TYPE SS BEDROCK 80 90 80 10 120
20% MME
PPM NON MAG PPM MAG VG 3131 3040 6.5 0
Au: 920 eAu: 2881 Ag: .6 eAg: 1.9 As: 928 eAs: 2906 Cu: 176 eCu: 551 Zn: 64 eZn: 200 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *E*IE*iFjHF* EEEE eAs * EEEE Cu 9F EEEE eCu * EEEE Zn * 8888 eZn * 8888 Sb N 8888 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIS IORESTAI£ I
H-86-57
DEPARTUREIXI LATITUDEtT: ELEVATIORIZ) 0 0 0
04-5
FROM TO TYPE SS BEDROCK 90 100 80 10 120
PPM NON MAG PPM MAO VG 3299 2226 0 0
Au: 90 eAu: 297 Ag: 1 eAg: 3.3 As: 564 eAs: 1861 Cu: 144 eCu: 475 Zn: 108 eZn: 356 Sb: 0 eSb: 0 Ba: 0 eBa: C Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F-)E EEEE: eAg *** EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX 1•10 N
eMo N Ni. N
eNi N W N
eW N
MAX
018 000E8741E 1
H-86-57
DEPARTURE(X) LATITUDE(Y) ELEiiATIOMIZ) 0 0 O
06
FROM TO TYPE SS BEDROCK 100 105 80 10 120
PPM NON MAG PPM MAG VG 3875 2396 0 0
eAu: 407 eAg: 3.1 eAs: 1054 eCu: 403 eZn: 221 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 105 Ag: .8 As: 272 Cu: 104 Zn: 57 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE: Au * EEEE eAu * EEEE Ag ** EEEE eAg 9E# EEEE As 'JE* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn -)E EEEE Sb N EEES eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OC lONE97AIE I
H-86-57
DEPARTUREtXI LATITUDEtY1 ELEi►ATI8ItZ1 0 0 0
07
FROM TO TYPE S8 BEDROCK 105 110 80 10 120
PPM NON MAG PPM MAG VO 3648 2870 0 0
Au: 5 eAu: 18 Ag: .6 eAg: 2.2 As: 302 eAs: 1102 Cu: 114 eCu: 416 Zn: 48 eZn: 175 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Q/d 9P!lËSIAXf 1
H-86-57
IEPARTUREIXI LATITUDEfTI ELESIATIOMIZI 0 0 O
08
FROM TO TYPE SS BEDROCK 110 115 80 20 120
PPM NON MAG PPM MAO VG 3281 1737 0 0
Au: 40 eAu: 131 Ag: .05 eAg: .2 As: 380 eAs: 1247 Cu: 88 eCu: 289 Zn: 51 eZn: 167 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 60 Ag: .8 As: 284 Cu: 110 Zn: 45 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0 Ni: O
W: O
eAu: 144 eAg: 1.9 eAs: 679 eCu: 263 eZn: 108 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Old 10l1ESTAIE I
H-86-57
DEPARTURE(X1 LATITUDE(YI ELEVATION(ZI 0 0 0
9-10
FROM TO TYPE SS BEDROCK 115 120 80 20 120
PPM NON MAG PPM MAO VO 2392 1892 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As *9F EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 440 Ag: .8 As: 616 Cu: 200 Zn: 68 Sb: O Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 599 eAg: 1.1 eAs: 839 eCu: 272 eZn: 93 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 1011151A,tE 1
H-86-58
lEPARTURE(XI U TITUBE (Y1 E1.EVATI0li iZ1 0 0 0
01-2
FROM TO TYPE SS BEDROCK 125 135 60 20 135
PPM NON MAO PPM MAG VG 1362 1104 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As iE9EjE*** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eSa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
ola eoeESTAaE r
H-86-59
DEPARTUREIX) LATITUDEIT) ELEVATIONID 0 0 0
01
FROM TO TYPE SS BEDROCK 60 63 60 10 70
PPM NON MAG PPM MAG VG 2400 1886 0 0
eAu: 684 eA9: 1.9 eAs: 1978 eCu: 408 eZn: 158 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 285 Ag: .8 As: 824 Cu: 170 Zn: 66 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As ******** EEEE eAs * EEEE Cu -)P EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
.0/3 90NESTASE 1
H-86-59
IEPARTOREtX1 LATITUDEEYI ELEVATIONEZI O 0 0
02-3
FROM TO TYPE SS BEDROCK 63 70 80 20 70
5% PYRITE
PPM NON MAG PPM MAG VG 1791
Au: 640 Ag: 1.2 As: 424 Cu: 142 Zn: 49 Sb: O Ba: O Cr: O Co: 0 Mo: O Ni: O W: 0
2169 2.4 0
eAu: 1146 eAg: 2.1 eAs: 759 eCu: 254 eZn: 88 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Sur-Face EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *IF* EEEE eAg * EEEE As **F* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 3333 Cr N 3333 eCr N 3333 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 8011fSTAlf I
H-86-60
BEPARTURE(X1 LATITUtE(Tl ELE4ATIOK(Z1 0 0 0
01
FROM TO TYPE SS BEDROCK 46 51 80 20 51
80S PYRITE
PPM NON MAO PPM MAG VG 26310 2714 15.2 0
Au: 55 Ag: .2 As: 402 Cu: 160 Zn: 60 Sb: 0 Ba: O Cr: O Co: O Mo: 0 Ni: O
W: 0
Surface EEEE MIN EEEE NM ******* EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg **** EEEE As *** EEEE eAs **** EEEE Cu * EEEE eCu ***** EEEE Zn * EEEE eZn *x EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 88a8 Cr N 8888 eCr N 888^c Co N XXXX eCo N XXXX Ma N
eMo N Ni N
eNi N W N
eW N
eAu: 1447 eAg: 5.3 eAs: 10576 eCu: 4210 eZn: 1579 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 325 Ag: .1 As: 252 Cu: 128 Zn: 98 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 906 eAg: .3 eAs: 703 eCu: 357 eZn: 273 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Ols 0093ST41E I
H-86-61
BEPARTUREtX) LATITUBEtY) ELEUATIOM(Z) 0 O 0
01-2
FROM TO TYPE SS BEDROCK 55 66 80 20 66
PPM NON MAG PPM MAG VG 2788 2083 0 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu ?E EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01110$EST4IL I
H-86-62
DEP8RT10tEtX) LATITUDE(Y) ELEVATIOR(Z) D O O
01
FROM TO TYPE SS BEDROCK 28 31 80 20 31
PPM NON MAG PPM MAG VG 4057 3007 0 0
eAu: 609 eAg: 1.6 eAs: 1444 eCu: 787 eZn: 243 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 ew: 0
Au: 150 Ag: .4 As: 356 Cu: 194 Zn: 60 Sb: O Ba: 0 Cr: O Co: O Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N- eW N
MAX
018 P0NES7A(E I
H-86-62
DEPARTURE(XI LATITUDE(YI ELriIATION(ZI 0 0 0
O1A
FROM TO TYPE SS BEDROCK 28 31 80 20 31
DPP 01 WASP
PPM NON MAG PPM MAG VG 5527 4602 1.7 0
eAu: 1161 eAg: 1.1 eAs: 2034 eCu: 1658 eZn: 420 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 210 Ag: .2 As: 368 Cu: 300 Zn: 76 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O
W: O
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu ** EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 70 Ag: .5 As: 146 Cu: 250 Zn: 69 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 15 eAg: .1 'eAs: 32 eCu: 54 eZn: 15 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OtP 50AE57Arff I
H-86-63
DEAARTUREIXI LATITUDEtY) ELE4AIIONIZ) 0 O 0
01-2
FROM TO TYPE SS BEDROCK 120 130 80 10 157
PPM NON MAG PPM MAG VG 218 1385 0 0
Surface EEEE MIN EEEE NM * EEEE MAG 4E EEEE Au * EEEE eAu * EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 105 Ag: .7 As: 304 Cu: 260 Zn: 96 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 140 eAg: .9 eAs: 405 eCu: 347 eZn: 128 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
DIN I MfS?Adf I
H-86-63
BEPARTUREI%1 LATITUBE(Y1 ELEVATIOR(21 0 0 0
03
FROM TO TYPE SS BEDROCK 130 135 80 10 157
los PYRITE
PPM NON MAG PPM MAG VG 1333 1415 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 115 Ag: .6 As: 224 Cu: 240 Zn: 84 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 213 eAg: 1.1 eAs: 414 eCu: 444 eZn: 155 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 ew: 0
011 10111V41F 1
H-86-63
IEPARTUIEtX) LATITUDEtYI ELE9ATI81IZl 0 0 0
04
FROM TO TYPE SS BEDROCK 135 145 80 10 157
PPM NON MAG PPM MAG VG 1849 1591 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 165 Ag: .3 As: 174 Cu: 132 Zri: 64 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 527 eAg: 1 eAs: 555 eCu: 421 eZn: 204 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi': 0 eNi: 0 eW: 0
013 B00E5.*AIE I
H-86-63
BEPARTIOtEtX) LATITüDE(Y) ELI:UATION(Z) 0 0 0
05
FROM TO TYPE SS BEDROCK 145 155 80 20 157
PPM NON MAG PPM MAG VG 3192 2606 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg ±E EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZrâ * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 175 Ag: .2 As: 95 Cu: 164 Zn: 62 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 621 eAg: .7 eAs: 337 eCu: 582 eZn: 220 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0!F AORfS1ASF 1
- H-86-63
DEPARTINtEIX) UTITUDEtY) ELE9ATIONIZ) 0 0 0
06
FROM TO TYPE SS BEDROCK 155 157 80 20 157
PPM NON MAG PPM MAG VG 3548 1810 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZ+., * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XX`!X, eCo N XXX.X Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Of! WRISTA f I
r H-86-64
BEPARTI0lEIX1 LATITI/E{T1 ELEIlATIONQI 0 0 0
01
FROM TO TYPE SS BEDROCK 70 75 80 20 76
•
PPM NON MAS PPM MAG VG 4524 3381 0 0
eAu: 1267 eAg: 2.7 eAs: 1579 eCu: 670 eZn: 308 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Au: 280 Ag: .6 As: 349 Cu: 148 Zn: 68 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *9E EEEE As *HF* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
OIE :9O1!fS?Aff I
H-86-64 DEPARTUREIX) LATITUDEIY) ELEUATIDNIZI
0 0 0
02
FROM TO TYPE SS BEDROCK 75 76 80 20 76
PPM NON MAG PPM MAG VG 3678 2575 0 0
eAu: 349 eAg: 2.6 eAs: 2472 eCu: 1140 eZn: 353 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Au: 95 Ag: .7 As: 672 Cu: 310 Zn: 96 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM ?E EEEE MAS * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ****** EEEE eAs -3E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZ:. * EEEE ^b N EEEE eSb PI EEEE Be. N EEEç eBa N EEEE Cr N 0000 eCr N 0000 Co N XX:•:X eCo N XXX.X M0 N
eMo N Ni N
a h) 1 N W r
eW N
MAX
Of! vnrtgTAdf I
H-86-65
DEPARTUREIX) LATITUDElY) ELEYATIOUIZI 0 0 0
01,
FROM TO TYPE SS BEDROCK 82 83 80 20 83
PPM NON MAO PPM MAG VO 2576 3684 1.8
eAu: 747 eAg: 1 eAs: 1896 eCu: 474 eZn: 747 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: C
Au: 290 Ag: .4 As: 736 Cu: 184 Zn: 290 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * FEE= eZn * EEEE Sb N EEEE eSb N. EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/3 BOAESTAIE 1
H-86-65
DEPARTURE(X) LATITUDE(T) ELEYATIONIZ) 0 0 0
OlA
FROM TO TYPE SS BEDROCK 82 83 80 20 83
DO? 01 MASO
PPM NON MAG PPM MAG VG 4850 3459 1.5 0
Au: 840 eAu: 4074 Ag: .9 eAg: 4.4 As: 808 eAs: 3919 Cu: 180 eCu: 873 Zn: 188 eZn: 912 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg **HE* EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
e M b N Ni N
=Ni N W. N
eW (`)
MAX
013 BO!lESTA:ff I
H-86-66
DEPARTUREIX) LATITUDE(Y) ELEYATION4Z) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 95 98 80 20 101
PPM NON MAG PPM MAG VG 2122 1856 0 0
eAu: 414 eAg: 1.1 eAs: 1341 eCu: 416 eZn: 272 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 195 Ag: .5 As: 632 Cu: 196 Zn: 128 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0 Ni: 0 W: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au j(- EEEE eAu * EEEE Ag * EEEE eAg * EEEE As i4-jF*-iE*E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 110 Ag: .3 As: 182 Cu: 160 Zn: 76 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 446 eAg: 1.2 eAs: 738 eCu: 649 eZn: 308 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Old OOffg7Açr I
H-86-66
àEPARTIIRElXI LATITUOE(Y) ELEVATIONiZ) 0 0 0
03
FROM TO TYPE SS BEDROCK 98 101 60 20 101
PPM NON MAG PPM MAG VG 4057 3467 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 95 Ag: .2 As: 106 Cu: 164 Zn: .72 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: O
eAu: 553 eAg: 1.2 eAs: 617 eCu: 954 eZn: 419 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
013 90NESTALE I
H-86-67
DEPARTIIREIXI LATIT11DEtY) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 83 84 80 20 84
PPM NON MAO PPM MAG VG 5818 4364 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE .eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 'Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
:!* OMETTAIT I
H-86-67
BEP1R?UREIXI LATITIIDEtYI ELEVIITIOIIIZI 0 0 t!
01A
FROM TO TYPE SS BEDROCK 83 84 80 20 84
DD? 01 WAS6
PPM NON MAG PPM MAO VO 3323 2072 0 0
eAu: 83 eAg: 2 eAs: 1010 eCu: 532 e2n: 492 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Au: 25 Ag: .6 As: 304 Cu: 160 Zn: 148 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZi7 * EEEE Sb N SEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N ' Ni N
eNi N W N
eW N
MAX
01! ,90RfSTAd: I
H-86-68
DEPARTURE(X) LATITUDE(Y) ELEYATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 65 68 80 20 68
PPM NON MAO PPM MAG VO 4042 3167 0 0
eAu: 141 eAg: .8 eAs: 1095 eCu: 663 eZn: 194 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: 35 Ag: .2 As: 271 Cu: 164 Zn: 48 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 170 Ag: 1.1 As: 1352 Cu: 200 Zn: 360 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 545 eA9: 3.5 eAs: 4332 eCu: 641 eZn: 1154 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
OIS BO7ES7AxE 1
H-86-68
BEPARTURE(X1 LATITUDE(YI ELEYATIUA(Z1 0 0 0
O1A
FROM TO TYPE SS BEDROCK 65 68 80 20 68
NP D! VASE
PPM NON MAO PPM MAG VG 3204 538 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu 9E EEEE Ag *** EEEE eA9 ### EEEE As ************* EEEE eAs * - EEEE Cu * EEEE eCu * EEEE Zn * LEE! eZn * EEEE Sb N EEEE eSb N EEEE Ba N LEE! eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01P °l!fSTRff I
H-86-70
ûPARTUREIX) LATITUDEIY) ELEVATIOAtZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 9 13 80 20 13
PPM NON MAG PPM MAO VG 3972 4361 0 0
eAu: 675 eAg: 1.6 eAs: 1533 eCu: 755 eZn: 302 eSb: 0 eBa: 0 eCr: 0 eCa: 0 eNi: 0 eNi: 0 eW: 0
Au: 170 Ag: .4 As: 386 Cu: 190 Zn: 76 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *#* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N 0000 eSb N 0000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIE SOnESTA.SE I
H-86-70
DEPARTUREIX) LATITUBE(Y) ELE'1ATIol((Z) 0 0 0
O1A
FROM TO TYPE SS BEDROCK 9 13 80 20 13
301 PYRITE De 01 YASB
PPM NON MAG PPM MAO VG 3652 3043 4.6 0
eAu: 986 eAg: 2.6 eAs: 1045 eCu: 643 eZn: 438 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 270 Ag: .7 As: 286 Cu: 176 Zn: 120 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ** EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * 2222 eZn * 2222 Sb N 2222 eSb N 2222 Ba N 2222 eBa N 2222 Cr N 2222 eCr N 2222 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
RUN 0/B INTERP
0/H AO!lESIAdE II
H-86-71
DEPARTUREIXI LATITUDEiY1 ELEYATIONiZ1 0 0 0
01
FROM TO TYPE SS BEDROCK 16 20 80 20 24
PPM NON MAG PPM MAG VG 4154 3308 0 0
eAu: 1869 eAg: 2.1 eAs: 964 eCu: 332 e2n: 183 eSb: 0 eBa: 0 eCr: O eCo: . O eNi: 0 eNi: 0
eW: O
Au: 450 Ag:: .5 As: 232 Cu: 80 2n: 44 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: O
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N 0000 eSb N O000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
eAu: 1169
eÂs. :- 2071
eCu: 399 eZn: 181 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Am: -375
` As: 664 ' Cu: .128 Zn: 58 Sb: O Ba: O .0 r : O
'- ";Co: 0 Mo: -0 Ni: 0, W: O
H-86-71
- IEPARTUIE(X) LATITUIEtYI ELEVATIOM Q) 0 0 0 .
02
FROM TO TYPE SS BEDROCK 20 24 80 20 24
PPM NON MAG PPM MAG VG 3119 2825 1.8 0
Old IODEST* U II
Surface-
EEEE MIN
EEEE NM * EEEE MAG * EEEE Au * EEEE eAu *
EEEE Ag * EEEE eAg * EEEE . As ****** EEEE eAs *
EEEE Cu * EEEE e~n ~* Ei~~ eiB fV EEEE eSb N
1111 Ba N 1111 eBa N 1111 Cr N 1111 eCr N
1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
DJd dOéESTAIE II
H-86-72
1X:f"ART1NlëtXJ LATITit1EtY1 ELEIIATIONtZ1 tl 0 0
01
FROM TO TYPE SS BEDROCK 50 55 70 10 80
OITYASI
PPM NON MAG PPM MAG VG 4000 3570 0 0
Au: 170 Ag: .3 As: 512 Cu: 112 Zn: 96 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg 9E EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 680 eAg: 1.2 eAs: 2048 eCu: 448 eZn: 384 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW; 0
MAX
02
Au: 175 Ag: .2 As: 36 Cu: 64 Zn: 52 Sb: 0 Ba: 0 Cr: O Co: 0, Mo: O Ni: 0 W: O
eAu: 237 eAg: .3 eAs: 49 eCu: 87 eZn: 70 eSb: 0 eBa:. O -eCr: 0 eCo: 0 eNi: O eNi: 0
eW: 0
f/S 10RESTAIf II
H-86-72
REPARTIIREIXf LATITU9EIYf ELFVATIOIIIL 0 0. 0
FROM TO TYPE SS BEDROCK 55 60 70 10 80
Or7VAS1
PPM NON MAG PPM MAG VG 1353 1469 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N OOOO eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIS /INSTALL II
H=86-72 EPARi11RFIX1 LATITU9ElT1 EIEVATI0NIZ1
0, 0 0
03
TO TYPE SS BEDROCK 65 . 80 . 10 80.
PPM NON MAG 3765
Au: 265 Ag: .1.3 As: 504 - Cu: 160 Zn.: 46 Sb: 0 Ba: O Cr: O Co: O Mo: 0 Ni: O W: 0 .
PPM MAG VG
2725 0 0
eAu: 998 eA9: 4.9 eAs: 1897 eCu: 602 eZn: 173 eSb: 0 eBa: 0 eCr: 0 eCo: .O eNi: O eNi: O eW: O
.›IF‘.
Surface EEEE. MIN EEEE " NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg iE**iE EEEE As iE*HHE* EEEE eAs ' * • EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE. eZn * EEEE Sb N 0000 'eSb N 0000 Ba N EEEE- eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N
.XXXX Mo N • eMo.N
Ni N eNi N
W N eW N
MAX
H-86-72
1EP8RTIIREtX1 LATITIiOE(YI ELEYATIOII(ZI 0 0 -0
04 •
FROM _TO TYPE SS BEDROCK 65 70 80 10 80
NI 90ëESTAtE II
PPM NON MAG PPM MAG VG 3903 2725 0 O
Au: Ag: As: Cu.: Zn: Sb: Ba: Cr: Co: Mo: Ni: W:
'Surface
, EEEE - MIN
EEEE NM * • EEEE 'MAG * 'EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu 9E 'EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
ePto N Ni N
eNi N W N
eW N
30 eAu: 117 .05 eAg: .2 52 eAs: 203 :i 04 . eCu: 406 32 eZn: 125 0 eSb: O O eBa: 0 0 eCr: 0 0 eCo: 0 0 eNi: 0 0 eNi: 0 O eW: O
MAX
Old IDRESThIE I1
FROM " TO i TYPE SS • BEDROCK 70 f 75 80 20 80
4 ~
-PPM. NON' MAG PPM .MAG VG - .3216 2098 0 . 0
Au: 70 eAu: 225 Ag: .3 eAg:
1
As:: 127. sAs: 408 Cu: 92 - ,:Cu: 296 Zn:.:56 :Zn: " 180 Sb:. 0 :Sb: 0 Ba: 0 eBa: 0 Cr: .O :Cr: 0 Co: O eCo: O Mo: 0 eNi: O Ni: •0 eNi: 0
W: -O eu: 0
Surface EEEE MIN 'EEEE NM * EEEE MA G iE EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As 9E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N.
