REPORT OF EXPLORATION ACTIVITIES, LAC GAGNON ...

GM 42417REPORT OF EXPLORATION ACTIVITIES, LAC GAGNON PROJECT

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http://gq.mines.gouv.qc.ca/documents/sigeom/Licence.pdf

http://gq.mines.gouv.qc.ca/documents/sigeom/license.pdf

REPORT OF EXPLORATION ACTIVITIES

1984

LAC GAGNON PROJECT (405)

WESTFIELD MINERALS LIMITED

lainlstbre de l'Energie et des Resources' Service de la GadInformation

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Alex. E. Marr Geologist June 1985

TABLE OF CONTENTS

Page

1.0 SUMMARY 1

2.0 INTRODUCTION 3

3.0 THE PROPERTY 3

3.1 ACCESS 3

3.2 CLIMATE 10

3.3 TOPOGRAPHY AND VEGETATION 10

4.0 PREVIOUS WORK 11

5.0 WORK PERFORMED 1984 12

6.0 GEOLOGY 13

6.1 PREVIOUS MAPPING 13

6.2 RECENT WORK 13

6.3 ECONOMIC GEOLOGY 16

7.0 GEOPHYSICAL SURVEYS 16

7.1 AIRBORNE GEOPHYSICAL SURVEYS 16

7.1.1 ELECTROMAGNETICS 17

7.1.2 TOTAL FIELD MAGNETICS 17

7.1.3 VLF-EM 18

7.2 GROUND GEOPHYSICAL SURVEYS 18

8.0 GEOCHEMISTRY 19

8.1 OVERBURDEN GEOCHEMISTRY 19

9.0 DIAMOND DRILLING 22

10.0 CONCLUSION AND RECOMMENDATIONS 25

LIST OF FIGURES AND TABLES

Figure 1

Figure 2

Table 1

Table 2

Figure 3

Figure 4

Location Map

Property/Claim Map

List of Claims

Table of Geophysical Conductors and the Results of Diamond Drilling

Compilation Map showing Overburden and Diamond Drill Hole Locations

Graph of the Distribution of Gold Analyses from Lac Gagnon Drill Core

LIST OF APPENDICES

Appendix I Overburden Drill Logs

Appendix 2 Diamond Drill Logs

Appendix 3 Overburden Assay Results

Appendix 4 Diamond Drill Assay Results

Appendix 5 Dighemiii Survey of the Raymond Twp. Area, Quebec for MPH Consulting Ltd. by Dighem Surveys and Processing Inc. t••4- -1‘SoS

Appendix 6 Report on Magnetometer, Horizontal Loop EM and IP/Resistivity Surveys, Lac Gagnon Project, Raymond Twp., Que. GIK1- 44 i

Appendix 7 Sampling Methodology for Overburden Drill Sampling

LIST OF MAPS

1 -

2 -

3 -

Overburden holes 1, 2, 3 & 4

Overburden holes 5, 6, 7

Overburden holes 8, 9, 10, 11, 12

4 - Overburden holes 11, 13, 14, 15, 16

5 Overburden holes 17, 18, 19, 20, 21, 22, 23, 24, 25, 26,

6 - Overburden holes 28, 29, 30

7 - Diamond drill hole 1

8 Diamond drill holes 2, 3, 4, 5


10 Diamond drill hole 7


12 - Diamond drill holes 9, 10, 11

13 - Diamond drill holes 12, 13

27

1.0 SUMMARY

During the months of July and September to December in 1984, Westfield

Minerals Ltd. conducted an extensive reconnaissance exploration program

on its wholly owned, 115-claim Lac Gagnon property in northwestern Quebec

near the Ontario border. The property is found approximately 10 miles to

the north of the Golden Pond gold discovery by Inco-Golden Knight

Resources Inc. in Casa-Berardi township.

Work consisted of line-cutting, reverse circulation overburden drilling;

airborne and ground geophysical surveys and diamond drilling.

Diamond drilling tested a series of conductors which were outlined first

by airborne and then by ground follow-up geophysical surveys. Drill

core was analyzed for gold with selected samples analyzed for arsenic

and copper. The gold analyses returned generally low values, with

105 ppb Au in a pyritiferous sediment being the highest value. The

highest copper value was 9100 ppm.

There appears to be a vague gold-copper association but no relationship

between gold and arsenic.

Geologically, the property is traversed by a broad sequence of interbedded

argillites, greywackes, extrusive volcanics and mafic intrusive rocks.

There is some evidence of localized alteration (carbonation and silici-

fication). Deformation is slight and folding, if present, may be long-

limbed isoclinal in style. Some degree of alteration and deformation is

probably related to the emplacement of the large granitic pluton to the

southwest of the property and also to the emplacement of broad gabbroic

bodies within the sedimentary sequence.

Virtually all ground exploration activity has concentrated in the western

part of the property except for some detailed ground geophysical work in

the eastern block. The entire property has been covered by an airborne

FIGURE 1

-3

DighemIII

EM survey. This survey allowed a preliminary appraisal of

conductors in preparation for the ground geophysics.

The results from the diamond drilling indicate that the best hope for

detecting economic mineralization appears to be in the vicinity of

drill hole 405-84-7 where interesting alteration accompanied by modest

gold and copper values were noted.

2.0 INTRODUCTION

This report briefly describes each of the activities undertaken in

Westfield Minerals Limited's 1984 exploration program on its Lac Gagnon

property. The results are discussed and recommendations are made based

upon these results. For the sake of brevity, the reader is referred to

existing reports which were completed in conjunction with this work;

namely, the MPH Consulting Ltd. geophysics report and the DighemIII

airborne survey report. Sufficient work has been filed to keep the claims

in good standing for in excess of two years. At the present time,

unfiled work, if submitted, will carry the claims for at least another

ten years under existing work requirements.

3.0 THE PROPERTY

The Lac Gagnon property is composed of a large block of 115 contiguous

claims which are located at 79°13'40" to 79°221 10"W longitude and

49°42'36" to 49°44'17"N latitude. They straddle Raymond, Recher and

Carheil Townships in the James Bay Frontier region of Quebec, Canada.

Westfield Minerals Limited staked the claims during the period August-

November 1983. Through an agreement with Tillicum Resources Ltd. that

company will be entitled to a seven and one half percent net profits

royalty in return for a finder's fee. See figure 2.

3.1 ACCESS

The simplest access to the property is by a gravel lumber road which

runs approximately north-south and bisects the property just to the east

of Lac Gagnon. The road connects the property with La Sarre, Quebec

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REV. DATE NTS

DRAWN 'DWG. NO.

5 -

TABLE 1

LAC GAGNON

LICENSE NO. CLAIM NO. TOWNSHIP STAKING DATE

417930 1 Recher August 27, 1983

2 Recher August 27, 1983


4- Raymond August 26, 1983

5 Raymond August 26, 1983

417931 1 Recher August 28, 1983





417932 1 Recher August 29, 1983





417933 1 Recher August 30, 1983





417934 1 Recher August 31;1983





417935 1 Raymond August 27, 1983


f. Raymond August 27, 1983.

4 Raymond August 27, 1983 5 Raymond August 27, 1983

LAC GAGNON - continued




3 . Raymond August 28, 1983






417938 1 - Raymond August 30, 1983









417941 1 Carheil August 28, 1983

2 Carheil August 28, 1983








5-- Carheil August 29, 1983

417943 1 Carheil August 30, 1q83





- 7 - LAC GAGNON - continued


417944

417945

417946

417947

417948

417949

417986

1 Raymond

2 Raymond

3 Raymond

4 Raymond

5. Raymond

1 Raymond

2 Raymond

3 Carheil

4 Carheil

5 _ Carheil

1 Raymond

2 Raymond

3 Raymond

4 Raymond

5 Raymond

1 Raymond

2 Raymond

3 Raymond

4 Raymond

5 Raymond

1 Raymond

2 Raymond

3 Raymond

4 Raymond

5 Raymond

1 Raymond

2 Raymond

3 Raymond

Raymond

Raymond

Recher

Recher

Recher

Recher

Recher

August 31, 1983 August 31, 1983 August 31, 1983 August 31, 1983 August 31, 1983 August 27, 1983 August 27, 1983 August 27, 1983 August 27, 1983 August 27, 1983 August 28, 1983 August 28, 1983 August 28., 1983 August 28, 1983 August 28, 1983 August 28, 1983 August 28, 1983 August 28, 1983 August 28, 1983 August 28, 1983 August 30, 1983 August 30, 1983 August 30, 1983 August 30, 1983 August 30, 1983 August 31, 1983 August 31, 1983 August 31, 1983 August 31, 1983 August 31, 1983. November 8, 1983 November 8, 1983 November 8, 1983 November 8, 1983 November 8, 1983

5

1 2

3 4 5 -11

- 8 -

LAC GAGNON - continued


417987 1 Recher November 9, 1983

2 Recher November 9, 1983

418695 1 Recher October 18, 1983

2 Recher October 18, 1983











3 Recher October. 20, 1983



418698A 1 Recher October 21, 1983

1`)

LAC GAGNON

License 0417986 - Cis 1-5 incl - Recher Township License 0417987 - Cis 1-2 - Recher Township • License #418695 - Cis 1-5 incl - Recher Township License #418696 - Cis 1-5 inci - Recher Township License #418697 - Cis 1-5 incl - Recher Township License #41869811- Cl 1 - Recher Township License #417930 - Cls 1-3 incl - Recher Township License #417931 - Cis 1-5 incl - Recher Township License #417932 - Cis 1-5 incl - Recher Township License #417933 - Cis 1-5 incl Recher Township License #417934 - Cis 1-3 incl - Recher Township License #417930 - Cis 4-5 - Raymond Township • License #417934 - Cis 4-5 - Raymond Township License #417945 - Cis 1-2 - Raymond Township License #417946 - Cis 1-5 incl - Raymond Township License #417947 - Cis 1-5 incl - Raymond Township License #417948 - Cis 1-5 incl - Raymond Township License 0417949 - Cis 1-5 incl - Raymond Township License #417945 - Cis 3-5 inci Carheil Township License #417940 - Cis 1-3 incl - Raymond Township License #417941 - Cis 3-5 incl - Raymond Township License #417942 - Cis 1-4 incl - Raymond Township License 0417943 - Cis 4-5 - Raymond Township License #417944 - Cis 1-5 incl - Raymond Township License #417941 - Cis 1-2 - Carheil Township License #417942 - Cl 5 - Carheil Township License #417943 - Cis 1-3 incl - Carheil Township License #417935 - Cis 1-5 incl - Raymond Township License #417936 - Cis 1-5 incl - Raymond Township License #417937 - Cis 3-5 incl - Raymond Township License #417938 - Cis 1-3 incl - Raymond Township License 0417939 - Cis 3-5 incl - Raymond Township

.t

.0,1•••

- 10 -

(100 km to the south) which is the nearest major commercial centre in

the region. The road is driveable for most of the year but care must

be taken to avoid occasional washouts. During the winter months the

road must be plowed to keep it open. Plows are available from the

Dieppe lumber camp 30 km to the south and at Cote et Freres Ltee of

Villebois 70 km to the south of Lac Gagnon. Rapid access can be made

by air from La Sarre. Les Helicopteres Abitibi are equipped with Bell

206's and La Sarre Air Service with a good complement of light water-

borne aircraft. Lac Gagnon is suitable for landing and take-off.

Regularly scheduled flights are available from Toronto, Montreal and

other major centres which terminate at either Timmins or Rouyn-Noranda.

Rouyn-Noranda is the nearest major airport serving the Lac Gagnon Region.

3.2 CLIMATE

The area suffers a typical subarctic winter - recent snowfall accumula-

tions are approximately six feet; conditions are generally cold and

windy. Summers are hot, humid and insect-ridden, frequent torrential

and often violent thunderstorms are common.

3.3 TOPOGRAPHY AND VEGETATION

The property area is largely muskeg swamp, especially to the east. A

small series of east-west ridges to the west of Lac Gagnon are uncharac-

teristically dry and in fact contain scattered outcrops. A recent forest

fire has greatly reduced the surface vegetation over most of the property

although several fingers of green timber remain, mainly south of Lac Gagnon.

Access to the western part of the property is by several cat-driven trails.

These are driveable by all-terrain-vehicle only after freeze-up. Several

minor creeks and seeps do not themselves impede progress, but continued

passage across them creates large muddy water holes. The eastern block of

the property remains inaccessible by wheeled or tracked vehicle to date

due to a series of large and deep creeks. So far the east has only been

reconnoitered by helicopter and on foot.

Overburden cover is generally thick and averages in the neighbourhood

of 25-30 m depth but this estimate varies considerably.

There is sufficient qualified manpower in the region. Bilingualism is

an asset and is recommended for companies operating in the region.

4.0 PREVIOUS WORK

A considerable amount of work is on file as having been done in the Lac

Gagnon area. Geophysical and geochemical surveys, diamond drilling and

minor trenching have been pursued by a number of companies through the

fifties to the seventies. Judging by the amount of drill core discovered

on the south shore of Lac Gagnon, far more diamond drilling took place

than was filed with the Quebec Government. Unfortunately, much of this

drill core has been rendered useless due to the process of weathering on

identification markers. The geophysical surveys which were filed show

remarkable concurrence with the recently conducted surveys. The

geochemical surveys are of questionable use in light of the thick over-

burden cover.

The old drill core shows that there has been much hydrothermal alteration,

in a rather broad section of the Lac Gagnon stratigraphy. Massive pyrite

over several feet has been noted in several holes - minor chalcopyrite and

sphalerite occur sporadically along with the rare speck of galena. There

does not appear to be any appreciable structural deformation in the old

drill core - in fact, most deformation is probably diagenetic with the

sediments. Extensive fracturing and faulting along graphitic horizons are

observed.

Specifically, five drill logs are on file by Selco Exploration Co. Ltd.

dated 1959 but these could not be correlated with the old drill core.

New Jersey Zinc Exploration Co. (Canada) Ltd. completed electromagnetic,

magnetic and gravimetric surveys in the immediate area in 1975. Canadian

Merril Ltd. also completed magnetic, electromagnetic and geochemical

surveys the same year. These reports are available from the Ministère

des Energie et Ressources at Rouyn, QuAec.

- 12 -

5.0 WORK PERFORMED 1984

In July of 1984, 268km of helicopter-borne geophysical surveys were flown

on roughly parallel lines 100 m apart and at an average altitude of 31 m

by Dighem Surveys and Processing Inc. The survey had three main components:

electromagnetics, total field magnetics, and VLF-EM. This survey

detected a series of distinctive conductors which were subsequently used

to plan a three-month exploration program in the autumn of 1984, (see

Dighem/II Survey of the Raymond Township Area, Quebec). A small reverse

circulation drilling program of 688 m (2260 ft.) was completed in

September by Heath and Sherwood Drilling Ltd. of Kirkland Lake, Ontario.

Overburden Drilling Management Ltd. of Nepean, Ontario provided expertise

in the sampling, overburden logging and laboratory analysis of the reverse

circulation samples. Concurrently, 54 kJ, of metric grid were cut by Henry

Gonzales Ltd. of Timmins and a ground geophysics program completed by

MPH Consulting Ltd. of Toronto. Magnetometer, MaxMin II Horizontal Loop

EM and Induced Polarization/Resistivity surveys were conducted over

several test areas in the eastern and western blocks of the property. A

system of access roads was prepared by Cote et Freres Ltee of Villebois.

After this work was completed a diamond drill program of 2,125 m (6972 ft.)

was commenced by Bradley Bros. Ltd. of Rouyn with the goal of examining

the numerous conductors and anomalous responses from both the geophysical

and geochemical surveys, and to delineate as much of the local stratigraphy

as possible.

The completion of the diamond drilling signalled the end of the exploration

program. All holes were split to varying extents and analyzed for gold;

several sections were also analyzed for As and Cu.

Supervisory work was conducted by A. E. Marr, Project. Geologist; Robert

Thibault, Field Technician; Luc Valade, Field Technician; and Daniel

Vandal, Field Assistant, all of Westfield Minerals Limited.

- 13 -

6.0 GEOLOGY

Regionally, the Lac Gagnon property is found on the boundary between

the Taiba Group sedimentary belt and the Allard Group Volcanic Belt

(Barnett et al., 1982).

6.1 PREVIOUS MAPPING

Due to most of the Lac Gagnon property being swampy, outcrops are

extremely rare. Conventional mapping, therefore, is of little use.

Diamond drilling and, to a lesser extent, reverse circulation drilling

were the main sources of geological information.

A good body of data could be had from the old Selco drill logs which,

presumably, contributed along with geophysical data to the Quebec

Government's geological compilation map. By necessity the government

compilation map is grossly oversimplified. The regional picture suggests

that a broad continuous sequence of interbedded tuffs and argillaceous

sediments, (V9, S4) which roughly sweeps from the WNW to the ESE and

crosses through Lac Gagnon, may be the core of a synform. If this is

correct then, these sediments and volcanic sediments are probably underlain

by a broader sequence of indeterminate pyroclastic rocks and mafic to

intermediate volcanic rocks. A large granitic batholith abuts against

the greenstone belt to the SW and may account for much of the hydrothermal

alteration observed in the old drill core found by Lac Gagnon. The last

significant lithology noted is a discontinuous but persistent horizon of

greywacke and argillite with indeterminate iron formation.

6.2 RECENT WORK

Westfield's drilling program of 1984 intersected a rather restricted set

of lithologies. In order of decreasing abundance they are: argillite,

greywacke, intermediate to mafic basalt, pyroxene gabbro, andesite,

mafic tuff, porphyritic dacite, pyritiferous graphite and granite. These

lithologies probably comprise 95-100% of the observed types. A localized

geological map has been constructed combining inferences from the

geophysical data, the drill hole data gathered by Westfield Minerals Limited

and earlier compilation work.

- 14 -

The picture which emerges presents a series of narrow sedimentary beds

intercalated with volcanic sediments, basaltic and andesitic flows.

These rocks tend to strike between 0700 in the western half of the

property and 0900 in the east. At some undetermined point large sills

of gabbro were intruded into the country rock; later numerous dykes and

sills of porphyritic dacite were intruded or, in some cases, extruded.

The geological environment in the area of the 1984 drilling appears to

be in the vicinity of a volcanic arc under deep marine conditions.

Thick sequences of dark argillites imply periods of volcanic quiescence

whereas thick sequences of greywacke imply a more agitated or more

proximal depositional environment. Many of the basalts observed in

drill core are probably pillowed but the selvages are very poorly

preserved making this conclusion difficult.

The degree of hydrothermal alteration observed in the rocks may be, to

some extent, syngenetic or syn-depositional as the case may be, but it

is felt that the alteration is a relatively late feature and is more

likely related to the emplacement of the large granitoid plutons to the

north and southwest or individual mafic intrusions.

The timing of these geological events is obscured since all lithologic

relationships must be determined from drill core which presents a very

poor three-dimensional picture. A broad structural interpretation is

tenuous at best and must await a greater data base. On a limited scale

however, two predominating fracture sets are observed in much of the

core. They appear to have been accentuated by hydrothermal alteration

in that they are characterized by bleached haloes which were probably

caused by the passage of hot, percolating solutions.

The dominant fracture set is usually subparallel to the plane of bedding.

The second set often has a similar dip to the dominant set but the strike

axis is usually rotated by about 45°. One often observes minor scale

faulting along these fractures. The fractures may have originated within

a tensional environment in the vicinity of larger-scale normal faults.

- 15 -

For a comprehensive description of various lithologies and structural

interpretations one is referred to the drill logs which have been

appended to this report.

The geology bears some resemblance to that seen at the Inco-Golden Knight

property 10 miles to the south. On their Casa-Berardi property the

lithologic suite comprises mainly clastic sediments, tuffs, iron formation,

conglomerate and agglomerate. The gold mineralization occurs mainly in

graphitic sediments and agglomerates. The discovery was made by following

up an airborne electromagnetic conductor which was detected on the flank

of a strong aeromagnetic anomaly. The gold discovery itself was a lucky

one in that the geophysical anomalies upon which the early drill holes were

targeted coincidentally bracketed a gold-bearing sedimentary and volcani-

clastic sequence. Geophysical methods became useful subsequently in

outlining responses of specific lithologies which, through drilling were

proven to have a gold association. Induced polarization and electro-

magnetic methods were shown to be the most effective geophysical tools

on this property. Induced polarization was useful because it was found

that part of the strong southern anomaly was due to the presence of

sulphides in agglomerate and gold was associated with these sulphides

to an indeterminate degree. Electromagnetic surveying, also, was useful

for tracing particular lithologies within the Golden Pond sequence.

The important differences between the Golden Pond geology and the Lac

Gagnon geology is the more clastic nature of the sediments at Golden. Pond

and the apparent proximity of an auriferous volcanic source indicated by

the agglomerates. Golden Pond also displays a distinctive 'potassicyanic

alteration which imparts a bright blue hue to the rock. This alteration

may be related to the presence of abundant arsenopyrite. The Lac Gagnon

lithologies suggest a finer, more distal environment and the alteration

seems to be less exotic.

Recent disclosures by Golden Knight Resources Inc. indicate an 'undiluted

drill-indicated mineral resource of 3 million tonnes at 9.9 g/t (0.29 oz/t),

- 16 -

has been identified in the Golden Pond east zone, and includes a higher

grade lens of one million tonnes at 14.3 g/t (0.42 oz/t).,1

Their latest exploration effort has involved the drilling of 59 diamond

drill holes to a depth of 17,161 m and 82 overburden holes to a depth

of 2,829 m.

6.3 ECONOMIC GEOLOGY

A discussion of economic mineralization at Lac Gagnon must embrace

potential massive sulphide deposits. Results from the rock geochemistry

on the drill core will be discussed in detail in Section 9.0. Anecdotally,

however, the results from the drilling program tended to promote base

metals rather than precious metals. Several sections of drill core

produced interesting copper results. Other base metals mineralization

such as galena or sphalerite were very rare in hand so the core was not

analyzed for these sulphides.

Gold results were almost universally disappointing. Except for a few

anomalous values which were usually related to pyritiferous argillites

and graphites, the background values for gold were very low.

There seems to be a relationship between copper and gold; that is, in

the few areas where one obtains a jump in the gold values there are

often corresponding highs in the copper values. This relationship is

less consistent between gold and arsenic where there are occasional

correlations but, more frequently, none at all.

7.0 GEOPHYSICAL SURVEYS

7.1 AIRBORNE GEOPHYSICAL SURVEYS

The Dighemin airborne electromagnetic survey was flown on flight lines

which were approximately 100 m apart for a total of 268 linear kilometers

including a ten kilometer tie line.

1 From Today's Market Line, issue TML 050/85, March 12, 1985

- 17 -

The specially outfitted ASTAR helicopter flew at about 126 km/h with an

EM instrument height of about 31 m. Other equipment included a Sonotek

PMH 5010 magnetometer, a Sperry radio altimeter, a Geocam sequence

camera, an RMS GR-33 analog recorder and a Herz Industries Totem 2-A

VLF-electromagnetometer. For the details of instrumentation one is

referred to the DighemIII

report by Dvorak, (1984).

7.1.1 Electromagnetics

The electromagnetic anomaly map is derived from a 'near-vertical half plane

model' which enhances 'discrete' bedrock conductors such as sulphide-rich

sheets or beds of iron formation. The resistivity map, by contrast,

emphasizes conductors of a broader or more regional character because

the results are interpreted on the basis of a 'half-space' model.

The electromagnetic map outlines three to four distinct, roughly parallel

conductors which are best expressed in the property's western block then

cross Lac Gagnon in an east-west sense where they seem to weaken then

terminate at the eastern edge of the lake. The eastern block of the

property contains very few high quality conductors.

The very 'discrete' nature of the western conductors promoted them as

likely drill targets. The resistivity map too, defines these strong

western conductors. The resistivity map in the east however shows a

generally flat profile with a trend which suggests that the strike of

the underlying lithologies suddenly sweep to the southeast.

7.1.2 Total Field Magnetics

During the fly-over, magnetic data is digitally recorded to an accuracy of

one nannotesla which is the equivalent of one gamma. The resultant data is then

processed by computer to yield a total field magnetic contour map. This

data can be further enhanced by filtering to produce a magnetic contour

map of the near surface geology.

- 18 -

According to the magnetic contour map and the enhanced magnetic contour

map the conductors which were detected by the EM survey are in fact

continuous and sweep eastwards across the property.

There is greater likelihood that a magnetic anomaly which coincides with

an EM anomaly is due to the presence of sulphides, although this is not

always the case. The government compilation map interprets these strong

linear trends as being iron formation. The geophysical interpretation

makes a similar prediction which is correct, insofar as drilling has shown

there to exist thin, continuous bands of massive pyrite.

The enhanced magnetics gives better resolution to the conductors on the

western side of the property. Here one can see at least three major

magnetic features.

7.1.3 VLF-EM

The VLF-EM response serves to confirm the conductors and anomalies detected

in the electromagnetic and magnetic surveys. Being a non-inductive

phenomenon, the VLF-EM response tends to reflect 'current gathering' rather

than the secondary induced fields which are detected by both EM and

magnetic measurements.

With a precision of 0.1%, readings are made and digitally recorded on

board the aircraft. Both the total field and quadrature components are

recorded in this way. As with the magnetic data the VLF-EM data is

filtered. When applied to VLF-EM data the filter removes effects due to

regional and wave transmission variations. The result is a map which

enhances local geological variations.

7.2 GROUND GEOPHYSICAL SURVEYS

MPH Consulting Ltd. of Toronto conducted magnetometer, horizontal loop EM

and I.P./resistivity surveys on the Lac Gagnon property during September

and October of 1984. Their final analysis is available with this report.

- 19 -

The ground geophysical surveys improved the localization and the resolution

of the airborne conductors.

The following chart summarizes the findings of MPH along with the results

of the diamond drilling which followed shortly after these surveys. (See

page 20.)

The diamond drilling indeed confirmed the existence of all targeted

conductors except for the questionable 'Y' conductor. The geophysical

methods were successful in locating the specific horizons of interest

but the interpretations were rarely accurate in defining the types of a

large number of essentially similar conductors. It is difficult,

therefore, to formulate a system whereby geological interpretations

could be made based upon future geophysical surveys.

The eastern block of the property revealed few conductors in spite of

the shallow overburden depth (10-25 m as determined by ground geophysics).

Two of the three major conductors in the east, M and 0, have been

interpreted as possible massive sulphide features but there is a likeli-

hood that one is dealing with a pyritiferous argillite as observed in the

west. In any event, they should be tested by drilling.

Further interpretations which are unrelated to the diamond drilling are

available in the MPH report.

8.0 GEOCHEMISTRY

8.1 OVERBURDEN GEOCHEMISTRY

Geochemical work at Lac Gagnon was restricted to overburden sampling and

drill core analysis.

The reverse circulation drill program was carried out by Heath and

Sherwood Drilling Ltd. using a small reverse circulation drill rig

mounted on the back of a Nodwell tracked carrier. A total of 30 reverse

TA_ __ 2

TABLE OF GEOPHYSICAL CONDUCTORS (TARGETS) AND THE RESULTS OF DIAMOND DRILLING

CONDUCTOR LOCATION EXPECTED CAUSE CAUSE AS DETERMINED BY DIAMOND DRILLING MAGNETIC RESPONSE

A 133W/1+505 to L37W/1+255

Narrow conductor at 35m depth on line 36+00W dipping at 800 to the south; probably graphite.

Drilling indicated a fault at 1+55S which is bound on the south by about 5m of.pyritiferous graphite; depth to bedrock is 35m according to reverse circulation drilling.

non-magnetic

C L33W/1+70N to 137W/1+30N

Narrow conductor at 10m depth with a dip at 75' south; possible fault between 35 & 36W with 40m sinistral d4placement; may be due to pyrrhotite.

Anomaly C correlates well with a 27m thick sequence of carbonaceous, pyritiferous argillite; no pyrrhotite reported.

weakly magnetic

E(EE) Interpolated to L31W at 6+20-6+40N

Conductor of variable thickness with a 90° dip, a depth of 5m; unit is no thicker than 15m; probably pyrrhotite (EE due to magnetic sulphides).

Drill hole 405-84-6 intersected two sulphide-rich sequences: one which corresponds to E is a 5m thick pyritiferous graphite which dips at approx. 8005 and is bound by variably altered basalts; the other more minor unit may thicken to the east to become conductor EE; in hole 6 however, one observes about 2m of carbonated and banded pyritiferous argillite at approximately 5+50S.

magnetic

Special Note

124+50W/ 5+40N and 6+00N

Drill hole 405-84-7 intersected two sulphide-rich zones which may be equivalent to conductors E & EE; in this hole the conducting zones are composed of pyritiferous arenites, graphite and chert.

?

_

W L21+00W/ ± B.L.

Conductor at 10m depth, dipping 75* to the south; pyrrhotite is probably a component.

Drill hole 405-84-12 intersected a narrow 3m band of pyritiferous argillite & arenite with a steep southerly to nearly vertical dip at a depth of 6m from the surface.

magnetic

Y L19-21W at approx. 3+00N

Probably due to conductive overburden, very weak.

According to drill hole 405-84-11 a possible cause may be a thin band of carbonaceous, black argillite; a pyrite zone occurs at 3+30N and may be related to the weak Y conductor.

?

C"

•

119-21W at approx. 4+20N

Narrow, vertical conductor at 27m on northern edge of positive magnetic feature at 10-20m depth & steeply southerly dipping; probably due to graphite.

Hole 405-84-10 intersected a 7m-wide section of altered pyritiferous argillite directly below C" at 15m depth; the unit dips at approx. 80* to the south & occurs at the boundary between interbedded andesite & gabbro on the south & clastic sediments to the north.

magnetic

--

L' L19-21W at 4+90N-5+10N

Conductor has dip of 90' at 20m depth, possibly a graphitic conductor associated with pyrrhotite.

Hole 405-84-9 intersected a series of thinly interbedded variably silicified pyritiferous argillites & carbonaceous argillites at E' dipping 80°S; depth from the surface to bedrock is estimated as 15m.

weakly magnetic

F 119-21W at 7+00N-7+50N

Conductor at 28m depth; dipping 90°, width of 8m; on south edge of a weak, broad magnetic anomaly; graphite probable cause; IP places depth of conductor at 20m,

Hole 405-84-8 intersected two wide zones of pyritiferous black argillite with graphite "under" conductor F. These zones are separated by 10m of amygdaloidal basalt; one zone is 9m wide & the other is about 5m thick; the zone is at approximately 21m depth and occurs in the midst of a series of altered basalts, andesites & gabbro.

non-magnetic

K 18-10E at about 9+50N

Narrow conductor dipping to south at 80° at a depth of 35m; massive sulphides probable cause.

