diamond drilling report of the cleaver property - Geology Ontario

Inspiration Mining - Cleaver Drilling Report - May 2014 1

DIAMOND DRILLING REPORT OF THE CLEAVER PROPERTY

(CLAIM 4215486-95)

(CLAIM 4212376-78)

IN THE

CLEAVER, MCNEIL, FASKEN & FALLON TOWNSHIPS, PORCUPINE & LARDER LAKE MINING DIVISIONS,

TEMISCAMING, ONTARIO

FOR

INSPIRATION MINING CORPORATION

BY

ANDRE CIESIELSKI, P.GEO.

MAY 13, 2014


TABLE OF CONTENT Page Introduction 3 Summary of Previous Geological & Exploration Works OGS Works 4 Summary of Exploration Works by Inspiration Mining Line Cutting 4 Ground Magnetic & Max-Min Survey 4 VTEM 4 Geological Compilation 4 2008 to 2010 Drill Program 8 Drill Collar Coordinates 8 Drill Hole Logs 9 Drill Hole Strip Logs 23 References 59 Statement of Qualification 60

List of Table

Table 1, DDH Collar Information 8

List of Figures

Figure 1, Property Location 3 Figure 2, Drill Hole Locations 7


INTRODUCTION

The following report describes the drilling program carried out by Inpiration Mining Corporation on the Cleaver property in 2008 and 2010. A total of 36 diamond holes were drilled and amounted to 9677 m. The Cleaver property comprises the Ontario Mining Claim no. 4215486 to 4215495 and 4212376 to 4212378. It is located 43 km SE of Timmins Ontario astride Fallon, Fasken, Cleaver and McNeil Townships and can be reached easily from South Porcupine using Stringer Road and further following well maintained dirt roads to the south, Figure 1.

FIGURE 1 : LOCATION OF THE CLEAVER PROPERTY, 43 KM SE OF TIMMINS, ON. AND 10 KM SOUTH OF THE NIGHT HAWK LAKE.


SUMMARY OF PREVIOUS GEOLOGICAL AND EXPLORATION WORKS

OGS WORKS - Geological study of the Fallon and Fasken Townships was carried out by D.R. Pyke in 1973 and includes a description of galena occurrence and magnetic and EM works on the area (Pyke 1973, OGS GR 104). - Geological study of gold distribution in glacial till was carried out by A.F. Bajc in 1996 and straddled Fallon, Fasken, Cleaver and McNeil Townships (Bajc, 1996, OGS OFR 5941). - Geological study of McNeil and Cleaver Townships was carried out by L.S. Jensen in 2002 and includes descriptions of copper, lead, zinc, molybdenum, gold and silver occurrences. Most of mineral exploration has been focussed on surface discoveries and geophysical anomalies (Jensen 2002, OGS OFR 5931. As stated by L.S. Jensen in the report above, sulfide mineralization was discovered southwest of Little Night Hawk Lake during the 1920s. Pits and trenches were excavated and pyrrhotite, arsenopyrite, galena, sphalerite and minor amounts of gold and silver were found in calcite and quartz veins. One described iron formation with pyrite, limonite, mispickel, galena, zinc blende, copper pyrites, cobalt bloom, quartz and calcite”. In 1950, a showing was analyzed and returned 0.06 oz/t Au, 1.27% Pb and 3.44% Zn. In 1956, a company conducted geological mapping, surface sampling and diamond drilling of 11 holes. A hole in the Gowganda Formation, about 975 m east of the north end of Little Night Hawk Lake returned 16.1% Pb, 8.7% Zn and 2.15 oz/t Ag across a surface width of 0.5 m. Nine intersections averaging 0.56 m, returned 2.73% Pb, 8.7% Zn and 0.395 oz/t Ag. The mineralization occurs in a west-striking calcite vein that intrudes felsic metavolcanic rocks. In 1970, southwest of Little Night Hawk Lake one conducted magnetic and electromagnetic surveys revealing conductive zones, but no further work was reported. In 1975-1976, one conducted a ground geophysical magnetic survey and a horizontal loop electromagnetic survey over 2 mining claims, southwest of Little Night Hawk Lake. Only one conductive zone was detected. In 1977, another group did further work on the 2 claims consisting of a ground magnetic survey and a vertical loop electromagnetic survey that detected an additional conductive zone. Trenching and pits were sunk on the conductive zones and exposed 3 separate zones of up to 20% pyrrhotite and pyrite in grey, siliceous, bedded, tuffaceous and graphitic metasedimentary rocks. In 1980, a company held a large group of claims that encompassed most of the area in Cleaver and Hincks townships that are underlain by Proterozoic sedimentary rocks. Exploration was focussed on potential placer gold mineralization at the basal contact between Proterozoic sedimentary rocks and the underlying Archean metavolcanic rocks. The company completed several ground geophysical magnetic surveys and a seismic refraction survey along the Fallon-Cleaver township boundary to determine the thickness of the Proterozoic cover. In 1981, 3 vertical diamond-drill holes were completed in Cleaver Township. The basal section of the Proterozoic rocks was not intersected in any of the 3 holes and no significant gold values. In 1982, one completed ground geophysical magnetic and vertical loop electromagnetic surveys over a 6 claim area that included an area previously explored. After detecting 4 conductive zones no further work was reported. In 1984, a group held 25 contiguous claims in northeast Cleaver Township. Bedrock exposures consist of altered mafic metavolcanic rocks intruded by syenite dikes and quartz-carbonate veins hosting pyrite with gold values up to 0.35 oz/t Au. The claims were optioned and one conducted ground geophysical surveys and diamond-drilled 2 holes totaling 81.4 m. The only mineralization was a narrow, pyritic, quartz-epidote alteration zone in mafic metavolcanic rocks that assayed 0.23 oz/t Au accross 0.3 m. In 1986, Asarco Exploration optioned the claims and the adjacent claims of D. Meunier. Between 1986 and 1988, the company conducted geological mapping and sampling as well as 600 m


of backhoe trenching and completed 11 overburden-drill holes to bedrock. This work was done in conjunction with additional overburden drilling on the Meunier property to the northeast. Trenching revealed several metre-wide granitic dikes intruding mafic metavolcanic rocks. Assays up to 0.02 ounce gold per ton were obtained from alteration zones in the granitic dikes. Two samples collected by the author returned no gold values and a third sample analyzed 0.2% Cu.

The Meunier property consists of 57 claims in northeast Cleaver Township and 28 claims in Fallon Township. The property was staked after a sample, collected from a large quartz-albite boulder, assayed 0.038 ounce gold per ton. In 1987, Asarco Exploration completed 21 overburden-drill holes totaling 465 m, 10 of which were on the Meunier property. This program was followed by another 13 holes totaling 472 m. In total, 23 holes intersected anomalous gold mineralization. Another 11 overburden holes were drilled in 1988. In 1989, 3 diamond-drill holes totaling 775 m were completed near the north boundary of Cleaver Township. The diamond-drill holes intersected altered mafic metavolcanic rocks intruded by syenite and feldspar porphyry dikes.

The Laramée property consisted of 6 claims located at the 4-mile post along the boundary between Fallon and Cleaver townships. The property was previously investigated and an electromagnetic conductor was drilled. In 1990, two 182 m holes were drilled. Hole G90-1 intersected sulphide-bearing, graphitic argillite interlayered with felsic metavolcanic rocks and intruded by feldspar porphyry and gabbro dikes. A 1.4 m wide zone containing 50% massive and globular pyrite was intersected as well as several zones of disseminated pyrite, pyrrhotite and chalcopyrite. Minor fuchsite was also reported in the drill logs. Hole G90-2 intersected pyrite- and pyrrhotite-bearing felsic metavolcanic rocks intruded by feldspar porphyry and gabbro dikes.

The Flinsky Claim property consisted in 37 claim units and is located in southern Cleaver twsp, south of the Little Nighthawk Lake. Stripping and trenching was carried out in 1995 and 1996 . Only one sample returned 2% Zn with minor copper and lead.


SUMMARY OF EXPLORATION WORKS BY INSPIRATION MINING LINE CUTTING In winter and spring 2008 a line-cutting program was undertaken on the Cleaver property by M.C. Exploration of Timmins, Ontario. North-trending lines are spaced every 100 m with east-trending tie lines every 800 m.

GROUND MAGNETIC & MAX-MIN SURVEY Following the line-cutting, a ground magnetic and EM max-min survey were carried out by M.C. Exploration and a report was produced by Johnston (2009).

VTEM A VTEM airborne survey was carried out in July 2008 on the Cleaver property and various maps including TMI, Time Constant Tau, vertical VD1 and VD2 and TMI horizontal derivative, etc. were produced in November 2008 by Geotech (2008).

GEOLOGICAL COMPILATION A geological compilation was carried out on the Cleaver property based on Pyke and Jensen geological mapping and given the lack of outcrops, the top lithologies in the various drill holes was used to complete the mapping, Figure 2. The property is underlain by pillow basalts in contact with felsic volcanics to the north crosscut by north-trending wrench faults. deformation trends to the southeast and south and show kilometer scale folding. In the southeast corner, the volcanic sequences are affected by NNW-trending probable shear or large folding that rotated the trends to the SE. Southwest of the property, the volcanic sequences show ultramafic rocks that may be extended at depth and to the east, Figure 2. It follows a major magnetic vertical gradiant anomaly on the airborne survey.

The Asarco RC and DDH drill data was used to carry out a topographic map of the basement under the glacial overburden that was integrated in the compilation, see above. It shows an interpreted fault intersection where depths down to 54 m in the overburden are recorded. High gold values have been recorded by Asarco drilling at the contact between basement and glacial till and clays. Gold values reaching 408 ppm, 126, 100, 27 and 20 ppm have been found in the deepest part of the Asarco trough. In order to properly locate the source of such high gold values, Inspiration commissioned a study on recent glacial deposit history in the area that was produced by Veillette (2010). In 2010, various holes attempted but failed to intersect such high grade gold sources, Figure 2.


FIGURE 2 : GEOLOGY OF THE CLEAVER PROPERTY SHOWING BASALTS (GREEN) TO THE SOUTH, FELSIC VOLCANICS (PALE BLUE-GREEN) AND ULTRAMAFICS (DARK GREEN). TO THE NORTH, AFTER PYKE (1972) AND JENSEN (2002). IN THE CENTER, CONTOURED DEPTH OF THE BASEMENT IS GIVEN IN METERS. IT ALSO SHOWS MAJOR EM CONDUCTORS

(STIPPLED LINES), FOLIATION (SOLID RED LINES), DYKES (ORANGE LINES) AND FAULTS (BLUE LINES). INSPIRATION MINING 2008 AND 2010 DRILL HOLES ARE SHOWN AS RED SYMBOLS.


2008 TO 2010 DRILL PROGRAM

A total of 35 NQ holes were completed on the Cleaver property adding to 9678 m. 22 holes were completed in 2008 in the western part of the property, Figure 2 and were located using mainly airborne conductors and anomalies and ground EM max-min conductors. In 2010, 13 holes were completed in the central and eastern part of the property and located mainly using EM max-min conductors. 6 holes attempted to reach a source of the alluvial gold concentrated in the topographic lows in the south central part of the property as documented by Asarco in 1987, Figure 2. All drilling was contracted to T-Drilling Inc of Timmins, Ontario. Cores are stored in the field on the Inspiration Mining Langmuir 1 mine site, west of Night Hawk Lake Carman Bay, Figure 1. Core samples were analyzed by Swastika Laboratory in Swastika, Ontario, maily for gold. Parts of the samples were also analyzed fo Ag, Co, Cu, Ni, Pb, and Zn. As shown on the various strip logs, no significant gold or silver mineralization was intersected.

Complete descriptions of the drill cores and spreadsheet of the Swastika Lab analysis are available on the CD attached to this report.

Drill collar coordinates

The following Table I, summarizes the collar information. All coordinates projected in UTM NAD83, zone 17N. Elevations are in meters and not precise.

TABLE I : CLEAVER DDH COLLAR INFORMATION

Hole Id Easting Northing Grid E Grid N Dip Az El EOH

C08-01 500175 5336438 1500 1200 -50 0 250 253,9

C08-02 500175 5336438 1500 1200 -60 0 250 349,7

C08-03 498874 5335588 200 350 -50 0 250 250,8

C08-04 498874 5335713 200 475 -50 0 250 250,4

C08-05 498874 5335837 200 600 -50 0 250 250,7

C08-06 498874 5335962 200 725 -50 0 250 251,3

C08-07 498774 5336789 100 1550 -50 0 300 301,9

C08-08 498774 5336789 100 1550 -60 0 300 347,4

C08-09 499174 5337390 500 2150 -50 0 300 251,3

C08-10 499174 5337390 500 2150 -50 0 300 41,5

C08-11 501975 5336038 3300 800 -50 0 300 296,3

C08-12 501975 5336188 3300 950 -50 0 300 300,0

C08-13 501975 5336338 3300 1100 -50 0 300 301,0

C08-14 501975 5335663 3300 425 -50 0 300 300,0

C08-15 501673 5335587 3000 350 -50 0 300 302,0

C08-16 502075 5335339 3400 100 -50 0 300 251,0

C08-17 500674 5337289 2000 2050 -50 0 300 293,0

C08-18 500874 5337437 2200 2200 -50 0 300 302,0

C08-19 500874 5337289 2200 2050 -50 0 300 302,0

C08-20 500774 5337289 2100 2050 -50 0 300 299,0

C08-21 500774 5337089 2100 1850 -50 0 300 299,0

C08-22 500574 5337014 1900 1775 -50 0 300 290,0

C10-24 503674 5337138 5000 1900 -55 0 298 299,3

C10-25 503974 5338138 5300 2900 -50 0 287 302,0

C10-26 504174 5338088 5500 2850 -50 0 290 301,0

C10-27 504373 5338063 5700 2825 -50 0 304 302,0

C10-28a 504573 5338013 5900 2575 -50 0 298 83,0

C10-28b 504573 5338013 5900 2575 -60 0 298 77,0


C10-29 504774 5338088 6100 2850 -55 230 306 338,0

C10-30 504573 5338139 5900 2900 -55 180 302 300,0

C10-31 503674 5337738 4900 2450 -55 200 291 236,0

C10-32 503375 5337037 4700 1800 -55 200 297 302,0

C10-33 503172 5336537 4500 1350 -55 220 281 350,0

C10-34 503272 5336436 4600 1200 -55 220 298 350,0

C10-35 503072 5336663 4400 1425 -55 220 300 353,0

Drill logs

The following logs and strip logs summarize the various geological units encountered in the holes as well as the gold content. See Table 1 and Figure 2 for locations of holes. Complete log data and assays are located on a CD attached to this report

Hole C08-01 Drilled : 2008 Logged : 11/28 - 12/3 2009

HoleID From To Length General Geology ID

C08-01 0,0 33,3 33,3 OVERBURDEN OB

C08-01 33,3 159,4 126,1 PILLOWED Basalt PBa

C08-01 159,4 168,9 9,5 PORPHYRIC INTRUSIVE/DYKE Por

C08-01 168,9 176,4 7,5 MAFIC INTRUSIVE/DYKE MaD



C08-01 186,6 188,6 2,0 GRAPHITE SILTSTONE GrS


Hole C08-02 Drilled : 2008


C08-2 0,0 27,5 27,5 OVERBURDEN OB

C08-2 27,5 178,9 151,4 FELSIC VOLCANICS FeV

C08-2 178,9 191,9 13,0 MASSIVE Basalt MBa


C08-2 206,5 210,3 3,8 FELSIC INTRUSIVE/DYKE FeD



C08-2 214,2 216,7 2,5 ULTRAMAFIC INTRUSIVE/DYKE UlD


C08-2 217,1 222,0 4,9 FELSIC TUFF FeT







C08-3 0,0 7,2 7,2 OVERBURDEN OB


C08-3 11,2 12,2 1,0 CARBONATE C

C08-3 12,2 17,7 5,5 INTERMEDIATE INTRUSIVE/DYKE InD

C08-3 17,7 19,5 1,9 CARBONATE C











C08-3 99,0 102,3 3,3 TALCOSE KOMATIITIC VOLCANICS TKBa


C08-3 129,1 138,1 8,9 BASALTIC KOMATIITIC VOLCANICS BaK



























C08-4 150,0 154,0 4,1 TALCOSE KOMATIITIC Basalt TKBa











C08-4 177,5 179,5 2,1 ALTERED Basalt ABa




















C08-5 3,6 19,2 15,7 BASALTIC KOMATIITIC VOLCANIC BaK


C08-5 29,8 35,1 5,3 TALCOSE KOMATIITIC VOLCANICS TaK




















C08-6 3,2 12,2 9,0 MAFIC TUFF MaT


C08-6 16,8 21,7 4,8 MAFIC TUFF MaT








C08-6 76,1 83,5 7,4 MAFIC TUFF MaT


C08-6 89,5 167,2 77,8 MAFIC TUFF MaT




C08-7 0,0 20,1 20,1 OVERBURDEN OB




C08-7 150,0 158,1 8,0 DYKE SWARM DS


C08-7 214,1 255,6 41,5 PILLOWED Basalt PMV





C08-8 0,0 18,3 18,3 OVERBURDEN OB







C08-8 249,9 269,6 19,6 MAFIC TUFF MaT




C08-8 314,3 326,5 12,2 SILICIFIED CONGLOMERATE SiCg




C08-9 0,0 24,3 24,3 OVERBURDEN OB



C08-9 64,9 78,4 13,5 MAFIC TUFF MaT





C08-10 0,0 21,4 21,4 OVERBURDEN OB


Hole C08-11 Drilled : 9/27 - 10/23 2008 Logged : 12/4 - 8 2009


C08-11 0,0 25,7 25,7 OVERBURDEN OB

C08-11 25,7 71,0 45,4 PILLOWED KOMATIITIC Basalt PiKBa






Hole C08-12 Drilled : 10/24 - 11/3 2008 Logged : 12/8 - 18 2009


C08-12 0,0 13,6 13,6 OVERBURDEN OB






Hole C08-13 Drilled : 2008 Logged : 3/15 - 18 2010


C08-13 0,0 18,0 18,0 Overburden OB

C08-13 18,0 78,1 60,1 Talcose Komatiite TaK

C08-13 78,1 82,4 4,3 Massive basalt MBa


C08-13 84,3 95,0 10,7 Mafic Dyke MaD

C08-13 95,0 139,7 44,7 Intermediate Dyke InD


C08-13 140,6 144,0 3,4 Mafic Dyke MaD


C08-13 144,3 145,7 1,4 Mafic Dyke MaD


C08-13 146,8 149,9 3,1 Mafic Dyke MaD








C08-13 168,3 237,5 69,2 Basalt Komatiite BaK

C08-13 226,2 240,2 14,0 Intermediate Dyke InD


C08-13 247,0 259,0 12,0 Diabase dyke DiD









C08-14 0,0 25,0 25,0 Overburden OB

C08-14 25,0 39,5 14,5 Andesite And

C08-14 39,5 60,2 20,7 Pillowed Andesite PAn


C08-14 62,6 69,4 6,8 Andesite And

C08-14 69,4 70,2 0,8 Felsic dyke FeD

C08-14 70,2 107,3 37,1 Andesite And

C08-14 107,3 114,4 7,1 Syenite SyD

C08-14 114,4 143,3 28,9 Andesite And

C08-14 143,3 145,8 2,6 Syenite SyD

C08-14 145,8 146,7 0,9 Andesite And

C08-14 146,7 147,7 1,0 Syenite SyD

C08-14 147,7 149,5 1,8 Andesite And

C08-14 149,5 172,6 23,1 Syenite SyD

C08-14 172,6 195,9 23,3 Andesite And

C08-14 195,9 197,6 1,7 Intermediate dyke InD

C08-14 197,6 210,1 12,6 Andesite And


C08-14 212,5 220,2 7,7 Andesite And


C08-14 224,3 225,4 1,1 Mafic Dyke MaD


C08-14 225,9 243,2 17,3 Andesite And

C08-14 243,2 245,3 2,1 Syenite SyD

C08-14 245,3 268,6 23,3 Andesite And

C08-14 268,6 270,3 1,7 Syenite SyD

C08-14 270,3 274,6 4,3 Andesite And

C08-14 274,6 276,5 1,9 Syenite SyD

C08-14 276,5 278,3 1,8 Andesite And

C08-14 278,3 300,0 21,7 Syenite SyD



C08-15 0,0 30,0 30,0 OVERBURDEN OB

C08-15 30,0 44,5 14,5 MASSIVE ANDESITE MAn

C08-15 44,5 93,2 48,7 PILLOWED ANDESITE PAn



C08-15 125,3 135,7 10,4 SYENITE DYKE SyD

















C08-16 0,0 6,0 6,0 Overburden OB


C08-16 17,0 26,8 9,8 Ultramafic Dyke UlD

C08-16 26,8 68,4 41,6 Andesite And


C08-16 70,4 74,5 4,1 MaficDyke MaD


C08-16 74,8 76,0 1,2 MaficDyke MaD

C08-16 76,0 79,6 3,6 Intermediate tuff InT

C08-16 79,6 125,7 46,1 Andesite And

C08-16 125,7 130,5 4,8 MaficDyke MaD


C08-16 133,5 164,9 31,4 Andesite And


C08-16 168,2 185,8 17,6 MaficDyke MaD


C08-16 192,9 195,8 3,0 MaficDyke MaD


C08-16 226,4 235,4 9,0 Andesite And



Hole C08-17 Drilled : 2008 Logged : 5/ 29 - 31 2010


C08-17 0,0 33,0 33,0 OVERBURDEN OB

C08-17 33,0 87,0 54,0 INTERMEDIATE TUFF InT


C08-17 95,0 126,0 31,0 ALTERED ANDESITE AAn










C08-18 0,0 39,0 39,0 OVERBURDEN OB







Hole C08-19 Drilled : 2008 Logged : 2/1 2010


C08-19 0,0 39,0 39,0 Overburden OB

C08-19 39,0 101,7 62,7 Andesite And

C08-19 101,7 107,0 5,3 Feldspar Porphyry FP

C08-19 107,0 136,7 29,7 Lost Descriptions

C08-19 136,7 140,7 4,0

C08-19 140,7 143,6 2,9

C08-19 143,6 298,1 154,5

C08-19 297,5 302,0 4,5




C08-20 0,0 22,0 22,0 OVERBURDEN OB




Hole C08-21 Drilled : 2008 Logged : 1/10 2010








C08-22 0,0 20,5 20,5 Overburden OB

C08-22 20,5 246,5 226,0 Andesite And

C08-22 246,5 261,7 15,2 Graphite siltstone GrS

C08-22 261,7 290,0 28,3 Andesite And

Hole C08-24 Drilled : 1/6 - 10 2010 Logged : 5/27 - 28 2010


C10-24 0,0 40,0 40,0 OVERBURDEN OB


C10-24 44,6 62,9 18,3 FELSIC METAVOLCANICS FeV












C10-25 0,0 44,6 44,6 OVERBURDEN OB










Hole C08-26 Drilled : 1/16 - 20 2010 Logged : 5/31 - 6/2 2010


C10-26 0,0 39,0 39,0 OVERBURDEN OB











C10-27 0,0 33,0 33,0 OVERBURDEN OB
















Hole C08-28a Drilled : 2/2 - 3 2010 Logged : 6/2 2010


C10-28a 0,0 61,5 61,5 OVERBURDEN OB

C10-28a 61,5 83,0 21,5 INTERMEDIATE TUFF InT

Hole C08-28b Drilled : 2/3 - 5 2010 Logged : 6/2 2010


C10-28b 0,0 54,0 54,0 OVERBURDEN OB

C10-28b 54,0 77,0 23,0 INTERMEDIATE TUFF InT



C10-29 0,0 40,3 40,3 OVERBURDEN OB





C10-29 82,7 136,2 53,5 DIABASE DYKE DiD























C10-30 0,0 49,0 49,0 OVERBURDEN OB









C10-31 0,0 11,0 11,0 OVERBURDEN OB







C10-32 0,0 46,0 46,0 OVERBURDEN OB










C10-33 0,0 40,5 40,5 OVERBURDEN OB














Hole C08-34 Drilled : 3/20 - 24 2010 Logged : 5/28 - 6/9 2010


C10-34 0,00 28,10 28,10 OVERBURDEN OB


























C10-35 0,00 23,00 23,00 OVERBURDEN OB














Drill Strip Logs


REFERENCES

Geotech, 2008 : Helicopter borne VTEM geophysical survey – Langmuir, Douglas and Cleaver Blocks, Timmins, Ontario; unpublished report for Inspiration Mining Corp. by Geotech Ltd., November 2008, 61 p.

Jensen, L.S., 2002 : Precambrian geology of the McNeil, Robertson, Hincks and Cleaver townships; Ontario Geological Survey, Open File Report 5931, 77p.

Johnston, M., 2007 : Magnetic survey and line cutting on the Douglas property, Douglas Township, Ontario; unpublished report for Inspiration Mining Ltd. by Matthew Johnston Consulting Geophysicist, Timmins, Ontario,

Pyke, D.R., 1972 : Fallon and Fasken Townships, District of Temiscaming, OGS Map 2253, 1972.

Veillette, J. J., 2010 : Overburden drill program Hawk project; unpublished study for Inspiration Mining, 18 p.


STATEMENT OF QUALIFICATION

I, André Ciesielski, P. Geo. do hereby certify that : I am a Canadian citizen, living at 1777 Du Manoir Av., Montreal, H2V 1B7, Qc, Canada. I have a bachelor degree in geology from Université de Montréal (BSc. geol) a DEA and a Doctorat from "Université Pierre et Marie Curie" (Paris VI). I practise geology since my graduation. I am a member of "L’Ordre des Géologues du Québec", OGQ licence no. 514. I was granted a Special Exemption for Incidental Practice in Ontario under APGO By-law No. 11 in May 6, 2014. This May 13, 2014 André Ciesielski, P. Geo.

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 N

C-08-01 L-1500E 1200N 250 Grid North-50 254m 22/06/2008 04/07/2008 G.Spyratos Nov 28 - Dec 3, 2009

From To Length Id Rock type Photo0,00 33,33 33,33 Overburden33,33 159,38 126,05 Pillowed Mafic Calc-Alkalic Metavolcanics

159,38 168,90 9,52 Felsic Intrusive (Feldspar Porphyry)

168,90 176,44 7,54 Mafic Intrusive

176,44 182,21 5,77 Pillowed Mafic Calc-Alkalic Metavolcanics

182,21 186,55 4,34 Mafic Intrusive

186,55 188,55 2,00 Pillowed Mafic Metavolcanics with Graphitic Argillites

188,55 202,11 13,56 Pillowed Mafic Calc-Alkalic Metavolcanics (Pillow Breccia)

202,11 253,90 51,79 Pillowed Mafic Calc-Alkalic Metavolcanics

253,90 EOH

Pale brownish-green to pale grey-green and pale green to greenish-buff. Locally grey-green to dark grey. Common greyish-buff, patches. Aphanitic to fine grained. Pillowed, with common pillow selvages and interpillow breccias. Locally fragmental. Occasional qtz-calcite or chlorite filled, amygdules. Local hydrofracturing. Irregular qtz-calcite, veining. Hard. Non-magnetic. LC, at approximately 35 deg tca.Pale grey to pale greenish-grey, with pale greyish-buff and pinkish-buff patches. Fine grained matrix, with numerous feldspar phenocrysts. Weakly fractured. Rare qtz-calcite stringers. Very hard. Non-magnetic. Hole partly sampled as per Andre Ciesielski's instruction. LC, broken.

Pale grey-green to grey-green and medium green. Fine to medium grained. Massive. Weakly fractured. Rare qtz-calcite stringers. Moderately hard to hard. Non-magnetic. LC, at 65 deg tca.Unusual unit. Pale greyish-brown to pale grey-green. Fine grained, with local scattered chloritic phenocrysts. Pillowed, with occasional to rare, pillow selvages. Weakly fractured, with qtz-calcite filled fractures. Rare amygdules. Hard. Non-magnetic. LC, broken.

DDH Depth Main Unit LithologyComments

0-33(?): Casing

Grey-green to grey. Fine grained matrix, with common feldspar phenocrysts and occasional mafic phenocrysts. Hard. Non-magnetic. Contacts are questionable due to the poor core condition. LC, broken.Dark grey to black and greyish-brown, locally. Aphanitic. 45% argillite beds. Local bedding. Negligible amount of calcite filled fractures. Hard. Non-magnetic. LC, at 50 deg tca.Pale grey-green to pale green and greenish-buff, locally. Aphanitic to fine grained. Occasional to common, pillow selvages. Strong breccia, throughout. Locally fragmental. Negligible amount of veining. Hard. Non-magnetic. LC, sharp and brecciated.

Pale grey-green, with greenish-buff patches. Aphanitic to fine grained. Common mafic phenocrysts. Pillowed, with occasional pillow selvages. Rare pillow breccias. Common hydrofracturing. Rare qtz-calcite stringers. Hard. Non-magnetic.

From To Length Id Rock types, Change in grain size, colour, etc. Photo33,33 41,00 7,67 Fragmental section

35,65 36,77 1,12 Lost core39,00 39,33 0,33 Mafic Dyke

43,00 46,00 3,00 20% qtz-calcite/mylonite healed, breccias43,23 43,44 0,21 Mafic Dyke47,00 49,00 2,00 Amygdaloidal section50,85 51,84 0,99 Intermediate Dyke

51,84 57,07 5,23 Fragmental section

53,47 53,80 0,33 Mafic Dyke57,07 60,00 2,93 15% qtz-calcite/mylonite healed, breccias60,00 68,84 8,84 Occasional chlorite filled amygdules60,74 60,88 0,14 Tuffaceous inclusion68,84 69,26 0,42 Mafic Dyke69,26 76,75 7,49 15% qtz-calcite/mylonite healed, breccias70,86 71,30 0,44 Mafic Dyke73,13 73,98 0,85 Mafic Dyke76,75 79,33 2,58 Fragmental section

79,33 99,19 19,86 5% pillow breccias99,19 100,20 1,01 Strong breccia100,20 109,88 9,68 15% pillow breccias109,88 110,50 0,62 Mafic Dyke

110,50 111,97 1,47 25% pillow breccias111,97 112,26 0,29 Mafic Dyke112,26 115,00 2,74 Fragmental section115,00 128,70 13,70 15% pillow breccias128,70 132,35 3,65 5% pillow breccias

DDH Depth Lithology of Sub-unitsComments

Chlorite healing breccias and fragmental sections. Grey-green to dark grey. Mostly pale grey-green fragments.

Pale grey-green. Fine grained matrix, with occasional feldspar phenocrysts. UC, at 45 deg tca. LC, at 35 deg tca.Chlorite healing breccias and fragments. Grey-green to dark grey. Mostly pale grey-green fragments. LC, at 20 deg tca.

Pale grey-green. UC, at 55 deg tca. LC, at 60 deg tca.

Pale grey-green. Fine grained. Massive. UC, at 40 deg tca. LC, at 45 deg tca.

Dark grey. UC, at 65 deg tca. LC, at 60 deg tca.

Grey-green. UC, at 50 deg tca. LC, at 55 deg tca.Grey-green. UC, at 40 deg tca. LC, at 35 deg tca.Chlorite healing breccias and fragments. Grey-green to dark grey. Mostly pale grey-green to grey-green fragments.

Bedding at 50-60 deg tca. UC, at 70 deg tca. LC, at 55 deg tca.Grey-green. UC, at 20 deg tca. LC, at 85 deg tca.

UC, at 40 deg tca. LC, at 45 deg tca.

Greenish-brown to pale green, with a pinkish hue. Fine grained matrix, with occasional mafic phenocrysts and rare mafic clasts. UC, at 90 deg tca. LC, at 40 deg tca.

Dark grey-green to dark grey

132,35 133,61 1,26 Graphitic Argillites

133,61 134,51 0,90 Mafic Dyke134,51 134,68 0,17 Graphitic Argillites134,68 137,35 2,67 Mafic Dyke

137,35 139,58 2,23 Pillowed mafic metavolcanics, mixed in with graphitic argillites

139,58 159,38 19,80 Pillowed mafic metavolcanics

140,88 141,40 0,52 Pillowed mafic metavolcanics, mixed in with graphitic argillites

154,56 154,71 0,15 Lost core155,89 156,15 0,26 Mafic Dyke168,45 168,90 0,45 Lost core168,90 169,30 0,40 Pillowed mafic metavolcanics169,30 169,40 0,10 Pillowed mafics with graphitic argillites170,51 170,76 0,25 Pillowed mafic metavolcanics171,68 171,77 0,09 Pillowed mafic metavolcanics176,20 176,44 0,24 Graphitic Argillites180,21 181,18 0,97 Mafic Dyke184,77 185,15 0,38 Inclusions of different lithologies. Contacts hard to

determine, due to poor core condition.188,89 188,97 0,08 Mafic Dyke193,10 193,26 0,16 Mafic Dyke193,50 195,15 1,65 Unit becomes dark grey, with pale green patches196,53 196,62 0,09 Mafic Dyke198,46 198,55 0,09 Mafic Dyke221,85 225,40 3,55 Fragmental section225,40 233,00 7,60 Amygdaloidal section227,83 228,10 0,27 Mafic Dyke229,14 229,21 0,07 Mafic Dyke229,27 230,12 0,85 Mafic Dyke243,00 244,50 1,50 Amygdaloidal section245,55 246,09 0,54 Mafic Dyke253,00 253,90 0,90 Amygdaloidal section

Pale grey-green. Fine grained matrix, with common mafic and occasional feldspar phenocrysts. LC, at 65 deg tca.Dark grey to black, with pale grey-green patches. 15% graphitic argillite beds. Local bedding. LC, at 70 deg tca.Pale grey-green to pale brownish-green, with occasional grey-green to grey patches. Occasional qtz-calcite filled amygdules. Rare pillow breccias.Dark grey to black. 35% graphitic argillite beds. Local bedding. UC, at 65 deg tca. LC, at 50 deg tca.

Dark grey to black. Aphanitic. Bedded. Minor veining. UC, at 70 deg tca. LC, at 80 deg tca.LC, at 60 deg tca.LC, at 70 deg tca.

LC, at 70 deg tcaUC, at 75 deg tca. LC, at 60 deg tca.UC, at 85 deg tca. LC, at 75 deg tca.UC, broken

Dark green. UC, at 65 deg tca. LC, at 45 deg tca.

LC, at 75 deg tca

UC, at 45 deg tca. LC, at 50 deg tca.UC, at 40 deg tca. LC, at 40 deg tca.

Purplish-grey. UC, at 40 deg tca. LC, at 35 deg tca.

UC, at 45 deg tca. LC, at 50 deg tca.UC, at 40 deg tca. LC, at 40 deg tca.

UC, at 40 deg tca. LC, at 50 deg tca.

UC, at 35 deg tca. LC, at 45 deg tca.UC, at 55 deg tca. LC, at appr 80 deg tca.UC, at 50 deg tca. LC, at 35 deg tca.

Comments PhotoFrom To Length Id BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW33,33 41,00 7,67 5 3 Irregular stringers41,00 43,00 2,00 4 5 Locally brecciated43,00 46,00 3,00 5 15 Qtz-cal/mylonite veining46,00 50,85 4,85 3 5 Locally brecciated51,84 57,07 5,23 5 357,07 60,00 2,93 4 10 50 10 Qtz-cal/mylonite veining60,00 68,84 8,84 3 3 Locally brecciated68,84 76,75 7,91 3 10 Qtz-cal/mylonite veining76,75 79,33 2,58 4 2 Locally brecciated79,33 99,19 19,86 2 3 Locally brecciated99,19 100,20 1,01 5 15100,20 111,00 10,80 2 5 Locally brecciated111,00 111,97 0,97 3 40 3 10112,26 115,00 2,74 4 45 4 10115,00 128,70 13,70 2 10 Locally brecciated128,70 132,35 3,65 2 3 Locally brecciated132,35 133,61 1,26 5 50 1137,35 139,58 2,23 3 65 2 1 Local bedding139,58 155,00 15,42 1 3155,00 159,38 4,38 1 10159,38 168,90 9,52 3168,90 176,44 7,54 3176,44 182,21 5,77 5182,21 186,55 4,34 1186,55 188,55 2,00 3 40 1 Local bedding188,55 202,11 13,56 5202,11 217,00 14,89 2 2 Locally brecciated217,00 233,00 16,00 2 5 Locally brecciated233,00 253,90 20,90 2 2 Locally brecciated

DDH Depth Structure (Intensity 1-5) Veining (%)

From To Length Id Cal Ank Ser Hem Chl SI Bio Fel Epi Lim Cal Ank Ser Hem Chl SI Bio Fel Epi Lim Comments33,33 41,00 7,67 3 35 341,00 50,85 9,85 3 550,85 51,84 0,99 551,84 57,07 5,23 3 1557,07 60,00 2,93 360,00 76,75 16,75 3 576,75 79,33 2,58 3 2579,33 99,19 19,86 3 399,19 100,20 1,01 3 25100,20 112,26 12,06 3 3112,26 115,00 2,74 3 35115,00 128,70 13,70 3 3128,70 132,35 3,65 4 15132,35 133,61 1,26 3133,61 134,68 1,07 3134,68 137,35 2,67 5137,35 139,58 2,23 4139,58 159,38 19,80 2159,38 168,90 9,52 5168,90 176,44 7,54 4176,44 180,21 3,77 2 4 Patchy silicification180,21 181,18 0,97 4181,18 182,21 1,03 2 4 Patchy silicification182,21 186,55 4,34 4186,55 188,55 2,00 3188,55 202,11 13,56 2202,11 220,00 17,89 1220,00 234,00 14,00 1 4 Patchy silicification234,00 253,90 19,90 1

DDH Depth Alteration (1-5) Weak to Strong Fracture controlled alteration (%)

From To Length Id Description SUL PY PO CPY SPH GAL MAG HEM

33,33 45,00 11,67 0,5

45,00 47,00 2,00 1

47,00 50,85 3,85 0,5

50,85 51,84 0,99 0,1

51,84 57,07 5,23 0,5

57,07 60,00 2,93 1 0,1

60,00 68,84 8,84 0,5

68,84 69,26 0,42 2

69,26 70,86 1,60 1

70,86 71,30 0,44 2

71,30 73,13 1,83 1

73,13 73,98 0,85 2

73,98 76,75 2,77 1

76,75 79,33 2,58 0,5

79,33 99,19 19,86 0,5

99,19 100,20 1,01 0,5

100,20 112,26 12,06 0,5

112,26 115,00 2,74 0,5

115,00 128,70 13,70 0,5128,70 130,40 1,70 2130,40 132,35 1,95 3 5132,35 133,61 1,26 15133,61 134,51 0,90 2134,51 134,68 0,17 10134,68 137,35 2,67 0,5137,35 138,90 1,55 8138,90 139,58 0,68 15139,58 140,88 1,30 0,5140,88 141,40 0,52 5141,40 157,00 15,60 0,5157,00 159,38 2,38 2159,38 168,90 9,52 Disseminated py 10168,90 176,44 7,54 2176,44 178,20 1,76 3178,20 180,21 2,01 1180,21 181,18 0,97 2

DDH Depth Mineralization (%)

181,18 182,21 1,03 1182,21 184,40 2,19 0,5184,40 186,55 2,15 3186,55 188,55 2,00 Finely disseminated PY, or in clusters 15188,55 191,00 2,45 Scattered PY or in bands 10 0,5191,00 192,00 1,00 3192,00 202,11 10,11 1202,11 207,00 4,89 0,5207,00 208,00 1,00 0,5 0,1208,00 228,10 20,10 0,5228,10 234,00 5,90 1234,00 253,90 19,90 0,5

Sample Number From To Length Comments Id Au Ag37605 33,33 34,10 0,7737606 34,10 34,90 0,8037607 34,90 35,65 0,75

1 35,65 36,77 1,12 Lost core37608 36,77 37,60 0,8337609 37,60 38,40 0,8037610 38,40 39,33 0,9337611 QUARTZ Purchased37612 39,33 40,20 0,8737613 40,20 41,00 0,8037614 41,00 42,00 1,0037615 42,00 43,00 1,0037616 43,00 44,00 1,0037617 44,00 45,00 1,0037618 45,00 46,00 1,0037619 46,00 47,00 1,0037620 47,00 48,00 1,0037621 48,00 49,00 1,0037622 49,00 50,00 1,0037623 50,00 50,85 0,8537624 50,85 51,84 0,9937625 51,84 52,90 1,0637626 52,90 54,00 1,1037627 54,00 55,00 1,0037628 OREAS 15Pa Batch 2 Can37629 55,00 56,00 1,0037630 56,00 57,07 1,0737631 57,07 58,00 0,9337632 58,00 59,00 1,0037633 59,00 60,00 1,0037634 60,00 61,00 1,0037635 61,00 62,00 1,0037636 62,00 63,00 1,0037637 63,00 64,00 1,0037638 64,00 65,00 1,0037639 65,00 66,00 1,0037640 66,00 67,00 1,0037641 67,00 68,00 1,00

Assays

37642 68,00 68,84 0,8437643 68,84 69,26 0,4237644 69,26 70,00 0,7437645 70,00 70,86 0,8637646 70,86 71,30 0,4437647 71,30 72,20 0,9037648 72,20 73,13 0,9337649 73,13 73,98 0,8537650 73,98 75,00 1,0237651 75,00 75,90 0,9037652 75,90 76,75 0,8537653 OREAS 6Pc Batch 1 Can37654 76,75 77,60 0,8537655 77,60 78,40 0,8037656 78,40 79,33 0,9337657 79,33 80,20 0,8737658 80,20 81,00 0,8037659 81,00 82,00 1,0037660 82,00 83,00 1,0037661 83,00 84,00 1,0037662 84,00 85,00 1,0037663 85,00 86,00 1,0037664 86,00 87,00 1,0037665 87,00 88,00 1,0037666 88,00 89,00 1,0037667 89,00 90,00 1,0037668 90,00 91,00 1,0037669 91,00 92,00 1,0037670 92,00 93,00 1,0037671 93,00 94,00 1,0037672 DIABASE 108.0-108.537673 94,00 95,00 1,0037674 95,00 96,00 1,0037675 96,00 97,00 1,0037676 97,00 98,10 1,1037677 98,10 99,19 1,0937678 99,19 100,20 1,0137679 100,20 101,00 0,8037680 101,00 102,00 1,0037681 102,00 103,00 1,0037682 103,00 104,00 1,00

37683 104,00 105,00 1,0037684 105,00 106,00 1,0037685 106,00 107,00 1,0037686 107,00 108,00 1,0037687 108,00 109,00 1,0037688 OREAS 15Pa Batch 2 Can37689 109,00 109,88 0,8837690 109,88 110,50 0,6237691 110,50 111,40 0,9037692 111,40 112,26 0,8637693 112,26 113,10 0,8437694 113,10 114,00 0,9037695 114,00 115,00 1,0037696 115,00 116,00 1,0037697 116,00 117,00 1,0037698 117,00 118,00 1,0037699 118,00 119,00 1,0037700 119,00 120,00 1,0037701 120,00 121,00 1,0037702 121,00 122,00 1,0037703 122,00 123,00 1,0037704 123,00 124,00 1,0037705 124,00 125,00 1,0037706 125,00 126,00 1,0037707 126,00 127,00 1,0037708 127,00 127,90 0,9037709 127,90 128,70 0,8037710 128,70 129,50 0,8037711 129,50 130,40 0,9037712 130,40 131,40 1,0037713 131,40 132,35 0,9537714 132,35 133,00 0,6537715 OREAS 6Pc Batch 1 Can37716 133,00 133,61 0,6137717 133,61 134,68 1,0737718 134,68 135,50 0,8237719 135,50 136,40 0,9037720 136,40 137,35 0,9537721 137,35 138,10 0,7537722 138,10 138,90 0,8037723 138,90 139,58 0,68

37724 139,58 140,20 0,6237725 140,20 140,88 0,6837726 140,88 141,40 0,5237727 141,40 142,40 1,00

Sampling gap37728 155,00 155,89 0,8937729 155,89 157,00 1,1137730 157,00 157,80 0,8037731 157,80 158,60 0,8037732 158,60 159,38 0,7837733 159,38 160,40 1,0237734 DIABASE 108.5-109.037735 160,40 161,40 1,0037736 161,40 162,40 1,0037737 162,40 163,40 1,0037738 163,40 164,40 1,0037739 164,40 165,40 1,0037740 165,40 166,40 1,0037741 166,40 167,40 1,0037742 167,40 168,45 1,05

1 168,45 168,90 0,45 Lost core37743 168,90 169,80 0,9037744 169,80 170,76 0,9637745 170,76 171,77 1,0137746 OREAS 15Pa Batch 2 Can37747 171,77 172,70 0,9337748 172,70 173,60 0,9037749 173,60 174,50 0,9037750 174,50 175,50 1,0037751 175,50 176,44 0,9437752 176,44 177,30 0,8637753 177,30 178,20 0,9037754 178,20 179,20 1,0037755 179,20 180,21 1,0137756 180,21 181,18 0,9737757 181,18 182,21 1,0337758 182,21 183,30 1,0937759 183,30 184,40 1,1037760 184,40 185,50 1,1037761 185,50 186,55 1,0537762 186,55 187,55 1,00

37763 OREAS 6Pc Batch 1 Can37764 187,55 188,55 1,0037765 188,55 189,40 0,8537766 189,40 190,20 0,8037767 190,20 191,00 0,8037768 191,00 192,00 1,0037769 192,00 193,00 1,0037770 193,00 194,00 1,0037771 194,00 195,00 1,0037772 195,00 196,00 1,0037773 196,00 197,00 1,0037774 197,00 198,00 1,0037775 198,00 199,00 1,0037776 199,00 200,00 1,0037777 200,00 201,00 1,0037778 201,00 202,11 1,1137779 202,11 203,00 0,8937780 203,00 204,00 1,0037781 204,00 205,00 1,0037782 205,00 206,00 1,0037783 206,00 207,00 1,0037784 207,00 208,00 1,0037785 DIABASE 108.5-109.037786 208,00 209,00 1,00

Sampling gap37787 227,10 228,10 1,0037788 228,10 229,10 1,0037789 229,10 230,12 1,0237790 230,12 231,00 0,8837791 231,00 232,00 1,0037792 232,00 233,00 1,0037793 233,00 234,00 1,0037794 234,00 235,00 1,00

CommentsFrom To Length % Length % Comments From To From To From To

0 33,33 OB33,33 35 1,67 100,00 0,47 71,86 33,83 34,55

35 38 1,88 62,67 0,16 91,49 Lost core 37,75 38,0738 41 3,00 100,00 0,27 91,00 41,72 41,8741 44 3,00 100,00 0,45 85,00 42,36 42,6644 47 3,04 101,33 0,06 98,0347 50 3,06 102,00 0,00 100,0050 53 3,02 100,67 0,06 98,0153 56 2,97 99,00 0,05 98,3256 59 3,00 100,00 0,19 93,6759 62 3,05 101,67 0,08 97,3862 65 2,89 96,33 0,00 100,0065 68 3,02 100,67 0,09 97,0268 71 2,93 97,67 0,06 97,9571 74 3,00 100,00 0,00 100,0074 77 2,96 98,67 0,14 95,2777 80 3,07 102,33 0,10 96,7480 83 2,90 96,67 0,12 95,8683 86 2,97 99,00 0,05 98,3286 89 2,97 99,00 0,19 93,60 86,68 86,8989 92 2,97 99,00 0,16 94,6192 95 3,04 101,33 0,21 93,0995 98 2,97 99,00 0,21 92,9398 101 2,96 98,67 0,56 81,08 100,22 100,71101 104 3,05 101,67 0,00 100,00104 107 2,98 99,33 0,00 100,00107 110 3,00 100,00 0,12 96,00110 113 2,96 98,67 0,19 93,58113 116 3,03 101,00 0,00 100,00116 119 3,01 100,33 0,00 100,00119 122 2,95 98,33 0,00 100,00122 125 3,04 101,33 0,00 100,00125 128 2,98 99,33 0,00 100,00128 131 2,88 96,00 0,39 86,46131 134 3,09 103,00 0,15 95,15134 137 2,94 98,00 0,16 94,56137 140 3,00 100,00 0,16 94,67140 143 2,96 98,67 0,50 83,11 141,4 141,76143 146 3,02 100,67 0,00 100,00146 149 3,04 101,33 0,30 90,13 146,41 146,57149 152 2,99 99,67 0,25 91,64 149,28 149,46

Geotechnical LogDDH Depth Recovery RQD Blocky core Crumbly core Fault gouge

152 155 2,85 95,00 0,05 98,25 Lost core155 158 3,06 102,00 0,06 98,04158 161 3,04 101,33 0,72 76,32 158,58 159,13161 164 3,00 100,00 0,12 96,00 159,62 160,03164 167 2,97 99,00 0,33 88,89 166,62 166,78167 170 2,55 85,00 1,15 54,90 Lost core 167,36 168,45170 173 2,99 99,67 0,47 84,28 169,17 169,4173 176 3,00 100,00 0,12 96,00 170,7 170,87176 179 3,00 100,00 1,00 66,67 172,07 172,3179 182 3,00 100,00 0,49 83,67 175,61 176,53182 185 3,00 100,00 1,06 64,67 181,17 181,52185 188 3,00 100,00 1,50 50,00 183,65 185,49188 191 3,10 103,33 0,16 94,84 186,36 187,22191 194 3,13 104,33 0,05 98,40194 197 3,06 102,00 0,11 96,41 196,53 196,78197 200 3,01 100,33 0,00 100,00200 203 2,97 99,00 0,00 100,00203 206 3,03 101,00 0,00 100,00206 209 2,96 98,67 0,00 100,00209 212 3,05 101,67 0,00 100,00212 215 2,98 99,33 0,00 100,00215 218 3,05 101,67 0,00 100,00218 221 2,89 96,33 0,17 94,12 220,83 221221 224 2,98 99,33 0,00 100,00224 227 3,04 101,33 0,00 100,00227 230 3,03 101,00 0,14 95,38230 233 2,92 97,33 0,00 100,00233 236 2,98 99,33 0,00 100,00236 239 3,00 100,00 0,05 98,33239 242 2,96 98,67 0,00 100,00242 245 2,96 98,67 0,52 82,43 244,3 245,57245 248 3,04 101,33 0,74 75,66 247 247,19248 251 2,99 99,67 0,17 94,31 249,66 249,84251 254 3,00 100,00 0,00 100,00


C-08-02 1500 1200 350 0 -60 350 07-avr-08 09-juil-08

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 27,45 27,45 OB overburden27,45 179,89 152,44 MAn fg green-pale grey, pillowed, loc fractured

179,89 191,87 11,98 grey-green, fg-mg mafic clasts, felsic fragment

191,87 206,50 14,63 dark grey-green, fg-mg, loc mafic phX, 3-5% py

206,50 210,27 3,77 grey-brown, fg matrix, w loc fd phX, silicified, 2-3% py

210,27 211,65 1,38 mixed graphite siltstone, bedding 25-40 to CA, 5-8% py, 1% po211,65 214,15 2,50 grey-green, fg-mg, massive, hard214,15 216,7 2,55 medium-pale green, chlo alt

216,70 217,14 0,44 GSiS fg black, bedding 35-50 to CA, 5% py, tr po217,14 219,34 2,20 Tuf pale-brown-grey, fg, clasts, 35-50 to CA, 15-35 % py219,34 222 2,66 Tuf pale-brown-grey, fg, clasts, 35-50 to CA, 1-2 % py

222,00 255,59 33,59 MAn fg green-pale grey, pillowed, loc fractured, minor-2% py255,59 266,51 10,92 grey-pinkish, fg, silicified, 8-10% py266,51 349,67 83,16 pale grey-green, fg, pillow

DDH Depth

DDH Depth Structure (Intensity 1-5) Veining (%)From To Length Id comments BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW Photo139,40 141,80 2,40 SZ

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments27,45 35,20 7,75 Intense breccia, 5% irr qz-cal, 1% fine diss py34,67 34,8 0,13 MaD dark green, mafic dyke35,70 52,6 16,90 PAn pale grey-green, pillow, stringer, py, po52,60 57,40 4,8057,40 66,00 8,60

62,33 62,60 0,27 MaD grey-brown, 2% pyrite very weak suscept66,00 72,00 6,00 PAn 20% interpillow breccia72,00 77,00 5,00 Tuf 25% tuff pyroclastics77,00 93,00 16,00 Tuf 50% tuff pyroclastics93,00 104,00 11,00 PAn pillow, interpillow breccia104,00 129,90 25,90 grey-green, well formed pillow w breccia