eMo N Ni N
eNi N W N
eW N
MAX
Au: 155 Ag: .3 As: 167 Cu: .120 Zn: 48 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 608 eAg: 1.2 eAs: 655 eCu: 471 eZn: 188 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
O/d :90. (STAKE II
H-96-72
DEpARTURE)X) LATITUDE)Y) ELEYATIONfZ) 0 0 0
06
FROM TO TYPE SS BEDROCK 75 80 80 20 80
PPM NON MAG PPM MAG VG 3922 2745 0 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu iE' EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Pl PORESME 17
H-86-73
DEPARTDRE(Xl LATITUDE(YI ELEVATION(Zl 0 O O
01-2
FROM TO TYPE SS BEDROCK 10 20 80 10 90
PPM NON MAG PPM MAG VG 2429 2095 1 0
eAu: 340 eAg: .5 eAs: 1418 eCu: 272 eZn: 165 eSb: 0 eBa: 0 eCr: 0 eCo: J eNi: 0 eNi: 0 eW: 0
Au: 140 Ag: .2 As: 584 Cu: 112 Z n : 68 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN 1111 NM * 1111 MAG * 1111' Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **HF*HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N - W N eW N
MAX
Au: 100 A9: .05 As: 146 Cu: 64 Zn: 36 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
eAu: 318 eAg: .2 eAs: 465 eCu: 204 eZn: 115 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 80/1ESTAtE 11
H-86-73
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 O 0
03-4
FROM TO TYPE SS BEDROCK 20 30 80 20 90
PPM NON MAO PPM MAG VO 3184 2115 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * 0000 Au * 0000 eAu * 0000 Ag TE EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn ->F EEEE Sb N EEEE eSb N EEEE Ba N EEEE eEa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 2.5 Ag: .05 As: 57 Cu: 68 Zn: 54 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: 0
eAu: 21 eAg: .4 eAs: 484 eCu: 577 eZn: 458 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
012 AOAESTRRE 11
H-86-73 DEPARTUREfX) LATITUDElY1 ELEVATI08tZl
0 0 0
OS
FROM TO TYPE SS BEDROCK 30 32 80 10 90
PPM NON MAG PPM MAG' VG 8487 11949 C O
Surface EEEE MIN EEEE NM ** EEEE MAG **HE* EEEE Au * EEEE eAu * 0000 Ag * 0000 eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/3 llOAESTAdE II
H-86-73
DEPARTURE(X) LATITUDEIY) ELEYATION(Z) 0 0 '0
06-7
FROM TO TYPE SS BEDROCK 32 45 70 10 90
PPM NON MAG PPM MAG VG 5731 2699 0 0
Au: 40 Ag: .2 As: 68 Cu: 62 Zn: 40 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F 0000 eAg * 0000 As * 0000 eAs * 0000 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE' eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 229 eAg: 1.1 eAs: 390 eCu: 355 eZn: 229 eSb: 0 eBa: O eCr: 0 eCo: O eNi: 0 eNi: 0
eW: O
MAX
Old 1091S7A.Sf 11
H-86-74
OEPARTUREfX) LATITU6EIT) ELEVATIO)IIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 22 25 80 20 30
!Z PYR17f
PPM NON MAG PPM MAS VG 4000 1859 6.5 0
Au: 800 eAu: 3200 Ag: .05 eAg: 2 As: 71 eAs: 23~ Cu: 220 eCu: 880 Zn: 162 eZn: 648 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 CO: O eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 2222 Sb N 2222 eSb N 2222 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/3 ®OAE57ALE II
H-86-74
DEPARTUREtX) LATITUDEIYI ELEVATIOfItZ) 0 0 0
02
FROM TO TYPE SS BEDROCK 25 30 80 20 30
Sz PYRITE
PPM NON MAG PPM MAG VG 2058 4585 3.7 0
Au: 400 eAu: 823 Ag: .3 eAg: .6 As: 7 eAs: 14 Cu: 68 eCu: 140 Zn: 34 eZn: 70 Sb: 0 eSb: O Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 2222 Ba N 2222 eBa N 2222 Cr N 2222 eCr N 2222 Co N XXXX eCo N . XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 20 Ag: .05 As: 31 Cu: 44 Zn: 42 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: 0
W: 0
eAu: 375 eAg: .9 eAs: 582 eCu: 826 eZn: 788 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 NOAESIAIE II
H-86-74
DEPARTURE(X1 LATITUDE(T1 ELEUATIOfi(Z1 O O o
03
FROM TO TYPE SS BEDROCK 30 33 90 30 30
Jot PT PROCESSED BEDROCI
PPM NON MAO PPM MAG VG 18765 824 0 0
Surface EEEE MIN EEEE NM 4HHE** EEEE MAG f: EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9F EEEE eCu * EEEE Zn 9F EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N 0000 Co N 0000 eCo N XXXX Mo N
eMo N • Ni N eNi N
W N eW N
MAX
Old 5O!IS7AJE II
H-86-75
DEPARTUREIX! LATITUDFIY? ELEUBTIONiZ? 0 0 O
01-2
FROM TO TYPE SS BEDROCK 43 50 70 10 83
PPM NON MAO PPM MAO VG 2925 2667 0 0
eAu: 190 eAg: .6 eAs: 246 eCu: 281 eZn: 105 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 65 Ag: .2 As: 84 Cu: 96 Zn: 36 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * 0000 Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 115 Ag: .05 As: 28 Cu: 68 Zn: 24 Sb: O Ba: O Cr: O Co: O Mo: 0 Ni: 0
W: 0
eAu: 383 eAg: .2 eAs: 93 eCu: 226 eZn: 80 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Old RORESTAUE II
H-86-75
DEPARTURE(8) LATITUDE(Y) ELEVATIOM(Z) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 50 60 80 10 83
ZS PYRITE
PPM NON MAG PPM MAG VG 3328 1829 3.3 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As 9E EEEE eAs * EEEE Cu * EEEE eCu * 4444 Zn * 4444 eZn * 4444 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Oh! ROAES7AdE II
H-86-75
SEPARTURE(Xl LATITUDE(Y) LEilATiG?i(Zl 0 0 C
05
FROM TO TYPE SS BEDROCK 60 65 80 10 S3
2S PYRITE
PPM NON MAG PPM MAG VG GALENA 3475 2077 5.2 1
Au: 185 eAu: 643 Ag: .1 eAg: .3 As: 36 eAs: 125 Cu: 162 eCu: 563 Zn: 29 eZn: 101 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * 3333 Sb N 3333 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Old OOMESTAII II
H-86-75
DEPARTURE(X) LATITUDEfY) ELEVAIIC1!(Z) 0 O O
06
FROM TO TYPE SS BEDROCK 65 70 80 10 83
PPM NON MAG PPM MAG VG 4000 2754 1.7 0
Au: 15 eAu: 60 Ag: .05 eAg: .2 As: 46 eAs: 184 Cu: 92 eCu: 368 Zn: 28 eZn: 112 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: O Mo: 0 eNi: 0 Ni: 0 eN:: 0
W: 0 eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/8 !O1lESIARE II
H-86-75
èEPARTURE(X1 LATITUDE(Y1 ELEVATION(Z1 -0 o 0
07
FROM TO TYPE SS BEDROCK 70 74 80 10 83
SS PYRITE
PPM NON MAO PPM MAO VO 3075 1742 3.4 0
eAu: 92 eAg: 1.2 eAs: 1673 eCu: 769 eZn: 123 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 30 Ag: .4 As: 544 Cu: 250 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 2222 Ba N 2222 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
011l lfoAESTAKE 1I
H-86-75
DEPARTUREtXI LATITUDEIY) ELEUATIOItt.) 0 0 0
08
FROM TO TYPE SS BEDROCK 74 80 80 20 83
PPM NON MAG PPM MAG VG 5857 4524 0 0
Au: 10 eAu: 59 Ag: .05 eAg: As: 65 eAs: 381 Cu: 130 eCu: 761 Zn: 36 eZn: 211 Sb: O eSb: 0 ' Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O el+ii : 0 Ni: O eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX- eCo N XXXX Mo N
ego N Ni N
eNi N W N
eW N
MAX
D/d 908E37AutE 11
H-86-75
IEPARTUREIXI LATIiU8EfY1 ELEVATIONIZI 0 0 0
09
FROM TO TYPE SS BEDROCK 80 83 80 20 83
PPM NON MAG PPM MAG VG 4768 2101 1.6 0
eAu:AIMM. eAg: .5 eAs: 691 eCu: 172 eZn: 133 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 155 Ag: .1 As: 145 Cu: 36 Zn: 28 Sb: 0 Ba: 0 Cr: O Co: O Mo: O Ni: O W: 0
Surface
EEEE MIN
EEEE NM 9P EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N
_ EEEE Cr N 1111 eCr N
1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
NI BORESTIPIE 11
H-86-76
DEPARTURE(X) LATITBDE(T) ELEVATIOM(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 65 70 80 10 110
PPM NON MAG PPM MAG VG 2860 2551 0 0
eAu: 229 eAg: ! eAs: 541 eCu: 355 eZn: 189 eSb: 0 eBa: O eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 80 Ag: As: 411/1119 Cu: 124 Zn: Sb: Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 165 Ag: .05 As: 996 Cu: 120 Zn: 40 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
eAu: 390 eAg: .1 eAs: 2116 eCu: ~GJ eZn: 94 eSb: 0 eBa: C Cr:a 0
eCo: 0 :
eAii: C? eW: 0
018 BOdESTARE II
H-86-76
DEPARTURE(X1 LATITLDE(Y) ELE{iATIOM(Z) 0 0 0
04-5
FROM TO TYPE SS BEDROCK 74 85 80 10 110
R PYRITE
PPM NON MAG PPM MAS VG 2361 1425 3.3 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu -)E EEEE Zn * 4444 e'rn * 4444 Sb N 4444 eSb N E_EE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XX;'.`f eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
~» 9e+Fs=at: I!
H-86-76
DEPARTUREIXI LATITUDEIYI ELEVATIORIZI 0 Q 0
06-7
FROM TO TYPE 8S BEDROCK 85 90 80 10 110
PPM NON MAO PPM MAO VO 4836 18898 0 0
eAu: 266 eAg: .5 eAs: 1480 eCu: 435 eZn: 193 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 55 Ag: .1 As: 306 Cu: 90 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAO ******** EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE EEEE Sb N 0000 eSb N 0000 Ba N EEEE ena N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 145 Ag: .4 As: 168 Cu: 84 Zn: 38 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 395 eAg: 1.1 eAs: 457 eCu: 229 eZn: 103 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/d 90AES7AIE II
H-86-76
DEPARTURE(%1 LATITUDECY) ELEVATIOJI(ZI O O 0
08
FROM TO TYPE SS BEDROCK 90 95 80 10 110
PPM NON MAG PPM MAG VG 2722 1926 3 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 2222 Ba N 2222 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 195 Ag: .2 As: 234 Cu: 64 Zn: 30 Sb: 0 Ba: . 0 Cr: 0 Co: O Mo: 0 Ni: O W: 0
eAu: 591 eAg: .6 eAs: 709 eCu: 194 eZn: 91 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 NOAES1A,fE II
H-86-76
DEPARTUREIXI LATITUDE(Y) ELEVATIONIZI O O 0
09
FROM TO TYPE SS BEDROCK 95 102 60 10 110
IS PYRITE
PPM NON MAG PPM MAG VG 3032 1881 7.3 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 5555 eBa N 5555 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
O/ d 901!fSTAIf II
H-86-76
/EPARTURE(X1 LATITUDE(T1 ELEVATION(Z1 0 0 0
10
FROM TO TYPE SS BEDROCK 102 104 80 20 110
J>i PT1175
PPM NON MAG PPM MAG VG MARCAS 5897 3887 19.5 100
eAu: 3037 eAg: .3 eAs: 3019 eCu: 566 eZn: 248 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 515 Ag: .05 As: 512 Cu: 96 Zn: 42 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu °1E EEEE Ag * EEEE eAg * EEEE As ***9E* EEEE eAs 9E EEEE Cu * EEEE eCu 9P EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N ++++ Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
013 3^PfSTRSf 11
H-86-76
DEPARTUREIXI LATITULEIYI ELEYATIONIZI O O 0
11
FROM TO TYPE S3 BEDROCK 104 110 80 20 110
PPM NON MAG PPM MAG VG 6250 "5333 0 O.
Au: 55 Ag: .05 As: 254 Cu: 92 Zn: 30 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au "* EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As *HE EEEE eAs * EEEE Cu * EEEE eCu * .EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 344 eAg: .3 eAs: 1587 eCu: 575 eZn: 187 eSb: 0 eBa: 0 eCr: O eCo: O eNi: 0 eNi: 0 eW: 0
MAX
Au: 170 Ag: .05 As: 54 Cu: 60 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
eAu: 693 eAg: .2 eAs: 220 eCu: 245 eZn: 179 eSb: O eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
OC 90MfSTAlf II
H-86-77
DEPARTURE(X) LATITUDE(Yl ELSUATIOM(Zl 0 0 0
01
FROM TO TYPE SS BEDROCK 39 45 60 10 59
PPM NON MAG PPM MAG VG 4077 2205 2.1 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9F EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 1 1 1 1 eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O/D MUTAI: 11
H-86-77
. HEPARTUREfXI LATITUOE(9l ELEt'ATION(Z) 0 0 0
02
FROM TO TYPE SS BEDROCK 45 49 80 IC 59
PPM NON MAG PPM MAG VO 2012 1406 1.9 0
Au: 75 Ag: .2 As: 185 Cu: 84 Zn: 76 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: O W: 0
eAu: 151 eAg: .•4 eAs: ti72 eCu: 169 eZn: 153 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zr. T4- EEEE eZr, 9E EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY, eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 50 Ag:.~ ' As: 240 Cu: 44 Zn: 40 Sb: C Ba: 0 Cr: 0 Co: O Mo: C Ni: 0 W: 0
eAu: 126 eAg: .4 eAs: 891 eCu: 163 eZn: 143 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 9i'RESTddE II
H-86-77 DEPARTURE(X) LATITUEE(Y) ELE4ATIO!!(Z)
O O 0
03 FROM TO TYPE SS EEDRCCn 49 55 SO 20 55
PPM NON MAG PPM MAO VG 3711 1975. 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE A= *# EEEE eAs * EEEE Cu * EEEE eCu * EEEE 7n * EEEE eZn * EEE_ Sb M ESSE eSb N C7^0 Ba N 0000 eBa. N 0000 Cr N EEEE eCr• N EEEE Cm N XXXX eCo N Y,`!Y" Mo N
eMo N Ni N eNi N
w r eW N
MAX
nrs enrrS7,prr jr
H-86-77
➢EPARTL•REIXi LATITItOEIYI ELEVATIONI2l O 0 0
04-5
FROM TO TYPE SS BEDROCK 55 59 80 20 59
PPM NON MAG PPM MAG VG 4776 2618 1.9 0
Au: 255 A7: .6 As: 101 Cu: 16 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mc: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *HE EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 1213 eA9: 2.9 eAs: ~12 eCu: 76 eZ:,: 115 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 310 Ag: .3 As: 264 Cu: 98 Zn: 76 Sb: 0 Ba• 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 967 2Ag: eAs: 8^3 eCu: 306 aZn: 237 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: C eW: 0
O/B AORfS7A.fE II
H-86-78
DEPARTUREIX) LATITUDEIYI ELEVATIO8IZI 0 0 0
01
FROM TO TYPE SS 3EDROCK 40 46 60 10 97
PPM NON MAG- PPM MAO VG 3119 2429 1.9 C
Sui-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -)E EEEE AS * EEEE eAg * 1111 A s ** 1111 eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo .N XXXX Mo P1
eMo N Ni N eNi N W N
eW N
MAX
Au: 65 Ag: .4 As: 160 Cu: 66 Zn: 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
eAu: 113 eAg: .7 eAs: 279 eCu: 115 eZn: 98 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: C eW: C
0/II BOAESTR(F :I
H-86-78
DEPARTUREfXI LATITUDElY1 ELEiIATIOM(Z1 0 0 0
02-3
FROM TO TYPE SS BEDROCK 46 55 80 10 97
PPM NON MAG PPM MAG VG 1744 1755 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9F EEEE Ag * EEEE eAg * EEEE As * 0000 eAs * 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 35 Ag: .05 As: 86 Cu: 28 Zn: 36 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: 0 W: 0
eAu: 158 eAg: .2 eAs: 388 eCu: 136 eZn: 162 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: C
O!! N^!lfS7ARE 11
H-86-78
DPARTUREIX) LATITUDE(Y) ELEVATIONIZ) 0 0 0
04
FROM TO TYPE SS BEDROCK 55 65 60 10 97
PPM NON. MAG PPM MAG VG 4511 3376 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCF• N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
e W N
MAX
?/B 9CI:57ASf II
H-86-78
DEPINITUREIX1 LATITUDEIYI ELEVATIOtiIZ1 0 0 0
05
FROM TO TYPE SS BEDROCK 65 75 60 10 97
PPM NON MAG PPM MAG VG 2105 1310 0 0
Au: 30 eAu: 4.3 Ag: .05 eAg: .1 As: 20 eAs: 42 Cu: 9 eCu: 19 Zn: 36 e2n: 76 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: C Ni: 0 eNi: 0 W: 0 eW: 0
Surface' EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs 1E EEEE Cu * EEEE eCu * EEEE Zn * O000 eZn :f 0000 Sb N 0000 EGi N EEEE T'a N EEEE eBa N EEEE Cr N ESSE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/B P.04EB741E II
H-86-78
DEPARTUREIX) LATITUDE(T1 ELEVATI08IZ) 0 0 0
06
FROM TO TYPE SS BEDROCK 75 85 60 10 97
PPM NON MAG PPM MAG VG 1359 667 0 0
Au: 10 eAu: 14 Ag: .05 eAg: .1 As: 33 eAs: 45 Cu: 14 eCu: 19 Zn: 40 eZn: 54 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: O Co: 0 eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -)E EEEE Ag * EEEE eAg * EEEE As * EEEE eAs
.#
EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 3820 A9: .1 As: 64 Cu: 52 Zn: 59 Sb: 0 Ba: O Cr: O Co: O Mo: O Ni: 0
W: 0
eAu: 9243 eAg: .2 eAs: 155 eCu: 126 eZn: 143 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: O
O18 BORES7pIE II
H-86-78
BEPARTUREIXI LATITUIE(Y1 ELEVATIOUIZ) 0 0 0
•
07
FROM TO TYPE SS BEDROCK 85 91 80 20 97
PPM NON MAG PPM MAG VG 2420 3556 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au ** EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu *
n
EEEE eSb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX- Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 34286 Ag: 1.7 As: 712 Cu: 144 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: O Ni: 0 W: 0
eAu: 40336 eAg: 2 eAs: 838 eCu: 169 eZn: 52 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
018 801lfSIAdf II
H-86-78
DEPARTURE(X) LATITUDE(T1 ELEVATION(Z) 0 0 0
08
FROM TO TYPE SS BEDROCK 91 97 80 20 97
AO CDI fX1! 78000
PPM NON MAG PPM MAG VG 1176 2098 1.6 0
Surface EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au ******************* EEEE eAu **** EEEE A9 **** EEEE eAg * EEEE As *?HP**** EEEE eAs * EEEE Cu * ESSE eCu * EEEE Zn. * EEEE eZn * EEEE Sb N FEES eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
d 1F 941!ES711.(E II
H-86-79
DEPARTURE(X) LATITUDEIT) ELEVATIDNIZ) 0 0 0
01
FROM ' TO TYPE SS BEDROCK 44 55 70 10 75
PPM NON MAO PPM MAO VO 2918 1932 0 0
Au: 580 eAu: 1692 Ag: .. 1 eAg: .3 As: 90 eAs: 263 Cu: 120 eCu: 350 Zn: 68 eZn: 198 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi,: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu -)P 0000 eCu *
ffle) erZn 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi IJ W N eW N
MAX
'd R011FS7AIf Ii
H-86-79
DEPARTUREIXf LATITUDEITI ELEVATIONI21 0 0 0
FROM TO T9IgE SS BEDROCK 55 65
PPM NON MAG PPM 2567
70 10
MAO VG 2726 0
75
C
Au: 235 eAu: 603 Ag: .2 eAg: .5 As: 146 eAs: 375 Cu: 192 eCu: 493 Zn: 76 eZn: 195 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 QCo: O Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
SuagEe MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn *
7 888$ e ~6 ~ 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
011 10M.ESIA1E II
H-86-79
DfPARTUR_IX) LATITifDGST} `LFUATIOf1(Z) 0 0 0 -
03
FROM TO TYPE SS BEDROCK 65 69 80 20 75
PPM NON MAO PPM MAO VO 3910 3548 0 0
eAu: 1603 eAg: .8 eAs: 3472 eCu: 485 eZn: 172 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
Au: 410 Ag: .2 As: 888 Cu: 124 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0• Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 35 Ag: .2 As: 1072 Cu: 132 Zn: 53 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0
0 W: 0
eAu: 142 eAg: .8 eAs: 4342 eCu: 535 eZn: 215 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
OIB AOXfS7Alf II
H-86-79
DEPARTURE(X) LATITUDE(Y) ELE4ATI0))(Z) O Q 0
04-5
FROM TO TYPE SS BEDROCK 69 75 80 20 75
PPM NON MAG PPM MAG VG 4051 4293 .8 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ********** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eEa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 200 Ag: .05 As: 84 Cu: 88 Zn: 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
eAu: 767 eAg: .2 eAs: 322 eCu: 337 eZn: 215 eSb: 0 eBa: C eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE EOAES7ALf 11
H-86-80
DEPAP.TUREIXI LATITUDE(Yl ELEVATIOiitZl 0 0 0
01
FROM TG TYPE SS BEDROCK 30 40 70 10 81
PPM NON MAG PPM MAG VG 3833 2979 1.7 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * 1111 eAg -1E 1111 As TF 1111 eAs * EEEE Cu * EEEE eCu * EEEE Zr, * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 170 Ag: .2 As: 226 Cu: 48 Zn: 28 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 580 eAg: .7 eAs: 771 eCu: 164 eZn: 95 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIS ROIDES?ARE II
H-86-80
DEPARTUREIX1 LATITUDEIYI ELEVATIUDDIZ1 0 0 0
02
FROM TO TYPE SS BEDROCK 40 43 70 10 81
PPM NON MAG PPM MAG VG 3410 2885 1.7 0
Surface EEEE MIN EEEE .NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** 1111 eAs * 1111 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Ca N XXXX eCo N XXXX Mc N
eMo N Ni N
eNi N W N
e,W N
MAX
Au: 15 Ag: .05 As: 186 Cu: 20 Zn: 42 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
eAu: 48 eAg: .2 eAs: 59â eCu: 64 eZn: 135 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
DI!? NONESTRdF 7:
H-86-80
DEPARTUREIXI LATITUDEIYI ELEIIATIORIZI 0 0 0
03
FROM TO TYPE SS BEDROCK 43 48 60 10 81
PPM NON MAG PPM MAG VG 3214 2000 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs ?E 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIE el!lfST@SË II
H-86-80
DEPARTURE(X) LATITUDE(Y) ELEVATIOU Q1 0 O O
04
FROM TO TYPE SS BEDROCK 48 53 80 10 81
PPM NON MAG PPM MAG VG 3167 2021 0 0
eAu: 1298 eA9: .2 eAs: 143 eCu: 152 eZn: 152 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 410 Ag: .05 As: 45 Cu: 48 Zn: 48 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: -0 Ni: 0 W: O
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu 9E EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N ESEE Co N XXXX eCo N XXXY. Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 55 Ag: .05 As: 143 Cu: 64 Zn: 43 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mc: O Ni: 0 W: 0
eAu: 193 eAg: .2 eAs: 502 eCu: 225 eZn: 151 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Dlè !lDRfSTA.tf II
H-86-80
DEPARTURE)X) LATITUDE)Y; ELEIIATIOII(Z) 0 O D
05
FROM TO TYPE SS BEDROCK 53 57 80 10 81
PPM NON MAG PPM MAG VG 3511 3022 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu °)E EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
a/a eaBfsTARI II
H-86-80
JEPARTURE(X) LATITUDEIYI ELE9ATIOHIZI 0 0 ~
06-7
FROM TO TYPE SS BEDROCK 57 62 80 10 81
. 1% PMI!
PPM NON MAG PPM MAG VG 5158 5251 8.3 0
Au: 250 eAu: 1289 Ag: .6 . eAg: 3.1 As: 26 eAs: 134 Cu: 50 eCu: 25Z Zn: 30 eZn: 155 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: O Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * ++++ Sb N ++++ eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
^Id :IO!IESTARE 11
H-86-80
DEPARTOREtX; LATITL'tE'{Y? ELEitATIiiIliZl 0 0 0
OBA
FROM TO TYPE SS BEDROCK 62 66 80 10 81
PPM NON MAG PPM MAG VG 4306 2601 0 0
Au: 100 eAu: 431. Ag: .05 eAg: .2 As: 61 eAs: 263 Cu: 420 eCu: 1809 Zn: 38 eZn: 164 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: O Mo: C eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM ;E EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu ## EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb ^? 0000 Ea N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
OC BOlES?A,fF ri
H-86-80
DEPARTURE(X) LATITUDE(T) ELEYATIOM(Z) 0 0 0
09
FROM TO TYPE SS BEDROCK 66 71 80 10 81
PPM NON MAG PPM MAG VG 4739 3549 1.6 0
eAu: 450 eAg: .5 eAs: 95 eCu: 284 eZn: 152 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 95 Ag: .1 As: 20 Cu: 60 Z n : 32 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0 Ni: 0 W: 0
Sur-face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 2000 Ag: .05 As: 43 Cu: 60 Zn: 28 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
eAu: 6698 eAg: .2 eAs: 144 eCu: 201 eZn: 94 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/8 ROBESTAtE II
H-86-80
AEPARTURE(Xl LATITU9E(YI ELEVATIOM(Zl O O O
1011
FROM TO TYPE SS BEDROCK 71 76 80 20 81
IS PYRITE
PPM NON MAG PPM MAG VG 3349 3318 5 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 6666 eBa N 6666 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW 1`.'