Hole 405-84-1 intersected a 4m-wide zone of graphite beside a 2m-wide band of silicified pyritiferous argillite; this section correlates with conductor K; the section dips at between 85 & 87' to the south

magnetic

-21 -

circulation holes were drilled approximately 200 feet downdrift

(glaciation) from the geophysical conductors. The material returned

in the reverse circulation flow was identified, logged and sampled by

Overburden Drilling Management Ltd. of Nepean, Ontario. The rationale

behind reverse circulation drilling involves the sampling of glacial

till horizons in the hope of detecting fragments of gold, the state of

which indicate the degree of transport from their bedrock source.

Battered fragments imply long distance transport whereas delicate flakes

suggest a nearby provenance. The overburden samples were analyzed by

Bondar-Clegg Ltd. of Ottawa and Overburden Drilling Management Ltd. For

the methodology and results of these analyses please see Appendix 7.

Overall it is believed that the overburden sampling was inconclusive.

The analyses of the heavy metal concentrates, which purportedly give a

good indication of locally transported gold, produced only a few specks

of battered gold implying long distance transport.

Within the population of overburden sample results, there are many

anomalous gold values. The significance of these values cannot be

accurately gauged given three prime factors: firstly, the uncertainty

inherent in emplacement due to glacial transport during two major

glaciations; that is, one cannot assume a simple vectorial displacement

of till, other factors may be in play such as fluvial transport.

Secondly, the nature of gold analysis is often inconsistent due to the

physical properties of gold, for example, one may obtain several thousand

ppb Au on one run from a sample but in the next run less than 100 ppb.

Thirdly, and most importantly there is no standard by which to compare the

gold results to determine true anomalousness which is to say that drill

testing up-drift from the highest overburden values produced no confirma-

tion of the gold's provenance.

It would appear that the effectiveness of a reverse circulation drill

program is enhanced by the uniformity and geometry of coverage. Drilling

on a close-spaced grid would permit a more rigorous statistical handling

of the data. Furthermore, the bedrock data (depth and geology) would be

-22-

indispensable to a meaningful interpretation of the area's economic

potential. Were the Lac Gagnon project to develop at a more sober pace

such an approach would be strongly recommended. The ability to core

several feet of bedrock with each overburden test is perhaps the most

attractive feature of this sampling method.

9.0 DIAMOND DRILLING

As was previously stated, the purpose of diamond drilling was to test

various geophysical conductors and geochemical anomalies for their gold

and base metals potential as well as to develop a geological map.

All of the sulphide-rich zones which were intersected as well as promising-

looking sections in the drill core were split and assayed by Bondar-Clegg

using fire-assay and atomic absorption methods on samples prepared by

crushing and pulverization to -200 mesh.

1170 samples were analyzed for gold. Of these 216 were simultaneously

analyzed for arsenic and 70 for copper. Figure 4 presents the gold

results against the total number of samples. Clearly the majority of

samples (99.25%) fall into the 25 ppb and under bracket which implies

that any sample which returns greater than 25 ppb Au is definitely

anomalous for this population. Eight samples fall into this category:

84-3 from 486'-488': in lightly pyritiferous, fractured turbidites.

84-7 from 82'-84': altered basalt with pyrite, pyrrhotite and chalcopyrite, quartz-carbonate veins.

84-13 from 126-128': pyritiferous black argillite (4-5% pyrite).

84-7 from 217'-219': vesicular basalt no sulphide reported.

84-7 from 80'-82': altered basalt with pyrite, pyrrhotite, chalcopyrite, quartz-carbonate veins.

84-5 from 424'-426': dark altered argillites, 3-4% pyrite, carbonate-filled fractured.

84-13 from 122'-124': variably altered, pyritiferous black argillite.

84-1 from 298'-300': variably altered pyritiferous argillite, 80% pyrite over section.

105 ppb Au Hole

100 ppb Au Hole

90 ppb Au Hole

65 ppb Au Hole

55 ppb Au Hole

55 ppb Au Hole

40 ppb Au Hole

35 ppb Au Hole

Canton

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Gralserai CORIOCILAC GAGNON

. r.P. Anomaly

L AC GAGNON - CASA BERARDI

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-24 -

Although the assay results are not spectacular they nevertheless indicate

that gold is often present usually in altered rocks containing abundant

sulphides (especially chalcopyrite). There may be a lens of intense

alteration, fracturing and silicification which might be auriferous in

the vicinity of holes 405-84-6 and 405-84-7. Hole 7 especially, shows

far greater alteration and sulphide-content than any other hole. The

gold which has been detected in the quartz veins in the core may be part

of a low-grade feeder system. Further drilling would be required to test

this hypothesis.

The arsenic values fluctuated considerably. The highest value was 264 ppm

which occurred along with a 105 ppb gold value in old drill core which was

split and sampled by Westfield - this was probably due to a bit of auriferous

arsenopyrite. Within the recently drilled core, however, the highest

arsenic value was 45 ppm in pyritiferous graphite (hole 1-C1272) which had

no associated anomalous gold value. In the same hole there are two

combined gold-arsenic anomalies, C1288 and C1293 of hole 405-84-1 which

returned 35 ppm Au, 22 ppm As and 10 ppb Au and 39 ppm As. These occur

in altered pyritiferous argillite with up to 8% pyrite and graphitic

argillite with bands of massive pyrite respectively. The relative abundance

of disseminated chalcopyrite has produced several interesting assays from

hole 7. Of 70 samples which were analyzed for copper the average runs

535 ppm. Highlights from this hole include 8 samples of greater than

1000 ppm copper.

9100 ppm Z1355 sulphide-rich altered basalt quartz veins

1500 Z1366 same unit as above

1350 Z1375 altered basalt pyrrhotite and chalcopyrite clots

1500 Z1376 same as above

1350 Z1378 pyritiferous andesite 129-139 contains 30% pyrite

2900 Z1383 altered pyritiferous and chalcopyritiferous basalt

2200 Z1408 altered pyritiferous chert 10% pyrite over section

4550 Z1409 same unit as above

-25 -

These copper results bring a different light to the Lac Gagnon property.

Apart from the vague yet evident correlation of copper and gold data

(see 21352-1421), one definitely sees in hole 7 the promising effects

of alteration, along the northern contact, of the sediments and volcanics

for economic mineralization.

10.0 CONCLUSION AND RECOMMENDATIONS

The problematic nature of exploring a property in the predominantly swampy

Abitibi Lowlands is typified by the Lac Gagnon project. In an area where

outcrop is rare, or non-existent, one must rely on either relatively

inexpensive, indirect exploration methods such as geophysics and soil

geochemistry, or one must employ considerably expensive, direct methods

such as trenching and diamond drilling.

The geophysical surveys (both airborne and ground-based) have finished a

skeleton upon which to base and extend the more expensive drill data..

This process has been applied to the western block of the property with

a modest degree of success. The causes of the numerous electromagnetic

conductors and magnetic anomalies have been determined and the promise of

detecting economic mineralization (Cu-Au) in the vicinity of hole 405-84-7

has been established.

The eastern block of the property has been well covered by geophysics but

there has been no drilling to give geological meaning to the quite

different geophysical signatures. There is every possibility that one may

be looking at similar lithologies as were seen in the west, but there is

also the possibility of finding alteration and deformation of a more

exotic nature - the geophysical signature appears to indicate more intense

faulting and with this there may be a suitable environment for the

emplacement of gold.

To summarize what is known about the Lac Gagnon property one must talk

mainly of the west where one finds a broad sequence of argillaceous to

fine clastic sediments interbedded with mafic and mafic to intermediate

9°.)5

GRAPI-I OF THE DISTRIBUTION OF GOLD ANALYSES FROM

LAC GAGNON( 'DRILL CORE -

67

44

21

5 /0 15 20 15 30 .15 40 4 50 eo 65 90 too /OS no fir

PART., PR iSILLION GoLP ftOre. ( 4 )

-27 -

volcanic flows and intrusives. These units are punctuated by the

geophysically conspicuous pyritiferous graphitic argillites. Much of

the drill core displayed a mild to locally intense hydrothermal

alteration which was characterized b,y- bleaching, numerous quartz veins

and occasional quartz-carbonate veins. Some of these quartz veins

hosted the few aggregates of sphalerite and galena which were seen on

the property.

Drill hole 405-84-7 displayed a great deal of alteration much of which

was silicification and carbonation. The abundant mineralization seen

in this hole (mainly chalcopyrite associated with minor gold) appears

to point to the region along the northern conductor as having the

greatest potential for economic mineralization.

The next priority on the property is to obtain a drill section from the

eastern block perhaps in the neighbourhood of the two main eastern

conductors between lines 39+00 to 41+00E. It is estimated that 3,000

feet of drilling would establish a geological continuity from east to

west and allow some footage to further test the area around hole 405-84-7.

If this drilling program were to generate any positive results then one

might consider filling in the gaps on the metric grid and the ground

geophysics. There remains approximately 100 km of line to be cut in order

to complete the grid. Further geophysical surveys could be tailored

according to drill results.

Continued overburden drilling is not recommended unless diamond drilling

produces a more concentrated target. However, in the event of the

discovery of a gold-bearing zone by diamond drilling, overburden drilling

could be beneficial in the evaluation of a much larger area.

To conclude, the Lac Gagnon project thus far has produced a reasonable

amount of encouragement in that various sulphides have been observed on

the property some of which have a probable gold association. These

-28 -

sulphide-rich zones can, in theory, be traced using the pyritiferous

argillite horizons as geophysical markers. Further work is required

to determine whether these sulphides (mainly chalcopyrite) are parts

of a larger body or are mainly sporadic occurrences. In addition,

the eastern block of the property must be considered in its own right.

A helicopter-assisted drill program of 3,000 feet is therefore recommended

with 2,000 feet of stratigraphic drilling to be conducted in the east, and

the remaining footage to be spent in the proximity of drill hole 405-84-7

(24+50W / 5+00N). At present rates ($30/ft. inclusive) such a program

might cost approximately $130,000 all-in. This is suggested as the

minimum work commitment to properly evaluate the property.

A. E. Marr Project Geologist Westfield Minerals Limited

AEM:ds May/85

APPENDIX 1

OVERBURDEN DRILL LOGS

OVERBURDEN DRILL! NG MANAGEMENT LIMITED REVERSE CIRCULATION DRILL HOLE LOG

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OVERBURDEN DRILLING MANAGEMENT LIMITED REVERSE CIRCULATION DRILL HOLE LOG

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... , P7A,kr, ao d.....--..1..” e-" 6fiat . e coda.47 i

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C 3 ...... ) /71•11/744~- ' ii"4".40‘41,14 h Cup-aol...1

27.1- 2a r:ritr-s..reire t ---.1t -

// / _ - _ : _ _ - - - _ _ - — ... -

E_ _ _ _ _ _ _ - .. - _ - E - — _ - - —

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11.-.4...-./ cac.....

APPENDIX 2

DIAMOND DRILL LOGS

NTS WESTFIELD MINERALS LIMITED PROPERTY AREA LAC AGN0N

Depth 495'

Location 18+88E/9+00N

Logged AEM

Started 21/10/84

Completed 24/10/84

0 • , > FROM TO DESCRIPTION 4" '8 s',I SAMPLE FROM TO C.L. ppb Au ppb Ag ppm As

CC

CA= 0 107.5 Overburden/casing 0° % .

107.5 108.5 ARGILLITE/SILTSTONE: 40'100 C1251 108.5 109.8 . <5 <2 108.5 109.8 GREYWACKE: 52 109.8 111.8 <5 <2

- dark grey-green,f.gr. rock E numerous small white fragments 53 111.8 113.8 5 3 (may be original play. XLs or authigenic Carbonate; some 54 113.8 116.0 k5 2 dissem'd py & po XLs (<1%). ADD: small frays. may be 55 124.0 126.0 <5 <2 Al 2

S1O2'

i.e. (andalusite, kyanite, sillimanite).

109.8 115.8 ARGILLITE/SILTSTONE: 56 137.6 139.8 <5 2 - dark f.gr.with increasing level of alteration towards the

bottom of the section: very fine, streaked po is abund. throughout and esp. in bleached or silicified fractures.

30' 65

115.8 116.0 FRACTURED & ALTERED CONTACT: - carb (?) - filled fractures appear to be responsible for a

narrow alteration halo; some limonite on fracture surfaces. 116.0 116.7 GREYWACKE: 116.7 118.3 ARGILLITE/SILTSTONE: 118.3 118.5 GREYWACKE: 118.5 122.5 BANDED ARGILLITE: 48° 80 122.5 128.1 ANDESITE: 40° 100 •

- med. gr. (granular) green rock; msv with no distinct fabric; upper & lower contacts are knife sharp & appear to cross cut the bedding of the bounding units implying that the rock is intrusive.

.

- 55% play. (albite-andesine?) 30% pyroxene 15% chlorite. - late fracture planes are often covered with a chloritic smear

& botryoidal py which is also associated with carbonate. 128.1 137.6 INTERBEDDED ARGILLITES & GREYWACKE: 47°

- thin altered section at 135.6 - bleached buff & pale green with minor po

137.6 139.8 MAFIC TO INTERMEDIATE CRYSTAL TUFF (PORPHYRITIC): 47° - probably a waterlain volcanogenic sediment; has a distinc-

tive porphyritic texture, i.e. white to grey-white XLs (cont'd page 2)

Azimuth 000 0 Tests 495' = 470 Hole 405-84-1

Core BQ

ClaiM

Latitude Departure

Elevation

Dip -50° Sheet 1 0 5

HOLE 405-84-1 SHEET 2 OF 5

FROM TO DESCRIPTION 2.. NtdiT w

> _ 8 E. SAMPLE FROM TO C.L. ppb Au oz Au/t ppm As

(K2mm) in a med-fine gr. matrix - green-buff; matrix also appears to contain an argillaceous component; good foliation.

139.8 143.0 GRITTY ARGILLITES:

143.0 148.5 MAFIC TO INTERMEDIATE PORPHYRITIC CRYSTAL TUFF: C1257 144 146 <5 <2

148.5 150.8 GRITTY ARGILLITE:

150.8 152.5 MAFIC TO INTERMEDIATE PORPHYRITIC CRYSTAL TUFF: t

152.5 161.9 GRITTY ARGILLITE WITH CRYSTAL TUFF COMPONENT: -

161.9 166.0 MAFIC TUFF/BASALT: - fine gr., green, poss. fine gr. XL tuff; some crystalline

material visible.

166.0 180.2 BANDED ARGILLITES: 80 C1258 178 180 <5 <2 - black to dark brown; lower 5 feet of section is variably

silicified; some py & po on fracture surfaces.

180.2 182.8 MAFIC TO INTERMEDIATE PORPHYRITIC CRYSTAL TUFF: 90 - silicified sections below & above this unit may in fact imply

that it is in intrusive rock.

182.8 191.6 BANDED ARGILLITES: silicified section at top foot 35° C1259 182.8 185 <5 <2

191.6 194.9 SILICIFIED ARGILLITE: C1260 191.6 193.5 <5 <2 - very fine gr.; lighter grey than other argillites. 61 193.5 194.9 < 5 3

194.9 213.0 BANDED ARGILLITES:

213.0 218.5 EXHALITIVE SEDIMENT(?): 85 C1262 213.0 215.0 <5 3 - appears to be a very siliceous (also carb'd), highly py's 63 215.0 217.0 <5 4

sediment (15-25% py); graphite occurs locally in thin bands. 64 217.0 218.5 <5 9


FROM TO DESCRIPTION '4:3' _ .i

> _ F.:-c_ m

SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag ppm As

218.5 235.0 PYRITIFEROUS GRAPHITE: 50 C1265 218.5 220.0 5 20 - py is abundant to msv, rating about 10% over the entire 66 220.0 222.0 <5 9

section 67 222.0 224.0 <5 27 - a green, possibly volcanic component (greenish) is mixed 68 224.0 226.0 <5 11

with the graphite in the upper 6 feet of the section; the 69 226.0 228.0 <5 15 graphite & the pyrite occur as compressed "nodules"; strong 70 228.0 230.0 <5 24 conductor. 71 230.0 232.0 <5 15

72 232.0 235.0 <5 45 235.0 244.2 SILICIFIED (CHERTY) PYRITIFEROUS ARGILLITE: 45' 73 235.0 237.0 <5 7

- banded unit containing overall 25-30% py in nodular & 74 237.0 239.0 5 6 dissem'd form; sediment is generally grey & very fine 75 239.0 241.0 (5 2 grained; some sections contain "swirled" bedding & what 76 241.0 242.5 < 5 6 appears to be a few unconformities. 77 242.5 244.2 4 5 5

244.2 257.0 CARBONACEOUS BANDED ARGILLITE: 78 244.5 246.0 <5 9 -v.fine gr. to gritty; some dissem'd py & occass., large py C1279 ? ? <5 7

nodules (254.5) up to 2-3 cm lengthwise. C1280 ? ? 10 2

257.0 266.1 GREYWACKE: - fine to coarse; dark buff-brown; some minor argillaceous

bands; some irreg. bleached qtz-carb-filled fractures.

266.1 271.9 BASALT/VOLCANIC SEDIMENT: - similarly textured to the greywacke with a distinct colour

change to green (-1.chl.); fine to med. gr. with abundant fine crystalline fragments; one amygdule at 268.3 & a cluster of amygdules at the base would favour this unit being a basalt; msv; some local alteration.

271.9 289.0 INTERBEDDED ARGILLITE & GREYWACKE: C1281 271.9 274.0 <5 <2 - argillites contain nodular py. while the coarse grained 82 274.0 276.0 <5 5

greywackes contain an abundance of dissem'd to fine grained py. (10% over section).

83 276.0 278.0 <5 3

289.0 289.9 AMYGDALOIDAL BASALT: 84 289.9 292.0 <5 <2 - amygdules are abundant & account for 50-60% of the section;

flecks of py are also common at 8-10%; matrix appears to be intermed. in compos.


FROM TO DESCRIPTION 4(3.; > gt SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag ppm As

289.9 308.2 VARIABLY ALTERED PYRITIFEROUS ARGILLITE: 50' 80 C1285 292.0 294.0 <5 5

- silicification/carbonation at 294.5' (.5'), 303.2-304.5 86 294.0 296.0 ' <5 9

(intense brx.); 305.5-307.3 (irreg. bleached fracturing 87 296.0 298.0 <5 34

& local recrystallization); py is variably abundant 88 298.0 300.0 35 22

(8%/section); variably conductive. 89 300.0 302.0 <5 12

90 302.0 304.0 <5 21

308.2 312.6 GRAPHITIC ARGILLITE & MASSIVE PYRITE: 40' 91 304.0 306.0 <5 15

- uppermost foot is approx. 60% black, carbonaceous argillite 92 306.0 308.0 <5 11

with 40% "swirled" pyrite; 309.4-310.9 is 80-85% py (fine gr.) 93 308.0 310.9 10 39

with 15-20% wispy argillite; 310.9-312.6 is characterized by a green, very fine gr. clayey matrix in which are suspended a snowflake pattern of carbonate crystals & fine dissem'd py-.may be flow top indicator in basalt.

94 310.9 312.6 <5 13

312.6 321.0 ALTERED ARGILLITE & GREYWACKE: - section is characterized by an abundance of bleaching fractures at",40° to the main core axis; there appears to be an orthogonal set of fractures which cross-cuts the bedding plane.

321.0 322.4 ALTERED BASALT: - similarly cross-cut by bleaching fractures as unit above.

322.4 328.2 ALTERED ARGILLITE & GREYWACKE: 95 - as above

328.2 330.9 ALTERED BASALT:

330.9 333.4 ALTERED ARGILLITE & GREYWACKE:

333.4 334.8 ALTERED BASALT (AMYGDALOIDAL?):

334.8 346.0 ALTERED ARGILLITE & GREYWACKE:

346.0 351.0 CHLORITIC ARGILLITE/FINE GRAINED BASALT: - notable decrease in degree of fracturing in this unit.


FROM TO DESCRIPTION c) • 4-).< KILig

u > >. 3 s_

Iv SAMPLE FROM TO C.L. ppb Au oz Au/t ppb A9 ppm As

351.0 363.6 PSEUDOBRECCIATED ARGILLITE & INTERCALATED GREYWACKE WITH DARK CHERT: 95 C1295 351.0 353.0 5 2 - degree of fracturing has created a pseudo brx'd texture 96 353.0 355.0 5 2 throughout section; some large fractures (i.e. .2-.3 feet) 97 355.0 357.6 5 2 have been filled with qtz-carb; 355.2-357.2 contains mainly 98 357.6 359.6 5 2 buff-brown greywacke intercalated with dark grey chert - 99 359.6 361.6 5 2 this may indicate exhalitive activity concurrent with sediment dumping from a nearby foreland; some thin bands of near-massive py & some nodular py.

C1300 361.6 363.6 5 2

363.6 413.2 ALTERED ARGILLITE & GREYWACKE: C1301 393.0 395.0 5 2 - section has several greenish units Which may indicate some

distal, volcanic activity; pyrite spheroids occur abundantly around 394'; py also occurs commonly in fractures with qtz It carb.

413.2 425.2 ALTERED BASALT?/CHLORITIC ARGILLITE: 60° 90 C1302 421.0 423.0 30 2 - essentially same unit as found at 310.9-312.6; bright green, fine grained rock with snowflake patterned crystals

100

(qtz-carb?) & abundant wispy & dissem'd pyrite in matrix; cp at 422.2; bleaching, cross-cutting fractures are very common in upper half of section (py: 10%/section).

425.2 434.9 PORPHYRITIC DIORITE (INTRUSIVE): C1303 425.0 427.0 <5 <2 - coarse-grained, grey, intermed. matrix with white plag. 04 427.0 429.0 <5 <2

phenocrysts & lathed dark green amphiboles (which delineate 05 429.0 431.0 <5 <2 the foliation). 06 431.0 433.0 <5 <2

07 433.0 435.0 <5 <2 434.9 446.2 ALTERED BASALT?: 08 435.0 437.0 <5 <2

- same unit as above (413.2-425.2). 09 437.0 439.0 <5 <2 10 439.0 441.0 <5 <2

446.2 490.9 ALTERED ARGILLITE: 11 441.0 443.0 <5 <2 - intense bleached fracturing; some minor arkosic sections 12 443.0 445.0 <5 <2

scattered to finely dissem'd py. 13 445.0 447.0 <5 <2

490.9 495 PYRITIFEROUS BLACK ARGILLITE: 50° 80 14 491.0 493.0 <5 4 - blocky & fractured core; py is localized (7%/section). 15 493.0 495.0 <5 4

- [Oil -

NTS UESTFIELO MINERALS LIMITED PROPERTY AREA LAC GAGNON - QUEBEC

Started 29 Oct./84

Completed 1 Nov./84

Departure Depth 597'

Elevation • Core BQ

Location 2+005/34+40W

Logged AEM

Claim Azimuth 0000

Latitude Dip -45°

Hole 305-84-2

Sheet 1 of 4

Tests

at 597' - 42°

FROM TO DESCRIPTION SAMPLE FROM TO •

C.L. Core Re- coverv

PPb Au PPb Ag 4...LC.A. 90=_LCA ppm As

0 56 casing 56.0 116.0 PYROXENE GABBRO: C1316 56 58 ' 45 <2

- medium- to coarse-grained intrusive rock; altered (wide-spread 17 58 60 <5 4 carbonation?); large, dark green, lathy pyx LXs supported in a very 18 87 89 95-100 <5 40-55° <2 fine grained feldspathic, chl'c, & carb'd(?) matrix; coarseness of 19 89 91 <5 <2 rock texture seems to be directly porportional to the amount of 20 91 93 <5 3 interstitial carbonate; pyx XLs show good preferred orientation; 21 93 95 <5 <2 some minor sulphides especially in carb.-filled fractures; 22 95 97 <5 <2 mineralized quartz vein at 93.0' )po': 5% over 10 cm); numerous carb'd fractures perpendicular to main foliation.

23 97 99 <5 <2

116.0 122.7 SILICIFIED GREYWACKE: C1324 116 118 <5 <2 - partially bleached, very fine-grained greywacke; probably 25 118 120 <5 <2

recrystalized during gabbroid intrusion; bleached fractures would 26 120 121.5 <5 <2 appear to be pre-intrusive or at best, syngenetic; some 27 121.5 123 <5 <2 • homogeneous sections are altered argillite; some large chl.-filled

fractures run coplanar with core axis. . .

122.7 137.9 ALTERED PYROXENE GABBRO: - finer grained than gabbro above, more intensely cross-cut by fractures; suggesting either two or more phases of bleached fracturing or one phase roughly contemprareous with emplacement.

137.9 177.5 SILICIFIED TUFFACEOUS FLOWS(?): C1328 137 139 <5 16 - very altered unit; generally dark gray with some green sections; 29 139 141 <5 25

very fine-grained; mainly plag, some mafic minerals (biot, chi, 30 141 143 100 <5 50° <2 pyx(?)); forcibly intruded by some large irreg. veins containing 31 143 145 <5 . <2 hydrothermal minerals (qtz, ank, rhodochr., tourmaline(?), porph'c 32 145 147 <5 <2 plag; also a garnet-like mineral(?); some vuggy sections with 33 147 149 <5 <2 large qtz. - possibly celestite XL? 34 149 151 <5 <2

HOLE 405-84-z SHEET 2 OF 4

FROM TO DESCRIPTION SAMPLE FROM TO C.L. Recovery

ppb Au oz Au/t ppb Ag 41.1C.A. 90=1._CA

ppm As

177.5 179.2 ALTERED BASALT/CHLORITIC ARGILLITE: C1335 151 153 <5 2 - dark gray to green; volcanic (flow top?), contains abundant porph'c, 36 153 155 <5 3

mauve amygdules or crystals; described as snowflake texture in 37 155 157 <5 11 405-84-1; minor banded pyrite. 38 157 159 <5 22

39 159 161 <5 ' 30 179.2 180.4 PYRITIFEROUS GRAPHITE: C1340 161 163 <5 36

- highly conductive graphite with 15% banded & dissem'd py. 41 163 165 10 21 42 165 167 90% <5 50° 24

180.4 188.6 VARIABLY SILICIFIED GREYWACKES & BRANDED ARGILLITES: 43 167 169 <5 6 - generally fine-grained, bleached sediments; sporadic py-filled 44 169 171 <5 4 fractures; good examples of microfaulting along bedding planes 45 171 173 5 7 (esp. @ 188'); some rhodochrosite in fracture at 186.1'. 46 173 175 <5 <2

47 175 177 <5 <2 188.6 197.0 PYRITIFEROUS GRAPHITE & QUARTZ VEINING: 48 177 179 <5 5

- soft, very conductive graphite with abundant stringers of yrite; 49 179 180.4 35% 5 2 two small qtz veins intrude the section at 188.9 (7.5 cms) & at C1350 180.4 182 <5 <2 approx. 190'; core is very blocky; approx. 15% py over section. 51 182 184 <5 <2

52 184 186 <5 <2 197.0 221.8 FAULT BRECCIATION ZONE IN ARGILLITES: 53 186 188.6 <5 2

- mainly banded argillites in fine to coarse breccia; groundmass is 54 188.6 191.0 40% <5 <2 carbonate, some py in fracture surfaces.' • 55 191 193 <5 <2

56 193 195 15 4 221.8 237.5 GREYWACKE?/ANDESITE TUFF?: 57 195 197 35% 15 8

- dark brown matrix, speckled with light feldspathic fragments; bears some compositional resemblance to pyroxene gabbro; numerous bleached fractures; some poorly preserved compositional banding implies some form of sedimentary deposition; may also be andesitic water-lain crystal tuff.

237.5 239.9 BASALT: - greenish, partially recrystallized basalt; possible flow top at

239.4 indication tops to south.

239.9 289.2 GREYWACKE: - coarse to fine-grained, generally dark grey-brown; localized

bleached fractures. 50°

•


FROM TO DESCRIPTION SAMPLE FROM TO C.L.

Recovery ppb Au oz Au/t ppb Ag UC.A.

90=1_CA ppm As

289.2 294.5 TUFFACEOUS WACKE: - increased greenish component (chlorite) may indicate increased

volcanic sediment at time of deposition; wacke texture - med- to coarse-grained. .

294.5 367.0 VARIABLY TEXTURES GREYWACKES: ,

- very finely bedded to broadly bedded, fine-grained to very coarse- grained; mainly brown with greenish colour in neighbourhood of bleaching fractures; some minor py in fractures.

95%

367.0 374.0 ALTERED TUFFACEOUS WACKE/BASALT: - bright, distinctive green with numerous irreg. carb-filled fractures; some py in fractures.

700

374.0 382.5 GRAYWACKE:

382.5 386.7 ALTERED TUFFACEOUS WACKE/BASALT

386.7 388.1 GRAYWACKE

388.1 389.6 TUFFACEOUS WACKE/BASALT?

389.6 396.9 GRAYWACKE

396.9 398.3 TUFFACEOUS WACKE/BASALT?: - is probably an altered graywacke with recrystallized chlorite.

398.3 439.2 VARIABLY ALTERED GREYWACKES & GRITTY ARGILLITES: C1358 414 416 <5 60-620 <2 - some minor qtz. veining at 417.8, 420.5, minor py mineralization. 59 416 418 95-100% <5 <2

C1360 418 420 <5 <2 439.2 441.9 ALTERED BASALT/ANDESITE: : 61 420 422 <5 <2

- abundant plag, amount of qtz is uncertain up to 15%, hornblende in fine, irregular, brown laths; msv, no pronounced foliation.

441.9 471.4 GRAYWACKES & BANDED ARGILLITES: - significant increase in number of discrete argillite bands. 50°


FROM TO DESCRIPTION SAMPLE FROM TO C. L.

Recovery ppb Au oz Au/t ppb Ag 411.C.A.