127,58 127,98 0,40 MaD brownish-grey, fg, w mafic phX, 3% py129,90 136,56 6,66 grey-green, well formed pillow w breccia, w loc po136,56 137,78 1,22

137,78 146,35 8,57 MAn 1-2% fine py, 146,35 149,69 3,34 MaD grey-brown w mafic phX149,69 162,46 12,77 MAn 30% tuff, 1-2% py, tr po162,46 164,12 1,66 MaD grey-brown, hom, loc mafic phX, w 8-10% py164,12 171,84 7,72 MAn pale grey-green, pillow, stringer, py171,84 174,85 3,01 GSiS brownish-green w dark, 1% py, 5-8% po174,85 179,89 5,04 MAn pale grey-green, pillow175,12 175,52 0,40 InD pale brown, fg, fd phX, hom

183,49 183,92 0,43 70% graphitic siltstone, 5% py187,47 187,58 0,11 pinkish-brown, fg, intensely fractured, silicified, 20% py190,75 191,87 1,12 grey-green, fg, loc hard, loc soft, 3% py205,36 205,83 0,47 MaD dark purplish brown, silicified, hard, 5% py205,83 206,02 0,19 UlD medium green, fg, loc hard, loc soft, 3% py206,02 206,13 0,11 MaD dark brownish-grey, fg, hom206,13 206,5 0,37 UlD same as previous, lineation 25-40 to CA217,14 217,9 0,76 35% py217,90 218,6 0,70 25% py218,60 219,34 0,74 15% py219,34 219,91 0,57 MaD grey-green, fg, massive, hard, 15% py285,98 286,31 0,33 MaD dark brown, fg, strong calcite alteration338,00 349,67 11,67 Tuf tuffaceous pyroclastics349,67 -349,67

DDH Depth

HoleIDSample Number

From (m) To (m) Length (m) Au(g/t)Au(g/t) Check

Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-02 18377 27,45 28,30 0,85 0,010 0,010C08-02 18378 28,30 29,10 0,80 0,020 0,020C08-02 18379 29,10 30,00 0,90 0,010 0,010C08-02 18380 30,00 31,00 1,00 0,010 0,010C08-02 18381 31,00 32,00 1,00 0,010 0,010C08-02 18382 32,00 33,00 1,00 0,010 0,010C08-02 18383 33,00 34,00 1,00 0,030 0,010 0,020C08-02 18384 34,00 34,90 0,90 0,000 0,000C08-02 18385 34,90 35,70 0,80 0,000 0,000C08-02 18386 35,70 36,70 1,00 0,020 0,020C08-02 18387 36,70 37,70 1,00 0,010 0,010C08-02 18388 37,70 38,70 1,00 0,010 0,010C08-02 18389 38,70 39,70 1,00 0,010 0,010C08-02 18390 QUARTZ Purchased 0,010 0,010C08-02 18391 39,70 40,70 1,00 0,010 0,010C08-02 18392 40,70 41,68 0,98 0,000 0,010 0,005C08-02 18393 41,78 42,70 0,92 0,010 0,010C08-02 18394 42,70 43,60 0,90 0,010 0,010C08-02 18395 43,60 44,60 1,00 0,010 0,010C08-02 18396 44,60 45,60 1,00 0,010 0,010C08-02 18397 45,60 46,60 1,00 0,010 0,010C08-02 18398 46,60 47,60 1,00 0,000 0,000 0,000C08-02 18399 47,60 48,60 1,00 0,000 0,000C08-02 18400 48,60 49,60 1,00 0,010 0,010C08-02 18401 49,60 50,60 1,00 0,010 0,010C08-02 18402 50,60 51,60 1,00 0,010 0,010C08-02 18403 51,60 52,60 1,00 0,010 0,010C08-02 18404 52,60 53,50 0,90 0,010 0,010C08-02 18405 53,50 54,50 1,00 0,000 0,000C08-02 18406 54,50 55,50 1,00 0,010 0,010C08-02 18407 OREAS 14P Batch 8 Aus 0,060 0,060C08-02 18408 55,50 56,50 1,00 0,020 0,020C08-02 18409 56,50 57,40 0,90 0,020 0,020C08-02 18410 57,40 58,20 0,80 0,010 0,010C08-02 18411 58,20 59,00 0,80 0,010 0,010C08-02 18412 59,00 60,00 1,00 0,010 0,010

C08-02 18413 60,00 61,00 1,00 0,010 0,010C08-02 18414 61,00 62,00 1,00 0,010 0,020 0,015C08-02 18415 62,00 63,00 1,00 0,010 0,010C08-02 18416 63,00 64,00 1,00 0,010 0,010C08-02 18417 64,00 65,00 1,00 0,020 0,020C08-02 18418 65,00 66,00 1,00 0,000 0,000C08-02 18419 66,00 67,00 1,00 0,010 0,010C08-02 18420 67,00 68,00 1,00 0,010 0,010C08-02 18421 68,00 69,00 1,00 0,010 0,020 0,015C08-02 18422 69,00 70,00 1,00 0,000 0,000C08-02 18423 70,00 71,00 1,00 0,010 0,010C08-02 18424 71,00 72,00 1,00 0,010 0,010C08-02 18425 72,00 73,00 1,00 0,010 0,010C08-02 18426 73,00 74,00 1,00 0,010 0,010C08-02 18427 74,00 75,00 1,00 0,010 0,010C08-02 18428 75,00 76,00 1,00 0,010 0,010C08-02 18429 76,00 77,00 1,00 0,020 0,000 0,010C08-02 18430 77,00 78,00 1,00 0,010 0,010C08-02 18431 78,00 79,00 1,00 0,010 0,010C08-02 18432 79,00 80,00 1,00 0,020 0,020C08-02 18433 OREAS 14P Batch 8 Aus 0,050 0,050C08-02 18434 80,00 81,00 1,00 0,000 0,000C08-02 18435 81,00 82,00 1,00 0,010 0,010C08-02 18436 82,00 83,00 1,00 0,010 0,010C08-02 18437 83,00 84,00 1,00 0,000 0,000C08-02 18438 84,00 85,00 1,00 0,000 0,000C08-02 18439 85,00 86,00 1,00 0,000 0,000C08-02 18440 86,00 87,00 1,00 0,000 0,000C08-02 18441 87,00 88,00 1,00 0,020 0,020C08-02 18442 88,00 89,00 1,00 0,010 0,010C08-02 18443 89,00 90,00 1,00 0,010 0,010C08-02 18444 90,00 91,00 1,00 0,000 0,010 0,005C08-02 18445 91,00 92,00 1,00 0,000 0,000C08-02 18446 92,00 93,00 1,00 0,010 0,010C08-02 18447 93,00 94,00 1,00 0,000 0,000C08-02 18448 94,00 95,00 1,00 0,000 0,000C08-02 18449 95,00 96,00 1,00 0,010 0,010C08-02 18450 96,00 97,00 1,00 0,000 0,000

C08-02 18451 97,00 98,00 1,00 0,010 0,000 0,005C08-02 18452 98,00 99,00 1,00 0,010 0,010C08-02 18453 99,00 100,00 1,00 0,010 0,010C08-02 18454 DIABASE 87.6-88 0,000 0,000C08-02 18455 100,00 101,00 1,00 0,010 0,010C08-02 18456 101,00 102,00 1,00 0,010 0,010C08-02 18457 102,00 103,00 1,00 0,000 0,000C08-02 18458 103,00 104,00 1,00 0,010 0,010C08-02 18459 104,00 105,00 1,00 0,000 0,000C08-02 18460 105,00 106,00 1,00 0,000 0,000C08-02 18461 106,00 107,00 1,00 0,000 0,000 0,000C08-02 18462 107,00 108,00 1,00 0,000 0,000C08-02 18463 OREAS 14P Batch 8 Aus 0,060 0,060C08-02 18464 108,00 109,00 1,00 0,000 0,000C08-02 18465 109,00 110,00 1,00 0,000 0,000C08-02 18466 110,00 111,00 1,00 0,000 0,000C08-02 18467 111,00 112,00 1,00 0,000 0,000C08-02 18468 112,00 113,00 1,00 0,010 0,010C08-02 18469 113,00 114,00 1,00 0,000 0,000C08-02 18470 114,00 115,00 1,00 0,000 0,000C08-02 18471 115,00 116,00 1,00 0,000 0,000C08-02 18472 116,00 117,00 1,00 0,010 0,010C08-02 18473 117,00 118,00 1,00 0,010 0,010C08-02 18474 118,00 119,00 1,00 0,010 0,010C08-02 18475 119,00 120,00 1,00 0,010 0,010C08-02 18476 120,00 121,00 1,00 0,000 0,010 0,005C08-02 18477 121,00 122,00 1,00 0,010 0,010C08-02 18478 122,00 123,00 1,00 0,010 0,010C08-02 18479 123,00 124,00 1,00 0,000 0,000C08-02 18480 124,00 125,00 1,00 0,010 0,010C08-02 18481 125,00 126,00 1,00 0,040 0,040C08-02 18482 126,00 127,00 1,00 0,000 0,000C08-02 18483 127,00 128,00 1,00 0,000 0,000C08-02 18484 128,00 129,00 1,00 0,000 0,000C08-02 18485 129,00 129,90 0,90 0,010 0,010C08-02 18486 129,90 130,80 0,90 0,050 0,000 0,025C08-02 18487 130,80 131,70 0,90 0,000 0,000C08-02 18488 131,70 132,60 0,90 0,010 0,010

C08-02 18489 132,60 133,60 1,00 0,010 0,000 0,005C08-02 18490 133,60 134,60 1,00 0,000 0,000C08-02 18491 134,60 135,60 1,00 0,010 0,010C08-02 18492 135,60 136,56 0,96 0,050 0,050C08-02 18493 OREAS 14P Batch 8 Aus 0,050 0,050C08-02 18494 136,56 137,20 0,64 0,030 0,030C08-02 18495 137,20 137,78 0,58 0,020 0,020C08-02 18496 137,78 138,70 0,92 0,000 0,000C08-02 18497 138,70 139,60 0,90 0,010 0,000 0,005C08-02 18498 139,60 140,50 0,90 0,010 0,010C08-02 18499 140,50 141,40 0,90 0,000 0,000C08-02 18500 141,40 142,40 1,00 0,020 0,020C08-02 18501 142,40 143,40 1,00 0,010 0,010C08-02 18502 143,40 144,40 1,00 0,020 0,020C08-02 18503 144,40 145,40 1,00 0,030 0,030C08-02 18504 145,40 146,35 0,95 0,010 0,010C08-02 18505 146,35 147,20 0,85 0,020 0,020C08-02 18506 147,20 148,10 0,90 0,000 0,000 0,000C08-02 18507 148,10 148,90 0,80 0,010 0,010C08-02 18508 148,90 149,69 0,79 0,010 0,010C08-02 18509 149,69 150,60 0,91 0,010 0,010C08-02 18510 150,60 151,50 0,90 0,010 0,010C08-02 18511 QUARTZ Purchased 0,000 0,000C08-02 18512 151,50 152,50 1,00 0,000 0,000C08-02 18513 152,50 153,50 1,00 0,010 0,010C08-02 18514 153,50 154,50 1,00 0,000 0,000C08-02 18515 154,50 155,50 1,00 0,010 0,010C08-02 18516 155,50 156,50 1,00 0,010 0,010C08-02 18517 156,50 157,50 1,00 0,010 0,010C08-02 18518 157,50 158,50 1,00 0,000 0,010 0,005C08-02 18519 158,50 159,50 1,00 0,000 0,000C08-02 18520 159,50 160,40 0,90 0,000 0,000C08-02 18521 160,40 161,40 1,00 0,000 0,000C08-02 18522 161,40 162,46 1,06 0,000 0,000C08-02 18523 162,46 163,30 0,84 0,020 0,020C08-02 18524 163,30 164,12 0,82 0,030 0,030C08-02 18525 164,12 165,00 0,88 0,010 0,010C08-02 18526 165,00 166,00 1,00 0,000 0,000

C08-02 18527 166,00 167,00 1,00 0,000 0,000C08-02 18528 167,00 168,00 1,00 0,000 0,000C08-02 18529 168,00 169,00 1,00 0,000 0,010 0,005C08-02 18530 169,00 170,00 1,00 0,000 0,000C08-02 18531 170,00 171,00 1,00 0,010 0,010C08-02 18532 171,00 171,84 0,84 0,000 0,000C08-02 18533 171,84 172,85 1,01 0,010 0,010C08-02 18534 172,85 173,85 1,00 0,000 0,000C08-02 18535 OREAS 14P Batch 8 Aus 0,030 0,030C08-02 18536 173,85 174,85 1,00 0,000 0,000C08-02 18537 174,85 175,90 1,05 0,000 0,000C08-02 18538 175,90 177,00 1,10 0,000 0,000C08-02 18539 177,00 178,00 1,00 0,020 0,020C08-02 18540 178,00 179,00 1,00 0,000 0,010 0,005C08-02 18541 179,00 179,89 0,89 0,000 0,000C08-02 18542 179,89 181,00 1,11 0,000 0,000C08-02 18543 181,00 182,00 1,00 0,010 0,010C08-02 18544 182,00 183,00 1,00 0,000 0,000C08-02 18545 183,00 184,00 1,00 0,000 0,000C08-02 18546 184,00 185,00 1,00 0,000 0,000C08-02 18547 185,00 186,00 1,00 0,000 0,000 0,000C08-02 18548 OREAS 14P Batch 8 Aus 0,040 0,040C08-02 18549 186,00 187,00 1,00 0,000 0,000C08-02 18550 187,00 188,00 1,00 0,000 0,000C08-02 18551 188,00 189,10 1,10 0,000 0,000C08-02 18552 189,10 189,90 0,80 0,000 0,000C08-02 18553 189,90 190,75 0,85 0,000 0,000C08-02 18554 190,75 191,25 0,50 0,000 0,000C08-02 18555 191,25 191,87 0,62 0,010 0,010C08-02 18556 191,87 192,80 0,93 0,000 0,000C08-02 18557 192,80 193,70 0,90 0,010 0,010C08-02 18558 193,70 194,60 0,90 0,010 0,010 0,010C08-02 18559 194,60 195,50 0,90 0,010 0,010C08-02 18560 195,50 196,50 1,00 0,000 0,000C08-02 18561 196,50 197,50 1,00 0,000 0,000C08-02 18562 197,50 198,50 1,00 0,040 0,030 0,035C08-02 18563 198,50 199,50 1,00 0,000 0,000C08-02 18564 199,50 200,50 1,00 0,000 0,000

C08-02 18565 200,50 201,50 1,00 0,000 0,000C08-02 18566 201,50 202,50 1,00 0,000 0,000C08-02 18567 202,50 203,50 1,00 0,000 0,000C08-02 18568 203,50 204,40 0,90 0,000 0,000C08-02 18569 204,40 205,36 0,96 0,000 0,010 0,005C08-02 18570 205,36 205,83 0,47 0,000 0,000C08-02 18571 205,83 206,50 0,67 0,010 0,010C08-02 18572 206,50 207,50 1,00 0,000 0,000C08-02 18573 DIABASE 87.6-88 0,000 0,000C08-02 18574 207,50 208,50 1,00 0,000 0,000C08-02 18575 208,50 209,40 0,90 0,000 0,000C08-02 18576 209,40 210,27 0,87 0,000 0,000C08-02 18577 210,27 211,00 0,73 0,010 0,010C08-02 18578 211,00 211,65 0,65 0,020 0,020C08-02 18579 211,65 212,50 0,85 0,000 0,000C08-02 18580 212,50 213,30 0,80 0,000 0,000C08-02 18581 213,30 214,15 0,85 0,000 0,000C08-02 18582 214,15 215,03 0,88 0,000 0,000C08-02 18583 215,03 215,90 0,87 0,000 0,000C08-02 18584 215,90 216,70 0,80 0,010 0,010C08-02 18585 216,70 217,14 0,44 0,010 0,010C08-02 18586 217,14 217,90 0,76 0,020 0,020C08-02 18587 OREAS 14P Batch 8 Aus 0,060 0,060C08-02 18588 217,90 218,60 0,70 0,010 0,010C08-02 18589 218,60 219,34 0,74 0,010 0,010C08-02 18590 219,34 219,91 0,57 0,000 0,000C08-02 18591 219,91 221,00 1,09 0,010 0,010C08-02 18592 221,00 222,00 1,00 0,000 0,000C08-02 18593 222,00 223,00 1,00 0,000 0,000C08-02 18594 223,00 224,00 1,00 0,000 0,000C08-02 18595 224,00 225,00 1,00 0,000 0,000C08-02 18596 225,00 226,00 1,00 0,000 0,000C08-02 18597 226,00 227,00 1,00 0,010 0,010 0,010C08-02 18598 227,00 228,00 1,00 0,000 0,000C08-02 18599 228,00 229,00 1,00 0,000 0,000C08-02 18600 229,00 230,00 1,00 0,000 0,000C08-02 18601 230,00 231,00 1,00 0,000 0,000C08-02 18602 231,00 232,00 1,00 0,000 0,000

C08-02 18603 232,00 233,00 1,00 0,000 0,000C08-02 18604 233,00 234,00 1,00 0,000 0,000C08-02 18605 234,00 235,00 1,00 0,010 0,010C08-02 18606 OREAS 14P Batch 8 Aus 0,050 0,050C08-02 18607 235,00 236,00 1,00 0,000 0,000C08-02 18608 236,00 237,00 1,00 0,000 0,000C08-02 18609 237,00 238,00 1,00 0,000 0,000C08-02 18610 238,00 239,00 1,00 0,000 0,000C08-02 18611 239,00 240,00 1,00 0,000 0,000C08-02 18612 240,00 241,00 1,00 0,000 0,000C08-02 18613 241,00 242,00 1,00 0,010 0,030 0,020C08-02 18614 242,00 243,00 1,00 0,000 0,000C08-02 18615 243,00 244,00 1,00 0,000 0,000C08-02 18616 244,00 245,00 1,00 0,000 0,000C08-02 18617 245,00 246,00 1,00 0,000 0,000C08-02 18618 246,00 247,00 1,00 0,000 0,000C08-02 18619 247,00 248,00 1,00 0,000 0,000C08-02 18620 248,00 249,00 1,00 0,000 0,000C08-02 18621 249,00 250,00 1,00 0,010 0,010C08-02 18622 250,00 251,00 1,00 0,010 0,010C08-02 18623 251,00 252,00 1,00 0,010 0,010C08-02 18624 252,00 253,00 1,00 0,010 0,010C08-02 18625 253,00 254,00 1,00 0,000 0,000C08-02 18626 254,00 254,80 0,80 0,000 0,000C08-02 18627 254,80 255,59 0,79 0,010 0,000 0,005C08-02 18628 255,59 256,50 0,91 0,000 0,000C08-02 18629 256,50 257,50 1,00 0,010 0,010C08-02 18630 257,50 258,50 1,00 0,000 0,000C08-02 18631 QUARTZ Purchased 0,010 0,010C08-02 18632 258,50 259,50 1,00 0,000 0,000C08-02 18633 259,50 260,50 1,00 0,010 0,010C08-02 18634 260,50 261,50 1,00 0,000 0,000C08-02 18635 261,50 262,50 1,00 0,000 0,000C08-02 18636 262,50 263,50 1,00 0,000 0,000C08-02 18637 263,50 264,50 1,00 0,000 0,000 0,000C08-02 18638 264,50 265,50 1,00 0,000 0,000C08-02 18639 265,50 266,51 1,01 0,000 0,000C08-02 18640 266,51 267,40 0,89 0,010 0,010

C08-02 18641 267,40 268,20 0,80 0,000 0,000C08-02 18642 268,20 269,00 0,80 0,060 0,060C08-02 18643 269,00 270,00 1,00 0,000 0,000C08-02 18644 270,00 271,00 1,00 0,000 0,000C08-02 18645 271,00 272,00 1,00 0,010 0,010C08-02 18646 272,00 273,00 1,00 0,000 0,000C08-02 18647 273,00 274,00 1,00 0,000 0,000C08-02 18648 274,00 274,75 0,75 0,010 0,010C08-02 18649 274,89 276,00 1,11 0,000 0,000 0,000C08-02 18650 276,00 277,00 1,00 0,010 0,010C08-02 18651 277,00 278,00 1,00 0,000 0,000C08-02 18652 278,00 279,00 1,00 0,000 0,000C08-02 18653 279,00 280,00 1,00 0,010 0,010C08-02 18654 280,00 281,00 1,00 0,000 0,000C08-02 18655 281,00 282,00 1,00 0,010 0,010C08-02 18656 OREAS 14P Batch 8 Aus 0,010 0,010C08-02 18657 282,00 283,00 1,00 0,020 0,020C08-02 18658 283,00 284,00 1,00 0,000 0,000C08-02 18659 284,00 285,00 1,00 0,000 0,000 0,000C08-02 18660 285,00 285,98 0,98 0,000 0,000C08-02 18661 285,98 287,00 1,02 0,000 0,000C08-02 18662 287,00 288,00 1,00 0,020 0,020C08-02 18663 288,00 289,00 1,00 0,000 0,000C08-02 18664 289,00 290,00 1,00 0,000 0,000C08-02 18665 290,00 291,00 1,00 0,000 0,000C08-02 18666 291,00 292,00 1,00 0,000 0,000C08-02 18667 292,00 293,00 1,00 0,010 0,010 0,010C08-02 18668 293,00 294,00 1,00 0,000 0,000C08-02 18669 294,00 295,00 1,00 0,000 0,000C08-02 18670 295,00 296,00 1,00 0,000 0,000C08-02 18671 296,00 297,00 1,00 0,000 0,000C08-02 18672 OREAS 14P Batch 8 Aus 0,020 0,020C08-02 18673 297,00 298,00 1,00 0,000 0,000C08-02 18674 298,00 299,00 1,00 0,000 0,000C08-02 18675 299,00 300,00 1,00 0,000 0,000C08-02 18676 300,00 301,00 1,00 0,000 0,000C08-02 18677 301,00 302,00 1,00 0,000 0,000C08-02 18678 302,00 303,00 1,00 0,000 0,000

C08-02 18679 303,00 304,00 1,00 0,000 0,000C08-02 18680 304,00 305,00 1,00 0,000 0,000C08-02 18681 305,00 306,00 1,00 0,010 0,010C08-02 18682 306,00 307,00 1,00 0,010 0,010C08-02 18683 307,00 308,00 1,00 0,020 0,010 0,015C08-02 18684 308,00 309,00 1,00 0,010 0,010C08-02 18685 DIABASE 88.0-88.5 0,040 0,040C08-02 18686 309,00 310,00 1,00 0,010 0,010C08-02 18687 310,00 311,00 1,00 0,010 0,010C08-02 18688 311,00 312,00 1,00 0,010 0,010C08-02 18689 312,00 313,00 1,00 0,010 0,010C08-02 18690 313,00 314,00 1,00 0,010 0,010C08-02 18691 314,00 315,00 1,00 0,000 0,000C08-02 18692 315,00 316,00 1,00 0,020 0,020C08-02 18693 316,00 317,00 1,00 0,000 0,000C08-02 18694 317,00 318,00 1,00 0,000 0,000C08-02 18695 318,00 319,00 1,00 0,010 0,010C08-02 18696 319,00 320,00 1,00 0,000 0,000C08-02 18697 320,00 321,00 1,00 0,000 0,000 0,000C08-02 18698 321,00 322,00 1,00 0,000 0,000C08-02 18699 322,00 323,00 1,00 0,010 0,010C08-02 18700 323,00 324,00 1,00 0,000 0,000C08-02 18701 324,00 325,00 1,00 0,000 0,000C08-02 18702 325,00 326,00 1,00 0,010 0,010C08-02 18703 326,00 327,00 1,00 0,010 0,010C08-02 18704 327,00 328,00 1,00 0,010 0,010C08-02 18705 328,00 329,00 1,00 0,000 0,000C08-02 18706 329,00 330,00 1,00 0,000 0,000C08-02 18707 330,00 331,00 1,00 0,000 0,000C08-02 18708 331,00 332,00 1,00 0,010 0,010C08-02 18709 332,00 333,00 1,00 0,010 0,010C08-02 18710 333,00 334,00 1,00 0,000 0,000C08-02 18711 334,00 335,00 1,00 0,010 0,010C08-02 18712 335,00 336,00 1,00 0,000 0,000C08-02 18713 OREAS 14P Batch 8 Aus 0,070 0,070C08-02 18714 336,00 337,00 1,00 0,010 0,010C08-02 18715 337,00 338,00 1,00 0,020 0,020C08-02 18716 338,00 339,00 1,00 0,000 0,000

C08-02 18717 339,00 340,00 1,00 0,000 0,000C08-02 18718 340,00 341,00 1,00 0,000 0,000C08-02 18719 341,00 342,00 1,00 0,010 0,010C08-02 18720 342,00 343,00 1,00 0,010 0,010C08-02 18721 343,00 344,00 1,00 0,000 0,000C08-02 18722 344,00 345,00 1,00 0,000 0,010 0,005C08-02 18723 345,00 346,00 1,00 0,010 0,010C08-02 18724 346,00 347,00 1,00 0,010 0,010C08-02 18725 347,00 348,00 1,00 0,000 0,000C08-02 18726 348,00 348,80 0,80 0,000 0,000C08-02 18727 348,80 349,67 0,87 0,010 0,010

DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge CommentsBox no. From To Length % Length % Comments % % From To

27,45 29 1,55 1,55 100% 1,1 71% 50 contains 5% cm quaternary pebbles 29 32 3 3,04 101% 2,70 90% 60 contains 1% cm quaternary pebbles 32 35 3 3 100% 2,91 97% 3035 38 3 2,96 99% 2,62 87% 338 41 3 2,97 99% 2,67 89% 041 44 3 2,9 97% 2,86 95% 044 47 3 3 100% 2,92 97% 047 50 3 3,01 100% 3,00 100% 050 53 3 2,99 100% 3,00 100% 053 56 3 3 100% 2,91 97% 056 59 3 3,05 102% 3,00 100% 059 62 3 3,01 100% 3,00 100% 162 65 3 2,95 98% 3,00 100% 065 68 3 3,05 102% 2,78 93% 068 71 3 2,96 99% 3,00 100% 071 74 3 2,98 99% 2,87 96% 074 77 3 3,02 101% 3,00 100% 077 80 3 2,97 99% 2,88 96% 080 83 3 3,02 101% 2,97 99% 083 86 3 2,94 98% 3,00 100% 486 89 3 3,05 102% 3,00 100% 089 92 3 2,98 99% 2,95 98% 092 95 3 3,05 102% 3,00 100% 095 98 3 2,98 99% 3,00 100% 198 101 3 2,98 99% 2,96 99% 3101 104 3 3,01 100% 3,00 100% 0104 107 3 3,00 100% 3,00 100% 0107 110 3 3,02 101% 3,00 100% 0110 113 3 3,00 100% 2,86 95% 0113 116 3 3,00 100% 3,00 100% 0116 119 3 2,92 97% 3,00 100% 0119 122 3 3,06 102% 3,00 100% 1122 125 3 3,03 101% 2,86 95% 0125 128 3 2,98 99% 2,94 98% 0128 131 3 3,05 102% 2,81 94% 0131 134 3 3,00 100% 3,00 100% 0134 137 3 2,97 99% 2,89 96% 0137 140 3 3,03 101% 2,73 91% 0140 143 3 2,98 99% 2,93 98%143 146 3 2,99 100% 2,55 85%146 149 3 3,04 101% 2,72 91%149 152 3 3,01 100% 3,00 100%152 155 3 2,95 98% 2,80 93%

155 158 3 3,06 102% 2,86 95%158 161 3 3,04 101% 2,93 98%161 164 3 2,97 99% 3,00 100%164 167 3 3,00 100% 3,00 100%167 170 3 2,96 99% 2,87 96%170 173 3 3,07 102% 3,00 100%173 176 3 3,00 100% 2,88 96%176 179 3 3,02 101% 2,86 95%179 182 3 2,99 100% 2,32 77%182 185 3 2,98 99% 2,43 81%185 188 3 2,93 98% 2,94 98%188 191 3 2,95 98% 2,74 91%191 194 3 3,00 100% 3,00 100%194 197 3 3,00 100% 3,00 100%197 200 3 3,03 101% 3,00 100%200 203 3 3,04 101% 3,00 100%203 206 3 2,97 99% 2,95 98%206 209 3 2,95 98% 2,82 94%209 212 3 3,02 101% 3,00 100%212 215 3 3,07 102% 2,91 97%215 218 3 2,90 97% 2,78 93%218 221 3 2,99 100% 2,77 92%221 224 3 3,04 101% 3,00 100%224 227 3 3,01 100% 3,00 100%227 230 3 3,06 102% 3,00 100%230 233 3 2,92 97% 3,00 100%233 236 3 3,05 102% 2,93 98%236 239 3 2,96 99% 3,00 100%239 242 3 3,02 101% 3,00 100%242 245 3 2,98 99% 2,44 81%245 248 3 3,07 102% 2,93 98%248 251 3 2,94 98% 2,90 97%251 254 3 2,90 97% 2,91 97%254 257 3 3,03 101% 2,77 92%257 260 3 3,01 100% 2,52 84%260 263 3 3,00 100% 2,95 98%263 266 3 2,97 99% 2,24 75%266 269 3 3,00 100% 2,94 98%269 272 3 2,99 100% 2,83 94%272 275 3 2,86 95% 2,88 96%275 278 3 2,96 99% 2,87 96%278 281 3 3,01 100% 2,91 97%281 284 3 2,99 100% 2,27 76%284 287 3 3,04 101% 2,79 93%287 290 3 3,00 100% 2,85 95%

290 293 3 3,00 100% 2,87 96%293 296 3 2,99 100% 3,00 100%296 299 3 3,02 101% 2,90 97%299 302 3 3,04 101% 2,92 97%302 305 3 3,06 102% 2,92 97%305 308 3 2,93 98% 2,83 94%308 311 3 2,99 100% 2,96 99%311 314 3 3,01 100% 2,81 94%314 317 3 2,99 100% 2,92 97%317 320 3 3,00 100% 2,97 99%320 323 3 3,01 100% 2,92 97%323 326 3 3,04 101% 3,00 100%326 329 3 3,03 101% 2,77 92%329 332 3 2,98 99% 2,76 92%332 335 3 2,99 100% 3,00 100%335 338 3 3,02 101% 3,00 100%338 341 3 2,98 99% 2,85 95%341 344 3 2,95 98% 3,00 100%344 347 3 3 100% 3,00 100%347 350 3 2,75 92% 3,00 100%


C-08-03 L-200E 350N 250 0 -50 251m 10-juil-08 14-juil-08

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments9,90 10,20 0,30 lost core13,82 14,45 0,63 grey-green carbonates, brecciated, honey sphalerite, minor py14,45 14,9 0,45 lost core15,59 15,82 0,23 grey-green carbonates, brecciated, honey sphalerite, minor py17,35 17,65 0,30 lost core17,87 18,08 0,21 felsic dyke, reddish-brown, silicified, 3% diss py67,74 68,19 0,45 felsic dyke, pinkish-brown to orange, silicified, 1% py80,00 80,64 0,64 mafic dyke, grey-green, fmg, calcite alteration99,39 99,58 0,19 intermediate dyke, medium green with pink, py99,98 100,62 0,64 intermediate dyke, purplish-brown101,16 101,41 0,25 intermediate dyke, pinkish-brown106,47 106,96 0,49 ultramafic inclusion, pale grey-green, fg, foliation 20-40 to CA, talcose, 3% py107,05 107,24 0,19 red felsic dyke, syenite?? feldspar phenocryst, 3% py107,24 107,54 0,30 ultramafic inclusion, fg, spiderweb veining, talcose, 2% py108,16 108,63 0,47 ultramafic inclusion, fg, spiderweb veining, talcose, 3% py118,31 118,69 0,38 red felsic dyke, syenite?? feldspar phenocryst, 2% py122,18 122,34 0,16 mafic dyke, purplish-grey, aphanitic, massive122,34 122,41 0,07 ultramafic inclusion122,71 122,97 0,26 ultramafic inclusion, grey-green, fg, foliation 15-45 to CA, talcose, 3% py123,56 123,89 0,33 red felsic dyke, phenocryst, 5% py142,84 142,9 0,06 ultramafic inclusion

142,97 144,2 1,23basaltics komatiite, pale grey-green, fg, foliation 30-45 to CA, spinifex texture, talcose, 2% py

144,58 144,82 0,24 basaltic komatiite146,30 147,13 0,83 basaltic komatiite, grey-green, fg, foliation 50-70 to CA, talcose, 3% py150,83 151,59 0,76 felsic dyke, pale reddish-brown, fg matrix, mafic phenocryst, 5% py152,45 152,87 0,42 intermediate dyke, greenish-brown, fg matrix, phenocryst, 3% py153,44 155,7 2,26 ultramafic inclusions156,44 157,88 1,44 basaltic komatiite, pale grey-green, fg 1% py172,10 173,51 1,41 intermediate dyke, felsic remnants, 1% py177,19 178,1 0,91 brecciated intermediate dyke, 40% felsic remnant, 3% py180,00 181,3 1,30 intermediate dyke, 20% felsic remnant, 2% py183,20 183,42 0,22 pinkish-red felsic dyke184,94 185,08 0,14 lost core211,97 215,53 3,56 basaltic komatiite, 35% intermediate-felsic inclusion, foliation 45-60 to CA

DDH Depth

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 7,19 7,19 OB overburden7,19 11,18 3,99 grey-green, fg matrix with mafic phenocryst, weakly fractured, calcite alteration, minor py11,18 12,16 0,98 grey-green carbonates, fg possibly pillowed, weak foliation 30-50 to CA, spiderweb veining

12,16 17,65 5,49Intermediate intrusive, pinkish-brown to greyish-brown, phenocryst, patchy chlorite alteration.

17,65 19,50 1,85grey-green carbonates, fg, pale grey-green, local foliation 45-60 to CA, honey sphalerite, fuschite alteration and 8-10% py

19,50 45,47 25,97Intermediate intrusive, greyish-brown, pinkish, fg matrix with phenocryst, local hematite, calcite and silica alteration

45,47 51,30 5,83 mafic intrusive, dark grey-green, fg massive with felsic fragments, 3-5% scattered cubic py51,30 60,77 9,47 felsic intrusive, pale greyish-brown, fg matrix with mafic phenocryst60,77 63,13 2,36 intermediate intrusive, pale grey-green with pinkish, fg matrix with mafic phenocryst

63,13 66,83 3,70felsic intrusive, pale greyish-brown, fg matrix with mafic phenocryst, calcite and silica alteration

66,83 70,14 3,31 intermediate intrusive, pale grey-green with pinkish, fg matrix with mafic phenocryst

70,14 83,15 13,01felsic intrusive, pinkish brown, fg matrix with few phenocryst, hematite, calcite, feldspar and silica alteration

83,15 87,38 4,23intermediate intrusive, grey-brown, fg matrix with feldpar and mafic phenocryst, hematite, calcite and silica alteration

87,38 94,55 7,17 felsic intrusive, pinkish brown, fg matrix, hematite, calcite, feldspar and silica alteration94,55 99,00 4,45 intermediate intrusive, purplish-brown, fg matrix with mafic phenocryst, silification

99,00 102,26 3,26Talcose Komatiite, green-grey, fg with foliation 20-50 to CA, 10-15% carbonate/talc, soft, 2-3% suphides

102,26 129,13 26,87Intermediate intrusive, greyish-brown, pinkish, fg matrix with phenocryst, local hematite, calcite and silica alteration

129,13 138,06 8,93basaltic komatiite, medium green, fg, possibly pillowed, foliated 20-50 to CA, 5-10% calcite/talc, leucoxene alteration, 2-3% pyrite

138,06 149,70 11,64felsic intrusive, syenite, red-pinkish, fg matrix, hematite, calcite alteration, silicified, very hard, 2-3% py

149,70 153,44 3,74basaltic komatiite, medium green, fg, possibly pillowed, foliated 20-50 to CA, 5-10% calcite/talc, leucoxene alteration, 1-2% pyrite

153,44 168,12 14,68Intermediate intrusive, reddish-brown, fg matrix, local ultramafic inclusions, alteration, 1-2% py

168,12 182,86 14,74basaltics komatiite, pale grey-green, fg, brecciated, 10-15% carbonates/talc, alteration, 1-2% py

182,86 187,06 4,20 intermediate intrusive, green to brownish-green, fg matrix, alteration, hard, 2-3% py

187,06 189,88 2,82basaltics komatiite, pale grey-green, fg, brecciated, 15-20% carbonates/talc, alteration, 1-2% py

189,88 196,63 6,75intermediate intrusive, purplish-brown, fg matrix with mafic phenocryst, silification, 2-3% scattered py

196,63 203,37 6,74 mixed zone, basaltic komatiite and intermediate intrusive, foliation 30-60 to CA, 2-3% py

DDH Depth

203,37 227,96 24,59intermediate intrusive, reddish-brown, fg matrix, local ultramafic inclusions, alteration, hard, weakly magnetic, 2-3% py

227,96 235,80 7,84 basaltic komatiite, grey-green, fg, brecciated, foliation 30-50 to CA, 1-2% py

235,80 238,56 2,76felsic to intermediate intrusive, reddish-brown, fg matrix, phenocryst, calcite alteration, hard, 3-5% py

238,56 250,83 12,27basaltic komatiite, grey-green, fg, brecciated, foliation 15-45 to CA, 1-2% py and leucoxene alteration

EOH

DDH Depth Structure (Intensity 1-5) Veining (%)From To Length Id comments BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW Photo101,41 102,26 shear zone, brecciated125,95 126,08 breccia with 50% ultramafic fragments134,30 134,85 spinifex texture

162,42 166,00brecciated section with 25% ultramafic inclusions

HoleIDSample Number

From (m) To (m) Length (m) Au(g/t) Au(g/t) Check

Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-03 18728 7,19 8,34 1,15 0,000 0,000 0,019C08-03 18729 8,34 8,70 0,36 0,030 0,030 0,030 0,090C08-03 18730 OREAS 14P Batch 8 Aus 0,060 0,060 2,100C08-03 18731 8,70 9,30 0,60 0,010 0,010 0,032C08-03 18732 9,30 9,90 0,60 0,010 0,010 0,026C08-03 18733 10,20 11,18 0,98 0,000 0,000 0,034C08-03 18734 11,18 12,16 0,98 0,010 0,010 0,093C08-03 18735 12,16 13,00 0,84 0,000 0,000 0,021C08-03 18736 13,00 13,82 0,82 0,000 0,000 0,013C08-03 18737 13,82 14,45 0,63 0,000 0,000 0,078C08-03 18738 14,90 15,82 0,92 0,010 0,010 0,030C08-03 18739 15,82 16,60 0,78 0,000 0,000 0,021C08-03 18740 16,60 17,35 0,75 0,000 0,000 0,021C08-03 18741 17,65 18,60 0,95 0,000 0,000 0,064C08-03 18742 18,60 19,50 0,90 0,010 0,010 0,060C08-03 18743 19,50 20,50 1,00 0,000 0,000 0,018C08-03 18744 20,50 21,50 1,00 0,010 0,010 0,010 0,017C08-03 18745 21,50 22,50 1,00 0,010 0,010 0,016C08-03 18746 22,50 23,50 1,00 0,010 0,010 0,012C08-03 18747 23,50 24,50 1,00 0,000 0,000 0,017C08-03 18748 24,50 25,50 1,00 0,000 0,000 0,023C08-03 18749 25,50 26,50 1,00 0,020 0,020 0,018C08-03 18750 26,50 27,50 1,00 0,020 0,020 0,017C08-03 18751 27,50 28,50 1,00 0,010 0,010 0,022C08-03 18752 28,50 29,50 1,00 0,000 0,000 0,034C08-03 18753 QUARTZ Purchased 0,000 0,000 0,001C08-03 18754 29,50 30,50 1,00 0,010 0,010 0,019C08-03 18755 30,50 31,50 1,00 0,010 0,010 0,024C08-03 18756 31,50 32,50 1,00 0,010 0,010 0,010 0,020C08-03 18757 32,50 33,50 1,00 0,010 0,010 0,016C08-03 18758 33,50 34,50 1,00 0,000 0,000 0,020C08-03 18759 34,50 35,50 1,00 0,020 0,010 0,015 0,022C08-03 18760 35,50 36,50 1,00 0,010 0,010 0,020C08-03 18761 36,50 37,50 1,00 0,010 0,010 0,025C08-03 18762 37,50 38,50 1,00 0,020 0,020 0,024C08-03 18763 38,50 39,50 1,00 0,010 0,010 0,020C08-03 18764 39,50 40,50 1,00 0,010 0,010 0,021C08-03 18765 40,50 41,50 1,00 0,010 0,010 0,027C08-03 18766 41,50 42,50 1,00 0,000 0,000 0,013

C08-03 18767 42,50 43,50 1,00 0,010 0,010 0,015C08-03 18768 43,50 44,50 1,00 0,000 0,000 0,021C08-03 18769 44,50 45,47 0,97 0,000 0,000 0,020C08-03 18770 45,47 46,30 0,83 0,000 0,000 0,102C08-03 18771 46,30 47,10 0,80 0,010 0,010 0,065C08-03 18772 OREAS 14P Batch 8 Aus 0,040 0,040 2,080C08-03 18773 47,10 48,00 0,90 0,000 0,000 0,039C08-03 18774 48,00 49,00 1,00 0,050 0,050 0,038C08-03 18775 49,00 49,80 0,80 0,020 0,020 0,035C08-03 18776 49,80 50,60 0,80 0,010 0,010 0,030C08-03 18777 50,60 51,30 0,70 0,000 0,000 0,049C08-03 18778 51,30 52,10 0,80 0,000 0,000 0,019C08-03 18779 52,10 53,00 0,90 0,010 0,010 0,020C08-03 18780 53,00 54,00 1,00 0,000 0,000 0,015C08-03 18781 54,00 55,00 1,00 0,000 0,000 0,012C08-03 18782 55,00 56,00 1,00 0,000 0,000 0,007C08-03 18783 56,00 57,00 1,00 0,040 0,040 0,040 0,008C08-03 18784 57,00 58,00 1,00 0,010 0,010 0,009C08-03 18785 58,00 59,00 1,00 0,010 0,010 0,014C08-03 18786 59,00 59,90 0,90 0,050 0,050 0,013C08-03 18787 59,90 60,77 0,87 0,060 0,060 0,017C08-03 18788 60,77 61,60 0,83 0,010 0,010 0,025C08-03 18789 OREAS 14P Batch 8 Aus 0,060 0,060 2,090C08-03 18790 61,60 62,40 0,80 0,030 0,030 0,021C08-03 18791 62,40 63,13 0,73 0,030 0,030 0,021C08-03 18792 63,13 64,00 0,87 0,000 0,000 0,012C08-03 18793 64,00 65,00 1,00 0,020 0,020 0,010C08-03 18794 65,00 66,00 1,00 0,020 0,020 0,004C08-03 18795 66,00 66,83 0,83 0,000 0,000 0,004C08-03 18796 66,83 67,74 0,91 0,060 0,060 0,013C08-03 18797 67,74 68,19 0,45 0,050 0,050 0,007C08-03 18798 68,19 69,20 1,01 0,000 0,000 0,022C08-03 18799 69,20 70,14 0,94 0,000 0,000 0,019C08-03 18800 70,14 71,00 0,86 0,020 0,020 0,008C08-03 18801 71,00 72,00 1,00 0,020 0,020 0,007C08-03 18802 72,00 73,00 1,00 0,000 0,010 0,005 0,007C08-03 18803 73,00 74,00 1,00 0,010 0,010 0,008C08-03 18804 74,00 75,00 1,00 0,000 0,000 0,008C08-03 18805 75,00 76,00 1,00 0,000 0,000 0,009C08-03 18806 76,00 77,00 1,00 0,020 0,020 0,008C08-03 18807 77,00 78,00 1,00 0,010 0,010 0,008

C08-03 18808 78,00 79,00 1,00 0,050 0,050 0,008C08-03 18809 79,00 80,00 1,00 0,010 0,010 0,009C08-03 18810 80,00 80,64 0,64 0,070 0,090 0,080 0,019C08-03 18811 80,64 81,50 0,86 0,000 0,000 0,010C08-03 18812 81,50 82,30 0,80 0,000 0,000 0,012C08-03 18813 82,30 83,15 0,85 0,010 0,010 0,011C08-03 18814 DIABASE 88.0-88.5 0,000 0,000 0,002C08-03 18815 83,15 84,00 0,85 0,010 0,010 0,002C08-03 18816 84,00 84,90 0,90 0,010 0,010 0,021C08-03 18817 84,90 85,80 0,90 0,010 0,010 0,020C08-03 18818 85,80 86,60 0,80 0,010 0,010 0,022C08-03 18819 86,60 87,38 0,78 0,010 0,010 0,021C08-03 18820 87,38 88,40 1,02 0,000 0,000 0,011C08-03 18821 88,40 89,50 1,10 0,000 0,000 0,010C08-03 18822 89,50 90,50 1,00 0,020 0,000 0,010 0,010C08-03 18823 90,50 91,50 1,00 0,000 0,000 0,010C08-03 18824 91,50 92,50 1,00 0,040 0,040 0,008C08-03 18825 92,50 93,50 1,00 0,020 0,020 0,012C08-03 18826 93,50 94,55 1,05 0,010 0,010 0,010C08-03 18827 94,55 95,40 0,85 0,020 0,020 0,034C08-03 18828 95,40 96,20 0,80 0,010 0,010 0,033C08-03 18829 96,20 97,00 0,80 0,000 0,000 0,036C08-03 18830 97,00 98,00 1,00 0,010 0,010 0,032C08-03 18831 98,00 99,00 1,00 0,000 0,020 0,010 0,032C08-03 18832 99,00 99,98 0,98 0,000 0,000 0,039C08-03 18833 OREAS 14P Batch 8 Aus 0,040 0,040 2,090C08-03 18834 99,98 100,62 0,64 0,010 0,010 0,035C08-03 18835 100,62 101,41 0,79 0,000 0,000 0,032C08-03 18836 101,41 102,26 0,85 0,000 0,000 0,045C08-03 18837 102,26 103,10 0,84 0,000 0,000 0,031C08-03 18838 103,10 104,00 0,90 0,010 0,010 0,031C08-03 18839 104,00 104,90 0,90 0,000 0,000 0,030C08-03 18840 104,90 105,70 0,80 0,000 0,000 0,029C08-03 18841 105,70 106,47 0,77 0,010 0,020 0,015 0,029C08-03 18842 106,47 107,54 1,07 0,000 0,000 0,043C08-03 18843 107,54 108,16 0,62 0,010 0,010 0,024C08-03 18844 108,16 108,63 0,47 0,010 0,000 0,005 0,038C08-03 18845 OREAS 14P Batch 8 Aus 0,080 0,080 2,080C08-03 18846 108,63 109,50 0,87 0,020 0,020 0,027C08-03 18847 109,50 110,30 0,80 0,000 0,000 0,025C08-03 18848 110,30 111,10 0,80 0,000 0,000 0,024

C08-03 18849 111,10 112,00 0,90 0,010 0,010 0,026C08-03 18850 112,00 113,00 1,00 0,000 0,000 0,025C08-03 18851 113,00 114,00 1,00 0,000 0,000 0,021C08-03 18852 114,00 115,00 1,00 0,000 0,000 0,025C08-03 18853 115,00 116,00 1,00 0,010 0,010 0,027C08-03 18854 116,00 117,00 1,00 0,020 0,000 0,010 0,029C08-03 18855 117,00 118,00 1,00 0,010 0,010 0,030C08-03 18856 118,00 119,00 1,00 0,000 0,000 0,027C08-03 18857 119,00 120,00 1,00 0,000 0,000 0,029C08-03 18858 120,00 121,00 1,00 0,000 0,000 0,027C08-03 18859 121,00 122,00 1,00 0,000 0,000 0,024C08-03 18860 122,00 123,00 1,00 0,000 0,000 0,030C08-03 18861 123,00 124,00 1,00 0,000 0,000 0,016C08-03 18862 124,00 125,00 1,00 0,000 0,000 0,017C08-03 18863 125,00 126,08 1,08 0,000 0,000 0,025C08-03 18864 126,08 127,10 1,02 0,010 0,010 0,010 0,026C08-03 18865 127,10 128,10 1,00 0,010 0,010 0,023C08-03 18866 128,10 129,13 1,03 0,000 0,000 0,026C08-03 18867 129,13 130,00 0,87 0,000 0,000 0,046C08-03 18868 130,00 131,00 1,00 0,000 0,000 0,048C08-03 18869 QUARTZ Purchased 0,000 0,000 0,001C08-03 18870 131,00 132,00 1,00 0,000 0,000 0,044C08-03 18871 132,00 133,00 1,00 0,020 0,020 0,040C08-03 18872 133,00 134,00 1,00 0,020 0,020 0,036C08-03 18873 134,00 135,00 1,00 0,010 0,010 0,041C08-03 18874 135,00 136,00 1,00 0,000 0,000 0,040C08-03 18875 136,00 137,00 1,00 0,000 0,000 0,032C08-03 18876 137,00 138,06 1,06 0,000 0,000 0,036C08-03 18877 138,06 139,00 0,94 0,000 0,000 0,011C08-03 18878 139,00 140,00 1,00 0,000 0,000 0,003C08-03 18879 140,00 141,00 1,00 0,010 0,010 0,004C08-03 18880 141,00 142,00 1,00 0,010 0,010 0,018C08-03 18881 142,00 142,97 0,97 0,000 0,000 0,021C08-03 18882 142,97 143,60 0,63 0,010 0,010 0,046C08-03 18883 OREAS 14P Batch 8 Aus 0,080 0,080 2,100C08-03 18884 143,60 144,20 0,60 0,000 0,000 0,052C08-03 18885 144,20 144,82 0,62 0,000 0,000 0,021C08-03 18886 144,82 145,55 0,73 0,010 0,010 0,017C08-03 18887 145,55 146,30 0,75 0,000 0,000 0,017C08-03 18888 146,30 147,13 0,83 0,010 0,000 0,005 0,043C08-03 18889 147,13 148,00 0,87 0,000 0,000 0,005

C08-03 18890 148,00 148,90 0,90 0,010 0,010 0,004C08-03 18891 148,90 149,70 0,80 0,010 0,010 0,003C08-03 18892 149,70 150,83 1,13 0,010 0,010 0,040C08-03 18893 150,83 151,59 0,76 0,010 0,010 0,022C08-03 18894 151,59 152,45 0,86 0,000 0,000 0,051C08-03 18895 152,45 153,44 0,99 0,000 0,000 0,046C08-03 18896 153,44 154,50 1,06 0,000 0,000 0,030C08-03 18897 154,50 155,50 1,00 0,010 0,010 0,010 0,034C08-03 18898 155,50 156,44 0,94 0,010 0,010 0,026C08-03 18899 156,44 157,15 0,71 0,010 0,010 0,048C08-03 18900 157,15 157,88 0,73 0,000 0,000 0,048C08-03 18901 157,88 158,60 0,72 0,000 0,000 0,025C08-03 18902 158,60 159,60 1,00 0,000 0,000 0,022C08-03 18903 159,60 160,50 0,90 0,000 0,000 0,020C08-03 18904 160,50 161,50 1,00 0,000 0,000 0,013C08-03 18905 161,50 162,42 0,92 0,000 0,000 0,000 0,021C08-03 18906 162,42 163,30 0,88 0,000 0,000 0,016C08-03 18907 163,30 164,20 0,90 0,000 0,000 0,021C08-03 18908 OREAS 14P Batch 8 Aus 0,070 0,070 2,100C08-03 18909 164,20 165,10 0,90 0,010 0,010 0,014C08-03 18910 165,10 166,00 0,90 0,010 0,010 0,011C08-03 18911 166,00 166,61 0,61 0,000 0,000 0,043C08-03 18912 166,61 167,40 0,79 0,010 0,010 0,010 0,020C08-03 18913 167,40 168,12 0,72 0,010 0,010 0,019C08-03 18914 168,12 169,10 0,98 0,010 0,010 0,046C08-03 18915 169,10 170,10 1,00 0,010 0,010 0,066C08-03 18916 170,10 171,10 1,00 0,010 0,010 0,055C08-03 18917 171,10 172,10 1,00 0,000 0,000 0,060C08-03 18918 172,10 172,80 0,70 0,000 0,000 0,012C08-03 18919 172,80 173,51 0,71 0,000 0,010 0,005 0,011C08-03 18920 173,51 174,40 0,89 0,010 0,010 0,049C08-03 18921 174,40 175,30 0,90 0,010 0,010 0,059C08-03 18922 175,30 176,20 0,90 0,000 0,000 0,062C08-03 18923 176,20 177,19 0,99 0,010 0,010 0,056C08-03 18924 DIABASE 88.5-89.0 0,000 0,000 0,003C08-03 18925 177,19 178,10 0,91 0,040 0,010 0,025 0,015C08-03 18926 178,10 179,00 0,90 0,010 0,010 0,052C08-03 18927 179,00 180,00 1,00 0,010 0,010 0,047C08-03 18928 180,00 180,60 0,60 0,000 0,000 0,015C08-03 18929 180,60 181,30 0,70 0,000 0,000 0,009C08-03 18930 181,30 182,05 0,75 0,000 0,000 0,049