MAX
Au: 50 Ag: .05 As: 13 Cu: 104 Zn: 80 Sb: O Ba: 0 Cr: O Co: O Mo:. O Ni: 0 W: O
eAu: 213 eAg: .2 eAs: 55 eCu: 442 eZn: 340 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
013 30dfSTAIF 11
H-86-80
DEPARTUREIX! LATITUDEIrI ELEYATIOIIIZ! 0 0 0
12
FROM TO TYPE SS BEDROCK 76 78 80 20 81
PPM NON MAG PPM MAG VG 4252 3774 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE. eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Ols 1O107AlE II
H-86-80
DEPARTURE(XI LATITUDEIYI ELEVATIONIZI 0 0 0
13
FROM TO TYPE SS BEDROCK 78 81 80 20 81
PPM NON MAG PPM MAG VG 4644 4713 1.8 0
Au: 700 Ag: .05 As: 70 Cu: 90 Zn: 60 Sb: 0 Ba: 0 Cr: O Co: O Ma: O Ni: O W: O
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu '1E EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
eAu: 3251 eAg: .2 eAs: 325 eCu: 418 eZn: 279 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
MAX
Au: 185 Ag: .05 As: 109 Cu: 98 Zn: 60 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 405 eAg: .1 eAs: 238 eCu: 214 eZn: 131 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 30RfS1A:tf II
H-86-81
DEPARTUREIX) LATITUDEIY) ELEVATIOSIZ) 0 0 0
01-2
FROM TO TYPE SS BEL CC): 34 45 80 10 118
PPM NON MAO PPM MAS
VG 2188 2042 .ô. 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au 9E 1111 eAu * 1111 Ag * 1111 eQ3 * EEEE As * EEEE eAs ?E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EcEE Sb N EEEE eSb N EEEE Ba N EEEE eBa. N EEEE Cr N EEEE sLr N EEEE Cc N XXXX eCo N ,,.... ~\~,:\~~ Mo N
eMo N Mi N eNi N W N eW N
MAX
^I! BOOES7AdE II
H-86-81
DEPARTURE(X) LATITUDE(Y) ELEliATION(Z) 0 0 0
03
FROM TO TYPE SS BEDROCK 45 50 80 10 118
PPM NON MAG PPM MAG VG 4083 1972 2.2 0
Au: 235 eAu: 960 Ag: .05 eAg: .2 As: 129 eAs: 527 Cu: 80 eCu: 327 Zn: 38 eî.r: 155 Sb: 0 eSb: C Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: G W: 0 eW: 0
Surface ELLE MIN
:1.AX
EEEE NM 1E EEEE MAC * ELLE Au * EEEE eAu _)E ELLE Ag * 1111 e.43 * 1111 As * EEEE eAs * EEEE Cu * EEce eCu * -LEE! Zn * EEEE eZn * ESSE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
Au: 8100 Ag: .2 As: 290 Cu: 230 Zn: 52 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 4025 eAg: .4 eAs: 144 eCu: 114 eZn: 26 eSb: 0 eBa: 0 eCr: 0 eCo: C eNi: 0 eNi: 0 eW: 0
01B 110!l1ST4f.E 11
H-86-81
DEPARTURE(X) LATITUDE(Y) ELE9ATIUX:2) o o o
04-5
FROM TO TYPE
âEDRO C:< 50 60 80 10 iiâ
~S PYB1T1
PPM NON MAO PPM MAG VO 497 1030 3.9 0
Surface EEEE MIN EEEE NM * EEEE - MAO * EEEE Au **** EEEE eAu * EEEE Ag ?E* EEEE eAg * 4444 A s ** 4444 eAs -)E 4444 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE S5 N EEEE eSb N EEEE ia a N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
rrr gOxçera{r rr
H-86-81
CEPARTUREtXI LATITL+1'EiY1 ELE'rAT10:It21 0 0 0
08-9
FROM TO TYPE SS _ZDROC? 71 81 80 30 118
PPM NON MAG PPM MAO VG 3058 2045 0
Au: 50 Ag: .05 As: 376 Cu: 170 Zn: 68 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni 0
W: 0
Sur-face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9(- EEEE eAg * EEEE As *?F# EEEE eAs ?4 EEEE Cu * EEEE eCu * 1 1 1 1 Zn * 1111 eZn * EEEZ Sb 1°! EEEE eSb N EEEE Be. N EEEE aB a N EEEE Cr N EEEE eCr N EEEE Co N X?:XX eCo N XX:<Y Mo N !
eMo f! Ni N
eNi N W N
eW N
eAu: 153 eAg: .2 eAs: 1027 eCu: v ^ v'
eZr7: , e8b. eEa: C eCr: 0 eCo: 0 eNi: O eNi: O
eW: O
MAX
D!B SONESTAdE Il
H-86-81
DEPARTURE(XI LATITUDE(Y) ELEVATION(ZI 0 O O
1011
FROM TO TYPE SS BEDROCK 81 90 SO 10 118
10% PYRITE
PPM NON MAG PPM MAG VG 3918 2513 5.7 0
eAu: 1097 eAg: 2.7 eAs: 1254 eCu: 940 eZn: 266 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 280 Ag: .7 As: 320 Cu: 240 Zn: 68 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9F EEEE eAg *# EEEE As *3E* EEEE eAs a; EEEE Cu 'r. EEEE eCu * EEEE 7n ?F 7777 eZn * 7777 Sb N 7777 eSb N EEEE Pa N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
^rs goIesraxE tr
H-86-81
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
1213
FROM TO TYPE SS BEDROCK 90 92 SO 10 118
PPM NON MAG PPM MAG VG 2562 3296 0 0
Au: 25
eAu: 64 Ag: .2
eAg: .5 As: 195
eAs: 500 Cu: 192
eCu: 4çc Zn: 74 eZn: 190
Sb: 0 eSb: 0
Ba: 0
eBa: 0 Cr: 0 eCr: 0
Co: 0
eCo: 0 Mo: 0 eNi: 0
Ni: 0
eNi: 0 W: O
eu: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIS POAESTAtE 11
H-86-81
DEPARTUREIXI LATITiIDEIYJ ELEYATIONIZI 0 0 O
1415
FROM TO TYPE SS BEDROCK 92 100 80 10 118
25% PY 1000 OC FOSS CA7h
PPM NON MAG PPM MAG VG ASPY 8608 4853 3.4 5
Au: 560 Ag: .2 As: 103 Cu: 152 Zn: 52 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM ** EEEE .MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 4444 eSb N 4444 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 4820 eAg: 1.7 eAs: 887 eCu: 1308 eZn: 448 eSb: 0 -eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 25 Ag: .2 As: 144 Cu: 132 Zn: 58 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 133 eAg: 1.1 eAs: 768 eCu: 704 eZn: 309 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Old lpO1.'ESTAKf II
H-86-81
DEPARTOREtXI. LATITtfOEtYI ELEVATiOXII: 0 0 0
16
FROM TO TYPE SS BEDROCK 100 105 SO 10 118
PPM NON MAG PPM MAO VG 5333 3838 0 0
• Surface
EEEE MIN EEEE NM * EEEE HAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N OOCC Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Ma N
eMo N Ni N
eNi N W N
eW N
MAX
O!! YOREST KI I1
H-86-81
DEPARTURE(X) LATITUDE(Y) ELEYATIOp(Z) 0 0 0
17
FROM TO TYPE SS BEDROCK 105 110 60 10 118
PPM NON MAG PPM MAG VG 4831 2995 1.5 0
Au: 545 Ag: .3 As: 73 Cu: 84 Zn: 34 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG 9P EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs 9E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 2633 eAg: 1.4 eAs: 353 eCu: 406 eZn: 164 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
9/8 899£S7Adf II
H-86-81
DEPARTURE(X) LATITUDEIT) ELEVATIMtZ) 0 0 0
18
FROM TO TYPE SS BEDROCK 110 115 80 20 118
PPM NON MAG PPM MAG VG 3519 1889 0 0
Au: 390 eAu: 1372 Ag: .05 eAg: .2 As: 79 eAs: 278 Cu: 96 eCu: 338 Zn: 84 eZn: 296 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 w: o ew: o
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As 9E EEEE eAs * EEEE Cu 9F EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
e W N
MAX
018 BOHESTARE II
H-86-81 DEPARTURE(X) LATITUDE(Y) ELE4ATIW((Z1
0 0 0
19
FROM TO TYPE SS BEDROCK 115 118 80 20 118
PPM NON MAG PPM MAG VG 7111 2822 0 0
Au: 40 Ag: .9 As: 131 Cu: 220 Zn: 320 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mc: 0 Ni: O
W: 0
Surf ace EEEE MIN EEEE NM #* EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag *# EEEE eAg **?HF* EEEE As * EEEE eAs * EEEE EEEE eCu * EEEE Zn * EEEE eZn ** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N- W N
eW N
eAu: 234 eAg: 6.4 eAs: 932 eCu: 1564 eZn: 2276 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
e44: 0
MAX
Au: 200 Ag: .05 As: 98 Cu: 96 Zn: 68 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: -0 Ni: 0
W: O
eAu: 921 eA9: .2 eAs: 451 eCu: 442 eZn: 313 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/3 NONESTARE II
H-86-82
DEPARTUREIX) LATITUDEIY) ELEVATIOMIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 34 43 60 10 97
PPM NON MAG PPM MAG VG 4606 2133 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * 0000 eAg * 0000 As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi hl W N
eW N
MAX
0111 !O f$7A1: 11
H-86-62
. DEPARTUREfX) LATITUDEtTI ELE1iATIulI{2l 0 0 0
02
FROM TO TYPE SS BEDROCY. 43 55 80 10 97
PPM NON MAG PPM MAG VG 5711 2556 0 0
Au: 10 eAu: 57 Ag: .05 eAg: .3 As: 128 eAs: 731 Cu: 88 eCu: 503 Zn: 30 eZn: 171 Sb: O eSb: 0 Ba: 0 eBa: O Cr: 0 eCr: 0 Co: O eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag -* EEEE eAg * 0000 As 9E 0000 eAs * 0000 Cu * 0000 eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo. N Ni N
eNi N W N
eW N
MAX
Au: 100 Ag: .05 As: 101 Cu: 90 Zn: 68 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: O Ni: 0 W: 0
eAu: 382 eAg: .2 eAs: =86 eCu: 344 eZn: 260 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
DIE N!l1STAIÊ II
H-86-82
DEPARTURE(X) LATITUDE(Y) ELEVATION Q) 0 0 0
03
FROM TO TYPE SS BEDROCK 55 65 80 10 97
PPM NON MAG PPM MAG VG 3818 2222 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * O000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE' eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 50 Ag: .05 As: 40 Cu: 132 Zn: 68 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: o
eAu: 296 eAg: .3 eAs: 236 eCu: 780 eZn: 402 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 ?01lf57Adf II
H-86-82
6EPARTUREiX! LATITUI:ElY1 ELEUATIEJEQi 0 0 0
04-5
FROM TO TYPE SS BEDROCK 65 82 80 10 97
?0S PYRITE
PPM NON MAG PPM MAG VG GALENA 5912 4918 2 1
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 2222 eZn * 2222 Sb N 2222 eSb N 2222 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
e N i N- W N
eW N
MAX
01! AOAESIAdE 11
H-86-82 9EPARTURE(X1 LATITU9E(Y) ELEt(ATI011IZ)
0 0 0
06
FROM TO TYPE SS BEDROCK 82 86 80 10 97
PPM NON MAG PPM MAG VG 4240 2361 0 0
Au: 70 eAu: 297 Ag: .05 eAg: .2 As: 16 eAs: 68 Cu: 170 eCu: 721 Zn: 96 eZn: 407 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01H 901l: S7AdF I:
H-86-82
IN:PARTUREIXI I.ATITUpEIYI ELEYAT10NIZ) 0 0 0
07
FROM TO TYPE SS BEDROCK 86 93 80 20 97
PPM NON MAG PPM MAG VG 4287 2851 1.6 0
Au: 140 eAu: 600 Ag: .05 eAg: .2 As: 188 eAs: 806 Cu: 62 eCu: 266 Zn: 60• eZn: 257 Sb: 0. eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: O W: 0 eW: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O/B ROIIESTAIE II
H-86-82
DEPARTUREi%) LATITUDEIT? ELEVATIONIZ) 0 0 0
08
FROM TO TYPE SS BEDROCK 93 97 80 20 97
PPM NON MAG PPM MAO VG 4451 2255 O 0
Au: 30 eAu: 134 Ag: .2 eAg: .9 As: 296. eAs: 1317 Cu: 320 eCu: 1424 Zn: 144 eZn: 641 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Ma N
eMD N Ni N
eNi N W N
aW hi
MAX
O1d MOINE II
H-86-84
DEPARTURE(X) LATITUDE(Y1 ELEVATION(Zl 0 O O
01
FROM TO TYPE SS BEDROCK 23 35 70 10 72
PPM NON MAG PPM MAO VG 3644 2333 0 0
Au: 130 Ag: .05 As: 338 Cu: 80 Zn: 38 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * 0000 Ag * 0000 eAg * 0000 As *** 0000 eAs * EEEE Cu * EEEE eCu * EEEE Zn 9F EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 474 eAg: .2 eAs: 1232 eCu: 292 eZn: 138 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: O eW: 0
MAX
OJE IPOIIESIA,fE II
H-86-84
DEPARTUREIXI LATITUDEITI ELEVATION(Z) 0 0 0
02
FROM TO TYPE SS BEDROCK 35 40 80 10 72
PPM NON MAG PPM MAG VG 65333 42667 35.6 0
Au: 95 eAu: 6207 Ag: .2 eAg: 13.1 As: 85 eAs: 5553 Cu: 88 eCu: 5749 Zn: 40 eZn: 2613 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN MAX EEEE NM jE**-1E*lHHE*IE*HE9E#**iE* EEEE MAG *HE*fE EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *******HHF9E** EEEE As 9F 1111 eAs *HE 1111 Cu * 1111 e C u *HP*lE**HE EEEE Zn * EEEE eZn *** EEEE Sb "N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
0/I 1011107111 11
H-86-84
lEPARTUREIXJ LATITUBEIYI ELEYATIOMIZI 0 0 0
03
FROM TO TYPE SS BEDROCK 40 45 80 10 72
PPM NON MAG PPM MAG VG 3628 2273 1.7 0
Au: 45
eAu: 163 Ag: .05 *Ag: .2
As: 5
eAs: 18 Cu: 56
eCu: 203 Zn: 24
eZn: 87 Sb: O
eSb: 0 Ba: 0
eBa: 0 Cr: 0
eCr: 0 Co: O
eCo: 0 Mo: 0
eNi: 0 Ni: O
eNi: 0 W: O
eW: 0
Sur4ace EEEE MIN EEEE NM 9P EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE' eAg * EEEE As * EEEE eAs * EEEE Cu * 1111 eCu * 1111 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 120 Ag: .1 As: 4 Cu: 84 Zn: 24 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O
W: 0
eAu: 766 eAg: .6 eAs: 26 eCu: 536 eZn: 153 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Olé BOAESTAIE II
H-86-84
DEPARTUREtXt LATITUDEST) ELEVATIOM(Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 45 50 80 10 72
PPM NON MAG PPM MAG VG 6381 2357 1.9 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 1111 Zn * 1111 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 25 Ag: .05 As: 129 Cu: 104 Zn: 42 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O
W: O
eAu: 100 eAg: .2 eAs: 519 eCu: 418 eZn: 169 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O
eW: 0
9/1 BOBESTALE 11
H-86-84
OEPARTURE(X) LATITUDE(Y) ELEYATION(Z) 0 0 0
05
FROM TO TYPE SS BEDROCK 50 55 80 10 72
PPM NON MAG PPM MAG VG 4020 3059 O 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn, * 0000 Sb N 0000 eSb N EEEE Ba. N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O/d 80AfSTIIRf :.'
H-86-84
DEPARTUREIXI LATITUDE(YI ELEYATIOMIII O O 0
06
FROM TO TYPE SS BEDROCK 55 60 80 10 72
PPM NON MAG PPM MAG VG 2866 1990 0 0
Au: 120 eAu: 344 Ag: .05 eAg: .1 As: 125 eAs: 358 Cu: 120 eCu: 344 Zn: 42 eZn: 120 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: O Ni: 0 eNi: O W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
e N i PJ W N
eW N
MAX
Au: 10 Ag: .05 As: 238 Cu: 76 Zn: 32 Sb: O Ba: 0 Cr: O Co: O Mo: 0 -
Ni: 0 W: O
eAu: 18 eAg: .1 eAs: 429 eCu: 137 eZn: 58 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0!! 9OAES7A1E II
H-86-84
DEPARTURE(X) LATITUDEIY) ELEyATIOU(Z) 0 0 0
07
FROM TO TYPE SS BEDROCK 60 65 80 10 72
PPM NON MAG PPM MAG VG 1804 1922 0 .0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9E EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N O000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0!! AONfS7A,tf II
H-86-84
BEPAP.TUREIXI LATITUBEIT)'ELEVATIONIZI 0 O 0
08
FROM TO TYPE SS BEDROCK 65 70 80 20 72
PPM NON MAG PPM MAG VG 2536 1727 0 0
Au: 25 eAu: 63 Ag: .1 eAg: .3 As: 544 eAs: 1379 Cu: 84 eCu: 213 Zn: 44 eZn: 112 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: O eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W. N
eW N
MAX
0111 AO!!ES7Adf II
H-86-84
IEPARTUREfX) LATITUDEIY) ELEVATIONIZI 0 0 0
09
FROM TO TYPE SS BEDROCK 70 72 80 20 72
40% PURE
PPM NON MAG PPM MAG VG GALENA 11887 2355 2.3 2
Au: 100 eAu: 1189 Ag: .3 eAg: 3.6 As: 190 eAs: 2258 Cu: 160 eCu: 1902 Zn: 60 eZn: 713 Sb: 0 eSb: O Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM **E EEEE MAG 9E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *** EEEE As * EEEE eAs * EEEE Cu * EEEE eCu ** EEEE Zn 9E EEEE eZn -)E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
- eW N
MAX
Au: 300 Ag: .3 As: 214 Cu: 124 Zn: 56 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: O W: O
eAu: 9667 eAg: 9.7 eAs: 6896 eCu: 3996 eZn: 1804 eSb: O eSa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
0/11 RORES7AAE II
H-86-85
DEPARTURE(X1 LATITUDE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 16 18 80 10 23
PPM NON MAG PPM MAG VG 32222 25778 0 0
Sur-Face EEEE MIN EEEE NM iE*IE***-IE*HE EEEE M A G ****jF*jF**** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ***xxxx** EEEE As ** EEEE eAs ** EEEE Cu * EEEE eCu *?E** EEEE Zn * 0000 eZn ** 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 15 A9: .05 As: 354 Cu: 104 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 20 eAg: .1 eAs: 472 eCu: 139 eZn: 53 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
918 POMME II
H-86-85
DEPARTURESX1 LATITUDE(Y) ELEVATI0111Z1 0 0 D
02
FROM TO TYPE SS BEDROCK 18 23 80 20 23
PPM NON MAG PPM MAG VG 1333 1310 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *#* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
01è N0NfS7AdE 11
H-86-86
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 52 62 80 10 81
PPM NON MAG PPM NAG VG 3065 2388 1.6 0
Au: 515 Ag: .05 As: 41 Cu: 40 Zn:. 34 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 1111 Zn * 1111 eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 1578 eAg: .2 eAs: 126 eCu: 123 eZn: 104 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: O
MAX
Au: 625 w.r
As: 12 Cu: 88 Zn: -ro Sb: 0
v Cr: O Co: O Mo: 0 Ni: O
W: O
eAu: 761 eAg: .: eAs: 15 _' . 107 eZn: 46 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
PIE NOMITIAdf II
H-86-86
DEPARTUREf%f LATITUDE(YI ELE9ATI01((Z1 0 0 0
02-3
FROM TO TYPE SS BEDROCK 62 72 80 10 '81
PPM NON MAG PPM MAG VG 1218 1260 .8 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au .* EEEE eAu * EEEE Ag • * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE CO N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
)!I 9ol}ESTAIf 11
H-86-86
IEPARTUREIXI LATITUDEIYI ELEVATIONIII o- o 0
04
FROM TO TYPE SS BEDROCK 72 77 80 20 81
PPM NON MAG PPM MAG VG 2263 1838 0 0
eAu: 600 eAg: 1.1 eAs: 1231 eCu: 362 eZn: 109 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 265 Ag: .5 As: 544 Cu: 160 Zn: 48 Sb: 0 Ba: O Cr: 0 Co: O Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****# EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 150 A9: .6 As: 218 Cu: 88 Zn: 1040 Sb: 0 Ba: 0 Cr: 0 Co: 0 _ Mo: 0 Ni: 0
W: O
eAu: 481 eAg: 1.9 eAs: 699 eCu: 282 eZn: 3337 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0!B 80107A11 11
H-86-86
DEPARTUREIXI LATITUDEIY) ELEVATIGIItZ) 0 0 0
05
FROM TO TYPE SS BEDROCK 77 81 80 20 81
PPM NON MAG PPM MAG VG 3208 1333 0 0
Sur-face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As #* EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn *9E EEEE eZn **** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/1 110R15TAR1 11
H-86-87
1EPARTUREIXI LATITUBE(YI ELEVATION(Zl 0 0 0
01
FROM TO TYPE SS BEDROCK 46 55 80 10 82
PPM NON MAG- PPM MAG VG 4199 3104 0 0
eAu: 462 eAg: .8 eAs: 1201 eCu: 470 eZn: 403 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW : 0
Au: 110 Ag: .2 As: 286 Cu: 112 Zn: 96 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: O
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * 0000 eCu 9E 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIS 8M!lEME 11
H-86-87
lEPARTUREIXI LATITUDEIYI ELEVATIOY121 0 0 0
02
FROM TO TYPE SS BEDROCK 55 65 80 10 82
PPM NON MAO PPM MAG VG 3795 2892 0 0
Au: 30 eAu: 114 Ag: .1 eAg: .4 As: 174 eAs: 660 Cu: 47 eCu: 178 Zn: 48 eZn: 182 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0
_ Co: O eCo: 0 Mo: 0 eNi: O Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * _ EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn .* O000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N, XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 70 Ag: .05 As: 212 Cu: 98 Zn: 64 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 103 eAg: .1 eAs: 586 eCu: 271 eZn: 177 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIB Rfl!fSTAdf II
H-86-87
OEPARTUREtX) LATITUDE(Y) ELEVATIONtZ) 0 O 0
03
FROM TO TYPE SS BEDROCK. 65 71 80 10 82
PPM NON MAG PPM MAG VG 2762 1924 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -)E EEEE Ag * EEEE eAg * EEEE As *HE EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn ?E EEEE' eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 75 Ag: .1 As: 284 Cu: 180 Zn: 80 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 179 eAg: .2 eAs: 676 eCu: 429 eZn: 190 eSb: O eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Of! 9O!lfS7Wdf 11
H-86-87
DEPARTUREIXI LATITUDEI1i ELEVATIOMIZI 0 O 0
04-5
FROM TO TYPE SS BEDROCK 71 80 80 20 82
PPM NON MAG PPM MAG VG 2381 - 1524 0 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au * EEEE eAu * EEEE ,Ag * EEEE eAg * EEEE As 9E* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 250 Ag: .5 As: 342 Cu: 1200 Zn: 84 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: O W: 0
eAu: 1315 eAg: 2.6 eAs: 1799 eCu: 6311 eZn: 442 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
01! AOAESTILlE ll
H-86-87
DEPARTURE(%1 1ATITUDE(Y1 ELEVATION(Zl 0 0 0
06
FROM TO TYPE SS BEDROCK 80 82 80 20 82
PPM NON MAG PPM MAG VG 5259 2222 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu **## EEEE e C u ******* EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
012 MUTAI( II
H-86-88
IEPARTURE(Xf LATITUDE(T1 ELEVATIOM(Il 0 0 0
01
FROM TO TYPE SS BEDROCK 50 60 80 10 70
PPM NON MAO PPM MAG VG 3032 2817 0 0
Au: 185 eAu: 561 Ag: .05 eAg:. .2 As: 324 eAs: 982 Cu: 76 eCu: 230 Zn: 73 eZn: 221 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu ?E EEEE Zr. * EçEE eZn * 0000 Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni. N
eNi N W N
eW N
MAX
OIS 90!lESTARE f.