90=i_CA ppm As

471.4 475.2 ALTERED BASALT

475.2 559.0 GRAYWACKES & ARGILLITES: - monotonous sequence of thinly to grossly interbedded graywackes & C1362 500 502 95-100% <5 60° 4

argillites punctuated by small quartz veins at 505.2, 505.6, 529.0, 63 502 504 <5 5

536.0, 540.0; generally barren with rare dendritic py 4% qtz veins 64 504 506 <5 2 are associated with intensely fractured sections (i.e. bleaching). 65 506 508 <5 3

66 508 510 <5 • 4 559.0 560.3 BASALT/TUFF: 67 526 528 10 <2

- partially recrystallized volcanic flow or sediment; knife-sharp lower 68 528 530 <5 3 contact; ragged upper contact (may be overturned tops to N?). . 69 530 532 <5 <2

C1370 532 534 <5 6 560.3 595.0 GRAYWACKE & BANDED ARGILLITE: 71 534 536 <5 3

- generally knife-sharp upper contacts with some faint upward grading 72 536 538 95-100% <5 64° 2 downwards in the hole, once again suggesting tops to the N. 73 538 540 <5 2

- EOH -

'

Logged AEM

Started 1 Nov./84

acid test at 625' m Sheet 1 of 4

43° Latitude Dip -45°


BQ Completed 4 Nov,/84 Elevation • Core

?fiUCkYY Ai(EA LAC GAGNON - QUEBEC

Location 34+40W/0+85S Claim Azimuth 000° Hole 405-84-3 Tests

FROM TO DESCRIPTION SAMPLE •

FROM TO C.L.

Recovery ppb Au ppb Ag 4 C.A.

• . 0 102 casing .

102 109.8 GRITTY ARGILLITE & GRAYWACKE C1374 105 107 <5

109.8 113.0 ALTERED BASALT? INTRUSIVE?: C1375 110 112 <5 - green, medium-grained to porph'c rock, contains numerous large crystals (1-2 mm) which may be corroded fspars (lab-bytownite) or pyroxenes; some fine-grained irreg. frags may be pieces of country rock; lower contact is knife-sharp - upper contact is indistinct.

113.0 151.2 GRAYWACKE g (BANDED) ARGILLITE: - typical sequence of thinly & coarsely interbedded graywacke & C1376 144 146 <5 . 50° @ argillite; increasing abundance of thin carbonate bleached 77 146 148 <5 130' fractures towards the bottom of the section - alteration halo around fractures is a distinctive gray-green; most fractures are

78 148 150 <5 ,

' approx. 450 off the core axis but one set is very close to coplanar with the core axis: some minor dissem'd sulphide (4.1.1%/section). •

_ 151.2 156.6 ALTERATION ZONE IN GRAYWACKE(?):

- coarse, recrystallized graywacke - appears to be a gradational contact on top & bottom; central part of section contains a one cm- wide qtz-carb vein at 155.1' with some unidentified blue minerali-zation; two conspicuous zones have a slush-brecciated texture; i.e., an intrusion by a qtz-carb solution (possibly endogenetic) with a resultant recrystallization of wall-rock within the slush zone - hence a fine breccia.

.



ppb Au oz Au/t pPb Ag 4 CA

156.6 329.3 GRAYWACKE & ARGILLITE: C1379 160 162 <5 70°@175 - typical sequence; a few contacts (truncated bedding, grading) C1380 162 164 <5 62°@210 indicate that the sediments are not overturned but young to the 81 164 166 <5 40°@240 south; fracturing is of low intensity but some small sections dis- 82 186 188 (5 55°@267 play good alteration; fault brx'n at 191.5, 223.5; small qv is at 83 188 190 <5 600@285 232.2 & 244.9; some fine disseminated sulphide in some subsections; 84 190 192 90% <5 some good evidence for small scale faulting along several of the 85 192 194 <5 bleached fractures; fractures appear to be in the ab plane of a 86 194 196 <5 synclinal fold; fault brx. at 271.5; argillaceous comp. increases 87 222 224 <5 250-280; small qv at 305.8'; excellent fault-brx at 308.5'. 88 231 233 <5 600

89 244 246 <5 @ 330' 329.3 332.8 CHLORITIZED, PARTIALLY RECRYSTALIZED ARGILLITE: C1390 270 272 <5

- med-fine grained homogeneously green rock; fine hairline fractures 91 305 307 95-100% <5 may be responsible for alteration; small qcv's at 330.2 &-331.2 92 308 310 <5 associated with clots of chi. 93 329 331 <5

94 331 333 <5 332.8 391.9 ARGILLITES & MINOR GRAYWACKE: 67°

. - variably altered section of typical argillites; main altered section 95 348 350 <5 @ 379' runs from 348 to 365 feet; alt'n consists mainly in very localized 96 350 352 <5 intense bleached fracturing & irreg. qv veining. 97 352 354 <5

98 354 356 <5 391.9 397.0 ALTERATION ZONE IN ARGILLITES: 99 356 358 <5

- discrete beds of recrystallized argillite interbedded with variably altered & silicified argillite; recrystallized sections are charactarized by 1-2 mm mauve to buff crystals suspended in a fine to medium-grained groundmass (may be alumino-silicates).

C1400 358 360 <5

397.0 408.9 ARGILLITE: - typical black argillite with increasing alteration lower in the section.

• 408.9 411.2 PORPHYRITIC ANDESITE: C1401 408.9 411.2 <5

- medium- to coarse-grained rock composed mainly of fspar. qtz. chi.; fspars occur as large gray-white subhedral crystals & as the bulk of the groundmass; chi appears to be an abundant interstitial mineral with qtz as occasionally visible blebs; upper contact indis-tinct, lower contact knife-sharp; may be intrusive.



ppb Au oz Au/t ppb Ag 4 CA

411.2 428.4 VARIABLY ALTERED ARGILLITES: • 53° - partial recrystallization in some sections; small scale slip along

foliation planes. @ 417'

428.4 430 ALTERED BASALT: - green, med-grained rock with a few amygdules; lower contact sharp,

upper contact indistinct.

430.0 453.1 ALTERED & DEFORMED ARGILLITES: C1402 430 432 <5 - weakly silicified; local, intense qtz-carb-filled fracturing with 03 432 434 ' <5 small-scale "en echelon" shear deformation at 441.0-441.5; several 04 434 436 <5 annealled fault brecciae; locally pyritiferous/marcasite(?). 05 436 438 <5

06 438 440 <5 453.1 455.9 ALTERED BASALT: 07 440 442 95100% <5

- rare amygdules; med-grained rock; fractured & blocky. 08 442 444 <5

455.9 466.4 GRAYWACKE & ARGILLITE 09

C1410 444 446

446 448

<5 <5

. •

11 448 450 <5 466.4 471.8 AMYGDALOIDAL BASALT: 12 450 452 <5

- some sections are intensely amygdaloidal & may represent flow tops 13 460 462 <5 57' of a finer grained flow; amygdoloidal sections at top of section ' @ 467' (10 cm) & at 469.5 (1 cm); basalt is fine grained & some sections may in fact be altered argillite.

471.8 497.8 TURBIDITES: ARGILLITE & GRAYWACKE: 14 480 482 <5 • - some subsections would appear to display a grading or upward fining, 15 - 484 <5 from coarse graywackes upwards through black argillites which is 16 - 484 <5 66° again capped by a similar sequence; the implication is younging to 17 - 488 95-100% 105 @ 486' the south; i.e. not overturned; degree of fracturing is quite 18 - 490 <5 intense in this section with the amount of sulphide mineralization 19 - 492 <5 similarly increasing.,' C1420 - 494 <5

21 - 496 <5 497.8 569.6 ALTERED PYRITIFEROUS ARGILLITES: 22 - 498 . <5

- some well silicified & py's sections 502-509; 546.5-approx. 553.5'; 23 - ' 500 <5 this section displays some good fault brecciation in various stages 24 - 502 90-100% <5 of development - at 545' there is a very coarse breccia welded with 25 - 503.5 (blocky) <5 carbonate & rock flour; the beginning of a haemotite alt'n zone is 26 - 505 <5 found at 556' and downwards - here one tends fb find reddish-orange 27 - 507 5 streaks in the rock (may also be rhodochrosite); the alt'n is 28 - 509 <5 65° probably related to the major fault just below this section. 29 - 511 <5 @ 502'

fault plane

bedding


SAMPLE FROM TO C.L. Recover)

pPb Au oz Au/t ppbAg A CA

C1430' 513 75-80% <5 65° 31 - 515 blocky <5 @ 502' 32- 517 & frac- <5

33 - 519 tured) <5 62° 34 521 <5 @533' 35 523 <5 36 - 525 <5 37 - 527 <5 38- 529 <5 39 531 <5

C1440 - 533 <5 41 - 535 70% <5 42' 537 'blocky <5 43 539 & frac- <5 44 - 541 tured) <5

45 - 543 <5 46- 545 <5 47 - 546.5 80% <5 48 - 548 <5 49 - 550 <5

C1450- 552 <5 Z1001- 553.5 <5

02 - 560 562 <5 03 - 564 <5 04 566 <5 55.,

05 568 <5 @ 610' 06- 570 <5 07 - 572 <5 08 - 574 <5 09 - 576 <5

Z1010 578 <5 11 580 <5 12 582 95% <5 13 584 <5 14 594 596 <5 15 598 600 <5 16 606 608 <5 17- 616 618 <5

FROM TO DESCRIPTION

AMYGDALOIDAL BASALT & MAJOR FAULT BRECCIA: - fault breccia becomes very coarse in lower part of section; spectacular textures of country rock frags welded in carbonate & rock flour matrix.

PYRITIFEROUS & ALTERED ARGILLITE IN MAJOR FAULT BRECCIA: - heart of fault is in this section; fault appears to be in a plane coaxial with the strike of the rocks but perpendicular to the bedding (see below):

some well-mineralized sections 579'-583'.

ARGILLITE & GRAYWACKE WITH MINOR FAULT EPECCIA: - thinly interbedded argillite & graywacke with localized zones of fault brecciation - some breccia are well mineralized, e.g. 595-595.4; 598.9-599.0; 606.5-607.0; 617-617.3; haem. alt'n continues to bottom of hole

- EON -

596.6

574.0

583.0

574.0

583.0

625

Depth 324'

• Core BQ

Claim

Latitude

Departure

Elevation

Tests None Hole 405-84-4

Sheet 1 of 3

Azimuth anon

Dip -450

'Location 34+40W/0+15N

Logged Alex E. NUrr

Started Nov. 5/84

Completed Nov, 9/84

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag AI C.A. Recoveryr

0.0 164.0 CASING Z1018 164 , 165.7 65@210' 19 167.5 164-200 1 70@222'

164.0 294.9 ALTERED ARGILLITES AND EXTENSIVE FAULT BRECCIATION 20 169.2 70% 60°262' -this wide section is predominantly composed of dark, fine-grained 21 171.0 <5

silicified argillites with abundant dendritic and streaked pyrite 22 172.7 200-237

blebs 23 174.4 95% I

'

-approx. 6-7% pyrite over section 24 176.2

-core return is generally poor with abundant fault brecciation 25 177.9 237-251 10

-core is intensely streaked with bleached fracturing 26 179.7 70%

-unlike other holes, the fracturing is very irregular 27 181.4 28 183.1 251-290

208.5 -- small irregular dark qtz vein 29 184.9 95% 212.0-212.5 -- greywacke 1030 186.6 212.5-227.0 -- banded argillite (due to increased clastic content) 31 188.3 290-293 237.0-249.5 -- zone of intense fault brecciation (sub-mylonitic 32 190.1 70%

textures); zone also contains some highly altered 33 191.8 veinlets of qtz-carbonate 34 193.6 <5

252.0 -- coarse fault brecciation (6") 35 195.3 293-304

-strong evidence of faulting throughout remainder of section; 36 197.0 90%

260.0-294.9' is particularly fine-grained, silicified and py's 37 198.8 304-311 60% -qtz-chlorite veinlets in fractures which run paralel with the 38 200.5

core axis are particularly common in the lower section 39 202.3

-the hematite alteration zone which accompanied the fault in hole 1040 204.0

405-84-3 starts at approx. 227' and continues to the end of the 41 205.7

hole 42 207.5 43 209.2 15

294.9 312.0 MYLONITE ZONE 44 211.0

-presumably a welded rock flour in the walls of a significant fault, 45 212.7

all original textures have been obliterated 46 214.4 10

-at 298' rock takes on a green colour perhaps because of a volcanic Z1047 , 216.2 10

PROPERTY AREA LAC GAGNON WESTF-HLD MINERALS LIMITED NTS

HOLE 405-84-4 SHEET 2 OF 3 .

FROM TO DESCRIPTION

.•

SAMPLE FROM TO

.

C.L. ppb Au ppb Ag

' 294.9 - 312.0 (con't) Z1048 216.2 217.9 <5 49 219.7 <5 • •

lithology in the fault zone or due to a crecrystallization of 50 221.4 <5 chlorite from the argillite within the fault 51 23.1 5 -at 311.0-312.0 there is a dense grey-green mud seam 52 224.9 5

53 226.6 •

312.0 323.0 VOLCANIC ? BASALT . 54 228.3 55 230.1 • 56 231.8

• 57 233.6 . 58 235.3

59 237.0 1060 238.8 61 240.5 62 242.3

' 63 244.0 . 64 245.7

65 247.5 • 66 249.2

67 251.0 68 252.7 69 254.4 ,

• . 70 256.2 • <5 1071 257.9 .

• 72 259.6 73 261.4

• 74 263.1 75 264.9 76 266.6 77 268.3

. 78 270.1 . . • 79 271.8

1080 273.6 81 • 275.3 82 277.0 83 278.8 84 280.5

. 85 282.3 86 • 284.0 -87 285.7

21088 287.5


FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 4.1..C.A.

Z1089 287.5 289.2 90 291.0 91 292.7 92 294.4 93 296.2 94 297.9 95 299.7 96 301.4 97 303.1

, 98 304.9 99 306.6 45

Z1100 308.3 01 310.1 02 311.8 03 313.6 04 315.3 05 317.0 06 318.8 07 320.5 08 322.3

Z1109 324.0

MIS WESTFIELD MINERALS LIMITED PROPERTY AREA LAC GAGNON

Location 34+40W/0+80N

Logged A. E. Marr

Started 9 Nov/84

Completed 13 Nov/84

Claim

Latitude

Departure

Elevation

Azimuth 0000

Dip -45°

Depth 647'

• Core BQ

Tests test at 647' Hole 405-84-5

42° Sheet 1 of 41

FROM TO DESCRIPTION SAMPLE FROM

i

TO C.L. ppb Au ppb Ag 741..Lc.A.

0 138 casing 21203 162. 164

LO

LO

LO

ID Lil LL

, LO

LO LC

1 LO

LI, L

O in

LO

in in LO

LO

VV

VV

Nev v

s,V

V .......

v

V

4 164 166 138 161.5 GRITTY ARGILLITE AND GREYWACKE: 5 166 168 60-700

- typical to slightly altered sediments; banding/bedding quite 6 168 170 evident; some local sections appear to be sheared (140.7-142) and 7 170 172 display a smeared porphyritic texture; very minor disseminated 8 172 174 sulphide («1%); occasional bleached, carbonate-filled fractures. 9 174 176

1210 176 178 161.5 163.6 DIABASIC INTRUSIVE: 11 178 180

- fine-grained (aphanitic) gray rock with fine porphyritic texture; 12 196 198 upper contact is very irregular with chloritic and pyritized halo 13 206 208 in country rock; lower part of section is suddenly coarser grained 14 212 214 with abundant carbonate blebs; lower contact is less distinct than 15 214 216 upper. 16 216 218

. 17 218 220 163.6 165.5 SILICIFIED/CARBONATED GREYWACKE?: 18 220 222

- some abundant carbonate-filled hairline fractures; mineralized 19 240 242 quartz-carbonate vein at 165.2-165.5; contains pyrite, pvrrhotite, 1220 242 244 chalcopyrite, sphalerite (1-2% of quartz-carbonate vein). 21 244 246 .

165.5 178.9 COARSE GREYWACKE AND BANDED ARGILLITE: - some sections contain abundant clots of pyrite (5-7% over 6"); thin,

highly irregular diabase intrusion at 175-176.5.

178.9 185.5 ALTERED DIABASE: - section is characterized by lathy, corroded feldspar crystals in a

dark fine-grained matrix; section of argillite at 184.0-184.4.

185.5 192.7 FINE ARGILLITE WITH DIABASE DIKELETS: - lower part of section is predominately diabase with irregular small blebs of pyrite; up to 3% over 6" sections.

. .


FROM TO

-

DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 44.C.A.

192.7 250.9 FINE ARGILLITE WITH MINOR GREYWACKE: 65° - some slfght alteration often associated with fine carbonate-filled fractures; occasional irregular quartz veinlets; en echelon fracturing well-developed (especially at 218')

250.9 280 AMYGDALOIDAL BASALT FLOWS: Z1154 300 302 <5 - variability of textures implies the superposition of several basaltic 55 302 304 ' <5

flows; lower part of section from 268' to end of section is badly 56 104 306 <5 ground and blocky; this could be in part due to water-conducting 57 306 308 <5 fractures within a fault zone; there is very little in the way of 58 308 310 <5 fracturing or alteration through most of this unit. 59 310 312 <5

Z1160 312 314 C5 280.0 281.7 CARBONACEOUS ARGILLITE: 61 314 316 <5

- very blocky section of very slightly conductive argillite. 62 316 318 c5 63 318 320 <5 •

281.7 303.5 AMYGDALOIDAL BASALT: 64 320 322 (5 - fine to medium-grained basalt with occasional amygdules. 65 322 324 <5

66 324 326 <5 303.5 348.5 ALTERED, PYRITIFEROUS ARGILLITE: 67 326 328 <5

- section is characterized by variable pinkish-red haematite 68 328 330 <5 alteration; fine quartz-carbonate veinlets; pyrite occurs as fine 69 330 332 <5 1-2 mm snowflake-like blebs up to 3% over 1-foot subsections; some Z1170 332 334 <5 silicification is noted especially in the pyritiferous sections; 71 334 336 <5 mud/sand seam at 339-340; section becomes increasingly conductive 72 336 338 <5 towards the base of the section implying increased carbon/graphite 73 338 340 <5 content. 74 340 342 <6

75 342 344 <5 348.5 359.0 CARBONACEOUS PYRITIFEROUS ARGILLITE: 76 344 346 <5

- variably altered, partially silicified argillite with generally 77 346 348 <5 abundant fine-grained pyrite (up to 20% over 4') disseminated to 78 348 350 <5 massive; coarse crystalline pyrite and dark gray "black smoker" type 79 350 352 <5 pyrite also occurs; well-ground core. Z1180 352 354 <5

81 354 356 5 359.0 366.0 REWORKED FAULT BRECCIA IN BASALT: 82 356 358 <5

- also pyritiferous (5% over section). 83 358 360 5 84 360 362 5 85 362 364 <5 86 364 366 <5

HOLE 405-84-5

SHEET 3 OF

FROM TO

_

DESCRIPTION SAMPLE FROM TO C.L. ppb Au wt/ Au 91R

Ag 4 3.C.A.

366.0 387.0 CARBONACEOUS PYRITIFEROUS ARGILLITE: 11187 366 368 <5 - section characterized by very abundant to massive pyrite; 379.6- 88 368 370 <5

385 contains approximately 50-55% massive coarse- to fine-grained 89 370 372 <5 pyrite; the rest of the section contains abundant disseminated pyrite Z1190 372 374 <5 In a carbonaceous matrix. 91 374 376 <5

92 376 378 <5 387.0 393.6 ALTERATION ZONE: 93 378 380 <5

- white to bluish-gray with pyritiferous streaks and limonitic 94 380 382 <5 fractures; section shows relict banding; alteration becomes a darker 95 382 384 <5 bluish-gray towards the end of the section accompanied by chlorite- 96 384 386 <5 filled fractures. 97 386 388 <5

98 388 390 <5 10.00 393.6 396.8 PYRITIFEROUS. CARBONACEOUS ARGILLITE: 99 390 392 <5 10.00

- 8-10% pyrite over section. Z1200 392 394 <5 10.00 Z1201 394 396

396.8 428.0 DARK ALTERED ARGILLITES: 02 396 397 <5 10.00 - the section is everywhere cross-cut by carbonate-filled hairline 22 397 398.5 <5

fractures; several thin (<1 cm) irregular bands of massive pyrite 23 398.5 400 <5 occur throughout; altered argillite is characterized by carbonate 24 400 402 <5 blotchingwhich varies in intensity; estimate of pyrite is 3-4% over 25 402 404 <5 section. 26 404 406 <5

27 406 408 <5 428.0 440.5 VARIABLY SILICIFIED ARGILLITE: 28 408 410 <5

- rock is a light gray and very fine grained; numerous thin to large 29 410 412 <5 quartz and quartz-carbonate veins are noted: 428.0-429.5 (10% Z1230 412 414 5 sulphides); 430.9-431.2 (4% sulphides); smaller veins are generally 31 414 416 <5 irregular and well mineralized in pyrite and porphyrite. ' 32 416 418 <5

33 418 420 5 440.5 449.2 FAULT BRECCIA: 34 420 422 <5

- poorly ground core with irregular siliceous fragments in a chloritic 35 422 424 <5 groundmass; at 445.0 there is a 2.5" section of massive pyrite; some 36 424 426 55 of the siliceous fragments may in fact be carbonate or quartz- 37 426 428 <5 carbonate veins which have entered the fault and have been brecciated. 38 428 430 5

39 430 432 <5 449.2 460.8 ALTERED BASALIWRGILLITE? Z1240 432 434 <5

- textures have been obliterated by alteration; greenish tinge may suggest a basaltic composition but argillite is favoured as the original rock type.

HOLE 405-84-5 SHEET 4 OF GI

FROM TO

_

DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 4-LC.A.

460.8 472.5 ALTERED PYROXENE GABBRO Z1241 434 436 5 42 436 438 5

472.5 476.2 PORPHYRITIC FLOWINTRUSION? 43 438 440 5 - intensely abundant subhedral feldspar crystals within an andesitic 44 444 446 5

matrix, local pink alteration - haematite - rhodocrosite?; upper and 45 560 562 <5 lower contacts are sharp and regular with the size of the porphyro- 46 562 564 <5 blasts decreasing significantly at these margins; this may be a chill 47 564 566 <5 feature related to an intrusion but the nature of the contacts might 48 566 568 <5 suggest a regular lithologic superposition. 49 568 570 <5

Z1250 570 572 <5 476.2 611.0 VARIAdLY ALTERED PYROXENE GABBRO: 51 572 574 <5 700

- generally a dark, coarse-grained mafic rock with a porphyritic 52 574 576 <5 texture due to an abundance of coarse pyroxene crystals (14mm); some 53 576 578 <5 localized bands are modestly mineralized in pyrite and pyrrhotite; 54 578 580 <5 section of sporadic silicification occurs between 562.5 - 582.2 with 55 580 582 <5 minor associated pyrrhotite mineralization; some localized sections grade up to 10% over 1 foot.

56 582 584 <5

611.0 624.4 ALTERED BASALT: Z1257 623 625 <5 - banded?, very fine-grained, bright green rock with abundant carbonate 58 642 644 <5 flecks and occasional, small mineralized quartz veins (623.5 - 59 644 645.5 <5 623.5 E 8% pyrite); also some minor rhodochrosite in irregular Z1260 645.5 647 <5 veinlets. .

624.4 642.1 PYROXENE GABBRO: - 1-2% disseminated pyrite; gradational lower contact into alteration zone.

642.1 647.0 CARBONATE ALTERATION ZONE IN GABBRO? 450 - buff coloured section; original textures are almost obliterated but

there is some resemblance to the gabbroic rock found above; breccia at 643.5 - 644.0 with altered country rock in a quartz-carbonate matrix; minor pyrite mineralization.

END OF HOLE

MIS PROPERTY AREA WESTFIELD MINERALS LIMITED

• Location 5+00N/31+00W Claim Azimuth 000° Tests at 624' . Hole 405-84-6

Sheet 1 of 5 41-42° Latitude Dip -45°


Elevation Core BQ

,

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag 4;_i_C.A.

0 52 casing 11261 84 ' 86 <5 .

2 86 88 <5 • . 52 128.3 VARIABLY ALTERED GREYWACKE AND BANDED ARGILLITE: 3 88 90 <5

- typical interbedded greywackes and argillites; contacts between 4 143 145 <5 units show several disconformities, small scale normal faulting 5 161 163 <5 due to sedimentary slump, load cast features and convolute bedding; 6 180 182 <5 altered section at 69.8 - 70.8, may be a volcanogenic unit - 7 182 184 <5 contains abundant subhedral plagiocase crystals - rock is generally 8 184 186 <5 bleached with a greenish cast; 87.5 - 87.9 contains abundant 9 186 188 <5 "bronze" mica (phlogopite?) - this feature is associated with a Z1270 188 190 5 thin, I" irregular quartz vein which is lightly mineralized in pyrite and chalcopyrite; overall the section contains very few sulphides (<<1%); sedimentary structures indicate that rock is not overturned and youngs to the south; thin fractures with bluish bleached haloes are found throughout section but increase in intensity from 95' downwards.

71 190 192 <5

128.3 129.2 AMYGDALOIDAL BASALT: - sharp upper and lower contacts; strong foliation; calcareous blebs.

129.2 143.0 GREYWACKE AND ARGILLITE: 55° @ - same as above 135'

143.0 145.5 PORPHYRITIC DACITE: - large, zoned plagioclase phenocrysts in a dark, medium-grained

groundmass composed of feldspar, quartz and amphibole; sharp lower contact; flow top? upper contact.

145.5 161.9 GREYWACKE AND ARGILLITE

Logged A.E. Marr

Started 14 Nov/84

Completed 16 Nov/84


FROM TO

-

DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 41.4-C.A.

•

161.9 163.5 PORPHYRITIC DACITE: - finer grained than unit above; thin, irregular quartz vein near upper contact with 5% pyrite over i".

163.5 185.7 GREYWACKE AND ARGILLITE

185.7 188.6 CARBONATE PYRITIFEROUS ARGILLITE: 600 @ - fine euhedral pyrite crystals in a light grey, strongly carbonated argillite; up to 7% disseminated pyrite over section.

182'

188.6 190.6 BANDED PYRITIFEROUS GRAPHITE: - highly conductive graphite with numerous thin bands of massive

pyrite 5-10% over section.

190.6 191.5 CARBONATED ARGILLITE: - grey, fine-grained, very lightly pyritiferous rock with minor inter-

bedded graphite bands; (2% pyrite over section).

191.5 195.0 ALTERED ARGILLITE: Z1272 192 193.5 <5 - foliated, partially recrystallized argillite, may have been "cooked" 73 193.5 195 <5

by the lithology below if it be intrusive. 74 260 262 <5 75 262 264 <5

195.0 202.1 PORPHYRITIC DACITE (probably extrusive): 76 264 266 <5 - similar to uppermost &cite with better flow textures; dark green 77 266 268 <5

mineral (pyroxene?) also occurs as phenocrysts; upper and lower 78 320 322 <5 contacts are knife-sharp; 199.1 - 200.3 - amygdaloidal basalt with 79 322 324 <5 amygdules clustering near upper contact. Z1280 340 342 5

81 342 344 <5 202.1 241.8 PILLOW? BASALTS:

- textural varTations throughout the basaltic sequence may represent either flow tops or pillow selvages; section is composed of numerous thin flows ranging from a few inches to several feet.

241.8 243.3 PORPHYRITIC ANORTHOSITE? - large subhedral calcic, zoned plagioclase phenocrysts (Sicm) predomi-

nate in a medium fine-grained equigranular matrix composed of dark fine, plagioclase, calcite and possibly quartz.

243.3 261.9 ANDESITIC BASALT: - dark grey, very fine-grained, moderately hard rock; some sections with carbonate specks; occasional to rare blebs of pyrrhotite.


FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 4.JLC.A.

261.9 266.9 ALTERED BASALT: - section is characterized by a strong, irregularly foliated texture

caused by a dark brown, very fine-grained mineral (amphibole?).

266.9 287.9 BASALTIC FLOWS: - several differently textured basaltic (andesitic) flows; lightly carbonated in some sections; generally aphanitic with some recrystallized sections; occasional stringers of pyrrhotite.

287.9 316.4 PYROXENE GABBRO: - medium-coarse grained rock with porphyritic pyroxene crystals, density and size of pyroxene phenocrysts vary considerably suggesting perhaps a near surface emplacement (i.e. variably cooled); may be porphyritic andesite.

316.4 352.0 VARIABLY ALTERED BASALT: 600 @ - broad partially recrystallized section associated with fracturing at 352' 340 - 342.5; some irregular anastomozing porphyrite-filled fractures; thin 2" quartz vein at 321.5 with a cluster of large porphyrite and pyrite blebs also with a massive amphibole-biotite?

352.0 353.5 PORPHYRITIC DACITE

353.5 388.4 BASALT: Z1282 358 360 <5 - generally aphanitic, dark grey rock with occasional carbonated 3 360 362 <5 sections; 358.5 - 367 is conspicuously altered - irregular bleaching 4 362 364 <5 occurs throughout subsection with three two-to five-inch sections 5 364 366 (5 which resemble the porphyritic anorthosite above; pyrrhotite and 6 366 368 (5 pyrite are common as thin elongated blebs within altered subsection 7 408 410 <5 (S3%). 8 410 412 <5

9 412 414 <5 388.4 390.7 ALTERED PORPHYRITIC DACITE: Z1290 414 416 <5

- central part of section contains large plagioclase phenocrysts in 1 416 418 <5 excess of lcm. 2 418 420 <5

3 420 422 <5 390.7 405.3 VARIABLY ALTERED BASALT: 4 422 424 <5

- occasional pyrrhotite blebs. 5 424 426 <5 . 6 426 428 <5 7 428 430 <5 . 8 430 432 <5 9 432 434 15

HOLE 405-84-6 SHEET a OF 5

FROM TO -

DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 141C.A.

405.3 409.4 PORPHYRITIC DACITE: Z1300 434 436 <5 - unit is characterized by an abundance of dense plagioclase phenocrysts 01 436 438 (5

2mm and large green pyroxene phenocrysts (41cm) with a fine grey 02 438 440 <5 groundmass 03 440 442 <5

04 442 444 <6 409.4 410.4 PORPHYRITIC DACITE: 05 444 446 <5

- dark version of above; small plagioclase phenocrysts (2mm) with a 06 446 448 <5 dark grey-green, aphanitic groundmass. 07 448 450 <5

08 450 452 5 410.4 411.8 PORPHYRITIC DACITE: 09 452 454 <5

- same as 305.3 - 409.4 Z1310 454 456 (5 11 456 458 <5

411.8 461.0 BASALTS: 12 458 460 10 - numerous flows of variably textured and altered basalts; 430.5-452 is 13 460 467 5 zone of most intense alteration - mainly carbonation - several 14 462 464 5 reddish bands may be syngenetic oxidation rinds; section of alteration 15 464 466 <5 may represent a broad unit of pillows; pyrrhotite is common (2-3% per 16 466 468 (5 section); amygdaloidal section 244.9 - 246.2. 17 468 470 20

18 470 472 5 461.0 481.9 PYRITIFEROUS GRAPHITE: 19 472 474 10 700 @

- typical, intercalated massive pyrite and graphite bands; large part Z1320 474 476 10 478' of central section (i.e. 466-472) is well silicified and/or 21 476 478 5 carbonated; pyrite occurs up to 10% of section. 22 478 480 15

23 480 482 <5 481.9 489.5 ALTERED BASALT: 24 482 484 (5

- highly altered basalt; same mineral segregation evident; well 25 484 486 <5 carbonated locally; up to 6% porphyrite and pyrite over 1-foot 26 486 488 <5 subsections. 27 488 490 (5

489.5 490.2 PYRITIFEROUS GRAPHITE: - as above (510% pyrite per section).