C08-03 18931 182,05 182,86 0,81 0,000 0,000 0,047C08-03 18932 182,86 183,90 1,04 0,000 0,000 0,012C08-03 18933 183,90 184,94 1,04 0,000 0,000 0,000 0,011C08-03 18934 185,08 186,05 0,97 0,000 0,000 0,011C08-03 18935 186,05 187,06 1,01 0,000 0,000 0,012C08-03 18936 187,06 188,00 0,94 0,000 0,000 0,045C08-03 18937 188,00 189,00 1,00 0,000 0,000 0,056C08-03 18938 189,00 189,88 0,88 0,000 0,000 0,049C08-03 18939 189,88 190,90 1,02 0,000 0,000 0,000 0,010C08-03 18940 190,90 192,00 1,10 0,010 0,010 0,006C08-03 18941 192,00 193,00 1,00 0,000 0,000 0,017C08-03 18942 193,00 194,00 1,00 0,000 0,000 0,007C08-03 18943 194,00 195,00 1,00 0,010 0,010 0,010C08-03 18944 195,00 195,80 0,80 0,010 0,010 0,004C08-03 18945 195,80 196,63 0,83 0,000 0,000 0,000 0,005C08-03 18946 196,63 197,44 0,81 0,010 0,010 0,027C08-03 18947 197,44 198,36 0,92 0,010 0,010 0,033C08-03 18948 198,36 199,22 0,86 0,010 0,010 0,034C08-03 18949 199,22 200,07 0,85 0,000 0,000 0,032C08-03 18950 200,07 201,00 0,93 0,010 0,010 0,017C08-03 18951 201,00 201,83 0,83 0,000 0,000 0,018C08-03 18952 201,83 202,64 0,81 0,000 0,000 0,038C08-03 18953 OREAS 14P Batch 8 Aus 0,050 0,050 2,120C08-03 18954 202,64 203,37 0,73 0,000 0,000 0,027C08-03 18955 203,37 204,30 0,93 0,000 0,010 0,005 0,023C08-03 18956 204,30 205,20 0,90 0,000 0,000 0,024C08-03 18957 205,20 206,10 0,90 0,000 0,000 0,027C08-03 18958 206,10 207,00 0,90 0,000 0,000 0,022C08-03 18959 207,00 207,97 0,97 0,000 0,000 0,025C08-03 18960 207,97 209,00 1,03 0,010 0,010 0,019C08-03 18961 209,00 210,00 1,00 0,020 0,020 0,027C08-03 18962 210,00 211,00 1,00 0,000 0,000 0,023C08-03 18963 211,00 211,97 0,97 0,010 0,010 0,022C08-03 18964 211,97 212,80 0,83 0,030 0,000 0,015 0,018C08-03 18965 212,80 213,56 0,76 0,040 0,040 0,022C08-03 18966 213,56 214,50 0,94 0,010 0,010 0,030C08-03 18967 OREAS 14P Batch 8 Aus 0,070 0,070 2,100C08-03 18968 214,50 215,53 1,03 0,010 0,010 0,030C08-03 18969 215,53 216,40 0,87 0,020 0,020 0,024C08-03 18970 216,40 217,30 0,90 0,010 0,010 0,025C08-03 18971 217,30 217,83 0,53 0,020 0,020 0,030

C08-03 18972 217,83 218,70 0,87 0,000 0,000 0,012C08-03 18973 218,70 219,60 0,90 0,040 0,040 0,012C08-03 18974 219,60 220,50 0,90 0,020 0,020 0,010C08-03 18975 220,50 221,50 1,00 0,000 0,000 0,009C08-03 18976 221,50 222,50 1,00 0,000 0,000 0,020C08-03 18977 222,50 223,50 1,00 0,010 0,010 0,010C08-03 18978 223,50 224,50 1,00 0,000 0,000 0,000 0,013C08-03 18979 224,50 225,04 0,54 0,000 0,000 0,038C08-03 18980 225,04 226,00 0,96 0,010 0,010 0,012C08-03 18981 226,00 227,00 1,00 0,000 0,000 0,013C08-03 18982 227,00 227,96 0,96 0,000 0,000 0,011C08-03 18983 227,96 228,55 0,59 0,020 0,020 0,020 0,040C08-03 18984 228,55 229,15 0,60 0,000 0,000 0,029C08-03 18985 229,15 229,90 0,75 0,000 0,000 0,020C08-03 18986 229,90 230,90 1,00 0,010 0,010 0,034C08-03 18987 230,90 231,90 1,00 0,000 0,000 0,034C08-03 18988 QUARTZ Purchased 0,000 0,000 0,001C08-03 18989 231,90 232,90 1,00 0,000 0,000 0,039C08-03 18990 232,90 233,90 1,00 0,010 0,010 0,026C08-03 18991 233,90 234,90 1,00 0,000 0,000 0,026C08-03 18992 234,90 235,80 0,90 0,000 0,000 0,026C08-03 18993 235,80 236,48 0,68 0,000 0,000 0,014C08-03 18994 236,48 237,00 0,52 0,000 0,000 0,043C08-03 18995 237,00 237,80 0,80 0,000 0,000 0,017C08-03 18996 237,80 238,56 0,76 0,000 0,000 0,007C08-03 18997 238,56 239,40 0,84 0,000 0,000 0,040C08-03 18998 239,40 240,20 0,80 0,010 0,010 0,037C08-03 18999 240,20 241,00 0,80 0,000 0,000 0,030C08-03 19000 241,00 242,00 1,00 0,000 0,000 0,032C08-03 19001 242,00 243,00 1,00 0,000 0,000 0,037C08-03 19002 243,00 244,00 1,00 0,030 0,030 0,044C08-03 19003 244,00 245,00 1,00 0,020 0,020 0,041C08-03 19004 OREAS 14P Batch 8 Aus 0,050 0,050 2,110C08-03 19005 245,00 246,00 1,00 0,000 0,000 0,038C08-03 19006 246,00 247,00 1,00 0,020 0,020 0,049C08-03 19007 247,00 248,00 1,00 0,000 0,010 0,005 0,056C08-03 19008 248,00 249,00 1,00 0,000 0,000 0,034C08-03 19009 249,00 250,00 1,00 0,000 0,000 0,040C08-03 19010 250,00 250,83 0,83 0,000 0,000 0,041


7,19 8 0,81 0,81 100% 0,45 56%8 11 3 2,7 90% 1,26 42%11 14 3 2,92 97% 2,43 81%14 17 3 2,55 85% 1,67 56%17 20 3 2,7 90% 2,65 88%20 23 3 3,05 102% 2,47 82%23 26 3 3,08 103% 2,82 94%26 29 3 2,96 99% 2,64 88%29 32 3 3,01 100% 2,67 89%32 35 3 2,98 99% 2,95 98%35 38 3 3,06 102% 2,64 88%38 41 3 3 100% 2,48 83%41 44 3 2,94 98% 2,18 73%44 47 3 3 100% 1,11 37%47 50 3 3 100% 1,25 42%50 53 3 3 100% 0,97 32%53 56 3 3,1 103% 2,1 70%56 59 3 3,04 101% 2,54 85%59 62 3 2,99 100% 2,92 97%62 65 3 2,98 99% 2,37 79%65 68 3 3,00 100% 2,53 84%68 71 3 3,04 101% 2,79 93%71 74 3 2,97 99% 2,87 96%74 77 3 2,98 99% 2,60 87%77 80 3 3,00 100% 2,88 96%80 83 3 3,00 100% 2,35 78%83 86 3 2,99 100% 2,55 85%86 89 3 3,01 100% 2,66 89%89 92 3 2,97 99% 2,48 83%92 95 3 3,03 101% 2,08 69%95 98 3 2,95 98% 2,83 94%98 101 3 3,00 100% 2,58 86%101 104 3 2,95 98% 2,78 93%104 107 3 3,04 101% 2,83 94%107 110 3 3,02 101% 2,75 92%110 113 3 3,03 101% 2,81 94%113 116 3 3,00 100% 2,73 91%116 119 3 3,03 101% 2,81 94%119 122 3 2,99 100% 1,78 59%122 125 3 3,01 100% 2,73 91%125 128 3 2,94 98% 2,65 88%128 131 3 3,09 103% 2,90 97%131 134 3 2,93 98% 3 100%

134 137 3 3,00 100% 2,73 91%137 140 3 3,07 102% 1,79 60%140 143 3 2,95 98% 2,69 90%143 146 3 3,08 103% 2,96 99%146 149 3 2,97 99% 2,04 68%149 152 3 2,98 99% 2,75 92%152 155 3 2,97 99% 2,75 92%155 158 3 3,06 102% 2,8 93%158 161 3 3,03 101% 2,97 99%161 164 3 2,97 99% 2,85 95%164 167 3 2,94 98% 2,75 92%167 170 3 3,06 102% 2,57 86%170 173 3 3,03 101% 2,69 90%173 176 3 2,94 98% 2,86 95%176 179 3 2,95 98% 3,00 100%179 182 3 3,00 100% 2,91 97%182 185 3 2,86 95% 3,00 100%185 188 3 2,99 100% 2,73 91%188 191 3 2,98 99% 3,00 100%191 194 3 3,02 101% 2,88 96%194 197 3 2,99 100% 2,71 90%197 200 3 2,93 98% 2,92 97%200 203 3 3,06 102% 3,00 100%203 206 3 2,92 97% 2,76 92%206 209 3 2,96 99% 2,86 95%209 212 3 3,03 101% 2,98 99%212 215 3 3,00 100% 2,90 97%215 218 3 2,97 99% 2,91 97%218 221 3 3,00 100% 2,93 98%221 224 3 3,04 101% 2,76 92%224 227 3 2,90 97% 2,96 99%227 230 3 3,03 101% 2,86 95%230 233 3 2,93 98% 2,97 99%233 236 3 2,97 99% 2,98 99%236 239 3 2,96 99% 2,96 99%239 242 3 2,93 98% 3 100%242 245 3 3,05 102% 3,00 100%245 248 3 3,12 104% 2,79 93%248 251 3 2,97 99% 3,00 100%


C08-04 L-200E 475N 250 0 -50 250m 14-juil-08 22-juil-08

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 3,90 3,90 OB overburden3,90 17,30 13,40 felsic intrusive, pale grey-green, fg matrix, silicified

17,30 27,89 10,59felsic to intermediate intrusive, pale purplish-grey, fg matrix with mafic phenocryst, brecciated

27,89 63,13 35,24intermediate intrusive, greenish-brown, fg matrix with mafic phenocryst, alteration, hard, minor py

63,13 101,02 37,89basaltic komatiite, pale grey-green, fg, pillowed, 5-10% carbonate/talc, magnetic

101,02 106,24 5,22 mafic intrusive, medium green, hard

106,24 119,91 13,67intermediate intrusive, pinkish-brown, fg matrix, alteration, hard, 2-3% py

119,91 130,76 10,85basaltic komatiite, medium green, possibly pillowed, 10-15% carbonate/talc, alteration

130,76 135,89 5,13intermediate intrusive, pinkish-brown, fg matrix, alteration, hard, 1-2% py

135,89 138,34 2,45basaltic komatiite, pale grey-green, fg, pillowed, 5-10% carbonate/talc, magnetic, leucoxene alteration

138,34 143,02 4,68felsic intrusive, reddish-brown, fg matrix with mafic phenocryst, hematite, calcite, silica alteration, 3-5% py

143,02 149,95 6,93intermediate intrusive, pinkish-brown, fg matrix, hematite and calcite alteration, hard, 2-3% py

149,95 154 4,05Talcose komatiite, grey, fg matrix, foliation 15-60 to CA, 20-30% talc/carbonate, magnetic, 2-3% cubic py

154,00 162,33 8,33basaltic komatiite, pale grey-green, fg, pillowed, foliation 20-70 to CA, 10-15% carbonate/talc, non-magnetic, 1-2% py

162,33 163,6 1,27intermediate dyke, pale reddish-brown, fg matrix with mafic phenocryst, hematite and calcite alteration, hard, 1% py

163,60 165,09 1,49mafic volcanics, pale grey-green, fg, 10% mafic and felsic fragments, irregular bedding 50-70 to CA, breccia, 1% py

165,09 166,78 1,69felsic intrusive, pink-brown, fg matrix with large 3-8 mm feldspar phenocryst, silicified, very hard, 8-10% cubic py

166,78 167,79 1,01intermediate intrusive, greyish-brown, fg matrix with ghost feldspar phenocryst, calcite alteration, hard

167,79 170,19 2,40Felsic intrusive, pink-brown, fg matrix with large 3-8 mm feldspar phenocryst, silicified, very hard, 5-8% cubic py

170,19 172,16 1,97

Intermediate dyke, purplish-brown, fg matrix with ghost feldspar phenocryst, 5% irregular, calcite stringers, calcite alteration, hard, 3% disseminated py

172,16 173,42 1,26Felsic intrusive, pinkish-red, fg matrix with feldspar phenocryst (3-8mm) silicified, very hard, 5% scattered py

173,42 176,57 3,15Intermediate intrusive, reddish/pinkish/purplish-brown, fg matrix, hematite and calcite alteration, hard, 1-2% py

DDH Depth

176,57 177,47 0,90

Felsic intrusive, pale brownish-pink, fg matrix with coarse feldspar phenocryst (2-5mm) 45% qtz-calcite veining, silicified, very hard, 8% scattered py

177,47 179,52 2,05

Bleached mafic volcanics, pale brown, yellow/green/pink-buff, aphanitic to fg, brecciated, 5-10% qtz-calcite stringers, sericite and calcite alteration, silicification, hard, 10-15% scattered py

179,52 188,6 9,08intermediate intrusive, greyish-brown, fg matrix with ghost feldspar phenocryst, calcite alteration, hard

188,60 190,52 1,92felsic intrusive, pale pinkish-brown, fg matrix with coarse fds phenocryst, silicified, very hard, 5% scattered py

190,52 194,99 4,47

intermediate to mafic intrusive, purplish brown, local reddish, fg matrix with mafic and fds phenocryst, calcite, hematite and chlorite alteration, hard

194,99 195,87 0,88Felsic intrusive, pinkish buff, fg matrix with coarse fds phenocryst, silicified, very hard, 5% py

195,87 197,41 1,54Intermediate intrusive, reddish/pinkish/purplish-brown, fg matrix, hematite and calcite alteration, hard

197,41 198,91 1,50felsic intrusive, pale pinkish-brown, fg matrix with coarse fds phenocryst, silicified, very hard, 5% scattered py

198,91 201,74 2,83

Bleached mafic volcanics, pale brown, yellow/green/pink-buff, aphanitic to fg, brecciated, 5% qtz-calcite stringers, sericite and calcite alteration, silicification, hard, 5-8% scattered py, irregular bedding (15-40 to CA)

201,74 202,42 0,68Intermediate intrusive, pale purplish-grey, fg matrix with mafic phenocryst, calcite alteration, hard, 5% py

202,42 209,7 7,28

Altered mafic volcanics, pale grey-green, green/pink buff, aphanitic to fg, irregular bedding (5-30 to CA), brecciated, feldsparization, hard, 3-5% py

209,70 214,19 4,49intermediate intrusive, pale pinkish-brown, fg matrix with mafic and ghost fds phenocryst, foliation (20-40 to CA) hard, 2-3% py

214,19 217,62 3,43

altered mafic volcanics, pale grey-green, green/pink buff, aphanitic to fg, irregular bedding (10-40 to CA), brecciated, feldsparization, hard, tuff

217,62 223,92 6,30felsic intrusive, pink to pinkish buff, fg matrix with coarse fds phenocryst, brecciated, silicified, very hard, 3-5% py

223,92 233,79 9,87mafic to intermediate intrusive, grey-green, fg matrix with phenocryst, calcite and hematite alteration, hard

233,79 237,05 3,26intermediate intrusive, pale pinkish-brown, fg matrix with mafic and ghost fds phenocryst, hard, 3-5% py

237,05 244 6,95Altered mafic volcanics, grey-green, aphanitic to fg, brecciated, 5-10% stringers, sericite alteration and silification, hard, 5-8% py

244,00 250,4 6,40felsic intrusive, grey, green, fg matrix with coarse fds phenocryst, silicified, very hard, 3-5% scattered py

EOH

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments3,90 5,15 1,25 felsic dyke, pale purplish-grey41,47 42,28 0,81 basaltics komatiite, pale grey-green, fg, foliation 30-60 to CA42,28 42,55 0,27 numerous mafic and feldspar phenocryst42,55 43,48 0,93 basaltics komatiite, pale grey-green, fg, foliation 25-50 to CA

73,75 77,78 4,03felsic to intermediate dyke, reddish-brown, fg matrix, silification, hard, 3-5% py

105,38 105,69 0,31 intermediate dyke, pale pinkish-brown, 8% py

147,87 149,53 1,66basaltic komatiite, medium green, fg matrix, breccia, 5% carbonate veining, 3% py

181,68 182,15 0,47Pink feldspar porphyry, coarse feldspar phenocryst, 5% qtz-calcite stringers, 5% pyrite

188,04 188,17 0,13 idem with 3% pyrite192,32 192,77 0,45 idem with 8% py193,34 193,80 0,46 idem with 3% pyrite194,29 194,4 0,11 pinkish-brown intermediate dyke

202,60 204,40 1,80mafic dyke, medium green, fg, lineation 5-30 to CA, calcite alteration

215,16 216,14 0,98 intermediate tuff, foliated, 2% py

216,14 216,66 0,52intermediate dyke, pale pinkish-brown, fg matrix with phenocryst, lineation (30-50 to CA) 3% py

216,66 217,62 0,9635% felsic fragments and inclusions, strongly brecciated, 15% irregular veining, 5% py

218,80 219,6 0,80 brecciated section, with chlorite, 25% irregular, mafic volcanics, inclusion

220,34 221,19 0,85mafic volcanics inclusion, medium green, fg, irregular foliation (5-30 to CA), 15% felsic fragments, 1% py

223,92 226,45 2,53intermediate intrusive, 15-20% inclusions, foliation (40-60 to CA), chlorite, 2-3% py

226,45 227,14 0,69 mafic intrusive, grey-green, rare phenocryst

227,14 228,37 1,23intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, lineation 40-50 to CA, calcite alteration, 2-3% py

228,37 231,67 3,30mafic to intermediate section with 15-20% felsic fragments, 1-2 % py

230,24 230,55 0,31 orange-red aplite dyke, 1% py

231,67 232,53 0,86intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, hematite and calcite alteration,

232,53 233,79 1,26mafic dyke, grey green, phenocryst, 5% intermediate remnants, 3% stringers, 1% py

248,96 249,83 0,87mafic volcanics inclusion, medium green, fg, 10% felsic fragments, 2% py

DDH Depth

249,83 -249,83

DDH Depth Structure (Intensity 1-5) Veining (%)From To Length Id comments BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW Photo52,17 52,34 SZ65,95 66,20 strong breccia with 10% gouge66,20 66,62 spinifex texture77,78 78,10 irregular foliation, 20-45 to CA

113,45 119,9135% fragment and irregular foliation 50-70 to CA

HoleIDSample Number

From (m) To (m) Length (m) Au(g/t) Au(g/t) CheckAu(g/t) Average

Ni (%) Ni (%) CheckNi(%) Average

C08-04 19011 3,90 4,50 0,60 0,000 0,000 0,010C08-04 19012 4,50 5,15 0,65 0,000 0,000 0,012C08-04 19013 5,15 6,00 0,85 0,000 0,000 0,010C08-04 19014 6,00 7,00 1,00 0,000 0,000 0,009C08-04 19015 7,00 8,00 1,00 0,010 0,010 0,012C08-04 19016 8,00 9,00 1,00 0,010 0,010 0,029C08-04 19017 9,00 10,00 1,00 0,000 0,000 0,015C08-04 19018 10,00 11,00 1,00 0,010 0,010 0,010 0,015C08-04 19019 11,00 12,00 1,00 0,000 0,000 0,014C08-04 19020 12,00 13,00 1,00 0,000 0,000 0,014C08-04 19021 13,00 14,00 1,00 0,050 0,050 0,013C08-04 19022 14,00 14,90 0,90 0,010 0,010 0,014C08-04 19023 14,90 15,70 0,80 0,010 0,010 0,012C08-04 19024 15,70 16,50 0,80 0,000 0,000 0,013C08-04 19025 16,50 17,30 0,80 0,000 0,000 0,012C08-04 19026 17,30 18,07 0,77 0,000 0,000 0,011C08-04 19027 18,07 19,00 0,93 0,010 0,010 0,010C08-04 19028 19,00 20,00 1,00 0,010 0,000 0,005 0,012C08-04 19029 OREAS 14P Batch 8 Aus 0,030 0,030 2,090C08-04 19030 20,00 21,00 1,00 0,000 0,000 0,017C08-04 19031 21,00 22,00 1,00 0,000 0,000 0,013C08-04 19032 22,00 23,00 1,00 0,000 0,000 0,015C08-04 19033 23,00 24,00 1,00 0,000 0,000 0,019C08-04 19034 24,00 25,00 1,00 0,000 0,000 0,011C08-04 19035 25,00 26,00 1,00 0,000 0,000 0,014C08-04 19036 26,00 27,00 1,00 0,000 0,000 0,013C08-04 19037 27,00 27,89 0,89 0,000 0,000 0,019C08-04 19038 27,89 28,47 0,58 0,000 0,000 0,000 0,033C08-04 19039 28,47 29,50 1,03 0,000 0,000 0,025C08-04 19040 29,50 30,50 1,00 0,000 0,000 0,020C08-04 19041 30,50 31,50 1,00 0,000 0,000 0,021C08-04 19042 31,50 32,50 1,00 0,000 0,000 0,019C08-04 19043 32,50 33,50 1,00 0,000 0,000 0,018C08-04 19044 DIABASE 88.5-89.0 0,010 0,020 0,015 0,003C08-04 19045 33,50 34,50 1,00 0,000 0,000 0,020C08-04 19046 34,50 35,50 1,00 0,000 0,000 0,000 0,019C08-04 19047 35,50 36,50 1,00 0,000 0,000 0,026C08-04 19048 36,50 37,50 1,00 0,000 0,000 0,020C08-04 19049 37,50 38,50 1,00 0,000 0,000 0,020C08-04 19050 38,50 39,50 1,00 0,020 0,010 0,015 0,021C08-04 19051 39,50 40,50 1,00 0,000 0,000 0,024

C08-04 19052 40,50 41,47 0,97 0,000 0,000 0,025C08-04 19053 41,47 42,28 0,81 0,010 0,010 0,047C08-04 19054 42,28 42,90 0,62 0,000 0,000 0,033C08-04 19055 42,90 43,48 0,58 0,000 0,000 0,042C08-04 19056 43,48 44,30 0,82 0,000 0,000 0,028C08-04 19057 44,30 45,10 0,80 0,000 0,000 0,000 0,021C08-04 19058 45,10 46,00 0,90 0,000 0,000 0,020C08-04 19059 46,00 47,00 1,00 0,010 0,010 0,016C08-04 19060 47,00 48,00 1,00 0,010 0,010 0,018C08-04 19061 48,00 49,00 1,00 0,010 0,010 0,020C08-04 19062 49,00 50,00 1,00 0,010 0,010 0,012C08-04 19063 50,00 51,00 1,00 0,010 0,010 0,012C08-04 19064 51,00 52,00 1,00 0,010 0,010 0,015C08-04 19065 52,00 53,00 1,00 0,000 0,000 0,017C08-04 19066 53,00 54,00 1,00 0,010 0,010 0,013C08-04 19067 54,00 55,00 1,00 0,000 0,000 0,012C08-04 19068 55,00 56,00 1,00 0,010 0,010 0,012C08-04 19069 56,00 57,00 1,00 0,000 0,000 0,010C08-04 19070 57,00 58,00 1,00 0,010 0,010 0,012C08-04 19071 OREAS 14P Batch 8 Aus 0,060 0,060 2,110C08-04 19072 58,00 59,00 1,00 0,000 0,000 0,012C08-04 19073 59,00 60,00 1,00 0,010 0,010 0,023C08-04 19074 60,00 61,00 1,00 0,000 0,000 0,027C08-04 19075 61,00 62,00 1,00 0,010 0,010 0,028C08-04 19076 62,00 63,13 1,13 0,020 0,020 0,040C08-04 19077 63,13 64,00 0,87 0,010 0,010 0,053C08-04 19078 64,00 65,00 1,00 0,010 0,010 0,054C08-04 19079 65,00 66,00 1,00 0,000 0,010 0,005 0,042C08-04 19080 66,00 67,00 1,00 0,010 0,010 0,043C08-04 19081 67,00 68,00 1,00 0,000 0,000 0,049C08-04 19082 68,00 69,00 1,00 0,010 0,010 0,048C08-04 19083 69,00 70,00 1,00 0,010 0,010 0,047C08-04 19084 70,00 71,00 1,00 0,000 0,000 0,051C08-04 19085 71,00 72,00 1,00 0,010 0,010 0,054C08-04 19086 72,00 72,90 0,90 0,010 0,010 0,055C08-04 19087 72,90 73,75 0,85 0,010 0,010 0,057C08-04 19088 73,75 74,75 1,00 0,020 0,010 0,015 0,005C08-04 19089 74,75 75,75 1,00 0,010 0,010 0,005C08-04 19090 75,75 76,75 1,00 0,010 0,010 0,010 0,032C08-04 19091 76,75 77,78 1,03 0,010 0,010 0,031C08-04 19092 77,78 78,60 0,82 0,030 0,050 0,040 0,057C08-04 19093 78,60 79,40 0,80 0,010 0,010 0,050C08-04 19094 79,40 80,20 0,80 0,020 0,020 0,060

C08-04 19095 80,20 81,00 0,80 0,030 0,030 0,063C08-04 19096 OREAS 14P Batch 8 Aus 0,080 0,080 2,110C08-04 19097 81,00 82,00 1,00 0,000 0,000 0,063C08-04 19098 82,00 83,00 1,00 0,010 0,010 0,058C08-04 19099 83,00 84,00 1,00 0,030 0,010 0,020 0,056C08-04 19100 84,00 85,00 1,00 0,010 0,010 0,067C08-04 19101 85,00 86,00 1,00 0,010 0,010 0,071C08-04 19102 86,00 87,00 1,00 0,020 0,020 0,054C08-04 19103 87,00 88,00 1,00 0,010 0,010 0,059C08-04 19104 88,00 89,00 1,00 0,010 0,010 0,054C08-04 19105 89,00 90,00 1,00 0,010 0,010 0,059C08-04 19106 QUARTZ Purchased 0,000 0,000 0,001C08-04 19107 90,00 91,00 1,00 0,000 0,000 0,063C08-04 19108 91,00 92,00 1,00 0,000 0,000 0,058C08-04 19109 92,00 93,00 1,00 0,000 0,000 0,058C08-04 19110 93,00 94,00 1,00 0,000 0,000 0,068C08-04 19111 94,00 95,00 1,00 0,020 0,020 0,073C08-04 19112 95,00 96,00 1,00 0,010 0,010 0,060C08-04 19113 96,00 97,00 1,00 0,000 0,000 0,061C08-04 19114 97,00 98,00 1,00 0,000 0,000 0,064C08-04 19115 98,00 99,00 1,00 0,010 0,010 0,059C08-04 19116 99,00 100,00 1,00 0,000 0,000 0,058C08-04 19117 100,00 101,02 1,02 0,000 0,000 0,064C08-04 19118 101,02 102,00 0,98 0,010 0,010 0,059C08-04 19119 102,00 103,00 1,00 0,010 0,010 0,069C08-04 19120 103,00 103,80 0,80 0,000 0,000 0,074C08-04 19121 103,80 104,60 0,80 0,000 0,000 0,078C08-04 19122 104,60 105,38 0,78 0,000 0,000 0,077C08-04 19123 105,38 106,24 0,86 0,010 0,010 0,055C08-04 19124 106,24 107,10 0,86 0,010 0,010 0,026C08-04 19125 107,10 108,00 0,90 0,000 0,000 0,000 0,027C08-04 19126 108,00 109,00 1,00 0,000 0,000 0,017C08-04 19127 109,00 110,00 1,00 0,000 0,000 0,034C08-04 19128 OREAS 14P Batch 8 Aus 0,060 0,060 2,100C08-04 19129 110,00 111,00 1,00 0,010 0,010 0,015C08-04 19130 111,00 112,00 1,00 0,010 0,010 0,018C08-04 19131 112,00 113,00 1,00 0,010 0,010 0,016C08-04 19132 113,00 114,00 1,00 0,000 0,000 0,009C08-04 19133 114,00 115,00 1,00 0,010 0,010 0,015C08-04 19134 115,00 116,00 1,00 0,010 0,010 0,010 0,016C08-04 19135 116,00 117,00 1,00 0,020 0,020 0,029C08-04 19136 117,00 118,00 1,00 0,000 0,000 0,038C08-04 19137 118,00 119,00 1,00 0,010 0,010 0,008

C08-04 19138 119,00 119,91 0,91 0,000 0,000 0,020C08-04 19139 119,91 120,60 0,69 0,000 0,000 0,031C08-04 19140 120,60 121,18 0,58 0,000 0,000 0,011C08-04 19141 121,18 122,15 0,97 0,000 0,000 0,043C08-04 19142 122,15 123,16 1,01 0,000 0,000 0,044C08-04 19143 123,16 124,05 0,89 0,010 0,010 0,022C08-04 19144 124,30 125,30 1,00 0,000 0,000 0,000 0,033C08-04 19145 OREAS 14P Batch 8 Aus 0,040 0,040 2,090C08-04 19146 125,30 126,20 0,90 0,000 0,000 0,056C08-04 19147 126,20 127,10 0,90 0,010 0,010 0,057C08-04 19148 127,10 128,00 0,90 0,000 0,000 0,064C08-04 19149 128,00 128,90 0,90 0,000 0,000 0,053C08-04 19150 128,90 129,80 0,90 0,000 0,000 0,062C08-04 19151 129,80 130,76 0,96 0,010 0,010 0,068C08-04 19152 130,76 131,80 1,04 0,020 0,020 0,018C08-04 19153 131,80 132,80 1,00 0,010 0,010 0,040C08-04 19154 132,80 133,80 1,00 0,010 0,010 0,022C08-04 19155 133,80 134,80 1,00 0,000 0,000 0,020C08-04 19156 134,80 135,89 1,09 0,000 0,000 0,018C08-04 19157 135,89 136,70 0,81 0,000 0,010 0,005 0,066C08-04 19158 136,70 137,50 0,80 0,000 0,000 0,067C08-04 19159 137,50 138,34 0,84 0,000 0,000 0,051C08-04 19160 138,34 139,30 0,96 0,010 0,010 0,009C08-04 19161 139,30 140,20 0,90 0,010 0,010 0,006C08-04 19162 140,20 141,10 0,90 0,000 0,000 0,004C08-04 19163 141,10 142,00 0,90 0,000 0,000 0,011C08-04 19164 142,00 143,02 1,02 0,000 0,000 0,025C08-04 19165 143,02 144,00 0,98 0,000 0,000 0,000 0,011C08-04 19166 144,00 145,00 1,00 0,000 0,000 0,013C08-04 19167 145,00 146,00 1,00 0,000 0,000 0,017C08-04 19168 146,00 147,00 1,00 0,000 0,000 0,029C08-04 19169 147,00 147,87 0,87 0,000 0,000 0,025C08-04 19170 147,87 148,80 0,93 0,000 0,000 0,048C08-04 19171 DIABASE 89.0-89.5 0,000 0,000 0,005C08-04 19172 148,80 149,53 0,73 0,000 0,000 0,046C08-04 19173 149,53 149,95 0,42 0,000 0,000 0,027C08-04 19174 149,95 151,00 1,05 0,000 0,000 0,048C08-04 19175 151,00 152,00 1,00 0,020 0,020 0,043C08-04 19176 152,00 153,00 1,00 0,050 0,130 0,090 0,019C08-04 19177 153,00 154,00 1,00 0,010 0,010 0,033C08-04 19178 154,00 155,00 1,00 0,000 0,000 0,036C08-04 19179 155,00 156,00 1,00 0,010 0,010 0,038C08-04 19180 156,00 157,00 1,00 0,010 0,010 0,048

C08-04 19181 157,00 158,00 1,00 0,020 0,020 0,045C08-04 19182 158,00 159,00 1,00 0,020 0,020 0,036C08-04 19183 159,00 159,90 0,90 0,020 0,020 0,032C08-04 19184 159,90 160,70 0,80 0,030 0,010 0,020 0,044C08-04 19185 160,70 161,50 0,80 0,010 0,010 0,038C08-04 19186 161,50 162,33 0,83 0,010 0,010 0,036C08-04 19187 162,33 163,00 0,67 0,010 0,010 0,008C08-04 19188 163,00 163,60 0,60 0,010 0,010 0,007C08-04 19189 163,60 164,30 0,70 0,020 0,020 0,010C08-04 19190 164,30 165,09 0,79 0,020 0,020 0,011C08-04 19191 165,09 165,75 0,66 0,000 0,000 0,003C08-04 19192 OREAS 14P Batch 8 Aus 0,060 0,060 2,090C08-04 19193 165,75 166,78 1,03 0,030 0,030 0,011C08-04 19194 166,78 167,79 1,01 0,020 0,020 0,018C08-04 19195 167,79 168,60 0,81 0,010 0,010 0,008C08-04 19196 168,60 169,40 0,80 0,010 0,010 0,004C08-04 19197 169,40 170,19 0,79 0,000 0,000 0,002C08-04 19198 170,19 171,20 1,01 0,000 0,000 0,013C08-04 19199 171,20 172,16 0,96 0,000 0,000 0,013C08-04 19200 172,16 172,80 0,64 0,000 0,000 0,004C08-04 19201 172,80 173,42 0,62 0,010 0,010 0,002C08-04 19202 173,42 174,50 1,08 0,010 0,000 0,005 0,016C08-04 19203 174,50 175,50 1,00 0,010 0,010 0,016C08-04 19204 175,50 176,57 1,07 0,000 0,000 0,017C08-04 19205 176,57 177,47 0,90 0,010 0,010 0,001C08-04 19206 177,47 178,50 1,03 0,020 0,020 0,008C08-04 19207 OREAS 14P Batch 8 Aus 0,060 0,060 2,110C08-04 19208 178,50 179,52 1,02 0,030 0,040 0,035 0,004C08-04 19209 179,52 180,60 1,08 0,000 0,000 0,013C08-04 19210 180,60 181,68 1,08 0,010 0,010 0,013C08-04 19211 181,68 182,15 0,47 0,030 0,030 0,002C08-04 19212 182,15 183,00 0,85 0,010 0,010 0,016C08-04 19213 183,00 184,00 1,00 0,010 0,010 0,016C08-04 19214 184,00 185,00 1,00 0,010 0,010 0,017C08-04 19215 185,00 186,00 1,00 0,010 0,010 0,017C08-04 19216 186,00 187,00 1,00 0,010 0,010 0,017C08-04 19217 187,00 187,80 0,80 0,010 0,030 0,020 0,016C08-04 19218 187,80 188,60 0,80 0,010 0,010 0,015C08-04 19219 188,60 189,60 1,00 0,040 0,040 0,002C08-04 19220 189,60 190,52 0,92 0,040 0,040 0,002C08-04 19221 190,52 191,40 0,88 0,010 0,010 0,016C08-04 19222 191,40 192,32 0,92 0,030 0,030 0,006C08-04 19223 192,32 192,77 0,45 0,010 0,010 0,002

C08-04 19224 192,77 193,34 0,57 0,030 0,030 0,027C08-04 19225 193,34 193,80 0,46 0,010 0,010 0,007C08-04 19226 193,80 194,40 0,60 0,000 0,000 0,031C08-04 19227 194,40 194,99 0,59 0,020 0,020 0,033C08-04 19228 194,99 195,87 0,88 0,020 0,020 0,005C08-04 19229 195,87 196,60 0,73 0,100 0,100 0,015C08-04 19230 196,60 197,41 0,81 0,020 0,020 0,014C08-04 19231 197,41 198,15 0,74 0,030 0,040 0,035 0,002C08-04 19232 198,15 198,91 0,76 0,030 0,030 0,003C08-04 19233 198,91 199,80 0,89 0,020 0,020 0,004C08-04 19234 QUARTZ Purchased 0,000 0,000 0,001C08-04 19235 199,80 200,80 1,00 0,020 0,020 0,002C08-04 19236 200,80 201,74 0,94 0,020 0,020 0,002C08-04 19237 201,74 202,42 0,68 0,000 0,000 0,015C08-04 19238 202,42 203,50 1,08 0,010 0,000 0,005 0,039C08-04 19239 203,50 204,40 0,90 0,000 0,000 0,052C08-04 19240 204,40 205,30 0,90 0,000 0,000 0,007C08-04 19241 205,30 206,20 0,90 0,000 0,000 0,004C08-04 19242 206,20 207,10 0,90 0,010 0,010 0,004C08-04 19243 207,10 208,00 0,90 0,000 0,000 0,004C08-04 19244 208,00 208,90 0,90 0,020 0,020 0,003C08-04 19245 OREAS 14P Batch 8 Aus 0,050 0,050 2,080C08-04 19246 208,90 209,70 0,80 0,010 0,010 0,004C08-04 19247 209,70 210,60 0,90 0,000 0,000 0,017C08-04 19248 210,60 211,50 0,90 0,010 0,010 0,020C08-04 19249 211,50 212,40 0,90 0,000 0,000 0,020C08-04 19250 212,40 213,30 0,90 0,000 0,000 0,019C08-04 19251 213,30 214,19 0,89 0,020 0,020 0,019C08-04 19252 214,19 215,16 0,97 0,030 0,030 0,008C08-04 19253 215,16 216,14 0,98 0,000 0,010 0,005 0,019C08-04 19254 216,14 216,66 0,52 0,010 0,010 0,017C08-04 19255 216,66 217,62 0,96 0,000 0,000 0,028C08-04 19256 217,62 218,50 0,88 0,010 0,010 0,002C08-04 19257 218,50 219,40 0,90 0,010 0,010 0,009C08-04 19258 219,40 220,34 0,94 0,010 0,010 0,004C08-04 19259 220,34 221,19 0,85 0,010 0,010 0,026C08-04 19260 221,19 222,10 0,91 0,010 0,010 0,005C08-04 19261 222,10 223,00 0,90 0,010 0,010 0,010C08-04 19262 223,00 223,92 0,92 0,020 0,020 0,001C08-04 19263 223,92 224,80 0,88 0,000 0,000 0,000 0,016C08-04 19264 224,80 225,60 0,80 0,000 0,000 0,029C08-04 19265 225,60 226,45 0,85 0,000 0,000 0,018C08-04 19266 226,45 227,14 0,69 0,010 0,010 0,029

C08-04 19267 227,14 227,75 0,61 0,010 0,010 0,020C08-04 19268 227,75 228,37 0,62 0,010 0,000 0,005 0,008C08-04 19269 228,37 229,20 0,83 0,010 0,010 0,029C08-04 19270 229,20 230,00 0,80 0,020 0,020 0,028C08-04 19271 230,00 230,80 0,80 0,000 0,000 0,019C08-04 19272 OREAS 14P Batch 8 Aus 0,060 0,060 2,110C08-04 19273 230,80 231,67 0,87 0,020 0,020 0,026C08-04 19274 231,67 232,53 0,86 0,000 0,000 0,000 0,012C08-04 19275 232,53 233,10 0,57 0,020 0,020 0,029C08-04 19276 233,10 233,79 0,69 0,020 0,020 0,027C08-04 19277 233,79 234,60 0,81 0,000 0,000 0,011C08-04 19278 234,60 235,40 0,80 0,010 0,010 0,010C08-04 19279 235,40 236,20 0,80 0,020 0,020 0,011C08-04 19280 236,20 237,05 0,85 0,030 0,030 0,011C08-04 19281 237,05 238,00 0,95 0,020 0,020 0,015C08-04 19282 238,00 239,00 1,00 0,030 0,020 0,025 0,021C08-04 19283 239,00 240,00 1,00 0,010 0,010 0,008C08-04 19284 240,00 241,00 1,00 0,070 0,070 0,070 0,003C08-04 19285 241,00 242,00 1,00 0,100 0,100 0,004C08-04 19286 242,00 243,00 1,00 0,280 0,250 0,265 0,009C08-04 19287 243,00 244,00 1,00 0,110 0,110 0,012C08-04 19288 DIABASE 89.0-89.5 0,010 0,010 0,002C08-04 19289 244,00 245,00 1,00 0,030 0,030 0,003C08-04 19290 245,00 246,00 1,00 0,010 0,010 0,001C08-04 19291 246,00 247,00 1,00 0,040 0,040 0,001C08-04 19292 247,00 248,00 1,00 0,000 0,000 0,001C08-04 19293 248,00 248,96 0,96 0,010 0,010 0,002C08-04 19294 248,96 249,83 0,87 0,010 0,010 0,019C08-04 19295 249,83 250,40 0,57 0,010 0,010 0,003


3,9 5 1,1 1,1 100% 0,52 0,58 53%5 8 3 3 100% 0,80 2,20 73%8 11 3 3 100% 1,05 1,95 65%11 14 3 2,95 98% 0,16 2,84 95%14 17 3 3 100% 0,31 2,69 90%17 20 3 2,91 97% 0,09 2,91 97%20 23 3 2,95 98% 0,20 2,8 93%23 26 3 3,04 101% 0,07 2,93 98%26 29 3 3,01 100% 0,08 2,92 97%29 32 3 3,04 101% 0,07 2,93 98%32 35 3 2,91 97% 0,29 2,71 90%35 38 3 3,04 101% 0,00 3,00 100%38 41 3 2,96 99% 0,03 2,97 99%41 44 3 3,13 104% 0,46 2,54 85%44 47 3 2,88 96% 0,25 2,75 92%47 50 3 2,98 99% 0,04 2,96 99%50 53 3 3,04 101% 0,19 2,81 94%53 56 3 3,04 101% 0,03 2,97 99%56 59 3 2,93 98% 0,07 2,93 98%59 62 3 3,04 101% 0,00 3,00 100%62 65 3 2,97 99% 0,10 2,9 97%65 68 3 3,05 102% 0,21 2,79 93%68 71 3 3,03 101% 0,10 2,9 97%71 74 3 2,95 98% 0,21 2,79 93%74 77 3 3,00 100% 0,31 2,69 90%77 80 3 2,92 97% 0,56 2,44 81%80 83 3 2,93 98% 0,03 2,97 99%83 86 3 3 100% 0,00 3,00 100%86 89 3 2,96 99% 0,23 2,77 92%89 92 3 3,00 100% 0,16 2,84 95%92 95 3 2,95 98% 0,28 2,72 91%95 98 3 3,09 103% 0,27 2,73 91%98 101 3 3,09 103% 0,71 2,29 76%101 104 3 3,00 100% 0,17 2,83 94%104 107 3 3,03 101% 0,12 2,88 96%107 110 3 3,00 100% 0,06 2,94 98%110 113 3 3,01 100% 0,15 2,85 95%113 116 3 3,00 100% 0,06 2,94 98%116 119 3 2,97 99% 0,00 3 100%119 122 3 3,05 102% 0,26 2,74 91%122 125 3 2,75 92% 0,27 2,73 91%125 128 3 2,95 98% 0,04 2,96 99%128 131 3 2,96 99% 0,07 2,93 98%131 134 3 2,98 99% 0,06 2,94 98%134 137 3 3,02 101% 0,08 2,92 97%137 140 3 2,98 99% 0,04 2,96 99%

140 143 3 2,98 99% 0,00 3 100%143 146 3 3,02 101% 0,02 2,98 99%146 149 3 3,03 101% 0,00 3 100%149 152 3 3,05 102% 0,53 2,47 82%152 155 3 3,06 102% 0,31 2,69 90%155 158 3 2,98 99% 0,00 3,00 100%158 161 3 3,03 101% 0,07 2,93 98%161 164 3 2,97 99% 0,14 2,86 95%164 167 3 3,00 100% 0,15 2,85 95%167 170 3 2,97 99% 0,49 2,51 84%170 173 3 3,03 101% 0,13 2,87 96%173 176 3 2,94 98% 0,52 2,48 83%176 179 3 3,03 101% 0,18 2,82 94%179 182 3 3,05 102% 0,22 2,78 93%182 185 3 3,00 100% 0,14 2,86 95%185 188 3 3,00 100% 0,23 2,77 92%188 191 3 2,95 98% 0,29 2,71 90%191 194 3 3,05 102% 0,20 2,80 93%194 197 3 3,05 102% 0,28 2,72 91%197 200 3 2,96 99% 0,52 2,48 83%200 203 3 3,02 101% 0,22 2,78 93%203 206 3 3,06 102% 0,25 2,75 92%206 209 3 3,03 101% 0,53 2,47 82%209 212 3 3,03 101% 0,30 2,70 90%212 215 3 2,97 99% 0,25 2,75 92%215 218 3 3,04 101% 0,41 2,59 86%218 221 3 2,96 99% 0,17 2,83 94%221 224 3 3,00 100% 0,29 2,71 90%224 227 3 3,06 102% 0,98 2,02 67%227 230 3 3,02 101% 1,15 1,85 62%230 233 3 3,01 100% 0,04 2,96 99%233 236 3 2,93 98% 0,23 2,77 92%236 239 3 2,95 98% 0,11 2,89 96%239 242 3 3,05 102% 0,08 2,92 97%242 245 3 2,95 98% 0,10 2,9 97%245 248 3 2,99 100% 0,00 3,00 100%248 251 3 2,44 81% 0,20 2,8 93%


C08-05 L-200E 600N 250 0 -50 251m 28-juil-08 02-août-08

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 3,55 3,55 OB overburden

3,55 19,24 15,69

Basaltic komatiite volcanics, grey-green, aphanitic to fg, pillowed, with 5-10% carbonates/talc, talc/chlorite/leucoxene alteration, soft, magnetic

19,24 29,75 10,51

intermediate intrusive, pinkish-brown, fg matrix with ghost fds phenocryst, breccia, ultramafic inclusions, hematite, chlorite and silica alteration, hard, 2-3% py

29,75 35,08 5,33

talcose komatiite volcanics, grey- pale grey, fg, brecciated, foliation 20-60 to CA, 15-20% carbonates/talc, talc alteration, soft, magnetic, 1-2% py

35,08 44,89 9,81

intermediate intrusive, pinkish-brown, fg matrix with ghost fds phenocryst, breccia, ultramafic inclusions, hematite, chlorite and silica alteration, hard, 3-5% py

44,89 56,24 11,35

basaltic komatiite volcanics, grey-green, aphanitic to fg, foliation 50-60 to CA, pillowed, with 10-15% carbonates/talc, talc/chlorite/leucoxene alteration, soft, magnetic, 1-2% py

56,24 59,93 3,69

felsic to intermediate intrusive, pinkish-brown, fg matrix with mafic and fds phenocryst, calcite and hematite alteration, silicification, hard, 2-3% py

59,93 62,66 2,73

basaltic komatiite volcanics, grey-green, fg, brecciated, 5-10% carbonates/talc, talc and leucoxene alteration, soft, magnetic, 1-2% py

62,66 69,96 7,30intermediate intrusive, pinkish-brown, fg matrix with mafic and ghost fds phenocryst, calcite and hematite alteration, hard, 1-2% py

69,96 95,61 25,65

mafic to intermediate intrusive, greenish-brown, fg matrix with mafic and ghost fds phenocryst, calcite and hematite alteration, silicification, hard, 1-2% py

95,61 99,84 4,23

basaltic komatiite volcanics, pale grey-green, fg, irregular foliation 5-30 to CA, 15-20% carbonates/talc, chlorite and leucoxene alteration, 1-2% py

99,84 102,18 2,34felsic intrusive, brownish-red, fg matrix with mafic and ghost fds phenocryst, hematite and calcite alteration, silicified, hard, 1-2% py

102,18 126,16 23,98

intermediate intrusive, pinkish-brown, fg matrix with mafic and ghost fds phenocryst, calcite and hematite alteration, silicification, hard, 1-2% py

126,16 157,6 31,44

basaltic komatiite volcanics, grey-green, fg, foliation 10-50 to CA, brecciated, 15-20% carbonate/talc, chlorite/talc/leucoxene alteration, magnetic, 2-3% py

157,60 162,5 4,90mafic intrusive, grey-green, fg to mg, massive with epidote clasts, epidote and calcite alteration, hard, 2-3% py

162,50 169,52 7,02altered mafic volcanics, pale grey-green, aphanitic to fg, brecciated, pillowed, hard, 3-5 scattered py

DDH Depth

169,52 177,95 8,43intermediate intrusive, grey brown, fg matrix with mafic and ghost fds phenocryst, calcite alteration, 2-3% py

177,95 185,25 7,30altered mafic volcanics, pale grey-green, aphanitic to fg, brecciated, pillowed, hard, calcite alteration, 2-3 scattered py

185,25 193,75 8,50tholeiitic volcanics, grey-green, aphanitic to fg, pillowed, breccia, chlorite and minor graphite, calcite alteration, hard, 2-3% py

193,75 207,08 13,33mafic calc-alkalic volcanics, pale grey-green, aphanitic to fg, pillowed, brecciated, calcite alteration, hard, 2-3-5% py

207,08 222,7 15,62tholeiitic volcanics, grey-green, aphanitic to fg, pillowed, breccia, chlorite and minor graphite, calcite alteration, hard, 1-2% py

222,70 250,73 28,03mafic calc-alkalic volcanics, pale grey-green, aphanitic to fg, pillowed, brecciated, calcite alteration, hard, 1-2% py

EOH

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments6,95 7,45 0,50 lost core9,40 10,35 0,95 lost core

14,63 15,19 0,56reddish-brown felsic dyke, fractured, silicified, 5% dissminated py

17,78 18,27 0,49intermediate dyke, pinkish-brown, fg, 5% felsic remnant, calcite alteration

20,56 21,52 0,96 basaltic komatiite volcanics, pale grey-green30,55 30,90 0,35 lost core

46,86 47,70 0,84brecciated intermediate dyke, reddish brown, fg, 35% ultramafic fragments, 2% py

48,76 48,94 0,18felsic dyke, brownish-red, fg matrix with mafic phenocryst, 5% py

49,52 49,78 0,26 strong foliation 45-60 to CA, 5% intermediate fragments

49,78 50,53 0,75brecciated intermediate dyke, reddish brown, fg, 45% ultramafic fragments, 2% py

50,90 51,20 0,30 Spinifex texture51,70 52,1 0,40 Spinifex texture75,64 76,65 1,01 basaltic komatiite volcanics, pale grey-green

90,31 91,20 0,89idem, with strong foliation 20-45 to CA, 25% carbonates/talc, 2% py

98,56 98,85 0,29 intermediate dyke118,09 118,52 0,43 mafic dyke, grey-green, fg, massive, chlorite alteration, 3% py

118,52 120,72 2,20basaltic komatiite volcanics, medium green, fg, foliation 20-40 to CA, brecciated, chlorite alteration, 2-3% py

120,72 121,42 0,70felsic dyke, pink, fg matrix with mafic phenocryst, hematite alteration, 5% py

132,17 132,33 0,16 intermediate dyke

138,18 139,87 1,69intermediate dyke, pinkish-brown, fg matrix with mafic and ghost fds phenocryst, 2% py

140,88 141,75 0,87intermediate dyke, pinkish-brown, fg matrix with mafic and ghost fds phenocryst

148,74 148,96 0,22 felsic dyke, pale purplish-brown149,50 149,68 0,18 intermediate dyke, greyish-brown, 10% dissminated py162,85 163,55 0,70 intermediate dyke213,52 213,75 0,23 mafic dyke226,00 227 1,00 minor silver graphite in veining236,00 236,64 0,64 brecciated qtz-cal vein with 25% mafic fragments237,69 238,24 0,55 mafic dykeEOH