H-86-88
I#PARTUREIX) LATITUCEtY) ELEVATIONIZI tl O tl
02
FROM TO TYPE SS BEDROCK 60 70 80 20 70
PPM NON MAO PPM MAO VG 4156 3244 0 0
Au: 60 eAu: 249 Ag: .2 eAg: .8 As: 194 eAs: 806 Cu: 68 eCu: 283 Zn: 92 eZn: 382 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag 9F EEEE eAg * EEEE As * EEEE eAs -1F EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa. N 0000 Cr N 0000 eCr N 0000 Co N SSXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
!B PO!lES7A.lE I1
H-86-89
DEPARTUREIX) LATITUDEIY) ELEVATIONIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 44 46 80 20 46
PPM NON MAG PPM MAG VG 4216 2627 0 0
Au: 450 eAu: 1897 Ag: .5 eAg: 2.1 As: 254 eAs: 1071 Cu: 80 eCu: 337 Zn: 78 eZn: 329 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XX"X eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
R?RfSTARf II
H-86-89
DEPARTURE(X) LATITUDE(Y) ELEUATION(Z) 0 0 0
O1A
FROM TO TYPE SS BEDROCK 44 46 80 20 46
D9' 01 I1R91!
PPM NON MAG PPM MAG VG 3673 2717 0 0
Au: 500 Ag: .1 As: 254 Cu: 76 Zn: 52 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: O
Surface EEEE AIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu iE EEEE Ag * EEEE eAg ~E EEEE As ** EEEE eAs * EEEE Cu 9F EEEE eCu ~E EEEE Zn * EEEE eZn ~ EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 1836 eAg: .4 eAs: 933 eCu: 279 eZn: 191 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
MAX
^IB N4NfS7Adf 12
H-86-90
IEPARTUREIXI LATITUDE(Y) ELEVATIIbI(Z) - 0 0 0
01
FROM TO TYPE SS BEDROCK 30 35 80 20 37
PPM NON MAG PPM MAG VG 4333 4412 0 0
Au: 280 eAu: 1213 Ag: .4 eAg: 1.7 As: 185 eAs: 802 Cu: 95 eCu: 412 Zn: 34 eZn: 147 Sb: 0 eSb: O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN
MAy EEEE NM * EEEE MAG ?E EEEE Au * EEEE eAu ?'r EEEE As * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * E_EE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0C^^ Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCc ~J XXXX Mo N
eMo N Ni N eNi N W N eW N
nra on4EçTp!E :1
H-86-90
DEPAP.TUREIXI LATITUDEIY) ELEVATIOUIZ) D 0 0
O1A
FROM TO TYPE SS BEDROCK, 30 37 80 20 37
OVERLAP 01 AND 02 YASB
PPM NON MAG PPM MAG VG 3045 2746 0 0
Au: 120 eAu: 365 Ag: .4 eAg: 1.2 As: 326 eAs: 993 Cu: 102 eCu: 311 Zn: 40 eZn: 122 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg '1F EEEE As **E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N O000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 65 Ag: .4 As: 334 Cu: 95 Zn: 240 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 192 eAg: 1.2 eAs: 985 eCu: 280 eZn: 708 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OC soeEs7atc rr
H-86-90
DEPARTUREI%1 LATITUDEIYI ELE4ATIOBIZI 0 0 0
02
FROM TO TYPE SS BEDROCK 35 37 80 20 37
15% PYDITF
PPM NON MAG PPM MAG VG 2949 1859 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **# EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn .~ EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/B 90R£SlARf II
H-86-91
DEPARTUREIXI LATITUDEfY) ELEYATIONIII O O O
01
FROM TO TYPE SS BEDROCK 44 50 80 10 57
22, PYRITE
PPM NON MAG PPM MAG VG 4121 2715 0 0
Au: 70 eAu: 288 Ag: .3 eAg: 1.2 As: 368 eAs: 1517 Cu: 83 eCu: 342 Zn: 58 eZn: 239 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *1E* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW h<
MAX
018 AONESTARE 11
H-86-91
DEPARTUREi%) LATITUDEiYI ELEVATION(I) 0 0 0
02
FROM TO TYPE SS BEDROCK 50 55 80 20 57
PPM NON MAG PPM MAG VG 4429 2833 5.7 0
eAu: 1838 eAg: .9 eAs: 341 eCu: 177 e=n: 106 eSb: 0 eBa: O eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Au: 415 Ag: .2 As: 77 Cu: 40 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu -)E EEEE Zn * EEEE eZn * • EEEE Sb N EEEE eSb N EEEE Ba N 3333 eBa N 3333 Cr N 3333 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 135 Ag: .2 As: 67 C u : 32 Zn: 24 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0
W: O
eAu: 628 eAg: .9 eAs: 312 eCu: 149 eZn: 112 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
018 IoRFs>•acr II
H-86-91
JEPARTIIREIXI LATITULEIY) ELE9ATIOXIZ) 6 0 0
03
FROM TO TYPE SS BEDROCK 55 57 80 20 57
PPM,NON MAO PPM MAO VG 4650 2146 2.6 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
0111 NOAFSTAIf 11
H-86-92
DEPARTUREIXI LATITUàEIYI ELEYATIONIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 43 45 80 20 48
PPM NON MAG PPM MAG VG 3933 2700 2.7 0
Au: 220 eAu: 865 Ag: .4 eAg: 1.6 As: 196 eAs: 771 Cu: 80 eCu: 315 Zn: 46 eZn: 181 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE Az * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 70 Ag: .3 As: 144 Cu: 82 Zn: 108 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0 Ni: 0 W: 0
eAu: 302 eAg: 1.3 eAs: 620 eCu: 353 eZn: 465 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O/D ,9411ESTRdf II
H-86-92
DEPARTUREIX) LATITUDEITI ELEUATIONIZI 0 0 0
02
FROM TO TYPE SS BEDROCK 45 48 80 20 48
PPM NON MAG PPM MAG VG 4308 2359 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As 9F EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 65 Ag: .4 As: 193 Cu: 172 Zn: 52 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
eAu: 242 eAg: 1.5 eAs: 712 eCu: 640 eZn: 19Z eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: C eNi: 0 eW: C
01d 0O10T41( 11
H-86-93
DEPARTUREIX) LATITUDEtY) ELEVATI3StZ) , 0 t) D
01
FROM TO TYPE SS BEDROCK 49 55 80 20 58
PPM NON MAG PPM MAG VG 3719 2363 0 0
Surface EEEE MIN LEE! NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE ee5 N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O1T 90AESTARE II
H-86-93
DEPARTURE(X) LATITUDE(Y) ELEDAIICB(Z) 0 o a
OlA
FROM TO TYPE SS BEDROCK 49 58 80 20 58
OVERLAP.0! ARD 02 WAS!
PPM NON MAO PPM MAG. VG 3294 2588 0 0
eAu: 494 eAg: 1.3 eAs: 1028 eCu: 428 eZn: Z11 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: v eNi: 0 eW: v
Au: 150 Ag: .4 As: 312 Cu: 130 Z n : 64 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG -)F EEEE Au * EEEE eAu .x EEEE Ag * EEEE: eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N O000 Ba N 0000 eBa N O000 Cr N O000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 30 Ag: .2 As: 226 Cu: 145 Zn: 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 120 eAg: .8 eAs: 904 eCu: 580 eZn: 224 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 10107AlE 11
H-86-93
DEPARTUREtXI LATITUDEtY) ELE9ATIOtttZl 0 . 0 0
02
FROM TO TYPE SS BEDROCK 55 58 80 20 58
PPM NON MAG PPM MAO VG 4000 2286 0 0
Surface EESE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As '1F* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XY.XY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/1 841!ESTA1E 11
H-86-94
DEPARTUREIXt LATITUDEIYI ELEVATIOlIRf ' 0 0 0
01
FROM TO TYPE SS BEDROCK 42 45 80 10 54
PPM NON MAG PPM MAG VG 2796 1419 0 0
Au: 45 Ag: .6 As: 464 Cu: 117 Zn: 106 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag IF EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 126 eAg: 1.7 eAs: 1297 eCu: 327 eZn: 296 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 160 Ag: .6 As: 1008 Cu: 240 Zn: 116 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 487 eAg: 1.8 eAs: 3066 eCu: 730 eZn: 353 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
OIE ROMESTARE II
H-86-94 0
DEPARTURE(X) LATITUDE(T) ELEVATION(Z) 0 0 0
O1A
FROM TO TYPE SS BEDROCK 45 54 80 20 54
2% PT OVERLAP 2i3 WASH
PPM NON MAG PPM MAG VG 3042 2750 1.7 0
Surface EEEE MIN EEEE NM 4 EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ********** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEE2 Sb N EEEE eSb N 1111 Ba N 1111 eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
018 ADNESIAdE II
H-86-94
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 . 0 0
02
FROM TO TYPE SS BEDROCK 45 50 80 20 54
PPM NON MAG PPM MAG VG 3085 2388 0 0
Au: 255 Ag: .5 As: 736 Cu: 68 Zn: 50 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O. Ni: O W: C
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 787 eAg: 1.5 eAs: 2270 eCu: 210 :eZn: 154 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Olé UOMESTAIE II
H-86-94 DEPARTURE(X) LATITUDE{Y) ELEVATIOIIiZ)
0 O O
03
FROM TO TYPE SS BEDROCK 50 54 80 20 54
PPM NON MAG PPM MAG VG 3462 2436 0 0
Au: 110 eAu: 381 Ag: .4 eAg: 1.4 As: 512 eAs: 1772 Cu: 95 eCu: 329 Zn: 44 eZn: 152 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: O eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG . * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***F* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
e W N
MAX
018 A0IlfSTAff II
4
H-86-95
1EPARTUREIX) LATITUlE(Y) ELfVATI0NIZ1 0 0 0
01
FROM TO TYPE SS BEDROCK 41 45 80 10 52
PPM NON MAG PPM MAG VG 4175 3439 0 0
Au: 110 eAu: 459 Ag: .4 eAg: 1.7 As: 856 eAs: 3574 Cu: 105 eCu: 438 Zn: 72 eZn: 301 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: O eNi: O Ni: O eNi: 0 w: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *IE**dEiHE* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIS BOlIEST/lNF II
H-86-95
DEPARTUREtXI LATITUDE(Y) ELEVATIONtZI 0 0 0
02
FROM TO TYPE SS BEDROCK 45 50 80 20 52
20% MITE
PPM NON MAO PPM MAO VG ASPY 4585 3415 5.2 5
Au: 95 Ag: .5 As: 760 Cu: 90 Zn: 36 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAO ;E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As *HF*IE*** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 2222 eBa N 2222 Cr N 2222 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 436 eAg: 2.3 eAs: 3485 eCu: 413 eZn: 165 eSb: O eBa: 0 eCr: O eCo: 0 eNi: O eNi: 0
eW: O
MAX
Au: 390 Ag: .4 As: 1040 Cu: 150 Zn: 76 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0
W: O
eAu: 1606 eAg: 1.6 eAs: 4292 eCu: 618 eZn: 313 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
011 WYMESTAIE 11
H-86-95
IEPARTUREtX) LATITUDEf1) ELEUATIOliQ) 0 0 0
03
FROM TO TYPE SS BEDROCK 50 52 80 20 52
PPM NON MAG PPM MAG VG' 4118 4000 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au* iE EEEE eAu .t 9E EEEE Ag' _ * EEEE eAg * EEEE As ********** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn .* EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OC BO1!ESTA1( 11
H-86-96 DEPARTIDtE IX) LATITUDE IT) ELEVATION II)
0 0 0
01
FROM TO TYPE SS BEDROCK 39 43 80 20 43
PPM NON MAG PPM MAG VO 4281 3754 0 0
Au: 280 eAu: 1199 Ag: .6 eAg: 2.6 As: 1040 eAs: 4452 Cu: 160 eCu: 685 Zn: 56 eZn: 240 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: O Co: 0 eCo: 0 Mo: .0 " eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ********** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
03 0081574dE II
H-86-96
DERARTt)REIX) LATITI)DEIY) ELE9ATIODIZ) 0 O 0
O1A
FROM TO TYPE SS BEDRCCX 39 43 80 20 4Z
20% PYIITf DO 01 WASH
PPM NON MAG PPM MAG VG 3505 3226 1.7 0
Au: 140 eAu: 491 Ag: .6 eAg: 2.1 As: 944 eAs: 3309 Cu: 160 eCu: 561 Zn: 58 eZn: 203 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: O
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As ********* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
MAX
~ld AOAfSTAlf 11
H-86-97
DEPARTUREIX) LATITUDEIY) ELE'vATIC4IZ) 6 D 0
01
FROM TO TYPE SS BEDROCK 32 35 SO 20 41
PPM NON MAO PPM MAO VG 4123 3467 1.6 0
Au: 165 eAu: 680 Ag: .2 eAg: .8 As: 712 eAs: 2936 Cu: 115 eCu: 474 Zn: 44 eZn: 151 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: C Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: C W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * =EEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
e N i N W N eW N
MAX
01B PO!lf57A,(f II
H-86-97
DEPARTUREIXI LATITUDEIY) ELEYATIONIZ1 0 0 0
02
FROM TO TYPE SS BEDROCK 35 40 80 20 41
PPM NON MAG PPM MAO VG 3714 2819 0 0
Au: 135 Ag: .2 As: 696 Cu: 90 Zn: 60 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 501 eAg: .7 eAs: 2585 eCu: 334 eZn: 223 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
CIF AeeEST411 11
H-86-97
HEPARTUREIX) LATITUBEIYI ELEUATIO))IZ) 0 o 0
03
FROM TO TYPE SS BEDROCK 40 41 80 20 41
PPM NON MAO PPM MAG VG 3148 2093 1.5 0
Au: 140 eAu: 441 Ag: .3 eAg: .9 As: 528 eAs: 1662 Cu: 120 eCu: 378 Zn: 58 eZn: 183 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * ESSE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N ESSE eSb N EEEE Ba N EE= eBa N EEEE Cr N 1111 eCr N 1111 Co N `fXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Oil IMIESTASE II
H-86-98 DEPARTUREIX) LATITUDE(Y) ELEVATICK(Z)
D D 0
01
FROM TO TYPE SS BEDROCK 25 30 20 10 37
PPM NON MAG PPM MAG VG 4225 3812 0 0
Au: 170 eAu: 718 Ag: .6 eAg: 2.5 As: 880 eAs: 3718 Cu: 200 eCu: 845 Zn: 78 eZn: 330 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM 9E EEEE MAG 9E EEEE Au * EEEE eAu 9E EEEE Ag 9E EEEE eAg 96# EEEE As ******** EEEE eAs 9E EEEE Cu * EEEE eCu 96 EEEE Zn 9E 0000 eZn 96 0000 Sb N 0000 eSb N 000^ Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
018 AC!!fSTA.it Il
H-86-98
9EPARTURE(XI LATITULE(YI ELEVATIONIZI 0 0 0
02
FROM TO TYPE SS BEDROCK 30 35 80 20 37
PPM NON MAG PPM MAG VG 3505 3562 0 0
Au: 165 eAu: 578 Ag: .6 eAg: 2.1 As: 592 eAs: 2075 Cu: 125 eCu: 438 Zn: 56 eZn: 196 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs 9F EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N OOCO Ba N 0000 eBa N OOCO Cr N EESE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OFF g0:7f57P..ir I!
H-86-98
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
03
FROM TO TYPE SS BEDROCK 35 37 80 20 37
PPM NON MAG PPM MAG VG 3323 2544 0 0
Au: 105 eAu: 349 Ag: .5 eAg: 1.7 As: 608 eAs: 2020 Cu: 125 eCu: 415 Zn: 108 eZn: :59 Sb: 0 eSb: O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag . * EEEE eAg * EEEE As ****-IF* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0!8 90107Adf II
H-86-99
DEPARTUREIXI LATITUDE(Y) ELEUATI08(21 a o 0
01
FROM TO TYPE SS BEDROCK 51 55 80 20 61
PPM NON MAG PPM MAG VG 5400 3000 0 0
eAu: 783 eAg: 2.2 eAs: 49dS: eCu: 9C7 eZn : 227 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 145 Ag: .4 As: 920 Cu: 168 Zn: 42 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: C Ni: 0
W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ********* EEEE eAs *# EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXX`/, eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIS EOMESTASE II
H-86-99
DEPARTUREiX) LATITUBEIT) ELEVATION(Z) 0 0 0
02
FROM TO TYPE SS BEDROCK 55 61 SO 20 61
PPM NON MAG PPM MAG VG 3176 2627 0 0
eAu: 842 eAg: .2 eAs: 1093 eCu: 238 eZn: 108 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 265 Ag: .05 As: 344 Cu: 75 Zn: 34 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: C Ni: 0
W: 0
Surface EEEE MIiJ EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * çççE eZn * EEEE Sb N
eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXX;: Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 1145 Ag: .05 As: 832 Cu: 240 Zn: 50 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 4155 eAg: .2 eAs: 3019 eCu: 871 eZn: 181 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
VI 90AfSTA1IË II
H-86-100 DEPARTURE!%) LATITUDEIY) ELEVATIOIUZI
O 0 0
01
FROM TO TYPE SS BEDROCK 31 35 80 10 42
PPM NON MAO PPM MAG VG 3628 3191 1.7 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Oil 9O1)ESTIILE II
H-86-100
DEPARTURE{Xl LATITUDEtY1 ELEVATIQAiZI O D O
02
FROM TO TYPE SS BEDROCK 35 40 80 20 42
PPM NON MAG PPM MAG VG 3297 3225 0 0
eAu: 577 eAg: 2.6 eAs: 2453 eCu: 346 eZn: 211 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Au: 175 Ag: .8 As: 744 Cu: 105 Zn: 64 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *HE EEEE eA9 ** EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 160 Ag: .05 As: 312 Cu: 75 Zn: 36 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni : 0 W: 0
eAu: 502 eAg: .2 eAs: 979 eCu: 235 eZn: 113 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
0l1 900ESTAdf II
H-86-100
DEPARTUREIX) LAIITUDEIY) ELEVAIIORIZ) 0 0 0
03
FROM TO TYPE SS BEDROCK 40 42 80 20 42
PPM NON MAG PPM MAG VG 3138 2421 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIE .9oREs?a:cf rT
H-86-102
DEPARTURE(XI LATITUDEIYI ELEYATION(Z1 0 0 0
01
FROM TO TYPE SS BEDROCK 68 75 80 10 87
PPM NON MAG PPM MAG VG 2909 2121 0 0
eAu: 1513 eAg: 1.2 eAs: 1932 eCu: 262 eZn: 192 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 520 Ag: .4 As: 664 Cu: 90 Zn: 66 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIB 1OI!ES7AfE II
H-86-102
DEPARTUREfX) LATITUDE(Y) ELEVATION Q) D O 0
02
FROM TO TYPE SS BEDROCK 75 80 80 10 37
PPM NON MAG PPM MAG VG 3042 2035 0 0
eAu: 259 eAg: .9 eAs: 3018 eCu: 319 eZn: 116 eSb: 0 eBa: 0 eCr: 0 eCo: G eNi: 0 eNi: 0 eW: 0
Au: 85 Ag: .7) As: 992 Cu: 105 Zn: 38 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * ESSE eAu ?E- E=rS Ag * ESSE eAg * EEEE As ********* EEEE eAs ~E ESSE Cu * SEE= eCu * EEEE Zn * ESSE eZn * EEEE Sb N ESSE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE ECr, N EEEE Co N XXXX eCo N `;`:Y" Mo N ..
eMo N Ni N ?Ni N W N eW N
MAX
HONESTAIf I!