490.2 491.7 ALTERED ARGILLITE: • - carbonate section(slightly bleached) of argillite.

'


FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Auit ppb Ag 4.1.C.A.

491.7 624.0 VARIABLY ALTERED BASALTS: Z1328 490 492 <5 - "swirled" Textures, bleached streaks and irregular pyrite, 29 492 494 <5 PYrrhotite, chalcopyrite? elots are common from 491.7 - 524 feet; Z1330 494 496 15 bleached streaks strongly resemble those seen above at 353.5 - 388.4; 31 496 498 <5 as above some textures resemble flow top brecciae and others suggest 32 498 500 C5 pillow selvages; some rare quartz carbonate veins occur at 511.5 33 500 502 <5 (2"); 517 - 519 (thin i" vein parallel to core axis - well mineralized 34 502 504 20 In pyrite); remainder of section contains small sporadic pyrrhotite 35 504 506 <5 and pyrite blebs; another altered section occurs at 593' to 606' - 36 506 508 10 here one notes carbonation and an associated recrystallization of the 37 508 510 <5 rock; 606 - 608.5 there is a thin porphyritic dacite unit. 38 510 512 <5

39 512 514 <5 Z1340 514 516 <5

41 516 518 <5 END OF HOLE 42 518 520 <5

43 520 522 <5 44 522 524 <5 45 593 595 <5 46 595 597 <5 47 597 599 <5 48 599 601 <5 49 601 603 <5

Z1350 603 604.5 <5 51 604.5 606 <5

39 - 40°

Depth 625

• Core BQ

Claim

Latitude

Departure

Elevation

Hole 405-84-7

Sheet 14 7 Dip -450

Azimuth 000° Tests test at 625' Location 24+50W/5+00N

Logged Alex E. Mayor

Started Nov. 17 /84

Completed Nov. 20/84

PROPERTY AREA LAC GAGNON NTS

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppbAR• ppbAu ppm Cu

0.0 78.0

80.5

111.9

118.7

127.0

129.0

133.0 137.2

78.0 80.5

111.9

118.7

127.0

129.0

133.0

137.2 142.0

CASING PORPHYRITIC DACITE:

-dark, fine grained matrix; large zoned plag. with pyx (?) XL' ALTERED BASALT

-well foliated to massive, med. grained basalt; coarse texture is due to recrystallization; small qtz/carbonate veins occur throughout section and are often well mineralized in py, po and occasionally cp, large clot of cp with po occurs at 84.4,

-streaks of fine grained pyrite are common; pyrite ‘.4%/sxn INTENSELY ALTERED BASALT

-colourful section with an imbricated brecciation texture due to flooding of host rock by calcareous and siliceous hydrothermal solutions, fine streaks of po occur throughout 2%/sxn

TRANSITIONAL ALTERED BASALT -section is characterized by irregular calcareous and siliceous streaks/veinlets

-approximately half of section maintain its original textures -"subbrecciated" -po and fine grain cp is common as clots or streaks (..3%/sxn)

SAMTJTIC ANDESITE

PYRITIFEROUS ANDESITE -dark, siliceous, very fine grained rock -120.0-130.0 contains approx. 30% pyrite

PYROXENE GABBRO INTENSELY ALTERED PYRITE AND CP'S BASALT

-as above (111.9-118.7) with greater concentrations of sulfides 139.6-140.6 is massive pyrite, remainder of section grades up to 5-6% of sxn

21352 1353 1354 1355 1356 1357 1358 1359 1360 1361 1362 1363 1364 1365 1366 1367 1368 1369 1370 1371 1372 1373 1374 1375 1376 1377 1378 1379 1380

8

78.0 80.0 82.0 84.0 86.0 88.0 90.0 92.0 94.0 96.0 98.0

100.0 102.0 104.0 106.0 108.0 110.0 112.0 114.0 116.0 118.0 120.0 122.0 124.0 125.5 127.0 129.0 131.0. 133.0

80.0 82.0 84.0 86.0 88.0 90.0 92.0 94.0 96.0 98.0

100.0 102.0 104.0 106.0 108.0 110.0 112.0 114.0 116.0 118.0 120.0 122.0 124.0 125.5 127.0 129.0 131.0 133.0 135.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 1.5 1.5 2.0 2.0 2.0 2.0

<5 55

100 15 < 5 <5 <5 <5 <5 <5 <.5 15 <5 <5 <5 < 5 < 5 < 5 < 5

5 <5 < 5 ‹ 5 <5 <5 ‹ 5 <5 10 <5

14 177 570

9100 375

35 270

27 10

9 4 4

34

1500 325 99

270 182 375 167 215 435

1350 1500

23 1350

11 8


HOLE . SHEET 1 OF

FROM TO -

DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag ppm Cu 4 C.A.

142.0

178.2

182.0

185.8

196.1

205.0

211.0

235.0

236.3

237.5

178.2

182.0

185.8

196.1

205.0

211.0

235.0

236.3

237.5

239.7

ALTERED BASALT/ARGILLITE ? -dark grey-green, fine grain rock with numerous bleached fractures, occasional pyrite streaks (51% sxn)

ALTERED PYRITIFEROUS CHERT WITH ARGILLACEOUS COMPONENT -mainly a grey swirled chert intercalated with siliceous argillite -pyrite occurs abundantly as irregular, occasionally vuggy bands more or less within the foliation; 10-12% pyrite/sxn

SILICIFIED ARGILLITE -very fine grain dark grey rock with sporadic banded nodular pyrite

ARGILLACEOUS ALTERED PYRITIFEROUS CHERT -as above (178.2-182.0) -some minor isolated argillaceous sections and a thin amygdaloidal basalt; pyrite occurs in frequent bands of lacey to near massive habit -- it is generally fine grained in this section but some bands are coarse grained and vuggy; up to 10I/sxn

ALTERED BASALT -fine grained greenish rock with broad irregular, altered streaks alteration is mainly a bleaching of the rock with subsequent recrystallization of rock and the emplacement of massive chlorite/ carbonate/silica; most of the altered streaks contain a few percent of po and lesser pyrite

101311141YRITIC ANDESITE -variably altered andesite with isolated bands containing zoned plag. phenocrysts; some sections are distinctly amygdaloidal

VESICULAR (?) BASALT -fine grained dark green rock with abundant small white crystalline vesicles (?)

ALTERED PYRITIFEROUS CHERT -as above (185.8-196.1) -6% pyrite/sxn, also po.

BASALT -lightly altered; vesides may be recrystallized carbonate or low temperature silicate

ALTERED PYRITIFEROUS CHERT -transitional unit from typical lithology as seen above to a more nodular, irregular alteration at the bottom of section; py and po up to 5-7%/sxn

Z1381 1382 1383 1384 1385 1386 1387 1388 1389 1390 1391 1392 1393 1394 1395 1396 1397 1398 1399

Z1400 1401 1402 1403 1404 1405 1406 1407 1408 1409 1410 1411 1412 1413 1414 1415 1416 1417 1418 1419 1420 1421

135.0 137.0 139.0 141.0 143.0 145.0 147.0 149.0 151.0 153.0 155.0 157.0 159.0 161.0 163.0 165.0 167.0 169.0 171.0 173.0 175.0 177.0 179.0 181.0 183.0 185.0 187.0 189.0 191.0 193.0 195.0 197.0 199.0 201.0 203.0 205.0 207.0 209.0 211.0 213.0 215.0

137.0 139.0 141.0 143.0 145.0 147.0 149.0 151.0 153.0 155.0 157.0 159.0 161.0 163.0 165.0 167.0 169.0 171.0 173.0 175.0 177.0 179.0 181.0 183.0 185.0 187.0 189.0 191.0 193.0 195.0 197.0 199.0 201.0 203.0 205.0 207.0 209.0 211.0 213.0 215.0 217.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2,0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

5 <5 15 <5 <5 < 5 <5 <5 <5 (5 <5 <5 <5 <5 <5 <5 15

5 <5 <5 20 <5 <5 <5

5 <5 <5

5 5

<5 <5 <5 <5 <5 <5 <5 45 <5 <5 <5 <5

7, 660

2900 325 305 162 178 117 140

98 15 23 26 25

132 129 315 235 117 139 132 263' 570 367 230 435 540

2200 4550

780 380 225 275 350 385 515

26 127

96 275 11

•

50'

1

HOLE tw, 44_ 1 SHEET

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag ppm Cu A. C.A.

239.7

262.7

284.0

383.2

402.5

404.8

406.5

416.0

418.4

262.7

284.0

383.2

402.5

404.8

406.5

416.0

418.4

419.2

BASALTS

239.7-245.5 unaltered fine grain dark green basalt

245.5-249.0 partially recrystallized basalt, some very local intense alteration; few percent minor sulfides

249.0-253.0 unaltered basalt

253.0-257.0 variably altered porphyritic andesitic basalt

257.0-262.2 highly altered basalt; well carbonated, obliterated textures

262.2-262.7 irregular qtz vein with 10-12% po and py

PORMAJTIC DACITE -some slightly altered sections; may be an incremental intrusion

LIGITLY ALTERED TO RECRYSTALLIZED BASALT -light altered basalt resembles flecked vesicular (?) basalt seen above; recrystallized section occurs from approx. 316.0-370.1 -this section is generally coarse-grained and contains abundant local sulfide mineralization (py, po, cp); up to 10-12%/sxn; -there are abundant sulfides, disseminated throughout the rock -broad mineralized sections at 336.9-337.8 (qtz and py) 339.7-340.1, cp and po (15%)

PYRTTIFEROUS ARENITE (7) RECRYSTALLIZED CHERT -light buff to dark grey, fine grained rock with abundant very disseminated pyrite; estimated mineralization gives sulfide up to 15% over the sxn; fuchsite is noted at 385.0; dark grey colour is due to argillaceous component -two thin pyrites graphite bands occur within section

PYRITIFEROUS GRAPHITE

PYRITIFEROUS ARENITE (?) RECRYSTALLIZED CHERT -as above -some hematite alteration -- fault -core becomes progressively more ground

ALTERED BASALT -highly fractured and ground core -amygdules are preserved; probably within a fault

PYRITIFEROUS ARENITE -as above, highly fractured

PORPHYMTIC ANDESITE -corroded texture, probably due to fault

Z1422 1423 1424 1425 1426 1427 1428 1429 1430 1431 1432 1433 1434 1435 1436 1437 1438 1439 1440 1441 1442 1443 1444 1445 1446 1447 1448 1449

1451 1452 1453 1454 1455 1456 1457 1458 1459 1460 1461

217.0 219.0 221.0 223.0 225.0 227.0 229.0 231.0 233.0 235.0 237.0 239.0 241.0 243.0 245.0 247.0 249.0 251.0 253.0 255.0 257.0 259.0 261.0 263.0 265.0 267.0 269.0 271.0 273.0 275.0 277.0 279.0 281.0 283.0 285.0 287.0 289.0 291.0 293.0 295.0

2.01450

219.0 221.0 223.0 225.0 227.0 229.0 231.0 233.0 235.0 237.0 239.0 241.0 243.0 245.0 247.0 249.0 251.0 253.0 255.0 257.0 259.0 261.0 263.0 265.0 267.0 269.0 271.0 273.0 275.0 277.0 279.0 281.0 283.0 285.0 287.0 289.0 291.0 293.0 295.0 297.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2,0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

2.0 2.0 2.0 " 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

65 15

10 <5 <5 <5 <5 <5 (5 <5 <5 <5 <5 <5 45 <5 <5 <5 .45 <5 <5 <5 <5 (5

,

5

V,

700

OF .

HOLE SHEET q OF -1

FROM TO DESCRIPTION SAMPLE FROM TO C.L. .,,

ppb Au oz Au/t ppb Ag ppm Cu 4 C.A.

419.2

430.0

432.9

437.0

445.0

463.8

467.2

473.7

475.6

480.0

430.0

432.9

437.0

445.0

463.8

467.2

473.7

475.6

480.0

526.4

ALTERED GREYWACKE -coarse, altered arenaceous rock, porous, highly fractured -fractures filled with calcite, chl, qtz, py and po; -small scale faulting

PORPHYRITIC ANDESIT

DIMLY INTERBEDDED LAMINATED CHERT AND BASALT -very fractured section, hematite staining -thin band of massive pyrite at 435.0-435.4; also at 435.5-436.0 -irregular qtz veins are common in bottom of sxn

MRPHWITIC DACITE

ANDESITE -dark, very fine grain, moderately hard rock -between 448 and 451 there are several clusters of peculiar hallow cylindrical structures which have no simple explanation

e.g.

-they appear almost organic but this is highly unlikely

PORPHYRITIC DACITE

ANDESITE ? SILICIFIED ARGILLITE ? -basically a very fine grained dark grey rock with a few minor carbonate filled fractures

PYRITIFEROUS ARENITE ? RECRYSTALLIZED CHERT -pyrite is 30-40% of section -small amygdaloidal basalt unit (474.3-474.6)

PYRITIFEROUS BLACK ARGILLITE -approximately 8-10% banded pyrite over sxn

VARIABLY ALTERED ANDESITE -section is characterized by braod greenish bleaching halos around irregular fractures

-some contain bluish qtz veins . -py and po occur in various habits ( 2%/sxn)

-at 499.7 there is a band of a bright green mineral (tourmaline ?)

2.0E

Z1462 1463 1464 1465 1466 1467 1468 1469 1470 1471 1472 1473 1474 1475 1476 1477 1478 1479 1480 1481 1482 1483 1484 1485 1486 1487 1488 1489 1490 1491 1492 1493 1494 1495 1496 1497 1498 1499 Z1500

297.0 299.0 301.0 303.0 305.0 307.0 309.0 311.0 313.0 315.0 317.0 319.0 321.0 323.0 325.0 327.0 329.0 331.0 333.0 335.0 337.0 339.0 341.0 343.0 345.0 347.0 349.0 351.0 353.0 355.0 357.0 359.0 361.0 363.0 365.0 367.0 369.0 371.0 373.0

299.0 301.0 303.0 305.0 307.0 309.0 311.0 313.0 315.0 317.0 319.0 321.0 323.0 325.0 327.0 329.0 331.0 333.0 335.0 337.0 339.0 341.0 343.0 345.0 347.0 349.0 351.0 353.0 355.0 357.0 359.0 361.0 363.0 365.0 367.0 369.0 371.0 373.0 375.0

2.0 2.0 2.0 2.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

<

<5

.

60°

HOLE LIDS 84i SHEET r OF 1 .

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag ppm Cu . 4. C.A.

526.4

529.4

531.0

578.2

580.1

618.3

529.4

531.0

578.2

580.1

618.3

625.0

. 625 0

ALTERED ANDESITE IN FAULT -intensely deformed rock, generally pale white to bluish grey with some vague brecciation textures and well carbonated and silicified (3-5% py/sxn)

RELMIFIED ROCK FLOUR ?/MYLONITE • -pale rock with ghosts of brecciation textures; shot through with fine qtz veins; matrix of rock appears mylonitic

VARIABLY ALTERED ANDESITE -in general rock is very fine grained with broad strips of bleaching within which the grain size tends to coarsen

-the appearance of a distinctive blue-green mineral of unknown composition occurs at 248 and is especially well-developed at 569.5 where it has a hematite halo

• PORPHYRITIC ANDESITE

VARIABLY ALTERED ANDESITE -similar to unit above -qtz breccia in bleached andesite at 586.7-588.3 -occasional aggregates of sulfide - mainly pyrite with some minor cp ( 2%/sxn)

DIORITE .

-medium grain rock composed mainly of feldspar with some minor free qtz

EN D OF HUE

' •

'

Z1501 1502 1503 1504 1505 1506 1507 1508 1509 1510 1511 1512 1513 1514 1515 1516 1517 1518 1519 1520 1521 1522 1523 1524 1525 1526 1527 1528 1529 1530 1531 1532 1533 1534 1535 1536 1537 1538 1539 1540 1541 1542

375.0 377.0 379.0 381.0 383.0 385.0 387.0 389.0 391.0 393.0 395.0 397.0 399.0 401.0 403.0 405.0 407.0 409.0 411.0 413.0 415.0 417.0 419.0 421.0 423.0 425.0 427.0 429.0 431.0 433.0 435.0 437.0 439.0 441.0 443.0 445.0 447.0 449.0 451.0 453.0 455.0 457.0

377.0 379.0 381.0 383.0 385.0 387.0 389.0 391.0 .393.0 395.0 397.0 399.0 401.0 403.0 405.0 407.0 409.0 411.0 413.0 415.0 417.0 419.0 421.0 423.0 425.0 427.0 429.0 431.0 433.0 435.0 437.0 439.0 441.0 443.0 445.0 447.0 449.0 451.0 453.0 455.0 457.0 459.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2,0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

45

.

45 10

.

.

... -

HOLE . SHEET L OF

FROM TO DESCRIPTION SAMPLE FROM TO C.L. 1,..

ppb Au ppb Ag ppm Cu

Z1543 459.0 461.0 2.0 10 1544 461.0 463.0 2.0 10 1545 463.0 465.0 2.0 <5 . 1546 465.0 467.0 2.0 1547 467.0 469.0 2.0 1548 469.0 471.0 2.0 . 1549 471.0 473.0 2.0 1550 473.0 475.0 2.0 1551 475.0 477.0 2.0 1552 477.Q 479.0 2.0 1553 479.0 481.0 2.0 1554 481.0 483.0 2.0 1555 483.0 485.0 2.0

• 1556 1557

485.0 487.0

487.0 489.0

2.0 2.0

.

1558 489.0 491.0 2.0 1559 491.0 493.0 2.0 1560 493.0 495.0 2.0 1561 495.0 497.0 2.0 1562 497.0 499.0 2.0 1563 499.0 501.0 2.0 1564 501.0 503.0 2.0

. 1565 503.0 505.0 2.0 20 , 1566 505.0 507.0 2.0 <5

1567 507.0 509.0 2.0 1568 509.0 511.0 2.0 1569 511.0 513.0 2.0

I -

1570 513.0 515.0 2.0 1571 515.0 517.0 2.0 <5 1572 517.0 519.0 2.0 1573 519.0 521.0 2.0 1574 521.0 523.0 2.0 1575 523.0 525.0 2.0

I

1576 525.0 527.0 2.0 1577 527.0 529.0 2.0 1578 529.0 531.0 2.0 1579 531.0 533.0 2.0 10

* 1580 533.0 535.0 2.0 10 1581 535.0 537.0 2.0 10 1582 537.0 539.0 2.0 10 1583 539.0 541.0 2.0 <5 1584 541.0 543.0 2.0 <5

HOLE q05, SHEET OF

FROM TO DESCRIPTION SAMPLE FROM TO C.L. 7 i :

._

ppb Au ppb Ag pp m Cu

21585 543.0 545.0 2.0 <5 1586 545.0 547.0 2.0 <5 1587 547.0 549.0 2.0 5 1588 549.0 551.0 2.0 5 1589 551.0 553.0 2.0 5 1590 553.0 555.0 2.0 5 1591 555.0 557.0 2.0 5 1592 557.0 559.0 2.0 5 1593 559.0 561.0 2.0 5 1594 561.0 563.0 2.0 5 1595 563.0 565.0 2.0 5 1596 565.0 567.0 2.0 5 1597 567.0 569.0 2.0 5

• 1598 1599

569.0 571.0

571.0 573.0

2.0 2.0

<5 5

21600 573.0 575.0 2.0 5 1601 575.0 577.0 2.0 5 1602 577.0 579.0 2.0 5 1603 579.0 581.0 2.0 5 1604 581.0 583.0 2.0 5 1605 583.0 585.0 2.0 5 1606 585.0 587.0 2.0 5'

• 1607 587.0 589.0 2.0 5 1608 589.0 591.0 2.0 5 1609 591.0 593.0 2.0 15 1610 593.0 595.0 2.0 15 1611 595.0 597.0 2.0 15 1612 597.0 599.0 2.0 15 1613 599.0 601.0 2.0 15

. 1614 601.0 603.0 2.0 15

. 1615 1616

603.0 605.0

605.0 607.0

2.0 2.0

15 15

1617 607.0 609.0 2.0 15 1618 609.0 611.0 2.0 15 1619 611.0 613.0 2.0 45 1620 613.0 615.0 2.0 <5

. 1621 615.0 617.0 2.0 <5 1622 617.0 619.0 2.0 <5 1623 619.0 621.0 2.0 <5 1624 621.0 623.0 2.0 <5 1625 623.0 625.0 2.0 <5

NTS PROPERTY AREA LAC GAGNON WEFFIELD MINERALS LIMITED

Azimuth 0000

39 - 40°

Depth 500'

• Core •BQ

Dip -45°

Claim

Latitude

Departure

Elevation

Hole 405-84-8

Sheet 1

Tests 500' at Location 20+80W/6+20N

Logged Alex E..Mhrr

Started Nov. 21/84

Completed Nov. 27/84*

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag 4CIC.A.

0.0 103.0 CASING

103.0 165.1 INTERCALATED BASALT AND GABBRO -alternating layers of typical green apharitic to amygdaloidal basalt with coarse grained gabbroic layers -frequent minor qtz - eight qtz-carbonate veinlets -occasional blebs of pyrite (1=1%/sxn) -some evidence of micro-faulting along main fracture set at 300 off C.A. 1 -some minor hematite staining of fracture-filling material -a contact at 153.1 suggests the rock to be overturned, that is, a fine grained basalt fills in an irregular unconformity in a foliated rock: porphyritic

165.1 172.6 PORPHYRITIC DACITE Z1710 172.0 174.0 2.0 5 -knife sharp upper and lower contact 1711 174.0 176.0 2.0 6 -equigranular, white plag. phenocrysts 1712 176.0 178.0 2.0 22 -also aome pale olive green phenocrysts, esp. at bottom of sxn 1713 178.0 180.0 2.0 14

1714 180.0 182.0 2.0 <5 172.6 178.8 PYRITIFEROUS ARGILLITE 1715 182.0 184.0 2.0 <5

-typical pyrites argillite with numerous thin massive pyrite bands 1716 184.0 186.0 2.0 <5 and one broad section of lacey pyrite, (15% py/sxn) 1717 186.0 188.0 2.0 <5

1718 188.0 190.0 2.0 <5 178.8 210.2 VARIABLY ALTERED BASALT 1719 190.0 192.0 2.0 <5

-in general this is a fine grained green rock with several localized 1720 192.0 194.0 2.0 <5 sections of alteration which are characterized by mineral segre- 1721 194.0 196.0 2.0 <5 . gation and a reddish-brown color change of the basalt, most 1722 196.0 198.0 2.0 <5 altered sections contain recrystallized pyrite and po with 1723 198.0 200.0 2.0 <5

occasional specks of cp (1-2% sulfides/sxn); irregular cross- 1724 200.0 202.0 2.0 <5 cutting bleached fractures are commonplace and tend to run at 1725 202.0 204.0 2.0 <5

*After three attempts

HOLE 'Jo(- 84 A SHEET 2 OF 4

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag &I.c.A.

178.8 - 210.2 (con't) - •

50°LC.A. with a finer set at 350 C.A., approx.IL to the first set 21726 204.0 206.0 2.0 <5 1727 206.0 208.0 2.0 <5

I \c/ ei L 1 1728 208.0 210.0 2.0 <5

210.2 219.0 PORPHYRITIC ANDESITE -dark to pale green rock with abundant white to pinkish phenocrysts most of which have indistinct and ghosting rims -section is similarly cross-cut by the fracture sets mentions above -some minor po.

219.0 260.6 ALTERED BASALT -rock is altered as above (178.8-210.2), the alteration is however more pervasive

Z1729 220.0 224.0 2.0 <5

-occasional sections are moderately pyritiferous 21730 234.0 236.0 2.0 <5 60o@236

-235.2-236.0 is a subsection of pyritiferous argillite running approx. 12% over the subsection; in general, the pyrite runs 2-3% over entire section

-well developed fault at 221.6-222.5

260.6 263.5 ALTERED PORPHYRITIC ANDESITE (?) -dark, hard, very fine-grained rock with ghostly white to pink phenocrysts

-habit of phenocrysts suggests that they have been strongly foliated some have an flaugen-like" appearance suggesting some pressure-shadowing

263.5 280.3 ALTERED BASALT -extensively altered and recrystalized basalt 21731 276.0 278.0 2.0 <5

-intense anastomozing qtz-carbonate veinlet 1732 278.0 280.0 2.0 <5

-sulfides are rare 1733 280.0 282.0 2.0 5 1734 282.0 284.0 2.0 7

280.3 285.1 PYRITIFEROUS TRANSITION ZONE 1735 284.0 286.0 2.0 12

-original textures have been nearly obliterated by the injection of 1736 286.0 288.0 2.0 8

mineralized fluids 1737 288.0 290.0 2.0 10

-some dark argillaceous bands occur lower in section 1738 290.0 292.0 2.0. <5 -section is characterized by buff cherty sections and abundant 1739 292.0 294.0 2.0 <5 .

finely disseminated crystalline pyrite (py .4-20%/sxn) 1740 294.0 296.0 2.0 8

,

HOLE 4105%134 _8 SHEET ,/ OF 4 .

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 41.c.,4

285.1 319.1 PYRITIFEROUS BLACK ARGILLITE AND.GRAPHITE -typical black argillite with abundant oblate nodules of massive 21741 296.0 298.0 2.0 6 pyrite 1742 298.0 300.0 2.0 10 -subsection of altered (silicified) and brecciated argillite at 1743 300.0 302.0 2.0 6 290.4-293.6 1744 302.0 304.0 2.0 14

-subsection of graphite at 293.6-301.1 1745 304.0 306.0 2.0 12 -basaltic subsection at 303.0-304.7 1746 306.0 308.0 2.0 12 50 @308 -thereafter occasional thin basaltic bands are interbedded with the 1747 308.0 310.0 2.0 8 argillite 1748 310.0 312.0 2.0 8

1749 312.0 314.0 2.0 6 319.1 357.5 AMYGDALOIDAL BASALTS (may be core of isocunal fold) 1750 314.0 316.0 2.0 <5

-typical unaltered basalt with amygdaloidal caps to the individual 1751 316.0 318.0 2.0 6 flows 1752 318.0 320.0 2.0 <5 -pyrites argillite subsection at 325.1-326.4

357.5 377.3 PYRITIFEROUS ARGILLITE AND GRAPHITE -section is characterized by large subspherical and rectangular 21753 356.0 358.0 2.0 <5 nodules of massive pyrite floating in black argillite; some 1754 358.0 360.0 2.0 <5 nodules are well over an inch in diameter but most are in the 3/4 1755 360.0 362.0 2.0 <5 inch range 1756 362.0 364.0 2.0 <5 -a basaltic subsection is found at 363.4-365.0 (30% py/sxn) 1757 364.0 366.0 2.0 <5

1758 366.0 368.0 2.0 <5 377.3 378.0 PYRITIFEROUS TRANSITION ZONE 1759 368.0 370.0 2.0 <5

-similar to zone above with lacey crystalline pyrite in silicified 1760 370.0 372.0 2.0 <5 rock (20% py/sxn) 1761 372.0 374.0 2.0 <5

1762 374.0 376.0 2.0 14 378.0 464.0 VARIABLY ALTERED BASALT 1763 376.0 378.0 2.0 <5

-mixed aphanitic -relatively unaltered basalt and amygdaloidal basalt with minor localized sections of extensive alteration near top of section

Z1764 378.0 380.0 2.0 <5

-spectacular fault breccia between 387.0-390.1 characterized by 1765 386.0 388.0 2.0 <5 bright hematite in tillings 1766 388.0 390.0 2.0 <5 -occasional py's bands are found well spaced through section

464.0 468.8 BLEACHED BASALT -broad section of lightly bleached basalt -edges of section are reminiscent of the swathy alteration seen in other holes

.

HOLE 41û'-84-8 SHEET 4 OF y

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 41. c.n.

468.8 489.3 ALTERED BASALT -swathy bleached sections -some irregular carbonate-filled veinlets

489.3 495.3 PORPHYRITIC ANDESITE-DACITE -equigranular medium grained porphyry

495.3 500.0 LIGHTLY ALTERED BASALT -fine grained basalt with finely bleached sections

500.0 END OF HOLE

NTS PROPERTY AREA LAC GAGNON , WESTFIELD MINERALS LIMITED

=40°

• Core B(,)

Depth 500'

Claim

Latitude

Departure

Elevation

Tests at 500' Azimuth 0000

Dip -45° Sheet 1

Hole 405-84-9 Location 20+80W/4+20N

Logged Alex E. Marr

Started 27 Nov/84

Completed 29 Nov/84

• . FROM TO • DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag

0.0 76.0 CASING ,

76.0 82.8 GRITTY ARGILLITE

82.8 84.0 BASALT -fine grain, greenish, streaky rock -may be a volcanogenic sediment, i.e. a water-lain tuff or an argillaceous sediment with a high chlorite component


87.6 101.1 GROWACKE -variably textured dark brown clastic rock with some local banding caused by increased argillaceous content

-rare bleached fracturing

, 95.1-95.8 small basalt flow

101.1 102.5 GRITTY ARGILLITE .

102.5 104.7 ARKOSIC MACKE ? / PORPH'C BASALT ? -dark brownish-grey rock with abundant small (41 mm) plagioclase clasts ?/phenocrysts ?

.

-there appears to be a foliation to the rock but no appreciable bedding

104.7 109.0 GRITTY ARGILLITES -several minor argillaceous, wacke-like bands within a general Z1810 104.0 106.0 2.0 5

sso

mudstone lithology 1811 106.0 108.0 2.0 4,5 -.5 foot altered subsections at top and bottom of section 1812 108.0 110.0 2.0 <5

HOLE Vos -a4_9 SHEET OF 6

FROM TO DESCRIPTION SAMPLE FROM

. .

TO C.L.

.

ppb Au

.

oz Au/t ppb Ag

109,0 112.3 VOLCANIC SEDIMENT . -porphyritic, pale grey-green rock with fine bedding textures -phenocrysts appear to be elongated as if by foliation -probably altered slightly -lower contact appears to be an unconformity

112.3 134.3 BANDED GRITTY ARGILLITES .