DDH Depth

HoleIDSample Number


Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-05 19296 3,55 4,40 0,85 0,010 0,010 0,061C08-05 19297 4,40 5,20 0,80 0,010 0,010 0,063C08-05 19298 5,20 6,00 0,80 0,000 0,000 0,000 0,067C08-05 19299 6,00 6,95 0,95 0,000 0,000 0,070C08-05 19300 7,45 8,40 0,95 0,000 0,000 0,054C08-05 19301 8,40 9,40 1,00 0,010 0,010 0,052C08-05 19302 10,35 11,20 0,85 0,000 0,000 0,062C08-05 19303 11,20 12,00 0,80 0,010 0,010 0,062C08-05 19304 12,00 12,90 0,90 0,010 0,010 0,056C08-05 19305 12,90 13,80 0,90 0,010 0,010 0,051C08-05 19306 13,80 14,63 0,83 0,000 0,000 0,053C08-05 19307 14,63 15,19 0,56 0,010 0,000 0,005 0,010C08-05 19308 15,19 16,20 1,01 0,000 0,000 0,041C08-05 19309OREAS 14P Batch 8 Aus 0,060 0,060 2,100C08-05 19310 16,20 17,20 1,00 0,000 0,000 0,045C08-05 19311 17,20 18,27 1,07 0,000 0,000 0,040C08-05 19312 18,27 19,24 0,97 0,000 0,000 0,056C08-05 19313 19,24 19,84 0,60 0,010 0,010 0,028C08-05 19314 19,84 20,56 0,72 0,000 0,000 0,000 0,016C08-05 19315 20,56 21,52 0,96 0,000 0,000 0,066C08-05 19316 21,52 22,40 0,88 0,000 0,000 0,023C08-05 19317 22,40 23,40 1,00 0,000 0,000 0,025C08-05 19318 23,40 24,40 1,00 0,010 0,010 0,024C08-05 19319 24,40 25,40 1,00 0,000 0,000 0,027C08-05 19320 25,40 26,40 1,00 0,010 0,010 0,015C08-05 19321 26,40 27,27 0,87 0,000 0,000 0,021C08-05 19322 27,27 28,11 0,84 0,000 0,000 0,057C08-05 19323 28,11 29,00 0,89 0,000 0,000 0,007C08-05 19324 29,00 29,75 0,75 0,020 0,000 0,010 0,009C08-05 19325 29,75 30,55 0,80 0,010 0,010 0,042C08-05 19326 30,90 32,00 1,10 0,010 0,010 0,041C08-05 19327 32,00 33,00 1,00 0,000 0,000 0,041C08-05 19328OREAS 14P Batch 8 Aus 0,060 0,060 2,090C08-05 19329 33,00 34,00 1,00 0,000 0,000 0,043C08-05 19330 34,00 35,08 1,08 0,010 0,010 0,010 0,045C08-05 19331 35,08 36,05 0,97 0,000 0,000 0,009C08-05 19332 36,05 36,97 0,92 0,010 0,010 0,048C08-05 19333 36,97 37,90 0,93 0,000 0,000 0,030C08-05 19334 37,90 38,90 1,00 0,010 0,010 0,034

C08-05 19335 38,90 39,90 1,00 0,010 0,000 0,005 0,029C08-05 19336 39,90 40,39 0,49 0,010 0,010 0,043C08-05 19337 40,39 40,75 0,36 0,000 0,000 0,036C08-05 19338 40,75 41,40 0,65 0,010 0,010 0,056C08-05 19339 41,40 42,31 0,91 0,000 0,000 0,021C08-05 19340 42,31 43,20 0,89 0,010 0,010 0,021C08-05 19341 43,20 44,00 0,80 0,000 0,000 0,026C08-05 19342 44,00 44,89 0,89 0,000 0,000 0,022C08-05 19343 44,89 45,90 1,01 0,000 0,000 0,051C08-05 19344 45,90 46,86 0,96 0,000 0,000 0,055C08-05 19345 46,86 47,70 0,84 0,000 0,000 0,021C08-05 19346 47,70 48,45 0,75 0,010 0,010 0,044C08-05 19347 48,45 48,94 0,49 0,000 0,000 0,000 0,025C08-05 19348 48,94 49,78 0,84 0,000 0,000 0,043C08-05 19349 49,78 50,53 0,75 0,000 0,000 0,028C08-05 19350 50,53 51,40 0,87 0,010 0,010 0,038C08-05 19351 51,40 52,30 0,90 0,010 0,010 0,037C08-05 19352 QUARTZ Purchased 0,000 0,000 0,001C08-05 19353 52,30 53,20 0,90 0,000 0,000 0,037C08-05 19354 53,20 54,20 1,00 0,010 0,010 0,038C08-05 19355 54,20 55,20 1,00 0,000 0,000 0,038C08-05 19356 55,20 56,24 1,04 0,000 0,000 0,049C08-05 19357 56,24 57,10 0,86 0,000 0,000 0,013C08-05 19358 57,10 58,00 0,90 0,000 0,000 0,013C08-05 19359 58,00 58,90 0,90 0,000 0,000 0,017C08-05 19360 58,90 59,93 1,03 0,000 0,000 0,021C08-05 19361 59,93 60,80 0,87 0,000 0,000 0,056C08-05 19362 60,80 61,70 0,90 0,000 0,000 0,041C08-05 19363OREAS 14P Batch 8 Aus 0,070 0,070 2,110C08-05 19364 61,70 62,66 0,96 0,000 0,010 0,005 0,040C08-05 19365 62,66 63,50 0,84 0,000 0,000 0,017C08-05 19366 63,50 64,30 0,80 0,010 0,010 0,010 0,016C08-05 19367 64,30 65,10 0,80 0,010 0,010 0,017C08-05 19368 65,10 66,00 0,90 0,010 0,010 0,017C08-05 19369 66,00 67,00 1,00 0,000 0,000 0,016C08-05 19370 67,00 68,00 1,00 0,100 0,100 0,016C08-05 19371 68,00 69,00 1,00 0,010 0,010 0,010 0,016C08-05 19372 69,00 69,96 0,96 0,000 0,000 0,018C08-05 19373 69,96 71,00 1,04 0,010 0,010 0,050C08-05 19374 71,00 72,00 1,00 0,010 0,010 0,029C08-05 19375 72,00 73,00 1,00 0,010 0,010 0,019

C08-05 19376 73,00 74,00 1,00 0,020 0,020 0,019C08-05 19377 74,00 74,80 0,80 0,000 0,000 0,017C08-05 19378 74,80 75,64 0,84 0,000 0,000 0,025C08-05 19379 75,64 76,65 1,01 0,010 0,010 0,044C08-05 19380 76,65 77,50 0,85 0,020 0,010 0,015 0,017C08-05 19381 77,50 78,30 0,80 0,000 0,000 0,018C08-05 19382 78,30 79,10 0,80 0,010 0,010 0,010C08-05 19383 79,10 80,00 0,90 0,010 0,010 0,020C08-05 19384 80,00 81,00 1,00 0,000 0,000 0,021C08-05 19385 81,00 82,00 1,00 0,010 0,010 0,019C08-05 19386OREAS 14P Batch 8 Aus 0,070 0,070 2,090C08-05 19387 82,00 83,00 1,00 0,010 0,010 0,029C08-05 19388 83,00 84,00 1,00 0,010 0,010 0,035C08-05 19389 84,00 85,00 1,00 0,010 0,010 0,034C08-05 19390 85,00 86,00 1,00 0,010 0,010 0,020C08-05 19391 86,00 87,00 1,00 0,030 0,030 0,012C08-05 19392 87,00 88,00 1,00 0,090 0,120 0,105 0,017C08-05 19393 88,00 88,80 0,80 0,000 0,000 0,013C08-05 19394 88,80 89,60 0,80 0,010 0,010 0,013C08-05 19395 89,60 90,31 0,71 0,010 0,000 0,005 0,014C08-05 19396 90,31 91,20 0,89 0,010 0,010 0,021C08-05 19397 91,20 92,00 0,80 0,000 0,000 0,014C08-05 19398 92,00 93,00 1,00 0,000 0,000 0,021C08-05 19399 93,00 94,00 1,00 0,000 0,000 0,031C08-05 19400 94,00 94,80 0,80 0,000 0,000 0,026C08-05 19401 94,80 95,61 0,81 0,000 0,000 0,025C08-05 19402 95,61 96,50 0,89 0,010 0,010 0,062C08-05 19403 96,50 97,40 0,90 0,150 0,160 0,155 0,060C08-05 19404 97,40 98,30 0,90 0,010 0,010 0,032C08-05 19405 98,30 99,10 0,80 0,020 0,020 0,021C08-05 19406 99,10 99,84 0,74 0,010 0,010 0,020C08-05 19407 DIABASE 89.5-90.0 0,010 0,010 0,003C08-05 19408 99,84 100,60 0,76 0,020 0,010 0,015 0,020C08-05 19409 100,60 101,40 0,80 0,020 0,020 0,025C08-05 19410 101,40 102,18 0,78 0,000 0,000 0,013C08-05 19411 102,18 103,16 0,98 0,020 0,020 0,031C08-05 19412 103,16 104,24 1,08 0,040 0,040 0,028C08-05 19413 104,24 104,84 0,60 0,080 0,080 0,053C08-05 19414 104,84 105,90 1,06 0,010 0,010 0,027C08-05 19415 105,90 107,00 1,10 0,010 0,010 0,022C08-05 19416 107,00 108,00 1,00 0,060 0,060 0,023

C08-05 19417 108,00 109,00 1,00 0,010 0,010 0,026C08-05 19418 109,00 110,00 1,00 0,110 0,110 0,022C08-05 19419 110,00 111,00 1,00 0,010 0,010 0,021C08-05 19420 111,00 112,00 1,00 0,010 0,010 0,027C08-05 19421 112,00 113,00 1,00 0,070 0,070 0,070 0,027C08-05 19422 113,00 114,00 1,00 0,010 0,010 0,028C08-05 19423 114,00 115,00 1,00 0,010 0,010 0,026C08-05 19424 115,00 116,00 1,00 0,010 0,010 0,027C08-05 19425 116,00 117,00 1,00 0,010 0,000 0,005 0,025C08-05 19426 117,00 118,09 1,09 0,020 0,020 0,025C08-05 19427 118,09 118,52 0,43 0,000 0,000 0,076C08-05 19428 118,52 119,20 0,68 0,040 0,040 0,067C08-05 19429OREAS 14P Batch 8 Aus 0,040 0,040 2,090C08-05 19430 119,20 119,89 0,69 0,000 0,000 0,101C08-05 19431 119,89 120,72 0,83 0,000 0,000 0,047C08-05 19432 120,72 121,42 0,70 0,000 0,000 0,002C08-05 19433 121,42 122,20 0,78 0,000 0,000 0,000 0,003C08-05 19434 122,20 123,20 1,00 0,020 0,020 0,003C08-05 19435 123,20 124,20 1,00 0,010 0,010 0,011C08-05 19436 124,20 125,20 1,00 0,010 0,010 0,005C08-05 19437 125,20 126,16 0,96 0,010 0,010 0,019C08-05 19438 126,16 127,00 0,84 0,000 0,000 0,056C08-05 19439 127,00 128,00 1,00 0,080 0,100 0,090 0,043C08-05 19440 128,00 129,00 1,00 0,000 0,000 0,056C08-05 19441 129,00 130,00 1,00 0,010 0,010 0,046C08-05 19442 130,00 131,00 1,00 0,010 0,010 0,038C08-05 19443OREAS 14P Batch 8 Aus 0,060 0,060 2,090C08-05 19444 131,00 132,00 1,00 0,010 0,010 0,045C08-05 19445 132,00 133,00 1,00 0,000 0,000 0,039C08-05 19446 133,00 134,00 1,00 0,000 0,000 0,048C08-05 19447 134,00 135,00 1,00 0,000 0,000 0,037C08-05 19448 135,00 136,00 1,00 0,000 0,000 0,040C08-05 19449 136,00 137,10 1,10 0,000 0,010 0,005 0,022C08-05 19450 137,10 138,18 1,08 0,000 0,000 0,034C08-05 19451 138,18 139,00 0,82 0,000 0,000 0,018C08-05 19452 139,00 139,87 0,87 0,000 0,000 0,017C08-05 19453 139,87 140,88 1,01 0,000 0,000 0,041C08-05 19454 140,88 141,75 0,87 0,000 0,000 0,000 0,030C08-05 19455 141,75 142,60 0,85 0,000 0,000 0,000 0,057C08-05 19456 142,60 143,40 0,80 0,000 0,000 0,054C08-05 19457 143,40 144,20 0,80 0,010 0,010 0,031

C08-05 19458 144,20 145,00 0,80 0,010 0,010 0,053C08-05 19459 145,00 146,00 1,00 0,000 0,000 0,059C08-05 19460 146,00 147,00 1,00 0,000 0,000 0,062C08-05 19461 147,00 148,00 1,00 0,010 0,010 0,036C08-05 19462 148,00 149,00 1,00 0,000 0,000 0,038C08-05 19463 149,00 150,00 1,00 0,000 0,000 0,028C08-05 19464 QUARTZ Purchased 0,000 0,000 0,001C08-05 19465 150,00 151,00 1,00 0,000 0,000 0,029C08-05 19466 151,00 152,00 1,00 0,000 0,000 0,039C08-05 19467 152,00 153,00 1,00 0,000 0,000 0,038C08-05 19468 153,00 154,00 1,00 0,010 0,010 0,041C08-05 19469 154,00 155,00 1,00 0,010 0,010 0,043C08-05 19470 155,00 156,00 1,00 0,000 0,000 0,044C08-05 19471 156,00 156,80 0,80 0,000 0,000 0,032C08-05 19472 156,80 157,60 0,80 0,000 0,000 0,007C08-05 19473 157,60 158,50 0,90 0,020 0,010 0,015 0,004C08-05 19474 158,50 159,50 1,00 0,010 0,010 0,004C08-05 19475 159,50 160,50 1,00 0,010 0,010 0,004C08-05 19476 160,50 161,50 1,00 0,010 0,010 0,004C08-05 19477 161,50 162,50 1,00 0,000 0,000 0,005C08-05 19478 162,50 163,55 1,05 0,010 0,010 0,012C08-05 19479 163,55 164,50 0,95 0,010 0,010 0,008C08-05 19480 164,50 165,50 1,00 0,010 0,010 0,006C08-05 19481 165,50 166,50 1,00 0,010 0,010 0,006C08-05 19482 166,50 167,50 1,00 0,010 0,020 0,015 0,008C08-05 19483 167,50 168,50 1,00 0,010 0,010 0,006C08-05 19484 168,50 169,52 1,02 0,010 0,010 0,008C08-05 19485OREAS 14P Batch 8 Aus 0,040 0,040 2,100C08-05 19486 169,52 170,40 0,88 0,010 0,000 0,005 0,023C08-05 19487 170,40 171,20 0,80 0,010 0,010 0,026C08-05 19488 171,20 172,00 0,80 0,000 0,000 0,023C08-05 19489 172,00 173,00 1,00 0,000 0,000 0,019C08-05 19490 173,00 174,00 1,00 0,010 0,020 0,015 0,015C08-05 19491 174,00 175,00 1,00 0,020 0,020 0,012C08-05 19492 175,00 176,00 1,00 0,000 0,000 0,016C08-05 19493 176,00 177,00 1,00 0,010 0,010 0,018C08-05 19494 177,00 177,95 0,95 0,000 0,000 0,020C08-05 19495 177,95 179,00 1,05 0,000 0,000 0,006C08-05 19496 179,00 180,00 1,00 0,000 0,000 0,010C08-05 19497 180,00 181,00 1,00 0,000 0,010 0,005 0,006C08-05 19498 181,00 182,00 1,00 0,000 0,000 0,010

C08-05 19499 182,00 182,80 0,80 0,000 0,000 0,006C08-05 19500 182,80 183,60 0,80 0,020 0,010 0,015 0,018C08-05 19501 183,60 184,40 0,80 0,010 0,010 0,008C08-05 19502 184,40 185,25 0,85 0,000 0,000 0,006C08-05 19503 185,25 186,10 0,85 0,010 0,010 0,007C08-05 19504OREAS 14P Batch 8 Aus 0,050 0,050 2,090C08-05 19505 186,10 187,00 0,90 0,000 0,000 0,006C08-05 19506 187,00 188,00 1,00 0,000 0,000 0,006C08-05 19507 188,00 189,00 1,00 0,000 0,000 0,005C08-05 19508 189,00 190,00 1,00 0,010 0,000 0,005 0,007C08-05 19509 190,00 191,00 1,00 0,000 0,000 0,005C08-05 19510 191,00 192,00 1,00 0,000 0,000 0,006C08-05 19511 192,00 192,90 0,90 0,010 0,010 0,007C08-05 19512 192,90 193,75 0,85 0,000 0,000 0,006C08-05 19513 193,75 194,60 0,85 0,000 0,000 0,006C08-05 19514 194,60 195,40 0,80 0,000 0,000 0,005C08-05 19515 195,40 196,20 0,80 0,000 0,000 0,006C08-05 19516 196,20 197,00 0,80 0,000 0,000 0,005C08-05 19517 197,00 198,00 1,00 0,000 0,000 0,005C08-05 19518 198,00 199,00 1,00 0,000 0,000 0,004C08-05 19519 199,00 200,00 1,00 0,000 0,000 0,005C08-05 19520 200,00 201,00 1,00 0,000 0,000 0,005C08-05 19521 201,00 202,00 1,00 0,000 0,000 0,006C08-05 19522 DIABASE 89.5-90.0 0,000 0,020 0,010 0,002C08-05 19523 202,00 203,00 1,00 0,000 0,000 0,005C08-05 19524 203,00 204,00 1,00 0,000 0,000 0,006C08-05 19525 204,00 205,00 1,00 0,000 0,000 0,006C08-05 19526 205,00 206,00 1,00 0,000 0,000 0,006C08-05 19527 206,00 207,08 1,08 0,000 0,000 0,005C08-05 19528 207,08 208,00 0,92 0,000 0,000 0,005C08-05 19529 208,00 209,00 1,00 0,000 0,000 0,006C08-05 19530 209,00 210,00 1,00 0,000 0,010 0,005 0,005C08-05 19531 210,00 211,00 1,00 0,000 0,000 0,006C08-05 19532 211,00 212,00 1,00 0,000 0,000 0,006C08-05 19533 212,00 213,00 1,00 0,010 0,010 0,006C08-05 19534 213,00 214,00 1,00 0,010 0,010 0,006C08-05 19535 214,00 215,00 1,00 0,000 0,000 0,005C08-05 19536 215,00 216,00 1,00 0,000 0,000 0,005C08-05 19537 216,00 217,00 1,00 0,000 0,000 0,005C08-05 19538 217,00 218,00 1,00 0,000 0,000 0,005C08-05 19539 218,00 219,00 1,00 0,000 0,000 0,005

C08-05 19540 219,00 220,00 1,00 0,010 0,000 0,005 0,005C08-05 19541 220,00 221,00 1,00 0,010 0,010 0,005C08-05 19542 221,00 221,90 0,90 0,000 0,000 0,006C08-05 19543 221,90 222,70 0,80 0,010 0,010 0,007C08-05 19544 222,70 223,50 0,80 0,020 0,020 0,006C08-05 19545 223,50 224,30 0,80 0,020 0,020 0,006C08-05 19546 224,30 225,10 0,80 0,010 0,010 0,006C08-05 19547OREAS 14P Batch 8 Aus 0,080 0,080 2,090C08-05 19548 225,10 226,00 0,90 0,000 0,000 0,000 0,007C08-05 19549 226,00 227,00 1,00 0,010 0,010 0,005C08-05 19550 227,00 228,00 1,00 0,010 0,010 0,005C08-05 19551 228,00 229,00 1,00 0,000 0,000 0,005C08-05 19552 229,00 230,00 1,00 0,000 0,000 0,007C08-05 19553 230,00 231,00 1,00 0,000 0,000 0,005C08-05 19554 231,00 232,00 1,00 0,010 0,010 0,004C08-05 19555 232,00 233,00 1,00 0,010 0,010 0,003C08-05 19556 233,00 234,00 1,00 0,010 0,010 0,003C08-05 19557 234,00 235,00 1,00 0,010 0,010 0,005C08-05 19558 235,00 236,00 1,00 0,010 0,010 0,006C08-05 19559 236,00 236,64 0,64 0,000 0,000 0,007C08-05 19560 236,64 237,69 1,05 0,000 0,000 0,004C08-05 19561 237,69 238,24 0,55 0,000 0,000 0,018C08-05 19562 238,24 239,10 0,86 0,000 0,000 0,003C08-05 19563 239,10 240,00 0,90 0,010 0,010 0,004C08-05 19564 240,00 241,00 1,00 0,000 0,000 0,000 0,005C08-05 19565OREAS 14P Batch 8 Aus 0,070 0,070 2,080C08-05 19566 241,00 242,00 1,00 0,010 0,010 0,004C08-05 19567 242,00 243,00 1,00 0,000 0,000 0,005C08-05 19568 243,00 244,00 1,00 0,000 0,000 0,006C08-05 19569 244,00 245,00 1,00 0,000 0,000 0,005C08-05 19570 245,00 246,00 1,00 0,000 0,000 0,005C08-05 19571 246,00 247,00 1,00 0,000 0,000 0,005C08-05 19572 247,00 248,00 1,00 0,000 0,000 0,006C08-05 19573 248,00 249,00 1,00 0,000 0,000 0,006C08-05 19574 249,00 249,90 0,90 0,030 0,030 0,006C08-05 19575 249,90 250,73 0,83 0,000 0,000 0,000 0,005


3,55 5 1,45 1,45 100% 1,35 0,10 7%5 8 3 2,5 83% 1,95 1,05 35%8 11 3 2,05 68% 1,43 1,57 52%11 14 3 2,97 99% 1,16 1,84 61%14 17 3 2,99 100% 0,48 2,52 84%17 20 3 2,96 99% 0,53 2,47 82%20 23 3 3,05 102% 0,58 2,42 81%23 26 3 3,05 102% 0,56 2,44 81%26 29 3 2,91 97% 0,93 2,07 69%29 32 3 2,65 88% 0,95 2,05 68%32 35 3 3,02 101% 0,79 2,21 74%35 38 3 3,08 103% 1,02 1,98 66%38 41 3 2,94 98% 0,65 2,35 78%41 44 3 3,1 103% 0,21 2,79 93%44 47 3 3,02 101% 0,98 2,02 67%47 50 3 3,01 100% 0,84 2,16 72%50 53 3 3,05 102% 0,27 2,73 91%53 56 3 3,04 101% 0,15 2,85 95%56 59 3 3,02 101% 0,13 2,87 96%59 62 3 3,05 102% 0,04 2,96 99%62 65 3 2,99 100% 0,20 2,80 93%65 68 3 2,97 99% 0,17 2,83 94%68 71 3 3,10 103% 0,17 2,83 94%71 74 3 3,00 100% 0,12 2,88 96%74 77 3 2,98 99% 0,16 2,84 95%77 80 3 3,03 101% 0,26 2,74 91%80 83 3 3,00 100% 0,13 2,87 96%83 86 3 2,94 98% 0,00 3,00 100%86 89 3 2,99 100% 0,03 2,97 99%89 92 3 3,00 100% 0,14 2,86 95%92 95 3 3,00 100% 0,13 2,87 96%95 98 3 3,02 101% 0,17 2,83 94%98 101 3 2,95 98% 0,26 2,74 91%101 104 3 2,99 100% 0,27 2,73 91%104 107 3 2,95 98% 0,25 2,75 92%107 110 3 2,99 100% 0,17 2,83 94%110 113 3 3,00 100% 0,60 2,40 80%113 116 3 2,99 100% 0,23 2,77 92%116 119 3 3,06 102% 0,15 2,85 95%119 122 3 2,93 98% 0,56 2,44 81%122 125 3 3,00 100% 0,50 2,50 83%125 128 3 2,97 99% 0,00 3,00 100%128 131 3 3,04 101% 0,11 2,89 96%131 134 3 2,97 99% 0,02 2,98 99%134 137 3 3,00 100% 0,16 2,84 95%137 140 3 3,02 101% 0,20 2,80 93%

140 143 3 3,04 101% 0,06 2,94 98%143 146 3 2,98 99% 0,00 3,00 100%146 149 3 2,96 99% 0,62 2,38 79%149 152 3 3,00 100% 0,51 2,49 83%152 155 3 3,01 100% 0,19 2,81 94%155 158 3 2,95 98% 0,09 2,91 97%158 161 3 3,01 100% 0,00 3,00 100%161 164 3 3,00 100% 0,77 2,23 74%164 167 3 2,94 98% 0,32 2,68 89%167 170 3 3,10 103% 0,47 2,53 84%170 173 3 3,09 103% 0,20 2,80 93%173 176 3 2,96 99% 0,09 2,91 97%176 179 3 3,01 100% 0,08 2,92 97%179 182 3 2,95 98% 0,38 2,62 87%182 185 3 3,09 103% 0,42 2,58 86%185 188 3 2,93 98% 0,60 2,40 80%188 191 3 3,00 100% 0,62 2,38 79%191 194 3 2,95 98% 0,10 2,90 97%194 197 3 3,05 102% 0,00 3,00 100%197 200 3 3,01 100% 0,12 2,88 96%200 203 3 3,02 101% 0,21 2,79 93%203 206 3 3,02 101% 0,02 2,98 99%206 209 3 3,00 100% 0,00 3,00 100%209 212 3 3,02 101% 0,08 2,92 97%212 215 3 2,96 99% 0,00 3,00 100%215 218 3 2,97 99% 0,00 3,00 100%218 221 3 3,06 102% 0,08 2,92 97%221 224 3 3,03 101% 0,11 2,89 96%224 227 3 3,06 102% 0,06 2,94 98%227 230 3 2,98 99% 0,03 2,97 99%230 233 3 2,97 99% 0,00 3,00 100%233 236 3 2,99 100% 0,15 2,85 95%236 239 3 3,00 100% 0,40 2,60 87%239 242 3 3,02 101% 0,05 2,95 98%242 245 3 2,99 100% 0,00 3,00 100%245 248 3 3,01 100% 0,00 3,00 100%248 250,5 2,5 2,44 98% 0,00 2,50 100%


C08-06 L-200E 725N 250 0 -50 252m 03-août-08 07-août-08


3,18 12,19 9,01Tuffaceous mafic calc-alkalic volcanics, grey-green, aphanitic to fg, bedding 25-50 to CA, brecciated, calcite alteration, hard

12,19 16,84 4,65intermediate intrusive, greenish-grey, fg matrix with mafic and fds phenocryst, calcite alteration, hard

16,84 21,67 4,83tuffaceous mafic calc-alkalic volcanics, grey-green, aphanitic to fg, bedding 10-60 to CA, brecciated, calcite and sericite alteration, hard

21,67 35,95 14,28felsic intrusive, pinkish-red, fg matrix with coarse fds phenocryst, silicified, hematite alteration, very hard, 3-5% disseminated py

35,95 50,83 14,88intermediate intrusive, greenish-grey, fg matrix with mafic and ghost fds phenocryst, calcite and hematite alteration, hard, 2-3% py

50,83 58,16 7,33felsic intrusive, pinkish-red, fg matrix with coarse fds phenocryst, silicified, hematite alteration, very hard, 3-5% disseminated py

58,16 64,73 6,57

altered mafic calc-alkalic volcanics, pinkish-brown, aphanitic to fg with mafic phenocryst, brecciated, bleached, chlorite, calcite alteration, hard

64,73 67,95 3,22lamprophyre dyke, dark brown, fg matrix with mafic and ghost fds phenocryst, hematite and calcite alteration, hard

67,95 74,12 6,17

altered mafic calc-alkalic volcanics, pinkish-brown, aphanitic to fg with mafic phenocryst, brecciated, bleached, chlorite, calcite, sericite and hematite alteration, hard

74,12 76,1 1,98lamprophyre dyke, dark brown, fg matrix with mafic and ghost fds phenocryst, calcite alteration, hard

76,10 83,54 7,44mafic calc-alkalic volcanic, pale grey-green, aphanitic to fg, pillowed, brecciated, calcite alteration, 5-15% py

83,54 89,49 5,95

mafic to intermediate intrusive, pale grey-green, fg matrix with mafic and fds phenocryst, lineation 40-50 to CA, calcite alteration, hard, 1-2% py

89,49 167,24 77,75mafic calc-alkalic volcanic, pale grey-green, aphanitic to fg, pillowed, brecciated, calcite alteration, 5-8% py

167,24 251,27 84,03mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, pillowed, brecciated, chlorite, calcite alteration, hard

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments3,18 5,90 2,72 2-3% py3,18 4,4 1,22 vuggy with common limonite staining5,90 6,15 lost core7,20 9,2 2,00 3-5% py9,20 12,19 2,99 2-3% py16,84 19,70 2,86 2-3% py

19,70 21,67 1,97 3-5% py22,40 22,97 0,57 intermediate dyke37,92 38,44 0,52 felsic dyke, pinkish-red, very coarse, fds phenocryst, 5% py45,00 47,10 2,10 felsic dyke, pinkish-red, very coarse, fds phenocryst, 5% py

56,81 57,61 0,80lamprophyre dyke, reddish-brown, fg matrix with mafic phenocryst, calcite and hematite alteration, 2% py

58,16 59,80 1,64 5-8% py

61,38 62,17 0,79intermediate dyke, brown, fg matrix with mafic and ghost fds phenocryst, calcite alteration, hard

62,17 62,90 0,73 15% py

62,90 63,67 0,77tuffaceous section, pale grey-green, fg, bedding 20-45 to CA, sericite and calcite alteration, 15% py

63,67 64,61 0,94intermediate dyke, brown, fg matrix with mafic and fds phenocryst, calcite alteration, hard

67,95 69,16 1,21dark greenish-brown, mafic phenocryst, bedding 15-45 to CA, 10% py

69,16 70,15 0,99 10% py69,16 69,82 0,66 felsic dyke, grey, brecciated, silicified

70,15 70,8 0,65pale grey-green, mafic phenocryst, bedding 15-45 to CA, 8% py

70,80 74,12 3,32 10-15% py76,10 77,9 1,80 10-15% py77,90 79,1 1,20 8-10% py79,20 83,5 4,30 5-8% py89,49 91,1 1,61 5-8% py91,10 104 12,90 3-5% py94,00 95 1,00 1% pyrrhotite104,00 106 2,00 5-8% py and minor pyrrhotite106,00 108 2,00 3-5% py and 1% pyrrhotite108,00 120 12,00 1-2% py, tr pyrrhotite120,00 121 1,00 5% py and minor po121,00 127 6,00 2-3% py, tr po127,00 139 12,00 3-5% py, tr po

DDH Depth

139,00 146,09 7,09 1-2 % py, tr po

146,09 148,25 2,16intermediate dyke, grey, fg to mg, mafic and felsic remnants, calcite alteration, 3% py

146,38 146,7 0,32 mafic dyke, calcite alteration, tr py148,25 153 4,75 2-3% py, tr po153,00 160 7,00 1-2% py, tr pyrrhotite155,85 156,57 0,72 mafic dyke, 1% py160 167,24 7,24 unit becomes increasingly brecciated with chlorite, 2-3% py167,24 195 27,76 1-2% py179,65 180,27 0,62 mafic dyke, grey, fg, 10% irregular veining, calcite alteration195 206 11,00 2-3% fg to mg py206 226 20 1-2% py217 stringer with minor cpy226 234,12 tuffaceous pyroclastics, brecciated, 5-8% py234,12 251,27 1-2% py251,03 251,27 mafic dyke

From To Length Id Description CA Py Po Cpy Sph Gal Mag3,18 5,90 2,72 2-3% py 27,20 9,2 2,00 3-5% py 39,20 12,19 2,99 2-3% py 216,84 19,70 2,86 2-3% py 2

19,70 21,67 1,97 3-5% py 337,92 38,44 0,52 felsic dyke, pinkish-red, very coarse, fds phenocryst, 5% py 5

45,00 47,10 2,10 felsic dyke, pinkish-red, very coarse, fds phenocryst, 5% py 5

58,16 59,80 1,64 5-8% py 5

62,17 62,90 0,73 15% py 15

62,90 63,67 0,77tuffaceous section, pale grey-green, fg, bedding 20-45 to CA, sericite and calcite alteration, 15% py 15

67,95 69,16 1,21dark greenish-brown, mafic phenocryst, bedding 15-45 to CA, 10% py 10

69,16 70,15 0,99 10% py 1070,15 70,8 0,65

pale grey-green, mafic phenocryst, bedding 15-45 to CA, 8% py 8

70,80 74,12 3,32 10-15% py 1076,10 77,9 1,80 10-15% py 1077,90 79,1 1,20 8-10% py 879,20 83,5 4,30 5-8% py 589,49 91,1 1,61 5-8% py 591,10 104 12,90 3-5% py 394,00 95 1,00 1% pyrrhotite 1104,00 106 2,00 5-8% py and minor pyrrhotite 5 tr106,00 108 2,00 3-5% py and 1% pyrrhotite 3 1108,00 120 12,00 1-2% py, tr pyrrhotite 1 tr120,00 121 1,00 5% py and minor po 5 tr121,00 127 6,00 2-3% py, tr po 2 tr127,00 139 12,00 3-5% py, tr po 3 tr139,00 146,09 7,09 1-2 % py, tr po 1 tr

146,09 148,25 2,16intermediate dyke, grey, fg to mg, mafic and felsic remnants, calcite alteration, 3% py 3

146,38 146,7 0,32 mafic dyke, calcite alteration, tr py tr


148,25 153 4,75 2-3% py, tr po 2 tr153,00 160 7,00 1-2% py, tr pyrrhotite 1 tr155,85 156,57 0,72 mafic dyke, 1% py 1160 167,24 7,24 unit becomes increasingly brecciated with chlorite, 2-3% py 2167,24 195 27,76 1-2% py 1195 206 11,00 2-3% fg to mg py 2206 226 20 1-2% py 1217 stringer with minor cpy tr226 234,12 tuffaceous pyroclastics, brecciated, 5-8% py 5234,12 251,27 1-2% py 1

HoleIDSample Number


Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-06 12012 3,18 4,00 0,82 0,020 0,020C08-06 12013 4,00 5,00 1,00 0,010 0,010 0,010C08-06 12014 5,00 5,90 0,90 0,000 0,000C08-06 12015 6,15 7,20 1,05 0,000 0,000C08-06 12016OREAS 15Pa Batch 1 Can 1,040 1,040C08-06 12017 7,20 8,20 1,00 0,000 0,000C08-06 12018 8,20 9,20 1,00 0,000 0,000C08-06 12019 9,20 10,20 1,00 0,000 0,000C08-06 12020 10,20 11,20 1,00 0,010 0,010C08-06 12021 11,20 12,19 0,99 0,010 0,010C08-06 12022 12,19 13,00 0,81 0,000 0,000C08-06 12023 13,00 14,00 1,00 0,000 0,000 0,000C08-06 12024 14,00 15,00 1,00 0,000 0,000C08-06 12025 15,00 16,00 1,00 0,000 0,000C08-06 12026 16,00 16,84 0,84 0,000 0,000C08-06 12027 16,84 17,80 0,96 0,000 0,000C08-06 12028 17,80 18,70 0,90 0,000 0,000C08-06 12029 18,70 19,70 1,00 0,010 0,010C08-06 12030OREAS 15Pa Batch 1 Can 1,010 1,010C08-06 12031 19,70 20,70 1,00 0,010 0,010C08-06 12032 20,70 21,67 0,97 0,010 0,010C08-06 12033 21,67 22,40 0,73 0,030 0,030C08-06 12034 22,40 22,97 0,57 0,000 0,000C08-06 12035 22,97 24,00 1,03 0,030 0,030C08-06 12036 24,00 25,00 1,00 0,010 0,010 0,010C08-06 12037 25,00 26,00 1,00 0,030 0,030C08-06 12038 26,00 27,00 1,00 0,010 0,010C08-06 12039 27,00 28,00 1,00 0,020 0,020C08-06 12040 28,00 29,00 1,00 0,080 0,080C08-06 12041 29,00 30,00 1,00 0,030 0,030C08-06 12042 30,00 31,08 1,08 0,040 0,040C08-06 12043 31,08 32,00 0,92 0,010 0,010C08-06 12044 32,00 33,00 1,00 0,010 0,010C08-06 12045DIABASE 101.5-102.0 0,010 0,010C08-06 12046 33,00 34,00 1,00 0,000 0,000C08-06 12047 34,00 35,00 1,00 0,010 0,010

C08-06 12048 35,00 35,95 0,95 0,010 0,020 0,015C08-06 12049 35,95 37,00 1,05 0,000 0,000C08-06 12050 37,00 37,92 0,92 0,010 0,010C08-06 12051 37,92 39,00 1,08 0,010 0,010C08-06 12052 39,00 40,00 1,00 0,310 0,340 0,325C08-06 12053 40,00 41,00 1,00 0,010 0,010C08-06 12054 41,00 42,00 1,00 0,010 0,010C08-06 12055 42,00 43,00 1,00 0,010 0,010C08-06 12056 43,00 44,00 1,00 0,050 0,050C08-06 12057 44,00 45,00 1,00 0,000 0,000C08-06 12058 45,00 46,00 1,00 0,000 0,000C08-06 12059 46,00 47,10 1,10 0,000 0,000C08-06 12060 47,10 48,00 0,90 0,000 0,000 0,000C08-06 12061 48,00 49,00 1,00 0,000 0,000C08-06 12062 49,00 50,00 1,00 0,000 0,000C08-06 12063 50,00 50,83 0,83 0,000 0,000C08-06 12064 50,83 51,80 0,97 0,010 0,010C08-06 12065 51,80 52,80 1,00 0,010 0,010C08-06 12066 52,80 53,80 1,00 0,030 0,030C08-06 12067OREAS 15Pa Batch 1 Can 0,990 0,990C08-06 12068 53,80 54,80 1,00 0,040 0,040C08-06 12069 54,80 55,80 1,00 0,020 0,020C08-06 12070 55,80 56,81 1,01 0,020 0,020C08-06 12071 56,81 57,61 0,80 0,000 0,000 0,000C08-06 12072 57,61 58,16 0,55 0,020 0,020C08-06 12073 58,16 59,00 0,84 0,000 0,000C08-06 12074 59,00 59,80 0,80 0,020 0,020C08-06 12075 59,80 60,60 0,80 0,010 0,010C08-06 12076 60,60 61,38 0,78 0,020 0,020C08-06 12077 61,38 62,17 0,79 0,000 0,000C08-06 12078 62,17 62,90 0,73 0,040 0,040C08-06 12079 62,90 63,67 0,77 0,040 0,080 0,060C08-06 12080 63,67 64,73 1,06 0,000 0,000C08-06 12081 64,73 65,80 1,07 0,000 0,000C08-06 12082 65,80 66,90 1,10 0,000 0,000C08-06 12083 66,90 67,95 1,05 0,000 0,000C08-06 12084 67,95 68,55 0,60 0,010 0,010 0,010C08-06 12085 68,55 69,16 0,61 0,010 0,010

C08-06 12086 69,16 70,15 0,99 0,030 0,030C08-06 12087 70,15 70,80 0,65 0,000 0,000C08-06 12088 70,80 71,70 0,90 0,030 0,030C08-06 12089OREAS 15Pa Batch 1 Can 0,990 0,990C08-06 12090 71,70 72,50 0,80 0,020 0,020C08-06 12091 72,50 73,30 0,80 0,010 0,010C08-06 12092 73,30 74,12 0,82 0,010 0,010C08-06 12093 74,12 75,10 0,98 0,000 0,000C08-06 12094 75,10 76,10 1,00 0,000 0,000C08-06 12095 76,10 77,00 0,90 0,050 0,050C08-06 12096 77,00 77,90 0,90 0,040 0,040C08-06 12097 77,90 78,80 0,90 0,010 0,010 0,010C08-06 12098 78,80 79,70 0,90 0,010 0,010C08-06 12099 79,70 80,60 0,90 0,010 0,010C08-06 12100 80,60 81,60 1,00 0,010 0,010C08-06 12101 81,60 82,60 1,00 0,000 0,000C08-06 12102 82,60 83,54 0,94 0,000 0,000C08-06 12103 83,54 84,50 0,96 0,000 0,000C08-06 12104 84,50 85,50 1,00 0,000 0,000C08-06 12105 85,50 86,50 1,00 0,000 0,000C08-06 12106 86,50 87,50 1,00 0,010 0,010C08-06 12107 87,50 88,60 1,10 0,010 0,010C08-06 12108 88,60 89,49 0,89 0,000 0,000C08-06 12109 89,49 90,30 0,81 0,000 0,020 0,010C08-06 12110 90,30 91,10 0,80 0,010 0,010C08-06 12111 QUARTZ Purchased 0,000 0,000C08-06 12112 91,10 92,00 0,90 0,000 0,000C08-06 12113 92,00 93,00 1,00 0,000 0,000C08-06 12114 93,00 94,00 1,00 0,000 0,000C08-06 12115 94,00 95,00 1,00 0,010 0,010C08-06 12116 95,00 96,00 1,00 0,010 0,000 0,005C08-06 12117 96,00 97,00 1,00 0,000 0,000C08-06 12118 97,00 98,00 1,00 0,000 0,000C08-06 12119 98,00 99,00 1,00 0,020 0,020C08-06 12120 99,00 100,00 1,00 0,000 0,000C08-06 12121 100,00 101,00 1,00 0,010 0,010C08-06 12122 101,00 102,00 1,00 0,000 0,000C08-06 12123 102,00 103,00 1,00 0,000 0,000

C08-06 12124 103,00 104,00 1,00 0,000 0,000C08-06 12125 104,00 105,00 1,00 0,020 0,040 0,030C08-06 12126 105,00 106,00 1,00 0,010 0,010C08-06 12127 106,00 107,00 1,00 0,000 0,000C08-06 12128 107,00 108,00 1,00 0,000 0,000C08-06 12129 108,00 109,00 1,00 0,000 0,000C08-06 12130 109,00 110,00 1,00 0,010 0,010C08-06 12131 110,00 111,00 1,00 0,000 0,000C08-06 12132OREAS 15Pa Batch 1 Can 1,010 1,010C08-06 12133 111,00 112,00 1,00 0,020 0,020C08-06 12134 112,00 113,00 1,00 0,000 0,010 0,005C08-06 12135 113,00 114,00 1,00 0,000 0,000C08-06 12136 114,00 115,00 1,00 0,010 0,010C08-06 12137 115,00 116,00 1,00 0,000 0,000C08-06 12138 116,00 117,00 1,00 0,000 0,000C08-06 12139 117,00 118,00 1,00 0,000 0,000C08-06 12140 118,00 119,00 1,00 0,010 0,010C08-06 12141 119,00 120,00 1,00 0,010 0,010C08-06 12142 120,00 121,00 1,00 0,010 0,010C08-06 12143 121,00 122,00 1,00 0,010 0,010C08-06 12144OREAS 15Pa Batch 1 Can 1,020 1,020C08-06 12145 122,00 123,00 1,00 0,000 0,000C08-06 12146 123,00 124,00 1,00 0,010 0,010C08-06 12147 124,00 125,00 1,00 0,010 0,010C08-06 12148 125,00 126,00 1,00 0,000 0,000C08-06 12149 126,00 127,00 1,00 0,000 0,000C08-06 12150 127,00 128,00 1,00 0,010 0,010C08-06 12151 128,00 129,00 1,00 0,000 0,000 0,000C08-06 12152 129,00 130,00 1,00 0,000 0,000C08-06 12153 130,00 131,00 1,00 0,010 0,010C08-06 12154 131,00 132,00 1,00 0,020 0,020C08-06 12155 132,00 133,00 1,00 0,010 0,000 0,005C08-06 12156 133,00 134,00 1,00 0,010 0,010C08-06 12157 134,00 135,00 1,00 0,010 0,010C08-06 12158 135,00 136,00 1,00 0,010 0,010C08-06 12159 136,00 137,00 1,00 0,020 0,020C08-06 12160 137,00 138,00 1,00 0,020 0,020C08-06 12161 138,00 139,00 1,00 0,000 0,000

C08-06 12162 139,00 140,00 1,00 0,010 0,010C08-06 12163 140,00 141,00 1,00 0,000 0,000C08-06 12164 141,00 142,00 1,00 0,000 0,000C08-06 12165 142,00 143,00 1,00 0,000 0,000C08-06 12166 143,00 144,00 1,00 0,000 0,000C08-06 12167DIABASE 102.0-102.5 0,000 0,000 0,000C08-06 12168 144,00 145,00 1,00 0,000 0,000C08-06 12169 145,00 146,09 1,09 0,000 0,000C08-06 12170 146,09 147,20 1,11 0,000 0,000C08-06 12171 147,20 148,25 1,05 0,010 0,010C08-06 12172 148,25 149,10 0,85 0,010 0,010C08-06 12173 149,10 150,00 0,90 0,010 0,010C08-06 12174 150,00 151,00 1,00 0,030 0,000 0,015C08-06 12175 151,00 152,00 1,00 0,010 0,010C08-06 12176 152,00 153,00 1,00 0,020 0,020C08-06 12177 153,00 154,00 1,00 0,000 0,000C08-06 12178 154,00 155,00 1,00 0,010 0,010C08-06 12179 155,00 155,85 0,85 0,000 0,000C08-06 12180 155,85 156,90 1,05 0,010 0,010C08-06 12181 156,90 158,00 1,10 0,010 0,010C08-06 12182 158,00 159,00 1,00 0,010 0,010C08-06 12183 159,00 160,00 1,00 0,010 0,010C08-06 12184 160,00 161,00 1,00 0,010 0,010C08-06 12185 161,00 162,00 1,00 0,000 0,000C08-06 12186 162,00 163,00 1,00 0,000 0,000C08-06 12187 163,00 164,00 1,00 0,000 0,000C08-06 12188OREAS 15Pa Batch 1 Can 1,010 1,010C08-06 12189 164,00 164,80 0,80 0,010 0,010C08-06 12190 164,80 165,60 0,80 0,000 0,010 0,005C08-06 12191 165,60 166,40 0,80 0,000 0,000C08-06 12192 166,40 167,24 0,84 0,010 0,010C08-06 12193 167,24 168,10 0,86 0,020 0,020 0,020C08-06 12194 168,10 169,00 0,90 0,000 0,000C08-06 12195 169,00 170,00 1,00 0,000 0,000C08-06 12196 170,00 171,00 1,00 0,000 0,000C08-06 12197 171,00 172,00 1,00 0,000 0,000C08-06 12198 172,00 173,00 1,00 0,000 0,000C08-06 12199 173,00 174,00 1,00 0,000 0,000

C08-06 12200 174,00 175,00 1,00 0,000 0,000C08-06 12201 175,00 176,00 1,00 0,000 0,000C08-06 12202 176,00 177,00 1,00 0,000 0,000C08-06 12203 177,00 178,00 1,00 0,000 0,000C08-06 12204 178,00 178,80 0,80 0,000 0,000C08-06 12205 178,80 179,65 0,85 0,000 0,010 0,005C08-06 12206 179,65 180,27 0,62 0,000 0,000C08-06 12207 180,27 181,10 0,83 0,000 0,000C08-06 12208 181,10 182,00 0,90 0,000 0,000C08-06 12209 182,00 183,00 1,00 0,000 0,000C08-06 12210 183,00 184,00 1,00 0,000 0,000C08-06 12211 184,00 185,00 1,00 0,000 0,000C08-06 12212OREAS 15Pa Batch 1 Can 1,010 1,010C08-06 12213 185,00 186,00 1,00 0,000 0,000C08-06 12214 186,00 187,00 1,00 0,010 0,010C08-06 12215 187,00 188,00 1,00 0,000 0,000C08-06 12216 188,00 189,00 1,00 0,010 0,010C08-06 12217 189,00 190,00 1,00 0,000 0,000C08-06 12218 190,00 191,00 1,00 0,000 0,000 0,000C08-06 12219 191,00 192,00 1,00 0,000 0,000C08-06 12220 192,00 193,00 1,00 0,000 0,000C08-06 12221 193,00 194,00 1,00 0,000 0,000C08-06 12222 194,00 195,00 1,00 0,000 0,000C08-06 12223 195,00 196,00 1,00 0,010 0,010C08-06 12224 196,00 197,00 1,00 0,010 0,010C08-06 12225 197,00 198,00 1,00 0,010 0,030 0,020C08-06 12226 198,00 199,00 1,00 0,010 0,010C08-06 12227 199,00 200,00 1,00 0,000 0,000C08-06 12228 200,00 201,00 1,00 0,000 0,000C08-06 12229 201,00 202,00 1,00 0,020 0,020C08-06 12230 202,00 203,00 1,00 0,000 0,000C08-06 12231 203,00 204,00 1,00 0,000 0,000C08-06 12232 204,00 205,00 1,00 0,000 0,000C08-06 12233 QUARTZ Purchased 0,010 0,010C08-06 12234 205,00 206,00 1,00 0,000 0,000 0,000C08-06 12235 206,00 207,00 1,00 0,000 0,000C08-06 12236 207,00 208,00 1,00 0,000 0,000C08-06 12237 208,00 209,00 1,00 0,000 0,000

C08-06 12238 209,00 210,00 1,00 0,000 0,000C08-06 12239 210,00 211,00 1,00 0,000 0,000C08-06 12240 211,00 212,00 1,00 0,000 0,000C08-06 12241 212,00 213,00 1,00 0,000 0,000C08-06 12242 213,00 214,00 1,00 0,010 0,000 0,005C08-06 12243 214,00 215,00 1,00 0,000 0,000C08-06 12244 215,00 216,00 1,00 0,000 0,000C08-06 12245 216,00 217,00 1,00 0,000 0,000C08-06 12246 217,00 218,00 1,00 0,000 0,000C08-06 12247 218,00 219,00 1,00 0,000 0,000C08-06 12248OREAS 15Pa Batch 1 Can 1,000 1,000C08-06 12249 219,00 220,00 1,00 0,000 0,000C08-06 12250 220,00 221,00 1,00 0,000 0,000C08-06 12251 221,00 222,00 1,00 0,000 0,000C08-06 12252 222,00 223,00 1,00 0,000 0,000 0,000C08-06 12253 223,00 224,00 1,00 0,000 0,000C08-06 12254 224,00 225,00 1,00 0,000 0,000C08-06 12255 225,00 226,00 1,00 0,000 0,000C08-06 12256 226,00 227,00 1,00 0,000 0,000C08-06 12257 227,00 228,00 1,00 0,000 0,000C08-06 12258 228,00 229,00 1,00 0,020 0,020C08-06 12259 229,00 230,00 1,00 0,010 0,010C08-06 12260 230,00 231,00 1,00 0,010 0,000 0,005C08-06 12261 231,00 232,00 1,00 0,000 0,000C08-06 12262 232,00 233,00 1,00 0,000 0,000C08-06 12263 233,00 234,12 1,12 0,010 0,010C08-06 12264OREAS 15Pa Batch 1 Can 0,990 0,990C08-06 12265 234,12 235,00 0,88 0,000 0,000C08-06 12266 235,00 236,00 1,00 0,000 0,000C08-06 12267 236,00 237,00 1,00 0,020 0,020C08-06 12268 237,00 238,00 1,00 0,000 0,000C08-06 12269 238,00 239,00 1,00 0,010 0,010C08-06 12270 239,00 240,00 1,00 0,010 0,010C08-06 12271 240,00 241,00 1,00 0,000 0,000C08-06 12272 241,00 242,00 1,00 0,000 0,000C08-06 12273 242,00 243,00 1,00 0,000 0,000C08-06 12274 243,00 244,00 1,00 0,000 0,000C08-06 12275 244,00 245,00 1,00 0,000 0,000

C08-06 12276 245,00 246,00 1,00 0,000 0,000C08-06 12277 246,00 247,00 1,00 0,000 0,010 0,005C08-06 12278 247,00 248,00 1,00 0,000 0,000C08-06 12279 248,00 248,80 0,80 0,000 0,000C08-06 12280 248,80 249,60 0,80 0,000 0,000C08-06 12281 249,60 250,40 0,80 0,000 0,000C08-06 12282 250,40 251,27 0,87 0,000 0,000