H-86-102 DEPARTURE(X) LATITUDE(Y) ELEVATIDN(Z)
0 D 0
03
FROM TO TYPE SS BEDROCK 80 S5 80 20 87
PPM NON MAG PPM MAO VG 4077 2493 0 0
Au: 235 eAu: 958 Ag: .4 eAg: 1.6 As: 1112 eAs: 4534 Cu: 130 eCu: 530 ?n: 52 EZn: 212 Sb: 0 eSb: 0 Ea: 0 eBa: 0 Cr: 0 eCr: v Co: 0 eCo: 0 °')o: 0 eNi: 0 Ni: 0 eNi: C W: 0 eW: G
Surface EEEE MIN EEEE NM * ELLE MAG * ELLE Au Y- ELLE eAu * =Lm= ,g * EEEE =A7 -)E =cc! As *********** rr_f= eAs * EEEE Cu * EL= eCu * EEEE Zn * EEEE * EEEE Sb N =EE= eSb N EFEC Es. N EEEE eBa N 0000 Cr N O000 eCr N EEEE Co N x::X;: eCo N ?.xxx Mo N
eMo N Ni N
eNi N W N
eW N
MAX
!'Ig IfS16.{f 7I
H-86-102
DEpARTUREIX) LATITUIEtYf ELEVATIOAili 0 0 0
04
FROM TO TYPE SS BEDROCK 85 c^7 80 20 S~
P!''M NON MAG PPM MAO VG 37E2 • 2121 0 C
Au: 115 eAu: 4:6 Ag: .6 eAg: 2.3 As: 369 eAs: 1398 Cu: 120 e;. u: 455 Zn: 32 eZn: 121 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: O Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EPEE MIN EEEÇ NM * EEEE MAG * EEEE Au * EEEE eAu .. EEEE Ag * EEEE eAg ** EEEE As *** rE== eAs * crE E Cu * EEEE eCu * SE!! Zn * EEEE eZn * EEE= Sb N EEEE eSb N EEEE Pa N EEEE era EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
e t+! o N Ni N eNi N W N eW N
MAX
C!? gnRrg`q(c I'
H-86-103
DEPARTCRE(X; LATITL'EEtY; ELEiIATIBH2; C 0 0
01
FROM TO TYPE 62 68 sO
Ÿ v
20 BEDROCK
b$
PPM NON MAG PPM MAG VG 2724 1905 1.5 0
Au: 2000 eAu: 5448 A9: .05 eAÿ: .1 As: 480 eAs: 131+7 Cu: 105 eC:.t: 236 Zn: 46 eZn: 125 Sb: eSb: 0 Ba: 0 era: 0 Cr: 0 ec:~ . 0 Co: 0 e^.o: v Mo: 0 eNi: 0 Ni: 0 eNi: v W: O evi: v
Surface EEL_ MIN EEEE NM .. EEEE MAO * EEEE ».i EEEE eAu * EEEE A-3 * rL~r eng * EEEE As **** ET6r eAs * EEEE Cu ?F
*
EE_ E ~,,-. * *
3b N
__--~ ;a -SEE :11: Cr N
_11 - N
1111 Co AJ eCo N Mo N eMo N Ni N
e N i N W N eW N
f!!. rMçTA.{E .'1
H-86-104
DEPARTUREIX) LATITUNIY1 ELHiATID1IZ) C 0 0
01
FROM TO TYPE SE BEDROCK 64 70 $0 20 70
PPM NON MAO PPM MAO VO 3939 2'47 0 O
eAu: 19' eAg: 2.4 eAs: 2553 eCu: 414 eZn: 355 eSb: 0 eÿ G: V eCr: C eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 50 Ag: .6 As: 648 Cu: 105 Zn: 90 Sb: 0 Ba: 0 Cr: C Co: 0 Mo: C Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO '9t- EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZr, * EEEE Sb N EEEE eSb ?: EEEE Fa N EEEE ePâ N 0000 Cr N 0000 eCr N 0000. Co N X..= eCo N XXXX Mo N
eMa N Ni N
eNi N W N
eW N
MAX
n/g 9OrfS7Adf II
H-86-104
DEPARTUREIXI LATITUDEtYJ ELEVATIDRIZ) 0 0 0
01A
FROM TO TYPE SS BEDROCK 64 70 80 20 70
2UP Cl MAS!
PPM NON MAG PPM MAG VG 5173 2667 0 0
eAu: 336 eAg: 7.2 eAs: 2814 eCu: 1035 eZn: 724 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 65 Ag: 1.4 As: 544 Cu: 200 Zn: 140 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag **#* EEEE eAg ****** EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE EEEE eZn * EEEE Sh N CEEE
eSb N
EPEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
3!B ATPIT74f.f II
H-86-105
DEPARTUREIX) LATITUDEIY) ELEYATIOMIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 64 66 8C 10 SO
PPM NON MAG PPM MAG VG 9333 2200 0 0
Au: 175 A9: .6 As: 504 Cu: 340 Zn: 50 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM ** EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ***** EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu *** EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
eAu: 1633 eAg: 5.6 eAs: 4704 eCu: 3173 eZn: 467 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
0lB ROfESTAdE II
H-86-105
DEPARTUREiX1 LATITUDElY1 ELEYATIDRfZ1 0 0 0
02
FROM TO TYPE SS BEDROCK 66 72 80 10 80
PPM NON MAG PPM MAG VG 3810 2190 1.9 0
Au: 225 eAu: 857 Ag: .8 eAg: 3 As: 364 eAs: 1387 Cu: 560 eCu: 2133 Zn: 48 eZn: 183 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag *# EEEE eAg ** EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu *# EEEE Zn * EEEE eZn * EEEE Sb N EEEE e8b N 1111 Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
nrF SONfSTx(f 1!
H-86-105
I)EPARTUREIX) LATITLBEtY) EiEVhTIGNIZ; () 0 t)
03
FROM TO TYPE SS BEDROCK 72 77 80 20 80
PPM NON MAO PPM MAG VG 2772 1841 0 0
Au: 95 Ag: .05 As: 688 Cu: 55 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
Sur-Face EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **#*** EEEE eAs * EEEE Cu * EEEE eCu ;x EESE Zn * EEEE eZn * EEEE . Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 263 eAg: .1 eAs: 1907 eCu: 152 eZn: 122 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 180 Ag: .6 As: 330 Cu: 110 Zn: 270 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 535 eAg: 1.8 eAs: 981 eCu: 327 eZn: 802 eSb: O eBa: 0 eCr: C eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE !MUE 11
H-86-105
DEPARTtNtE{X) LATITEIDE(T) ELEUATIONaI 0 0 0
04
FROM TO TYPE SS BEDROCK 7? SO 80 20 SO
PPM NON MAG PPM MAG VG 2971 1638 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As #** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE a3a N EEEE Cr N OCCO eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
^!P °^!!ES?A{E II
H-86-106
DEFARTUREI%1 LATITUDEIT► ELEYATIOktZl 0 0 0
01
FROM TO TYPE SS BEDROCK 78 80 10 85
PPM NON MAO PPM MAO vG 4912 2877 0 0
Au: 105 Ag: .5 As: 370 Cu: 150 Zn: 54 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ** EEEE As #** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
ët+10 N Ni N eNi N W N eW N
eAu: 516 eAg: 2.5 eAs: 1ô18 eCu: 737 eZn: 265 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
0!1 P.01!ESTAIE II
H-86-106
DEPARTURE(X) LATITL'bEIY) ELEYATIOP+iZ) o o o
01A
FROM TO TYPE SS BEDROCK 73 85 SO 20 85
OVERLAP 1 70 J VAS!
PPM NON MAG PPM MAG VG 3419 3214 0 0
Au: 180 Ag: .6 As: 632 Cu: 168 Zn: 80 Sb: 0 Ba: O Cr: 0 Co: C Mo' 0 Ni: 0
W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE: eAs * EEEE Cu * EEEE eCu * EEEE Zr: * EEEE eZn * EEEE Sb N
eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 615 eAg: 2.1 eAs: 2161 eCu: 574 eZn: 274 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Dra NORESTA1E II
H-86-106
DEPlIRTUREIXI LAIITUDEfY) ELEUATIONIZ) 0 0 0
02
FROM TO TYPE SS BEDROCK 78 83 80 20 85
PPM NON MAG PPM MAG VG 3045 1990 0 0
eAu: 320 eAg: 1.2 eAs: 2022 eCu: 289 eZn: 134 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 105 Ag: .4 As: 664 Cu: 95 Zn: 44 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0!I 90MESTAIf 11
H-86-106
DEPARTURE(X) LATIT!lDEIYI ELE4fATI1D1(Z) 0 0 O
03
FROM TO TYPE SS BEDROCK 83 85 80 20 85
PPM NON MAG PPM MAG VG 3148 1759 0 0
Au: 70 eAu: 220 Ag: .4 eAg: 1.3 As: 292 eAs: 919 Cu: 70 eCu: 220 Zn: 52 eZn: 164 Sb: O eSb: O Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: O W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu *-EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
013 B0NESTALE 11
H-86-107
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 79 85 80 10 103
PPM NON MAG PPM MAG VG 4303 2636 0 0
eAu: 538 eAg: 2.2 eAs: 1360 eCu: 301 eZn: 224 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 125 Ag: .5 As: 316 Cu: 70 Zn: 52 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXY. Mo N
eMo N Ni N eNi N
W N eW N
MAX
01B POA£STAI£ II
H-86-107
DEPARTURE(XD LATITUDEIY1 ELEUATION(21 0 0 0
02
FROM TO TYPE SS BEDROCK 85 90 80 10 103
PPM NON MAG PPM MAG VG 3520 2507 4.3 0
Au: 340 eAu: 1197 Ag: .3 eAg: 1.1 As: 388 eAs: 1366 Cu: 68 eCu: 239 Zn: 58 eZn: 204 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9F EEEE eZn * EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
OIB .9O1lfS?A.if II
H-86-107
DEPARTUREIX) LATITUDEIYt ELE'JATIONIZJ O O 0
03
FROM TO TYPE SS BEDROCK 90 95 80 10 103
PPM NON MAO PPM MAG VG 3977 2292 0 0
eAu: 775 eAg: 1.6 eAs: 1217 eCu: 219 eZn: 310 eSb: 0' eBa: .0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 195 Ag: .4 As: 306 Cu: 55 Zn: 78 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE M I iv EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **3E EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EGFç eSb N EEEE Ba N 0000 eBa N 000C Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
x:~
MAX
9?F ?NOME I!
H-86-107
BEPARTUREIXf LATITUDEIYi ELEVATIONIZf 0 0 0
04
FROM TO TYPE SS BEDROCK 95 100 SO 20 103
PPM NON MAG PPM MAG VG 2788 2352 1.9 ~
Au: 2095 eAu: 5841 Ag: 1 eAg: 2.8 As: 356 eAs: 992 Cu: 70 eCu: 195 Zn: 56 eZn: 156 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg ** EEEE As *E* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 1111 Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
011 RDRESTAIE II
H-86-107
DEPARTI)P.EIX) LATITüBElY1 ELE9ATIONtZ) 0 0 0
05
FROM TO TYPE SS BEDROCK 100 103 80 20 103
25S PYRITE
PPM NON MAG PPM MAG VG GALENA 3067 2827 2.1 30
eAu: 767 eAg: 1.2 eAs: 2969 eCu: 399 eZn: 215 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Au: 250 Ag: .4 As: 968 Cu: 130 Zn: 70 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ********* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 835 Ag: 1.2 As: 0 Cu: 164 Zn: 600 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
eAu: 334 eAg: .5 eAs: 0 eCu: 66 eZn: 240 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
n r n anrESTAIE II
H-86-108
DEPARTUREIXI LATITUDEITI ELEUATIONIZI O O O
01A
FROM TO TYPE SS BEDROCK 73 74 80 20 75
POOR VASBED SAMPLE
PPM NON MAG PPM MAG VG 400 133 10.7 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg * EEEE As N EEEE eAs N EEEE Cu * EEEE eCu -)E EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
)Id POMME 17
H-86-109
DEPARTURE(X) LATITUDEIYI ELEVATIOM(Zl D D 0
01
FROM TO TYPE SS BEDROCK 75 80 80 10 88
PPM NON MAG PPM MAG VG 3686 2863 0 0
Au: 240 Ag: .6 As: 636 Cu: 140 Zn: 104 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *HE EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZri * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
eAu: 835 eAg: 2.2 eAs: 2344 eCu: 516 eZn: 383 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 1365 Ag: .6 As: 386 Cu: 130 Zn: 64 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0
W: 0
eAu: 3868 eAg: 1.7 eAs: 1094 eCu: 368 eZn: 181 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE POMME 11
H-86-109
DEPARTURE(X) LATITUDE(Yl ELEUATIOM(Zl 0 0 0
02
FROM TO TYPE SS BEDROCK 80 85 80 20 88
PPM NON MAG PPM MAG VG 2833 2367 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **9F EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N O000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 210 Ag: .5 As: 368 Cu: 90 Zn: 42 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 548 eAg: 1.3 eAs: 960 eCu: 235 eZn: 110 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE 10fESTAXE 11
H-86-109
DEPARTUREIX) LATITUDEIY) ELEVATIONII) 0 0 0
03
FROM TO TYPE SS BEDROCK 85 88 80 20 88
PPM NON MAO PPM MAG VG 2607 2074 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * ELLE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
O!F OMETTRE II
H-86-110
DEPARTURE{X) LATITUDE(Y) ELEVATION)1) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 85 95 80 10 125
15S PYRITE
PPM NON MAG PPM MAG VG 2370 1852 2.4 0
Au: 295 Ag: .5 As: 528 Cu: 120 Zn: 42 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **##* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 2222 eZn * 2222 Sb N 2222 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
eAu: 699 eAg: 1.2 eAs: 1252 eCu: 284 eZn: 100 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eu: 0
MAX
013 MOMIE ll
H-86-110
DEPARTUREIX) LATITUDEIY) ELEYATIOIIIZI 0 0 0
03
FROM TO TYPE SS BEDROCK 95 99 80 10 125
PPM NON MAO PPM MAG VG 3939 2061 0 0
Au: 70 Ag: .4 As: 258 Cu: 82 Zn : 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N COCO eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 276 eAg: 1.6 eAs: 1016 eCu: 323 eZn: 221 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Old p0.RE8TAEf II
H-86-110
BEPARTUREiXI LATITUBEIY) ELEVATIOAIZI 0 " 0 0
04
FROM TO TYPE S8 BEDROCK 99 105 80 10 125
PPM NON MAG PPM MAG VG 2886 2411 0 0
eAu: 144 eAg: .9 eAs: 1039 eCu: 332 eZn: 139 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 50 Ag: .3 As: 360 Cu: 115 Zn: 48 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N OOOC Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Old 9OAESTAIE II
H-86-110
DEPARTURE!%) LATITUDECT) ELEVATION)Z) 0 0 0
05
FROM TO TYPE SS BEDROCK 105 109 80 10 125
PPM NON MAG PPM MAG VG 2645 1923 0 0
Au: 185 eAu: 489 Ag: .2 eAg: .5 As: 260 eAs: 688 Cu: 57 eCu: 151 Zn: 35 eZn: 93 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Old NOMES7Adf II
H-86-110
BEPARTUREIX) LATITUDEIY) ELEVBTIOMi1) 0 0 0
06
FROM TO TYPE SS BEDROCK 109 115 80 10 125
PPM NON MAG PPM MAG VG 3065 2468 1.6 0
Au: 1380 eAu: 4229 Ag: .4 eAg: 1.2 As: 334 eAs: 1024 Cu: 160 eCu: 490 Zn: 80 eZn: 245 Sb: 0 eSb: 0 Ba: 0 'eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MA::
O/B AOAÉS7Adf 11
H-86-110
DEPARTIIREIX) LATITIIDE{Y) ELEVATIO!(iZ) D 0 O
07
FROM TO TYPE SS BEDROCK 115 120 80 20 125
PPM NON MAG PPM MAG VG 3969 2419 0 0
eAu: 357 eAg: 1.6 eAs: 1905 eCu: 496 eZn: 333 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 90 Ag: .4 As: 480 Cu: 125 Zn: 84 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE A s **** EEEE eAs :Y EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Be. N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
018 90AFS7RRf II
H-86-110
DEPARTURE(X) LATITUDEIYI ELEVATIOIiiZI 0 O D
08
FROM TO TYPE SS BEDROCK 120 125 SO 20 125
PPM NON MAO PPM MAO VG 3135 2054 0 0
Au: 60 eAu: 188 Ag: .4 eAg: 1.3 As: 238 eAs: 746 Cu: 140 eCu: 439 Zn: 76 eZn: 238 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCc: 0 Mo: O eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N -EEE eBa N EEEE Cr N 0000 eCr N O000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/3 :YOMESTAIE II
H-86-111
DEPARTUREIX) LATITUDEIY) ELEYATIONIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 81 85 80 20 88
PPM NON MAG PPM MAG VG 2621 1793 O 0
eAu: 262 eA9: 1 eAs: 1300 eCu: 278 eZn: 294 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 100 Ag: .4 As: 496 Cu: 106 Zn: 112 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * cEEE eZn * EEEE Sb N E2EE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAY.
Au: 240 Ag: .2 As: 1096 Cu: 77 zn. t4
Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAt, : 608 eag: .5 eAs: 2777 eCu: 195 eZn: 142 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
are P IISTAIE II
H-86-111
DEPARTUREIXI LATITUDEIYI ELEVATIONiZ1 O 0 0
02
FROM TO TYPE SS BEDROCK 85 88 80 20 88
PPM 25:3 1307
PPM _nMAG VG
~.A ~..} 1 .J V ! ~ • -
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ********** EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn * EEEE eZn * EEEE Sb N "EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0IP 900(S7A1E 11
H-86-112
DEPARTUREIX) LATITU9EIY1 ELEVATIO)lIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 83 85 80 10 150
PPM NON MAG PPM MAG VG 3744 2487 0 0
eAu: 412 eAg: 1.5 eAs: 1198 eCu: 468 eZn: 314 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 110 Ag: .4 As: 320 Cu: 125 Zn: 84 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * O000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIE ROEESTAff II
H-86-112
DEPARTUREIXI LATITUDEtY1 ELEUATIINI(Z1 0 0 0
02
FROM TO TYPE SS BEDROCK 95 90 80 10 150
PPM NON MAG PPM MAG VG 2116 1820 0 0
eAu: 1968 eAg: 1.1 eAs: 1422 eCu: 614 eZn: 220 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 930 Ag: .5 As: 672 Cu: 290 Zn: 104 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni : O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * 0000 eCu -JE 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
0/3 NONESTARE II
H-86-112
6EPARTUREIX) LATITURE(Y) ELEVATIOM(Z) 0 0 0
03
FROM TO TYPE SS BEDROCK 90 95 80 10 150
PPM NON MAG PPM MAG VG 3729 2976 1.5 0
Au: 1865 eAu: 6955 Ag: .2 eAg: .7 As: 352 eAs: 1313 Cu: 120 eCu: 448 Zn: 38 eZn: 142 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE _MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * 1111 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 1305 Ag: .8 As: 704 Cu: 105 Zn: 48 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 4287 eAg: 2.6 eAs: 2313 eCu: 345 eZn: 158 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0il 80AE£TAff II
H-86-112
DEPARTUREIXI LATITUDEIYI ELEVATIONIZI 0 0 0
04
FROM TO TYPE SS BEDROCK 95 100 80 10 150
PPM NON MAG PPM MAG VG 3285 2976 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag ** EEEE eA9 ** EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
013 AOAESTAIE II
H-86-112
BEPARTURE(X1 LATITU4E(Y) ELEVATIQN(Zl 0 0 0
O5
FROM TO TYPE SS BEDROCK 100 105 80 10 150
PPM NON MAG PPM MAG VG 4207 2441 0 0
Au: 530 eAu: 2229 Ag: 1 eAg: 4.2 As: 1128 eAs: 4745 Cu: 168 eCu: 707 Zn: 84 eZn: 353 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *E EEEE eAg **9E EEEE As *********** EEEE eAs ** EEEE Cu * EEEE eCu * EEEE Zn * O000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0!S .90PESTAdf II
H-86-112
DEPARTURE(XI LATITUDE(Y] ELEVATIOlIQ] O 0 D
06
FROM TO TYPE SS BEDROCK 105 110 80 10 150
10S PYRITE
PPM NON MAG PPM MAG VG 4048 2158 3.9 0
Au: 450 eAu: 1822 Ag: .4 eAg: 1.6 As: 451 eAs: 1826 Cu: 95 eCu: 385 Zn: 46 eZn: 186 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 2222 Sb N ESEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
C!* P.PAES7AdE II
H-86-112
DEPARTUREtX1 LATITUDE(Y) ELEVATION(Z) 0 0 0
07
FROM TO TYPE. SS BEDROCK 110 115 80 10 150
PPM NON MAG PPM MAG VG 3106 1951 0 C
Au: 190 eAu: 590 Ag: .4 eAg: 1.2 As: 560 eAs: 1 739 Cu: 100 eCu: 311 Zn: 46 eZn: 143 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn -)F EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
013 80MES1AI: 11
H-86-112
DEPARTURE(X) LATITUDE;Y) ELEVATIONUZ) 0 0 0
O8
FROM TO TYPE SS BEDROCK 115 120 80 10 150
15S PYRITE
PPM NON MAG PPM MAG VG 3563 2208 3.5 0
eAu: 1746 eAg: 1.4 eAs: 2594 eCu: 534 eZn: 143 eSb: 0 eBa: C eCt,. 0 eCo: 0 eNi: O eNi: O
e 1v : 0
Au: 490 Ag: .4 As: 728 Cu: 150 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: C Mo: 0 Ni: 0
W: o
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EÇEE eAu * EEEE Ag * rEEE eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N 22?2 eSb N 2222 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW .N
MAX
OIE B??fSTA(f 11
H-86-112
DEPARTURE(X) LATITUDE(Y) ELEUATION(1) O O O
09
FROM TO TYPE SS BEDROCK 120 125 80 10 150
PPM NON MAG PPM MAG VG 6049 1679 0 0
Au: 155 eAu: 933 Ag: .3 eAg: 1.8 As: 194 eAs: 1174 Cu: 75 eCu: 454 Zn: 64 eZn: 387 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: C Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE *'+. I N EEEE NM * EEEE MAG ;E ESEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
71d 401f87Rdf 11
H-86-112
DEPARTUREIXI LATITUDEIY) ELEJATIONIZ) 0 0 0
10
FROM TO TYPE SS BEDROCK 125 130 80 10 150
PPM NON MAG PPM MAG VG 2698 1492 2.5 0
eAu: 944 eAg: 1.1 eAs: 1015 eCu: 162 e?n: 108 eSb: C eBa: ~ eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: C
Au: 350 Ag: .4 As: 376 Cu: 60 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Sur-Face EEEE MIN EEEE NM * EEEE MAG -)E EEEE Au * EEEE eAu -)F EEEE Ag * EEEE eAg * EEEE As *** =rEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn -)E EEEE Sb N EEEE eS~ N 1111 Za N 1111 eFa N EEE- Cr N EEEE eCr N EEEE Co N XXXX eCo N XXX:t Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 72.5 Ag: .8 As: 0 Cu: 80 Zn: 90 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 19 eAg: .2 eAs: 0 eCu: 21 eZn: 24 eSb: 0 eBa: 0 eCr: 0 eCm: 0 eNi: 0 eNi: 0 eW: 0
HB pn1r~Tpfr .1
H-86-112
BEPARTURE(Xl LATITUBE(Yl ELEVATION(Z) 0 O O
11
FROM TO TYPE SS BEDROCK 130 133 80 10 150
PPM NON MAG PPM MAG VO 267 0 0 0
Sur-face EEEE MIN EEEE NM * EEEE MAO N EEEE Au * EEEE eAu * EEEE Ag ** EEEE eAg * EEEE As N EEEE eAs N EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIE AOMESIA..E II
H-86-113
DEPAR'UREI%1 LATITUDEIYI ELEUATIOMIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 39 45 60 10 105
PPM NON ''AG PPM MAG V3
1521 1371 0 C
Au: -" eAu: 5= A9:_- eAg: .1 As: C_? eAs: 485 Cu: 1:7 eCu: 224 Zn: 47 e_:-: : 60 Sb: C eSb: C Ba: C eBa: 0 Cr: C eCr: G Co: C eCo: 0 Mc: C e N i : 0 N:, C eNi: 0
W: C eW: C
Sur-face EEEE MIN EeEE -m •,t * EEEE - 3 * EEEE EEEE e - u * EEEE -9 * C0r0 e 5 * 0000 s *** E~EE E S * EEEE u * Er':E =__t * ErçE ~n * EEEE F,1 * EEEE :t N
N EcEE :a ErrE E=c. I'i EEEE :r N
N EEEE :o N XX>;X = :o N Y.XX;; 'o N
e D N N
t '; N W N :J N
Au: 3520 Ag: .05 As: 138 Cu: 96 Zn: 25 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 7868 eAg: .1 eAs: 308 eCu: 215 eZn: 56 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: O eNi: 0 eW: 0
anxrSTm :.'