-section is banded by virtue of the changing clastic content -some subsections border on greywacke -a few greenish sections appear to be locally altered sections rather than a distinctive lithology -within these subsections there is a significant increase in the number of fine bleached fractures

134.3 142.9 GREYWACKE •


145.2 162.9 GREYWACKES -very variable textures -several subsections are very coarsely clastic and arkosic, in fact, porphyritic like the lithology seen at 102.5-104.7 above

-once again greenish subsections are the product of light hydro-thermal alteration

162.9 182.6 11JRB1DITES ? -cyclic, immature turbidites with fining upwards, seggesting that sequence youngs to the south

182.6 183.0 CHERTY BRECCIA . -altered unit probably within a fault -several greenish cherty fragments have been welded with qtz and carbonate .

183.0 184.9 DARK ARGILLITE -more carbonaceous nudstOne with several fine hairline carbonate-filled fractures .

HOLE 4,1;-.414-7 SHEET OF tr,

-

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag

184.9 274.0 VARIABLY ALTERED GREYWACKE WITH LESSER WILLITE -section is characterized by the appearance of more intensely altered subsections, more intense bleached fractures and a darker more carbonaceous greywacke -some altered subsections have a distinctive bluish snowflake-like recrystallization patern

-some irregular clots of po at 199.0 -clots of pyrite and carbonate within bleached fractures begins at 225.0'

-the irregular snowflake recrystallization texture increases downwards in the section to where it dominates from about 230 to 254.

.

-minor basaltic flow at 250.6-251.4 -minor dendritic po at 261.5 -two sets of bleached fractures noted at 255.0'

274.0 279.5 ALTERED BASALT -recrystallized greenish basalt, hydrothermal alteration, abundant chlorite

279.5 288.2 THINLY INTERBEDDED GREYWACK AND ARGILLITE (gritty brown)

288.2 290.9 PDRPHYRITIC ANDESITE ' -fine equigranular composed mainly of feldspar, amphiboles (?) and, . some fine quartz


291.4 295.0 PORPHYRITIC ANDESITE -as above

HOLE yes -84_ / SHEET 4 OF c,

FROM TO DESCRIPTION SAMPLE' FROM

1

TO C.L. ppb Au oz Au/t ppb Ag

295.0 307.1 VARIABLY ALTERED ARGILLITE , -"snowflake" type recrystallization in upper 5 feet of section -brown, slightly gritty argillite becomes darker (more carbmaceous)

21813 1814

ï 300.0 i 302.0

302.0 304.0

2.0 2.0

5 '5

in middle of section giving way to a lower four feet of bleached 1815 1 304.0 305.5 1.5 45 .argillite 1816 305.5 307.0 1.5 45

1817 307.0 309.0 2.0 10 307.1 313.3 PYRITIFEROUS BLACK ARGILLITE 1818 309.0 311.0 2.0 <5

-section is characterized by the presence of large oblate nodules 1819 311.0 313.0 2.0 s

of 'banded' pyrite 1820 313.0 315.0 2.0 [5 -may be clasts of ripped up iron formation (15-20 py/sxn) 1821 315.0 316.5 1.5 <5

313.3 315.3 ANDESITE .

315.3 316.6 PYRITIFEROUS BLACK ARGILLITE -as above -minor gravel seam near lower contact

316.6 318.3 SILICIFIED PYRITIFEROUS ARGILLITE -pyrite is more disseminated and crystalline (10-15i /sxn) than is seen in the unaltered argillite

21822 316.5 318.5 2.0

318.3 320.3 PYRITIFEROUS BLACK ARGILLITE -as above 21823 318.5 320.5 2.0 10 -nodular tend to be more ovoid in this section (20% py/sxn?)

320.3 321.8 SILICIFIED PYRITIFEROUS.ARGILLITE -as above with 5-7t py/sxn 21824 320.5 322.0 1.5 <5

321.8 323.1 FINELY BANDED PYRITIFEROUS ARGILLITE -nodular pyrite gives way to a very fine laminar pyrite (45-50% py/sxn)

21825 322.0 323.0 1.0 20 .

323.1 324.0 SILICIFIED PYRITIFEROUS ARGILLITE -3-5% py/sxn 21826 323.0 324.0 1.0 10

324.0 324.9 PYRITIFEROUS BLACK ARGILLITE

324.9 329.0 SILICIFIED PYRITIFEROUS ARGILLITE -somewhat coarse grained 21827 324.0 325.0 1.0 15 -pyrite is more coarsely crystalline 1828 325.0 327.0 2.0 <5 -minor indications of hematite staining 1829 327.0 329.0 2.0 10

HOLE 465%84_ 7 SHEET OF d,


329.0 331.8 PYRITIFEROUS BLACK ARGILLITE -pyrite has returned to the nodular habit seen higher in the Z1830 329.0 331.8 2.8 <5 stratigraphy (20-23% py/sxn) ,

331.8 332.1 VARIEGATED BANDED CHERT -finely laminated cherts in pale greens, whites, mauves and buffs 1831 331.8 332.1 0.3 10 (orange) -some clots of. pyrite (3,4% py/sxn)

332.1 335.1 SILICIFIED WACKE -small section of what may have been a wacke 1832 332.1 333.5 1.4 <5 -some fine disseminated sulfides ( 3% py/sxn)

1852 333.5 335.0 1.5 5 335.1 337.5 SLIGHTLY ALTERED BASALT

337.5 358.6 SILICIFIED PYRITIFEROUS WACKE -5-7% py/sxn 1833 337.0 339.0 2.0 <5

338.6 344.6 BANDED ARGILLITE AND CHERT ? -chert-like sections may simply be altered or silicified

344.6 365.1 ALTERED GREYWACKE -bleached bands and swaths in a brown and greenish gritty rock 1634 360.0 362.0 2.0 <5 -some subsections appear to be argillaceous 1835 362.0 364.0 2.0 5 -some massive pyrites and po at 364.0' 1836 364.0 366.0 2.0 5 -some sulfide mineralization associated with qtz vein at 363.0'

365.1 366.1 ALTERED PYRITIFEROUS ARGILLITE ...,, -10-12% pyrite in an altered, partially recrystallized argillite

366.1 406.0 PYROXENE GABBRO / PORPH'C ANDESITE -variably altered cdarse grained grey rock, numerous bleached 1837 380.0 382.0 2.0 <5 fractures 1838 382.0 384.0 2.0 <5 -mineralized mainly in po, py and cp respectively 1839 384.0 386.0 2.0 <5

1840 386.0 388.0 2.0 <5 406.0 418.4 LIGHTLY ALTERED GRAYWACKE AND ARGILLITE 1841 388.0 390.0 2.0 <5

418.4 499.7 VARIABLY TEXTURED PYROXENE GABBRO -medium to coarse grained, dark grey green rock Characterized by 1842 418.0 420.0 2.0 <5 irregular lathy green pyx phenocrysts 1843 420.0 422.0 2.0 (5

-bleached cartnnated filled fractures are ubiquitous 1844 422.0 424.0 2.0 <5

HOLE 05-..ey-i, SHEET 4 OF 4

FROM DESCRIPTION SAMPLE FROM C.L. ppb Au oz Au/t ppbAg TO TO

418.4 - 499.7 (con't)

-upper contact with sediments is highly altered with qtz veining po and py mineralization -minor cp associated with po occurs at 472.0' -lower part of section is quite coarse grained and appears to have undergone greater hydrothermal alteration

ALTERED BASALT -light grey green, partially recrystallized basalt

ND OF HOLE

499.7

5 45 45 <5

<5 <5 500.0

500.0

21845 424.0 426.0 2.0 1846 426.0 428.0 2.0 1847 465.0 467.0 2.0 1848 467.0 469.0 2.0 1849 469.0 471.0 2.0 1850 471.0 473.0 2.0 1851 473.0 475.0 2.0

WEST-FIELD MINERALS LIMITED PROPERTY AREA LAC GAGNON NTS

Location 20+801V3+35N Claim Azimuth 0000 Tests acid test at Hole 405-84-10

Logged Alex E. Marr Latitude Dip -45 451' = Sheet I of 3

Started 28 Nov/84 Departure Depth 471 40°

Completed 1 Dec/84 Elevation .Core BQ

•-,-

FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au ppb Ag

0.0 10.0 CASING ,

10.0 121.9 LIGIITLY ALTERED PYROXENE GABBRO -characterized by abundant specks -silicified, altered section at 82.2-83.0 and 86.9-87.6 -some minor sulfide mineralization associated with thin qtz-carb veins •

121.9 134.0 ALTERED BASALT -very fine to medium grained volcanic with occasional aggregates of Z1893 126.0 128.0 2.0 < 5 po and pyrite (‘1% /sxn) 1894 128.0 130.0 2.0 <5

134.0 163.0 LIGHTLY ALTERED PYROXENE GABBRO -as above Z1895 150.0 152.0 2.0 <5 -thin (.5") mineralized qtz vein at 151.4 -swathy alteration (411% py/sxn)

163.0 164.3 PORPHYRITIC ANDESITE Z1896 163.0 165.0 2.0 <5 .

164.3 176.0 LIGHTLY ALTERED PYROXENE GABBRO

176.0 179.2 BASALT '

179.2 218.0 VARIABLY ALTERED PYROXENE GABBRO

218.0 222.1. PORPIIYRITIC DACITE Z1897 218.0 240.0 2.0 <5 -occasional small aggregates of po (QS po/sxn) 1898 220.0 222.0 2.0 10

222.1 261.0 VARIABLY ALTERED PYROXENE GABBRO

. .

HOLE 40.5..94_1 SHEET 2. OF ,3


261.0 270.5 PORPHYRITIC ANDESITE \ . -abundant large zoned plag. crystalt 21899 261.0 263.0 2.0 10 -matrix is dark grey with abundant disseminated and clotted sulfide 21900 263.0 265.0 2.0 10 po, py and cp (5-7% sul./sxn) 1901 265.0 267.0 2.0 <5

1902 267.0 269.0 2.0 5 !270.5 282.4 PYROXENE GABBRO 1903 269.0 271.0 2.0 <5

-medium to fine grained gabbroic rock -some small subsections may be basaltic

282.4 287.0 FINE PORPHYRITIC ANDESITE 21904 284.0 286.0 2.0 15

287.0 300.0 ALTERED PYROXENE GABBRO , -

300.0 317.3 BASALT ' -very fine grained dark grey rock 21905 300.0 302.0 2.0 <5 -swathy alteration dominates the upper three feet of section 1906 302.0 304.0 2.0 <5 ' -remainder of section remains relatively unaltered

317.3 343.4 VARIABLY ALTERED, PYRITIFEROUS BANDED ARGILLITE •

-pyrite occurs as nodular to lacey aggregates with some rare, thin 1907 317.0 319.0 2.0 <5 massive sections 1908 319.0 321.0 2.0 5 -332.5-335.9 silicified section (8-101 py/sxn) 1909 321.0 323.0 2.0 <5

1910 323.0 325.0 2.0 5 343.4 355.6 GRITTY ARGILLITE 1911 325.0 327.0 2..0 10

-generally fine grained, brown banded sediment 1912 327.0 329.0 2.0 <5 -hematite stain in qtz vein at 348' 1913 329.0 331.0 2.0 10

1914 331.0 333.0 2.0 10 355.6 358.0 BASALT FLOW 1915 333.0 335.0 2.0 S

-altered, partially recrystallized basalt '1916 335.0 337.0 2.0 5 -minor po associated with qtz vein at 356.8' 1917 337.0 339.0 2.0 10 600@338'

1918 339.0 341.0 2.0 5 358.0 370.0 INTERBEDDED GREYWACKE AisID GRITTY BROWN ARGILLITE 1919 341.0 343.0 2.0 <5

1920 347.0 349.0 2.0 <5 370.0 373.7 BASALT FLOWS / TUFF 1921 356.0 358.0 2.0 <5

' -amygdaloidal and apharitic greenish basalt -some phenocrysts suggest that the lithology may be more tuf faceous in origin than an altered basalt

.

HOLE tos_ qq_ SHEET 3 OF _..

FROM TO

•

DESCRIPTION SAMPLE FROM TO

._._

C.L.

_

ppb Au oz Au/t ppb Ag

-- 373.7 459.9 INTERBEDDED GREYWACKE GRITTY ARGILLITE AND BASALT FLOWS

-aside from several basaltic and tuffaceous flows/beds which are usually less than one foot in thickness, this section represents a monotonous sequence of lightly clastic mudstones and siltstones

700@444'

459.9 464.5 ALTERED GREYWACKE ? -original rock type is obscured by 4 "grainy" texture due to carbonate alteration -may be a clastic sediment

469.5 471.0 GREYWACKE

471.0 END OF HOLE

*intensity of bleached fracturings is very low, below the pyritiferous argillites in this hole accounting for the low degree of alteration

This hole hit a very large sand seam and was terminated at 471'

•

, .

MIS PROPERTY AREA LAC GAGNON WESTFIELD MINERALS LIMITED

Azimuth 000° Tests

@ 500' - 39° Sheet 1 of 3 Dip -450

Depth 500'

• COre BQ

Location 20+80W/2+50N

Logged Alex E. Marr

Started 28 Nov/84

Completed 30 Nov/84


t

ii- 44 CA.

0.0 82.0 CASING '

82.0 223.0 111INLY INTERBEDDED GREYWACKE AND GRITTY ARGILLITES -a broad sequence of mainly dark brown clastic sediments displaying varying degrees of minor alteration

Z1853 109.0 111.0 2.0 <5 60°@92'

-bleached fracturing occurs from the top to the bottom of the Z1854 164.0 166.0 2.0 <5 section and appears to be responsible for the alteration 21855 166.0 168.0 2.0 <5 53o@114 -a biotite or plogopite rich subsection occurs from 109.1-110.3 -small mineralized qtz vein at 166.3 (minor py) -minor basalt flow at 186.2-186.8 and 210.8-211.1

223.0 225.8 BLACK ARGILLITE -minor disseminated pyrite -numerous hairline carbonate-filled fractures -non conductive

225.8 226.8 SILICIFIED ARGILLITE

226.8 228.0 ALTERED BLACK ARGILLITE Z1856 225.0 227.0 2.0 <5 -less silicified than the pale grey silicified argillite above

228.0 228.4 BASALT .

228.4 231.0 ARGILLITE AND TUFFACEOUS COMPONENT -rock has cored very poorly probably due to a heterogeneity in the matrix -it seems the rock is largely argillaceous with a slightly gritty and chloritic component which may originate from a water-lain tuff

Hole 405-84-11 Claim

Latitude

Departure

Elevation

HOLE ',Os-R./Ai SHEET 2 OF 3

FROM TO DESCRIPTION . •

SAMPLE FROM TO C.L. ppb Au ppb Ag 4 -la C.4

231.0 305.0 ARGILLACEOUS MOOS AND ARGILLITE ' . -broad sequence of notably argillaceous (dark, t fissile) greywackes interbedded with brown argillites

• •

-most sulfide appears restricted to Conductive fractures -upper forty feet of section contains numerous subsections of re- . crystallized 'snowflake' textured sediment . -occasional very localized altered sections

305.0 305.9 BASALT • . •

305.9 307.6 HOMY ALTERED ARGILLITE - • -lightly silicified and carbonated 21857 306.0 308.0 2.0 <5 50o@133'

21858 308.0 310.0 2.0 <5 307.6 320.9 WELL SILICIFIED AND CARBONATED ARGILLITE Z1859 310.0 312.0 2.0 <5

-5-7% disseminated sulfide over section • 21860 312.0 314.0 2.0 <5 -alteration varies, some sections show wispy alteration Z1861 314.0 316.0 2.0 <5

Z1862 316.0 318.0 2.0 <5 320.9 335.0 PYRITIFEROUS BLACK ARGILLITE 21863 318.0 320 ..0 2.0 <5

-mainly black argillite with lacey and nodular py . 21864 320.0 322.0 2.0 <5 • -some altered sections 325.9-327.2 and 331.7-333.0 contains Z1865 322.0 . 324.0 2.0 <5

abundant disseminated py (10% py/sxn) 21866 324.0 326.0 2.0 <5 21867 326.0 328.0 2.0 <5

335.0 341.0 AMYGDALOIDAL BASALT ' 21868 328.0 330.0 2.0 10 ...'' . -variably altered amygdaloidal basalt with abundant aggregates 21869 330.0 332.0 2.0 <5

of pyrite at 336.5; 338.0 (3-5% PY/sxn) 21870 332.0 334.0 2.0 <5 21871 334.0 336.0 2.0 <5 •

341.0 357.8 VARIABLY TEXTURED/ALTERED ARGILLITE 21872 336.0 338.0 2.0 <5 -generally a py's argillite with mainly disseminated sulfide Z1873 338.0 340.0 2.0 <5

(3-71 /sxn) Z1874 340.0 342.0 2.0 <5 -lower seven feet is cherty with some clots of garnet ? tourmaline ? 21875 342.0 344.0 2,0 <5 -degree of alteration is quite intense here 21876 344.0 346.0 2.0 <5

. 21877 346.0 348.0 2.0 15 357.8 396.0 WELL ALTERED BASALT 21878 348.0 350.0 2.0 15

-coarse recrystallized basalt 21879 350.0 352.0 2.0 5 ' -very well carbonated with abundant disseminated and clotted po 21880 352.0 354.0 2.0 10 -small qtz-carbonate veins tend to cluster in upper 15 feet of sxn 21881 354.0 356.0 2.0 <5 • -bleached fractures often are well mineralized in po and often have Z1882 356.0 358.0 2.0 <5 •

a considerable bleached halo 21883 358.0 360.0 2.0 5

'

,

HOLE SHEET OF

FROM TO DESCRIPTION . SAMPLE FROM ' TO • C.L. ppb Au ppb Ag 31. 4o C.4.

396.0 42/.5 ALTERED PYROKEND GABBRO -Carbonate flecked and locally mineralized in po and py 21884 360.0 362.0 2.0 45 • -bleached fractures are common 21885 342.0 364.0 2.0 ',5

21886 364.0 366.0 2.0 45 427.5 436.4 ALTERED BASALT .

• Z1687 21888

366.0 368.0

368.0 370.0

.2.0 2.0

45 “

.

436.4 439.0 PYRITIFEROUS SILICIFIED BASALT . -fine grained 2188.9 410.0 412.0 2.0 5 -silicified basalt with several thin streaks of massive to irregular aggregated pyrite

21890 412.0 414.0 2.0 45

-middle of section is districtly dierty (6-7% py/sxn) 21891 436.0 438.0 2.0. 5 21892 438.0 440.0 2.0 5

439.0 461.0 PYROXENEGABBRO. -variably altered - lightly carbonated

• 461.0 462.1 PORMITITIC ANDESITE

• 462.1 492.5 PYROXENE GABBRO'

• 492.5 494.3 PORIUMTIC ANDESITE

.

494.3 500.0 PYROXENE GABBRO . . ' ,

500.0 END OF HOLE . .

•

. . .

• •

•

• . •

PROPERTY AREA MIS WESTFIELD MINERALS LIMITED

Hole 40S-84-12

Sheet 1 of 4

Tests test at 5001 =

"P-40

Location 20+80W/0+50S

Logged A. E. Marr

Started 25 November/84

Completed 27 November/84

ClaiM Azimuth 000"

Latitude Dip -45°


Elevation • Core BO

•

FROM TO DESCRIPTION SAMPLE FROM TO •

C.L. ppb Au ppb Ag

• •

0 28.0 casing O Z1767 28 30 5 .

68 30 32 <5 28.0 39.3 ALTERED BASALT: 69 32 34 5

- typical reddish-brown basalt with "swathy" bleached sections; 11770 34 36 <5 -

altered sections contain abundant recrystallized pyrite 71 36 38 <5 (2% pyrite over section). 72 38 40 <5

73 46 48 <5 74 48 50 <5

39.3 46.0 SILTSTONMANDESITE?: 75 50 52 <5 - very fine grainea, very dark reddish-brown rock; faint ghosts of 76 52 54 <5

bedding remain. 77 54 56 <5 78 56 58 <5

46.0 64.1 ALTERED ANDESITE: 79 58 '60 <5 - hard, also reddish-brown rock with numerous, irregular bleached 11780 60 62 <5 , sections, also veinlike alteration with abundant garnet(?); some 81 62 64 <5

haematite alteration. 82 64 66 <5 . 83 66 68 <5 . 64.1 65.4 ALTERED PYRITIFEROUS PORPHYRY: 84 68 70 5

- original rock type is obscured by alteration - may be a porphyritic andesite; contains 7% pyrite over section; well foliated.

85 96 98 <5 . .

• 65.4 65.8 BASALT .

65.8 66.9 PORPHYRITIC ANDESITE: • - some minor garnets in a lightly bleached matrix.

66.9 67.8 BASALT

, ,


FROM TO DESCRIPTION

_

SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 4 C.A.

67.8 69.7 ALTERED PORPHYRITIC ANDESITE(?): - alteration has created numerous streaks throughout section that are

reminiscent of chert; a central carbonated section contains several euhedral pyrite crystals.

69.7 87.1 ALTERED BASALT: - swathy alteration in fine-grained, aphanitic to slightly

recrystallized basalt, several minor aggregates of pyrrhotite and pyrite (,1.4% over section); argillite subsection at 78.6-79.3. .

87.1 103.9 VARIABLY ALTERED GABBRO: - coarse grained intermediate-mafic gabbro with occasional altered swaths.

103.9 107.6 PORPHYRITIC DACITE: - equigranular

107.6 182.6 • ALTERED BASALTS: Z1786 128 130 <5 - broad section of variably textured volcanic flows and possibly 7 130 132 <5

intrusive sills (i.e. coarse-grained subsections); swathy alteration 8 132 134 <5 is very common with some occasional aggregates of pyrrhotite and 9 134 136 <5 minor chalcopyrite especially at 131.5; curious nebular textures 90 181 183 <5 are noted at 150' - these seem to be due to an internal exsolution 1 183 185 <5 of fluids creating a local "slush" within the rock; this might be 2 185 187 <5 a precursor to the swathy alteration noted elsewhere. 3 212 214 <5

182.6 183.2 • TRANSITION ALTERATION ZONE: 4 5

214 234

216 236

5 <5

- altered section within which the original textures have been 6 236 238 5 oblitered; composed mainly of quartz carbonate and plagioclase with 7 238 240 10 some contamination from the bounding lithologies. 8 240 242 5

99 242 244 <5 183.2 186.8 PYRITIFEROUS ARGILLITE 8. CHERTY SEDIMENT: 11800 244 246 15

- section is mainly pyritiferous argillite with approximately 5% 01 246 248 10 pyrite over section; some subsections appear to have a cherty 2 248 250 <5 nature which has been rendered friable by the rock's argillaceous 3 250 252 5 component. 4 252 254 5

5 254 256 <5 50° @ 186.8 195.9 ALTERED SEDIMENT: GREYWACKE AND SILTSTONE(?): 6 256 258 <5 185'

7 258 260 5


FROM TO DESCRIPTION SAMPLE FROM TO C.L. ppb Au oz Au/t ppb Ag 111.4.C.A.

195.9 197.3 ALTERED BASALT '

197.3 201.8 ALTERED SEDIMENTS: - textural variations abound suggesting thinly interbedded argillite and greywacke; the typical swathy alteration makes difficult the distinction between sedimentary and volcanic rocks here.

201.8 235.8 SILTSTONE: - very uniform, dark brown, fine-grained rock; probably altered

lightly; some bedding planes are clearly visible; sulphides are limited to fracture surfaces.

235.8 246.7 PYRITIFEROOS ARGILLITE AND ARENITE: - banded, black argillite with abundant lacey and nodular pyrite;

banding is caused by arenaceous component; 5 broad bands of pyritiferous arenite are evenly interbedded with the argillite; overall sulphide is S8-10% pyrite over section.

246.7 260.0 GARNETIFEROUS BASALT: - large snowflake garnets(?) of varying size (41") occur abundantly

through section, lower part of section contains very fine garnets(?).

260.0 275.1 ALTERED BASALTS: - relatively highly altered basalt with scattered bleached fractures.

275.1 306.9 DARK PORPHYRITIC ANDESITE/GABBRO?: Z1808 308 310 5

. - dark, hard rock with fine-grained plagioclase matrix and pyroxene phenocrysts; occasional sulphide aggregates (pyrite, pyrrhotite 01% over section).

9 410 412 <5

306.9 312.0 PORPHYRITIC DACITE-ANDESITE: - fine-grained plagioclase matrix with abundant light plagioclase

phenocrysts - some appear zoned; fine clots of free quartz(?).

312.0 372.2 DARK PORPHYRITIC ANDESITE: - dark, hard, medium- to coarse-grained rock composed mainly of dark

plagioclase (labradorite-anorthite) and pyroxene phenocrysts (as above).

HOLE 405-84-12 SHEET 4 OF. 4


372.2 381.2 DACITIC GABBRO: - composition seems intermediate between dacite and andesite.

381.2 473.3 DARK GABBRO: - sporadically lightly altered dark, coarse-grained mafic gabbro; 4" quartz vein at 411.2; some minor sulphides in hangingwall.

473.3 477.1 ANDESITE: =WI-it—fine-grained dark gray rock.

477.1 479.2 DARK GABBRO: - as above

479.2 482.9 PORPHYRITIC DACITE

482.9 500.0 DARK GABBRO: - as above

- END OF HOLE -

•

, ,

PROPERTY AREA LAC GAGNON NTS

'= 40 ° Azimuth 0000 Tests at 564 Hole 405-84-13 Location 1+80S/20+80W

Logged Alex E. Marr Sheet 1 of 4 Dip -45°

Started 20 Nov/84 Depth 564'

• Core BQ

Claim

Latitude

Departure

Elevation Completed 23 Nov/84



0.0 60.0 CASING '

60.0 65.7 SILICIFIED PYRITIFEROUS ARGILLITE • -medium to dark grey altered argillite with numerous irregular 21626 66.0 68.0 2.0 5 aggregates of pyrite 21827 68.0 70.0 2.0 <5 -core is blocky and fractured 21828 70.0 72.0 2.0 15 -pyrite grades up to approx 12-15% over section due to finely Z1829 72.0 74.0 2.0 <5 disseminated pyrite 21830 74.0 76.0 2.0 <5

21831 76.0 78.0 2.0 <5 65.7 67.3 PYRITIFEROUS BLACK ARGILLITE Z1832 78.0 80.0 2.0 <5

-moderately conductive argillite and large irregular pyrite 21833 80.0 82.0 2.0 <5 aggregates (py- 40% sxn) 21834 82.0 84.0 2.0 <5

21835 84.0 86.0 2.0 <5 67.3 77.5 SILICIFIED PYRITIFEROUS ARGILLITE 21836 86.0 88.0 2.0 <5

-as above 21837 88.0 90.0 2.0 <5 -vary considerably from banded to massive 21838 90.0 92.0 2.0 <5 -very little sulfide to abundant, disseminated py; py ‘10-12%

77.5 92.4 BANDED PYRITIFEROUS BLACK ARGILLITE -black argillite intercalated with light grey silicified bands and thin bands of massive pyrite; (py.-10%)

92.4 115.8 INTERBEDDED BASALT AND ANDESITE -massive, aphanitic grey green rock with altered flow tops (possible garnets) -lower contact is anunconformity, upper contact is uncertain

115.8 143.0 VARIABLY ALTERED PYRITIFEROUS BLACK ARGILLITE -typical black py's argillite with numerous grey, silicified Z1839 116.0 118.0 • 2.0 <5 bands 21840 118.0 120.0 2.0 <5 50o@891

-sulfides occur as massive bands (..5,3 feet) and as irregular Z1841 120.0 122.0 2.0 <5 aggregates (py-S%) 21842 122.0 124.0 2.0 40

Hou 40jr..8413 SHEET z OF cL

TO FROM TO DESCRIPTION SAMPLE FROM C.L. ppb Au oz Au/t ppb Ag

ALTERED ANDES ITE -1-2% pyrite -locally garnet-rich

160.1 ARGILLITE -dark brown, very fine grain, across aggregates of pyrite 1%

172.6 TURBATED GREWACKE -upper 6 feet of section shows some banding with a cherty or siliceous component -the bands have been folded on some spots like large rip-up clasts -lower part of section appears to be a slightly foliated typical greywacke

214.4 VOLCANIC INTERMEDIATE AGGLOMERATE (?) -there appears to be numerous large assorted rock fragments in an andesitic matrix -fragments are mainly gabbroic and basaltic with oxidized orange reaction rims in some cases -some sbusections appear to be brecciated -lower part of section (200.7-211.0) is predominantly a bluish andesite -some very minor sulfide ( 1%)

228.9 PYRRIMITIFEROUS ALTERED BASALT -section is characterized by broad, irregular bleached swaths -top of section remains typically basaltic -fine grained, disseminated po occurs ubiquitously throughout section ( 10% po) -louer contact is a .5' breccia

270.0 ALTERED PYROXENE GABBRO' -coarse plag. matrix with large lathy pyx crystals -occasional q-c-filled fractures -occasional aggregates of po

ANDESITE

143.0

154.1

160.1

172.6

214.4

228.9

270.0 273.4

154.1 21643 21644 Z1645 Z1646 Z1647 Z1648 Z1649 Z1650 Z1651 Z1652 21653 Z1654 21655 Z1656 Z1657

21658 21659 11660 21661 21662 21663 Z1664 21665 Z1666 21667 Z1668 Z1669 21670 Z1671 Z1672 21673 21674 21675 Z1676 Z1677 Z1678

124.0 126.0 128.0 130.0 132.0 134.0 136.0 138.0 140.0 142.0 144.0 146.0 148.0 150.0 152.0

172.0 174.0 176.0 178.0 180.0 182.0 184.0 186.0 188.0 190.0 192.0 194.0 196.0 198.0 200.0 202.0 204.0 206.0 208.0 210.0 212.0

126.0 128.0 130.0 132.0 134.0 136.0 138.0 140.0 142.0 144.0 146.0 148.0 150.0 152.0 154.0

174.0 176.0 178.0 180.0 182.0 184.0 186.0 188.0 190.0 192.0 194.0 196.0 198.0 200.0 202.0 204.0 206.0 208.0 210.0 212.0 214.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0 2.0

90 <5

5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5

<5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5 <5

HOLE 40g. gq..13 SHEET

OF 4


273.4 352.5 VARIABLY ALTERED ANDESITES -mainly interbedded fine grained and porphyritic andesites charact- .Z1679 220.0 222.0 2.0 <5 orized by sections of the same swathy alteration seen between 21680 222.0 224.0 2.0 <5 214.4-228.9 -frequently these bleached swaths contain small blebs of po Z1681 353.0 355.0 20 5

352.5 355.5. ALTERED PORPHYRITIC DACITE •

355.5 357.3 ANDESITE Z1682 370.0 372.0 2.0 <5 21683 372.0 374.0 2.0 <5

357.3 358.3 SILICIFIED PORPHYRITIC DACITE -10-12% po 21684 448.0 450.0 2.0 <5

Z1685 450.0 452.0 2.0 <5 358.3 396.0 VARIABLY ALTERED ANDESITES , Z1686 452.0 454.0 2.0 <5

-as above Z1687 454.0 456.0 2.0 <5 - 3-5% po 21688 456.0 458.0 2.0 <5 -some garnets occur locally 21689 458.0 460.0 2.0 <5

Z1690 460.0 462.0. 2.0 <5 396.0 411.4 CREYWACKE Z1691 462.0 464.0 2.0 5

-dark brown fine grained rock with abundant whitish.clasts and 21692 464.0 466.0 2.0 <5 specks 21693 466.0 468.0 2.0 <5 -upper 5 feet are altered in the fashion of the bleached swaths 21694 468.0 470.0 2.0 <5 seen higher up Z1695 470.0 472.0 2.0. <5

Z1696 472.0 474.0 2.0 <5 411.4 449.3 VARIABLY ALTERED ANDESITES Z1697 474.0 476.0 2.0 (5

-as above 21698 476.0 478.0 2.0 <5 -2-3% po/sxn; lower contact is knife sharp Z1699 478.0 480,0 2.0 <5

Z1700 480.0 482.0 2.0 <5 449.3 485.4 SILICIFIED AND BLEACHED ANDESITE (?) Z1701 482.0 484.0 2.0 <5

-consipicuously altered rock characterized by intense bleached fracturing

21702 484.0 486.0 2.0 <5

-alteration has produced a waxy lustre to the cored surface

. -contains very finely disseminated sulfides, probably po (15%) .