3,18 5 1,82 1,82 100% 0,97 0,85 47%5 8 3 2,75 92% 0,25 2,75 92%8 11 3 3,04 101% 0,65 2,35 78%11 14 3 2,92 97% 0,52 2,48 83%14 17 3 3,01 100% 0,50 2,50 83%17 20 3 3,01 100% 0,16 2,84 95%20 23 3 2,98 99% 0,31 2,69 90%23 26 3 3,01 100% 0,21 2,79 93%26 29 3 2,87 96% 0,52 2,48 83%29 32 3 3,07 102% 0,26 2,74 91%32 35 3 3,05 102% 0,61 2,39 80%35 38 3 3,05 102% 0,82 2,18 73%38 41 3 2,96 99% 0,68 2,32 77%41 44 3 2,98 99% 0,50 2,50 83%44 47 3 3 100% 1,10 1,90 63%47 50 3 2,95 98% 0,15 2,85 95%50 53 3 3,04 101% 0,22 2,78 93%53 56 3 3,02 101% 0,30 2,70 90%56 59 3 3,03 101% 0,50 2,50 83%59 62 3 2,96 99% 0,00 3,00 100%62 65 3 3,06 102% 0,22 2,78 93%65 68 3 3,00 100% 0,22 2,78 93%68 71 3 2,98 99% 0,42 2,58 86%71 74 3 3,01 100% 0,00 3,00 100%74 77 3 3,03 101% 0,19 2,81 94%77 80 3 3,01 100% 0,00 3,00 100%80 83 3 3,00 100% 0,00 3,00 100%83 86 3 3 100% 0,90 2,10 70%86 89 3 2,94 98% 0,37 2,63 88%89 92 3 3,10 103% 0,04 2,96 99%92 95 3 3,04 101% 0,23 2,77 92%95 98 3 3,01 100% 0,00 3,00 100%98 101 3 2,99 100% 0,00 3,00 100%101 104 3 3,03 101% 0,05 2,95 98%104 107 3 2,95 98% 0,14 2,86 95%107 110 3 3,07 102% 0,00 3,00 100%110 113 3 2,98 99% 0,18 2,82 94%113 116 3 2,93 98% 0,00 3,00 100%116 119 3 3,06 102% 0,16 2,84 95%119 122 3 3,05 102% 0,11 2,89 96%122 125 3 3,01 100% 0,22 2,78 93%125 128 3 2,94 98% 0,00 3,00 100%128 131 3 2,98 99% 0,00 3,00 100%131 134 3 3,04 101% 0,08 2,92 97%134 137 3 3,04 101% 0,04 2,96 99%137 140 3 2,95 98% 0,07 2,93 98%

140 143 3 3,01 100% 0,07 2,93 98%143 146 3 3,00 100% 0,00 3,00 100%146 149 3 3,00 100% 0,29 2,71 90%149 152 3 2,90 97% 0,00 3,00 100%152 155 3 3,05 102% 0,00 3,00 100%155 158 3 3,05 102% 0,08 2,92 97%158 161 3 3,00 100% 0,70 2,30 77%161 164 3 3,00 100% 0,95 2,05 68%164 167 3 3,00 100% 1,40 1,60 53%167 170 3 2,99 100% 0,00 3,00 100%170 173 3 3,03 101% 0,00 3,00 100%173 176 3 2,96 99% 0,11 2,89 96%176 179 3 3,00 100% 0,67 2,33 78%179 182 3 3,00 100% 0,38 2,62 87%182 185 3 2,96 99% 0,18 2,82 94%185 188 3 3,01 100% 0,00 3,00 100%188 191 3 2,93 98% 0,00 3,00 100%191 194 3 3,09 103% 0,00 3,00 100%194 197 3 3,00 100% 0,05 2,95 98%197 200 3 2,96 99% 0,00 3,00 100%200 203 3 3,07 102% 0,00 3,00 100%203 206 3 3,03 101% 0,00 3,00 100%206 209 3 2,98 99% 0,26 2,74 91%209 212 3 3,00 100% 0,00 3,00 100%212 215 3 3,01 100% 0,07 2,93 98%215 218 3 3,02 101% 0,00 3,00 100%218 221 3 2,98 99% 0,65 2,35 78%221 224 3 3,15 105% 0,00 3,00 100%224 227 3 2,95 98% 0,00 3,00 100%227 230 3 3,03 101% 0,00 3,00 100%230 233 3 2,96 99% 0,08 2,92 97%233 236 3 2,95 98% 0,02 2,98 99%236 239 3 3,00 100% 0,11 2,89 96%239 242 3 2,95 98% 0,75 2,25 75%242 245 3 3,00 100% 0,28 2,72 91%245 248 3 3,03 101% 0,24 2,76 92%248 251 3 2,99 100% 0,00 3,00 100%


C08-07 L-100E 1550N 300 0 -50 302m 08-août-08 15-août-08


20,05 125,26 105,21mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, spherules, brecciated, calcite alteration, silicification, hard, 1-2% py

125,26 135,85 10,59mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, spherules, brecciated, calcite alteration, silicification, hard to very hard, variolitic


150,04 158,07 8,03 Dyke Swarm see Geol 2 for more info


214,08 255,6 41,52

mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, spherules, brecciated, calcite alteration, silicification, hard to very hard, variolitic and pillowed

255,60 299,7 44,10mafic intrusive, diabase dyke, grey-green, mg to coarse grain, massive, uniform, epidote alteration, hard, magnetic

299,70 301,94 2,24chert/graphitic argillites, pinkish-buff, mixed graphitic argillites, bedding 15-30 to CA, silicified, very hard

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments21,54 21,86 0,32 mafic dyke24,82 25,05 0,23 lost core45,58 46,06 0,48 mafic dyke, vuggy, medium green, tr py60,10 60,31 0,21 mafic dyke

90,54 90,78 0,24mafic dyke, dark brown, fg matrix with mafic phenocryst, 5% py

96,18 96,45 0,27 mafic dyke, dark brown, fg matrix with mafic phenocryst, tr py

97,67 98,83 1,16mafic dyke, dark brown, fg matrix with mafic phenocryst, hematite staining, 5% py

100,45 101,05 0,60mafic dyke, dark brown, fg matrix with mafic and fds phenocryst, hematite staining, 5% py

102,20 102,54 0,34mafic dyke, grey-green with mafic phenocryst, hematite staining, tr py

114,89 115,30 0,41 mafic dyke, pinkish-brown, with mafic phenocryst, minor py125,26 127,00 1,74 2-3% py126,13 126,32 0,19 25 irregular and brecciated chert fragment127,00 135,00 8,00 1-2% py135,00 135,85 0,85 5% py135,27 135,76 0,49 shear zone, foliation 35-50 to CA, breccia

135,76 135,85 0,09mafic dyke, purplish-grey, fg matrix and mafic phenocryst, 10% disseminated py

140,18 140,62 0,44 mafic dyke, grey-green with mafic phenocryst149,21 149,48 0,27 brecciated veinlet, 10% scattered py

150,04 151,52 1,48

Lamprophyre dyke, dark brown, fg matrix with mafic phenocryst, lineation 40-60 to CA, calcite alteration, hard, 2% py

151,52 154,56 3,04Mafic dyke, grey-green, fg matrix with mafic phenocryst, hematite and calcite alteration, hard, 2-3% py

154,56 155,7 1,14

Lamprophyre dyke, dark brown, fg matrix with mafic phenocryst, lineation 35-60 to CA, calcite alteration, hard, 3% py

155,70 156,59 0,89

Syenite dyke, pinkish-red, aphanitic matrix with fds phenocryst, shearing 50-60 to CA, brecciated, hematite staining, hard, 5% py

156,59 158,07 1,48Mafic dyke, grey-green, fg matrix with mafic phenocryst, hematite and calcite alteration, hard, 1-2% py

159,48 159,74 0,26 mafic dyke, grey-green with mafic phenocryst, tr py

161,74 162,23 0,49mafic dyke, greenish-brown, fg matrix with mafic phenocryst, minor py

DDH Depth

173,73 173,89 0,16 grey mafic dyke

199,03 202,56 3,53Variolitic felsic volcanics, common clusters of pale greenish, varioles 3mm to 1cm, 2-3% py

214,08 217 2,92 1-2% py217,00 220 3,00 3-5% py220,00 222,28 2,28 2-3% py222,28 223,06 0,78 grey mafic dyke, fg, calcite alteration, 2% py223,06 223,38 0,32 2% py

223,38 224,87 1,49Lamprophyre dyke, greyish-brown, fg matrix with mafic phenocryst, lineation 30-40 to CA, calcite alteration, 3% py

224,87 231,8 6,93 2-3% py231,80 233,81 2,01 3-5% py

233,81 236,1 2,29Lamprophyre dyke, pinkish-brown, fg with mafic phenocryst, lineation 40-60 to CA, brecciated, calcite alteration, 3-5% py

235,36 235,54 0,18 mafic dyke, 3% py236,1 237,46 1,36 2-3% py

237,46 241,29 3,83Lamprophyre dyke, greyish-brown, fg matrix with mafic phenocryst, lineation 30-40 to CA, calcite alteration, 3-5% py

241,29 249,58 8,29 unit becomes pale greenish-grey, 1-2% py

246,37 246,79 0,42Intermediate dyke, pale greenish-brown, fg matrix with mafic and fds phenocryst, calcite alteration, hard, minor py

249,58 251,68 2,10Intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, silicified, 3% py

251,68 253,75 2,07 2-3% py

253,75 254,49 0,74Intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, silicified, 2% py

254,49 255,6 1,11 2% py297,82 298,45 0,63 3% py

298,53 299,4 0,87Feldspar porphyry, purplish-brown, fg matrix with zoned fds phenocryst, brecciated, 5% diabase fragments, silicified, very hard, 5% py

299,7 300,6 0,90 pale green section, rare chert, no bedding, minor py300,6 301,94 1,34 5-8% py

From To Length Id Description CA Py Po Cpy Sph Gal Mag90,54 90,78 0,24

mafic dyke, dark brown, fg matrix with mafic phenocryst, 5% py 5

96,18 96,45 0,27mafic dyke, dark brown, fg matrix with mafic phenocryst, tr py tr

97,67 98,83 1,16mafic dyke, dark brown, fg matrix with mafic phenocryst, hematite staining, 5% py 5

100,45 101,05 0,60mafic dyke, dark brown, fg matrix with mafic and fds phenocryst, hematite staining, 5% py 5

102,20 102,54 0,34mafic dyke, grey-green with mafic phenocryst, hematite staining, tr py tr

114,89 115,30 0,41mafic dyke, pinkish-brown, with mafic phenocryst, minor py tr

125,26 127,00 1,74 2-3% py 2

127,00 135,00 8,00 1-2% py 1135,00 135,85 0,85 5% py 5

135,85 135,85 0,00mafic dyke, purplish-grey, fg matrix and mafic phenocryst, 10% disseminated py 10

149,21 149,48 0,27 brecciated veinlet, 10% scattered py 10

150,04 151,52 1,48

Lamprophyre dyke, dark brown, fg matrix with mafic phenocryst, lineation 40-60 to CA, calcite alteration, hard, 2% py 40 2

151,52 154,56 3,04

Mafic dyke, grey-green, fg matrix with mafic phenocryst, hematite and calcite alteration, hard, 2-3% py 2

154,56 155,7 1,14

Lamprophyre dyke, dark brown, fg matrix with mafic phenocryst, lineation 35-60 to CA, calcite alteration, hard, 3% py 35 3

155,70 156,59 0,89

Syenite dyke, pinkish-red, aphanitic matrix with fds phenocryst, shearing 50-60 to CA, brecciated, hematite staining, hard, 5% py 50 5

156,59 158,07 1,48

Mafic dyke, grey-green, fg matrix with mafic phenocryst, hematite and calcite alteration, hard, 1-2% py 1

199,03 202,56 3,53Variolitic felsic volcanics, common clusters of pale greenish, varioles 3mm to 1cm, 2-3% py 2

214,08 217 2,92 1-2% py 1217,00 220 3,00 3-5% py 3220,00 222,28 2,28 2-3% py 2222,28 223,06 0,78 grey mafic dyke, fg, calcite alteration, 2% py 2


223,06 223,38 0,32 2% py 2

223,38 224,87 1,49Lamprophyre dyke, greyish-brown, fg matrix with mafic phenocryst, lineation 30-40 to CA, calcite alteration, 3% py 30 3

224,87 231,8 6,93 2-3% py 2231,80 233,81 2,01 3-5% py 3

233,81 236,1 2,29Lamprophyre dyke, pinkish-brown, fg with mafic phenocryst, lineation 40-60 to CA, brecciated, calcite alteration, 3-5% py 40 3

235,36 235,54 0,18 mafic dyke, 3% py 3236,1 237,46 1,36 2-3% py 2

237,46 241,29 3,83Lamprophyre dyke, greyish-brown, fg matrix with mafic phenocryst, lineation 30-40 to CA, calcite alteration, 3-5% py 30 5

241,29 249,58 8,29 unit becomes pale greenish-grey, 1-2% py 1

249,58 251,68 2,10Intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, silicified, 3% py 3

251,68 253,75 2,07 2-3% py 2

253,75 254,49 0,74Intermediate dyke, pinkish-brown, fg matrix with mafic and fds phenocryst, silicified, 2% py 2

254,49 255,6 1,11 2% py 2297,82 298,45 0,63 3% py 3

298,53 299,4 0,87

Feldspar porphyry, purplish-brown, fg matrix with zoned fds phenocryst, brecciated, 5% diabase fragments, silicified, very hard, 5% py 5

300,6 301,94 1,34 5-8% py 5

HoleIDSample Number


Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-07 12283 20,05 21,00 0,95 0,000 0,010 0,005C08-07 12284 21,00 22,00 1,00 0,000 0,000C08-07 12285 22,00 23,00 1,00 0,000 0,000C08-07 12286 23,00 24,00 1,00 0,000 0,000C08-07 12287 24,00 24,82 0,82 0,000 0,000C08-07 12288 25,05 26,00 0,95 0,000 0,000C08-07 12289 26,00 27,00 1,00 0,000 0,000C08-07 12290 DIABASE 102.0-102.5 0,000 0,000C08-07 12291 27,00 28,00 1,00 0,000 0,000C08-07 12292 28,00 29,00 1,00 0,010 0,010C08-07 12293 29,00 30,00 1,00 0,010 0,000 0,005C08-07 12294 30,00 31,00 1,00 0,000 0,000C08-07 12295 31,00 32,00 1,00 0,000 0,000C08-07 12296 32,00 33,00 1,00 0,010 0,010C08-07 12297 33,00 34,00 1,00 0,010 0,010C08-07 12298 34,00 35,00 1,00 0,010 0,010C08-07 12299 35,00 36,00 1,00 0,010 0,010C08-07 12300 36,00 37,00 1,00 0,010 0,010C08-07 12301 37,00 38,00 1,00 0,010 0,010C08-07 12302 38,00 39,00 1,00 0,010 0,010C08-07 12303 39,00 40,00 1,00 0,010 0,010C08-07 12304 40,00 41,00 1,00 0,010 0,000 0,005C08-07 12305 41,00 42,00 1,00 0,020 0,020C08-07 12306 42,00 43,00 1,00 0,010 0,010C08-07 12307 43,00 44,00 1,00 0,010 0,010C08-07 12308 44,00 45,00 1,00 0,010 0,010C08-07 12309 45,00 46,06 1,06 0,050 0,050C08-07 12310 46,06 47,00 0,94 0,010 0,010C08-07 12311 47,00 48,00 1,00 0,010 0,010C08-07 12312 OREAS 15Pa Batch 1 Can 0,990 0,990C08-07 12313 48,00 49,00 1,00 0,000 0,000C08-07 12314 49,00 50,00 1,00 0,000 0,000C08-07 12315 50,00 51,00 1,00 0,030 0,030C08-07 12316 51,00 52,00 1,00 0,000 0,000C08-07 12317 52,00 53,00 1,00 0,010 0,010C08-07 12318 53,00 54,00 1,00 0,000 0,000 0,000C08-07 12319 54,00 55,00 1,00 0,000 0,000C08-07 12320 55,00 56,00 1,00 0,000 0,000C08-07 12321 56,00 57,00 1,00 0,000 0,000C08-07 12322 57,00 58,00 1,00 0,000 0,000

C08-07 12323 58,00 59,00 1,00 0,000 0,000C08-07 12324 59,00 60,00 1,00 0,010 0,010C08-07 12325 60,00 61,00 1,00 0,010 0,010C08-07 12326 61,00 62,00 1,00 0,000 0,000C08-07 12327 OREAS 15Pa Batch 1 Can 1,000 1,000C08-07 12328 62,00 63,00 1,00 0,020 0,020C08-07 12329 63,00 64,00 1,00 0,000 0,010 0,005C08-07 12330 64,00 65,00 1,00 0,000 0,000C08-07 12331 65,00 66,00 1,00 0,010 0,010C08-07 12332 66,00 67,00 1,00 0,000 0,000C08-07 12333 67,00 68,00 1,00 0,000 0,000C08-07 12334 68,00 69,00 1,00 0,000 0,000C08-07 12335 69,00 70,00 1,00 0,010 0,010C08-07 12336 70,00 71,00 1,00 0,000 0,000C08-07 12337 71,00 72,00 1,00 0,000 0,000C08-07 12338 72,00 73,00 1,00 0,020 0,000 0,010C08-07 12339 73,00 74,00 1,00 0,000 0,000C08-07 12340 74,00 75,00 1,00 0,010 0,010C08-07 12341 75,00 76,00 1,00 0,000 0,000C08-07 12342 76,00 77,00 1,00 0,000 0,000C08-07 12343 77,00 78,00 1,00 0,010 0,010C08-07 12344 QUARTZ Purchased 0,000 0,000C08-07 12345 78,00 79,00 1,00 0,010 0,010C08-07 12346 79,00 80,00 1,00 0,010 0,010C08-07 12347 80,00 81,00 1,00 0,000 0,000C08-07 12348 81,00 82,00 1,00 0,000 0,000C08-07 12349 82,00 83,00 1,00 0,010 0,010C08-07 12350 83,00 84,00 1,00 0,010 0,010 0,010C08-07 12351 84,00 85,00 1,00 0,010 0,010C08-07 12352 85,00 86,00 1,00 0,000 0,000C08-07 12353 86,00 87,00 1,00 0,010 0,010C08-07 12354 87,00 88,00 1,00 0,010 0,010C08-07 12355 88,00 89,00 1,00 0,010 0,010C08-07 12356 89,00 90,00 1,00 0,000 0,000C08-07 12357 90,00 91,00 1,00 0,000 0,000C08-07 12358 91,00 92,00 1,00 0,020 0,020C08-07 12359 92,00 93,00 1,00 0,000 0,000 0,000C08-07 12360 93,00 94,00 1,00 0,000 0,000C08-07 12361 94,00 95,00 1,00 0,000 0,000C08-07 12362 95,00 96,00 1,00 0,010 0,010C08-07 12363 96,00 96,80 0,80 0,020 0,020C08-07 12364 96,80 97,67 0,87 0,010 0,010

C08-07 12365 97,67 98,83 1,16 0,010 0,000 0,005C08-07 12366 98,83 99,65 0,82 0,010 0,010C08-07 12367 99,65 100,45 0,80 0,010 0,010C08-07 12368 100,45 101,05 0,60 0,010 0,010 0,010C08-07 12369 OREAS 15Pa Batch 1 Can 0,990 0,990C08-07 12370 101,05 102,00 0,95 0,010 0,010C08-07 12371 102,00 103,00 1,00 0,020 0,020C08-07 12372 103,00 104,00 1,00 0,000 0,000C08-07 12373 104,00 105,00 1,00 0,010 0,010C08-07 12374 105,00 106,00 1,00 0,000 0,000C08-07 12375 106,00 107,00 1,00 0,010 0,010C08-07 12376 107,00 108,00 1,00 0,010 0,010C08-07 12377 108,00 109,00 1,00 0,010 0,010C08-07 12378 109,00 110,00 1,00 0,010 0,000 0,005C08-07 12379 110,00 111,00 1,00 0,010 0,010C08-07 12380 111,00 112,00 1,00 0,010 0,010C08-07 12381 112,00 113,00 1,00 0,010 0,010C08-07 12382 113,00 114,00 1,00 0,010 0,010C08-07 12383 114,00 114,89 0,89 0,020 0,020C08-07 12384 114,89 116,00 1,11 0,010 0,010C08-07 12385 116,00 117,00 1,00 0,000 0,000C08-07 12386 OREAS 15Pa Batch 1 Can 0,990 0,990C08-07 12387 117,00 118,00 1,00 0,010 0,010C08-07 12388 118,00 119,00 1,00 0,010 0,010C08-07 12389 119,00 120,00 1,00 0,010 0,000 0,005C08-07 12390 120,00 121,00 1,00 0,010 0,010C08-07 12391 121,00 122,00 1,00 0,010 0,010C08-07 12392 122,00 122,80 0,80 0,010 0,010C08-07 12393 122,80 123,60 0,80 0,010 0,010C08-07 12394 123,60 124,40 0,80 0,010 0,010 0,010C08-07 12395 124,40 125,26 0,86 0,010 0,010C08-07 12396 125,26 126,10 0,84 0,010 0,010C08-07 12397 126,10 127,00 0,90 0,010 0,010C08-07 12398 127,00 128,00 1,00 0,000 0,000C08-07 12399 128,00 129,00 1,00 0,000 0,000C08-07 12400 129,00 130,00 1,00 0,010 0,010C08-07 12401 130,00 131,00 1,00 0,000 0,000C08-07 12402 131,00 132,00 1,00 0,010 0,010C08-07 12403 132,00 133,00 1,00 0,010 0,010C08-07 12404 133,00 134,00 1,00 0,010 0,010C08-07 12405 134,00 135,00 1,00 0,000 0,000C08-07 12406 135,00 135,85 0,85 0,010 0,010

C08-07 12407 DIABASE 102.5-103.0 0,010 0,000 0,005C08-07 12408 135,85 136,90 1,05 0,000 0,000C08-07 12409 136,90 138,00 1,10 0,000 0,000C08-07 12410 138,00 139,00 1,00 0,000 0,000C08-07 12411 139,00 140,00 1,00 0,010 0,010C08-07 12412 140,00 141,00 1,00 0,010 0,010C08-07 12413 141,00 142,00 1,00 0,000 0,000C08-07 12414 142,00 143,00 1,00 0,000 0,000C08-07 12415 143,00 144,00 1,00 0,000 0,000C08-07 12416 144,00 145,00 1,00 0,010 0,010C08-07 12417 145,00 146,00 1,00 0,000 0,000C08-07 12418 146,00 147,00 1,00 0,010 0,000 0,005C08-07 12419 147,00 148,00 1,00 0,010 0,010C08-07 12420 148,00 149,00 1,00 0,000 0,000C08-07 12421 149,00 150,04 1,04 0,010 0,010C08-07 12422 150,04 150,80 0,76 0,010 0,000 0,005C08-07 12423 150,80 151,52 0,72 0,010 0,010C08-07 12424 151,52 152,50 0,98 0,010 0,010C08-07 12425 OREAS 15Pa Batch 1 Can 1,030 1,030C08-07 12426 152,50 153,50 1,00 0,010 0,010C08-07 12427 153,50 154,56 1,06 0,000 0,000C08-07 12428 154,56 155,10 0,54 0,010 0,010C08-07 12429 155,10 155,70 0,60 0,010 0,010C08-07 12430 155,70 156,59 0,89 0,000 0,000C08-07 12431 156,59 157,30 0,71 0,010 0,000 0,005C08-07 12432 157,30 158,07 0,77 0,010 0,010C08-07 12433 158,07 159,00 0,93 0,010 0,010C08-07 12434 159,00 160,00 1,00 0,010 0,010C08-07 12435 160,00 160,90 0,90 0,010 0,010C08-07 12436 160,90 161,74 0,84 0,010 0,010C08-07 12437 161,74 162,23 0,49 0,010 0,000 0,005C08-07 12438 162,23 163,10 0,87 0,010 0,010C08-07 12439 163,10 164,00 0,90 0,010 0,010C08-07 12440 164,00 165,00 1,00 0,000 0,000C08-07 12441 165,00 166,00 1,00 0,010 0,010C08-07 12442 OREAS 15Pa Batch 1 Can 0,990 0,990C08-07 12443 166,00 167,00 1,00 0,010 0,010C08-07 12444 167,00 168,00 1,00 0,010 0,010C08-07 12445 168,00 169,00 1,00 0,000 0,000C08-07 12446 169,00 170,00 1,00 0,020 0,000 0,010C08-07 12447 170,00 171,00 1,00 0,010 0,010C08-07 12448 171,00 172,00 1,00 0,010 0,010

C08-07 12449 172,00 173,00 1,00 0,010 0,010C08-07 12450 173,00 174,00 1,00 0,010 0,010C08-07 12451 174,00 175,00 1,00 0,010 0,010C08-07 12452 175,00 176,00 1,00 0,010 0,010C08-07 12453 176,00 177,00 1,00 0,010 0,010C08-07 12454 177,00 178,00 1,00 0,000 0,000C08-07 12455 178,00 179,00 1,00 0,010 0,010C08-07 12456 179,00 180,00 1,00 0,000 0,000C08-07 12457 180,00 181,00 1,00 0,010 0,000 0,005C08-07 12458 181,00 182,00 1,00 0,000 0,000C08-07 12459 182,00 183,00 1,00 0,000 0,000C08-07 12460 183,00 184,00 1,00 0,010 0,010C08-07 12461 184,00 185,00 1,00 0,010 0,010C08-07 12462 185,00 186,00 1,00 0,000 0,000C08-07 12463 186,00 187,00 1,00 0,010 0,010C08-07 12464 187,00 188,00 1,00 0,010 0,010C08-07 12465 188,00 189,00 1,00 0,000 0,000C08-07 12466 QUARTZ Purchased 0,010 0,010C08-07 12467 189,00 190,00 1,00 0,010 0,010C08-07 12468 190,00 191,00 1,00 0,010 0,010 0,010C08-07 12469 191,00 192,00 1,00 0,010 0,010C08-07 12470 192,00 193,00 1,00 0,010 0,010C08-07 12471 193,00 194,00 1,00 0,010 0,010C08-07 12472 194,00 195,00 1,00 0,010 0,010C08-07 12473 195,00 196,00 1,00 0,010 0,010C08-07 12474 196,00 197,00 1,00 0,010 0,010C08-07 12475 197,00 198,00 1,00 0,000 0,000C08-07 12476 198,00 199,03 1,03 0,010 0,010 0,010C08-07 12477 199,03 199,90 0,87 0,010 0,010C08-07 12478 199,90 200,80 0,90 0,010 0,010C08-07 12479 200,80 201,70 0,90 0,010 0,010C08-07 12480 201,70 202,56 0,86 0,010 0,010C08-07 12481 202,56 203,40 0,84 0,010 0,010C08-07 12482 203,40 204,20 0,80 0,010 0,010C08-07 12483 204,20 205,00 0,80 0,000 0,000C08-07 12484 205,00 206,00 1,00 0,010 0,010C08-07 12485 206,00 207,00 1,00 0,000 0,000C08-07 12486 207,00 208,00 1,00 0,010 0,010C08-07 12487 208,00 209,00 1,00 0,010 0,010C08-07 12488 209,00 210,00 1,00 0,010 0,000 0,005C08-07 12489 210,00 211,00 1,00 0,010 0,010C08-07 12490 211,00 212,00 1,00 0,010 0,010

C08-07 12491 212,00 213,00 1,00 0,010 0,010C08-07 12492 213,00 214,08 1,08 0,010 0,010C08-07 12493 214,08 215,00 0,92 0,010 0,020 0,015C08-07 12494 215,00 216,00 1,00 0,000 0,000C08-07 12495 216,00 217,00 1,00 0,000 0,000C08-07 12496 217,00 218,00 1,00 0,000 0,000C08-07 12497 OREAS 15Pa Batch 1 Can 0,980 0,980C08-07 12498 218,00 219,00 1,00 0,010 0,010C08-07 12499 219,00 220,00 1,00 0,000 0,000C08-07 12500 220,00 220,80 0,80 0,010 0,010C08-07 12501 220,80 221,60 0,80 0,010 0,010 0,200 0,003 0,004 0,017 0,001 0,009C08-07 12502 221,60 222,28 0,68 0,000 0,000 0,200 0,003 0,007 0,016 0,001 0,007C08-07 12503 222,28 223,06 0,78 0,010 0,000 0,005 0,200 0,003 0,004 0,019 0,001 0,007C08-07 12504 223,06 223,38 0,32 0,000 0,000 0,200 0,003 0,003 0,017 0,001 0,009C08-07 12505 223,38 224,10 0,72 0,000 0,000 0,200 0,002 0,005 0,007 0,001 0,007C08-07 12506 224,10 224,87 0,77 0,000 0,000 0,200 0,002 0,006 0,006 0,001 0,007C08-07 12507 224,87 225,80 0,93 0,000 0,000 0,200 0,003 0,004 0,017 0,001 0,009C08-07 12508 OREAS 15Pa Batch 1 Can 0,990 0,990 0,200 0,003 0,005 0,011 0,001 0,007C08-07 12509 225,80 226,80 1,00 0,000 0,000 0,200 0,003 0,004 0,016 0,001 0,009C08-07 12510 226,80 227,80 1,00 0,000 0,000 0,200 0,002 0,004 0,014 0,001 0,007C08-07 12511 227,80 228,80 1,00 0,000 0,000 0,200 0,003 0,002 0,018 0,001 0,009C08-07 12512 228,80 229,80 1,00 0,000 0,000 0,200 0,003 0,002 0,019 0,001 0,011C08-07 12513 229,80 230,80 1,00 0,010 0,010 0,200 0,003 0,007 0,020 0,001 0,017C08-07 12514 230,80 231,80 1,00 0,000 0,000 0,200 0,003 0,003 0,019 0,001 0,010C08-07 12515 231,80 232,80 1,00 0,010 0,010 0,200 0,003 0,005 0,020 0,001 0,013C08-07 12516 232,80 233,81 1,01 0,010 0,010 0,010 0,200 0,003 0,008 0,017 0,001 0,016C08-07 12517 233,81 234,60 0,79 0,000 0,000 0,200 0,004 0,007 0,018 0,001 0,010C08-07 12518 234,60 235,36 0,76 0,000 0,000 0,200 0,003 0,008 0,012 0,002 0,007C08-07 12519 235,36 236,10 0,74 0,010 0,010 0,200 0,003 0,006 0,009 0,001 0,008C08-07 12520 236,10 236,80 0,70 0,010 0,010 0,200 0,003 0,004 0,015 0,001 0,007C08-07 12521 236,80 237,46 0,66 0,000 0,000 0,200 0,004 0,004 0,017 0,001 0,010C08-07 12522 237,46 238,40 0,94 0,000 0,000 0,200 0,002 0,006 0,007 0,001 0,007C08-07 12523 238,40 239,30 0,90 0,000 0,000 0,200 0,002 0,005 0,006 0,001 0,007C08-07 12524 239,30 240,30 1,00 0,000 0,000 0,200 0,002 0,005 0,007 0,001 0,008C08-07 12525 240,30 241,29 0,99 0,000 0,000 0,200 0,002 0,004 0,007 0,001 0,007C08-07 12526 241,29 242,10 0,81 0,000 0,000 0,200 0,004 0,005 0,016 0,001 0,007C08-07 12527 242,10 243,00 0,90 0,000 0,000 0,200 0,004 0,004 0,017 0,001 0,012C08-07 12528 243,00 244,00 1,00 0,000 0,010 0,005 0,200 0,003 0,002 0,015 0,001 0,010C08-07 12529 244,00 245,00 1,00 0,000 0,000 0,200 0,003 0,002 0,015 0,001 0,012C08-07 12530 245,00 246,00 1,00 0,000 0,000 0,200 0,002 0,002 0,013 0,001 0,008C08-07 12531 246,00 247,00 1,00 0,000 0,000 0,200 0,003 0,005 0,009 0,001 0,007C08-07 12532 247,00 248,00 1,00 0,000 0,000 0,200 0,002 0,001 0,011 0,001 0,006

C08-07 12533 248,00 248,80 0,80 0,010 0,010 0,010 0,200 0,003 0,001 0,015 0,001 0,008C08-07 12534 248,80 249,58 0,78 0,010 0,010 0,200 0,002 0,001 0,010 0,001 0,006C08-07 12535 DIABASE 102.5-103.0 0,000 0,000 0,200 0,002 0,013 0,002 0,001 0,007C08-07 12536 249,58 250,60 1,02 0,000 0,000 0,200 0,002 0,004 0,004 0,001 0,005C08-07 12537 250,60 251,68 1,08 0,000 0,000 0,200 0,003 0,006 0,006 0,001 0,008C08-07 12538 251,68 252,70 1,02 0,000 0,000 0,200 0,002 0,002 0,012 0,001 0,006C08-07 12539 252,70 253,75 1,05 0,010 0,010 0,200 0,003 0,008 0,015 0,001 0,008C08-07 12540 253,75 254,49 0,74 0,010 0,010 0,200 0,002 0,004 0,005 0,001 0,005C08-07 12541 254,49 255,60 1,11 0,000 0,000 0,200 0,003 0,004 0,013 0,001 0,007C08-07 12542 255,60 256,60 1,00 0,010 0,010 0,200 0,004 0,004 0,028 0,001 0,012C08-07 12543 296,90 297,82 0,92 0,010 0,000 0,005 0,200 0,004 0,003 0,027 0,001 0,005C08-07 12544 297,82 298,45 0,63 0,010 0,010 0,200 0,003 0,012 0,015 0,001 0,004C08-07 12545 298,45 299,10 0,65 0,000 0,000 0,200 0,001 0,003 0,010 0,001 0,005C08-07 12546 299,10 299,70 0,60 0,000 0,000 0,200 0,002 0,009 0,014 0,001 0,006C08-07 12547 299,70 300,60 0,90 0,000 0,000 0,200 0,003 0,001 0,016 0,001 0,012C08-07 12548 300,60 301,30 0,70 0,010 0,010 0,200 0,004 0,004 0,008 0,006 0,010C08-07 12549 OREAS 15Pa Batch 1 Can 0,990 0,990 0,200 0,003 0,006 0,011 0,001 0,007C08-07 12550 301,30 301,94 0,64 0,010 0,010 0,200 0,002 0,005 0,002 0,001 0,003


20,05 23 2,95 2,95 100% 0,14 2,81 95%23 26 3 2,77 92% 1,12 1,88 63%26 29 3 2,96 99% 0,21 2,79 93%29 32 3 2,98 99% 0,05 2,95 98%32 35 3 3,02 101% 0,03 2,97 99%35 38 3 3,04 101% 0,56 2,44 81%38 41 3 3 100% 1,00 2,00 67%41 44 3 3 100% 2,00 1,00 33%44 47 3 3 100% 0,90 2,10 70%47 50 3 2,99 100% 0,00 3,00 100%50 53 3 3 100% 0,00 3,00 100%53 56 3 2,94 98% 0,00 3,00 100%56 59 3 3,07 102% 0,04 2,96 99%59 62 3 2,87 96% 0,00 3,00 100%62 65 3 3,08 103% 0,09 2,91 97%65 68 3 3,02 101% 0,06 2,94 98%68 71 3 2,96 99% 0,00 3,00 100%71 74 3 3,02 101% 0,00 3,00 100%74 77 3 3,02 101% 0,00 3,00 100%77 80 3 3,00 100% 0,00 3,00 100%80 83 3 2,99 100% 0,00 3,00 100%83 86 3 3,01 100% 0,00 3,00 100%86 89 3 3,03 101% 0,00 3,00 100%89 92 3 2,94 98% 0,00 3,00 100%92 95 3 3,01 100% 0,10 2,90 97%95 98 3 3,04 101% 0,35 2,65 88%98 101 3 3,00 100% 0,12 2,88 96%101 104 3 2,9 97% 0,07 2,93 98%104 107 3 3,09 103% 0,00 3,00 100%107 110 3 2,98 99% 0,00 3,00 100%110 113 3 3,02 101% 0,00 3,00 100%113 116 3 2,98 99% 0,00 3,00 100%116 119 3 3,02 101% 0,04 2,96 99%119 122 3 2,97 99% 0,00 3,00 100%122 125 3 3,07 102% 0,08 2,92 97%125 128 3 2,96 99% 0,00 3,00 100%128 131 3 2,97 99% 0,05 2,95 98%131 134 3 3,05 102% 0,00 3,00 100%134 137 3 2,95 98% 0,02 2,98 99%137 140 3 3,07 102% 0,00 3,00 100%140 143 3 2,94 98% 0,00 3,00 100%143 146 3 3,04 101% 0,00 3,00 100%146 149 3 3,03 101% 0,00 3,00 100%149 152 3 2,89 96% 0,00 3,00 100%152 155 3 3,03 101% 0,00 3,00 100%155 158 3 2,94 98% 0,20 2,80 93%

158 161 3 3,11 104% 0,47 2,53 84%161 164 3 3,05 102% 0,00 3,00 100%164 167 3 3,01 100% 0,00 3,00 100%167 170 3 3,01 100% 0,00 3,00 100%170 173 3 2,98 99% 0,00 3,00 100%173 176 3 3,05 102% 0,05 2,95 98%176 179 3 3,00 100% 0,00 3,00 100%179 182 3 3,04 101% 0,14 2,86 95%182 185 3 2,97 99% 0,09 2,91 97%185 188 3 3,02 101% 0,06 2,94 98%188 191 3 3,03 101% 0,00 3,00 100%191 194 3 3,03 101% 0,00 3,00 100%194 197 3 2,96 99% 0,00 3,00 100%197 200 3 2,98 99% 0,07 2,93 98%200 203 3 3,02 101% 0,11 2,89 96%203 206 3 3,01 100% 0,09 2,91 97%206 209 3 3,00 100% 0,00 3,00 100%209 212 3 2,96 99% 0,00 3,00 100%212 215 3 3,02 101% 0,00 3,00 100%215 218 3 3,05 102% 0,00 3,00 100%218 221 3 2,99 100% 0,09 2,91 97%221 224 3 2,99 100% 0,00 3,00 100%224 227 3 3,00 100% 0,02 2,98 99%227 230 3 2,99 100% 0,00 3,00 100%230 233 3 3,00 100% 0,00 3,00 100%233 236 3 3,01 100% 0,09 2,91 97%236 239 3 2,97 99% 0,10 2,90 97%239 242 3 2,99 100% 0,09 2,91 97%242 245 3 3,02 101% 0,00 3,00 100%245 248 3 3,02 101% 0,21 2,79 93%248 251 3 3,03 101% 0,40 2,60 87%251 254 3 3,07 102% 0,75 2,25 75%254 257 3 3,00 100% 1,10 1,90 63%257 260 3 2,99 100% 0,64 2,36 79%260 263 3 2,94 98% 0,48 2,52 84%263 266 3 3,04 101% 0,22 2,78 93%266 269 3 3,04 101% 0,41 2,59 86%269 272 3 3,03 101% 0,25 2,75 92%272 275 3 2,99 100% 0,59 2,41 80%275 278 3 3,02 101% 0,03 2,97 99%278 281 3 2,96 99% 0,60 2,40 80%281 284 3 3,04 101% 0,15 2,85 95%284 287 3 3,00 100% 0,01 2,99 100%287 290 3 2,97 99% 0,00 3,00 100%290 293 3 3,03 101% 0,13 2,87 96%293 296 3 2,99 100% 0,06 2,94 98%296 299 3 3,00 100% 0,30 2,70 90%299 302 3 2,63 88% 0,14 2,86 95%


C08-08 L-100E 1550N 300 0 -60 375m 15-août-08 10-août-08


18,34 103,90 85,56

Mafic calc-alkalic volcanics, pale greenish-grey, aphanitic to fg, bedding, spherules, brecciated, calcite alteration, silicification, hard, 1-2% py

103,90 164,17 60,27

Mafic calc-alkalic volcanics, variolitic, pillowed, pale greenish-grey, aphanitic to fg, bedding, spherules, brecciated, calcite alteration, silicification, hard, 1-2% py

164,17 190,51 26,34Mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, brecciated, calcite alteration, silicification, hard, tr py

190,51 234,21 43,70

Mafic calc-alkalic volcanics, variolitic, pillowed, pale greenish-grey, aphanitic to fg, bedding, spherules, brecciated, calcite alteration, silicification, hard, 2-3% py

234,21 249,93 15,72Lamprophyre dyke, pale green-grey, fg matrix with mafic phenocryst, calcite alteration, 5-8% py

249,93 269,55 19,62Mafic calc-alkali volcanics, pale grey-green, pillowed, aphanitic to fg, brecciated, calcite alteration, hard

269,55 283,21 13,66Lamprophyre dyke, pale green-grey, fg matrix with mafic phenocryst, calcite alteration, 3-5% py

283,21 287,17 3,96Mafic calc-alkali volcanics, pale grey-green, aphanitic to fg, brecciated, calcite alteration, hard

287,17 314,3 27,13Mafic intrusive, grey-green, mg to cg, massive, hard, magnetic, 1-2% py

314,30 326,47 12,17Silicified conglomerate, grey-green, (feldspar porphyry), very hard, 2-3% py

326,47 347,4 20,93Greywacke/graphitic argillites, grey-brown, aphanitic to fg, bedding 5-50 to CA, calcite alteration, silicification, hard

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments

42,40 43,31 0,91Mafic dyke, purplish-grey, fg matrix with mafic and fds phenocryst, calcite alteration, hard, 2% py

44,75 45,1 0,35 lost core47,27 47,44 0,17 mafic dyke, medium green, fg, massive, 5% py

96,14 98,57 2,43Mafic dyke, purplish-grey, fg matrix with mafic and fds phenocryst, calcite alteration, hard, 8% py

123,54 124,09 0,55 dark-grey, mafic dyke

147,85 148,32 0,47mafic dyke, grey, fg matrix with mafic phenocryst, calcite alteration

161,87 163,42 1,55Lamprophyre dyke, dark-brown,fg matrix with mafic phenocryst, lineation 35-50 to CA, calcite alteration, 5-8% py

163,82 164,17 0,35mafic dyke, grey-brown, fg matrix with mafic phenocryst, 3% py

170,79 171,03 0,24intermediate dyke, pale pinkish-brown, fg matrix with mafic phenocryst, calcite alteration, minor py

176,15 176,31 0,16Lamprophyre dyke, purplish-brown, fg matrix with mafic phenocryst, calcite alteration, minor py

182,07 182,52 0,45 mafic dyke, dark-green, fg, massive, tr py203,90 205,76 1,86 mafic dyke, greenish-brown, fg, massive, calcite alteration, hard

207,07 207,76 0,69mafic dyke, grey-green, fg, massive, calcite alteration, hard, 2% py

208,55 211,81 3,26Intermediate dyke, purplish-grey, fg matrix with mafic phenocryst, calcite alteration, hard, 1% py

213,72 213,98 0,26 pale green, felsic dyke215,33 215,72 0,39 mafic dyke, grey-brown, fg, massive, minor py232,66 232,89 0,23 purplish-brown dyke

245,46 246,28 0,82mafic volcanics inclusion, bedding 20-60 to CA, calcite alteration, 3% py

249,93 257,1 7,17 3-5% py253,30 257,1 3,80 35% chert fragments, bedding 20-40 to CA

257,10 258,59 1,49mafic dyke, dark-grey, fg matrix with mafic phenocryst, calcite alteration, 5% py

258,59 258,84 0,25 8% scattered py258,84 259,53 0,69 mafic dyke, grey-green, fg, calcite alteration, 8% py259,53 263,5 3,97 3-5% py263,50 269,55 6,05 2-3% py283,21 285,27 2,06 2-3% py

285,27 286,17 0,90 graphitic argillite, dark grey, aphanitic, bedding 10-30 to CA, hard, 8% py286,17 287,17 1,00 tuffaceous mafic volcanics, breccia, 2% py

DDH Depth

317,47 317,66 0,19 mafic dyke326,47 332 5,53 50% argillites, 3-5% py332,00 334,93 2,93 mixed zone, mafic volcanics above chert, 3-5% py334,93 341,49 6,56 20-30% argillites, 2-3% py341,49 342,42 0,93 conglomerate, 1% py342,42 347,4 4,98 brownish-grey, greywacke, 10% argillite beds, 1-2% pyEOH

From To Length Id Description CA Py Po Cpy Sph Gal Mag

42,40 43,31 0,91Mafic dyke, purplish-grey, fg matrix with mafic and fds phenocryst, calcite alteration, hard, 2% py 2

47,27 47,44 0,17 mafic dyke, medium green, fg, massive, 5% py 5

96,14 98,57 2,43Mafic dyke, purplish-grey, fg matrix with mafic and fds phenocryst, calcite alteration, hard, 8% py 8

161,87 163,42 1,55

Lamprophyre dyke, dark-brown,fg matrix with mafic phenocryst, lineation 35-50 to CA, calcite alteration, 5-8% py 35 5

163,82 164,17 0,35mafic dyke, grey-brown, fg matrix with mafic phenocryst, 3% py 3

207,07 207,76 0,69mafic dyke, grey-green, fg, massive, calcite alteration, hard, 2% py 2

208,55 211,81 3,26Intermediate dyke, purplish-grey, fg matrix with mafic phenocryst, calcite alteration, hard, 1% py 1

245,46 246,28 0,82mafic volcanics inclusion, bedding 20-60 to CA, calcite alteration, 3% py 20 3

249,93 257,1 7,17 3-5% py 3

257,10 258,59 1,49mafic dyke, dark-grey, fg matrix with mafic phenocryst, calcite alteration, 5% py 5

258,59 258,84 0,25 8% scattered py 8258,84 259,53 0,69 mafic dyke, grey-green, fg, calcite alteration, 8% py 8259,53 263,5 3,97 3-5% py 3263,50 269,55 6,05 2-3% py 2283,21 285,27 2,06 2-3% py 2

285,27 286,17 0,90graphitic argillite, dark grey, aphanitic, bedding 10-30 to CA, hard, 8% py 10 8

286,17 287,17 1,00 tuffaceous mafic volcanics, breccia, 2% py 2326,47 332 5,53 50% argillites, 3-5% py 3332,00 334,93 2,93 mixed zone, mafic volcanics above chert, 3-5% py 3334,93 341,49 6,56 20-30% argillites, 2-3% py 2341,49 342,42 0,93 conglomerate, 1% py 1342,42 347,4 4,98 brownish-grey, greywacke, 10% argillite beds, 1-2% py 1


HoleIDSample Number


Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-08 12551 18,34 19,20 0,86 0,000 0,000 0,200 0,002 0,003 0,008 0,001 0,005C08-08 12552 19,20 20,00 0,80 0,010 0,010 0,200 0,002 0,003 0,011 0,001 0,006C08-08 12553 20,00 21,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,008C08-08 12554 21,00 22,00 1,00 0,010 0,000 0,005 0,200 0,002 0,003 0,013 0,001 0,009C08-08 12555 22,00 23,00 1,00 0,000 0,000 0,200 0,003 0,004 0,017 0,001 0,014C08-08 12556 23,00 24,00 1,00 0,010 0,010 0,200 0,003 0,003 0,014 0,001 0,009C08-08 12557 24,00 25,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,002 0,007C08-08 12558 25,00 26,00 1,00 0,010 0,010 0,200 0,002 0,003 0,012 0,001 0,006C08-08 12559 26,00 27,00 1,00 0,000 0,000 0,000 0,200 0,002 0,004 0,009 0,001 0,004C08-08 12560 27,00 28,00 1,00 0,000 0,000 0,200 0,002 0,005 0,010 0,001 0,004C08-08 12561 28,00 29,00 1,00 0,000 0,000 0,200 0,002 0,005 0,010 0,001 0,005C08-08 12562 29,00 30,00 1,00 0,000 0,000 0,200 0,002 0,003 0,008 0,001 0,004C08-08 12563OREAS 15Pa Batch 1 Can 0,990 0,990 0,200 0,003 0,006 0,011 0,001 0,007C08-08 12564 30,00 31,00 1,00 0,000 0,000 0,200 0,002 0,004 0,009 0,001 0,005C08-08 12565 31,00 32,00 1,00 0,000 0,000 0,200 0,002 0,004 0,010 0,001 0,005C08-08 12566 32,00 33,00 1,00 0,000 0,000 0,200 0,002 0,003 0,008 0,001 0,005C08-08 12567 33,00 34,00 1,00 0,000 0,000 0,200 0,002 0,002 0,008 0,001 0,006C08-08 12568 34,00 35,00 1,00 0,000 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,006C08-08 12569 35,00 36,00 1,00 0,000 0,000 0,200 0,002 0,004 0,009 0,001 0,006C08-08 12570 36,00 37,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,005C08-08 12571 37,00 38,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12572 38,00 39,00 1,00 0,000 0,000 0,200 0,002 0,004 0,009 0,001 0,004C08-08 12573 39,00 40,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,004C08-08 12574 40,00 40,80 0,80 0,000 0,000 0,200 0,002 0,004 0,010 0,001 0,006C08-08 12575 40,80 41,60 0,80 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,008C08-08 12576 41,60 42,40 0,80 0,010 0,010 0,200 0,002 0,004 0,010 0,001 0,006C08-08 12577 42,40 43,31 0,91 0,000 0,000 0,200 0,003 0,009 0,005 0,001 0,011C08-08 12578 43,31 44,00 0,69 0,000 0,000 0,200 0,002 0,004 0,010 0,001 0,007C08-08 12579 44,00 44,75 0,75 0,000 0,000 0,200 0,003 0,003 0,014 0,001 0,012C08-08 12580 45,10 46,00 0,90 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,009C08-08 12581 46,00 47,00 1,00 0,010 0,000 0,005 0,200 0,002 0,004 0,012 0,001 0,009C08-08 12582 47,00 48,00 1,00 0,000 0,000 0,200 0,002 0,007 0,007 0,001 0,008C08-08 12583 48,00 49,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12584 49,00 50,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,007C08-08 12585 50,00 51,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,007C08-08 12586 51,00 52,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,006C08-08 12587 52,00 53,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,006C08-08 12588 53,00 54,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,006C08-08 12589 54,00 55,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,006

C08-08 12590 QUARTZ Purchased 0,000 0,000 0,200 0,001 0,001 0,001 0,001 0,001C08-08 12591 55,00 56,00 1,00 0,020 0,000 0,010 0,200 0,002 0,003 0,012 0,001 0,011C08-08 12592 56,00 57,00 1,00 0,010 0,010 0,200 0,002 0,004 0,011 0,001 0,008C08-08 12593 57,00 58,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,007C08-08 12594 58,00 59,00 1,00 0,000 0,000 0,200 0,002 0,004 0,010 0,001 0,007C08-08 12595 59,00 60,00 1,00 0,000 0,000 0,200 0,003 0,006 0,014 0,001 0,008C08-08 12596 60,00 61,00 1,00 0,010 0,010 0,200 0,002 0,003 0,009 0,001 0,006C08-08 12597 61,00 62,00 1,00 0,030 0,030 0,200 0,002 0,003 0,009 0,001 0,007C08-08 12598 62,00 63,00 1,00 0,020 0,020 0,200 0,001 0,004 0,008 0,001 0,006C08-08 12599 63,00 64,00 1,00 0,000 0,000 0,000 0,200 0,001 0,003 0,007 0,001 0,004C08-08 12600 64,00 65,00 1,00 0,020 0,020 0,200 0,002 0,004 0,008 0,001 0,005C08-08 12601 65,00 66,00 1,00 0,070 0,070 0,200 0,001 0,003 0,009 0,001 0,004C08-08 12602 66,00 67,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,004C08-08 12603 67,00 68,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12604 68,00 69,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,004C08-08 12605 69,00 70,00 1,00 0,010 0,010 0,200 0,002 0,003 0,009 0,001 0,004C08-08 12606OREAS 15Pa Batch 1 Can 0,990 0,990 0,200 0,003 0,005 0,011 0,001 0,007C08-08 12607 70,00 71,00 1,00 0,010 0,010 0,200 0,003 0,003 0,013 0,001 0,006C08-08 12608 71,00 72,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12609 72,00 73,00 1,00 0,010 0,010 0,200 0,001 0,002 0,008 0,001 0,005C08-08 12610 73,00 74,00 1,00 0,000 0,000 0,200 0,002 0,003 0,009 0,001 0,005C08-08 12611 74,00 75,00 1,00 0,010 0,010 0,010 0,200 0,001 0,003 0,008 0,001 0,004C08-08 12612 75,00 76,00 1,00 0,000 0,000 0,200 0,001 0,003 0,008 0,001 0,005C08-08 12613 76,00 77,00 1,00 0,010 0,010 0,200 0,001 0,003 0,008 0,001 0,005C08-08 12614 77,00 78,00 1,00 0,010 0,010 0,200 0,001 0,003 0,007 0,001 0,004C08-08 12615 78,00 79,00 1,00 0,040 0,040 0,200 0,001 0,003 0,007 0,001 0,005C08-08 12616 79,00 80,00 1,00 0,000 0,000 0,200 0,001 0,003 0,009 0,001 0,005C08-08 12617 80,00 81,00 1,00 0,010 0,010 0,200 0,003 0,004 0,013 0,001 0,006C08-08 12618 81,00 82,00 1,00 0,000 0,000 0,200 0,002 0,004 0,011 0,001 0,006C08-08 12619 82,00 83,00 1,00 0,000 0,020 0,010 0,200 0,002 0,003 0,009 0,001 0,005C08-08 12620 83,00 84,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,006C08-08 12621 84,00 85,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12622 85,00 86,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,006C08-08 12623 86,00 87,00 1,00 0,000 0,000 0,200 0,002 0,003 0,013 0,001 0,007C08-08 12624OREAS 15Pa Batch 1 Can 1,030 1,030 0,200 0,003 0,006 0,012 0,001 0,007C08-08 12625 87,00 88,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,006C08-08 12626 88,00 89,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12627 89,00 90,00 1,00 0,010 0,010 0,200 0,002 0,003 0,012 0,001 0,006C08-08 12628 90,00 91,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12629 91,00 92,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,006C08-08 12630 92,00 93,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005