H-86-113
BEoARTUREIXI LATITL'9EtT1 ELEYATION(Z) 0 O O
02-3
PROM TO TYPE SS BEDROCK 45 55 80 10 105
PPM NON MAO PPM MAG VG 2235 1010 .8 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au ** EEEE eAu * EEEE Ag * EEEE eAg * 1111 As * 1111 eAs * 1111 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eEa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 7.5 A9: .05 As: 565 Cu: 117 Zn: 22 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
eAu: 9 eAg: .1 eAs: 690 eCu: 143 eZn: 27 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
BlB Nn!!rgYAdE II
H-86-113
DEPARTUREIX) LATITUDE(Y) ELEVATION(Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 55 65 80 10 105
PPM NON MAG PPM MAG VG 1221 2854 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As ****HE EEEE eAs * 0000 Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 15 Ag: .05 As: 84 Cu: 121 Zn: 30 Sb: 0 Ba: O Cr: O Co: 0 Mo: O Ni: 0
W: O
eAu: 16 eAg: .1 eAs: 90 eCu: 129 eZn: 32 eSb: •0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
018 HOMME II
H-86-113
DEPlIRTUREIX) LATITUDEIY) ELEYATIOMIZ) D O O
05
FROM TO TYPE SS BEDROCK 65 71 80 10 105
PPM NON MAG PPM MAG VG 1067 1884 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * O000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr P. EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 20 Ag: .05 As: 250 Cu: 131 Zn: 64 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 66 eAg: 2 eAs: 826 eCu: 43: eZn: 212 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
0/8 ROAfSTAK: II
H-86-113
DEPARTUREiX) LATITUDEIY) ELEVATIOMIZ) 0 0 0
06
FROM TO TYPE SS BEDROCK 71 75 80 10 105
PPM NON MAG PPM MAG VO 3306 2137 0 0
Sur-face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb- N EEEE zSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
018 BOAfSTAIf II
H-86-113
DEPARTUREIXI LATITUDE(T) ELEUATIONIZ) 0 0 0
07
FROM TO TYPE SS BEDROCK 75 80 80 10 105
PPM NON MAO PPM MAG VO 5746 2381 0 0
Au: 230 eAu: 1322 Ag: .2 eAg: 1.1 As: 166 eAs: 954 Cu: 150 eCu: 862 Zn: 74 eZn: 425 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg ->F EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
011 SOMESTAIE II
H-86-113
DEPARTUREIXI LATITUBEIY} ELEVATION Ri 0 O 0
08
FROM TO TYPE SS BEDROCK 80 84 80 10 105
PPM NON MAG PPM MAG VG 2874 2442 0 0
Au: 145 eAu: 417 Ag: .2 eAg: .6 As: 179 eAs: 515 Cu: 100 eCu: 287 2n: 32 eZn: 92 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 `eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 115 Ag: .05 As: 167 Cu: 232 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O W: 0
eAu: J16 eAg: eAs: 459 eCu: 638 eZn: 66 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O1 B 8O!lES7AIE II
H-86-113
DEPARTUREIX) LATITUDEIY) ELEVATIDNIZ) 0 0 0
09
FROM TO TYPE SS BEDROCK 84 90 80 10 105
PPM NON MAG PPM MAG VG 2750 2600 0 0
Surf ace EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag 9E EEEE eAg -)E EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 20 Ag: .05 As: 51 Cu: 108 Zn: 26 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0
W: 0
eAu: 90 eAg: 2 eAs: eCu: 4ôô eZn: 1iâ eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
?II NONES?ARE II
H-86-113
DEPARTURE IX) LATITUDEtY1 ELEUATIOAtZ) 0 0 0
10
FROM TO TYPE SS BEDROCK 90 95 90 10 105
PPM NON MAO PPM MAO VG 4523 4649 0 0
Surface ELLE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * ELLE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu 9F EEEE Zn * EEEE eZn * ELLE Sb N EEEE eSb N çEçE Ba N 0000 eBa N 0000 Cr N ELLE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
d/B aOlEST4{E Il
H-86-113
DEPARTURE(X) LATITUDE(Y) ELEVATION(Z) 0 D 0
11
FROM TO TYPE SS BEDROCK 95 100 SO 20 105
1/2% PYRITE
PPM NON MAG PPM MAG VG ASPY 3169 2557 3.5 30
Au: 20 eAu: .~.3 Ag: .05 eAg: .2 As: 16 eAs: 51 Cu: 46 eCu: 146 Zn: 26 eZn: S2 Sb: ^ eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: Ç W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu 9E EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE e2n * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 2222 Cr N 2222 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 105 Ag: .05 As: 145 Cu: 176 Zn: 56 Sb: 0 Ba: C Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 545 eA9: .3 eAs: 753 eCu: 914 eZn: 291 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
01B P.ORfSTBF.f II
H-86-113
DEPARflDtEIXI UTITUDEIYI ELE4ATIDIiII) 0 0 0
12
FROM TO TYPE SS BEDROCK 100 105 80 20 105
PPM NON MAG PPM MAG VG 5191 3040 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs -IF EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEE2 Sb N ELLE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
018 00,0T4RI II
H-86-114
DEPARTURE(%) LATITUDE(YI ELEVATION(Z) 0 0 0
01-2
FROM TO TYPE SS BEDROCK 24 36 80 10 89
PPM NON MAG PPM MAG VG 2233 2185 .6 0
eAu: 391 eAg: .2 eAs: 1215 eCu: 239 eZn: 130 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
Au: 175 Ag: .1 As: 544 Cu: 107 Zn: 58 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E 1111 eAu * 1111 Ag * 1111 eAg * 1111 As **#** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 15 Ag: .05 As: 141 Cu: 92 Zn: 36 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
eAu: 28 eAg: .1 eAs: 261 eCu: 170 eZn: 67 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
^!d RORfSTAIf II
H-86-114
LEPARTUREI%) LATITUDE)Y) ELEVATIaNIZI a • o. a
03
FROM TO TYPE SS BEDROCK 36 40 80 10 89
PPM NON MAG PPM MAG VG 1853 1680 1.4 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu ;E EEEE Ag * EEEE eAg * 1111 As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEFE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O1B RORESIAIf I1
H-86-114
DEPARTUREiX) LATITUDE(T) ELEVATION(Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 40 45 80 10 89
PPM NON MAG PPM MAO VG 1471 1118 0 0
Au: 160 eAu: 235 Ag: .1 eAg: .1 As: 164 eAs: 241 Cu: 157 eCu: 231 Zn: 68 eZn: 100 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: C eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * 0000 As * 0000 eAs * 0000 Cu * EEEE eCu 9E EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 210 Ag: .05 As: 40 Cu: 39 Zn: 30 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 595 eAg: .1 eAs: 113 eCu: 111 eZn: 85 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
HF SOMME II
H-86-114
DEPARTUREtXI LATITUDEIYI ELEYATIONfZI 0 0 0
O5
FROM TO TYPE SS BEDROCK 45 49 80 10 89
PPM NON MAG PPM MAG VG 2835 2278 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs 9E 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn -)E EEEE Sb N EEEE eSb r! EEEE Ba M EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N X>:Y:X eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 20 Ag: .05 As: 72 Cu: 26 Zn: 21 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 35 eAg: .1 eAs: 125 eCu: 45 eZn: 36 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
?!B Nt'RfSTAdf II
H-86-114
DEPARTUREIX) LATITUDEIY) ELEVATIONIZ) 0 0 O
06-7
FROM TO TYPE SS BEDROCK 49 60 80 10 89
PPM NON MAG PPM MAG VG 1733 1565 0 0
Surface ESEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W .N eW N
MAX
011 NOAfSTp,ff II
H-86-114
DEPARTUREIX) LATITUDEITI ELEVATION(Z) 0 Q 0
08
FROM TO TYPE SS BEDROCK 60 64 80 10 89
IITS PYRITE
PPM NON MAG PPM MAG VG 2172 2217 6 0
Au: 140 eAu: 304 Ag: .05 eAg: .1 As: 52 eAs: 113 Cu: 67 eCu: 146 Zn: 24 eZn: 52 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE 2n * 5555 eZn * 5555 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 170 Ag: .2 As: 39 Cu: 116 Zn: 30 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 235 eAg: 3
eAs: 54 eCu: 161 eZn: 42 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Ser.rSrAKE I!
H-86-114
DEPARTUREtX1 LATITUDEtY1 ELE9ATIGN!Z) 0 0 0
09
FROM TO TYPE SS BEDROCK 64 70 80 10 89
PPM NON MAG PPM MAG VG 1385 1558 0 C
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu ?f EEEE Ag * EEEE eA9 * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXX X eCo N XXX.: Mo N
eMo N Ni N eNi N W N eW N
MAX
»I qOalsT,AF >•:
H-86-114
DEPARTURE(%) LATITUDE(Y) ELEVATION(Z) 0 0 0
10
FROM TO TYPE SS BEDROCK 70 73 80 10 89
PPM NON MAO PPM MAO VG 15098 19922 1.6 0
eAu: 2416 eA9: .8 eAs: 75 eCu: 2808 eZn: 664 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 160 Ag: .05 As: 5 Cu: 186 Zn: 44 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM ***E EEEE MAO **-IEdF***HE EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu *** EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 1090 Ag: .05 As: 105 Cu: 74 Zn: 26 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O W: 0
eAu: 4360 eAg: .2 eAs: 420 eCu: 296 eZn: 104 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 N00ES7A1E II
H-86-114
DEPARTUREIXI LATITUDEIYI ELEUATIONIZI 0 0 0
11
FROM TO TYPE SS BEDROCK 73 77 SO 10 89
JS PYRITE
PPM NON MAG PPM MAG VG ASPY 4000 3561 5 750
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 4444 Ba N 4444 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXY. Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 2.5 Ag: .2 As: 22 Cu: 99 Zn: 24 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 11 eAg: .9 eAs: 95 eCu: 429 eZn: 104 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
)1F RO!lESIAdE II
H-86-114
DEPARTUREIXI LATITUDEIYI ELEVATIONIZI 0 0 0
12
FROM TO TYPE SS BEDROCK 77 82 80 20 89
PPM NON MAG PPM MAG VG 4338 2987 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -3E EEEE A9 * EEEE eAg * EEEE As * EEEE eAs 9E EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
O!B ROxFSTA1rf Ir
H-86-114
DEPARTURE(X) LATITUDE(Y) ELEVATI6MIZ) 0 0 0
13
FROM TO TYPE SS BEDROCK 82 87 80 20 89
PPM NON MAG PPM MAG VG 4444 3778 0 C
eAu: 89 eAg: .2 eAs: 524 eCu: 1093 eZn: 173 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 20 Ag: .05 As: 118 Cu: 246 Zn: 40 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
718 P.OIfS1Aff II
H-86-114
DEPARTURE!%l LATITUDEIY) ELEVATION(Z) O 0 0
14
FROM TO TYPE SS BEDROCK 87 89 80 20 89
BOS P19Pllf
PPM NON MAG PPM MAG VG ASPY 7604 4144 2.9 230
Au: 345 eAu: 2623 Ag: .2 eAg: 1.5 As: 800 eAs: 6083 Cu: 226 eCu: 1718 Zn: 164 eZn: 1247 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM ** EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *****P* EEEE eAs ** EEEE Cu * EEEE eCu *E EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSt N EEEE Ea N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 40 Ag: .05 As: 97 Cu: 80 Zn: 68 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 20 eAg: 0 eAs: 49 eCu: 40 eZn: 34 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
013 RO!!ES?RdE II
H-86-115
DEPARTllRE1X) LATITUDEITI ELEYATIONIZ) 0 0 O
01-2
FROM TO TYPE SS BEDROCK 44 .55 80 10 93
PPM NON MAG PPM MAG VG 503 2231 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * 0000 eAs * 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Da N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
91F NOMESlA.►.E I!
H-86-115
DEPARTURE(X) LATITUDE(T) ELE9ATIDN(Z) 0 0 0
03-4
FROM TO TYPE SS BEDROCK 55 65 80 10 93
PPM NON MAG PPM MAG VG 3458 3106 .7 0
Au: 810 Ag: .05 As: 40 Cu: 30 Zn: 24 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs ?F EEEE Cu * 1111 eCu * 1111 Zn * 1111 eZn * EEEE Sb N EEEE eSb N EEEE Be. N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 2801 eAg: .2 eAs: 138 eCu: 104 eZn: 83 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
VI EMPARE II
H-86-115
DEPARTOE[XI D.ATITUDE{Y) EiEVATIDN(2) O o 0
05-6
FROM TO TYPE SS BEDROCK 65 75 80 10 93
PPM NON MAG PPM MAG VG ASPY 3650 3228 3.9 60
Au: 880 Ag: .05 As: 12 Cu: 24 Zn: 19 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 6666 eZn * 6666 Sb N 6666 eSb N 6666 Ba N SEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
'eW N
eAu: 3212 eAg: .2 eAs: 44 eCu: 88 eZn: 69 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
MAX
la RDPESTA[E 11
H-86-115
DEPARTUREIX) LATITUDEIYI ELEVATIOMIZI 0 0 0
07
FROM TO TYPE SS BEDROCK 75 80 80 10 93
J0 PYRITE GRAINS
PPM NON MAG PPM MAG VG ASPY 988 3967 6.6 60
Au: 160 eAu: 158 Ag: .05 eAg: 0 As: 15 eAs: 15 Cu: 16 eCu: 16 Zn: 16 eZn: 16 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 5555 Ba N 5555 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0/8 POPES74(E II
H-86-115
DEPARTURE(X) LATITUDE(T) ELEVATIOk(Z) 0 0 0
08
FROM TO TYPE SS BEDROCK 80 85 80 10 93
30 COARSE PYR17E BRAINS
PPM NOM MAG PPM MAG VG ASPY 6532 5316 8.1 300
Au: 3160 eAu: 20640 Ag: .1 eAg: .7 As: 37 eAs: 242 Cu: 56 eCu: 366 Zn: 22 eZn: 144 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu *# EEEE Ag * EEEE eAg * EEçç As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE £a N 6666 eBa N 6666 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0!P A48E5741É II
H-86-115
DEPARTUREIXI LATITUDE(Y1 ELEVATIOMiZI 0 0 0
09
FROM TO TYPE SS BEDROCK 85 91 80 20 93
PPM NON MAG PPM MAG VG 2506 1586 0
Au: 155 eAu: 388 Ag: .1 eAg: .3 As: 248 eAs: 621 Cu: 91 eCu: 228 Zn: 28 eZn: 70 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
'13 MESURE II
H-86-115
DEPARTUREIX) LATITUDEIYI ELEVATIOR12) 4 0 0
10
FROM TO TYPE SS BEDROCK 91 93 80 20 93
PPM NON MAG PPM MAG VG 3310 2391 1.8 0
eAu: 1572 eAg: .2 eAs: 0 eCu: 314 eZn: 182 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 475 Ag: .05 As: O Cu: 95 Zn: 55 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni : 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As N EEEE eAs N EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XX"X eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0I8 90!lESTAdE II
H-86-116
DEPARTUREIX7 LATITUDEIY1 ELEYATIONIZ1 0 0 0
01
FROM TO TYPE SS BEDROCK 18 25 80 10 120
PPM NON MAG PPM MAG VG 2653 2246 1.1 0
eAu: 358 eAg: .1 eAs: 1846 eCu: 448 eZn: 318 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 135 Ag: .05 As: 696 Cu: 169 Zn: 120 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * 1111 MAG * 1111 Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
OIE 94RESTA,(E 17
H-86-116
DEPARTUREIXI LATITUDEIYI ELEVATIONIZI D a o
02
FROM TO TYPE SS BEDROCK 25 35 80 10 120
PPM NON MAG PPM MAG VG 2611 2077 1.1 0
Au: 120 eAu: 313 Ag: .1 eAg: .3 As: 282 eAs: 736 Cu: 102 eCu: 266 Zn: 72 eZn: 188 Sb: 0 eSb: 0 Ba: 0 eBa: O Cr: 0 eCr: 0 Co: 0 eCo: 0 Mc: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * 1111 Au * 1111 eAu * EEEE Ag * EEEE eAg * EEEE As *# EEEE eAs * EEEE Cu * EEEE eCu * LEE! Zn * EEEE eZn -X- LEE! Sb .N EEEE _S5 N EEEE Ba N ELLE eBa N EEEE Cr N EEEE eCr N EEEE Co N XX;;X eCo N XXXY, Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 170 Ag: .05 As: 230 Cu: 115 Zn: 136 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: C Ni: 0 W: 0
eAu: 478 eAg: .1 eAs: 647 eCu: 323 eDn: 382 eSb: C eBa: G eCr. 0 eCn: 0 eNi: 0 eNi: 0 eW: C
O!3 HO!lES7AIE II
H-86-116
DEPARTUREIX) LATITUDEfY) ELE4ATIDNIZ) 0 0 0
03
FROM TO TYPE SS BEDROCK 35 45 80 10 120
PPM NON MAS PPM MAC, VO 2512 2007 0 0
Surf ace EEEE MIN C=EC NM * EEEE MAS ?E EEEE Au * 0000 eAL * 0000 Ag * 0000 eAg * EEEE As *HE EEEE eAs )F EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn -)E SEçn- Sb N EI=EE eSb N EEEE Ba N EEEE eJa N EEEE N EEEE eCr N EEEE Co N X`:; ! eCc N X::= 'Sa N
eMo N Ni N eNi N W N eW N
MAX
O!? °O)!rgM, II
H-86-116
DEPARTUREI%) LATITUDEIT) ELEilATI0Ni2) 0 0 0
04
FROM TO TYPE SS BEDROCK 45 55 80 10 120
PPM NON MAO PPM MAG VG 2337 1633 1.2 0
Au: 110 eAu: 257 Ag: .1 eAg: .2 As: 87 eAs: 203 Cu: 99 eCu: 2:1 Zn: 48 eZn: 112 Sb: 0 eSb: 0 Ba: 0 eBa: O Cr: C eCr: 0 Co: 0 eCo: C Mo: 0 eNi: 0 Ni: 0 eNi: C W: 0 e4i: 0
Surface EEEE MIN EEEE NM * EEEE MAC * EEEE Au * SEEE =.^,u * EEEE Ag * 1 1 1 1 e A g *
As * '1'1 eAs * EEEE Cu * EEE'= eCu * EcçE Zn * EEEE zZn * EEEE Sb N EEEE eçb N EE
-m. Ba N EEEE eBa N EEEE Cr N EEEE eCr N SEEE Co N X;::!X eCo N XXXX Mo N
eMû N Ni N
eNi N W N
eW N
MAX
prg 90f1reTASf I1
H-86-116
DEPARTURECX) LATITUEEfY: ELEVATIO!iIZ) 0 0 0
05
FROM TO TYPE SS BEDROCK 55 64 80 10 120
PPM NON MAO PPM MAO VG 3353 3883 1 0
Au: 15 eAu: 50 Ag: .05 eAg: .2 As: 82 eAs: 275 Cu: 115 eCu: 386 Zn: 36 eZn: 121 Sb: C eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * ELLE As * . 1 1 1 i eAs * illi Cu ~ EE2_ 24u * EErE Zn * EEEE eZn * EEEE Sb N
LEE: Be. N EELS _Ba. N EEEE Cr N SEES eCr N EEEE Co N `:XX eCo N XXXX Ma N
eMo N Ni N eNi N W N eW N
MAX
Au: 15 Ag: .05 As: 157 Cu.: 121 Zn: 40 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 41 eAg: 1 aAs: 427 eCu: 329 eZn: 109 eSb: eBa: 0 eCr J eCo: 0 eNi: 0 eNi: 0 eW : 0
prn anrresilfr Zr
H-86-116
CEPARTURE(XJ LATITL'CE(YJ EIEti'ATICJI(II 0 0 0
06
FROM TO TYPE SS BEDROCK 64 70 80 10 120
PPM NON MAO PPM MAO VG 2722 2375 0 0
Surface EEE- MIN EEEE NM * EEEE MAO * EEEE AL * EEEE aAu * EEEE Ag * EFEE =Ag -IF Er.Eç As x FEEr eAs * 0000 Cu x 0000 eCu ?E EEEE Zr * EEEE e3i, * EEEr ,t N EEEE a -~ n,
EEFE ?'a. ç`=` `'i
FE=L Cr N EEEE eCr• N EEE;:- Co N XY.`<Y BCD N .;:",= Mo N
e,MO N Ni N eNi N W N eW N
MA::
7/e pnIrçrp{f ?.