I ,485.4 488.4 ALTERED PORPHYRITIC (?) ANDESITE -splotchy mauve to blackish-green textured rock -may be intrusive

HOLE 14 05- - i3 SHEET 4 OF q

FROM TO DESCRIPTION •

SAMPLE FROM TO C.L. ppb Au ppb Ag

488.4 490.7 AMYGDALOIDAL ANDESITE -fine grain dark rock with abundant dark green ovoids (amygdules)

490.7 507.0 ALTERED PORPHYRITIC (?).ANDESITE -as above with more textured variation -i.e. bleached swaths, fractures

, 507.0 512.2 ANDESITE .

' 512.2 517.9 ALTERED ANDESITE -

-some minor calcite bands ( 1 cm). . Z1703 512.0 514.0 2.0 5 -some light crystalline py mineralization ( 1%) Z1704 514.0 516.0 2.0 ' 5

Z1705 516.0 518.0 2.0 5 517.9 518.6 ALTERED WALL ROCK (ANDESITE)

-approx. 30-40% fine crystalline py disseminated through section -coarsely brecciated with'qtz-carb-chlorite as a groundmass

518.6 520.2 MASSIVE CALCITE VEIN -massive opagque crystalline calcite with some chloritic inclusions Z1706 518.0 518.2 0.2 20

520.2 522.3 PYRITIFEROUS, BRECCIATED, ALTERED ANDESITE -central section contains one foot flesh-coloured carbonate vein Z1707 518.2 520.0 . 1.8. 5 with a few percent crystalline py ZI708 520.0 522.0 2.0 5

522. 522.8 MASSIVE CALCITE VEIN -

522.8 524.4 ALTERED WALL ROCK (ANDESITE) ' -similar to above with fewer percent sulfides, approx 10-15% fine crystalline py Z1708 522.0 523.0 1.0 5

524.4 525.4 ANDESITE . -nice carbonate welded fault breccia at lower contact.

525.4 527.1 ALTERED ANDESITE

527.1 528.2 ANDESITE

528.2 564.0 ALTERED, BLEACHED ANDESITE . -as seen before -characterized by bleached swaths often mineralized with po (2-51/sxn)

564.0 END OF HOLE ,

APPENDIX 3

OVERBURDEN ASSAY RESULTS

ELEMENT LOWER

DETECTION LIMIT

.3,...•ORT; 014-3296

F7M; WESTFIELD MINERALS LIMITED E; 10-N0V-84 PROJECT:

METROD SIZE FRACTION SAMPLE TYPE

Tiré Assail AA -200 HEAVY MINERACCO. PULVERIZE -200

G ER

41.

sAfipLE PREPARATIONS EXTRACTION

NVDICE-TD1 KR. KCIIIIEN' • •• • • .ALEX BARR •

REKARKS; < MEANS LESS THAN. SAMPLE WEIGHT OF 20 GRAMS USED FOR GOLD DETERMINATION UNLESS OTHERWISE STATED.

CHECK-CONCENTRATION/SAMPLE-MEW RATIO FOR EFFECMETETECTIOLLEVEL-

SUBRITTED Sr; OVERBURDEN

& Company Ltd.

.notek Rd.. a. Ontario.

tda KU 8X3 .tone: (613) 749-2220

telex: 033-3233

Geochemical Lab Report

4,8, Company Ltd.

,notek Rd.. a. Ontario,

iada K1.1 8X5 none: (613) 749-2220

Telex: 053-3233

PNPAR7QLE Lab Report Geochemical

ts-br

PE 1 f—PkiFJEC'T:

IL 14-06-21374H - 165- 4L684-06-273/49 545 414'34-06-283/411 z 55 141 14-06-293/411 , 200 4Eb84-07-013/411 , 70

41-14474237!î DO 41:.34-07-033/411 10 • . 41084-07-043/4H • 5 41'14-07-053/411

315 IL 14-07-063/49

ts,AMPLE ELENERV-7—"Au TIUTEb iriER UNITS PPB • . -;••••

Si.-501=1}6463/411... Wr14-06-173/4} 90• . 41 1406-133/4.11. - 4L634-06*1?3/..411.. 60; . • !L4-06-2D3/4K 155

41:68.4't-0.47.727117.74.9.

41

LJ4-0L-243/4W 1050

4LC84-06-253/IH 30

41094-07-073149

dj 14;-07.*0831411.- 2°. <5 41:8E14-07-093/4H •5 it,,c44--

07:. 103/40 - 570 VI 14-07-113/411-. .

•

4L634=0T—T2si4H ,125 4r14-07-133/411 115

34-07-143/411 45 41684-07-153/411 175 ir14-07-163/411 •150

11:684-07-17..9411 15 J1484-07-183/411 170 41 34-07-193/49 50

RE IRTT-014-41Y6 • • •

DNDA

P." "clar-Gegg & Company Ltd.

•420 Canotek Rd., Ottawa. Ontario.

...,„Çanacla KU 8X5 I )hone: (613) 719-2220

relex: 053-3233 • . ••••Mt—irt---

• ,

Geochemieal Lab Report

= ; '‘ESTFIELD AijiERALS LIATTF.1) ; -'4ri't r'qri 11.i TT. - • •

-

-

• S17;: FRACTI511 St'inPLE TYPE - SAI1PLE.PiREPARATIORS'

Aq' :•F.P3: • RECitii• itT,f kti q it I l

NEPiVt 1:13 POLVF.RIZE

ItitiOICE 15: ALEX

WEIOHT..OF.."...2.4•Iii3A45;..VSED• FOR •

631i1.• GETFR3•I NAT ititi."...ONLES5-. iliftER14.1.;3E

. C.H.FCK. CONCEMTRt.ITIO.ilISARPLE . 11EIOHT - .RikTia.-.FOR•••EFFECTIVE -..DE.TEI:-TION . IEVEL..,•••••••... .• • . .

• . • . • ......• .•••:.- •

:-.r-7r COPIES TB: Af,`!(.7.LLEN ALtY; •

---.. -.•...---•....••••• -•••••.i. •-•••••:•••••••••••••••••••••.•:•....•••-•...".•••••••••••••

FAH . 41(01FCT,

"ndar-Clefat &Company Lid.

.5420 Canotek Rd* Otta%sa, Ontario, Canada K11 8X5 Phone: (613) 749-2220 Telex: 053-3233

Geochemical Lab Report QN1.;),API-CLE

••••

▪ RT; 014-3234

• 8.A?1PLE ELEPikf PIP PPB

'LE.ELERENT ER U.11..ITS

'i/Au rt3

34-01-3'

4.3't-01-5

tfopKii

95 17.44 20 20

30 18.6 <5

tiGL-34-05-r 451.—a4—r'r AA

61-84-05-07

R. —R4 —05 —09

-01 -6-

.ft.H07.

65..

UGL-34-05-10 WiL-84-05-11

VOL-24-06-02

45L-54-06-03

”

.;.•jE1734-06-07.::

<5 !4 .44 10

165 10 ...,4 .Y iéSZ'j

-a4-03-0 —34-03-0L

13.95 5.19 17.90

14.53

il6L —54 —06 —10 1-34—C'-11

VE11-84-44-12 iEL —i4 —06 —13

7.54

10.94 14.55

4.23

H1-34-06-14

-ra.-34-04-02 _14-04-03

4-04-04 . 7L-1

—34-04-05

4075

410 160

-D4 —07 -b4-047U-:

r;-...-34-04711

60 1r

25 18.64 300 110

• 1245 200 16.56 35 • 10— :11.55 20.... 17.53

adar-Clegg & Company Ltd.

4 Belfast Road Ottawa, Ontario Canada K1G 025

...Rhone: (613) 237-3110 iex: 053-4435

m11111

..2EPTIRTtA117211

'..-FROM:-HESIFIELD MINERALS. LIAITE -110CT-734' PRD/ECT:

SIZE FRAL-- .1,r111 SAMPLE. TTPE'..

t DRDER' 'ELEMENT DETECTION,LTRIT EKTRAC

Ii Ai - PP AQUA REGIA vtIA

REPDRT CGPIES TO:- IR. ACRILLEN INVOICE' TO; RR. MCiLLEH

REMO DETECTION LIAITS'FOR DOI') 10 GRAM SPiE 5 PnE

un n Li7--10—FP". 1. GRAM SARPIE;' -50 PPB,

UNLE3S..11THERHISE. TATED

NOTE:

Georletnical Lab Report

ndar-Oagg & Company Ltd.

" 64 Belfast Road Ottawa, Ontario

F—Sainada K IG OZ5

one: (613) 237-3110 elex: 053-4455

AL6-04f4̀-i3, 20.00' 2040 20...ao'.

<7.; 20.00

20.00 <2

20.00 ' 20.00

1!5-34-27703-i3 KG-34-28-27-B-

:11 ;?:-34-30-14-3

SANLE, ELEREN

. .

lits;a4431

21.314477 iitf3-84-qa-to vo-p,o7-a-

"11614-10-127

lilt -14 -I,. -!13

WLE -84 -14 -0'3 -3 gLL -B4 -15 -'

gifit14 -17405 -2i-

-ULt-i24-14424 ,

10 0 20.00

<5 20;00 <5 20 0i.)

'0.10

Lv.00

20.00 24.00

<5 20.00,

20.00. 20.00 20..00

:1 20-.00


& Company Ltd.

Belfast Road aawa, Ontario mada KIG 025 sone: (613)237-3110 tiex: 053-4455

RFPaRT: 1.4-207?

FROA:.VESTFIELI.RINEkALSLINITEOE -DATE: - -OCTit rjLh,

ALEX AAR‘ Ta: RR, MIL

RERARKS; ( DETECTION LIAITS F R SOLO

ID GRAA SARPLE: 5 PPD..

5 &RAP! SARPLE: 10 PPB. - P7R.

SAME UT; la . UN ES F;EJSE STATED

NeTE' . . CHECK- CONCENTRiTIOR/SItARIE VEIGH RAIL

FTIR FFFrCTTilF rrIF TTyfiNi7i,F;


& Company Ltd. Belfast Road

davra, Ontario ,-anada K1G 025

hone: (613)237-3110 dex: 053-4455

PAGE 1 ... • •

• . ••• .

f`4u NHADER- utlITS

40 18.00

iLii-84-01-10 30 17.0g iL6-84-01-11

r GLG.-34-0.1-12 , 45 , 43.71-

416-0442-07 20 1Ç 79.

270

195:36: , 0

415

42-t0 ?0

,165;.2-216 L6-84-2-11 -4-v,

- A1_41

/1

70 ' "

0 !9r...?! L ut

Iv -d.,

„ 81_8-84-04-11 445

81..0-84-0471'; 17it, 13 83 , 4-

30 •-••••• ••••• • ••• • • • • •••-••••-•-•••••---• • ••• •••••••-••••• • --"•••••••••• -•••••• •

, , LILC-8it-05-13

„

lit.' —4 05 14. •-• -., •

VIG-84-0631 - 210V 7 04. ,

33 ' - 1

,15 to. 4

.q/0 3,

44°0 10 --p '4

20

.1.20

111;3-04-09,-t17 315 15.74

1/1.11-84-08-0E 435 7 ,44

GLG-84-ao-o? 490 17.87 5i30 10.4:

""" VLB-34-147-15 220 13. SC •

110 17.94

— KG-84-09- 1600 815 0i 111G-84-10-0i 1 1

11.17r

81.6-04-10-03 5 14v J,10 10.94

014-2a79REPRT

_eORT: 014-2/46

-EROA: VESTFIELO AIMERAIS LIMITED ATE: 18-OCT-84 PROJECT:

LOWER: RDER1cELEAEHT DETECTION:

'EPORT COPIES TO: R. ACKILLEN ALEX AARR

SOBAITTED-BTTAVERBORDEN DRILLING

-ERRS:: ALL SARPLE$ ARE .SUFFIXE 8T.-314. 10TPIHE ORIGINAL IATERIAL FOR :SAME IL6-64-20-03 HAS LOST DURING THE FIRE

SAAPLEAS:FROM THE 1/4 SPLIT TAKEN BY DERBORDEWDRILLINS. <AENS LESS THAN

DETECTIGN LIAITS FOR SOLD 10 GRAA SAAPLE: 5 PPD.

5 GRAM SAMPLE: 10 PPB. 1-fftt

SAMPLE T. 10 S. UNLESS OTHERVISE STATED.

NOTE: . CHECK CONCENTRATION/SAARI, HEIGHT RATIO

""."-----rlr--rrt-T-T-rirF 7 F martrtiEL,_

ART: 014-2946

APLE ELEAEAT Au utiAu. „ , ABER UNITS PPB GA •

'i3-84-15-10 6-84-15-11 ,

-.L6-84-15--ttV via-84-ia-a-*- ' G-84-15-14 4

'11_6-84-16-04 G-84-16-05

(50 •1.18 10 D.00

;10 5,20 <10 6.59-

.8-a4-20-03 60 3.00 `," ..'f,;‘,10 6.82

via-84-21 10 5.97 _G-G4-217; <10 4.97 _G-84-21-04 *41:

<10 4.16

"'_8-84-21-05 _3-64-22-01

VL8-84-22-02 4L3-84-22-03

_3-84-23-01

10 - 24.44

50 5.66

3695 .5.93 ` 810 30.00

105 4.07

kILG-64-23-02 L6-84-23-03 -6-84-23-04

ULG-84-24-01 41_6-84-24-02

170 19.76 215 20.05 25 29.37

20 4.44

<10 4.08

VIA-84-24-03 „AL8-84-24-04

L6-84-24-05 .L8-84-24-06

85 16.10 160 - 16.51 115 21.78

1035 20.94

7'1


wi_G-84-17-01 VL6-84-17-02

.G-84-17-03 _G-S4-17-04

10 4.12- ,

(10 4.91 T3850 13.04

435 8,50

45 5.48

Geoehemical Lab Report

ondar-Clen & Company Lid.

7E4 Belfast Road Ottawa, Ontario canada K 1G 023

hone: (613) 237-3110 eke: 053-4453

••••

04f-iESTFIE1D-AI#ERALS LIALTE

.0.412:7PEc -8

GF 20 GRAS USED FOR fiDLA DE TE "I"

TE INATION rN-Er.'s 1THERVI3E R3

CHECK CONCERIRATION/SAAPIE VEIGRT RATIO FGR EFFECTIVE DETECTION ,LEVEL.

SIZE FRACTION AMPLT ;.,PREFARATIORS


. Company Ltd. ,ad

gaxie .1,0 023

013)237-3110 . 0$3-4355

PAGE PRildFCT;',

Z1802 r184.-1,

1304

...11130t:

11842 .11843 11844 11845 11846

;11PLE ELE1E{T Ai,wt./ Au NIITE .fl t1P I E 1.-.1..E8E14T WER UNIT

.76 117'

-17

LI PIJ Z1818 11817 714'20 21821

21822 . Z1823 119:-)4 71825 21824

11831

11632 L'1333 11334 11835 11936

11337 11838 11837 11840 21841

L1780

71737 1798

-177? 71-doo Asoi

15 <5 10 <5 10

Au PB

NOTE

<5

<5 <5

1797

Z1794

-PCRP: 014-361'

ROJECT; 405 PAGE -

iAPLE •ELEAE4I _3ABER: UNITs-

IAIPLE:,;„:ELEflE 148TE

1347 134a

Z1849 -2405

185

Z-1892 Z1893 Z1894 11895 1189&

11357

18'5? L1860

t.1362, 71147

L:4

R65

Z1897 Z1893 •Z1899 Z1900 Z1901 \

11902 Z1903 11904 11905 Z19011,

11907 Z1908 Z1909 Z1910- -11911

Z1912 Z1913 11914 Z1115 11916

21877 .373

i.1379 • 30:.,1 1381

7:1832

1334 ,

10-.00 10.00

<5 10.00 1C1 10.00 '- 10 10.00

B„t Company Ltd.

Jad .tario

.1G OZ5 6I3)237-3110

.053-4455


APPENDIX 4

DIAMOND DRILL ASSAY RESULTS

R.-ORT COPIES TO: RR. IICKILLEN ALEX tiARR

SAAPLE PREPARATIONS SIZE FRACTION SAtiPLE TYPE

-200 DRILL CORE CRUSIIT PULVERIZE -200 -200

RL. ORTr 01473400

F.-1: WESTFIELD HINERALS L D, E:'. 20710V-84 -PROJEL

SUBAITTED BY: A. AARR

LIAL.C.611

'LOVER G ER ELEHENT DETECTION LIBIT EXTRACTION

PPB AOUA REGIA Fire Assay AA ?PA 'NITRIC PERCHLOR DIG Colour isetr ic

ARKSv;:t MEANS LESS THAN NOTE: - _ SAME WEIGHT OF 20 GRABS --USED FOR GOLD DETERRINATION UNLESS OTHERWISE :

—STATED. CHECK CONCENTRATION/SABRE WEIGHT RATIO FOR EFFECTIVE DETECTION LEVEL.

Anon,

p.m

INVOICE TO: R. ACKILLEN

;onddr{:kidt &Company Ltd.

5420 Canotek Rd., Ottawa, Ontario,

anada KU 8X5 'hone: (618) 749-2220 &x:053-3233


Geoehemical Lab Report

& Company Ltd.

Canotek Rd.. dawa. Ontario.

Canada KIJ 8X5 ,.....Phone: (613) 749-2220

relex: 053-3233

PROJECT: 405

8421PLE ELERENT BER UNITS -

ALL-1115' 04-1116' f: -1117 ALL-111B 411-1119

i:l......-1110- 5 '2 ALL-1121 (5 <2 r-,-1122 <2 ; .-1123 5 <2 ALL-1124, t.5 50

.-1130

.-1131 ALL-1132 &.-1133

.-1134

01-1135 f .-1136

ALL-1138

ALL-1140 -1141

L-1142 ALL-1143 ALL-1144

ALL-1145. <5 <2

ALL-1146 45 4

L-1147: <5 3

<5 4

ALL-1149 <5 3

As PPR

ROTE SAMPLE ELERERT Au As RUBBER UNITS PPB PPIt

ROTE

R ORT: 014-3400

:r 11-0117-3345

-:ompany Lid.

Rd.. mark).

41.1 8X5 . (613) 749-2220

.: 053-3233

QNDAR- CLEGG Geochernical Lab Report

'SP WESTFIELD 'MINERALS-LIM fED ,TP- 12 -NOV -84 , PROJECT;

51TI1iTED BTT7A-NARR

LOVE.0. InD ELEMENT DETECTION LIMIT EXTRACTION METHOD SIZE FRACTION SAMPLE TYPE , SURLEIREPARATIONS

øi Au 5 PPO AgUA RESTA Fire Assay AA -200 DRILL CORE CRUSH,POLVERIZE -200

:PuiT-CPTES TO: ART-RtKILL ----TIVOItEl01-DE-DCKILLED ALEX RARR

RKS (MEANS LESS THAN NOTE: SARPLE HEIGHT OF 20 HAAS USED FOR GOLD DETERMINATION UNLESS OTHERUISE STATED. CHECK...CONCENTRATION/SAME...MUSH

RATIO-FOR-EFFECTIVE-DhieCHON-UEVEL.

C. -11-04--- <5

1?-4.405 <5

1,406 /r

C 1407 <5

1.408 <5

1444 (5 C 1445

C 1446 <5

C 1447 <5

C 1448 <5

F-PRIDECT: L

STAPLE N BER

ORT: 014-3335

NOTE SA:IRE ELERENT Au NURSER UNITS BBB

?ABE

C 1374 , <5 t, 1414 (5 C-375 <5 C 1415 <5 E 376 <5 C 1416 <5 E 1377 <5 C 1417 105 C "37g e:r

C 1418 <5

ç‘.1 E-11-19 <5 <5 C 1420 <5 <5 C 1421 <5 <5 C 1422 <5 <5 C 1423 <5

<5 ---1-14:E4 (5 <5 C 1425 <5 <5 C 1426 <5 <5 C 1427 5 <5 C 1428 <5

<5 -C-1429- <5 <5 C 1430 <5 <5 C 1431 <5 <5 C 1432 <5 <5 C 1433 <5

i L 1444 0 <5 C 1435 <5 <5 C 1436 <5 <5 C 1437 . <5 <5 C 1438 <5

<5- 1714,ii <5 <5 C 1440 <5 <5 C 1441 (,5 <5 C 1442 <5 <5 C 1443 <5

'E: 140777- -(5 : 1_, 04? iC 1410 - : <5 C. 1450

1411 : <5 • 11001 I 1412 . <5 11002 C 1413 ' <5 71003

C 1371 C '380 C 381 C` 1382 C,1383

C 1385 • C'386 C 39.7

1383

C 381 E 1390

t391 E 392 E ,393

C .400 1401

C 1402 C7 4 03

Company Lid.

.1( Rd.. ,ntario, IJ 8X5

. (613) 749.2220 053.3233

Geocheniteal Lab Report

. Company Lid.

41( Rd.: mark.,

KU 8X5 : (613) 749-2220

er 053.3233


FPROJECTI--PISE LE EtENENT

3ER UNITS ---110TFS

5

'10 <5 11

—1 11 <5 (5

7114.14 "KJ

:1015 •• 1,J

17 <5

&Company Ltd.

.20 Canotek Rd.. • —ttav.a. Ontario.

Canada KII 8X5 Phone: (613) 749-2220

relek: 053-3233


IT: 014-3436

WESTFIELD RINERALS LIAITED r: 2140V-84 PROJECT: 405

SUBMITTED BY; AARR

LOWER ELERENT DETECTION LIRIT EXTRACTION

"01 Au 5 PP B fi00A REGIA 112. wt/Au .01 gut

AE,Td00

Fire Assay AA

SIZE FRACTION SANE TYPE SARPLE PREPARATIONS

-200 GRILL CORE CRUSR.PULVERIZE -200 • -

1EPOR1 COPIES TO: RIG ACKILLEN

ALEX AARR

INVOICE TC: R. ACKILLEN

iilARKS: ' REARS LESS TRAg NOTE; SAMPLE WEIGHT OF 20 HAAS USED FOR - GOLD DETERMINATION UNLESS OTHERWISE

CHECK CONCENTRATION/SAMPLE WEIGHT RATIO FOR EFFECTIVE DETECTION LEVEL:.

11111111ft

7 L.

Geochernical Lab Report

.4.1ega &Company Ltd.

-20 Calumet: Rd.. Cztawa. Ontario. Canada. KIJ 8X5

P"'"Nane: (613) 749-2220 elvt: 03-3233

NOTE ir'LE ELENENT IER UNITS PPB

NOTE SANPLE ELENENT Au vtlAu HUBER UNITS PP B p

Z-758

:-1159

-_- 161 :'1162 =71163

2/4179 Z 180

1-1194 Z-1195 Z-1196 Z-1197 Z-1198

<5 <5

<5 10.00

<5 Z-1119 <5 10.00 <5 Z-1200 <5 10.00 <5 Z-I201 <5 10.00 <5 Z-1202 <5 10.00 <5

<5 <5 <5 <5 <5

<5 (5 <5

<5

<5 <5 <5 <5 <5

<5 <5

i;.1182 sJ

183 5

Z-1184 5

27185 <5

.136 <5

Z-1187 <5 <5

1189 (5

7-1 190 - (5

1191 (5

1192 <5

Z-1193 <5

-:E.„-JRT: .014,3436 PROJECT: 405

PAGE 1

K SA PLE.EI T. .......fiQUiljit.t. ERA.1.$4110tt. UN; ESS:-IfiTHR4ISE.

md2r-C1egg di Company Ltd.

764 Be Vast Road Ottawa, Ontario

mada RIG OZ5 lone: (613) 237-3110 tex: 053-4455

SIZE .SAMPLE TYPE

)1; UESTF1ELD

16


BondarClevg di Company Ltd.

764 Belfast Road Ottawa, Ontario Canada K1G 025 Phone: (613)237-3110 Telex: 053-4455

4•111

:PER t 11-1134

3AI121E ELEnENT .91-re

Z1 2t

21'

t • -

7.12:J 7.122?

r.:41231 ;5

El 232

Z1233 ""Z1234

—Z1235 ,

Z1236 55

1,--q.1231 ( r

PRgjECT:: GE

Z1246 1.124? 11250 11251

Z1253 21254 Z1255 Z1254 Z1257

egg & Company Ltd.

ast Road a, Ontario .

Ada K1G 025 .one: (613)237-3110

dex: 0534455

oviELD It—GCT,34,: PREEtt

< IEAA3LiSS 0EitLi1uit LINITS:FiR

's.10 GA A SAAPLE; 5 PP8. C?..41 AlrLEt 10 GRAA - SAAFL' '5G PPit

SAMPLE i; 10 G. U1LES3 YTHERV1Ri- STATE4

:5NCEN77ATIUU/SArtfIL ;iricF!T RMI - FR EFFECTIVE EIECT LEEi.



..gg &Company Ltd.

.ot Road Ontario

.da JOG 0Z5 Joe: (613)237-3110

elex: 033-4455

pROEST:.; 4

3P,F: !Kt

41,

21.

21.7-

''..

ammyLW..

ario. .1 8X5

,613) 749-2220 053-3233

C:N(DiNF3:7Qi__EG-71 Geochernical

Lab Report

T; 014-3275

001 gESTFIELIIIIIEEAFTTlifi TEO- T 10-NOV-84 PROJECT;

SDIVAITTEDITCRSTFIELD

LOYER Fr' , ELEMENT DETECTION LIMIT EXTRACTION METHOD' ' SIZE FRACTION SAMPLE TYPE . SAMPLE PREPARATIONS

. . . -- .

01 Au' - :1 PPB AQUA RESIA ' . Fire Assag AA -00 - DRILL CORE ,CRUSH,PULVERIZE, -200 . OA- - mt/Au.:,, 0 --:-As ' - -2' ',1-11111-L-L.--NITRIC-fERCHLOR-DIG-L:Colourisetric -200

-.

Pf T COPIES TO: RR. ACKILLEN INVOICE TO: R. ACKILLEN ALEX AARR

:r :KS: < MEANS LESS. THAN NOTE: SAMPLE WEIGHT 0F20 BARS USED FOR

DETERIINATIORAHLESS-OTHERWISE ..7STATED.

CHECK CONCENTRATION/SARRE WEIGHT RATIO FOR EFFECTIVE DETECTIONIEVEL.

£1285 <5 5 £1286 <5 9 £1287 <5 34 £1288 35 22

12 21 15 11 39

13 <2 <2 <2 2

(2 <2 <2 <2 <2

<2 <2 <2 <2

-ompany Ltd.

. Rd., Mario, tJ 8X5

(613) 749-2220 .: 053-3233

-EGG Geochemical Lab Report

PROJECT: FAME

<5 (5 <5 <5 <5

5 <5 <5

<5

15 24 15 45

7

6

AMALE ELERENT Au ut/Au As j.k1 UTI NOTE SAMPLE ELEMENT Au vt/Au As ,U ER , UNITS PP O PP R NUMBER UNITS PPB g PPR

,C1269 £1270 C1271 C1272 C1273

£1275 £1276 £1277 £1278

-£1279 (5 £1280 10 £1281 <5 (2 £1282 <5 £1283 <5 3

:132.9 1 -0

;1__1 ;1232

3

1234

:1 ;6

:1'48

E RI: 014-3275

:1 'IT 5 5 £1284 <5

C7-1V C: 50 C1251 Ct-152 C. 53

<5

<5 ----

2

'. <2

3

C12139---C1290 £1291 £1292 £1293

<5 (5 <5 10

C1254 (5- 2 C1274-- <5 C 55 <5 (2 £1295 <5 ',:..56 <5 2 £1296 (5 C1257 <5 (2 £1297 <5 C-58 <5 <2 £1298 <5

£125?— Ç2 C12YY (ti

C°460 <5 <2 £1300 <5 C 61 <5 3 £1301 <5 ci262 <5 C1302 30 C4:263 <5 4 £1303 <5

CI L64 <5- t1J04 C1265 CP-66

5 20 £1305 £1306

(5 (5

C. :.67 <5 27 £1307 <5 C1268 11 £1308

Company Ltd.

,ek Rd.. Ontario. KU SX5

.e: (613) 749.2220 .ex: 053-3233

4 ONDAR-7.CLE . • :••••• • • •


il AT; 014--3275

41 ER'

r,Tio it

r.1312 :r13

:1.1t5 <5

(5 <2

5 <2

5 <2 <2 <2

0,6

0,6.1

10666,0"

APPENDIX 5

DIGHEMIII

SURVEY OF THE RAYMOND TWP. AREA, QUEBEC FOR MPH CONSULTING LTD. BY DIGHEM SURVEYS AND

PROCESSING INC.