C08-08 12631 93,00 94,00 1,00 0,000 0,020 0,010 0,200 0,002 0,004 0,012 0,001 0,006C08-08 12632 94,00 95,10 1,10 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,006C08-08 12633 95,10 96,14 1,04 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005C08-08 12634 96,14 97,00 0,86 0,000 0,000 0,200 0,003 0,005 0,010 0,001 0,004C08-08 12635 97,00 97,80 0,80 0,000 0,000 0,200 0,003 0,005 0,012 0,001 0,005C08-08 12636 97,80 98,57 0,77 0,000 0,000 0,200 0,003 0,005 0,010 0,001 0,004C08-08 12637 98,57 99,40 0,83 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,006C08-08 12638 99,40 100,30 0,90 0,000 0,000 0,200 0,002 0,004 0,012 0,002 0,006C08-08 12639 100,30 101,20 0,90 0,000 0,000 0,200 0,002 0,004 0,013 0,001 0,007C08-08 12640 101,20 102,10 0,90 0,010 0,010 0,200 0,002 0,004 0,012 0,001 0,006C08-08 12641 102,10 103,00 0,90 0,000 0,000 0,200 0,002 0,003 0,013 0,001 0,005C08-08 12642 103,00 103,90 0,90 0,000 0,000 0,200 0,003 0,004 0,017 0,001 0,006C08-08 12643 103,90 105,00 1,10 0,020 0,000 0,010 0,200 0,003 0,005 0,016 0,001 0,010C08-08 12644 105,00 106,00 1,00 0,000 0,000 0,200 0,003 0,005 0,016 0,003 0,008C08-08 12645DIABASE 103.0-103.5 0,000 0,000 0,200 0,003 0,014 0,003 0,001 0,009C08-08 12646 106,00 107,00 1,00 0,000 0,000 0,200 0,003 0,004 0,016 0,001 0,006C08-08 12647 107,00 108,00 1,00 0,000 0,000 0,200 0,003 0,003 0,015 0,001 0,006C08-08 12648 108,00 109,00 1,00 0,000 0,000 0,200 0,004 0,009 0,019 0,001 0,010C08-08 12649 109,00 110,00 1,00 0,000 0,000 0,200 0,004 0,004 0,017 0,001 0,007C08-08 12650 110,00 111,00 1,00 0,010 0,010 0,200 0,003 0,003 0,016 0,001 0,007C08-08 12651 111,00 112,00 1,00 0,000 0,000 0,200 0,003 0,005 0,015 0,001 0,009C08-08 12652 112,00 113,00 1,00 0,000 0,000 0,200 0,002 0,004 0,012 0,001 0,008C08-08 12653 113,00 114,00 1,00 0,010 0,000 0,005 0,200 0,002 0,004 0,014 0,001 0,008C08-08 12654 114,00 115,00 1,00 0,000 0,000 0,200 0,003 0,004 0,016 0,001 0,007C08-08 12655 115,00 116,00 1,00 0,010 0,010 0,200 0,003 0,004 0,017 0,001 0,008C08-08 12656 116,00 117,00 1,00 0,000 0,000 0,200 0,002 0,007 0,014 0,001 0,007C08-08 12657 117,00 118,00 1,00 0,010 0,010 0,200 0,002 0,007 0,013 0,001 0,006C08-08 12658 118,00 119,00 1,00 0,000 0,000 0,200 0,002 0,005 0,015 0,001 0,008C08-08 12659 119,00 120,00 1,00 0,000 0,000 0,200 0,003 0,005 0,016 0,001 0,010C08-08 12660 120,00 121,00 1,00 0,000 0,000 0,200 0,003 0,004 0,016 0,001 0,008C08-08 12661 121,00 122,00 1,00 0,020 0,000 0,010 0,200 0,002 0,005 0,013 0,001 0,008C08-08 12662 122,00 123,00 1,00 0,000 0,000 0,200 0,003 0,006 0,016 0,001 0,007C08-08 12663 123,00 124,09 1,09 0,000 0,000 0,200 0,002 0,005 0,012 0,001 0,006C08-08 12664 124,09 125,00 0,91 0,000 0,000 0,200 0,003 0,005 0,018 0,001 0,008C08-08 12665 125,00 126,00 1,00 0,000 0,000 0,200 0,003 0,009 0,014 0,001 0,009C08-08 12666 126,00 127,00 1,00 0,000 0,000 0,200 0,002 0,007 0,014 0,001 0,009C08-08 12667OREAS 15Pa Batch 1 Can 1,020 1,020 0,200 0,003 0,006 0,012 0,001 0,007C08-08 12668 127,00 128,00 1,00 0,000 0,000 0,200 0,003 0,004 0,016 0,001 0,006C08-08 12669 128,00 129,00 1,00 0,000 0,000 0,200 0,002 0,004 0,014 0,001 0,006C08-08 12670 129,00 130,00 1,00 0,000 0,000 0,200 0,002 0,004 0,015 0,001 0,006C08-08 12671 130,00 131,00 1,00 0,000 0,020 0,010 0,200 0,002 0,004 0,014 0,001 0,004

C08-08 12672 131,00 132,00 1,00 0,000 0,000 0,200 0,002 0,005 0,014 0,001 0,006C08-08 12673 132,00 133,00 1,00 0,000 0,000 0,200 0,002 0,005 0,013 0,001 0,005C08-08 12674 133,00 134,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,005C08-08 12675 134,00 135,00 1,00 0,040 0,020 0,030 0,200 0,002 0,004 0,012 0,001 0,007C08-08 12676 135,00 136,00 1,00 0,020 0,020 0,200 0,002 0,005 0,012 0,001 0,009C08-08 12677 136,00 137,00 1,00 0,010 0,010 0,200 0,002 0,005 0,014 0,001 0,011C08-08 12678 137,00 138,00 1,00 0,010 0,010 0,200 0,002 0,006 0,016 0,001 0,008C08-08 12679 138,00 139,00 1,00 0,020 0,020 0,200 0,002 0,006 0,014 0,001 0,008C08-08 12680 139,00 140,00 1,00 0,010 0,010 0,200 0,002 0,004 0,015 0,001 0,008C08-08 12681 140,00 141,00 1,00 0,010 0,010 0,200 0,002 0,004 0,012 0,001 0,006C08-08 12682 141,00 142,00 1,00 0,010 0,010 0,200 0,002 0,004 0,014 0,001 0,010C08-08 12683 142,00 143,00 1,00 0,010 0,010 0,200 0,002 0,006 0,014 0,001 0,013C08-08 12684 143,00 144,00 1,00 0,010 0,010 0,200 0,002 0,003 0,013 0,001 0,007C08-08 12685 144,00 145,00 1,00 0,010 0,020 0,015 0,200 0,002 0,005 0,013 0,001 0,006C08-08 12686 145,00 146,00 1,00 0,010 0,010 0,200 0,002 0,005 0,014 0,001 0,005C08-08 12687 146,00 147,00 1,00 0,010 0,010 0,200 0,002 0,004 0,013 0,001 0,007C08-08 12688OREAS 15Pa Batch 1 Can 0,960 0,960 0,200 0,002 0,005 0,010 0,001 0,006C08-08 12689 147,00 147,85 0,85 0,010 0,010 0,200 0,002 0,004 0,014 0,001 0,009C08-08 12690 147,85 148,90 1,05 0,010 0,010 0,200 0,002 0,004 0,013 0,001 0,007C08-08 12691 148,90 150,00 1,10 0,010 0,010 0,200 0,002 0,005 0,014 0,001 0,010C08-08 12692 150,00 151,00 1,00 0,010 0,010 0,200 0,002 0,005 0,012 0,001 0,007C08-08 12693 151,00 152,00 1,00 0,020 0,020 0,200 0,002 0,004 0,014 0,001 0,006C08-08 12694 152,00 153,00 1,00 0,010 0,010 0,200 0,002 0,006 0,013 0,001 0,005C08-08 12695 153,00 154,00 1,00 0,010 0,010 0,200 0,002 0,005 0,012 0,001 0,008C08-08 12696 154,00 155,00 1,00 0,010 0,010 0,200 0,002 0,005 0,013 0,001 0,011C08-08 12697 155,00 156,00 1,00 0,010 0,010 0,200 0,002 0,003 0,013 0,001 0,008C08-08 12698 156,00 157,00 1,00 0,010 0,010 0,200 0,003 0,005 0,016 0,001 0,010C08-08 12699 157,00 158,00 1,00 0,020 0,020 0,020 0,200 0,003 0,003 0,016 0,001 0,010C08-08 12700 158,00 159,00 1,00 0,010 0,010 0,200 0,003 0,004 0,015 0,001 0,011C08-08 12701 159,00 160,00 1,00 0,010 0,010 0,200 0,002 0,004 0,014 0,001 0,010C08-08 12702 160,00 161,00 1,00 0,010 0,010 0,200 0,003 0,003 0,016 0,001 0,010C08-08 12703 161,00 161,87 0,87 0,010 0,010 0,200 0,002 0,004 0,013 0,001 0,008C08-08 12704 161,87 162,65 0,78 0,010 0,010 0,200 0,003 0,002 0,015 0,001 0,012C08-08 12705 162,65 163,42 0,77 0,010 0,010 0,200 0,003 0,003 0,018 0,001 0,011C08-08 12706 QUARTZ Purchased 0,000 0,000 0,200 0,001 0,001 0,001 0,001 0,001C08-08 12707 163,42 164,17 0,75 0,010 0,010 0,200 0,003 0,001 0,011 0,001 0,008C08-08 12708 164,17 165,00 0,83 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,012C08-08 12709 165,00 166,00 1,00 0,000 0,000 0,200 0,003 0,002 0,013 0,001 0,009C08-08 12710 166,00 167,00 1,00 0,000 0,000 0,200 0,002 0,003 0,013 0,001 0,009C08-08 12711 167,00 168,00 1,00 0,000 0,000 0,000 0,200 0,002 0,004 0,010 0,001 0,005C08-08 12712 168,00 169,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,006

C08-08 12713 169,00 170,00 1,00 0,000 0,000 0,200 0,002 0,002 0,012 0,001 0,007C08-08 12714 170,00 171,03 1,03 0,000 0,000 0,200 0,003 0,008 0,013 0,001 0,008C08-08 12715 171,03 172,00 0,97 0,000 0,000 0,200 0,002 0,027 0,011 0,001 0,007C08-08 12716 172,00 173,00 1,00 0,000 0,000 0,200 0,001 0,003 0,009 0,001 0,005C08-08 12717 173,00 174,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005C08-08 12718 174,00 175,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005C08-08 12719 175,00 176,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005C08-08 12720 176,00 177,00 1,00 0,000 0,000 0,200 0,002 0,005 0,012 0,001 0,007C08-08 12721 177,00 178,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,005C08-08 12722 178,00 179,00 1,00 0,000 0,000 0,200 0,002 0,003 0,012 0,001 0,006C08-08 12723 179,00 180,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,005C08-08 12724 180,00 181,00 1,00 0,000 0,000 0,200 0,002 0,004 0,011 0,001 0,005C08-08 12725 181,00 182,00 1,00 0,000 0,020 0,010 0,200 0,002 0,002 0,010 0,001 0,004C08-08 12726 182,00 183,00 1,00 0,000 0,000 0,200 0,002 0,004 0,009 0,001 0,005C08-08 12727 183,00 184,00 1,00 0,000 0,000 0,200 0,002 0,003 0,010 0,001 0,005C08-08 12728 184,00 185,00 1,00 0,000 0,000 0,200 0,002 0,008 0,011 0,001 0,006C08-08 12729OREAS 15Pa Batch 1 Can 1,030 1,030 0,200 0,003 0,006 0,011 0,001 0,007C08-08 12730 185,00 186,00 1,00 0,000 0,000 0,200 0,002 0,002 0,011 0,001 0,006C08-08 12731 186,00 187,00 1,00 0,000 0,000 0,200 0,002 0,004 0,011 0,001 0,006C08-08 12732 187,00 188,00 1,00 0,000 0,000 0,200 0,002 0,003 0,011 0,001 0,007C08-08 12733 188,00 188,90 0,90C08-08 12734 188,90 189,70 0,80C08-08 12735 189,70 190,51 0,81C08-08 12736 190,51 191,41 0,90C08-08 12737 191,41 192,20 0,79C08-08 12738 192,20 193,00 0,80C08-08 12739 193,00 194,00 1,00C08-08 12740 194,00 195,00 1,00C08-08 12741 195,00 196,00 1,00C08-08 12742 196,00 197,00 1,00C08-08 12743 197,00 198,00 1,00C08-08 12744OREAS 15Pa Batch 1 CanC08-08 12745 198,00 199,00 1,00C08-08 12746 199,00 200,00 1,00C08-08 12747 200,00 201,00 1,00C08-08 12748 201,00 202,00 1,00C08-08 12749 202,00 203,00 1,00C08-08 12750 203,00 203,90 0,90C08-08 12751 203,90 204,80 0,90C08-08 12752 204,80 205,76 0,96C08-08 12753 205,76 206,76 1,00

C08-08 12754 206,76 207,76 1,00C08-08 12755 207,76 208,55 0,79C08-08 12756 208,55 209,60 1,05C08-08 12757 209,60 210,70 1,10C08-08 12758 210,70 211,81 1,11C08-08 12759 211,81 212,90 1,09C08-08 12760 212,90 214,00 1,10C08-08 12761 214,00 215,00 1,00C08-08 12762 215,00 216,00 1,00C08-08 12763 216,00 217,00 1,00C08-08 12764 217,00 218,00 1,00C08-08 12765 218,00 219,00 1,00C08-08 12766DIABASE 103.0-103.5C08-08 12767 219,00 220,00 1,00C08-08 12768 220,00 221,00 1,00C08-08 12769 221,00 222,00 1,00C08-08 12770 222,00 223,00 1,00C08-08 12771 223,00 224,00 1,00C08-08 12772 224,00 225,00 1,00C08-08 12773 225,00 226,00 1,00C08-08 12774 226,00 227,00 1,00C08-08 12775 227,00 228,00 1,00C08-08 12776 228,00 229,00 1,00C08-08 12777 229,00 230,00 1,00C08-08 12778 230,00 231,00 1,00C08-08 12779 231,00 232,00 1,00C08-08 12780 232,00 233,10 1,10C08-08 12781 233,10 234,21 1,11C08-08 12782 234,21 235,00 0,79C08-08 12783 235,00 236,00 1,00C08-08 12784 236,00 237,00 1,00C08-08 12785 237,00 238,00 1,00C08-08 12786 238,00 239,00 1,00C08-08 12787OREAS 15Pa Batch 1 CanC08-08 12788 239,00 240,00 1,00C08-08 12789 240,00 241,00 1,00C08-08 12790 241,00 242,00 1,00C08-08 12791 242,00 243,00 1,00C08-08 12792 243,00 243,80 0,80C08-08 12793 243,80 244,60 0,80C08-08 12794 244,60 245,46 0,86

C08-08 12795 245,46 246,28 0,82C08-08 12796 246,28 247,20 0,92C08-08 12797 247,20 248,10 0,90C08-08 12798 248,10 249,00 0,90C08-08 12799 249,00 249,93 0,93C08-08 12800 249,93 251,00 1,07C08-08 12801 251,00 252,00 1,00C08-08 12802 252,00 253,00 1,00C08-08 12803 253,00 254,00 1,00C08-08 12804 254,00 255,00 1,00C08-08 12805 255,00 256,00 1,00C08-08 12806OREAS 15Pa Batch 1 CanC08-08 12807 256,00 257,10 1,10C08-08 12808 257,10 257,90 0,80C08-08 12809 257,90 258,70 0,80C08-08 12810 258,70 259,53 0,83C08-08 12811 259,53 260,50 0,97C08-08 12812 260,50 261,50 1,00C08-08 12813 261,50 262,50 1,00C08-08 12814 262,50 263,50 1,00C08-08 12815 263,50 264,50 1,00C08-08 12816 264,50 265,50 1,00C08-08 12817 265,50 266,50 1,00C08-08 12818 266,50 267,50 1,00C08-08 12819 267,50 268,50 1,00C08-08 12820 268,50 269,55 1,05C08-08 12821 269,55 270,40 0,85C08-08 12822 270,40 271,20 0,80C08-08 12823 271,20 272,00 0,80C08-08 12824 272,00 273,00 1,00C08-08 12825 273,00 274,00 1,00C08-08 12826 274,00 275,00 1,00C08-08 12827 275,00 276,00 1,00C08-08 12828 276,00 277,00 1,00C08-08 12829 277,00 278,00 1,00C08-08 12830 278,00 279,00 1,00C08-08 12831 279,00 280,00 1,00C08-08 12832 280,00 281,00 1,00C08-08 12833 281,00 282,10 1,10C08-08 12834 282,10 283,21 1,11C08-08 12835 283,21 284,25 1,04

C08-08 12836 284,25 285,27 1,02C08-08 12837 285,27 286,17 0,90C08-08 12838 QUARTZ PurchasedC08-08 12839 286,17 287,17 1,00C08-08 12840 287,17 288,10 0,93C08-08 12841 288,10 289,00 0,90C08-08 12842 313,30 314,30 1,00C08-08 12843 314,30 315,10 0,80C08-08 12844 315,10 316,00 0,90C08-08 12845OREAS 15Pa Batch 1 CanC08-08 12846 316,00 317,00 1,00C08-08 12847 317,00 318,00 1,00C08-08 12848 318,00 319,00 1,00C08-08 12849 319,00 320,00 1,00 0 - 0,000 0,2 0,001 0,001 0,002 0,001 0,007C08-08 12850 320,00 321,00 1,00 0 - 0,000 0,2 0,001 0,012 0,002 0,001 0,007C08-08 12851 321,00 322,00 1,00 0 - 0,000 0,2 0,001 0,004 0,002 0,002 0,006C08-08 12852 322,00 323,00 1,00 0 - 0,000 0,2 0,001 0,002 0,002 0,001 0,005C08-08 12853 323,00 324,00 1,00 0 - 0,000 0,2 0,001 0,003 0,002 0,004 0,01C08-08 12854 324,00 324,80 0,80 0 - 0,000 0,2 0,002 0,005 0,002 0,035 0,059C08-08 12855 324,80 325,60 0,80 0 - 0,000 0,2 0,001 0,003 0,002 0,018 0,017C08-08 12856 325,60 326,47 0,87 0,01 - 0,010 0,2 0,002 0,002 0,002 0,015 0,02C08-08 12857 326,47 327,30 0,83 0,01 - 0,010 0,3 0,002 0,002 0,003 0,017 0,224C08-08 12858 327,30 328,10 0,80 0 0 0,000 0,3 0,002 0,006 0,004 0,008 0,024C08-08 12859 328,10 329,00 0,90 0 - 0,000 0,3 0,002 0,007 0,004 0,002 0,006C08-08 12860 329,00 330,00 1,00 0,01 - 0,010 0,3 0,002 0,007 0,005 0,001 0,006C08-08 12861 330,00 331,00 1,00 0 - 0,000 0,2 0,002 0,005 0,004 0,001 0,004C08-08 12862OREAS 15Pa Batch 1 Can 1,03 - 1,030 0,2 0,003 0,005 0,011 0,001 0,006C08-08 12863 331,00 332,00 1,00 0 - 0,000 0,2 0,001 0,003 0,003 0,005 0,015C08-08 12864 332,00 333,00 1,00 0 - 0,000 0,4 0,002 0,005 0,009 0,028 0,048C08-08 12865 333,00 334,00 1,00 0 - 0,000 0,9 0,002 0,005 0,027 0,027 0,042C08-08 12866 334,00 334,93 0,93 0 0,02 0,010 0,4 0,003 0,006 0,016 0,024 0,053C08-08 12867 334,93 335,80 0,87 0 - 0,000 0,4 0,002 0,01 0,008 0,063 0,031C08-08 12868 335,80 336,70 0,90 0 - 0,000 0,4 0,002 0,007 0,006 0,009 0,042C08-08 12869 336,70 337,60 0,90 0,01 - 0,010 0,6 0,002 0,007 0,004 0,023 0,16C08-08 12870 337,60 338,50 0,90 0,01 - 0,010 0,3 0,001 0,004 0,006 0,007 0,038C08-08 12871 338,50 339,50 1,00 0 - 0,000 0,2 0,001 0,004 0,003 0,004 0,016C08-08 12872 339,50 340,50 1,00 0 - 0,000 0,3 0,001 0,002 0,002 0,018 0,05C08-08 12873 340,50 341,49 0,99 0 - 0,000 0,2 0,001 0,002 0,002 0,002 0,017C08-08 12874 341,49 342,42 0,93 0 - 0,000 0,2 0,001 0,002 0,001 0,006 0,024C08-08 12875 342,42 343,40 0,98 0 0,04 0,020 0,2 0,001 0,001 0,001 0,007 0,017C08-08 12876 343,40 344,40 1,00 0 - 0,000 0,2 0,001 0,001 0,001 0,003 0,009

C08-08 12877 344,40 345,40 1,00 0 - 0,000 0,2 0,001 0,001 0,001 0,001 0,011C08-08 12878 345,40 346,40 1,00 0 - 0,000 0,2 0,001 0,001 0,001 0,001 0,004C08-08 12879 346,40 347,40 1,00 0 - 0,000 0,2 0,001 0,001 0,002 0,001 0,004


18,34 20 1,66 1,66 100% 0,79 0,87 52%20 23 3 3 100% 1,93 1,07 36%23 26 3 3 100% 1,40 1,60 53%26 29 3 3,02 101% 0,36 2,64 88%29 32 3 2,97 99% 0,00 3,00 100%32 35 3 3,04 101% 0,08 2,92 97%35 38 3 3 100% 0,00 3,00 100%38 41 3 3,03 101% 0,48 2,52 84%41 44 3 2,95 98% 0,84 2,16 72%44 47 3 2,65 88% 1,22 1,78 59%47 50 3 3,03 101% 0,00 3,00 100%50 53 3 3,01 100% 0,00 3,00 100%53 56 3 2,93 98% 0,00 3,00 100%56 59 3 3 100% 0,00 3,00 100%59 62 3 2,92 97% 0,00 3,00 100%62 65 3 3,05 102% 0,38 2,62 87%65 68 3 2,95 98% 0,00 3,00 100%68 71 3 3,02 101% 0,09 2,91 97%71 74 3 3,02 101% 0,00 3,00 100%74 77 3 2,95 98% 0,03 2,97 99%77 80 3 3,03 101% 0,00 3,00 100%80 83 3 3,05 102% 0,00 3,00 100%83 86 3 3,03 101% 0,00 3,00 100%86 89 3 2,97 99% 0,17 2,83 94%89 92 3 3,03 101% 0,00 3,00 100%92 95 3 2,92 97% 0,02 2,98 99%95 98 3 3,09 103% 0,32 2,68 89%98 101 3 2,94 98% 0,02 2,98 99%101 104 3 2,98 99% 0,00 3,00 100%104 107 3 3,01 100% 0,31 2,69 90%107 110 3 3,03 101% 0,00 3,00 100%110 113 3 2,99 100% 0,00 3,00 100%113 116 3 3,00 100% 0,00 3,00 100%116 119 3 3,09 103% 0,00 3,00 100%119 122 3 2,98 99% 0,00 3,00 100%122 125 3 3,00 100% 0,42 2,58 86%125 128 3 2,94 98% 0,00 3,00 100%128 131 3 2,99 100% 0,09 2,91 97%131 134 3 2,97 99% 0,58 2,42 81%134 137 3 2,93 98% 0,00 3,00 100%137 140 3 3,06 102% 0,00 3,00 100%140 143 3 2,98 99% 0,15 2,85 95%143 146 3 3,04 101% 0,00 3,00 100%146 149 3 2,99 100% 0,04 2,96 99%149 152 3 3,03 101% 0,02 2,98 99%152 155 3 2,98 99% 0,21 2,79 93%

155 158 3 3,05 102% 0,19 2,81 94%158 161 3 2,96 99% 0,22 2,78 93%161 164 3 2,97 99% 0,24 2,76 92%164 167 3 2,97 99% 0,00 3,00 100%167 170 3 2,99 100% 0,03 2,97 99%170 173 3 3,03 101% 0,11 2,89 96%173 176 3 2,95 98% 0,00 3,00 100%176 179 3 3,02 101% 0,07 2,93 98%179 182 3 3,03 101% 0,00 3,00 100%182 185 3 3,01 100% 0,12 2,88 96%185 188 3 2,99 100% 0,00 3,00 100%188 191 3 3,04 101% 0,00 3,00 100%191 194 3 2,98 99% 0,09 2,91 97%194 197 3 3,00 100% 0,00 3,00 100%197 200 3 3,01 100% 0,00 3,00 100%200 203 3 3,05 102% 0,00 3,00 100%203 206 3 2,97 99% 0,00 3,00 100%206 209 3 3,00 100% 0,14 2,86 95%209 212 3 2,94 98% 0,00 3,00 100%212 215 3 3,12 104% 0,00 3,00 100%215 218 3 2,95 98% 0,00 3,00 100%218 221 3 3,02 101% 0,00 3,00 100%221 224 3 2,99 100% 0,00 3,00 100%224 227 3 2,99 100% 0,00 3,00 100%227 230 3 3,02 101% 0,10 2,90 97%230 233 3 3,00 100% 0,15 2,85 95%233 236 3 2,98 99% 0,00 3,00 100%236 239 3 2,95 98% 0,07 2,93 98%239 242 3 3,02 101% 0,03 2,97 99%242 245 3 2,99 100% 0,00 3,00 100%245 248 3 3,06 102% 0,12 2,88 96%248 251 3 3,04 101% 0,26 2,74 91%251 254 3 2,99 100% 0,08 2,92 97%254 257 3 3,00 100% 0,00 3,00 100%257 260 3 3,02 101% 0,09 2,91 97%260 263 3 3,04 101% 0,20 2,80 93%263 266 3 2,98 99% 0,07 2,93 98%266 269 3 2,93 98% 0,00 3,00 100%269 272 3 3,06 102% 0,00 3,00 100%272 275 3 2,98 99% 0,16 2,84 95%275 278 3 3,03 101% 0,00 3,00 100%278 281 3 3,00 100% 0,07 2,93 98%281 284 3 2,97 99% 0,06 2,94 98%284 287 3 3,10 103% 0,62 2,38 79%287 290 3 3,01 100% 0,03 2,97 99%290 293 3 2,99 100% 0,48 2,52 84%293 296 3 3,05 102% 0,14 2,86 95%296 299 3 2,99 100% 0,68 2,32 77%

299 302 3 3,02 101% 1,05 1,95 65%302 305 3 3,00 100% 0,34 2,66 89%305 308 3 3,00 100% 0,00 3,00 100%308 311 3 3,01 100% 0,07 2,93 98%311 314 3 2,99 100% 0,74 2,26 75%314 317 3 3 100% 0,68 2,32 77%317 320 3 3,11 104% 0,81 2,19 73%320 323 3 2,98 99% 0,05 2,95 98%323 326 3 2,97 99% 0,22 2,78 93%326 329 3 3,04 101% 0,24 2,76 92%329 332 3 2,97 99% 0,19 2,81 94%332 335 3 3,04 101% 0,24 2,76 92%335 338 3 2,99 100% 0,00 3,00 100%338 341 3 3,05 102% 0,00 3,00 100%341 344 3 3,06 102% 0,20 2,80 93%344 347 3 2,96 99% 0,60 2,40 80%


C08-09 L-500E 2150N 250 0 -50 251m 24-août-08 01-sept-08


24,26 59,30 35,04variolitic mafic calc-alkali volcanics, grey-green, aphanitic to fg, brecciated, calcite alteration, silicification, hard, 1% py

59,30 64,92 5,62

Lamprophyre dyke/feldspar porphyry, purplish-grey, fg matrix with fds and mafic phenocryst, calcite alteration and hematite staining, silicification, hard, 1-2% py

64,92 78,38 13,46mafic calc-alkalic volcanics, grey-green, aphanitic to fg, calcite alteration, hard

78,38 90,45 12,07mafic intrusive, grey-green, mg to cg matrix with mafic and fds phenocryst, calcite alteration, hard, 2-3% py, locally 8%

90,45 136 45,55pillowed mafic calc-alkalic volcanics, grey-green, aphanitic to fg, pillowed, calcite and hematite alteration, hard, 2-3% py, up to 5% py

136,00 251,3 115,30variolithic/pillowed mafic calc-alkalic volcanics, grey-green, aphanitic to fg, pillowed, calcite and hematite alteration, hard, 1-2% py

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments43,05 43,80 0,75 lost core45,60 46,8 1,20 tuffaceous pyroclastics56,50 59,3 2,80 tuffaceous pyroclastics

89,57 90,45 0,88chloritic mafic dyke, dark-green, fg matrix with mafic phenocryst, minor py

102,54 103,44 0,90lamprophyre dyke, purplish-brown, fg to mg matrix with mafic phenocryst, calcite alteration, 5% py

208,73 210,85 2,12lamprophyre dyke, grey-green, fg matrix with tabular mafic phenocryst, calcite alteration, hard, 3-5% py

210,85 235,66 24,81 tuffaceous pyroclastics, bedding at 15-40 to CA230,11 230,28 0,17 silicified breccia, 40% altered hostrock, 10% py232,92 233,25 0,33 mafic dyke, grey-green, fg, massive, calcite alteration, 2% py

235,30 235,66 0,36intermediate dyke, green, fg, massive, calcite alteration, hematite staining, 3% py

235,66 236,53 0,87lamprophyre dyke, grey-green, fg matrix with tabular mafic phenocryst, calcite alteration, hard, 3% py

238,45 239,05 0,60syenite dyke, brownish red, fg matrix with mafic phenocryst, calcite and hematite alteration, hard, 5% py

241,04 241,29 0,25mafic dyke, medium green, aphanitic to fg, massive, calcite alteration, 8% py

242,40 242,72 0,32mafic to intermediate dyke, medium green, fg matrix with mafic phenocryst, calcite alteration, 3% py

246,25 246,88 0,63 chloritic mafic dyke, medium green, fg, massive, minor pyEOH

DDH Depth

From To Length Id Description CA Py Po Cpy Sph Gal Mag

102,54 103,44 0,90lamprophyre dyke, purplish-brown, fg to mg matrix with mafic phenocryst, calcite alteration, 5% py 5

208,73 210,85 2,12lamprophyre dyke, grey-green, fg matrix with tabular mafic phenocryst, calcite alteration, hard, 3-5% py 3

230,11 230,28 0,17 silicified breccia, 40% altered hostrock, 10% py 10

232,92 233,25 0,33mafic dyke, grey-green, fg, massive, calcite alteration, 2% py 2

235,30 235,66 0,36intermediate dyke, green, fg, massive, calcite alteration, hematite staining, 3% py 3

235,66 236,53 0,87lamprophyre dyke, grey-green, fg matrix with tabular mafic phenocryst, calcite alteration, hard, 3% py 3

238,45 239,05 0,60syenite dyke, brownish red, fg matrix with mafic phenocryst, calcite and hematite alteration, hard, 5% py 5

241,04 241,29 0,25mafic dyke, medium green, aphanitic to fg, massive, calcite alteration, 8% py 8

242,40 242,72 0,32mafic to intermediate dyke, medium green, fg matrix with mafic phenocryst, calcite alteration, 3% py 3


HoleIDSample Number


Au(g/t) Average

Ni (%)Ni (%) Check

Ni(%) Average

C08-09 12880 24,26 25,10 0,84 0 0 0,2 0,002 0,001 0,011 0,001 0,007C08-09 12881 25,10 26,00 0,90 0 0 0,2 0,002 0,003 0,011 0,001 0,007C08-09 12882 26,00 27,00 1,00 0 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 12883 27,00 28,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,006C08-09 12884 28,00 29,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,007C08-09 12885 29,00 30,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,008C08-09 12886 30,00 31,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,008C08-09 12887 31,00 32,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,008C08-09 12888DIABASE 103.5-104.0 0,01 0,01 0,2 0,002 0,013 0,002 0,001 0,01C08-09 12889 32,00 33,00 1,00 0,01 0,01 0,2 0,002 0,004 0,012 0,001 0,008C08-09 12890 33,00 34,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,007C08-09 12891 34,00 35,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 12892 35,00 36,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,005C08-09 12893 36,00 37,00 1,00 0 0 0,2 0,002 0,002 0,012 0,001 0,006C08-09 12894 37,00 38,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 12895 38,00 39,00 1,00 0,01 0,01 0,2 0,002 0,004 0,014 0,001 0,008C08-09 12896 39,00 40,00 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,007C08-09 12897 40,00 41,00 1,00 0,01 0,01 0,2 0,002 0,002 0,015 0,001 0,008C08-09 12898 41,00 42,00 1,00 0,03 0,03 0,2 0,003 0,002 0,016 0,001 0,009C08-09 12899 42,00 43,05 1,05 0 0 0,2 0,003 0,004 0,015 0,001 0,007C08-09 12900 43,80 44,60 0,80 0,06 0,04 0,05 0,2 0,002 0,004 0,013 0,001 0,006C08-09 12901 44,60 45,50 0,90 0 0 0,2 0,002 0,003 0,014 0,001 0,007C08-09 12902 45,50 46,50 1,00 0 0 0,2 0,002 0,004 0,013 0,001 0,007C08-09 12903 46,50 47,50 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,007C08-09 12904 47,50 48,50 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,006C08-09 12905 48,50 49,50 1,00 0,01 0,01 0,2 0,002 0,004 0,011 0,001 0,005C08-09 12906 49,50 50,50 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-09 12907 50,50 51,50 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,007C08-09 12908 51,50 52,50 1,00 0 0 0,2 0,002 0,002 0,014 0,001 0,009C08-09 12909OREAS 15Pa Batch 1 Can 1,04 1,04 0,2 0,003 0,006 0,011 0,001 0,007C08-09 12910 52,50 53,50 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,009C08-09 12911 53,50 54,50 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,01C08-09 12912 54,50 55,50 1,00 0 0,02 0,01 0,2 0,002 0,004 0,013 0,001 0,011C08-09 12913 55,50 56,50 1,00 0 0 0,2 0,003 0,003 0,014 0,001 0,012C08-09 12914 56,50 57,50 1,00 0 0 0,2 0,002 0,004 0,013 0,001 0,01C08-09 12915 57,50 58,40 0,90 0 0 0,2 0,002 0,005 0,012 0,001 0,011C08-09 12916 58,40 59,30 0,90 0 0 0,2 0,003 0,005 0,012 0,001 0,014C08-09 12917 59,30 60,20 0,90 0 0 0,2 0,001 0,005 0,004 0,001 0,007C08-09 12918 60,20 61,10 0,90 0 0 0,2 0,002 0,004 0,005 0,001 0,007C08-09 12919 61,10 62,00 0,90 0 0 0,2 0,001 0,004 0,004 0,001 0,006

C08-09 12920 62,00 63,00 1,00 0 0 0,2 0,002 0,004 0,005 0,001 0,007C08-09 12921 63,00 64,00 1,00 0 0 0,2 0,002 0,003 0,005 0,001 0,007C08-09 12922 64,00 64,92 0,92 0,01 0 0,005 0,2 0,002 0,005 0,005 0,001 0,008C08-09 12923 64,92 66,00 1,08 0,01 0,01 0,2 0,003 0,004 0,013 0,001 0,013C08-09 12924 66,00 67,00 1,00 0 0 0,2 0,002 0,012 0,013 0,001 0,011C08-09 12925OREAS 15Pa Batch 1 Can 0,97 0,97 0,2 0,003 0,006 0,011 0,001 0,007C08-09 12926 67,00 68,00 1,00 0,01 0,01 0,3 0,002 0,036 0,013 0,001 0,011C08-09 12927 68,00 69,00 1,00 0 0 0,2 0,002 0,002 0,01 0,001 0,008C08-09 12928 69,00 70,00 1,00 0 0 0,2 0,002 0,007 0,013 0,001 0,012C08-09 12929 70,00 71,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,011C08-09 12930 71,00 72,00 1,00 0,01 0 0,005 0,2 0,002 0,004 0,013 0,001 0,013C08-09 12931 72,00 73,00 1,00 0 0 0,2 0,002 0,002 0,012 0,001 0,009C08-09 12932 73,00 74,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,008C08-09 12933 74,00 75,00 1,00 0,01 0,01 0,3 0,002 0,037 0,01 0,001 0,008C08-09 12934 75,00 76,00 1,00 0 0 0,2 0,002 0,009 0,011 0,001 0,008C08-09 12935 76,00 76,80 0,80 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,008C08-09 12936 76,80 77,60 0,80 0 0 0,2 0,002 0,003 0,011 0,001 0,007C08-09 12937 77,60 78,38 0,78 0 0 0,2 0,002 0,002 0,012 0,001 0,008C08-09 12938 78,38 79,40 1,02 0 0 0,2 0,002 0,006 0,019 0,001 0,006C08-09 12939 79,40 80,50 1,10 0 0 0,2 0,003 0,012 0,015 0,001 0,008C08-09 12940 80,50 81,50 1,00 0 0,02 0,01 0,2 0,004 0,008 0,024 0,001 0,01C08-09 12941 81,50 82,50 1,00 0 0 0,2 0,002 0,007 0,019 0,001 0,006C08-09 12942 82,50 83,50 1,00 0 0 0,2 0,002 0,007 0,018 0,001 0,006C08-09 12943 83,50 84,50 1,00 0 0 0,2 0,002 0,007 0,02 0,001 0,005C08-09 12944 84,50 85,50 1,00 0 0 0,2 0,002 0,008 0,016 0,001 0,005C08-09 12945 85,50 86,50 1,00 0 0 0,2 0,002 0,006 0,015 0,001 0,006C08-09 12946 86,50 87,50 1,00 0 0 0,2 0,002 0,007 0,015 0,001 0,006C08-09 12947 87,50 88,50 1,00 0 0 0,2 0,002 0,006 0,018 0,001 0,006C08-09 12948 88,50 89,57 1,07 0 0 0,2 0,002 0,005 0,012 0,001 0,005C08-09 12949 QUARTZ Purchased 0 0 0,2 0,001 0,001 0,001 0,001 0,001C08-09 12950 89,57 90,45 0,88 0,01 0,01 0,2 0,003 0,005 0,028 0,001 0,011C08-09 12951 90,45 91,50 1,05 0,01 0,01 0,2 0,002 0,003 0,013 0,001 0,006C08-09 12952 91,50 92,50 1,00 0 0 0,2 0,002 0,004 0,014 0,001 0,006C08-09 12953 92,50 93,50 1,00 0 0 0,2 0,001 0,001 0,008 0,001 0,006C08-09 12954 93,50 94,50 1,00 0 0 0,2 0,001 0,001 0,009 0,001 0,006C08-09 12955 94,50 95,50 1,00 0 0 0,2 0,002 0,001 0,012 0,001 0,006C08-09 12956 95,50 96,50 1,00 0 0 0,2 0,002 0,002 0,009 0,001 0,005C08-09 12957 96,50 97,50 1,00 0 0 0,2 0,002 0,003 0,014 0,001 0,008C08-09 12958 97,50 98,50 1,00 0 0 0,2 0,002 0,002 0,012 0,001 0,007C08-09 12959 98,50 99,50 1,00 0 0,01 0,005 0,2 0,002 0,002 0,011 0,001 0,007C08-09 12960 99,50 100,50 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,008C08-09 12961 100,50 101,50 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006

C08-09 12962 101,50 102,54 1,04 0 0 0,2 0,002 0,003 0,014 0,001 0,008C08-09 12963 102,54 103,44 0,90 0,01 0,01 0,2 0,003 0,008 0,006 0,001 0,008C08-09 12964OREAS 15Pa Batch 1 Can 0,98 0,98 0,2 0,003 0,005 0,012 0,001 0,007C08-09 12965 103,44 104,30 0,86 0 0 0,2 0,002 0,003 0,012 0,001 0,008C08-09 12966 104,30 105,10 0,80 0,05 0,05 0,2 0,002 0,003 0,01 0,001 0,008C08-09 12967 105,10 106,00 0,90 0 0 0,2 0,002 0,002 0,011 0,001 0,007C08-09 12968 106,00 107,00 1,00 0,01 0,01 0,2 0,002 0,002 0,012 0,001 0,007C08-09 12969 107,00 108,00 1,00 0,01 0,01 0,2 0,002 0,002 0,011 0,001 0,007C08-09 12970 108,00 109,00 1,00 0,03 0,01 0,02 0,2 0,002 0,002 0,01 0,001 0,006C08-09 12971 109,00 110,00 1,00 0 0 0,2 0,002 0,001 0,011 0,001 0,008C08-09 12972 110,00 111,00 1,00 0 0 0,2 0,002 0,001 0,009 0,001 0,006C08-09 12973 111,00 112,00 1,00 0 0 0,2 0,002 0,001 0,012 0,001 0,008C08-09 12974 112,00 113,00 1,00 0,01 0,01 0,2 0,003 0,001 0,012 0,001 0,007C08-09 12975 113,00 114,00 1,00 0 0 0,2 0,002 0,003 0,008 0,001 0,008C08-09 12976 114,00 115,00 1,00 0 0 0,2 0,001 0,002 0,01 0,001 0,006C08-09 12977 115,00 116,00 1,00 0,03 0,01 0,02 0,2 0,002 0,001 0,014 0,001 0,006C08-09 12978 116,00 117,00 1,00 0 0 0,2 0,002 0,001 0,012 0,001 0,007C08-09 12979 117,00 118,00 1,00 0 0 0,2 0,002 0,001 0,013 0,001 0,009C08-09 12980 118,00 119,00 1,00 0 0 0,2 0,002 0,001 0,008 0,001 0,008C08-09 12981 119,00 120,00 1,00 0 0 0,2 0,002 0,001 0,007 0,001 0,006C08-09 12982 120,00 121,00 1,00 0 0 0,2 0,002 0,002 0,008 0,001 0,007C08-09 12983 121,00 122,00 1,00 0 0 0,2 0,002 0,002 0,007 0,001 0,006C08-09 12984 122,00 123,00 1,00 0 0 0,2 0,002 0,001 0,01 0,001 0,008C08-09 12985 123,00 124,00 1,00 0 0 0,2 0,001 0,002 0,008 0,001 0,007C08-09 12986 124,00 125,00 1,00 0,01 0,01 0,2 0,001 0,002 0,006 0,001 0,005C08-09 12987 125,00 126,00 1,00 0 0 0,2 0,001 0,002 0,005 0,001 0,005C08-09 12988 126,00 127,00 1,00 0 0 0,2 0,001 0,002 0,005 0,001 0,005C08-09 12989OREAS 15Pa Batch 1 Can 1,02 1,02 0,2 0,002 0,005 0,01 0,001 0,006C08-09 12990 127,00 128,00 1,00 0 0 0,2 0,002 0,004 0,007 0,001 0,005C08-09 12991 128,00 129,00 1,00 0 0 0,2 0,001 0,002 0,007 0,001 0,006C08-09 12992 129,00 130,00 1,00 0 0 0,2 0,001 0,002 0,006 0,001 0,005C08-09 12993 130,00 131,00 1,00 0 0 0,2 0,002 0,002 0,01 0,001 0,007C08-09 12994 131,00 132,00 1,00 0 0 0 0,2 0,001 0,002 0,008 0,001 0,006C08-09 12995 132,00 133,00 1,00 0 0 0,2 0,001 0,003 0,008 0,001 0,006C08-09 12996 133,00 134,00 1,00 0 0 0,2 0,002 0,001 0,01 0,001 0,006C08-09 12997 134,00 135,00 1,00 0 0 0,2 0,002 0,002 0,012 0,001 0,006C08-09 12998 135,00 136,00 1,00 0 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 12999 136,00 137,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,01C08-09 13000 137,00 138,00 1,00 0 0 0,2 0,002 0,002 0,009 0,001 0,005C08-09 13001 138,00 139,00 1,00 0,01 0,01 0,2 0,003 0,002 0,016 0,001 0,01C08-09 13002 139,00 140,00 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,008C08-09 13003 140,00 141,00 1,00 0 0,01 0,005 0,2 0,002 0,003 0,012 0,001 0,007

C08-09 13004 141,00 142,00 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,004C08-09 13005 142,00 143,00 1,00 0 0 0,2 0,002 0,003 0,014 0,001 0,006C08-09 13006 143,00 144,00 1,00 0,01 0,01 0,2 0,002 0,005 0,013 0,001 0,007C08-09 13007DIABASE 103.5-104.0 0,01 0,01 0,2 0,002 0,012 0,002 0,001 0,008C08-09 13008 144,00 145,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,006C08-09 13009 145,00 146,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13010 146,00 147,00 1,00 0,01 0,01 0,2 0,003 0,007 0,013 0,001 0,008C08-09 13011 147,00 148,00 1,00 0,01 0,01 0,2 0,002 0,003 0,009 0,001 0,007C08-09 13012 148,00 149,00 1,00 0,01 0,01 0,2 0,002 0,002 0,012 0,001 0,007C08-09 13013 149,00 150,00 1,00 0,01 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13014 150,00 151,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13015 151,00 152,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,006C08-09 13016 152,00 153,00 1,00 0 0 0,2 0,002 0,002 0,01 0,001 0,006C08-09 13017 153,00 154,00 1,00 0 0 0,2 0,002 0,004 0,01 0,001 0,006C08-09 13018 154,00 155,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13019 155,00 156,00 1,00 0 0 0,2 0,002 0,003 0,009 0,001 0,005C08-09 13020 156,00 157,00 1,00 0,04 0,04 0,2 0,002 0,003 0,01 0,001 0,006C08-09 13021 157,00 158,00 1,00 0,02 0,02 0,2 0,002 0,003 0,013 0,001 0,008C08-09 13022 158,00 159,00 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,008C08-09 13023 159,00 160,00 1,00 0 0 0,2 0,002 0,004 0,013 0,001 0,008C08-09 13024 160,00 161,00 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,007C08-09 13025 161,00 162,00 1,00 0,01 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13026 162,00 163,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13027 163,00 164,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13028 164,00 165,00 1,00 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,006C08-09 13029 165,00 166,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13030 166,00 167,00 1,00 0,01 0,01 0,2 0,002 0,004 0,01 0,001 0,005C08-09 13031OREAS 15Pa Batch 1 Can 1,03 1,03 0,2 0,003 0,006 0,011 0,001 0,007C08-09 13032 167,00 168,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13033 168,00 169,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13034 169,00 170,00 1,00 0,01 0,01 0,2 0,002 0,004 0,01 0,001 0,005C08-09 13035 170,00 171,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13036 171,00 172,00 1,00 0 0 0,2 0,002 0,002 0,009 0,001 0,005C08-09 13037 172,00 173,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13038 173,00 174,00 1,00 0,04 0,04 0,2 0,002 0,003 0,01 0,001 0,006C08-09 13039 174,00 175,00 1,00 0,01 0,01 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13040 175,00 176,00 1,00 0,01 0,01 0,2 0,002 0,004 0,01 0,001 0,006C08-09 13041 176,00 177,00 1,00 0,03 0,03 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13042 177,00 178,00 1,00 0,01 0,01 0,2 0,002 0,004 0,012 0,001 0,007C08-09 13043 178,00 179,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13044 179,00 180,00 1,00 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13045 180,00 181,00 1,00 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,007

C08-09 13046OREAS 15Pa Batch 1 Can 1,1 1,1 0,2 0,003 0,005 0,011 0,001 0,007C08-09 13047 181,00 182,00 1,00 0,01 0,01 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13048 182,00 183,00 1,00 0 0 0,2 0,002 0,004 0,009 0,001 0,005C08-09 13049 183,00 184,00 1,00 0,01 0 0,005 0,2 0,002 0,003 0,009 0,001 0,005C08-09 13050 184,00 185,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,006C08-09 13051 185,00 186,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13052 186,00 187,00 1,00 0,01 0,01 0,2 0,002 0,004 0,011 0,001 0,006C08-09 13053 187,00 188,00 1,00 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13054 188,00 189,00 1,00 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13055 189,00 190,00 1,00 0,01 0,01 0,2 0,002 0,003 0,009 0,001 0,005C08-09 13056 190,00 191,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13057 191,00 192,00 1,00 0,01 0,01 0,2 0,002 0,002 0,009 0,001 0,005C08-09 13058 192,00 193,00 1,00 0,01 0,03 0,02 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13059 193,00 194,00 1,00 0,01 0,01 0,2 0,002 0,004 0,01 0,001 0,005C08-09 13060 194,00 195,00 1,00 0,01 0,01 0,2 0,002 0,002 0,012 0,001 0,006C08-09 13061 195,00 196,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13062 196,00 197,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13063 197,00 198,00 1,00 0 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13064 QUARTZ Purchased 0 0 0,2 0,001 0,001 0,001 0,001 0,001C08-09 13065 198,00 199,00 1,00 0 0 0,2 0,002 0,002 0,01 0,001 0,005C08-09 13066 199,00 200,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13067 200,00 201,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13068 201,00 202,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13069 202,00 203,00 1,00 0 0 0,2 0,002 0,004 0,01 0,001 0,005C08-09 13070 203,00 204,00 1,00 0 0 0,2 0,001 0,003 0,008 0,001 0,004C08-09 13071 204,00 205,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13072 205,00 206,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13073 206,00 207,00 1,00 0 0 0,2 0,002 0,002 0,009 0,001 0,005C08-09 13074 207,00 207,90 0,90 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13075 207,90 208,73 0,83 0 0 0,2 0,002 0,004 0,013 0,001 0,007C08-09 13076 208,73 209,80 1,07 0,01 0,01 0,2 0,003 0,006 0,012 0,001 0,009C08-09 13077 209,80 210,85 1,05 0,01 0,01 0,2 0,004 0,009 0,016 0,001 0,012C08-09 13078 210,85 211,90 1,05 0 0,01 0,005 0,2 0,002 0,004 0,011 0,001 0,006C08-09 13079 211,90 213,00 1,10 0 0 0,2 0,002 0,004 0,011 0,001 0,006C08-09 13080 213,00 214,00 1,00 0 0 0,2 0,002 0,002 0,012 0,001 0,006C08-09 13081 214,00 215,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,006C08-09 13082 215,00 216,00 1,00 0 0 0,2 0,002 0,003 0,013 0,001 0,008C08-09 13083 216,00 217,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13084 217,00 218,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13085 218,00 219,00 1,00 0 0 0,2 0,003 0,001 0,014 0,001 0,009C08-09 13086 219,00 220,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13087 220,00 221,00 1,00 0,01 0,02 0,015 0,2 0,002 0,002 0,011 0,001 0,007