H-86-116
TEPARTURE(X) LATITU:E(Y) ELEVATICN;Z: C 0 0
07
FROM TO TYPE SS bE2RùC:: 75 60 10 I20
PPM NON MAG PPM MAG VG 3347 J 12û 0 V
Au: 15 eAu: 50 Ag: .05 eAg: .2 As: 187 eAs: 626 Cu: 110 eCu: 368 Zn: 34 eZn: 114 Sb: 0 eSb: 0 Ba: 0 era: O Cr: 0 eCr: O Co: 0 eCo: 0 Mo: 0 eNi: O Ni: 0 eNi: 0
W: _ eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zr. * EEEE eZn * EEEE 3b N EEEE eSb N EEEr Ba N
MAX
e rL a N EEEE Cr. ') EEEE eCs, N EEEE Co N X::;CX eCo N ::X:::: Mo N
eMo N Ni N
eNi N W N eW N
Au: 15 A3: .05 As: 153 Cu: 212 Zn: 36 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni : 0 W: 0
eAu: 47 eAg: .2 eAs: 477 eCu: 661 eZn: 112 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
nrn gnmrrf•Âf i1
H-86-116
DEPARTURE!%) LATITL'9E{Y) ELEVATIOtI(Z1 a o o
os
FROM TO TYPE SS BEDROCK 75 SO SO IC. 120
PPM NON MAG PPM NAG VG 3120 2213 0 0
Surf ace
EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu *
EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * E=rE: eCu * 0000 Zn * 0000 eZn * EEEE Sb N ESSE eSb N EEEE Ba N EEEE eBa N EEEE Cr N çEEç eCr N EEEE Cc N XXXX eCo N :.,,~
,.,: , Mo N eMo N Ni N eNi N W N eW N
MAX
Au: 150 Ag: .05 As: 52 Cu: 71 Zn: 36 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 366 eAg: .1 eAs: 127 eCu: 173 eZn: 88 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
0/B BO!lfSTAdf 11
H-86-116
DEPARTUREIXI UITITUDEiV) ELE9ATIOlIIZ) 0 0 0
09
FROM TO TYPE SS BEDROCK 80 85 80 10 120
PPM NON MAG PPM MAG VG 2440 2973 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
0/8 AOMFSTAIf II
H-86-116
DEPARTUREIX) LATITUDEIT) ELEVATIONIZI 0 0 0
10
FROM TO TYPE SS BEDROCK 85 90 80 10 120
PPM NON MAG PPM MAO VG 3644 3067 1.8 0
eAu: 2004 eAg: .2 eAs: 211 eCu: 405 eZn: 87 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 550 Ag: .05 As: 58 Cu: 111 Zn: 24 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: O
Surf ace EEEE MIN EEEE NM 9E EEEE MAO * EEEE Au if-. EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
011 NON:S7Adf 11
H-86-116
DEPARTUREIXI LATITUDEIYI ELE9ATIONIZ1 O 0 0
11
FROM TO TYPE SS BEDROCK 90 95 80 10 120
PPM NON MAG PPM MAO VG 2318 2409 0 0
eAu: 556 eAg: .5 eAs: 1345 eCu: 408 eZn: 148 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: O eW: 0
Au: 240 Ag: .2 As: 580 Cu: 176 Z n : 64 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
ME SOOESTA,lE 11
H-86-116
DEPARTtD2EtX) LATITUDEIY) ELEUATIONiZ) 0 O 0
12
FROM TO TYPE SS BEDROCK 95 100 80 10 120
PPM NON MAG PPM MAG VG 3063 1766 0 0
eAu: 965 eAg: .3 eAs: 1470 eCu: 417 eZn: 184 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: C eNi: C eW: 0
Au: 315 Ag: .1 As: 480 Cu: 136 Zn: 60 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** +EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 000C Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
011 IOMESTAIE II
H-86-116
6EPARTURE(XI-LATITUDE(Y) ELEVATION(2) O 0 0
13
FROM TO TYPE SS BEDROCK 100 105 80 10 120
PPM NON MAG PPM MAG VG 2866 3050 0 0
eAu: 688 eAg: .9 eAs: 1399 eCu: 496 eZn: 241 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 240 Ag: .3 As: 488 Cu: 173 Zn: 84 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N O000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
h
DlB p,O!!fS7Adf 11
H-86-116
1EPARTURE(X) LATITUDE(Y) ELE4ATIOM(Z1 O O O
14
FROM TO TYPE SS BEDROCK 105 110 80 10 120
PPM NON MAG PPM MAG VG 3225 2505 1.4 0
Au: 35 Ag: .05 As: 344 Cu: 191 Zn: 80 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: O W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 1111 eBa N 1111 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
eAu: 113 eAg: .2 eAs: 1109 eCu: 616 eZn: 258 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Au: 130 Ag: .05 As: 186 Cu: 210 Zn: 52 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 585 eAg: .2 eAs: 837 eCu: 945 eZn: 234 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Of! MUTAI! II
H-86-116
DEPABTIUtEIXI LATITUDEIYI ELEVATIDAIZI 0 0 0
15
FROM TO TYPE SS BEDROCK 110 115 80 20 120
!SS REITF 1 61M 6ALERA
PPM NON MAG PPM MAG VG ASPY 4500 1606 3.6 100
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au .)I. EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 3333 Cr N 3333 eCr N EEEE Co N XXY' eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 30 Ag: .05 As: 176 Cu: 131 Zn: 50 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 74 eAg: .1 eAs: 433 eCu: 323 eZn: 123 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIS B0AES74IE II
H-86-116
DEPARTUREIx) LATITUDEIYI ELEVATIOMII) e o a
16
FROM TO TYPE SS BEDROCK 115 118 80 20 120
PPM NON MAG PPM MAG VG 2463 2384 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
018 SOAfS7AdF II
H-86-116
DEPARTURE(X1 LATITUDE(Y1 ELEYATION(Z1 0 0 0
17
FROM TO TYPE SS BEDROCK 118 120 80 20 120
PPM NON MAG PPM MAG VG 5111 4741 0 0
eAu: 102 eAg: .3 eAs: 1007 eCu: 1380 eZn: 450 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 20 Ag: .05 As: 197 Cu: 270 Zn: 88 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/3 BDMES?Adf II
H-86-117
DEPARTUREIXI LATITUDEIYf ELEYATIONIZ) O O O
01
FROM TO TYPE SS BEDROCK 50 60 80 10 86
PPM NON MAO PPM MAG VG 4119 3733 0 0
eAu: 885 eAg: .8 eAs: 1944 eCu: 642 eZn: 280 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 215 Ag: .2 As: 472 Cu: 156 Zn: 68 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *-3E** EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 235 Ag: .05 As: 0 Cu: 140 Zn: 48 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 735 eAg: .2 eAs: 0 eCu: 438 eZn: 150 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: O
7JF BOME57Artf 11
H-86-117
DEPARTURE)X) LATITUDEIY) ELEVATIONtZ) 0 O O
02
FROM TO TYPE SS BEDROCK 60 65 80 10 86
PPM NON MAG PPM MAG VG 3126 1639 0 0
Surf ace EEEE MIN EEEE NM 9(- EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As N EEEE eAs N EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N Y.XXY, Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 210 Ag: .05 As: 95 Cu: 123 Zn: 42 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 894 eAg: .2 eAs: 404 eCu: 524 eZn: 179 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 .90!lfS1AKf II
H-86-117
JEPARTUREIX) LATITUDEITI ElEVATIOKIZI O O O
03
FROM TO TYPE SS BEDROCK 65 75 80 10 86
PPM NON MAG PPM MAO VG 4256 3624 0 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb • N 0000 eSb N 0000 Ba N 0000 eSa N EEEE Cr N EEEE eCr N EEEE , Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 315 Ag: .05 As: 29 Cu: 103 Zn: 28 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 982 eAg: .2 eAs: 90 eCu: 321 eZn: 87 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
Olr NOMME II
H-86-117
DEPARTUREiXI LATITUDEfY1 ELEVATIONiZ1 O O D
04
FROM TO TYPE SS BEDROCK 75 86 80 20 86
PPM NON MAO PPM MAO VG 3117 2739 0 O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/3 10RESThKf 11
H-86-118
DEPARTURE)Xl LATITUDE{Y) ELEVATION(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 43 50 80 10 126
PPM NON MAG PPM MAO VG 3638 2667 1.3 0
eAu: 673 eAg: .2 eAs: 1397 eCu: 353 eZn: 146 eSb: O eBa: O eCr: O eCo: 0 eNi: 0 eNi: O eW: 0
Au: 185 Ag: .05 As: 384 Cu: 97 Zn: 40 Sb: O Ba: O Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * 1111 Ag * 1111 eAg * EEEE As *E* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX MO N
eMo N. Ni N
eNi N W N
eW N
MAX
Au: 1075 Ag: .1 As: 240 Cu: 71 Zn: 30 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 2212 eAg: .2 eAs: 494 eCu: 146 eZn: 62 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/3 RORES7ALE II
H-86-118
IEPARTUREIX) LATITUDEIYI ELEVATIONIZI 0 O O
02
FROM TO TYPE SS BEDROCK 50 59 80 10 126
PPM NON MAG PPM MAG VG 2058 1564 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * 0000 eAg * 0000 As ** 0000 eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 20 Ag: .05 As: 27 Cu: 13 Zn: 16 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: O W: 0
eAu: 54 eAg: .1 eAs: 73 eCu: 35 eZn: 43 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
018 1010TAdf 11
H-86-118
DEPARTUREIXf LATITUDEfYf ELEVATIDMfZ)
03
FROM TO TYPE SS BEDROCK 59 65 60 10 126
PPM NON MAO PPM MAG VG 2709 56 1.1 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * 1111 eAs * 1111 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 65 Ag: .05 As: 8 Cu: 8 Zn: 12 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0 W: O
eAu: 139 eAg: .1 eAs: 17 eCu: 17 eZn: 26 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
O!d NOMME II
H-86-118
BEPARflIREIR) LATITt1DE(Y1 ELEVATIONIZ1 D O O
04
FROM TO TYPE SS BEDROCK 65 68 60 10 126
PPM NON MAG PPM MAG VG 2142 142 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * 0000 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
1/3 1011S741f 11
H-86-118
DEPARTUREIXI LATITUDEITI ELEYATIOMIZI 0 0 0
05
FROM TO TYPE SS BEDROCK 68 75 80 10 126
PPM NON MAG PPM MAG VG 1961 800 0 0
Au: 45 eAu: 88 Ag: .05 eAg: .1 As: 13 eAs: 25 Cu: 39 eCu: 76 Zn: 16 eZn: 31 Sb: O eSb: 0 Ba: O eBa: 0 Cr: O eCr: O Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: O
Surface EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au ;E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * O000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 35 Ag: .1 As: 151 Cu: 79 Zn: 32 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: 0
eAu: 190 eAg: .5 eAs: 819 eCu: 428 eZn: 174 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: O eW: 0
0/P BOIJfS7Adf II
H-86-118
DEPARTUREIXI LATITUDEIYI ELEYATIfl11IZ1 0 0 0
06
FROM TO TYPE SS BEDROCK 75 80 80 10 126
PPM NON MAG PPM MAG VG 5422 4104 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As . * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
O/D 3011ESTI1,TE 11
H-86-118
IEPARTUREIXI LATITUDE(Y) ELEVATIOMII) 0 0 0
07
FROM TO TYPE SS BEDROCK 80 85 80 10 126
PPM NON MAG PPM MAG VG 2519 1900 0 0
Au: 195 eAu: 491 Ag: .05 eAg: .1 As: 146 eAs: 368 Cu: 83 eCu: 209 Zn: 28 eZn: 71 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
OIE IOM(STA1E II
H-86-118
DEPARTUREIXI LATITUOEITI ELEYATIONIZI O O O
08
FROM TO TYPE SS BEDROCK 85 90 80 10 126
PPM NON MAO PPM MAG VG 3231 2808 0 0
Au: 160 eAu: 517 Ag: .4 eAg: 1.3 As: 134 eAs: 433 Cu: 99 eCu: 320 Zn: 46 eZn: 149 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: 0 eNi: O Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Oil 90qESTAfE II
H-86-118
DEPARTURE(X) LATITUDE(YI ELE9AT10N(Z) 0 0 0
09
FROM TO TYPE SS BEDROCK 90 95 80 10 126
PPM NON MAO PPM MAO VG 3359 2251 0 0
Au: 390 eAu: 1310 Ag: .3 eAg: 1 As: 292 eAs: 981 Cu: 151 eCu: 507 Zn: 42 eZn: 141 Sb: O eSb: O Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: O Mo: O eNi: 0 Ni: 0 eNi: 0
W: O eW: O
Surf ace EEEE MIN EEEE NM 9E EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eA9 * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn - * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OJR RORES7AlE II
H-86-118
DEPARTURE(X) LATITULE(Y) ELEVATION(Z) O 0 0
10
FROM TO TYPE SS BEDROCK 95 100 80 10 126
PPM NON MAG PPM MAG VG 4114 3295 O O
Au: 10 eAu: 41 Ag: .1 eAg: .4 As: 272 eAs: 1119 Cu: 120 eCu: 494 Zn: 40 eZn: 165 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 70 Ag: .6 As: 2000 Cu: 472 Zn: 58 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
eAu: 413 eA9: 3.5 eAs: 11789 eCu: 2782 eZn: 342 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
0/1 BOA£STAIE II
H-86-118
DEPARTUREIX) LATITUDEIY) ELEYATIOIlIZI O D O
11
FROM TO TYPE SS BEDROCK 100 103 80 10 126
30% PY 100 PELLETS AARC
PPM NON MAG PPM MAG VG ASPY 5895 2930 0 30
Surface EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *HE* EEEE As *iE#iEdE**-lF*HE*E#-lE****3E EEEE eAs ***HF* EEEE Cu * EEEE eCu *** EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
011 S000T IE 11
H-86-118
DEPARTUREIXI LATITUDEIYI ELEVATIONIZI 0 0 0
12
FROM TO TYPE SS BEDROCK 103 105 80 10 126
PPM NON MAG PPM MAG VG 4700 2865 0 0
Au: 30 eAu: 141 Ag: .4 eAg: 1.9 As: 912 eAs: 4286 Cu: 177 eCu: 832 Zn: 88 eZn: 414 Sb: O eSb: 0 Ba: O eBa: O Cr: O eCr: 0 Co: O eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *******#* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
e/3 9.^AfSTAU 17
H-86-118
IEPARTUREI%) LATITUDEIYI ELEVATIONIZI 0 0 0
13
FROM TO TYPE SS BEDROCK 110 115 80 10 126
PPM NON MAO PPM MAG VO 4746 2552 0 0
Au: 70 eAu: 332 Ag: .4 eAg: 1.9 As: 632 eAs: 2999 Cu: 238 eCu: 1129 Zn: 190 eZn: SCU2 Sb: O eSb: O 3a: aBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: O eNi: O iJ: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg 9E EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu 9E EEEE Zn * EEEE e2n * EEEE Sb N EEEE eSb N EEEE Ba N O000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
013 BOAfSTA,fE ll
H-86-119
NPARTURE(XI LATITUBE(YI ELEVATIB((ZI 0 0 0
14
FROM TO TYPE SS BEDROCK 115 120 80 10 126
PPM NON MAG PPM MAG VG 6535 2658 0 0
eAu: 1078 eAg: 3.9 eAs: 4653 eCu: 1235 eZn: 1019 eSb: O eBa: O eCr: 0 eCo: 0 eNi: O eNi: 0
eW: O
Au: 165 Ag: .6 As: 712 Cu: 189 Zn: 156 Sb: O Ba: O Cr: O Co: 0 Mo: 0 Ni: O
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *** EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
DIB 90!lESTAdE II •
H-86-118
'PARME (X) LATITUDE( Y) ELEVATIOlI(1) 0 0 0
15
FROM TO TYPE SS BEDROCK 115 120 80 20 126
PPM NON MAG PPM MAG VG 5240 1933 0 0
Au: 220 Ag: .5 As: 848 Cu: 179 Zn: 160 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg *JE EEEE As ******** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
eAu: 1153 eAg: 2.6 eAs: 4444 eCu: 938 eZn: 838 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
MAX
Old BO/07Adf II
H-86-118
BEPARTIIBE(X) LATITU9E,(T) ELEVATION(D 0 0 0
16
FROM TO TYPE SS BEDROCK 120 122 80 20 126
PPM NON MAG PPM MAG VG 4174 1706 0 0
eAu: 355 eAg: 1.3 eAs: 2070 eCu: 793 eZn: 685 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 85 Ag: .3 As: 496 Cu: 190 Zn: 164 Sb: O Ba: 0 Cr: O Co: O Mo: 0 Ni: 0
W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *-IF** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
D/D 90RESIALE 11
H-86-118
1EPARTURE(X) LATITUDE(Y) ELEVATIOMIZI 0 O 0
17
FROM TO TYPE SS BEDROCK 122 124 80 20 126
PPM NON MAG PPM MAO VG 5072 1667 0 0
eAu: 2283 eAg: 1 eAs: 3287 eCu: 1202 eZn: 751 eSb: O eBa: O eCr: 0 eCo: 0 eN i : 0 eNi: 0
eW: O
Au: 450 Ag: .2 As: 648 Cu: 237 Zn: 148 Sb: O Ba: O Cr: O Co: 0 Mo: 0 Ni: O
W: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **9F*IE* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Old dORES7AIE II
H-86-118
DEPARTURE(X) LATITUDE(Y) ELEYATIOM(Z) 0 0 0
18
FROM TO TYPE SS BEDROCK 124 126 80 20 126
PPM NON MAG PPM MAG VG 9841 2286 0 0
Au: 15 eAu: 148 Ag: 1.1 eAg: 10.8 As: 1216 eAs: 11967 Cu: 257 eCu: 2529 Zn: 176 eZn: 1732 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: 0
W: O eW: 0
Surface EEEE MIN EEEE NM ** EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg ********** EEEE As *IE**HE9HHF*E** EEEE eAs ***** EEEE Cu * _EEEE eCu *** EEEE Zn * EEEE eZn *HE EEEE Sb. N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
O/d dOBESTArTE II
H-86-119
DEPARTUREIXI LATITUDElT1 ELEVATIDRIZI 0 0 0
01
FROM TO TYPE SS BEDROCK 25 30 80 10 60
9O% PYRITE
PPM NON MAG PPM MAG VO 40889 1778 2.5 0
Au: 15 eAu: 613 Ag: .3 eAg: 12.3 As: 248 eAs: 10140 Cu: 246 eCu: 10059 Zn: 120 eZn: 4907 Sb: 0 eSb: 0 Ba: O eBa: 0 Cr: O eCr: 0 Co: O eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM ************ EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg 1111 As ** 1 1 1 1 eAs **** 1111 Cu * EEEE eCu ********X X 1EX EEEE Zn * EEEE eZn ****** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Old OOMESThKE 11
H-86-119
1#PARTUREIX) LATITUIE(Y) ELEVATION(Z) o a o
02
FROM TO TYPE SS BEDROCK 30 35 80 10 60
PPM NON MAG PPM MAG VG 4119 2476 0 0
eAu: 700 eAg: .2 eAs: 1038 eCu: 400 eZn: 107 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 170 Ag: .05 As: 252 Cu: 97 Zn: 26 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
018 80107qKF II
H-86-119
IEPARTIptEfX! LATITU9EfTl ELEVATIUMf1l 0 0 0
03
FROM TO TYPE SS BEDROCK 35 40 80 10 60
PPM NON MAG PPM MAG VG 3785 2258 0 0
Au: 50 eAu: 189 Ag: .1 eAg: .4 As: 226 eAs: 855 Cu: 131 eCu: 496 Zn: 28 eZn: 106 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: O Co: O eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0
W: O eW' 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *HF EEEE eAs -I(- EEEE Cu * 0000 eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
ar! RORfS7Btf il
H-86-119 àEPARTiOtEIX) LATIT!)DEIT) ELEVATIONI2)
0 0 0
04
FROM TO TYPE SS BEDROCK 40 45 80 10 60
PPM NON MAG PPM MAG VG 4000 2930 0
Au: 30 Ag: .05 As: 276 Cu: 119 Zn: 30 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * O000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
eAu: 120 eAg: .2 eAs: 1104 eCu: 476 eZn: 120 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
MAX
0!! AOAfSTI)dE II
H-86-119
DEPARTURE(Xi LATITUDE(Y1 ELEVATIOM(Z) . 0 O 0
05
FROM TO TYPE SS BEDROCK 45 50 80 10 60
PPM NON MAG PPM MAG VG 3082 2026 0 0
eAu: 247 eAg: .9 eAs: 1190 eCu: 287 eZn: 96 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Au: 80 Ag: .3 As: 386 Cu: 93 Zn: 31 Sb: 0 Ba: 0 Cr: O Co: O Mo: 0.
Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 85 Ag: .05 As: 162 C u : 72 Zn: 19 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 255 eAg: .2 eAs: 487 eCu: 216 eZn: 57 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
013 40RE3741f II
H-86-119
DEPARTUREIX) LATITUDE(C) ELEVATI0N(Z) 0 0 0
06
FROM TO TYPE SS BEDROCK 50 55 80 20 60
PPM NON MAG PPM MAG VG 3004 1991 0 0.