(For maps and drawings accompanying appendix 5, please refer to previously filed work for 1984.)

Voir alg-91/5"-

APPENDIX 6

REPORT ON MAGNETOMETER, HORIZONTAL LOOP EM AND IP/RESISTIVITY SURVEYS

LAC GAGNON PROJECT, RAYMOND TWP., QUEBEC

(For maps and drawings accompanying appendix 6, please refer to previously filed work for 1984.)

Fell'. i)(34.1. ayNck .liAlmots see clwl - 442.44 16,

APPENDIX 7

SAMPLING METHODOLOGY FOR OVERBURDEN DRILL SAMPLING

OVERBURDEN DRILLING MANAGEMENT LIMITED

SAMPLE PROCESSING FLOW SHEET

+ 250g STORE

+17094 STORE

Light Fraction STORE

Bulk Sample 5 7 kg

Split

Wet Sieve 1700/4

Shaking Table & Gold Grain Count

Light Fraction STORE

4.--]

Heavy Liquid Separation (Methylene Iodide SG 3.3)

Magnetic Fraction STORE

1/4 STORE

Magnetic Separation

Split

3/4 Ship to

Analytical Laboratory

OV

ER

BU

RD

EN

DR

ILL

ING

MA

NA

GE

ME

NT

LIM

ITE

D

901

3

1d

111VS

AU

OIV

EIO

BV

1

Number assigned to sample in the field S

am

ple

Nu

mb

er

a 250 Weight of

gram whole representative

sample as received split (geochem)

from the field

,

less cn —1 vo -a

We

ight (k

g, we

t)

WeLght of sample greater than 10 mesh .

033 v.+ 608 mo.

fed WeLght

across of sabple

the less

shaicing than table.

10 uesh. This

,

pe?rt'-on is -1 m. m 1 a m - 0.07.0

Dry shaking

weight table

of heavy mineral split recovered from the -1 0. 0, 0 (IN

Weig

ht (g

ram

s d

ry)

We:..ght specific

of shaking gravity.

table

,

concentrate less than

e.

3.3

4 4

M. I .

Lig

hts

We:ght gravity

of with

table magnetic

cormentrate fractLon

heavier

.

reuoved than

4

3.3

_

spec:Jic z 0 = m 0

Magnetic fraction of neavy ninEral

- .

concentrate

.

m m 0

,

DescrLption visible on the

and size shaking

(in microns) of gold table

.

grains

.

p

m

DescrLption

Clast

Presence

percentages

of

of

other

texture:

materials

-

a.g

.

granules,

e.g. pure wocd

-4

cobbles,

alay ahips

clumpç

.

pebbLes

+ 8

0 CD C,) ,-, 6 8 m

DescrLption: e.g. sorted, unsorted, colour, texture c m - , _ .

DescrLption: Till, Gravel,

-

Sand

Cla

ssif

icatio

n

_

A

D

IR

SD

to OVERBURDEN DRILLING MANAGEMENT LIMITED

3 CLEOPATRA DRIVE, NEPEAN, ONTARIO K2G 3M9 (613) 226-1774

LIST OF ABBREVIATIONS USED ON LAB DATA SHEETS:

Tr Trace

Cobs Cobbles

Pebs Pebbles

GCls Gritty clay balls

SCls Smooth clay balls

V/S Volcanic and/or sedimentary rocks

Gr Granitic rocks

Lime Limestone

ABBREVIATIONS USED FOR GOLD DESCRIPTION:

Abraded

Rounded

Delicate

Irregular

Simple delicate

simple delicate

IRREGULAR

Some flat irregular grains may become curled

ABRADED

Curled irregular grains become spind-led abraded grains

DELICATE

Bedrock gold crystallizes as pitted granular masses with smooth protruding crystals

IRREGULAR

After short ice transport, crystals are removed leaving smaller pitted grain with several pro-trusions

ABRADED

With increasing trans-port, protrusions break off irregular grain, producing several smaller leaf-shaped grains. Pitted surfaces become smooth.

ROUNDED

After long transport, especially in streams, continued abrasion produces small, polished, spherical or ellipsoidal grains 0 1000

Microns

Effects of Glacial Transport on Gold Particle Size and Shape (Developed by OVERBURDEN DRILLING MANAGEMENT LTD.)

VISIBLE LD FROM SHAKING TABLE ANL \ ANNING

-AMPLE UMBER

SIZE OF A

GOLD BY IR

SHAPE D Remarks

SAMPLE NUMBER

SIZE OF A

_

GOLD IR

BY SHAPE D Remarks

- oz. -cq 100 x 100 15-0 x 'so

iso x zoo -.46)( 660

x .y..)0

6ut-t-Ides _

•

100 x i-.0 50x 1°C) Io xis° iL70 X QC>0 )50 X a5-0

TRACE

-PtIRIT (00°/0 sulActe

)

,

VISIBLE GOLD FROM SHAKING TABLE AND PANNING .

AMPLE 1UMBER

SIZE OF A •

GOLD IR

BY SHAPE D

-

Remark E SAMPLE NUMBER

SIZE A

OF GOLD IR.

BY SHAPE D Remarks

WiLtz -84 - —II —03

6-ax ISO /00Xi.ÇO

cCOK ZOO -‹ 1 cle,' • (-.11 -Pidez

• •

•

— , • .270 P } —

-- _

/60X/5 • 50A 5- CD

alin ci e_s- cee qfr a/ r_

Otte ctIltet clizte-4,cx. .

-

---/q.-02.

zirn,nîe Fx7rvie becatc; op j#,e,

NeD 1-12fcles

, -2COrt OVSOICF4/0 It

,

, ) ,t,arfrie,

—

—

/6o .'c /..5CD /00x / 0 0 -SC°X 1-oc '

7-ace Sul Fides

--c)4 - 05- 50 x 5 C /to A. /Go /c,ox /so

--..• 1 (7°A' su/-eitv,S

-:)£:3 pox /co

Job x 41:70

/ex .x 2 t

rr6i.ce_ so/Pc/fez

.1

,

,_

".„

_

•

rTi ni r' ni rTi V 3Ur _ LIN 'IAN .ME LIN 1 r-i LABORATORY SAMPLE LOG

Sample

Number

Weight (kg. wet) Weight (grams dry) Grains

V. G.

Desc ipt ion

Classification Table Split Rock

Chips Table Feed

Table Conc

M.I. Lights Non-mag Mag + 10 Matrix

AIL'-.84

-01 - 0 i -71 .6 6.1 /9,v. 0 is-5, / dq, I .8 - Pebs 40'7, vls Lel. Sr

unsorted beige wi+-1,1 silt TILL

'?.9 1.0 /. 9 /4-33 99,8 14. 3 19..2_ _ robs .5 - 5% OS ar 77-- L.S.

a vlsorket1 1 re9 - beige toil-li si 1-f II

8.1 0. 8 7.3 /2I• 6 9 1.1 30.4 14.7 -- 1)5-e ob;,. fr1) 7c -7--rv11, 5. Il ti

04, 7,5- 180.4 1.33,1 3..1.3 /4.9 _____

6 S-47. Sr Tr. L.S. Pe_bs 4 6.-% V/S

- or 7.I. O. ,:l 7.4- /86.4 1.16,7 44.4 /5, 3 .- Pe b s s5:::/c. VZSr avicaSif it-rt-1 cl s 1 ilf '3 e n

7:7 0.3 7.'1 101.8 53.0 36.9 II. 9 - il II ii

- 0 7 6,9 0.5- 4.4 //1.2 /30.5 ,26.4 10.3 - II h II

- 6 8 1, 7 I9.7 7.0 3.22.7 ..214,4 1 L. 0 / 2., 3 - 12c19 5-6% V /S 5-07, 6r il II

- 0 ,2 - 0 i 2.4. 0.1 '3. 6 41.4 35-.9 5,0 D. 5- - Fe'd Pe bs 6. or te,A be

e SAND

0.3 .7. / /38..7 /13,4 /9,! 6. ,2_ _ Cobs .1,6017 &. vIrs u ilosoi rf-ii-,ed 6.1!:irk e TILL

- 0 3 7. 5- 0.5 7.0 89.3 58,3 1,2, 0 9. o - CI° I's 5-6e7° v / s 5-6 °70 G r if

- 04 1. 2 1.2 6.0 /.26.1 111.7 - '7. 2 7.8 _ Pe b S 71)% V /5 307, Gr

r i ii

- 05 5.2 0.7 4.5 5 9.2 -14.5" 10-2 -I . 3- - IP LthSOrfed q Ve9 - beqefe toi -PG, sill-

,I

- Db 8.0 1.1- G, .3 /05- .8 q 0, 4 6. 5" 8,7 IIX .1f-g ,' uh.sorted ,Ci .r&, 7 Ci'reeri (.0ifli .5i It II

- 0 3 - 01 5,4 0„,2 5- .1 5-4.8 49, 3 5-, y .2.

0 Peb5 4.61C 46 407, A.-. 0 CL

ithSOri-C'd bei3t W4-/' c/ati

II

- 0,2 L • 6 0.3 6• .1 96.5" 84.2 -7,4 307c 1 I /5 7- 0%c Sr -re L.S.

ariSor+ed qr-e - beige 44:,i -t-1.4 c I a ti It

- 03 7.5 0, 6 6. 9 I se . g / , ,? . 8 .24, a /4. e ___ Peb 5 4400,7, voLys* belt hisgo:t eLocil 4_ resiTt, I.

7..1 0. 7,1 1S.2 1/0.0 - 01

30. g i s-, 4A 0 X IS-10

Pebs 11-01, vls

3 0'1, 6'r II if

- Or 7,1 0.6 6.6 191-5" 11,2.1 .2,,,,2 6.4 - If Il II

r ni r ni ni r-1

LABORATORY SAMPLE LOG

Sample

Number

Weight (kg, wet) Weight (grams dry) Grains

V. G.

Description

Classification Table Split

R 1 +07(

Chips Table-1 Feed

Table Conc

M.I. Lights Non-mag Mag +10 Matrix

A I 1-0 - 81-

- / • / 6 6 /35.71- -1.1. 3-1.-,5 / 7-D // /

6 C7c473 :11230 0C ;eVICS it- t41/7;e;tl-t7;;It Siff 77 /4---- /• 0 1.0 -57 -2 3.---). 3- /0-.2 8-6--

Cot,:-, 35-% \//.3 it /I

-06 61- /-1- 7.6) 199.5- 161.7 a...z, /2-8 cc-Ls so cA vi,s

00-A e4v. n

5.:2 /.,-.) 7-1-p b5J4 0.7 3 /.7 8-1. 11 11 if _

.o -i 6.1 0 .F --1.L 1673 /3n /77 10-0 p,h--,s 45%W.S 5-5-% Tie. e_,s.

ii 11

- 01- --01 ._73- -1- 0-1 33 76.7 6q.e 5-49 3./ PErno fv°. /̀ -̀0//.'2s. '1)°„1--/ef.e lvt, ititiZy ,6%)\-)D

-0Q e.3 / - .2 7 . 1 /5-g6 /06-3 ,3-).2 6 /3.8 l5 )(ie1ai-)6:-,°.cli-iT.s. tgeqe114k4A1-.

-03 0.3 0-6 .7-7 Ibq Q 117-033 6. 46-9 peloz- 90 Vo V /.7.) 10°/0 6r. -R. 1.--S-

11 Si

-01- -1-6 O. b.8 /77-7 a---3,7 f_.,0•3 /6:1 xhInsofoc- ii uwfrista-i--eccilfq.Kei Él

-06 7-S Of 7.1 q -7--2 '5-4.1- 27, 6- /6-: 3 F-èlc' ggiocti. 11 I 1 -714-

-o - (r) 6 .9 (J.:3 6. &) 146%0 /.5 6)8 o•C) e 67,3-- 3-6 c'kV/3

frr.• 017.SoKted bee

6-Oc/0 viii-frt cur. I i

-07 7.5- ,o.,, 7•3 1q9,5- /492 37°2 /3./ pekL 5-6--/Qvit

0,,vc, 6v. it if

-06 7-q C.3 7-6 03o-/ /4)7.3 45-13 / 7 0 --X-- •Pei(D

- 09 e,3 0.5- 7.S 75-.1 . 3 7.9 04.-1- 0 8. 1)<P'2.ic 'Pe ' ' ` - ' V:Itc).V6(iS/ it

- /0 0.3 002 e)./ /79.0 107-o 028:7-. /3.3 A1:14: /I WiZOrfeei ciraxi be ire ivitlit ._q11-- II

-- ll 6-1 07 7 7. ..;)f)P.).;2-.?a.-2.1 a.5.3--- 3Q.3 PekL In)t;‘,". u"tf°,(i=7-7 1,

•-/,. 7-6/ 6.6 7.3 15q.b 13q. ,31.2 /e-6 re-k, e..,0-ko5

40% 6e. 11

-osol 577 01 5-.3 /e/•:2_ 116-B .,?,6 9.8 6'663 --lovov/ Lii-70riceici retv.,

•-0,, .18 08 7-0 .-Iet)- 8 o.:31, 7 :3/-8 /0-3 V.Deio 45 c/01//..$

55"4; er. it ii

/ ( r--

I

1URI 1 Di AN( AN, MEI _IM


Sample

Number


V G.

Description

Classification Table

1,, Sp -

RIS Chips

;e T e

e ed

Table Conc

M. I. Lights Non-mag Mag + 10 Matrix

- '

-05-a3 7-9 <0 .1 73 ,7*-E.') IV.L .76 -2 q• 0 re bss ‘8,34_64„.. sôrted /.. e 1 'e

.fine -med . SAIOD

-01.- 7-9 <0.1 7.17 IIS.7 67-6 ,,3A 7-7 n ii ti

0.,-2. „TV 16,7s- /35-70 (>23-3 9.0Z -pejc, .23-c/0111.3

7.5-VoGie. onsoeted gra-jki bele WIPE ci TILL-

-00 g.o 06 7.1 c is-7 61 173.6,27-8 145- C-A27.etSLS Sc)f;e4///-47-_ h

-07 0-2 O7 7-6 ,5-.0-1- OW , C 33.7 /6 - '7 Fia3 10-/ows .3o70 f/.. Tr: Ls

unsorted grazi WI fit eladfy I

11

-06 f3-4 OS 7-6 0/•3-- 79.f c27. 3 / 41. Reis sovovi3

,.cpc/c>61-. 14/1..50,-1-ed qi-a4.i helve tAitiktif-

It

-oil 7-9 00 7./ 1.75-5/3.2-5 30-z 457-6, 1i it 11

•--10 -.1-., 0-5 6-8 17-6.6 /38.6 c,) 7. 3 107 tt fi

-I/ a5- 01 -lb LEAS" /so-? c.:)3.0 /0-6 Pe10.!') 9 5 ch V/..S /I ii

7:7 0-6 7-1 157-1- //g./ c 6-0 47.3 - tS.-1?/.3.„5-,/.71-erv.12s. ( •:/11n154VeCI 1 beg e H

--t0,2 7-6 04 7-02 04-4 F13.7 c5 9 (2. //.3 peia5 (o5Vc V/ 3.--/.6tt". Tr. LS.

un.5 Or ied t ' e tw nit ,sjj-f-.

II

-o-_,-3 e.1 1-0 •7.1 /53.7 /172 .2,3.? /c-6 co6,3 7 ocV01/13

,-307,,Y: li 11

-01 -0 0.6 7.Z q3.77- 6/.7 c2o6 //02_ e..k)

05--(1.0e. 11 11

- 7-9 (16 7.3 17q. 1433.3 ,30.7 /57 7 6 peios 4,5-'1/4) 6,-. bi7e viitm. clay if

- O -7 I 3 0- 71 Roi--0 /01. _3 _35 ,7,0- 6 Fia.,„ 40 clo&r.

il it

, -07 6.5 c-1- F-/ 13q. 7 ?la? o27-3 /5:,,2 P etos .---5:5-%vis -4-s--/oev..

II II

-08 1-3.1 01 0-0 po S got) cpe_et eg 1--- icL 5-Sttli,, II i I

_07 F)...4 6.6 7-b 051,.7,65-- 33.1 176 ":- rs-c8 Peic6 642://°c,Tr. II i I

CZ E-C) /60-I 101-4 40-4 /67J Rsias sown.)

6-070Gy- 1 1 I I

F-1

ET 1

F 0‘, /3UF J E LIN IAN iME LIN


D r

Sample

Number


V. G.

Desc iption

Classification Table Split Filo.g:13<

Chips T;tFe' Feed

Table Conc


WL_Q .-- P4 -

0.1 -TO /73.z 133-6 ‘- 2̀P),-S. ill petz ,__.,-oci,VisS

s-ocio6Y: Losorted gra-c/ heir with \s'ilf.

. TIL- I-

--1,_ -7 .(i ,o_,s- 7.1 IL5,,2 /0e..3 ,?q.0 /7-7 Pebs 4-scyc,9-- ii II -

-' 3 7, A 04 7.2_ icig.3.4 /51).0 3,3 7 /0 • 7 Pe icAs 5-0eic VAS 6-0 .̀/0 6r. 11 ii

- /T- g-0 0-1 IS 1(37.7 149.5- a3,/ As--7 70 6-yv: I/ h

-.-/Ô- ---fm al -11 93.c2 so./ a6./ x5-70 // /I II

.-1 ' .77 0,2_ 7.5- _ /460 //L).F5 -20-3 /4-?

-17 6-).7 067 b .1 73.1- lon 15--n 11,3 -rie-o-Tc:,-1677=t °L.I ub"s:°Ifet'elVtÊ,107 ii

-1e 0-7 0.5 - ' F)- :2 90-0 57-4 ..0-,D A.-D-1 Rio-ç &ockvis

-IC/ 1(0 0 0?_ 4.1 / 06 - LS e)6. I /4,s-- 57 Pe-6.' 55..-°4 S. 11 11

-o)0 OP) 7.7 p iT2 90).3 J./,. //f3 Pei(-_,3

7.1 k131 y 96,- 7 013. 5 /1.7 - Pei's' ggikt3)/ is J I

- ° '->- Fi• / 08 7.3 /43_ 1- 90_ ? (3.5"' /.--.7-40 il ii ii

-J3 g3.3 /-0 7.3 K3 .z 96-7 „7-4,-.5*-- /TB a 5-cic (Tv Il i I

-Of -4. ol- g3.O 14ao xr./ :>7.7- /,-).."2_ i-Lz.) 0 v. vis z:200/,e: il 11

1,7 0-6 71 /,-2 -3 ec6 -3Û-7 N.? /I /I il

--,--6, F34 07 '17 lt7-. 691 ( 2-6 -5- //7 AxY•s°0 57tétje"°. tV/ 1. 1-3 . i I I,

1,..;2. 7.:2_ ï4.429--3 17/ A, 45 ° é K. I i ii

/6 6-7 137-0 113.3 028:1 15.n Pe6s .75,-yok/i, Tr.L-s, (25-cyo&K i i if

'27 3-1 C--5.- 5-1- 70-1 47-3 /07-6 in ..-Z /0 "lo 6iv I i ri

ov 13UF IAN iME LIN


Sample Number

Weight (k g, wet) Weight ( grams dry) Grains

V. G.

Desc iption

Table Split RO1c0k

Chips TFV' Pe eed

Table Conc


Classification

Wi-C-1 - EA -

-07 -C)( 6-1- [o 6-.-1 47-61 h43.7 -Pe_io 6ovt) vIS 407c, 6'r. Tif".1-3

onier-1-ed 1:,, ,, e 77/_

-0,_ 4.6 n-1 4,z 1034: s,. ;, 145- &.3- Pelp s 7.3 crio V 1,5 -7(21,-)6ir V•LS

Wilk elcti'

ti I i

--(13 0-2_ 0.7 7.3 /3J. -8 q3.,..r? ,--,16--.0 / .3 cot,s tlovis.S 30`10 6e.T./. 1-S. W I M sli t- . '

il

-Of& ) - 3 Ô. .5-.7 -lb-7 41c). c;_20.( ) ion Cob-s s-cDvo VisS

-CS- ---5-- 0-3 5;2 33.3 16.6D /73 qf ("A--c)'0'1-iic/,:.s.

-ao 7-,P- 0.1 b.6 )331 /00.(.) fqi 91 peb,s -zovovhs 10Y061"- Tr-, L.,ç',. it

-07 71 0-3 b.E3 93-1 4q.?,g.Oi 1672 P-et--).-, -4.5-%vi.s

,575-ey„ C-1- Y: I I I '

-cP e.6 1,7 b.7 97z 59.6 (93.e /678 3.7-)0 3-- % U/3

-o(/ 6--.1 0.,z 5 2 60,8 6/ L;2_ j_af ita I, / 1 it

06 7-6 Or3.7 q81.6 -23.1- 12.7 Peic›s zsvons

(0 6/0C-_-.(c. --Trt. LS il 'I

--» 1-6 Oa 74- :iye-e 3cf.-7 2/6--- .76 60%6e. tt i 1

--i,2 7,3 05- Ls 90-e 5-5--z oc.-.)-6 1:3-0/6;ç'155160 PI/83-hg,)/.V.T.3. I f 11

-/3 .71 0 3 D.g 116.7 06).1 (,)c)..2 0.1 ce,63 5-cpy..11

,./. ii il

-If 7.7- 0...Z 7.5- /07-5- 73-6 0/. 7 ii. a C:clos --4-ove.v/-5

&O tic 63 v-1"?.L-S. it it

-1,.`; 6)3 0-/ & .8 /.5 /37./ lg..) 11.(2pei,-,, -10 ofo V13 ,30 706r.

11 I i

-1&. 7-0 o_(;) 6.1 ,ii(v.z 74o <;-0.1- ii5 ,8

cc-)1c6 6:,c7oviz

.1-6,-yo 4,--- --r./. L.S. H i l -

-17 7.1 OR. 7. Z id-LrR /DI- 3 c;26 0-) /4 0 F.. .f,_,s 50 oir,VI

-/B .71 Of 6,1 141.3 /071 /70 /67Q. Tfi,,,,;„ Eiscycvis

- 17 7.-3 ()I & -r J.6 70- 3 c,23. 7 /6.5-

Fe6s ciovevLs iC`ÎnEie.-77/, I-S.

it 11

'

-10V AURF- 1 D- IN AN ME I LIM )


Sample

Number


V. G.

Desc iption

Table I ,

Sp'"

+10 Rock Chips

-10 Table Feed

Table Conc


Classification

Vii.--C/ - S4 -

- CI-1-2 C) '7.7 (55- 7 - 2 c-31- /83.3.9.4 (_Ti./ 9gc-.19r6J-;v.e_i _s. licritlezWffr - -24 7 .S 0. 7 7•/ /7 /11./ /-,•,2 0731

.P.ebz, 9 0 ck, v'L.S T.-. L3 . ri 'I

-- 2- Z S3 6.6-- 7.S /69-3 ll26.5- ,,27.5 Peis 5% Or, --r.c.._s. ii 11

-Z3 71 0.1- -7,5 /oto ee-E .261 /3.8 j' i i ii

21 e3 (17 e-z /v./ / (2,2.4 ,2 7,c? .,20-e) - Fiect c.?,v4/3?

-25 04 C9. 7.-.S &3.0 /WI Q24.7 /1,2 ')', /g--'0 il fi II

-2-6 El .7 I• :2. 7.5- 020576 (71. 2 /6.Z 131 cot:).-.; ss-cy.w.) 4s-oicc.i,-. Tel c_,S• .

--7 2 6-3 o q' 7. 4- //7 .6 Oc;:2 • D 023.0 0.6 • Pe e,ovovAs )/ f j

.4 1.0 96e 63-4 . N? /3 .e

_t 13-V6V IS tn 50 (14 ed y vi

i e wi4-11 cl 1 f

6./ 1063 5-6.0 1.(3 /8.6- - Pea' 76-7:6\;fr-' 4.#76"vriitqra-t '-A kitr- . -03 ,c- .6/-6 5;578 4o I.E.

Cc..r,i„ 90Vc. lii-3

/0 c/o Ûf".

cir7.5Cyied i:::t/

-04 6.S o. Z .5-- /0- 6s--I (-4e,-. /.0 c6:4_-_,ss .36-kills- 6 6- '')/c

-os 4.e) 05- -4/-. 3 90 3 7 5" 11...3 -15- c/o CIK . I I I t

-o6 e_3 04 -7 .? 1673-.7 17o.c? /._31' /01 6,4--.5 6,6-.0kv/z f i I l

- CR -01 J3 D./ L.Q.02 5Y-0 4(7-5- 7-0 0-5- Peb,> -10`)/0(11,7.) OS' % 61K: 5% LS . 'I 1/

- 01 90 /.5- 7.5- /e6.4 1,36 y c>.1673 /8-D2 Peb3 g"--)'-̀;0% C/ . ca6Ped gill I- • /I

-03 6-3 /-02 77. 6 /6?)Z 40 0/..2 - I ii

-10-Of 7-7 0-2 7S .9 /5% / -

11

o -z 6.7 07 7,6 /53.6) /03- ,2D. -7-5 7 o? - (05--yow,3 ii II

OV 3UF J D _I N ANE- 1ME LIM D


Sample

Number


Desc iption

Classification

Table Split

+10

Chips

-10Rock Table

Feed Table Conc

M.I. Lights Non-mag Mag VG. +10 Matrix

Wi.-(i - PA' —

-10- CC S,S- 0.7 --7-‘ 40--.20.0 /4.9' PeLz 675-'4 w.s _WV", eir

tin sori- ed r•-a-q ble wilh :iii 7L-. 772-

--of .--_5 0:7 1- ),;a •35:3 /IQ / 0 -7 orq. 3 10 C .-70'.. Cok„,s 9,s5-0,)6vis

— 05— 0- 0-7 7 Ci .)70-277•/ —251 J77 (-7,d6s ,---x)ok,as

1 0% 671 onsorked ral , gre4,1 tu 'eh ,s / t

n_ 4(-) f> . Rout_pic

-o6 , 6, _,2 6.5- 5;7- ez3.E 575-.3 8 0 3- li 6r/sof 1-ed qral ,, be Ka* 771 1fr —

,

VISIBLE GOLD FROM SHAKING TABLE AND PANNING.

S, AMPLE LUMBER

SIZE OF A

GOLD IR

BY SHAPE D Remaxk

r SAMPLE

E NUMBER SIZE

A OF GOLD

IR BY SHAPE

D Remark:

„ W I-b . E4- sox-25o /56A 300

2cArat .nz cc.Joal.1-1..k.) 41 % su i Tides .

.

1

. -04. 0 6

R.T..

tooxioo 200x2i704. / 0 0

4 1 76 ça 1,erctez

•

ao.

MI.

*ma

)

..

•

•

El 7-1 [Ti r---mr----sur---14 E LIN AAN :ME Lin D F-1 F-1 F-1 1-1


Sample

Number


V. G.

Desc iption


R4Pic7< Chips

T;t:Pe Feed

Table Conc

M. I. Lights Non-mag Mag +10 Matrix

e4 -C6 i.e, c2-( 6.1 Q,Doo ,s .._, /b4.2 V/s

.23.4 /6 .9 -x- - -c-.°6 :342---,°//c.,,,. ur:AsIcr iciri -01 611 0.6 -1., /31.7 /c070 /57 7 h.. 8 'x i/To (Tc3PyoScr).ti°svl:s alit-,Teigedde,4"/ ii

-05 5.02 0.6 4.b 7, ---- 56.8 42.0 3.4 Cobs q 1 eh> vi s

CD:3 GA, 6r. Linsoried grk‘e-n .Lurfli 9rcuf Claq I f

1,32 - 01 7 . --4 0 .3 71 . - 0.3 /06.0 7. / c"1. Peio -30%viS

-706/06.1r. t -k* belo/10, bteJ wit ci f /I

1-7 '.-1-.1 1 .')(1._/6o.'7 /8./ //. 0 p.,/,,z 70 % tAS

30706e. unsoeted 12 q ;e

col fit silt. ' if

-03 q.o / ./ 77 /71.5- /48 ,5 /4./ 0-9' II It II

-Olt 6-6 0.5- g-I (X5',5' 177. 2_ /0.0 /0.3 4

PeickS .46% vi.S a56/0&or

il

-.96 e.,5 e9.2 . b,t) -).:25. 81.3 0)0 3 /08) ----- II it i)

--0 e)-i3 /./ 7.1 17:-53 /30.3 L,)3.z /14 Rk33 e3-4,,its

16-/o 6.1f It I,

- 077 & .0 a Z 5.8 ,)3,;2.6.,2/3.5 /4.6 4,5- >1. ;It Pe" ccD):31:kvc. uor":41V17-"4/ il

-06 7-a_ /0 6.-n- /74.7 /3.1 ,-9 7 /c2- F 'bs Sg://01-11, litv/VV9Yr-7 ZI I, *

13 -01 0.) • 7 02 06- 77.71- 7/:-/- 4.4 16 pet,,, 60% 6,-.

.250/0V1.5_4 15% (--.5 conoe teci tge with. qini beige_ clay

I i

- -02 66 i./ 7.,..5-"" /EL/ /17.9 .23.f /4-8 coe-ks e6eveuks

/6-0/0#--. un orfec I q...44 I 6:19,e IQ ittSlit

i l

-03 e.6 O. 7.? 0616- - ,,,2F.5. al-0 /6.67 __ zock co6s '70 'V 6 tlf,S

6if. /I ' h

-of e. 2 0-3 -7.7 c_)1_--5.0/700 -29.9 43-? - c---bk- E3e)c%0C.Ivi vs ri

-c6- -. o- glo N7-2 /561 2I e-7- ------ Tzi°3 gigc»2-. I, 1,

-06, 7 7 e 9 .a_ 7-7- ,66---./ 2f?.1 39.1 (:2.7 If it If

-07 743 0 -6. 7,3 - -//e- 167.2 112-5- '71 A;Irg-0 c'Db .370°:;:tcZ. c'gr-lelewdrb II

-OS 6-& (2, (49-4- 116- 134.6 341 10.a, 120 ii n il

OV UR DI _IN( AN, MEI -IM )


Sample

Number


V. G.

Desc ipt ion


+10 Rock Chips

-10 Table Feed

Table Conc

Ml. Lights No n-mag Mag + 10 Matrix

WU:7.8+1307 e'5- 05 , t) 6165- 694 ,, 3. ,_ 6-3 - " -132)'/..°V '1:e1"11e-',eii)e 1 trelfay ---rzi _ e__

- /0 e- 1. c,z 3f 161.i )43.4 /46- 3,2- Pl6s- sgt;,2r, cofge6,7- Zel'Ac- I I

/4 ' 0 5 0 0-02 5:6 04. g fib- 6 ..q to - f6ectlf,54-0I.12(..`midsZeeeb,re`96-14/ Il

•-oa 4. 6- Q.3 -f. ,./1 e5s -70.6 /o-b 2. 6 il il if

_03 7-1.-4. 0.0 6 .7 00 7t a / 7. ? II. ? Ax 6-4.!2c) C_;n)k,S 3gyVoi),V 3, , . tge 510 er t ewe Vi. 7 7 4 , H

- 01- 77 6.5 7..2. 03.7 %.6- /6 - 6 e. - coi,s 6,0y,friss

40 c/D etf. ri (I

6.7 7.47 /0.3 76,6 ,..). .2. /0-5: - )1 ll II

05 71- P6.6 e0-f .74 /01 si il Il

-04 9i2 c2.&. 6,(0 /66_4 49.1 3).6- /6-8 co& /66-07.:,/c4;- ')'7&scp/tr/37/767 ii - / 5 - - 01 64fr 0-34-,-).! (06.0 46-9 /b. b 3./ - rtgef'2°;g),)102s acunsiWeg/e/ e

-02 e- 6- / 1 -f-4- /of:4 .7b. ;2_ /7.1 /c; . / R.1"/066vcD-vtai . tgeistekTfedAalstyt.