C08-09 13088OREAS 15Pa Batch 1 Can 1,03 1,03 0,2 0,003 0,005 0,01 0,001 0,006C08-09 13089 221,00 222,00 1,00 0 0 0,2 0,003 0,003 0,014 0,001 0,008C08-09 13090 222,00 223,00 1,00 0 0 0,2 0,002 0,004 0,01 0,001 0,005C08-09 13091 223,00 224,00 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,007C08-09 13092 224,00 225,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13093 225,00 226,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006C08-09 13094 226,00 227,00 1,00 0,02 0,02 0,02 0,2 0,002 0,003 0,012 0,001 0,007C08-09 13095 227,00 228,00 1,00 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,006C08-09 13096 228,00 229,00 1,00 0 0 0,2 0,002 0,002 0,014 0,001 0,008C08-09 13097 229,00 230,00 1,00 0 0 0,2 0,002 0,002 0,013 0,001 0,007C08-09 13098 230,00 231,00 1,00 0 0 0,2 0,002 0,004 0,011 0,001 0,006C08-09 13099 231,00 232,00 1,00 0,02 0,02 0,2 0,003 0,003 0,014 0,001 0,008C08-09 13100 232,00 232,92 0,92 0,01 0 0,005 0,2 0,002 0,003 0,012 0,001 0,006C08-09 13101 232,92 233,80 0,88 0 0 0,2 0,003 0,006 0,01 0,001 0,006C08-09 13102 233,80 234,70 0,90 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,007C08-09 13103 234,70 235,66 0,96 0 0 0,2 0,002 0,002 0,013 0,001 0,007C08-09 13104 235,66 236,53 0,87 0,01 0,01 0,2 0,003 0,007 0,013 0,001 0,006C08-09 13105 236,53 237,50 0,97 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13106 237,50 238,45 0,95 0 0 0,2 0,002 0,001 0,011 0,001 0,006C08-09 13107 238,45 239,05 0,60 0 0 0,2 0,002 0,006 0,002 0,001 0,006C08-09 13108 239,05 240,00 0,95 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13109 240,00 241,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13110 241,00 242,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,005C08-09 13111OREAS 15Pa Batch 1 Can 0,99 0,99 0,2 0,003 0,005 0,01 0,001 0,006C08-09 13112 242,00 243,00 1,00 0,01 0,01 0,2 0,002 0,004 0,011 0,001 0,006C08-09 13113 243,00 244,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,005C08-09 13114 244,00 245,00 1,00 0,01 0,01 0,2 0,002 0,002 0,01 0,001 0,006C08-09 13115 245,00 246,00 1,00 0,01 0,02 0,015 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13116 246,00 247,00 1,00 0,01 0,01 0,2 0,002 0,005 0,008 0,001 0,005C08-09 13117 247,00 248,00 1,00 0,01 0,01 0,2 0,003 0,005 0,013 0,001 0,008C08-09 13118 248,00 248,90 0,90 0 0 0,2 0,003 0,001 0,013 0,001 0,009C08-09 13119 248,90 249,70 0,80 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-09 13120 249,70 250,50 0,80 0 0 0,2 0,002 0,003 0,011 0,001 0,005C08-09 13121 250,50 251,30 0,80 0 0 0,2 0,002 0,004 0,012 0,001 0,007


24,26 26 1,74 1,74 100% 0,32 1,42 82%26 29 3 3 100% 0,90 2,10 70%29 32 3 3,05 102% 0,77 2,23 74%32 35 3 3 100% 1,46 1,54 51%35 38 3 3 100% 2,75 0,25 8%38 41 3 3 100% 2,33 0,67 22%41 44 3 2,25 75% 1,82 1,18 39%44 47 3 3,06 102% 1,25 1,75 58%47 50 3 2,99 100% 0,00 3,00 100%50 53 3 2,98 99% 0,00 3,00 100%53 56 3 2,98 99% 0,00 3,00 100%56 59 3 3 100% 0,00 3,00 100%59 62 3 3,04 101% 0,01 2,99 100%62 65 3 3,05 102% 0,14 2,86 95%65 68 3 2,96 99% 0,05 2,95 98%68 71 3 2,97 99% 0,00 3,00 100%71 74 3 3,06 102% 0,00 3,00 100%74 77 3 2,96 99% 0,05 2,95 98%77 80 3 3,07 102% 0,12 2,88 96%80 83 3 3,00 100% 0,08 2,92 97%83 86 3 2,95 98% 0,06 2,94 98%86 89 3 3,02 101% 0,08 2,92 97%89 92 3 3,02 101% 0,07 2,93 98%92 95 3 3,01 100% 0,00 3,00 100%95 98 3 3,00 100% 0,14 2,86 95%98 101 3 2,95 98% 0,05 2,95 98%101 104 3 3,00 100% 0,08 2,92 97%104 107 3 3,04 101% 0,14 2,86 95%107 110 3 3,01 100% 0,09 2,91 97%110 113 3 3,00 100% 0,00 3,00 100%113 116 3 2,99 100% 0,00 3,00 100%116 119 3 3,04 101% 0,00 3,00 100%119 122 3 2,94 98% 0,14 2,86 95%122 125 3 3,01 100% 0,00 3,00 100%125 128 3 3,00 100% 0,00 3,00 100%128 131 3 3,02 101% 0,00 3,00 100%131 134 3 3,00 100% 0,00 3,00 100%134 137 3 3,00 100% 0,06 2,94 98%137 140 3 3,06 102% 0,00 3,00 100%140 143 3 3,00 100% 0,00 3,00 100%143 146 3 3,04 101% 0,03 2,97 99%146 149 3 2,93 98% 0,00 3,00 100%149 152 3 3,09 103% 0,00 3,00 100%152 155 3 2,96 99% 0,00 3,00 100%155 158 3 3,05 102% 0,00 3,00 100%158 161 3 2,98 99% 0,00 3,00 100%

161 164 3 3,03 101% 0,00 3,00 100%164 167 3 2,96 99% 0,00 3,00 100%167 170 3 3,01 100% 0,00 3,00 100%170 173 3 3,03 101% 0,00 3,00 100%173 176 3 3,03 101% 0,00 3,00 100%176 179 3 3,00 100% 0,00 3,00 100%179 182 3 2,96 99% 0,00 3,00 100%182 185 3 2,99 100% 0,00 3,00 100%185 188 3 2,98 99% 0,00 3,00 100%188 191 3 3,01 100% 0,00 3,00 100%191 194 3 3,03 101% 0,08 2,92 97%194 197 3 3,02 101% 0,03 2,97 99%197 200 3 2,96 99% 0,00 3,00 100%200 203 3 2,97 99% 0,00 3,00 100%203 206 3 3,04 101% 0,07 2,93 98%206 209 3 3,00 100% 0,06 2,94 98%209 212 3 3,02 101% 0,13 2,87 96%212 215 3 2,93 98% 0,00 3,00 100%215 218 3 3,02 101% 0,00 3,00 100%218 221 3 3,04 101% 0,00 3,00 100%221 224 3 3,01 100% 0,07 2,93 98%224 227 3 2,97 99% 0,06 2,94 98%227 230 3 3,01 100% 0,35 2,65 88%230 233 3 2,96 99% 0,00 3,00 100%233 236 3 3,04 101% 0,00 3,00 100%236 239 3 3,02 101% 0,06 2,94 98%239 242 3 3,00 100% 0,07 2,93 98%242 245 3 2,97 99% 0,00 3,00 100%245 248 3 3,00 100% 0,00 3,00 100%248 251 3 3,01 100% 0,05 2,95 98%


C08-10 L-500E 2150N 250 0 -60 42m 02-sept-08 03-sept-08


21,35 41,50 20,15variolitic mafic calc-alkalic volcanic, pale grey-green, aphanitic to fg, calcite alteration, silicification, hard, 1% py

EOHabandoned

DDH Depth

HoleID Sample Id From (m) To (m) Length (m) Au Au Check Au_avg Ag Co Cu Ni Pb ZnC08-10 13122 21,35 22,20 0,85 0,01 0,01 0,01 0,2 0,002 0,002 0,01 0,001 0,005C08-10 13123 22,20 23,00 0,80 0 0 0,2 0,002 0,003 0,012 0,001 0,007C08-10 13124 23,00 24,00 1,00 0,01 0,01 0,2 0,002 0,001 0,009 0,001 0,005C08-10 13125 24,00 25,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,006C08-10 13126 25,00 26,00 1,00 0 0 0,2 0,002 0,003 0,009 0,001 0,005C08-10 13127 26,00 27,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,005C08-10 13128 27,00 28,00 1,00 0 0 0,2 0,002 0,002 0,009 0,001 0,005C08-10 13129 DIABASE 104.0-104.5 0,01 0,01 0,2 0,002 0,013 0,002 0,001 0,008C08-10 13130 28,00 29,00 1,00 0 0 0,2 0,002 0,003 0,011 0,001 0,006C08-10 13131 29,00 30,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,006C08-10 13132 30,00 31,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,005C08-10 13133 31,00 32,00 1,00 0 0 0,2 0,002 0,003 0,01 0,001 0,006C08-10 13134 32,00 33,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-10 13135 33,00 34,00 1,00 0,01 0,01 0,2 0,002 0,003 0,011 0,001 0,006C08-10 13136 34,00 35,00 1,00 0,01 0,01 0,2 0,003 0,002 0,014 0,001 0,009C08-10 13137 35,00 36,00 1,00 0,02 0 0,01 0,2 0,003 0,003 0,013 0,001 0,008C08-10 13138 36,00 37,00 1,00 0,01 0,01 0,2 0,002 0,003 0,01 0,001 0,006C08-10 13139 37,00 38,00 1,00 0,01 0,01 0,2 0,002 0,002 0,012 0,001 0,007C08-10 13140 38,00 39,00 1,00 0 0 0,2 0,002 0,002 0,011 0,001 0,006C08-10 13141 39,00 39,90 0,90 0,01 0,01 0,2 0,002 0,003 0,012 0,001 0,007C08-10 13142 39,90 40,70 0,80 0 0 0,2 0,002 0,003 0,011 0,001 0,005C08-10 13143 40,70 41,50 0,80 0 0 0,2 0,002 0,003 0,01 0,001 0,005


21,35 23 1,65 1,65 100% 0,47 1,18 72%23 26 3 3 100% 1,30 1,70 57%26 29 3 3 100% 0,78 2,22 74%29 32 3 3 100% 1,00 2,00 67%32 35 3 3 100% 1,47 1,53 51%35 38 3 3 100% 1,82 1,18 39%38 41 3 3 100% 2,12 0,88 29%41 41,5 0,5 0,5 100% 0,50 0,00 0%


C-08-11 L-3300E 800N 300 0 -50 296m 05/09/08 13/09/08 G.Spyratos Dec 4 - Dec 8, 2009

From To Length Id Rock type Photo0,00 25,65 25,65 Overburden25,65 71,00 45,35 Pillowed Komatiitic Metavolcanics

71,00 110,58 39,58 Basaltic Komatiitic Metavolcanics

110,58 134,54 23,96 Pillowed Komatiitic Metavolcanics

134,54 176,72 42,18 Basaltic Komatiitic Metavolcanics


296,30 EOH

Dark grey-green to dark green and dark grey. Grey-green to medium green, locally. Fine grained. Pillowed, with occasional pillow selvages. Local pillow breccias. Moderately fractured, with carbonate/serpentine filled fractures. Local brecciated, shear zones. Rare qtz/carbonate stringers. Moderately hard to hard. Moderately to strongly, magnetic. LC, at 65 deg tca.

Medium green to pale grey-green and grey, locally. Fine grained. Pillowed, with occasional pillow selvages. Rare interpillow breccias. Weakly fractured, with chlorite filled fractures. Negligible amount of carbonate/talc veining. Patchy leucoxene alteration. Moderately hard to moderately soft. Weakly magnetic, locally. LC, at 70 deg tca.

Dark grey-green to dark grey. Grey-green to dark green, locally. Fine grained. Pillowed, with occasional pillow selvages. Local pillow breccias. Moderately fractured, with serpentine or carbonate/serpentine filled fractures. Rare qtz/carbonate stringers. Patchy leucoxene alteration. Moderately hard to hard. Moderately to strongly, magnetic.


0-25(?): CasingDark grey-green to dark green and dark grey. Grey-green, locally. Fine grained. Pillowed, with rare pillow selvages. Weakly fractured, with serpentine filled fractures. Weakly to moderately brecciated, locally. Local weak schistocity. Rare carbonate/serpentine stringers. Hard. Moderately to strongly, magnetic. Hole partly sampled as per Andre Ciesielski's instruction. LC, gradual.

Medium green to pale grey-green and grey, locally. Fine grained. Pillowed, with occasional pillow selvages. Rare interpillow breccias. Local varioles. Weakly fractured, with chlorite filled fractures. Negligible amount of carbonate/talc veining. Moderately hard to moderately soft. Weakly magnetic, locally. LC, broken.

From To Length Id Rock types, Change in grain size, colour, etc. Photo30,00 30,30 0,30 Lost core34,10 34,60 0,50 Lost core35,80 35,90 0,10 Spinifex texture, with crashed needles37,00 37,80 0,80 Lost core42,00 42,30 0,30 Lost core48,40 48,80 0,40 Spinifex texture, with crashed needles109,23 110,58 1,35 Intermediate Dyke

116,85 117,50 0,65 Lost core120,10 120,20 0,10 Spinifex texture, with crashed needles126,35 126,60 0,25 Spinifex texture, with crashed needles183,40 184,20 0,80 Spinifex texture, with crashed needles202,42 202,60 0,18 Spinifex texture, with crashed needles204,50 204,80 0,30 Lost core215,85 216,00 0,15 Spinifex texture, with crashed needles219,70 220,30 0,60 Spinifex texture, with crashed needles259,00 259,10 0,10 Spinifex texture, with crashed needles278,65 278,90 0,25 Spinifex texture, with crashed needles

Greyish-brown to greenish-brown. Fine grained matrix, with rare feldspar phenocrysts. Weakly fractured. Hard. Non-magnetic. UC, defined 2.5cm gouge, at 60 deg tca. LC, broken.


Comments PhotoFrom To Length Id BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW25,65 71,00 45,35 1 50 1 2 Locally brecciated71,00 89,96 18,96 1 2 Locally brecciated89,96 90,63 0,67 3 65 3 1090,63 109,23 18,60 1 2 Locally brecciated109,23 110,58 1,35 15 0110,58 111,05 0,47 3 45 4 5111,05 113,80 2,75 3 3113,80 114,28 0,48 4 50 5 5114,28 130,00 15,72 1 2 Locally brecciated130,00 132,00 2,00 4 5 Locally brecciated132,00 134,54 2,54 1 3 Locally brecciated134,54 137,25 2,71 1 1 Locally brecciated137,25 138,00 0,75 5 3138,00 176,72 38,72 1 1 Locally brecciated176,72 191,95 15,23 2 1 Locally brecciated191,95 192,40 0,45 3 50 4 5 Irregular foliation192,40 193,75 1,35 2 1 Locally brecciated193,75 194,00 0,25 4 60 4 5194,00 296,30 102,30 2 1 Locally brecciated


From To Length Id Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Comments25,65 66,00 40,35 3 1066,00 67,00 1,00 2 2 3 5 Patchy talc alteration67,00 71,00 4,00 3 1071,00 109,23 38,23 1 4 5 Patchy talc alteration109,23 110,58 1,35 3110,58 134,54 23,96 1 3 1 15 Patchy talc and chlorite134,54 176,72 42,18 1 4 5 Patchy talc alteration176,72 223,00 46,28 1 3 20 Patchy talc alteration223,00 224,00 1,00 1 2224,00 254,30 30,30 1 3 10 Patchy talc alteration254,30 254,60 0,30 1 2254,60 258,70 4,10 1 3 10 Patchy talc alteration258,70 259,20 0,50 1 2259,20 296,30 37,10 1 3 10 Patchy talc alteration


From To Length Id Description SUL PY PO CPY SPH GAL MAG HEM25,65 52,00 26,35 0,552,00 55,00 3,00 0,5 0,155,00 66,00 11,00 0,566,00 67,00 1,00 0,5 0,567,00 71,00 4,00 0,571,00 86,00 15,00 0,586,00 87,00 1,00 287,00 89,00 2,00 0,589,00 90,00 1,00 190,00 91,00 1,00 0,5 0,1 0,191,00 109,23 18,23 0,5109,23 110,58 1,35 0,5110,58 112,00 1,42 0,5112,00 113,00 1,00 2113,00 121,00 8,00 0,5121,00 122,00 1,00 2122,00 128,00 6,00 0,5128,00 129,00 1,00 0,5 0,1129,00 134,54 5,54 1134,54 139,00 4,46 0,5139,00 140,00 1,00 0,5 0,1140,00 155,00 15,00 0,5155,00 165,00 10,00 1165,00 176,72 11,72 0,5176,72 202,00 25,28 0,5202,00 203,00 1,00 0,5 0,5203,00 229,00 26,00 0,5229,00 230,00 1,00 0,5 0,1230,00 247,00 17,00 0,5247,00 248,00 1,00 0,5 0,5248,00 264,00 16,00 0,5264,00 265,00 1,00 1 0,1265,00 272,00 7,00 1272,00 273,00 1,00 1 0,5


273,00 275,00 2,00 1275,00 296,30 21,30 0,5

HoleID Sample Id From (m) To (m) Length (m) Au Au chk Ag Co Cu Ni Pb ZnC08-11 37795 46,00 47,00 1,00C08-11 37796 47,00 48,00 1,00C08-11 37797 48,00 49,00 1,00C08-11 37798 49,00 50,00 1,00C08-11 37799 50,00 51,00 1,00C08-11 37800 51,00 52,00 1,00C08-11 37801 52,00 53,00 1,00C08-11 37802 53,00 54,00 1,00C08-11 37803 54,00 55,00 1,00C08-11 37804 55,00 56,00 1,00C08-11 37805 56,00 57,00 1,00C08-11 37806 57,00 58,00 1,00C08-11 37807 58,00 59,00 1,00C08-11 37808 65,00 66,00 1,00C08-11 37809 66,00 67,00 1,00C08-11 37810OREAS 15Pa Batch 2 CanC08-11 37811 67,00 68,00 1,00C08-11 37812 85,00 86,00 1,00C08-11 37813 86,00 87,00 1,00C08-11 37814 87,00 88,00 1,00C08-11 37815 88,00 89,00 1,00C08-11 37816 89,00 90,00 1,00C08-11 37817 90,00 91,00 1,00C08-11 37818 91,00 92,00 1,00C08-11 37819 108,30 109,23 0,93C08-11 37820 109,23 109,90 0,67C08-11 37821 109,90 110,58 0,68C08-11 37822 110,58 111,30 0,72C08-11 37823 111,30 112,00 0,70C08-11 37824 112,00 113,00 1,00C08-11 37825 113,00 113,60 0,60C08-11 37826 113,60 114,28 0,68C08-11 37827 OREAS 6Pc Batch 1 CanC08-11 37828 114,28 115,20 0,92C08-11 37829 120,00 121,00 1,00C08-11 37830 121,00 122,00 1,00C08-11 37831 122,00 123,00 1,00C08-11 37832 127,00 128,00 1,00C08-11 37833 128,00 129,00 1,00C08-11 37834 129,00 130,00 1,00C08-11 37835 130,00 131,00 1,00C08-11 37836 131,00 132,00 1,00

C08-11 37837 132,00 132,90 0,90C08-11 37838 132,90 133,70 0,80C08-11 37839 133,70 134,54 0,84C08-11 37840 134,54 135,40 0,86C08-11 37841 135,40 136,30 0,90C08-11 37842 136,30 137,25 0,95C08-11 37843 137,25 138,00 0,75C08-11 37844 DIABASE 109.0-109.5C08-11 37845 138,00 139,00 1,00C08-11 37846 139,00 140,00 1,00C08-11 37847 140,00 141,00 1,00C08-11 37848 154,00 155,00 1,00C08-11 37849 155,00 156,00 1,00C08-11 37850 156,00 157,00 1,00C08-11 37851 157,00 158,00 1,00C08-11 37852 158,00 159,00 1,00C08-11 37853 159,00 160,00 1,00C08-11 37854 160,00 161,00 1,00C08-11 37855 161,00 162,00 1,00C08-11 37856 162,00 163,00 1,00C08-11 37857 163,00 164,00 1,00C08-11 37858 164,00 165,00 1,00C08-11 37859 165,00 166,00 1,00C08-11 37860 190,00 191,00 1,00C08-11 37861 191,00 192,00 1,00C08-11 37862 192,00 193,00 1,00C08-11 37863 193,00 194,00 1,00C08-11 37864 194,00 195,00 1,00C08-11 37865 195,00 196,00 1,00C08-11 37866 201,00 202,00 1,00C08-11 37867 202,00 203,00 1,00C08-11 37868OREAS 15Pa Batch 2 CanC08-11 37869 203,00 204,00 1,00C08-11 37870 228,00 229,00 1,00C08-11 37871 229,00 230,00 1,00C08-11 37872 230,00 231,00 1,00C08-11 37873 246,00 247,00 1,00C08-11 37874 247,00 248,00 1,00C08-11 37875 248,00 249,00 1,00C08-11 37876 263,00 264,00 1,00C08-11 37877 264,00 265,00 1,00C08-11 37878 265,00 266,00 1,00C08-11 37879 266,00 267,00 1,00

C08-11 37880 267,00 268,00 1,00C08-11 37881 268,00 269,00 1,00C08-11 37882 269,00 270,00 1,00C08-11 37883 270,00 271,00 1,00C08-11 37884 271,00 272,00 1,00C08-11 37885 272,00 273,00 1,00C08-11 37886 OREAS 6Pc Batch 1 CanC08-11 37887 273,00 274,00 1,00C08-11 37888 274,00 275,00 1,00


0 25,65 OB25,65 26 0,35 100,00 0,35 0,00 25,65 26,38

26 29 3,00 100,00 0,76 74,67 28,03 2929 32 2,70 90,00 1,09 59,63 Lost core 29,67 5132 35 2,50 83,33 1,80 28,00 Lost core35 38 2,20 73,33 1,87 15,00 Lost core38 41 3,00 100,00 1,70 43,3341 44 2,70 90,00 1,45 46,30 Lost core44 47 3,00 100,00 1,80 40,0047 50 3,00 100,00 2,10 30,0050 53 3,00 100,00 1,44 52,00 52,42 55,653 56 3,00 100,00 1,63 45,6756 59 3,00 100,00 1,25 58,33 58 59,0459 62 3,05 101,67 0,49 83,93 61,53 61,8762 65 2,91 97,00 0,83 71,48 63,04 63,2465 68 2,96 98,67 0,95 67,91 63,9 64,3668 71 3,10 103,33 1,42 54,19 65,68 65,971 74 3,03 101,00 0,39 87,13 66,45 70,6674 77 2,90 96,67 1,88 35,17 72,04 72,28 74,34 74,35 At 60 deg tca77 80 2,98 99,33 0,56 81,21 73,14 73,5180 83 3,05 101,67 1,47 51,80 74,25 76,1783 86 2,98 99,33 0,49 83,56 80,84 82,9886 89 3,03 101,00 1,26 58,42 85,72 87,0789 92 3,01 100,33 0,73 75,75 87,96 88,992 95 2,96 98,67 0,49 83,45 90,28 90,9795 98 2,98 99,33 0,44 85,23 92,45 92,6798 101 3,00 100,00 0,50 83,33 101,5 102,88101 104 3,00 100,00 1,10 63,33 104,53 106,05104 107 2,96 98,67 0,94 68,24 108,38 109,49107 110 3,05 101,67 0,72 76,39 110,04 110,7 109,23 109,26 At 60 deg tca.110 113 3,03 101,00 1,53 49,50 111,73 112,68113 116 3,05 101,67 1,17 61,64 113,53 113,87116 119 2,35 78,33 1,21 48,51 Lost core 114,26 114,7119 122 3,00 100,00 1,25 58,33 115,52 117,9122 125 3,00 100,00 0,55 81,67 118,75 119,18125 128 3,07 102,33 0,66 78,50 120,67 122,03128 131 2,97 99,00 0,41 86,20 123,75 124,31131 134 2,97 99,00 1,04 64,98 131,13 131,66134 137 3,00 100,00 0,14 95,33 132,19 132,46137 140 3,02 100,67 0,42 86,09 133,18 133,94

Fault gougeDDH Depth Recovery RQDGeotechnical Log

Blocky core Crumbly core

140 143 3,00 100,00 0,17 94,33143 146 3,02 100,67 0,00 100,00146 149 3,00 100,00 0,16 94,67 147,38 147,58149 152 2,98 99,33 0,08 97,32152 155 3,05 101,67 0,42 86,23 152,83 152,97155 158 2,94 98,00 0,21 92,86 154,88 155,11158 161 2,97 99,00 0,18 93,94161 164 3,04 101,33 0,30 90,13 162,04 162,24164 167 2,89 96,33 0,75 74,05 164,06 164,22167 170 3,10 103,33 0,63 79,68 164,88 165,36170 173 3,03 101,00 0,21 93,07 170 170,19173 176 2,92 97,33 0,69 76,37 175,06 175,87176 179 3,00 100,00 1,21 59,67 176,72 179179 182 3,00 100,00 0,83 72,33 180,91 183,28182 185 3,00 100,00 1,14 62,00 184,44 184,72185 188 3,00 100,00 0,92 69,33 185,42 186,3188 191 3,00 100,00 0,85 71,67 190,75 191,18191 194 3,00 100,00 1,90 36,67 191,95 196,25194 197 3,00 100,00 1,62 46,00197 200 3,00 100,00 1,65 45,00 197 202,1200 203 3,00 100,00 1,89 37,00203 206 2,70 90,00 2,25 16,67 Lost core 203 207,05206 209 3,00 100,00 0,97 67,67209 212 3,00 100,00 1,27 57,67 210,63 211,72212 215 3,00 100,00 0,60 80,00 214,42 216,62215 218 3,00 100,00 1,40 53,33218 221 3,05 101,67 0,41 86,56221 224 3,00 100,00 0,38 87,33 222,37 222,52224 227 3,03 101,00 0,50 83,50227 230 2,94 98,00 0,44 85,03230 233 3,00 100,00 0,85 71,67 230,02 231,17233 236 3,00 100,00 1,42 52,67 233,62 234,4236 239 3,00 100,00 1,50 50,00 234,8 237,61239 242 2,93 97,67 0,38 87,03 240,49 240,8242 245 3,00 100,00 1,23 59,00 244 245,48245 248 3,05 101,67 0,66 78,36 246,71 247,33248 251 3,00 100,00 0,37 87,67251 254 3,06 102,00 0,52 83,01 252,97 253,41254 257 2,99 99,67 0,24 91,97257 260 3,00 100,00 0,50 83,33 257,96 258,26260 263 2,99 99,67 0,47 84,28263 266 3,00 100,00 0,16 94,67266 269 2,96 98,67 0,32 89,19 266,67 266,91

269 272 3,00 100,00 0,44 85,33 271,3 271,9272 275 3,00 100,00 1,46 51,33 273,26 275275 278 3,00 100,00 0,49 83,67 276,05 276,29278 281 3,00 100,00 1,35 55,00 278 278,54281 284 3,00 100,00 2,00 33,33 279,52 280,42284 287 3,00 100,00 0,80 73,33 281,15 285,86287 290 3,00 100,00 0,70 76,67290 293 3,00 100,00 0,83 72,33 290,96 291,82293 296 3,30 110,00 0,95 71,21 295,38 296,13


C-08-12 L-3300E 950N 300 0 -50 300m 14-sept-08 20-sept-08 G.Spyratos Dec 8 - Dec 18, 2009

From To Length Id Rock type Photo0,00 13,55 13,55 Overburden13,55 167,10 153,55 Pillowed Komatiitic Metavolcanics

167,10 189,95 22,85 Talcose Komatiitic Metavolcanics


200,34 202,21 1,87 Talcose Komatiitic Metavolcanics


299,95 EOH.

Dark grey-green to dark grey and locally dark green and grey. Fine grained. Possibly pillowed, with hard to see pillow selvages. Commonly brecciated. Common shearing. Strongly fractured, with carbonate/talc and locally carbonate/serpentine, filled fractures. Moderately soft to soft. Weakly to moderately, magnetic. LC, at 40 deg tca.

Dark grey-green to dark green and dark grey. Medium green, locally. Fine grained. Pillowed, with occasional pillow selvages. Weakly to moderately fractured, with carbonate/serpentine or serpentine filled fractures. Weakly to moderately brecciated, locally. Patchy leucoxene and chlorite, alteration. Moderately hard. Weakly magnetic, locally. LC,at 50 deg tca.

Grey to dark grey-green. Fine grained. Commonly brecciated. Weak to moderate shearing. Moderately soft to soft. Moderately magnetic. LC, at 65 deg tca.

Dark grey-green, dark green, dark olive green and dark grey. Medium green, locally. Fine grained. Pillowed, with occasional pillow selvages. Weakly to moderately fractured, with mostly serpentine and lesser carbonate/serpentine, filled fractures. Weakly to moderately brecciated, locally. Patchy leucoxene and chlorite, alteration. Moderately hard to hard. Weakly to moderately magnetic.


0-13(?): CasingDark grey-green to dark green and dark grey. Grey-green to medium green, locally. Fine grained. Pillowed, with occasional pillow selvages. Weakly to moderately fractured, with carbonate/serpentine or serpentine filled fractures. Weakly to moderately brecciated, locally. Rare carbonate/serpentine stringers. Patchy leucoxene alteration. Hole partly sampled as per Andre Ciesielski's instruction. Hard. Moderately to strongly, magnetic. LC, broken.

From To Length Id Rock types, Change in grain size, colour, etc. Photo17,25 17,75 0,50 Spinifex texture, with crashed needles28,40 29,00 0,60 Spinifex texture, with crashed needles34,00 34,35 0,35 Spinifex texture, with crashed needles35,40 35,50 0,10 Spinifex texture, with crashed needles39,65 39,90 0,25 Spinifex texture, with crashed needles42,50 43,10 0,60 Spinifex texture, with crashed needles52,90 53,10 0,20 Spinifex texture, with crashed needles60,70 60,90 0,20 Spinifex texture, with crashed needles82,50 82,90 0,40 Spinifex texture, with crashed needles89,60 90,00 0,40 Lost core90,47 90,85 0,38 Spinifex texture, with crashed needles91,10 91,35 0,25 Spinifex texture, with crashed needles108,70 109,15 0,45 Lost core145,30 145,90 0,60 Spinifex texture, with crashed needles146,00 148,15 2,15 Local spinifex texture, with crashed needles152,60 153,20 0,60 Lost core174,94 175,65 0,71 Intermediate Dyke

175,65 176,10 0,45 Lost core177,42 179,28 1,86 Intermediate Dyke

179,28 179,45 0,17 Biotitic contact179,45 181,21 1,76 Shear Zone, with 5% gouge, near contacts181,21 181,22 0,01 Chloritic contact181,22 182,70 1,48 Intermediate Dyke

185,30 187,87 2,57 Ultramafic Dyke

187,87 187,90 0,03 Gouge188,49 188,72 0,23 Gouge197,15 198,30 1,15 Spinifex texture, with crashed needles199,00 199,18 0,18 Chloritic contact UC, broken. LC, at 20 deg tca.

LC, at 55 deg tca.Brown to grey-brown, with greyish-buff patches. Fine grained. Strongly fractured, with chlorite filled fractures. Locally brecciated. LC, at 15 deg tca.Dark grey. Fine to medium grained. Massive. Moderately hard to moderately soft. Weakly magnetic, locally. UC, at 60 deg tca. LC, at 65 deg tca.LC, at 65 deg tca.UC, at 60 deg tca. LC, at 55 deg tca.

Greyish-brown to brown. Fine grained matrix, with common mafic phenocrysts. No veining. UC, at 40 deg tca. LC, broken.

Greyish-brown to brown. Fine grained matrix, with common mafic phenocrysts and occasional feldspar phenocrysts. UC, irregular at appr 10 deg tca. LC, broken.LC, brokenLC, at 60 deg tca.


199,18 199,60 0,42 Biotitic Mafic Dyke199,60 199,72 0,12 Chloritic contact210,30 210,32 0,02 Gouge214,65 214,80 0,15 Spinifex texture, with crashed needles215,00 215,20 0,20 Spinifex texture, with crashed needles224,90 225,40 0,50 Spinifex texture, with crashed needles230,90 231,15 0,25 Spinifex texture, with crashed needles249,30 249,45 0,15 Spinifex texture, with crashed needles259,40 259,95 0,55 Spinifex texture, with crashed needles269,00 269,37 0,37 Spinifex texture, with crashed needles271,80 273,35 1,55 Spinifex texture, with crashed needles274,00 275,00 1,00 Local spinifex texture, with crashed needles288,15 288,45 0,30 Spinifex texture, with crashed needles291,35 291,50 0,15 Spinifex texture, with crashed needles293,32 294,60 1,28 Lamprophyre Dyke

LC, at 40 deg tca.LC, at 40 deg tca.At 40 deg tca.

Grey-brown to brown. Fine grained matrix, with common felsic fragments and occasional mafic fragments. Fragments are up to 5mm across. No veining. Chloritic at upper contact. Chloritic/biotitic near lower contact. Hard. Non-magnetic. Both contacts, broken.

Comments PhotoFrom To Length Id BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW13,55 26,42 12,87 1 1 Locally brecciated26,42 26,90 0,48 4 50 5 526,90 43,60 16,70 1 1 Locally brecciated43,60 48,30 4,70 1 5048,30 86,00 37,70 1 1 Locally brecciated86,00 89,00 3,00 1 5089,00 123,25 34,25 1 1 Locally brecciated123,25 123,70 0,45 1 50123,70 134,00 10,30 1 1 Locally brecciated134,00 140,30 6,30 1 50 1 2 Locally brecciated140,30 142,00 1,70 1 Locally brecciated142,00 142,55 0,55 5 15142,55 150,00 7,45 1 1 Locally brecciated150,00 152,60 2,60 1 45 1 1 Locally brecciated153,20 167,10 13,90 1 1 Locally brecciated167,10 171,20 4,10 3 5171,20 173,00 1,80 3 50 4 10173,00 174,50 1,50 3 5174,50 174,94 0,44 4 55 4 10176,10 177,42 1,32 1 3177,42 179,28 1,86 4 30179,45 181,22 1,77 3 45 2 10181,22 182,70 1,48 1 15 10182,70 185,30 2,60 3 45 3 5185,30 187,87 2,57 3187,87 189,95 2,08 4 50 4 10189,95 200,34 10,39 1 2 Locally brecciated200,34 202,21 1,87 2 50 3 5202,21 236,85 34,64 1 1 Locally brecciated236,85 237,18 0,33 4 45 5 5237,18 248,11 10,93 1 1 Locally brecciated248,11 250,15 2,04 3 15250,15 275,60 25,45 1 1 Locally brecciated275,60 280,10 4,50 1 50 1280,10 299,95 19,85 1 1 Locally brecciated


From To Length Id Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Comments13,55 28,30 14,75 3 1028,30 43,00 14,70 3 1 10 Patchy chlorite alteration43,00 57,55 14,55 3 1057,55 61,00 3,45 3 1 5 Patchy chlorite alteration61,00 81,00 20,00 3 1081,00 83,00 2,00 2 2 5 Patchy chlorite alteration83,00 90,00 7,00 3 1090,00 90,80 0,80 1 390,80 118,00 27,20 3 10118,00 119,28 1,28 1 3119,28 129,90 10,62 3 10129,90 132,35 2,45 1 3132,35 142,55 10,20 3 10142,55 148,15 5,60 1 3148,15 167,10 18,95 3 10167,10 171,20 4,10 2 1 1 15 Patchy talc and chlorite171,20 174,94 3,74 3 2 20 Patchy chlorite174,94 175,65 0,71 5176,10 177,42 1,32 1 3 5177,42 179,28 1,86 5179,28 179,45 0,17 4179,45 181,22 1,77 5 10181,22 182,70 1,48 5182,70 185,30 2,60 4 10185,30 187,87 2,57 2187,87 189,95 2,08 4 15189,95 199,00 9,05 3 1 10 Patchy chlorite alteration199,00 199,18 0,18 5199,18 199,60 0,42 5199,60 199,72 0,12 5199,72 200,34 0,62 3 1 10 Patchy chlorite alteration200,34 202,21 1,87 5 15202,21 214,00 11,79 4 5214,00 215,60 1,60 1 2215,60 224,00 8,40 4 5224,00 273,50 49,50 3 2 5 Patchy chlorite alteration273,50 293,32 19,82 4 10293,32 294,60 1,28 5 1 2294,60 299,95 5,35 4 10


From To Length Id Description SUL PY PO CPY SPH GAL MAG HEM13,55 20,00 6,45 0,520,00 27,00 7,00 127,00 67,00 40,00 0,567,00 71,00 4,00 0,5 0,171,00 86,00 15,00 0,586,00 87,00 1,00 0,5 0,187,00 124,00 37,00 0,5124,00 128,00 4,00 1128,00 140,00 12,00 0,5140,00 143,00 3,00 2143,00 148,15 5,15 0,5148,15 156,00 7,85 2156,00 167,10 11,10 0,5167,10 174,94 7,84 1174,94 175,65 0,71 Disseminated PY 10176,10 177,42 1,32 1177,42 179,28 1,86 10179,28 181,22 1,94 0,5181,22 182,70 1,48 5182,70 185,30 2,60 Honey sphalerite 1 0,1185,30 187,87 2,57 1187,87 189,95 2,08 1189,95 200,34 10,39 2200,34 202,21 1,87 2202,21 203,00 0,79 1203,00 205,00 2,00 0,5205,00 214,00 9,00 1214,00 259,00 45,00 0,5259,00 260,00 1,00 0,5 0,1260,00 264,00 4,00 1264,00 299,95 35,95 0,5


HoleID Sample Id From (m) To (m) Length (m) Au Au chk Ag Co Cu Ni Pb ZnC08-12 37889 19,00 20,00 1,00 < 0.01 - < 0.2 0.006 0.003 0.150 < 0.001 0.003C08-12 37890 20,00 21,00 1,00 < 0.01 - < 0.2 0.006 0.004 0.115 < 0.001 0.003C08-12 37891 21,00 22,00 1,00 < 0.01 - 0.2 0.006 0.004 0.121 < 0.001 0.003C08-12 37892 22,00 23,00 1,00 0.01 0.02 0.2 0.006 0.004 0.122 < 0.001 0.003C08-12 37893 23,00 24,00 1,00 < 0.01 - 0.2 0.006 0.004 0.112 < 0.001 0.003C08-12 37894 24,00 25,00 1,00 0.01 - < 0.2 0.006 0.003 0.111 < 0.001 0.003C08-12 37895 25,00 26,00 1,00 0.01 - 0.2 0.005 0.003 0.117 < 0.001 0.003C08-12 37896 26,00 27,00 1,00 0.01 - < 0.2 0.005 0.006 0.112 < 0.001 0.003C08-12 37897 27,00 28,00 1,00 < 0.01 - < 0.2 0.005 0.007 0.111 < 0.001 0.004C08-12 37898 66,00 67,00 1,00 0.01 - 0.2 0.006 0.004 0.147 < 0.001 0.002C08-12 37899 67,00 68,00 1,00 0.01 - 0.2 0.005 0.013 0.118 < 0.001 0.003C08-12 37900 68,00 69,00 1,00 < 0.01 0.02 0.3 0.006 0.005 0.136 < 0.001 0.003C08-12 37901 69,00 70,00 1,00 0.01 - 0.2 0.006 0.003 0.128 < 0.001 0.003C08-12 37902 70,00 71,00 1,00 0.01 - 0.2 0.006 0.002 0.126 < 0.001 0.003C08-12 37903 71,00 72,00 1,00 0.01 - < 0.2 0.006 0.003 0.123 < 0.001 0.003C08-12 37904 85,00 86,00 1,00 0.01 - 0.2 0.006 0.002 0.128 < 0.001 0.002C08-12 37905 86,00 87,00 1,00 0.01 - < 0.2 0.006 0.004 0.134 < 0.001 0.002C08-12 37906 87,00 88,00 1,00 0.02 - < 0.2 0.006 0.003 0.146 < 0.001 0.002C08-12 37907 88,00 89,00 1,00 0.01 - 0.2 0.006 0.003 0.148 < 0.001 0.003C08-12 37908 122,00 123,00 1,00 0.01 - < 0.2 0.006 0.004 0.132 < 0.001 0.002C08-12 37909 123,00 124,00 1,00 0.02 0.04 0.2 0.006 0.003 0.141 < 0.001 0.002C08-12 37910 DIABASE 109.0-109.5 0.01 - 0.3 0.002 0.015 0.005 < 0.001 0.009C08-12 37911 124,00 125,00 1,00 0.02 - < 0.2 0.006 0.003 0.150 < 0.001 0.002C08-12 37912 125,00 126,00 1,00 0.02 - 0.2 0.006 0.004 0.140 < 0.001 0.003C08-12 37913 126,00 127,00 1,00 0.02 - < 0.2 0.006 0.007 0.119 < 0.001 0.003C08-12 37914 127,00 128,00 1,00 0.02 - 0.3 0.006 0.003 0.109 < 0.001 0.003C08-12 37915 128,00 129,00 1,00 0.02 - 0.2 0.006 0.003 0.138 < 0.001 0.002C08-12 37916 133,00 134,00 1,00 0.02 - < 0.2 0.007 0.005 0.123 < 0.001 0.003C08-12 37917 134,00 135,00 1,00 0.02 0.04 < 0.2 0.006 0.005 0.142 < 0.001 0.003C08-12 37918 135,00 136,00 1,00 0.02 - < 0.2 0.007 0.004 0.127 < 0.001 0.003C08-12 37919 136,00 137,00 1,00 0.02 - < 0.2 0.007 0.003 0.161 < 0.001 0.003C08-12 37920 137,00 138,00 1,00 0.02 - < 0.2 0.006 0.004 0.135 < 0.001 0.002C08-12 37921 138,00 139,00 1,00 0.03 - < 0.2 0.006 0.004 0.133 < 0.001 0.002C08-12 37922 139,00 140,00 1,00 0.02 - < 0.2 0.006 0.004 0.142 < 0.001 0.002C08-12 37923 140,00 141,00 1,00 0.02 - < 0.2 0.006 0.004 0.131 < 0.001 0.003C08-12 37924 141,00 142,00 1,00 0.04 - < 0.2 0.006 0.003 0.122 < 0.001 0.003C08-12 37925 142,00 143,00 1,00 0.02 - < 0.2 0.005 0.008 0.077 < 0.001 0.003C08-12 37926 OREAS 15Pa Batch 2 Can - 1.01 0.2 0.002 0.005 0.011 < 0.001 0.007C08-12 37927 143,00 144,00 1,00 < 0.01 - 0.2 0.005 0.004 0.086 < 0.001 0.004C08-12 37928 148,15 149,00 0,85 0.01 - < 0.2 0.006 0.007 0.113 < 0.001 0.004C08-12 37929 149,00 150,00 1,00 < 0.01 - < 0.2 0.006 0.005 0.127 < 0.001 0.004C08-12 37930 150,00 151,00 1,00 0.01 - < 0.2 0.006 0.003 0.139 < 0.001 0.003C08-12 37931 151,00 151,80 0,80 < 0.01 - < 0.2 0.007 0.004 0.125 < 0.001 0.004C08-12 37932 151,80 152,60 0,80 < 0.01 - < 0.2 0.006 0.002 0.132 < 0.001 0.003C08-12 37933 153,20 154,00 0,80 < 0.01 - < 0.2 0.006 0.004 0.127 < 0.001 0.003

C08-12 37934 154,00 155,00 1,00 < 0.01 - < 0.2 0.006 0.004 0.105 < 0.001 0.003C08-12 37935 155,00 156,00 1,00 0.01 < 0.01 < 0.2 0.005 0.006 0.098 < 0.001 0.003C08-12 37936 156,00 157,00 1,00 0.01 - < 0.2 0.005 0.005 0.086 < 0.001 0.003C08-12 37937 166,10 167,10 1,00 0.01 - < 0.2 0.005 0.005 0.092 < 0.001 0.004

Au Au chk Au chk Ag Co Cu Ni Pb Zng/Mt g/Mt g/Mt ppm % % % % %

C08-12 37938 167,10 168,20 1,10 < 0.01 - - < 0.2 0.006 0.003 0.092 < 0.001 0.004C08-12 37939 168,20 169,20 1,00 0.01 < 0.01 - 0.2 0.006 0.002 0.103 < 0.001 0.003C08-12 37940 169,20 170,20 1,00 < 0.01 - - < 0.2 0.006 0.004 0.099 < 0.001 0.004C08-12 37941 170,20 171,20 1,00 < 0.01 - - 0.2 0.005 0.005 0.079 < 0.001 0.006C08-12 37942 171,20 172,00 0,80 < 0.01 - - 0.2 0.005 0.005 0.075 < 0.001 0.004C08-12 37943 172,00 173,00 1,00 < 0.01 - - < 0.2 0.006 0.004 0.085 < 0.001 0.005C08-12 37944 173,00 174,00 1,00 < 0.01 - - 0.2 0.005 0.003 0.074 < 0.001 0.004C08-12 37945 174,00 174,94 0,94 < 0.01 - - < 0.2 0.004 0.003 0.071 < 0.001 0.003C08-12 37946 174,94 175,65 0,71 < 0.01 - - < 0.2 0.001 0.002 0.005 0.001 0.005C08-12 37947 176,10 176,75 0,65 < 0.01 - - 0.2 0.003 0.006 0.046 < 0.001 0.004C08-12 37948 176,75 177,42 0,67 - < 0.01 - < 0.2 0.004 0.007 0.065 < 0.001 0.007C08-12 37949 177,42 178,40 0,98 0.20 0.35 - 0.2 0.002 0.002 0.005 < 0.001 0.004C08-12 37950 178,40 179,28 0,88 0.03 0.02 - 0.2 0.002 0.004 0.013 < 0.001 0.006C08-12 37951 179,28 180,20 0,92 < 0.01 - - < 0.2 0.003 0.007 0.054 < 0.001 0.003C08-12 37952 180,20 181,22 1,02 < 0.01 - - < 0.2 0.004 0.005 0.061 < 0.001 0.002C08-12 37953 181,22 182,00 0,78 0.11 - - < 0.2 < 0.001 0.003 0.001 < 0.001 0.002C08-12 37954 DIABASE 109.5-110.0 < 0.01 - - < 0.2 0.002 0.013 0.003 < 0.001 0.008C08-12 37955 182,00 182,70 0,70 0.04 - - < 0.2 0.002 0.003 0.028 < 0.001 0.004C08-12 37956 182,70 183,60 0,90 < 0.01 - - < 0.2 0.005 0.006 0.062 < 0.001 0.002C08-12 37957 183,60 184,50 0,90 < 0.01 - - < 0.2 0.005 0.004 0.079 < 0.001 0.002C08-12 37958 184,50 185,30 0,80 < 0.01 - - < 0.2 0.005 0.005 0.061 < 0.001 0.003C08-12 37959 185,30 186,10 0,80 - < 0.01 < 0.01 < 0.2 0.004 0.003 0.082 < 0.001 0.002C08-12 37960 186,10 187,00 0,90 0.02 - - < 0.2 0.004 0.002 0.095 < 0.001 0.003C08-12 37961 187,00 187,87 0,87 < 0.01 - - < 0.2 0.005 0.001 0.110 < 0.001 0.003C08-12 37962 187,87 188,90 1,03 < 0.01 - - < 0.2 0.004 0.004 0.079 < 0.001 0.003C08-12 37963 188,90 189,95 1,05 < 0.01 - - < 0.2 0.005 0.004 0.084 < 0.001 0.003C08-12 37964 189,95 191,00 1,05 < 0.01 - - < 0.2 0.005 0.005 0.088 < 0.001 0.003C08-12 37965 191,00 192,00 1,00 < 0.01 - - < 0.2 0.006 0.005 0.100 < 0.001 0.006C08-12 37966 192,00 193,00 1,00 < 0.01 - - < 0.2 0.005 0.007 0.086 < 0.001 0.004C08-12 37967 OREAS 6Pc Batch 1 Can 0.98 - - < 0.2 < 0.001 0.003 0.003 0.002 0.005C08-12 37968 193,00 194,00 1,00 < 0.01 - - < 0.2 0.006 0.005 0.104 < 0.001 0.004C08-12 37969 194,00 195,00 1,00 < 0.01 - - < 0.2 0.006 0.005 0.081 < 0.001 0.007C08-12 37970 195,00 196,00 1,00 - < 0.01 < 0.01 < 0.2 0.005 0.005 0.094 < 0.001 0.004C08-12 37971 196,00 197,00 1,00 < 0.01 - - < 0.2 0.005 0.007 0.086 < 0.001 0.004C08-12 37972 197,00 198,00 1,00 < 0.01 - - < 0.2 0.006 0.007 0.079 < 0.001 0.004C08-12 37973 198,00 199,00 1,00 < 0.01 - - < 0.2 0.005 0.006 0.086 < 0.001 0.004C08-12 37974 199,00 199,72 0,72 < 0.01 - - < 0.2 0.004 0.002 0.007 < 0.001 0.012C08-12 37975 199,72 200,34 0,62 < 0.01 - - < 0.2 0.005 0.002 0.106 < 0.001 0.004C08-12 37976 200,34 201,30 0,96 0.02 - - < 0.2 0.005 0.006 0.069 0.001 0.003C08-12 37977 201,30 202,21 0,91 < 0.01 - - < 0.2 0.004 0.005 0.084 < 0.001 0.002

C08-12 37978 202,21 203,00 0,79 < 0.01 0.03 - < 0.2 0.005 0.004 0.078 < 0.001 0.003C08-12 37979 203,00 204,00 1,00 < 0.01 - - < 0.2 0.005 0.004 0.092 < 0.001 0.003C08-12 37980 204,00 205,00 1,00 < 0.01 - - < 0.2 0.005 0.004 0.098 < 0.001 0.003C08-12 37981 205,00 206,00 1,00 < 0.01 - - < 0.2 0.005 0.004 0.093 < 0.001 0.004C08-12 37982 206,00 207,00 1,00 - 0.02 - < 0.2 0.005 0.006 0.108 < 0.001 0.004C08-12 37983 207,00 208,00 1,00 < 0.01 - - < 0.2 0.005 0.004 0.104 < 0.001 0.004C08-12 37984 DIABASE 109.5-110.0 < 0.01 - - < 0.2 0.002 0.013 0.003 < 0.001 0.008C08-12 37985 208,00 209,00 1,00 < 0.01 - - < 0.2 0.006 0.004 0.106 < 0.001 0.004C08-12 37986 209,00 210,00 1,00 < 0.01 < 0.01 - < 0.2 0.005 0.004 0.103 < 0.001 0.004C08-12 37987 210,00 211,00 1,00 < 0.01 - - < 0.2 0.006 0.005 0.105 < 0.001 0.004C08-12 37988 211,00 212,00 1,00 < 0.01 - - < 0.2 0.006 0.004 0.113 < 0.001 0.004C08-12 37989 212,00 213,00 1,00 < 0.01 - - < 0.2 0.005 0.006 0.091 < 0.001 0.004C08-12 37990 213,00 214,00 1,00 - 0.02 0.02 < 0.2 0.005 0.007 0.103 < 0.001 0.004C08-12 37991 214,00 215,00 1,00 < 0.01 - - < 0.2 0.005 0.003 0.073 < 0.001 0.004C08-12 37992 247,20 248,11 0,91 < 0.01 - - < 0.2 0.006 0.003 0.136 < 0.001 0.003C08-12 37993 248,11 249,15 1,04 < 0.01 - - < 0.2 0.005 0.007 0.091 < 0.001 0.004C08-12 37994 249,15 250,15 1,00 < 0.01 - - < 0.2 0.004 0.004 0.068 < 0.001 0.002C08-12 37995 250,15 251,00 0,85 < 0.01 - - < 0.2 0.005 0.005 0.144 < 0.001 0.002C08-12 37996 259,00 260,00 1,00 < 0.01 - - < 0.2 0.006 0.010 0.077 < 0.001 0.004C08-12 37997 260,00 261,00 1,00 < 0.01 < 0.01 - < 0.2 0.006 0.003 0.133 < 0.001 0.002C08-12 37998 261,00 262,00 1,00 < 0.01 - - < 0.2 0.006 0.003 0.136 < 0.001 0.002C08-12 37999 262,00 263,00 1,00 0.01 - - < 0.2 0.007 0.003 0.150 < 0.001 0.003C08-12 38000 263,00 264,00 1,00 0.02 - - < 0.2 0.006 0.002 0.137 < 0.001 0.003