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9E EEEE eCu * EEEE Zn 9f EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N. W N eW N
MAX
Au: 120 Ag: .05 As: 109 Cu: 131 Zn: 20 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: O
eAu: 407 eAg: .2 eAs: 370 eCu: 445 eZn: 68 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
OIE POMESTUE II
H-86-119
9EEPARTURE(XI LATITUBE(YI ELEVATI01i(2) 0 O 0
07
FROM TO TYPE SS BEDROCK 55 60 80 20 60
PPM NON MAG PPM MAG VG 3394 2130 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu 9P EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N 0000 Co N XXXY. eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
9/9 B0dE57AgE 11
H-86-120
DEPARTURE(X1 LATITUEE(Y) ELEVATIUB(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 64 74 80 10 130
PPM NON MAO PPM MAG VG 4870 3667 0 0
Au: 65 Ag: .1 As: 2000 Cu: 123 Zn: 36 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 317 eAg: .5 eAs : 9741 eCu: 599 eZn: 175 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Surface EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *9E*HHHE*******X X 1EX X 0000 eAs **** O000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
Old 803ES7A[E I1
H-86-120
lEPARTUREIXI LATITUOE{Yl ELEVATION(Z) 0 O O
02
FROM TO TYPE SS BEDROCK 74 80 80 10 130
PPM NON MAG PPM MAG VG 3884 3266 0 0
Au: 10 eAu: 39 Ag: .05 eAg: .2 As: 20 eAs: 78 Cu: 92 eCu: 357 Zn: 26 eZn: 101 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O eNi: 0 Ni: O eNi: 0 W: 0 eW' 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O/I SOMME II
H-86-120
DEPARTURE(X) LATITUDE(Yi ELEVATION(Z) 0 0 0
03
FROM TO TYPE SS BEDROCK 80 84 80 10 130
PPM NON MAG PPM MAG VG 3135 4180 0 0
eAu: 94 eAg: 1.3 eAs: 865 eCu: 426 eZn: 1630 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: O eW: 0
Au: 30 Ag: .4 As: 276 Cu: 136 Zn: 520 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * EEEE eZn *E EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 2720 Ag: .05 As: 768 Cu: 110 Zn: 27 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 166827 eAg: 3.1 eAs: 47104 eCu: 6747 eZn: 1656 eSb: O eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
OIE BOBËSTAutE II
H-86-120
lEPARTUREIXI LATITUDEIYI ELEYATIOMIZI 0 0 0
04
FROM TO TYPE SS BEDROCK 84 90 80 10 130
PPM NON MAG PPM MAS VG 61333 45867 21.3 0
Surface EEEE MIN MAX EEEE NM ****************** EEEE MAG lE*HE3E****HE*HEX X X1 EEEE Au * EEEE eAu iE**IE*iHHF*iHHHE**HFiHE* EEEE Ag * EEEE eAg ** EEEE As aHE***jHF EEEE eAs ******-1F*HHHE***-IE*#*HE EEEE Cu * EEEE eCu ******** 1111 Zn * 1111 eZn ** EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
Au: 95 Ag: .05 As: 22 Cu: 34 Zn: 15 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: O
eAu: 278 eAg: .1 eAs: 64 eCu: 100 eZn: 44 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: O eW: O
411 s4RESTAIE II
H-86-120
lEPARTUREfxI LATITUDEfTI ELEVATIOMlZI 0 0 0
05
FROM TO TYPE SS BEDROCK 90 95 80 IO 130
PPM NON MAG PPM MAG VG 2930 3358 0 0
Surface EEEE MIN EEEE NM * EEEE MAG 9E EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 45 Ag: .05 As: 74 Cu: 19 Zn: 13 Sb: 0 Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 176 eAg: .2 eAs: 290 eCu: 75 eZn: 51 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
O/D 9001S7AlE II
H-86-120
DEPARTURE(X) LATITUDE(YI ELEVATIOM(Z1 0 0 0
06
FROM TO TYPE SS BEDROCK 95 100 80 10 130
PPM NON MAG PPM MAG VG 3922 3686 1.3 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 1111 Sb N 1111 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 60 Ag: .05 As: 103 Cu: 75 Zn: 26 Sb: 0 Ba: O Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 200 eAg: .2 eAs: 343 eCu: 250 eZn: 87 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Of; BORESIALE II
H-86-120
DEPARTUREIXI LATITUDEIYI ELEiIATIONIZI 0 0 0
07
FROM TO TYPE SS BEDROCK 100 105 80 10 130
PPM NON MAO PPM MAG VG 3333 3220 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE e2n 9E EEEE Sb N O000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 90NESTAIE ll
H-86-120
IEPARTUREIX) LATITUDEIY) ELEVATION(I) 0 o a
Os
FROM TO TYPE SS BEDROCK 105 110 80 10 130
PPM NON MAG PPM MAO VG 3867 4057 0 0
eAu: 116 eAg: 1.2 eAs: 294 eCu: 336 eZn: 124 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 30 Ag: .3 As: 76 Cu: 87 Zn: 32 Sb: O Ba: 0 Cr: 0 Co: O Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE A9 * EEEE eAg -)E EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn 9E EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Old IOMESMAE( II
H-86-120
lEPARTUREf%) LATITUHEIY) ELEVATIOMi23 0 0 0
09
FROM TO TYPE SS BEDROCK 110 114 80 10 130
PPM NON MAG PPM MAO VG 4176 3392 0 0
Au: 40 eAu: 167 Ag: .2 eAg: .8 As: 448 eAs: 1871 Cu: 329 eCu: 1374 Zn: 198 eZn: 827 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: O eNi: O Ni: 0 eNi: 0 W: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N O000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
011 BOIIESTAIE II
H-86-121
DEPARTUREIX) LATITUDEIT) ELEVATI011111 0 0 0
01
FROM TO TYPE SS BEDROCK 63 74 80 10 128
PPM NON MAG PPM MAG VG 3117 3879 0 0
Au: 105 Ag: .2 As: 2000 Cu: 156 Zn: 64 Sb: 0 Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 327 eAg: .6 eAs: 6234 eCu: 486 eZn: 199 eSb: 0 eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: 0
Surface EEEE MIN MAX EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As **************jHF*** 0000 eAs ** 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
Au: 15 Ag: .5 As: 282 Cu: 143 Zn: 46 Sb: O Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 49 eAg: 1.6 eAs: 924 eCu: 468 eZn: 151 eSb: 0 eBa: O eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
011 BOAfSTAdF II
H-86-121
DEPARTtiREIXI LATITI)DEtYI ELEYATI1hitZ) 0 0 0
02
FROM TO TYPE SS BEDROCK 74 80 80 10 128
PPM NON MAG PPM MAG VG 3276 4305 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 75 Ag: .4 As: 139 Cu: 92 Zn: 38 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: O W: 0
eAu: 243 eAg: 1.3 eAs: 451 eCu: 298 eZn: 123 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Oti BOBESTAIE II
H-86-121
IEPARTUREIX) LATITUDEIY) ELEVATIOMiZ) 0 0 O
03
FROM TO TYPE SS BEDROCK 80 89 80 10 128
PPM NON MAG PPM MAG VG 3243 1964 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs 9E EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
011 BOAFSTALf II
H-86-121
BEPARTORE(X1 LATIT(1nE(TI ELEYATION(21 0 0 0
04
FROM TO TYPE SS BEDROCK 89 99 80 10 128
PPM NON MAG PPM MAG VG 3863 .2889 0 0
eAu: 251 eAg: .8 eAs: 93 eCu: 344 eZn: 62 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 65 Ag: .2 As: 24 Cu: 99 Zn: 16 Sb: O Ba: 0 Cr: O Co: O Mo: O Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 350 Ag: .2 As: 194 Cu: 72 Zn: 48 Sb: O Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: O
eAu: 963 eAg: .6 eAs: 534 eCu: 198 eZn: 132 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
Old SOSESTUE II
H-86-121
DEPARTUREtX) LATITUDEIT) ELEVATIOMtZ) O O 0
05
FROM TO TYPE SS BEDROCK 99 106 80 10 128
PPM NON MAG PPM MAG VG 2751 3359 1.4 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 1111 eSb N 1111 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
Au: 85 Ag: .2 As: 316 Cu: 237 Zn: 156 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
eAu: 121 eAg: .3 eAs: 451 eCu: 339 eZn: 223 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: O eW: 0
O/D OOOESTALE 11
H-86-121
EEPARTUREIXI LATITUDE(TI ELEVATIONIZI O O 0
06
FROM TO TYPE SS BEDROCK 106 111 80 10 128
PPM NON MAG PPM MAG VG 1429 2595 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N
'EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Old ROREST/UE II
H-86-121
DEPARTURE(X) LATITUDEfT) ELEVATIOR(Z) 0 O 0
07
FROM TO TYPE SS BEDROCK 111 116 80 10 128
PPM NON MAG PPM MAG VG 5055 1871 0 O
Au: 25 Ag: .2 As: 354 Cu: 293 Zn: 200 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
eAu: 126 eAg: 1 eAs: 1789 eCu: 1481 eZn: 1011 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
MAX
013 BOdESTA(E II
H-86-121
DEPARTUREIX) LATITUDE(Y) ELEVATIONIZ) 0 0 0
08
FROM TO TYPE SS BEDROCK 116 121 80 20 128
30S PYRITE
PPM NON MAG PPM MAG VG 7867
Au: 90 Ag: .6 As: 464 Cu: 359 Zn: 380 Sb: 0 Ba: O Cr: O Co: O Mo: 0 Ni: 0 W: 0
3233 0 0
eAu: 708 eAg: 4.7 eAs: 3650 eCu: 2824 eZn: 2989 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW' 0
Surface EEEE MIN EEEE NM ** EEEE MAG 4 EEEE Au 9E EEEE eAu * EEEE Ag 9F EEEE eAg ***)E EEEE As **** EEEE eAs * EEEE Cu * EEEE eCu *** EEEE Zn * EEEE eZn *#* EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
013 BOdESIAIF 11
H-86-121
DEPARTUREIX! LATITUDEITI ELEVATIONIZJ 0 0 O
09
FROM TO TYPE SS BEDROCK 121 124 90 20 128
PPM NON MAG PPM MAO VG 4352 2038 0 0
eAu: 87 eAg: 1.7 eAs: 1097 eCu: 1193 eZn: 635 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 20 Ag: .4 As: 252 Cu: 274 Zn: 146 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0!d BdAESTAIE II
H-86-121
BEPARTURE(X) LATITUbE(T) ELEVATIOMtZ) 0 0 0
10
FROM TO TYPE SS BEDROCK 124 128 80 20 128
PPM NON MAG PPM MAG VG 4491 5673 0 0
eAu: 90 eAg: 1.8 eAs: 1365 eCu: 921 eZn: 467 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 20 Ag: .4 As: 304 Cu: 205 Zn: 104 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: O W: O
Surface EEEE MIN EEEE NM * EEEE MAG *HE EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 0000 eCr N 0000 Co N XXXX eCo N XXXX Mo N
e(qo N Ni N eNi N W N
eW N
MAX
Au: 35 Ag: .2 As: 151 Cu: 115 Zn: 72 Sb: 0 Ba: O Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 126 eAg: .7 eAs: 546 eCu: 415 eZn: 260 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
DI! 9016S7/Uf 11
H-86-122
DEPARTIAtEIX1 LATITIIDEIY) ELEVATIONIZ) 0 0 0
01
FROM TO TYPE SS BEDROCK 57 62 80 10 102
PPM NON MAO PPM MAO VG 3613 2108 0 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu °1F EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OIS d011fS7/Uf 11
H-86-122
DEPARTURE IV LATITUDEITI ELEVATION III 0 0 ~ . 0
02
FROM TO TYPE SS BEDROCK 62 67 80 10 102
PPM NON MAG PPM MAG VG 4000 2364 0 0
eAu: 1200 eAg: 1.2 eAs: 1268 eCu: 384 eZn: 200 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 300 Ag: .3 As: 317 Cu: 96 Zn: 50 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 40 Ag: .05 As: 162 Cu: 110 Zn: 50 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 146 eAg: .2 eAs: 592 eCu: 402 eZn: 183 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
018 IlOAfSIW[f II
H-86-122
DEPARTURE(X) LATITUDE(Yl ELE1iATIIN)(2) 0 0 0
03
FROM TO TYPE SS BEDROCK 67 71 80 10 102
PPM NON MAG PPM MAG VG 3654 2173 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 40 Ag: .3 As: 188 Cu: 88 Zn: 70 Sb: O Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 159 eAg: 1.2 eAs: 749 eCu: 350 eZn: 279 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW • 0
011 10NES7AufE li
H-86-122
DEPARTUREIX) LATITUDE(Y) ELEVATIOM(Z) 0 0 0
04
FROM TO TYPE SS BEDROCK 71 76 80 10 102
PPM NON MAG PPM MAG VG 3981 2185 0 0
Surface EEEE MIN EEEE NM 9F EEEE MAG * EEEE Au *
• EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
NI NOMME II
H-86-122
DEPARTUREIX) LATITU9ElYl•ELEVATIONIZI 0 O 0
05
FROM TO TYPE SS BEDROCK 76 80 80 10 102
PPM NON MAG PPM MAG VG 3556 2255 0 0
eAu: 71 eAg: .4 eAs: 1372 eCu: 853 eZn: 178 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: O
Au: 20 Ag: .1 As: 386 Cu: 240 Zn: 50 Sb: O Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
O11 BORfS7A[E 11
H-86-122
DEPARTUREt%) LATITUDEtYI ELEVATION(Zl 0 0 0
06
FROM TO TYPE SS BEDROCK 80 85 80 10 102
PPM NON MAG PPM MAG VG 2404 2912 0 0
Au: 30 eAu: 72 Ag: .05 eAg: .1 As: 39 eAs: 94 Cu: 46 eCu: 115 Zn: 16 eZn: 38 Sb: 0 eSb: 0 Ba: 0 eBa:. 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: O W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Pli NOMME II
H-86-122
IEPARTUREIXI LATITUDEIYI ELE9ATIDMIZI D 0 0
07
FROM TO TYPE SS BEDROCK 85 90 80 10 102
PPM NON MAG PPM MAG VG 2846 2308 0 0
eAu: 14 eAg: .6 eAs: 182 eCu: 151 eZn: 60 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW • 0
Au: 5 Ag: .2 As: 64 Cu: 53 Zn: 21 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0 W: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 105 Ag: .2 As: 204 Cu: 160 Zn: 112 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 403 eAg: .8 eAs: 783 eCu: 614 eZn: 430 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 BOdfSTAdI II
H-86-122
1EPARTUREI%1 LATITUDE[Y1 ELEUATItUItZ) 0 0 0
08
FROM TO TYPE SS BEDROCK 90 93 80 10 102
PPM NON MAG PPM MAG VG 3836 2215 3.3 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 2222 eBa N 2222 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
OC 4O1!£BTAIf II
H-86-122
DEPARTUREIXI LATITUDEIY) ELEVATION!:) 0 0 O
09
FROM TO TYPE SS BEDROCK 93 99 80 20 102
PPM NON MAG PPM MAG VG 2557 6338 0 0
Au: 30 eAu: 77 Ag: .5 eAg: 1.3 As: 360 eAs: 921 Cu: 220 eCu: 563 Zn: 202 eZn: 517 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surf ace EEEE MIN EEEE NM * EEEE MAG ** EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As *** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N O000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 70 Ag: 1.2 As: 600 Cu: 250 Zn: 40 Sb: 0 Ba: O Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 1241 eAg: 21.3 eAs: 10635 eCu: 4431 eZn: 709 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
011 10l1fST1)If II
H-86-122
DEPARTURE(X) LATITUDE(Y1 ELEVATIONIZ) 0 0 0
10
FROM TO TYPE SS BEDROCK 99 102 80 20 102
94S PYRITE
PPM NON MAG PPM MAG VG 17725 3294 1.6 0
Surface EEEE MIN MAX EEEE NM ***** EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag *** EEEE eAg *lF*-3F***-1F*****?HE?E*** EEEE As ***E* EEEE eAs *-IF** EEEE Cu * EEEE eCu ***** EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 1111 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
OU 'NOIlESIAIE TI
H-86-123
DEPARTUREIX) LATITUDEIY) ELEVATIONI2l O D O
01
FROM TO TYPE SS BEDROCK 59 65 80 20 73
PPM NON MAG PPM MAG VG 4131 2216 0 0
Au: 45 eAu: 186 Ag: .2 eAg: .8 As: 220 eAs: 909 Cu: 420 eCu: 1735 Zn: 38 eZn: 157 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: O eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ** EEEE eAs * EEEE Cu * EEEE eCu ** EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N 0000 Ba N 0000 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 120 Ag: .5 As: 1408 Cu: 270 Zn: 35 Sb: O Ba: 0 Cr: 0 Co: O Mo: 0 Ni: O W: O
eAu: 225 eAg: .9 eAs: 2640 eCu: 506 eZn: 66 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: O eW: 0
013 S'OMETTAIT II
H-86-123
DEPARTURE(X) LATITODE(Y) ELEVATION(Z) 4 D 0
02
FROM TO TYPE SS BEDROCK 65 68 80 20 73
10% PYRITE
PPM NON MAG PPM MAG VG ASPY 1875 1375 0 30
Surface EEEE MIN EEEE NM * EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ************** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N 0000 eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
013 NOM(STAME II
H-86-124
DEPARTURE(X) LATITUDE(T) ELE1i,1TI0N(Z) 0 0 0
01
FROM TO TYPE SS BEDROCK 45 50 80 10 132
PPM NON MAG PPM MAG VG 3588 3216 0 0
Au: 60 eAu: 215 Ag: .4 eAg: 1.4 As: 736 eAs: 2641 Cu: 112 eCu: 402 Zn: 34 eZn: 122 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: O eNi: O W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * 0000 Ag 9F 0000 eAg * EEEE As ******* EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 30 Ag: .05 As: 204 Cu: 80 Zn: 37 Sb: 0 Ba: O Cr: 0 Co: O Mo: 0 Ni: 0 W: 0
eAu: 109 eAg: .2 eAs: 740 eCu: 290 eZn: 134 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
dld A4AfS7Adf II
H-86-124
DEPARTUREIXI LATITUDEIY) ELEVATIOMIZI 0 0 0
02
FROM TO TYPE SS BEDROCK 50 55 80 10 132
PPM NON MAO PPM MAG VG 3627 2902 0 0
Surface EEES MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * 0000 eAg 9E O000 As *HE EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 25 Ag: .2 As: 113 Cu: 1450 Zn: 32 Sb: O Ba: 0 Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 51 eAg: .4 eAs: 232 eCu: 2982 eZn: 66 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
ora aMlfS7/J.if II
H-86-124
DEPARTUREIXI LATITUDEIYI ELEVATIDN(Z1 0 0 0
03
FROM TO TYPE SS BEDROCK 55 59 80 10 132
PPM NON MAG PPM MAG VG 2056 1695 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * 0000 As * EEEE eAs * EEEE Cu **** EEEE . eCu 9E** EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
013 903fSTAIf II
H-86-124
DEPARTUREIXI LATITUDE(Yl ELEVATIONIZI 0 0 0
04
FROM TO TYPE SS BEDROCK 59 65 80 10 132
PPM NON MAG PPM MAO VG 2412 1882 0 0
Au: 45 eAu: 109 Ag: .2 eAg: .5 As: 97 eAs: 234. Cu: 160 eCu: 386 Zn: 22 eZn: 53 Sb: 0 eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: O eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 3
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * 0000 As * 0000 eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
nrE B0R£S7Rd1 17
H-86-124
DEPARTUREIX) LATITUDEIYI ELEYATION)D 0 0 4
05
FROM TO TYPE SS BEDROCK 65 70 80 10 132
PPM NON MAG PPM MAG VG 2103 1641 0 0
eAu: 1125 eAg: .2 eAs: 50 eCu: 168 eZn: 139 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW' 0
Au: 535 Ag: .1 As: 24 Cu: 80 Zn: 66 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0
W: O
Sur-Face EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE .eAu * EEEE A9 * EEEE eAg * EEEE As * 0000 eAs * 0000 Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co .N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
Au: 20 Ag: .05 As: 10 Cu: 60 Zn: 20 Sb: O Ba: O Cr: 0 Co: O Mo: 0 Ni: O
W: 0
eAu: 37 eAg: .1 eAs: 19 eCu: 112 eZn: 37 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0
eW: 0
0/1 RORESIAfE II
H-86-124
DEPARTUREIX) LATITUDEIY) ELÇ1iATIDIiIZ) 0 0 0
06
FROM TO TYPE SS BEDROCK 70 75 80 10 132
PPM NON MAG PPM MAG VG 1871 1930 0 0
Surface EEEE MIN EEEE NM *. EEEE MAO * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * 0000 Cu * 0000 eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0!3 30AFSTAdf 11
H-86-124
aEPARTURE(Xl LATITU6E(Y1 ELE9ATI0l1tZ1 0 11 0
07
FROM TO TYPE SS BEDROCK 75 80 80 10 132
PPM NON MAO PPM MAG VG 1752 1486 0 0
eAu: 105 eAg: .2 eAs: 58 eCu: 105 eZn: 65 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: O eNi: 0 eW: 0
Au: 60 Ag: .1 As: 33 Cu: 60 Zn: 37 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: O Ni: 0
W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * 0000 eCu * 0000 Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
Au: 7.5 Ag: .3 As: 27 Cu: 116 Zn: 24 Sb: 0 Ba: 0 Cr: O Co: 0 Mo: O Ni: 0 W: 0
eAu: 12 eAg: .5 eAs: 42 eCu: 181 eZn: 37 eSb: 0 eBa: 0 eCr: O eCo: 0 eNi: 0 eNi: 0 eW: 0
Old IOMESTAI( 11
H-86-124
DEPARTIfREIX1 LATITUDEITI ELEYATIONiZ1 O D 0
08
FROM TO TYPE SS BEDROCK 80 85 80 10 132
PPM NON MAG PPM MAG VG 1561 1351 0 0
Surf ace EEEE MIN EEEE NM * EEEE MAG * EEEE Au 9F EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * 0000 Zn * EEEE eZn * -EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N eW N
MAX
olB AOflES?Aff II
H-86-124
DEPARTUREIX) LATITUDEIT) ELEi)ATIOAIZI O 0 0
09
FROM TO TYPE SS BEDROCK 85 90 80 10 132
PPM NON MAG PPM MAG VG 1905 1581 1.5 0
Au: 435 eAu: 829 Ag: .2 eAg: .4 As: 552 eAs: 1051 Cu: 176 eCu: 335 Zn: 28 eZn: 53 Sb: O eSb: O Ba: O eBa: 0 Cr: O eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: ~ W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * 1111 Zn * 1111 eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
O/s AOAËSTA(f 11
H-86-124
DEPARTURE)X) LATITUAEfY) ELEYATIO)iIZ) 0 0 0
10
FROM TO TYPE SS BEDROCK 90 95 80 10 132
PPM NON MAG PPM MAG VG 2627 1824 0 0
eAu: 1406 eAg: 1.6 eAs: 1640 eCu: 420 eZn: 147 eSb: C eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 535 Ag: .6 As: 624 Cu: 160 Zn: 56 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * 0000 eZn * 0000 Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
0/3 30!}FS7A1f II
H-86-124
BEPARTUREI%1 LATITUBEIYi ELEVATIDKIII 0 0 0
11
FROM TO TYPE SS BEDROCK 95 100 80 10 132
PPM NON MAG PPM MAG VG 4316 2351 0 0
Au: 5660 eAu: 24427 Ag: .2 eAg: .9 As: 156 eAs: 673 Cu: 80 eCu: 345 •Zn: 44 eZn: 190 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0
W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au *** EEEE eAu ** EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * 0000 Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
0111 IJ9RESTAxE 11
H-86-124
DEPARTURE(X) LATITUDE(Y) ELEUATIW)iZ) 0 0 0
12
FROM TO TYPE SS BEDROCK 100 105 80 10 132
PPM NON MAG PPM MAO VG 2363 1544 0 0
Au: 90 eAu: 213 Ag: .4 eAg: .9 As: 142 eAs: 335 Cu: 148 eCu: 350 Zn: 90 eZn: 213 Sb: 0 eSb: 0 Ba: 0 - eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0 Mo: 0 eNi: 0 Ni: 0 eNi: 0 W: 0 eW: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu -)F EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N EEEE Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N
eW N
MAX
0I8 MOTU( II
H-86-124
DEPARTUREIX) UTITUDE(Y) ELEVATIOMtZ) O 0 O
13
FROM TO TYPE SS BEDROCK 105 110 80 10 132
PPM NON MAG PPM MAG VG 3333 2167 0 0
eAu: 1133 eAg: 1.7 eAs: 2160 eCu: 547 eZn: 260 eSb: O eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 340 Ag: .5 As: 648 Cu: 164 Zn: 78 Sb: O Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As ****** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N 0000 eSb N 0000 Ba N EEEE eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
)Jd 9410741F II
H-86-124
DEPARTUREIX) LATITUDEIY) ELEVATI08IZ) 0 0 0
14
FROM TO TYPE SS BEDROCK 110 115 80 10 132
PPM NON MAG PPM MAG VG 2726 1632 1.6 0
eAu: 191 eAg: 1.4 eAs: 1636 eCu: 573 eZn: 425 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
Au: 70 Ag: .5 As: 600 Cu: 210 Zn: 156 Sb: 0 Ba: 0 Cr: 0 Co: 0 Mo: 0 Ni: 0 W: 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag 9E EEEE eAg * EEEE As ***** EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn 9E EEEE Sb N EEEE eSb N 1111 Ba N 1111 eBa N EEEE Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N W N eW N
MAX
Au: 210 Ag: .6 As: 181 Cu: 112 Zn: 146 Sb: 0 Ba: O Cr: O Co: 0 Mo: 0 Ni: 0 W: 0
eAu: 497 eAg: 1.4 eAs: 428 eCu: 265 eZn: 345 eSb: 0 eBa: 0 eCr: 0 eCo: 0 eNi: 0 eNi: 0 eW: 0
01 RDRES?AdE I!
H-86-124
DEPARTUREfX) LATITUDE4Y1 ELE4ATIOM(Z) 0 0 0
15
FROM TO TYPE SS BEDROCK 119 125 80 20 132
PPM NON MAO PPM MAG VG 2366 1742 0 0
Surf ace EEEE MIN EEEE NM * EEEE MAS * EEEE Au 9E EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N EEEE eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N eNi N
W N eW N
MAX
Au: 20 Ag: .3 As: 164 Cu: 370 Zn: 114 Sb: 0 Ba: 0 Cr: 0 Co: O Mo: O Ni: 0 W: O
eAu: 51 eAg: .8 eAs: 417 eCu: 940 eZn: 290 eSb: O eBa: 0 eCr: 0 eCo: O eNi: 0 eNi: 0 eW: O
nsg 9DAESIAEE II
H-86-124
DEPARTIfREIXI LATITIIDEIYI ELEYATIOIIIZI 0 0 0
16
FROM TO TYPE SS BEDROCK 125 130 80 20 132
PPM NON MAO PPM MAO VO 2542 2083 0 0
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au * EEEE eAu * EEEE Ag * EEEE eAg * EEEE As * EEEE eAs * EEEE Cu * EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N 0000 Cr N 0000 eCr N EEEE Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
011 .90AESTAIE Zr
H-86-124
BEPARTURElX1 LATITULElYI ELEUATIOMiZ1 0 0 0
17
FROM TO TYPE SS BEDROCK 130 132 80 20 132
?Ss ?Y1171
PPM NON MAG PPM MAG VG GALENA
5103 2345 3.7 1
Au: 100 eAu: 510 Ag: .05 eAg: .3 As: 664 eAs: 3389 Cu: 86 eCu: 439 Zn: 84 eZn: 429 Sb: O eSb: 0 Ba: 0 eBa: 0 Cr: 0 eCr: 0 Co: 0 eCo: 0
- Mo: 0 eNi: 0 Ni: O eNi: 0
W: O eW: O
Surface EEEE MIN EEEE NM * EEEE MAG * EEEE Au IF EEEE eAu * EEEE Ag * EEEE, eAg •3E- EESE As ****** EEEE eAs * EEEE Cu •1F EEEE eCu * EEEE Zn * EEEE eZn * EEEE Sb N EEEE eSb N EEEE Ba N EEEE eBa N EEEE Cr N 11-11 eCr N 1111 Co N XXXX eCo N XXXX Mo N
eMo N Ni N
eNi N W N
eW N
MAX