-03 75- O. g 62 , :1- . ir-23 - f 5:e y c27? /6.6 • it i, ii

- 01 6 .0 03 3-,7 d.0 54.6 3 6.1 ,P6.3 petos -40.10vis

• 600/0 C..r. I 1 1(

-05- -7- & c-2. l'it 00-2 eD. e) 3? :2_ .2/. 0 f:- .10z, 46-0/. ViS 6S-Y0C.vi

-06,, -7., .7 ,,o. / 1.7 104 3 55,2

36.c2 /c2 . y .____. Fops lgo/ofooki.;? so„nretgi be Lei e sAtob .

-0-7 3, 6, 0.6 3,0 -6(0.1 5c).1 / 4.2_ 26 - ca's cVZ- °I ri g;. .e r/Te T/L-L--- -08 55- C).,Q 6.3 bcf4 3Q.9. a26.3 6 - (Q._ Ceb5 ci6 4YoVis

6c/b6r.

-07 e-4 I- 3 ' -,f lb-7. 71-7 &Tc>2._ 0 .7 1, 'rust% lit, ..i-a4/

- 0 eb i.b -7.D 136-.‘ 93-0 al? /1-6-11(1C)) Côt7‘3 gc /1 `16 oi°V- n ii

OV IUR 1 D _IN, IAN ME LIM D


Sample Number


V.G.

Desc ipt ion

Classification Table Split 11+old

Chips T;ge Feed

Table Conc

M.I. Lights Non-mag Mag +10 Matrix

WLZ-re4 15--li 7-8 0.tD 7.c3-- .157-2- 496).- ÷t-? /47 Coto.S q in eic V/S

1CP/06K Unsoried gray 1,4illit 3//t. / 771-L-

- J a- el 1.3 T1 01;2.3 167-6 3/1 /3.1 cob,5 95-6/ovis 60/061/.

ii If -

-13 61 .2 .1 3..5 131.'''...L_ /00?.5- ,Z.1- 6.3 I) uPso(4-cci cirec-ci green whiA 4i1t.

ii

.-11- 3.6 1.5- . .. /KO 137.7 6.a 17 Colos cis evals

)

'

16-01 6./ D-1 5:7 /03.7 90.6 10.0 al - J) 50/0 vLS 15%61 60 Vo GS

onscrted beige Wit,/ C / i

1--.11._z_.

-02 6./ 0.6 5,6- 01 90.,2 2.7 6.0 colos 498e/oVIS 0 Vo&/".

unsorted ber9e h

-o3 65" .2.1C, 6.6 /5/,'17 //6.6 ,..1.? /0./ ii ii Li

-01- ch >7.- &,c1 /60.3 qto 5-02.,2 /7/ egig&c,r'..677-7.n. ii /1

-05- ,3.a 10-5- , (::). --7 5-g-0 41.zi /1.02_ 54 cokas q 9 VoVIS / v . or'. 7?. 6S.

unsortecigree.01 cv/M sut.

7iL6._ ar,d ,S-c:ii ,o(2it

17 -a 67 O.5-- 4. -b . -5-.Ç3 47.0 6-9 /9 r/soci.,7zyjls hq./ ra.....c._

64 0 .3 1 63L 7.2-7 e.6--- c;,-1 F__1:: fovow,s 7 ocio (---7/•• ooyoe.,IT

a It ii

-03 e.3 .../ 57 l(th5 Ic>57 5- /0-3 0.2.77 '(3b°0°0 PScr oc--41,-6:;tove% ;,,,e115et"'ifii9xreit 4

-04 .3? 0_6 .3.3 '70.7- 67.5-. 13.5- 7.7 cob go V•e• v I 5-0v06-iie. Tit- Ls ..

i,i ',sorted ci ra-cl to sot sis-/-. 1 is

18_01 6.,, 0.,,,z É.-).0 _)E'). , 57.6 e-7 D2.3'f Feb,, io eioVZS

50Vo 6 r, -40701.-S bete Unsor ed i.

to m cia,./ il

-02_ 50 03 47 57.3 5/4 477- /..Z f-:371-Veras- ii ' - 1 q - - ", I :-). 3 6 . / 0- ,__ ,5-- - 6- .)„- ;), ._ 6 c:-.). L:. ) 5.L

.,, 0 i Pc47, -3c:-/t, v I rc 46,-(cati 31-)ex-Lci n Il

.-0---2 .--e /a- 466637 7j7.3 -Pgçl W- 6- (6--(4„'% q''avi-' wuZildfq."-Y T71-1-- a,k-leq

8 -CL-1DR OCK. -)E-

0/ /7. 9" 0- 3 7 7 '') /O3? -q 73 ---- . 3 F-:bb. 15% viL ,facir"71-670z_...s.

tutor tett M e a.,7114 el I

e) -17L-t-

__ 6.3 5_3 //b./ /33.6 76 3-0 - F.hs- '6%vis. oc-5.5,7ccv

)4ods . h 11

OV UF _14 C JLINI_ )IAK _IME. L11‘;


Sample

Number

Weight (kg, wet) Weight (grams dry) , Grains

V. G.

Desc iption

Table Split

ROCri< chips

Te ;a1 Fed

Table Conc

M. I. Lights Non-mag Mag +10 Matrix

Classification

141-67 - 84--C-L3 61.° C:'). ")--- 6 6 )90.0 1463 .-37- I c-26-D X- P=.6t°,-61(ia . mi)fle;refc (IS*/ Pi- L_ ar-cy 7.3 0.3 7. -) 119.1 /DTI 9- 6 -:'.1-

pe-.3 6--bkw.s 16YG6.15 Cf6c/a q6CL-

touorkd 6f, e wii-k cl n

o.a_ b.-..) h26.i / r 9-3 8h a-.5--

S-5-cic 6-if-. 4,(7/ 6Z. le it

-63 4 ,--Z O--- 4j- //hi- /D7. 6.7 (>2-o,- r.c-2°0 1 • ) _ /0 LS -EWS,, una*c/t2-7 /1 /I

-61 4, / 0-42 3.6-i 100.7 91-3 (0 .,-,2 „..7. Il n #

.-65 6.6- 0.6 'T el soq.7- /633 32.5- /3.7 per0,3 qe) €V0 WS /67,,6".. r». 1.-.S .

unsorted /ray bele whth &ill.

u

01 6-4 0- , 6-..2_ 131. b /..2i .o 8 I 0-7 %tscin0

‘i-1 3 . irs4Setgirfd claef d

0 .3 J.3 /II . 7 /i99., B. 1 3.3 ",%15-0°0 P.O/c11-,r(f-ZIAIL ZI;ce'rril./rer:r4 -li

, -0.. 6.8 06- 6.3 j4:2.6 l6, s9)1 g 1 112-0D0 /

Fèkz 700/0 AS . ,,-36,t/Q &r,•••

Gala)," fed belle/ totkic zilt.

if

3-01 8.? 01 3.g ioae gs--.9 58 c2 - / isvcoiri )vc./...7:_s . grel bei?e) cleful

10 -73 Jo.).j5 16L3? 027.0 i/ f- - R43z, r-7.5--/c,vis. ,005,06e-.6-vol-s.

unseeket gre-c6 I b2le cow( cl I,

a_ os- 7.'7 (,)/„)../ /750 c7 -_--, io-I 9,0e/ow

iccio6le.

1 uns6rie4eireci_ li_ kole with sVir il

-61 70 al 6.6 ,-).316 16,2-3 ,387 .M.6 cdo3

c>74-.n1 sy 0-__ 5.7 /07,2_ 9 .7 b. 7 16 pefo3 io tiot/i • 5;5-61,6-1r. at-,-voz.,,...

unso,redbeg9e aunt •c

I,

-0,-Q .‘.3 .L? Q. 3'7- /cF. is /0/3 57 0? -3 F-40.3 /0 tic vbs • -70v06r. (weid_s.berie

04$20( fed e

to#4 iv- c ---6,3 71 C).7 7.2 c9o_o /?0-0 (9( -5- /0.3- A ,n4 fl5€70cSc;-.1,1'S litY`f)rifiechi Jf fi -.0,f ,.6') /. n -7. c fr9). g /67S ,-Q.--1)-6 rf coiak:

5-610 eV: A II

-06 ?).0 it ,=:1 &_e ,f0.7 i9 çc7.3 71. 7 *- ebbs ‘g--ociVIC-1/0/ n //

-612 ?)..6.-- / '7 6.0 ...).21.0 /6(2o 0/27-7 1.3.3 dxlfb9,0 Cabs

'6°7: a // // •

10\/' 1UR: 'JAW 'Aft _ .1ME LIM


Sample

Number


V. G.

Description

Classification - Table

Split

Rfolok Chips

T ;t;t4 Feed

Table Conc


WI 6 . 84 - 24 -07 .7 7 0-5 7-2 -,-fq.5 6. 7 /4,3 9.5- - -(2)6 ,_.1 .-7. /...2 7.!.)- ,6-7.z cz)1.- 6 0,6:3

II .1./

-(311 1: 3 6 -i_ 1-.1. 10676' 9b,6"- 6•1 ,-..). 6R?bs /0fA vi.s 70ydir. -r.)°/0 4.5'

unsorted be/ ' e whtil rey a ‘ #

O.() 710 .930.8 195F3 163 /3.7 - Patgt 6/9r,l'it.3, °I.Nsc;g7c2//1 11

-03 0-1 D.S 7. ov6.7 /70.0 ,-)570 /3.7 Sfs-k12 6-16r. i I II - - -04 e,. b O. 0.0 p2/43 / 7 . 2 .* ,,L 1 /SS - AKVZ) P-0 1 69."1,9:1.. n II

-66- a 3 6.1 7. q .?-1.:.2.4i-,-500.1 ,b)7-I /4y . Pes .6-ook V.

6-0700r. .

-06 e - :2- 0-(7) 72 -9,;? 7 .1 1g9.6 -zs:,5-- 42.3 A/o.F° g:Va retik*,

Z61-51tr;,d illfi.

iii

-D3 eJd- e)-6 • 7 k II

---C1 7.S C)_.2 3-.10 ,X6.5 176_,),G7,,2./ /0-.Z ' coLks q.D.,„vis.ç 1..m.snefed,Q7rie.? . a

-Of 6,5- 0.6- tO 174.6- 114,3 00./ /0/ -ioci,G,-. -a2 5.6 0.1 602.. 'a e 13.16- /7 0 /0.3 - ii

-03 .7.5- 0.6- 70 HI . -7 /03.0 ‘,-5-.3 431_ ----- -f - - iS):1100\41;s/.. 0 11

03 5-, -, 2 c 4 .3 /0i., /b() 7/-R5..roz., 3 5 Vo V6

b 5 - try Eve i I 11

-01 -677 0-3 5-.1 /6c/.1- . 966 g/ 3.7 - 1-x;icsy".).:wx/2.,,s, ,..,ezvedefwye if

--e12 6---: O3 41 /36.6" //---21 /6.5 29.6 1`452-0 ÇÀSW,g.cY',-,/vty. 'fi`fir q ate 11

s a ,.. 61 V.? 10-S 5,2 /9 Pebs io ego lil-S . SSWir'. -26%1LS.

,11fiSetelerlielef bark ea

II

0---Z_ 50 95:5- gg.7 -. 3 ,23 . Petay oockvis . 16c70C-rr- /0704-S

unsorted b ' - w i IA q

Il

r- 1

1 OV-13UF7-11 D ILINI IIANI IME 1LIJ to l 1-1 r---1 fi FA 1 LABORATORY SAMPLE LOG

Sample

Number


V. G.

Desc iption


R+01°, Chips

T;bPe Feed

Table Conc


ittiLZ:r B4- 2R-Ce ‘-).3 0.5 59 /54.0 /.- it.- 7-/ et.3!.-, s5-ciovi.!.,

lif.. L.s. wtsorted aree4 b e 1 ci e to as cltui -7- /L_ i___

-01 70 0,6- (0.5- M7 no. /61 91 A)K752̀0 tno..v2 II 4

'of; 7 • ? 0.7 ‘7. a /%2.0 if-t/C) ca,." .7, /0.3

-0&) 710 O. .7.Q J0.;.a / 7/.0 /77 //_3- ig:g PS-le;S 7°E.1"11 /0 (-pf• TY- LS. 61433K/cdt. , - N/rpi 9r / e //

(0.3 0.5 5.b 1q5:7 /6531,3 j.y b3-- .1--44.0,3 fy)c/ans

y. Err • -rir. 61 n 1

ii

-OS b.5- 0, -) 5 ,?̀ Ina.? /47.7- ,.:0-/ 911 A;e0c$0 1

7g7t/oc't-? n //

- 07 7. 6--- 0.6 6.7 /S7. c/ /4-2-0 30t /373 Pe ss 9 ot/E.W3 . 'I t'

-/0 e 4 j. _.-5- e:), 9 ,e4. q 135-...:2 30.0 /v. 7 A}ÇI/G.:5pc) Co6,5 r,_57c. V IS onsoeied 5 Y C-rt"" ,

9raxgele Lobtit 712.7s11//- . il

-il , 0 616 7-.2 ,)),7 6-7- ,/71- é, ilg /73 11(TE.0jnife36 k§.) ii i,

-/a g./ /0 7.] 165.5 /30-0 30-2- 4)5:3 --*

-13 7-S 0.3 76 Z3.1 .166.3 c-'7-3 . 6 ii----5-- Pek7s eock, va

ow erK. &CC.-- r, II

-11 7-6-, 0-f 7.:2 :g. C /67-B G.?. .).1 ?../ AP;(0 Pe-6-1 1S)cclyc(16-11)(/ li /'

- 15- .7.6:7 01 7.2 /8576- /5/ 6 „..i..-2 i3 /4.17 1./.-3 40 tic U ./.S •

60 cit.) 7:711: n it

--lb 01 0.3 70 '-23-6 .3----01.1 .21.-s- 7.7 Ajic9)0 Mi31>s:li-f̀illi. 4 /1

• 0, 5' .75-- -20 5 / Z I :No /..7. R:lz.2.5-vow,3 7,5"°/,:: Cie - Tit - a •

/I Il

- / s S. 01 -7. e,„:-.)054.. /70.;2_ .23.;,_ 1.2.0 A./ jog2, 0 40 c/c., Vi ..

i-f- -/i. ts Pfitt

r; OnSOrk-detint?/e

t/Ewt yr - il ' I)

st

-i7 ..7-6,, c5./ 75 -2),f5-:f s.:-._:_)_ /7.7 55- .F_Jo_s wic tn:s_r:

0 6,3 (.1 77 ‘257,?. ,t,316-E ,.6 . 5-- 9- 5----- 1,

'-.C/ '0- 7 f -1- 73 1996 1-.3 36--,,I. /0.2.3 -

- - - - • .•e Tr- •-••• l. r- F

IOW: IURI I Dr IINC IAN): MU 1JM I (-1 LABORATORY SAMPLE LOG

Sample Number

Weight (k g, wet) Weight (grams dry) Grains

V. G.

Description Classification

Table Split -

Rfoa Chips

T ;I;Pe Feed

Table Conc

M. 1. L ights Non-mag M a g + 10 Matrix

WI_ 0 - B4

0.6 7.7 /63-6 K3C/ b - /f pebz gioik.viss to_c_e».-/ed cir-ettf

.3 ).,.] t) 7 0 /(2C.6 /35:1/. / /al PekiS 75% VI,S ,..6-./061,-. Tr LS, GeL

onst;rledqK 1?-91 e with 74;1,7 et

ii

--oil. 6.4 0-7 --7.7- .)(901 1m./ Jb.4- /1.b A n 0 o ,Zik;.: 4 &''.' Or: 't./- cl .v. Si , S6 a . - "wilSiZirif /1

, -os- 7.,) 03- b,.7.7. 193.e 16-4,0 „)6-,. /16

pei,:).5 -70,A viss ofisc.r-feel qdet./ beige IA» flit- el

ii

. -06 S.3 I. i 7,c,- 166.3 11.3. 02 4,.-.).0 ///

30%,6r.) Tr. 1-Z-,6Œ-- l R4--,.s- SoeYe.VI ,c, c1,,Eist. 17. 4.....S

1 it ii

. 0J go of 7.b /-13.6.,14).0._ c.--)J-f3 +6 -F6-Jos 6-kos,gs-% Cle 4670 L-Sr6CL. 1

q

- e.A o..5 7.7 179..2.1y,,2.o clso /..).0z cc,8.3 6-ocicvn h

-03 F.4 0-E) 7-6 -/''?t 167.4 -37 - ? //') c",s,k,3 --707,V I S -30YcGt5 77/: L-S,Gcz.,

orksor-i.eel 6p,Kr-cg, bey le._ i-0 fflt Weil ii

- 611 1. 06 43 153-z 1,33,5 X.5D 4.1- pel,s i5L) Will•S 11

-o6 al 0(0 7. Q77.47-0 ,-,'-ci.:2_ /0-6 - pefo -TS-VD v IS 05% Cie% ti

4 -a) -1- b 06 71 /3?.2. /38-6 c;26-1- /.'f..2__ --k's V--ci.:va ii if -

-67 6.3 0-5- .7.S ..?c)3.g (D7i_ /0D.6, Rek,,I 6.6 , /EV IS,

400/06/'. ti/160,- fed eri- ,a-g , be 1, to rtA col /I

-6") ci )-5---- __cf c;24,>?.0 (1.2.. _ (91.3 6.3- - pcio, 70 c/o w,s

'---.0- 61 L.L ci._ L.1- )120 g6.7 . 3 /5

-10V0C-tei -OVI) l-.S. to itA 6e/e 1c/kt it

-Oa $.{) 0-3 77.- /6Z-71 /VS 4.3 J3 Fè_10.s iovoW.S ecciuci.,, /ock L-..S . It

, 'I

-03 e- I ab 7,6 ,-.2t'?-..3 L-23,7. 6 03,0 /3.7 Pek.).s ovi 1-0v,6,-0/. 77'. .-

urisortedqratt . be i 9.e, tu tiii ekil /I

'-o :Jo a i 6 / .,_ c,13.6- 15.- erti),3 66-,./ews :5- c/c6re: ts, a t t

-1- 4!)-S- ..57`7 /97.8 170?-9 /4-.1 6:7 - Co .lc 5-5- ckw,s 46°A; 6r r:

I t II

-a) e•S Ob. (.-.(,- .20t.e /57.3 33.7 /576 ect,.s' 60e5AVI.S

cs..:20 7o 6v. ' I

7-1

3UF J C LIN 14A1" tME LIN


Sample

Number


V. G.

Desc ipt ion

Classif icat ion

Table Spl i t Spl "

RV° Chips

11Pe TFeed;I: Table

Conc M.I.

Lights Non -mag Mag + 10 Matrix

VVL-0 • E/-1 - •

- 3c-C1 77- 0 73. It)-7.ci 1-2 -s-- '- 7̀ 6 /16 pet _,,,., yoully

/0c/bCi4/

unzov-I-ed v/aq btoe to/fir agy

-CB 0,/ al .7 7 )o-i.? /661 (2-'2.61 13.1 pe6s P.,ovovis

Ls-Jot/06v. II I,

-6V 0-6 0.3, 7.7- -)45:7 -09./ -PI ? ii 7 PeL 80 'AVM

-IL) -& L')- 7.S c).31-. /•C /61 ii ,

II /1

08 7.5 ,c)e-7.3,:;-•11.-7 ::_t)..3 /53cob,,, so (joi,S ,c),/,,-,63,, -tr. ts. // 11

- Q 01 0:7 7.7 c9a8.6) L.6-:e ,J es- /13 'RA il-t-i) 'I N 1(

b 0_ 7-7 c9a).7 )0.9 06--).-, lé,- , z- 3c/o . /1

k

,

OV_ D...__IN_ IAN. ._ME... LIM.._D r-1 LABORATORY SAMPLE LOG

F-1 1-1 F-1 f- 1

Sample

Number


V. G.

Desc iption

Classification Table

Split

+10 Rock Chips

-10 Table Feed

Table Conc


\/L(3-

(Dl - 09 1.1- 0.9 (:) - g̀ t66.1- 1217+ 22., r s-. 3 - ?ass -To -Y. "h so.y. 64-. _

(.».1SriZlia- b Iftli25-No tz sicr. Li_ -T-1

- 10 i'? 0t 5.k 210 3 113.2_ 2.,( 13.0 - '13rtas , --fo-i.sq 'awl. Sc. 60-

upQS012..-rep (.g.e Y CZ ••

, 0.3 1- 1- R.C.1- 132.2- '20.3 13.s- _ C.Aas •ts,./. -is

IS"'t- Sr. ,

-Fl. S .ç 0:1 -9- .5t 1ST- I I I -2- •S- 19.1- r2.9 _ C...ot3S ciT°4. "qs 'V% 6( .

. .,

02 - 0-7 -3-.53' O.1. 7.41- Is-b. I 1 ( 3.1- 2-1.6 1 D . t %o'/. GK. _ ,

-cA .t 0.9 -4 .-2.- 153b.3 16_6 23...5 1-4.1- - *Pa ils 6c:s .4 -is dvs:1".. 0 r.

umseke.T-b %E.-14.G' m c.,,cuy CLAY. s

-09 S .4 1.1 -4.3 73V71- ( -4s--.c) 3Ç-..9- 2I-3 *s

-1 1.4% s'is lo % Gr .

toNISoRvit el --4.81GE

- I 0 9.1- I .1 %.3 23`1-.% i 96 .1. 2_1:3 i, .1 _ .,

4..»450 fa Tlel) tag.E'Y M 43ii--r-.

„

- I 1 3.'3 CI% S -0 2.c7 10.1 51.5 -.2._ _ locv. Sr. toils c:,°/..

3 - It 'i .2.

1-

0 .ia -4.6 20(0.2. I 8S.4- 9.o % -7 - Peas .-+c>.,. -is c.

utasoz-reb (R.w, - „

-12_ •,( 0.5 -3.6 I 1.3 1.4-1. 1 13-s- ‘..-+ - Peas ‘.gs 04. -is Sr.

tiNsoe rub lob. Emkeir - 2,.&ti.ae c..i..ix‘,e.

- rt 7' .3 sC3_ --4.s- 21'1• 1 I-3-7:2_ 21-1- 12--s. _ VellS. bs '9. -is rs,r. -r4 . Ls .

UNIS.c>V_Tuz iS e›.12i."1, -

*

- I 1" 51 .0 0.2_ -4.7 22_2. 6 I -IL .s" 32.7f V3.41- trisoxmo klx.16oRrab. (.2t5q - •,.

0:2- 'W.1 24'5.9 2to .1- 2_1:4 k S-S- _ 6o.V. Gr. -n . Lc .

'?a,S " .

041- • 1.1 -•3 o9 --4 .-1- 19-1-.1- I S-9-- I 2:3_5 1‘. 9 .... ?Eas So,yis

2.041.. GI . " • ,

- t41.. ,

---+ .9 0.41- 3 .5" KA- c, 123.E3 -2..T. 14+12, ir2c.4?),Zoo

I ,S. .-2_ C.)."a 74.1- V-F6.9 11.1-.3 19.0 13•6 _

- lb %.(, 0.<, 5-t-0 1-43.2. 132_1 23.9 1-7. -a_ - .. .. ..

OS - 17_ -7 .5/ 1.0 653 I to-2_ .3 1 2- 9.9 2_1. 6 to.7 triso.%- Coas c3o 04. -is vn\s.oP.. -t-eb sae- 4

--

fi ov- 3UP Till DC-11N _ 1AN ME .. LIM _D


Sample Number


VG.

Description Classification

Table Split

+10 Rock Chips

-10 Table Feed

Table Conc

M.I. Lights Non-may May +10 Matrix

kn./ L 6 - 41- -

oc - fl 9.1 1. 1 8.0 zoi. i I s-s-. s" '3 i .(.., 14.0 _ coess 90,./.% ka.`(.. 6r .

uk,sze-rwt. 12,xiaA?

CZ C.A.p.Y. -r-, LL

-Li- s.?- 1-1- -3- -3 113- 5 140.1 2_1.2.- 12.1- _

1941-.0 22.0 1271- -

- OC 3c) 4 .. 5 0.51 7-f" --1- I (02- 4- 13( .9 19 . o t 1 .S' vls..1.c '?Ees 60u4 6t • T. LS. „ ..

- -. 1 -4.o 0-s" G .5' 1 t's.S" 9+.I G.3 It cA)v"-° i -2_ . i., 1::ea-,.).4-T-',. Ls. ,.

- '--2- .41.• O. G c-. t I is.. ç t os-. I 1 1 I 6 - peas 60Y. 'is

- ..3 1,9 1_1 -4 . 1 % % S-. '3 1 S. ' 3 1 C. 4 10 • G ,, loolcz-c° ,%., €71s 6.r. •-ri . Ls ,

0-i .23 g .1- 63 SI. t 1-1-1-.9 is() .0 R. .1 51.53 _ Gkikts.)• SoV. -/& .̀-CYLI, 6.r. 6c..L.

Lp4SoeTab DCAVe - g eit.tr a 6.tuy Luay. „

-29 S'. I o. 1 'R• .0 (3 141-1 .6 IL:3 -4 .4 1,2.0.1.0 v"s 1€°b/- It vso 'K. Gr. thLt_.

-30 ça..1- 0.1 1.3 21'4.-1 1 4-$. t, --ei/ .1- 29.f _ 1, .. •,,

- 3 1 G.T 0 .S" S-.0 13-4••rs 11_1.1 1(3.3 (-1- _ 'Pe-zs 6e.4% 10% U.

-rr.1:S. . GO-. , ..

0% - 01 -1- 7+ 4-0.1 13 223 .5 1 90.-1 -2.5-.-2_ -1.6 .ic:),,i.. ,is SOR..rbD SR?_

c) .% .0 I. L 61- -2-0(.6 Isli .3 - e 31.9 mg.. N< -c-Et•S 51c) ". qs

-Ti.Ls. us•Iso R. rti b (74Rw :4- S1t---T. "77 LA_

-c59 .tL 1 . 0 S..1 16-1... 41- 11-1.4 2_%:41- 10.(3 _ ., „ „

09 - c)4- *a 4:, 1 .-7- (= .5 169 .1- 1 4-1 .1_ 1-4- ....s 1 c).(3 ..1,::::z- to as t. 1/14.

hr. „

. ,

-OS 9 . 0 1.53 -74.t (49-.2, 1it .o 2o.3 12..9 - 'Tess çar3,4, vs- -2_0'4 Gr. -r, , i_ . ., •.

- OG 11• .9 0. 6 V.3 1 -1L.--+ I2 .zi- -2-4 .4 20.S _ -2-`5 4r. St • GC.L...

w.lsc. el-w6 a/J.1N -

-0 9%.0 'S-2-.S. 12:2_ "3 .3 'is UmS0e-Te.11)

r - - "4 .1 O.(, (''S 139-4i- 111- 19.2_ g,s- 1,--2...,00 %um(' 'is -2_o V. 6...c. CLL.

..*.lsowtes. c.Rey-IliGZ a bitay LL.p.Y.

,.

0\ -.13LJE:i7N


Sample

Number

Weight (kg, wet)

_

Weight (grams dry) Grains

V.G.

Desc ipt ion


Rock +10

Chips

Table Feed

Table Conc

M.I. Lights Non-mag Ma g + 10 Matrix

4k1L-6 -B4

I o-0B 3, q 0 . 3.3 760-7- ei3.L 8:3- 3.8 = 60Aws

5-SOC/Or. beige: unsorte_ct gr

wilin am t- TILi-

-0c1 0-1 ab 77.5- 150.5 /020.6 /7.0 I. -,15tvkç awn;,freri

f

--/o sc7 h.1 c..6 -116.9 1/0.4 6:0 /,5- k's VlioIL.t . . it 1 i

- II 7.5- <0.1 74 cwo.8 /6574 .3.3.. 1/ 8 — Rt,s GCL_ lar-Fect oireti itAe.

/I- 0 ( 43" 0.1 4.4 61. 9 6a.a 7.3 cz)..1. ReSc, 6)0%0S 40% 6v.

tAnsov-fe crag buiffrt cia.k, —

_TILL_

.4 0).6 5:8 Pa? 78.6- ,),D_Ci /c 4peki,- eoc7jooveav. -,0,--t-earet) GicZAVO----

,

,

1

BIBLIOGRAPHY

1. Geology of the Agnico-Eagle Gold Deposit, Quebec; Barnett, ES., -Hutchinson, R.W., Adamcik, Anton Barnett, R. Precambrian Sulphide Deposits, H.S. Robinson Memorial Volume, ed. by Hutchinson, R.W., Spence, C.D., Franklin, J.M., Geological Association of Canada Special Paper 25, 1982.

2. Dighem III Survey of the Raymond Twp. Area, Quebec; Dvorak, Z., Dighem Surveys & Processing Inc., Aug. 28, 1984.

3. Report on Magnetometer, Horizontal Loop EM and IP/Resistivity Surveys, Lac Gagnon Project, Raymond Township, Quebec; J. Roth, M.A., MPH Consulting Ltd., November, 1984. (2 volumes)

4. Légende de la Compilation Géoscientifique; Symboles Lithologiques, Ministere Energie & Ressources, Secteur des Mines, Québec, 1983.

5. Today's Market Line; issue 050/85, March 12, 1985

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