0 13,55 OB13,55 14 0,45 100,00 0,25 44,44 13,55 16,37

14 17 3,00 100,00 2,07 31,00 17,86 21,7617 20 3,00 100,00 1,65 45,00 22,63 25,620 23 3,00 100,00 1,13 62,33 26,62 27,323 26 3,00 100,00 1,82 39,33 28,51 29,6526 29 3,00 100,00 1,53 49,00 30,84 31,5829 32 3,00 100,00 1,12 62,67 32,48 39,432 35 3,00 100,00 1,55 48,3335 38 3,00 100,00 1,27 57,6738 41 3,00 100,00 1,55 48,33 40,26 41,941 44 3,10 103,33 0,62 80,00 46,95 47,1844 47 2,90 96,67 0,30 89,66 49,83 51,4247 50 3,00 100,00 0,46 84,67 53,08 5950 53 3,08 102,67 0,98 68,18 64,12 64,4853 56 3,00 100,00 1,34 55,33 67,7 69,3356 59 3,00 100,00 1,30 56,67 70 70,5359 62 3,08 102,67 0,34 88,96 73,27 74,1862 65 3,01 100,33 0,41 86,38 76,5 77,3865 68 3,01 100,33 0,45 85,05 78,25 78,6268 71 2,88 96,00 1,23 57,29 79,45 81,7871 74 3,12 104,00 0,77 75,32 83,27 84,9474 77 2,97 99,00 0,75 74,75 85,44 86,1577 80 3,00 100,00 1,60 46,67 87,27 87,9780 83 3,00 100,00 1,48 50,67 88,57 88,8383 86 3,00 100,00 2,07 31,00 90 9186 89 3,00 100,00 1,64 45,33 91,9 92,3289 92 2,60 86,67 1,12 56,92 Lost core 93,56 94,1592 95 3,00 100,00 0,90 70,00 96 96,3695 98 3,00 100,00 1,05 65,00 97,33 97,9398 101 3,00 100,00 0,96 68,00 99,95 102,24101 104 3,00 100,00 1,51 49,67 103,64 104,53104 107 2,93 97,67 1,40 52,22 105,22 105,78107 110 2,55 85,00 1,05 58,82 Lost core 106,22 106,62110 113 3,07 102,33 0,85 72,31 107,08 107,27113 116 3,00 100,00 0,86 71,33 108,07 108,7116 119 3,05 101,67 0,55 81,97 110,94 111,27119 122 3,00 100,00 0,80 73,33 113,75 114,34122 125 2,95 98,33 0,25 91,53 119,69 120,05125 128 2,99 99,67 0,27 90,97 125,22 125,44

Fault gougeDDH Depth Recovery RQDGeotechnical Log

Blocky core Crumbly core

128 131 3,01 100,33 0,36 88,04131 134 3,04 101,33 0,17 94,41 135,46 135,92134 137 3,01 100,33 0,59 80,40 138,98 139,47137 140 3,00 100,00 0,49 83,67 141,04 141,48140 143 2,95 98,33 0,70 76,27 142,46 142,75143 146 2,95 98,33 0,00 100,00 147,72 148,05146 149 3,00 100,00 0,58 80,67 148,55 148,9149 152 3,00 100,00 0,65 78,33 151,14 151,46152 155 2,40 80,00 0,96 60,00 Lost core 151,86 152,6155 158 3,00 100,00 2,02 32,67 154,77 156158 161 3,00 100,00 1,69 43,67 156,31 161,14161 164 3,00 100,00 0,82 72,67 163,63 167,1164 167 3,00 100,00 1,80 40,00167 170 3,00 100,00 1,06 64,67 172,05 172,84170 173 3,00 100,00 0,98 67,33 175,34 175,65173 176 2,55 85,00 0,52 79,61 Lost core 176,6 177,42176 179 3,00 100,00 0,88 70,67 178,68 181,21179 182 3,00 100,00 1,52 49,33 181,69 182,24 179,45 179,52 At appr 45 deg182 185 3,00 100,00 1,74 42,00 182,7 185,3185 188 3,00 100,00 1,07 64,33 186,03 186,73 187,87 187,9 At 65 deg tca188 191 3,00 100,00 1,13 62,33 188,49 189,23 188,49 188,72 At 55 deg tca191 194 3,00 100,00 1,24 58,67 189,65 189,95194 197 3,00 100,00 1,66 44,67 192,18 195,54197 200 2,97 99,00 0,69 76,77 196,1 196,92200 203 3,02 100,67 0,75 75,17 199 200,5203 206 2,99 99,67 0,38 87,29 205,86 206,62206 209 2,97 99,00 0,52 82,49 208,09 208,32209 212 2,91 97,00 0,68 76,63 209,7 210,54 210,3 210,32 At 40 deg tca212 215 3,04 101,33 0,46 84,87 212,2 212,56215 218 3,03 101,00 0,17 94,39 213,58 213,99218 221 3,02 100,67 0,65 78,48 219,57 220,5221 224 2,99 99,67 0,49 83,61224 227 3,00 100,00 0,24 92,00227 230 3,06 102,00 0,32 89,54 229,68 229,95230 233 3,01 100,33 0,79 73,75 230,32 230,56233 236 2,99 99,67 0,82 72,58236 239 2,96 98,67 0,85 71,28 237,29 237,82239 242 2,97 99,00 0,83 72,05 241,87 242,45242 245 3,00 100,00 1,52 49,33 242,86 243,3245 248 2,92 97,33 0,85 70,89 243,91 244,8248 251 2,97 99,00 0,48 83,84 247 247,45251 254 2,98 99,33 0,75 74,83 248,72 249,3254 257 2,99 99,67 1,08 63,88 252,79 253,24

257 260 3,00 100,00 1,02 66,00 255,53 256,34260 263 3,00 100,00 0,90 70,00 257,78 258,61263 266 3,00 100,00 2,07 31,00 262,37 266,16266 269 3,00 100,00 1,52 49,33 267,51 271,89269 272 3,00 100,00 2,02 32,67272 275 3,06 102,00 0,47 84,64275 278 3,00 100,00 0,46 84,67278 281 3,05 101,67 0,07 97,70 282,54 283281 284 3,00 100,00 1,02 66,00 283,52 284284 287 3,00 100,00 1,23 59,00 284,4 285,38287 290 3,00 100,00 1,82 39,33 286,3 291,27290 293 3,00 100,00 1,62 46,00 292,15 293,32293 296 3,00 100,00 1,34 55,33 294,55 295,52296 299 3,00 100,00 1,11 63,00 296,45 296,55299 300 0,95 95,00 0,44 53,68 299,38 299,81


C-08-13 L-3300E 1100N 300 0 -50 301m 24/09/08 03/10/08 G.Spyratos March 15 - March 18, 2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 18,00 18,00 Overburden casing

18,00 78,10 60,10

black to dark green, hom, fg, loc coarser grain serpentinized chlorite ultramafic, loc qz-cal v, 2 to 60 cm w av CA 40 see geol 2 40-115 SI var

78,10 82,40 4,30 hom fg dark grey basic ? dyke or massive fg metabasites 45 SI

82,40 84,30 1,90idem ultramafic unit w loc cm spinifex zone w mm wide by cm long black amphibole in serp-chlo matrix 2 80-95 SI var

84,30 95,00 10,70

hom fg dark grey massive basic ? Dyke ?, loc highly fract w chlo coating, loc mm-cm chlo conc w cm breccia w mm-1 cm dyke elements in chlo matrix, w car angle 40-60 to CA 68-150 var SI loc 229

95,00 113,5 18,5

hom fg dark grey basic ? dyke, loc highly fract w mm chlo coating, loc mm-cm chlo-serp conc w cm breccia w mm-1 cm dyke elements in chlo matrix 50-124 SI var

113,50 139,7 26,2massive basic ? dyke, idem prev unit, highly fract w var angle 60-80 to CA, w 1-2 cm chlo conc, 25 to CA 35-120 SI var

139,70 140,6 0,9ultramafic same as precedent unit, w prob destroyed spinifex text

140,60 144 3,4

hom massive mafic dyke ? or massive fg metabasites, same as prec unit w cm chlo-serp zones loc ± // to CA & w 5-10 cm zone of ultramafic unit

144,00 144,3 0,3 ultramafic same as precedent unit144,30 145,7 1,4 mafic dyke, same as prec unit

145,70 146,8 1,1ultramafic same as precedent unit, w prob ± preserved spinifex text

146,80 149,9 3,1 mafic dyke, same as prec unit

149,90 152,7 2,8ultramafic unit same as prev w 20 cm hom fg mafic dyke @ 150.55

152,70 153,9 1,2 metabasite, same as prec unit153,90 158,15 4,25 ultramafic unit same as prev158,15 162,9 4,75 metabasite, same as prec unit162,90 166,6 3,7 ultramafic unit same as prev, slightly mag spinifex text remnants are weakly mag166,60 167,2 0,6 metabasite, same as prec unit loc wekly mag less than spinifexed ultramafics167,20 168,3 1,1 ultramafic unit same as prev

168,30 226,2 57,9

komatiitic metabasite, same as prec unit, w loc chlo-serp fract 40 to CA & weak brecciation w mm qz-cal veining, loc the unit shows fg talcose text, fg chlo S1 is developed @ 226.5m over 30 cm

226,2 237,5 11,3 same as prev unit w less chlo fract & 1% qz-cal veining

226,20 240,15 13,95fg hom leuco-meso int dyke w 2% mm white w contacts at 40 to CA

DDH Depth

240,15 247 6,85

komatiitic metabasite, same as prec unit, w loc chlo-serp fract 40 to CA & weak brecciation w mm qz-cal veining, loc the unit shows fg talcose text mag suscep gets lower near contact 1.2

247,00 259 12

fg-mg ± hom diabase dyke w low mag suscept .5-.8, 30 w low angle upper contact 10-15 to CA & cm fg chill margin at lower contact & prob assimilation of metabasic material in the last 2 m

259,00 263,5 4,5komatiitic metabasite, same as prec unit w weak brecciation w mm qz-cal veining low suscep at upper & lower contacts

263,50 270,2 6,7

fg-mg ± hom diabase dyke w low mag suscept .5-.8, 30 cm fg chill margin at lower contact, prob assimilation of komatiitic metabasite in the diabase for one meter at upper contact

270,20 272,6 2,4komatiitic metabasite, same as prec unit w weak brecciation w mm qz-cal veining

272,60 297,8 25,2

fg-mg ± hom diabase dyke w low mag suscept .5-.8, w chill margin at upper contact w intruding 2e phase diabse dyke at 276.4 & 277.3, w local decim size contaminated zone w kom metabasite

297,80 301 3,2komatiitic metabasite, same as prec unit w weak brecciation w mm qz-cal veining

301,00 EOH

MPP From To Length Id Rock types, Change in grain size, colour, etc.CA Photo Comment From To L Comments23,00 23,60 0,60 2 & 10 cm qz-cal v + qz-cal mm sw 4041,95 3 cm qz-cal fg SZ 85 27,50 34,00 6,50 C08-13A.txt

41 41,2 0,20brecciation w fine mm qz-cal veining 5% w cm elements

44,00 44,30 0,30brecciation w 1 cm elements in apanitic pale grey-blueish hard matrix (not qz or 2

60,10 62,90 2,80fg hom med gray mafic probable dyke, sharp contacts not visible,

mag susceptibility in the 150 SI

88,25 4 cm wide qz-cal-chlo vein 30

97,505 cm breccia w mm- 1 cm dyke rounded elements in chlo matrix

150,55 20 cm hom fg mafic dyke

158,50 158,75ultramafic unit, slightly mag w preserved spinifex text

162,50 162,75 ultramafic unit164,50 164,75 fg hom mafic dyke165,25 165,55 fg hom mafic dyke

204,00 204,30

1 cm chlo-talc SZ 60 to CA w 20 cm breccia w mm-1cm mafic elements in chlo-serp mx 60

211,30 212,00int leuco dyke w mm chlo fract, contact 20 to CA 20

229,20 1 cm qz-cal SZ 25237,3 4 cm qz-chlo-cal fg SZ 30242,60 1 cm qz-cal SZ 15

275,5 276,4fg diabase dyke w chill margin at upper contact

281,75 282,3 prob contamination nby kom metabsite

DDH Depth Lithology of Sub-units

Sample Id From To Length Comments Id Au Ag38271 31,50 33,00 1,5038272 52,60 54,00 1,4038273 71,70 73,00 1,30

Assays

DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge CommentsBox no. From To Length % Length % Comments % From To From To1 18 23 5 3,5 70% 0,6 12% 602 23 26 3 2,5 83% 0,70 23% 403 26 30,2 4,2 4,2 100% 1,60 38% 54 30,2 34,5 4,3 4,3 100% 2,20 51% 75 34,5 38,6 4,1 3,8 93% 0,40 10% 106 38,6 42,8 4,2 4 95% 1,20 29% 57 42,8 46,2 3,4 3,1 91% 0,45 13% 358 46,2 50,3 4,1 2,7 66% 0,60 15% 359 50,3 54 3,7 3,55 96% 2,00 54% 310 54 57,65 3,65 3,45 95% 0,35 10% 411 57,65 61,6 3,95 3,95 100% 1,50 38% -12 61,6 65,3 3,7 3,65 99% 1,30 35% 313 65,3 69,2 3,9 3,9 100% 0,90 23% 514 69,2 73 3,8 3,6 95% 0,80 21% 715 73 76,4 3,4 3,5 103% 1,80 53% 1216 76,4 80,25 3,85 3,45 90% 0,90 23% 317 80,25 84,3 4,05 4 99% 1,60 40% 218 84,3 88,65 4,35 4,35 100% 2,50 57% 219 88,65 92,6 3,95 3,8 96% 0,80 20% 7020 92,6 94,8 2,2 2,00 91% 0,35 16% 9521 94,8 98,4 3,6 3,40 94% 0,60 17% 5022 98,4 101,2 2,8 2,00 71% 0,60 21% 7023 101,2 106,1 4,9 3,50 71% 0,50 10% 5024 106,1 110,1 4 3,20 80% 0,70 18% 4025 110,1 113,5 3,4 3,20 94% 1,00 29% 3026 113,5 116,9 3,4 3,20 94% 0,45 13% 2027 116,9 121,3 4,4 2,40 55% 0,40 9% 2528 121,3 123,85 2,55 2 78% 0,15 6% 9029 123,85 127,9 4,05 1,80 44% 0,50 12% 6030 127,9 130,4 2,5 2,20 88% 0,00 0% 5031 130,4 133,7 3,3 3,00 91% 0,60 18% 3032 133,7 137,1 3,4 2,80 82% 0,45 13% 3533 137,1 140,15 3,05 3,00 98% 0,35 11% 3034 140,15 143,2 3,05 2,40 79% 0,00 0% 6035 143,2 147,1 3,9 3,50 90% 0,90 23% 2036 147,1 150,85 3,75 3,70 99% 2,40 64% 537 150,85 154,95 4,1 4,00 98% 1,10 27% 338 154,95 158,9 3,95 3,80 96% 2,70 68% 1039 158,9 162,8 3,9 3,80 97% 2,20 56% 540 162,8 166,8 4 3,90 98% 1,50 38% 541 166,8 170,3 3,5 3,30 94% 1,25 36% 2042 170,3 173,8 3,5 2,70 77% 0,70 20% 6043 173,8 177,8 4 2,80 70% 0,00 0% 9044 177,8 181,7 3,9 2,90 74% 0,70 18% 6545 181,7 185 3,3 2,90 88% 1,20 36% 4046 185 189,1 4,1 4,10 100% 2,30 56% 1

47 189,1 192,7 3,6 3,50 97% 2,40 67% 148 192,7 196,9 4,2 4,20 100% 1,90 45% 249 196,9 200,4 3,5 3,40 97% 1,50 43% 450 200,4 203,9 3,5 3,20 91% 1,00 29% 1051 203,9 207,5 3,6 3,50 97% 1,50 42% 1052 207,5 210,9 3,4 3,20 94% 0,70 21% 3053 210,9 214,2 3,3 3,10 94% 1,35 41% 2054 214,2 218,1 3,9 3,90 100% 1,50 38% 555 218,1 222,1 4 4,00 100% 1,40 35% 756 222,1 226,2 4,1 4,10 100% 2,30 56% 057 226,2 230,4 4,2 4,20 100% 3,45 82% 058 230,4 234,6 4,2 4,20 100% 3,25 77% 059 234,6 238,95 4,35 4,35 100% 3,70 85% 060 238,95 243,15 4,2 4,20 100% 3,80 90% 061 243,15 247,5 4,35 4,35 100% 3,25 75%62 247,5 251,6 4,1 4,10 100% 3,10 76%63 251,6 255,2 3,6 3,60 100% 2,50 69%64 255,2 259,8 4,6 4,60 100% 3,30 72%65 259,8 263,9 4,1 4,10 100% 3,60 88%66 263,9 268,3 4,4 4,40 100% 3,60 82%67 268,3 272,55 4,25 4,25 100% 2,90 68%68 272,55 276,7 4,15 4,15 100% 3,25 78%69 276,7 281,1 4,4 4,40 100% 3,20 73%70 281,1 285,55 4,45 4,45 100% 3,15 71%71 285,55 289,75 4,2 4,20 100% 3,75 89%72 289,75 294,1 4,35 4,35 100% 3,35 77%73 294,1 298,25 4,15 4,15 100% 3,05 73%74 298,25 301 2,75 2,75 100% 2,55 93%EOH


C-08-14 L-3300E 425N 300 0 -50 300m 04-oct-08 12-oct-08 G.Spyratos March 15 - March 18, 2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 25,00 25,00 Overburden casing25,00 39,50 14,50 mg hom med grey-green andesite

39,50 55,20 15,70

hom & massive, fg, med grey-green andesite, w cm breccia zones, possible meta pillow meta chill margins w pale green aph to fg matrix w mm andesite elements

55,20 58,70 3,50mg ± hom med green and w 2% mm cal-qz veining w var angle to CA & loc cm fol 30 to CA

58,70 60,20 1,50andesite same as prev unit w well def fol & 5% cal-qz mm veining 30 to CA

60,20 62,6 2,40 mg hom purplish diabase dyke, w upper contact 30 to CA

62,60 68,2 5,60SZ in and w 5% massive pegmatite & 30% qz-fpK sw 30 to CA, w mm-cm folds & mm chlo S2 stringer 40 to CA

68,20 69,4 1,20 brecciated fol chlo andesite w loc fol // to CA

69,40 70,2 0,80 hom fg salmon colour felsic intrusive70,20 73,2 3,00 chlo sz in andesite 2% loc 1 cm qz-cal veining

73,20 77 3,80 hom fg med green massive andesite w 5% mm qz-cal veining & sw82,40 Struct

77,00 90,6 13,60

hetero fg med green massive andesite same as previous without sw, contains cm & decim zone of differential alt from med green to pale green related to syn-genetic internal decim structure in the andesite flows, w local cm to decim syngenetic brecciation zones, see Geol 2 & photos

90,60 95 4,40 same without syngenetic brecciation95,00 97,5 2,50 hom mg med green and

97,50 99,3 1,80vfg pale green to purplish groid w chlo contamination, well developed fol 15 to CA

99,30 107,3 8,00hom massive mg to cg andesite, mg for the first 1.5 m and coarse gr for the rest of unit

107,30 114,4 7,10 fg hom massive pink groid, syenite w 1% diss py

114,40 137,15 22,75

hetero fg med green massive andesite same as previous w local cm zones of differential alt from med green to pale green related to syn-genetic internal decim structure in the andesite flows mostly pillow & loc cm chill margins, w local cm mg leuco gabbroic text zones & some cm pink pegmatite renmamt in chill margins or volc internal structures very low mag susceptibility

137,15 143,25 6,10 mg ± hom andesite w continuous zone of fg text from 141.5m143,25 145,8 2,55 hom fg syenite145,80 146,7 0,90 hom fg-mg and146,70 147,4 0,70 fol syenite 40 to CA w 5% qz-cal mm sw147,40 147,5 0,10 chlo pegm sheard vein 40 to CA

DDH Depth

147,50 147,65 0,15 qz-cal mm sw 60 to CA147,65 149,5 1,85 ± hom fg epi andesite w local fol // CA

149,50 158,6 9,10pink-brown-grey fg hom syenite w assimilation of grey monzonite from 155, w diss & loc conc 2% py & cpy & mm vein of specularite ?

158,60 159,7 1,10 alt fg hom grey monzonite159,70 164 4,30 fg hom pink-grey syenite 35 to CA at upper contact164,00 164,5 0,50 fg grey hom monzonite164,50 172,4 7,90 same unit, hom mg grey mznt172,40 172,6 0,20 synite w 10% qz-cal mm sw in SZ 30 to CA172,60 175,4 2,80 alt fg andesite w 10% qz-cal mm sw, w loc fol 60 to CA

175,40 185 9,60idem less alt or def, fg hom med green and w 3% mm-1 cm qz-cal veining & sw, also w 2 510 cm wide qz-cal SZ 40 to CA

185,00 195,85 10,85idem, and without veining, fg hom med green andesite without syun-genetic sytructures or chill margins

195,85 197,55 1,70mg hom med gray-green meta intermediate volc of undetermined origin

197,55 209,1 11,55idem, and without veining, fg hom med green andesite with limited syn-genetic sytructures

209,10 210,1 1,00 chlo-cal-rich fol andesite, 40 to CA210,10 212,5 2,40 mg hom chlo-cal purplish-green granodiorite

212,50 220,2 7,70± hom chlo-cal fg andesite w local internal structure marked by var in alt colour from med to pale green, w 1% qz-cal mm veining 35 to CA

220,20 222,25 2,05 hom mg qz-ser-chlo monzonite, loc fol222,25 224,3 2,05 idem finer gr more var fol

224,30 224,75 0,45clo schist, prob sheard and w 60 % qz-fp-cal vein 40 to CA in the first half of unit

224,75 225,4 0,65transition zone between schistosed chlo and & the purple-brown monzonitic unit that follow

225,40 225,9 0,50 purple brown hom fom mg monzonite w prob ser-chlo-hem alt225,90 226,65 0,75 fg hm chlo andesite

226,65 230,6 3,95mg to loc fg hom chlo-ser purplish-grey monzonite dyke, w 20 cm vfg portion of unit (chill margin) @ 227.2-227.45

230,60 233,55 2,95fg to mg ± hom chlo alt and, w loc mm shear 50 to CA & mm qz-cal veining rel to var fol

233,55 235,05 1,50 idem 226.65 w finer gr in the first 40 cm & more developed hem alt

235,05 243,2 8,15± hom chlo fg andesite w local internal structure marked by mm chlo conc & clo-qz-cal mm-cm coonc in chill margins (see 2 PHOTOS) 2

243,20 245,3 2,10 fg-mg porph syenite w 10% white-pinkish mm phX245,30 262,2 16,90 fg to mg ± hom and w local mm qz-cal v & clusters

262,20 263,45 1,25idem and w 60% cal-qz mmm matrix carrying mm to cm and elements

263,45 268,6 5,15 fg to mg ± hom and w local mm qz-cal v & clusters268,60 270,3 1,70 hom mg ± massive dark pink chlo syenite270,30 274,6 4,30 fg hom andesite

274,60 276,5 1,9 hom fol mg dark pink syenite w weak fol // CA276,50 278,3 1,8 mg chlo meta andesite w last 30 cm showing vfg text278,30 283,7 5,4 fg hom pinlk syenite w 1% diss py oin the first 60 cm283,70 287 3,3 fg hom porph syenite w 5% mm pinkish phX287,00 289,45 2,45 fg hom pinlk syenite w 1% diss py

289,45 291,5 2,05chlo meta and w well developed schjistosity w 5% qz-cal mm-2 cm veining 10 to CA, lower contact in SZ 10 to CA

291,50 299,2 7,7 fg ± hom chlo syenite, locally sheared from upper contact to 292.45

299,20 300 0,8sheared chlo schist w 15% qz-cal mm veining 15 to CA // to upper & lower contacts w chloi syenite // to CA

EOH

MPP From To Length Id Rock types, Change in grain size, colour, etc. CA Photo Comment From To L Comments

27,70 30,20 2,50brecciated zone w 10% cm andesite elements in fresh clay matrix

33,4 35,15 1,75 mg hom ^purplish diabase

45,65 cm brecciated zone w mm and elements in pale green aph to fg matrix 85 2

46 46,30 0,30 5% 1-2 cm qz-chlo clusters

79,4 80,40 1,00

intraformational brecciation w mm to cm alt andesite elements in minor vfg chlo matrix, possibly related to flow top breccia or hyaloclastic phenomenon 3

87,7 90,60 2,90 idem hyaloclastic breccia w mm & cm intraclasts 40 297,60 97,95 0,35 1 cm wide pegmatite vein 15 to CA 15119,30 119,65 0,35 vfg to fg silicification zone 50121,60 121,70 0,10 qz vein massive 60 to CA 60124,30 124,50 0,20 syenite vein136,35 136,60 0,25 mg hom and dyke 85

139,9 141,4 1,5epidotized alt & brecciated zone w 95% cm fg alt epidotised andesite elements in hem ? chlo matrix 80

141,90 142,30 0,40 alt qz-cal SZ w cm syenite section 20143,25 143,30 0,05 2 cm qz vein & ser SZ 35

152,85 153,10 0,25apahanitic pink paler zone, prob fpK w 2% diss mm py, 40 to CA at upper contact 40

160,15 160,35 0,20 alt grey monzonite unit, 30 to CA at upper contact 30163,7 164 0,3 fol pink fg syenite unit w mm qz-cal vein at lower contact 40 to CA 40157,20 167,40 10,20 50% qz-cal vein in chlo SZ 20

199,3 199,6 0,3hom mg meta int volc possibly idem 195.85 unit limited by mm qz-cal vein at both contacts 50

203,1 203,4 0,3 chlo SZ w 15% mm qz-cal veins 40208,95 4 cm qz-cal vein 60

201,8isolated 4 cm irregular qz-cal; cluster rel to loc mm qz-cal veining ± to CA

208,8 3 cm qz-fpk sheared v 50

215,3 215,7 0,4vfg to fg red brown chlo-cal syenite ?? W qz-cal; mm- 2 cm cluster in loc cm chlo shear 40

219,6 220,1 0,5 same as 215.3 w less mm chlorite 50219,15 qz-cal 3 cm vein 50220,05 5 cm of qz-cal mmm sw 50227,2 227,45 0,25 vfg chill margin monzonite see Geol1227,45 227,5 0,05 cqz-chlo SZ 35229,1 229,5 0,4 fg ± hom ser-hem alt red-brown syenite dyke 60236,5 10 cm qz-cal-chlo v 50251,3 251,7 fg hom red-brown syenite ? Dyke255 255,1 idem finer gr

DDH Depth Lithology of Sub-units

257 257,4 pale gray-green fg dyke of int comp ? 45258,6 258,85 fg hom red-brown syenite ? Dyke 45259,5 259,65 50% mm qz-cal v in chlo SZ 45264,3 264,7 fg hom syenite dyke 45265,2 265,85 40 % qz-cal matrix w mm to cm andesite hom elements267 267,25 10 cm chill margin w 40% aph chlo & 60% mm ser plag xtals 2 photos268,2 268,4 10% cal-qz matrix in hom fg-mg andesite brecciated zone288,7 289,35 15% qz-cal mm veining & cm clusters 15

DDH Depth Structure (Intensity 1-5) Veining (%)From To Length Id comments BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL CA ANK CA STW Photo

82,40 83,00 0,6030% mm-2 cm qz-cal ceining & sw in chlo schistosed andesite

From To Length Id Description CA Py Po Cpy Sph Gal Mag44,20 44,30 0,10 aph to fg qz-py fol dyke 90 2107,30 111,85 4,55 fg hom syenite w 1% diss py 1149,50 158,6 9,10 syenite w diss py & cm conc cpy 1 1287,00 288,70 1,70 syenite w diss py & cm conc cpy 1


Sample ID From To Length Comments Id Au Ag38274 64,30 65,10 0,80 70% cm qz vein & oegm in chlo SZ38275 65,10 66,60 1,50 40% mm qz-fpK sw in chlo SZ38276 151,30 152,60 1,30 synt w diss py38277 152,60 154,00 1,40 synt w diss py & cpy38278 153,90 155,30 1,40 synt w diss py38279 155,30 156,90 1,60 synt w diss py38280 156,90 158,30 1,40 synt w diss py38281 161,00 162,45 1,45 synt w diss py38282 287,00 288,70 1,70 synt w diss py38283 288,70 289,35 0,65 idem w 15% qz-cal veining & clusters

Assays

DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge CommentsBox no. From To Length % Length % Comments % % From To1 25 31 6 2 33% 2 33% 402 31 35,15 4,15 4,15 100% 3,25 78% 03 35,15 39,5 4,35 4,35 100% 3,95 91% 14 39,5 43,6 4,1 4,1 100% 3,60 88% 25 43,6 47,8 4,2 4,2 100% 4,05 96% 06 47,8 52,3 4,5 4,4 98% 4,25 94% 07 52,3 56,5 4,2 4,2 100% 3,40 81% 08 56,5 60,85 4,35 4,35 100% 3,90 90% 09 60,85 65 4,15 4,15 100% 3,45 83% 010 65 69,2 4,2 3 71% 2,70 64% 5011 69,2 73,1 3,9 2,35 60% 1,75 45% 4012 73,1 77,25 4,15 4,15 100% 3,85 93% 013 77,25 81,65 4,4 4,3 98% 4,05 92% 014 81,65 86,5 4,85 4,1 85% 4,45 92% 515 86,5 90,6 4,1 4,1 100% 3,50 85% 116 90,6 94,8 4,2 4 95% 3,85 92% 217 94,8 99 4,2 4,2 100% 3,90 93% 418 99 103,4 4,4 4,4 100% 4,20 95% 019 103,4 107,65 4,25 4,25 100% 4,10 96% 020 107,65 111,85 4,2 4,10 98% 3,40 81% 021 111,85 116 4,15 4,15 100% 3,25 78% 022 116 120,45 4,45 4,25 96% 4,00 90% 023 120,45 124,3 3,85 3,85 100% 3,15 82% 324 124,3 128,6 4,3 4,10 95% 3,70 86% 325 128,6 132,9 4,3 4,10 95% 4,10 95% 026 132,9 137,15 4,25 4,35 102% 4,25 100% 027 137,15 141,5 4,35 4,27 98% 4,10 94% 028 141,5 145,8 4,3 4,3 100% 4,10 95% 029 145,8 149,9 4,1 4,10 100% 3,50 85% 130 149,9 154 4,1 4,20 102% 3,55 87% 031 154 158,3 4,3 4,00 93% 3,85 90% 032 158,3 162,45 4,15 4,37 105% 3,85 93% 033 162,45 166,7 4,25 4,25 100% 3,80 89% 034 166,7 170,55 3,85 3,87 101% 3,25 84% 435 170,55 175,05 4,5 4,15 92% 3,75 83% 036 175,05 179 3,95 4,00 101% 3,05 77% 037 179 183,2 4,2 4,30 102% 3,05 73% 138 183,2 187,9 4,7 4,20 89% 3,95 84% 339 187,9 191,6 3,7 4,20 114% 3,55 96% 040 191,6 195,85 4,25 4,30 101% 4,00 94% 041 195,85 200,1 4,25 4,20 99% 4,15 98% 042 200,1 204,4 4,3 4,30 100% 4,30 100% 043 204,4 208,95 4,55 4,35 96% 4,30 95% 244 208,95 213,1 4,15 4,15 100% 3,95 95% 145 213,1 217,35 4,25 4,35 102% 4,15 98% 046 217,35 221,6 4,25 4,23 100% 4,05 95% 0

47 221,6 225,9 4,3 4,27 99% 3,75 87% 048 225,9 230,15 4,25 4,20 99% 3,95 93% 049 230,15 234,6 4,45 4,42 99% 4,25 96% 050 234,6 238,9 4,3 4,33 101% 4,05 94% 051 238,9 243,12 4,22 4,23 100% 4,00 95% 052 243,12 250,6 7,48 4,12 55% 6,78 91% 3 m missing 253 250,6 255 4,4 4,13 94% 3,85 88% 054 255 259,33 4,33 4,33 100% 3,87 89% 055 259,33 263,56 4,23 4,25 100% 4,03 95% 056 263,56 267,9 4,34 4,34 100% 3,94 91% 057 267,9 272,2 4,3 4,19 97% 3,95 92% 058 272,2 276,6 4,4 4,33 98% 4,05 92% 059 276,6 283,9 7,3 4,34 59% 3,99 55% 3 m missing 060 283,9 288,15 4,25 4,05 95% 3,70 87% 161 288,15 292,55 4,4 4,24 96% 3,90 89% 062 292,55 297,1 4,55 4,08 90% 4,35 96% 063 297,1 300 2,9 2,56 88% 2,35 81% 0EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC08-15 L-3000E 350N 300 0 -50 305m 19/01/09 24/01/09 MV 10/05/26-28

Principal Lithology

From To L Id rock type Photo

0,00 30,00 30 OB casing

30,00 44,50 14,5 MAnGray-green medium grained andesite. Feldspars, quartz and chlorite. No visible structures. Contact with following lithology is blocky.

44,50 93,20 48,7 PAnGreen, aphanitic andesite pillows, with calcite filled vacuoles. Borders between pillows are filled with quartz, carbonates and sometimes pyrite.

93,20 102,10 8,9 MaD

Green and black large-grained gabbro intrusion with 40% millimetric crystals of hornblende. Contacts with andesite are

sharp at 30o c.a.


125,30 135,70 10,4 SyD Red fine-grained syenite dyke. Contacts are at 70-90o c.a.


230,60 238,40 7,8 MAnGreen-brown fine-grained andesite. Contacts are sharp with andesite pillows at 60° c.a. Probably a dyke.


246,90 249,70 2,8 InDGray-brown fine-grained intermediate dyke. Contacts are sharp at 30° c.a.

249,70 254,00 4,3 MAn Green-brown fine-grained andesite.


256,90 264,60 7,7 SyDBeige very fine-grained syenite dyke. Magnetic due to dark veinlets containing magnetite and pyrite.


273,90 283,80 9,9 MAnGreen-gray fine to medium-grained andesite. Contacts are progressive with pillows.

DDH Depth



293,40 300,30 6,9 SyDRed fine-grained syenite dyke. 30% feldspar porphyrs between 294-296m. Contacts are sharp at 60° c.a.


Second Lithology

From To L Id rock types, grain size, etc. Photo

90,90 92,13 1,23 InD

Gray-green medium-grained intermediate dike. Millimetric rounded calcite masses near the borders. Contacts are sharp at

60o to c.a.105,00 106,50 1,50 SyD Red syenite dyke. Sharp contacts at 40o c.a.123,70 124,90 1,20 SyD Red syenite dyke. Sharp contacts at 70o c.a.138,00 138,80 0,80 SyD Red syenite dyke. Sharp contacts at 70o c.a.

170,40 171,70 1,30 InDGray-brown fine-grained intermediate dyke. Contacts are at 50° c.a. Andesite at upper contact is blocky.

176,70 177,50 0,80 SyDRed fine-grained syenite dyke. Upper contact is sharp at 30° c.a. The syenite is broken near the lower contact.

177,50 179,60 2,10 PoDGray-brown porphyric intermediate dyke with 40% millimetric plagioclase porphyrs. Weak foliation at 70° c.a. Lower contact at 70° c.a. Reddish color appears near the lower contact.

179,60 182,55 2,95 SyDRed fine-grained syenite dyke. A few large decimetric fragments of chlorite are present, most notably near the lower contact. Upper contact is sharp at 30° c.a.


195,80 197,15 1,35 InDGray-brown fine-grained intermediate dyke. Contacts are sharp at 30° c.a. A 4cm alteration border is present in the andesite: it is pale green and rich in calcite.


219,70 221,60 1,90 MAnGreen-brown fine grained biotite andesite. Well foliated at 70° c.a. Associated with quartz veins and sericitization.

227,00 227,80 0,80 InDGray-brown porphyric intermediate dyke with 40% millimetric feldspar porphyrs. Contacts are sharp at close to 90° c.a.

231,80 232,70 0,90 InDBrown fine-grained intermediate dyke with 20% calcite filled vacuoles. Two 1mm quartz veins with epidote borders at 232.4, striking at 30° c.a. Some pyrite mineralization.

245,30 246,90 1,60 MAnGreen-brown fine grained biotite andesite. Weakly foliated at 40° c.a. Associated with quartz veins and sericitization.

253,10 254,00 0,90 MAnGreen-brown fine-grained biotite andesite. Moderate foliation at 20° c.a. Associated with quartz vein with sericite borders and pyrite mineralization.

254,00 255,50 1,50 PAn Green aphanitic andesite pillows. Moderate foliation at 20° c.a.

264,70 265,50 0,80 InDGray-brown fine-grained intermediate dyke. Contacts are sharp at 70° and 50° but in the opposite direction.

Depth

273,90 274,30 0,40 InDBrown fine-grained intermediate dyke. Contacts are sharp at 70° c.a.



296,80 297,00 0,20 MAnGreen fine-grained andesite inclusion in the syenite dyke. Well foliated and folded. Contacts at 45° c.a.

304,00 304,90 0,90 SyDRed syenite dyke with 20% millimetric to centimetric biotite and chlorite crystals. Contacts are sharp at 50° c.a.

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal Tour Chl Hem

46,65 47,20 0,55 QTSmall quartz-tourmaline veins, and one 10cm quartz-carbonate vein. Epidote altreation of the wall-rock, and sulfide mineralization.

70o 20% 5% 5%

86,80 87,80 1,00 QCHeCarbonate-hematite-quartz filled breccias following a locally linear fracture, striking close to parallel to core axis.

10° 2% 5% 3%

128,50 130,70 2,20 QCChlSmall quartz-chlorite veinlets with associated potassic alteration of the wall-rock and pyrite mineralization, mostly in the veinlets themselves.

10° 2% 1% 2%

132,60 135,70 3,10 QChlSmall quartz-chlorite veinlets with associated potassic alteration of the wall-rock and pyrite mineralization, mostly in the veinlets themselves.

30° 2% 1% 2%

197,65 199,50 1,85 BrcLocal breccia. Fractures are filled with quartz, calcite and epidote. No visible mineralization.

207,10 209,70 2,60 BrcLocalized breccia in 3 pillow contacts. Black chlorite fragments in a quartz-carbonate matrix. No visible mineralization.

219,70 221,60 1,90 QChl

Quartz-chlorite veins. Quartz veins are at least twice folded. The strike in the central section is nearly sub-parallel, with minor tight folds with axis at 80° c.a. Associated with alteration and mineralization.

10° 10% 5%

245,30 246,90 1,60 QtzQuartz veins with strong sericitization of the wall-rock. Strik at 40° c.a. Associated with weak pyrite mineralization of the wall rock.

40° 5%

253,10 254,00 0,90 QtzFolded quartz veins with moderate sericitization of the wall-rock. Strik at 20° c.a. Associated with weak pyrite mineralization of the wall rock.

20° 5%

278,90 279,60 0,70 QtzSmall quartz veins with moderate sericitization and epidote alteration of the wallrock. Associated with strong pyrite mineralizationin the wallrock.

50-60° 10% 2%

283,80 285,60 1,80 BrcLocalized breccias near the contact between the two andesite units, filled with quartz, carbonate and chlorite. Moderate pyrite mineralization.

3% 3% 3%

287,80 288,90 1,10 QCaSeveral barren quartz-carbonate veins, with one pale green carbonate vein at the end of the zone with strong sulfide mineralization.

50° 5% 5%

291,30 291,35 0,05 QCa One barren 4cm quartz-carbonate vein 50° 80% 20%

301,10 301,15 0,05 QCa A few barren centimetric quartz-carbonate veins. 40° 50% 50%

Depth Veins(%)

From To L Id Description Serp Asb Chl Epi Alb Seric K Serp Asb Chl Epi Alb Seric K128,50 130,70 2,20 K Potassic alteration around quartz-chlorite veinlets. 2

132,60 135,70 3,10 K Potassic alteration around quartz-chlorite veinlets. 1

219,70 221,60 1,90 SeriStrong sericitic alteration associated with folded quartz veins and pyrite mineralization. 30%

245,30 246,90 1,60 SeriModerate sericitization near quartz veins (extending up to 4 cm from the vein). 8%

253,10 254,00 0,90 Seri Moderate sericitization near quartz veins. 5%

278,90 279,60 0,70 SeriSericitization and epidote alteration in the wall rock of quartz veins. 5% 15%

Depth Alteration (1-5) Pervasive Alteration (%) Frac-control

From To L Id Py Cpy Ars Cpy Po

46,65 47,20 0,55 PoMillimetric euhedral pyrite in the wall-rock near quartz veins. Anhedral pyrrhotite masses associated with epidote alteration.

10% 5%

128,50 130,70 2,20 PyEuhedral pyrite in quartz-chlorite veinlets and associated potassic alteration.

5%

132,60 135,70 3,10 PyEuhedral pyrite in quartz-chlorite veinlets and associated potassic alteration.

3%

219,70 221,60 1,90 PyMillimetric to centimetric subhedral pyrite associated with quartz veins and sericitization of the wall-rock.

8%

231,80 232,70 0,90 Py5% millimetric euhedral pyrite spread in an intermediate dyke.

5%

245,30 246,90 1,60 Py3% millimetric euhedral pyrite in quartz veins with sericitization alteration and in the wall rock.

3%

253,10 254,00 0,90 Py3% millimetric euhedral pyrite in quartz veins with sericitization alteration and in the wall rock.

3%

256,90 264,60 7,70 PyVery small black veinlets filled with calcite, magnetite and pyrite. Variable strike.

1%

278,90 279,60 0,70 Py8% centimetric euhedral pyrite crystals in the wall rock of quartz veins with sericite and epidote alteration.

8%

283,80 285,60 1,80 Py4% subhedral pyrite mineralization associated with breccias.

4%

287,80 288,90 1,10 PoEuhedral pyrite and stretched non-magnetic pyrrhotite in a pale green carbonate vein.

2% 5%

Mineralization (% sulphides)

Sample Number From To Length Comments Id Au Ag

38284 46,65 47,20 0,55Pyrite and pyrrhotite with quartz veins and epidote alteration

38285 86,80 87,80 1,00 Carbonate-hematite-quartz filled breccia

38286 128,50 129,60 1,10Pyrite with quartz-chlorite veins and potassic alteration.





38291 219,70 220,50 0,80 Pyrite with quartz veins and sericite alteration.


38293 231,80 232,70 0,90 Pyrite in an intermediate dyke.



38296 258,00 259,00 1,00Calcite-magnetite-pyrite veinlets in syenite dyke.


38298 278,90 279,60 0,70Pyrite in wall rock of quartz vein with epidote and sericite alteration.

38299 283,80 284,70 0,90 Pyrite in breccia.38300 284,70 285,60 0,90 Pyrite in breccia.

38301 287,80 288,90 1,10Pyrite and stretched non-magnetic pyrrhotite in green carbonate vein.

Assays

Logged by : MV Sheet of

Box number From To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 30,0 33,9 3,9 3,9 100% 3,10 79%2 33,9 38,0 4,1 4,1 100% 3,10 76%3 38,0 42,1 4,1 4,1 100% 3,14 76%4 42,1 46,6 4,4 4,0 91% 2,28 51%5 46,6 50,8 4,2 4,1 98% 3,35 80%6 50,8 54,9 4,2 4,2 100% 3,90 94%7 54,9 59,2 4,3 4,2 97% 3,62 85%8 59,2 63,5 4,3 4,3 100% 4,10 96%9 63,5 67,9 4,4 4,1 93% 3,60 81%

10 67,9 72,1 4,2 4,2 100% 3,50 83%11 72,1 76,3 4,2 4,2 100% 4,00 95%12 76,3 80,5 4,2 4,2 99% 3,96 94%13 80,5 84,7 4,2 4,2 100% 3,30 79%14 84,7 89,0 4,3 4,2 98% 3,40 79%15 89,0 93,1 4,1 4,1 100% 3,43 84%16 93,1 97,2 4,1 4,1 100% 3,65 89%17 97,2 101,2 4,0 4,0 100% 3,73 93%18 101,2 105,5 4,3 4,3 100% 4,00 93%19 105,5 109,9 4,4 4,4 100% 4,20 95%20 109,9 114,1 4,2 4,2 100% 3,53 84%21 114,1 118,2 4,1 4,1 100% 3,78 92%22 118,2 122,4 4,2 4,1 98% 4,00 95%23 122,4 126,7 4,3 4,3 100% 4,00 93%24 126,7 131,0 4,3 4,2 98% 3,63 84%25 131,0 135,2 4,2 4,0 95% 3,58 85%26 135,2 139,0 3,8 3,8 100% 3,10 82%27 139,0 142,9 3,9 3,9 100% 3,20 82%28 142,9 147,1 4,2 4,2 100% 3,50 83%29 147,1 151,4 4,3 4,3 100% 3,85 90%30 151,4 155,7 4,3 4,3 100% 4,24 99%31 155,7 160,0 4,3 4,3 100% 3,90 91%32 160,0 164,2 4,2 4,2 100% 3,24 77%33 164,2 168,7 4,5 4,5 100% 4,00 89%34 168,7 173,0 4,3 4,1 95% 3,02 70%35 173,0 177,0 4,0 3,9 98% 3,20 80%36 177,0 181,2 4,2 3,7 88% 2,24 53%37 181,2 185,2 4,0 4,0 100% 3,45 86%38 185,2 189,5 4,3 4,3 100% 3,85 90%39 189,5 193,8 4,3 4,3 100% 4,15 97%40 193,8 198,0 4,2 4,2 100% 4,02 96%41 198,0 202,2 4,2 4,1 98% 3,74 89%42 202,2 206,3 4,1 4,1 100% 3,70 90%43 206,3 210,5 4,2 4,2 100% 4,10 98%44 210,5 214,9 4,4 4,4 100% 4,10 93%45 214,9 219,1 4,2 4,2 100% 3,93 94%46 219,1 223,3 4,2 4,1 98% 2,60 62%47 223,3 227,5 4,2 4,1 98% 3,47 83%48 227,5 231,8 4,3 4,3 100% 3,93 91%49 231,8 236,0 4,2 4,2 100% 3,99 95%50 236,0 240,4 4,4 4,4 100% 4,18 95%51 240,4 244,7 4,3 4,3 100% 4,13 96%52 244,7 248,9 4,2 4,1 98% 3,90 93%

Geotechnical Log Hole No. :C08-15Date :10-05-26

Fracture Angle/Frequency Tally Highly Broken Fault Gouge

53 248,9 253,0 4,1 3,9 95% 2,95 72%54 253,0 257,0 4,0 4,0 100% 3,30 83%55 257,0 261,3 4,3 4,2 98% 3,92 91%56 261,3 265,7 4,4 4,4 100% 3,55 81%57 265,7 269,8 4,1 4,1 100% 3,83 93%58 269,8 274,0 4,2 4,2 100% 4,07 97%59 274,0 278,3 4,3 4,3 100% 4,03 94%60 278,3 282,5 4,2 4,2 100% 4,01 95%61 282,5 286,9 4,4 4,3 98% 4,00 91%62 286,9 291,0 4,1 4,1 100% 3,55 87%63 291,0 295,3 4,3 4,3 100% 4,09 95%64 295,3 299,5 4,2 4,2 100% 3,70 88%65 299,5 303,7 4,2 3,9 93% 3,06 73%66 303,7 305,0 1,3 1,3 100% 0,92 71%

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC08-16 L-3400E 100N 300 0 -50 251m 02/09/09 16-17/02/2009 AC Feb 8 - March 5, 2010

Princ Lithology

From To L Id rock type CA Photo

6 17 11 pillow and

hetero fg-mg pale to med green andesite w 5 mm chill margins (3-5%) forming cm pillows, w paler green and from 8 to 10.4 m showing 5-10% mm vesicle qz phX loc hexagonal. Chill margins are composed of qz 80% & py 20% w loc brecciation. 1 m of mm proto-pillow breccia or flow top breccia at lower contact w mm rounded fragments. Loc mm-2 cm qz-cal v 5

17 26,75 9,75 ultramafichom fg dark-green / black ultramafic w talc touch w 50 cm transition zone at upper contact from massive and to massive ultramafic. Only few 1 cm qz=-cal vein w var angles 45 to CA, tr of py

26,75 28,2 1,45 SZ fg SZ w qz minor epi-py in sheared and 35

28,2 33 4,8 Si zone fg ± hom med grey silicified zone w 1% sub-mm diss py 0 & 4033 34,15 1,15 SZ fg hetero qz SZ w minor epi & .5% sub-mm diss py 0-2034,15 34,6 0,45 qz v 40% 1-5 cm qz v 50 to CA in massive fg Si zone 5034,6 35,5 0,9 Si zone fg ± hom beige light grey massive Si zone w .5% sub mm diss py

35,5 37,4 1,9 SZhetero mg SZ w banded zone (mm-1cm), cm more massive fg serp black zone, cm brecciation and sw w 10% mm-1 cm qz deformed veining and 5% assimilated ultramafic mat over 1 m 0-35

37,4 38,25 0,85 Si zone massive to fol fg to mg Si zone med grey to light greyu-green due to epi

38,25 46,4 8,15 SZfg to mg hetero qz & Si SZ w chlo-epi, 3% cm qz veining 0-30 to CA, w cm more massive py-bearing zone at upper contact & mm to cm banding, cm sheared pegmatite, chlo-pl-epi-py 0 & 35

46,4 48,8 2,4 sheared andfg-mg hetero sheared and w cm fg Si zone w 1% sub-mm diss py, 20 cm quartz veining 40 to CA at lower contact, cm massive zone at upper contact & 5% mm qz sw 40

48,8 52,1 3,3 epi sheared andSZ w mm qz veining in fol fg epi (3%) andesite w 5-7 % mm-1cm qz v & sw.unit contains a % of ultramafic material (talc touch) 35

52,1 59,5 7,4 bx and

fg to mg med green hetero andesite w 4-20 cm cm thick chill margin ? zones carrying mm pale green spherule zone in black chlo/ serp? mx 1-4 cm thick, brecciation w qz-cal mx & loc mm sheared qz v. Chill margins are 30 to 60 cm apart. Whole unit is brecciated w angular fragmentation & 4-7% mm-2cm qz-cal sw & veining. 40 first cm of unit is carrying some epidotisation. unit is massive w loc brecciation 20-35 to CA 20

59,5 68,35 8,85 hetero andsame as 52.1 w much less angular qz-cal brecciation, 2% w loc 20 to CA, unit ends w 4 cm spherulitic zone 80 to CA 20

68,35 70,4 2,05 int dyke hom fg-mg int dyke med grey purplish w 3% white mm phX and 5% sub-mm chlo phX

70,4 74,5 4,1 mg gabbrohom mg meg green gabbro w 10 cm fg chill margin at upper contact w 3% qz-cal 1-2 cm wide veins 30 to CA

74,5 74,8 0,3 int dyke idem previous dyke wo phX 74,8 75,95 1,15 fg gabbro hom fg gabbro w similar 1-2 cm wide qz-cal veining 20 to CA75,95 79,6 3,65 int tuff hom fg med grey sedimentary like unit may be metased ou metatuff, wek fol 20 to CA 20

79,6 88,6 9 spherulitic pil and

fg light green hom and w 20-100cm spaced interpreted piollow chill margins 3-10 cm wide 50-80 to w mm spherule zone in black chlo-Si matrix & central brecciated zone w mm-1 cm qz-cal-chlo and loc shear (see photos) 4

88,6 125,65 37,05 spherulitic pil and

same as previous unit w spherule zones 1.2 m apart w mg babbro text at center of pillow or smaller pillow w spherule inner part. Loc the spherule margin zones show up to 30 cm of pale green silicification or qz-cal veining & brecciation up to 20 cm 6

125,65 130,5 4,85 gabbrofg-mg hom light-med green gabbro w 35% local fg decim and zones w mm spherule in black chlo-Si mx, possibly chill margin remnant, also loc gabbro shows sharp contact w fg and

DDH Depth

130,5 133,5 3 int dykefg-mg hom int dyke meg-grey purplish w 15% white mm phX, contact 40 to CA, upper contact shows mm-1 cm apophysis and veins

133,5 164,9 31,4 spherulitic pil and same as 125.65, and w interpreted pillow chill margins 3

164,9 168,2 3,3 int dykefg-mg hom int dyke meg-grey purplish w 15% white mm phX, contact 40 to CA, upper contact shows mm-1 cm apophysis

168,2 185,8 17,6 same as 125.65, and w interpreted pillow chill margins185,8 192,85 7,05 int dyke hom mg cal-chlo int dyke192,85 195,8 2,95 fg-mg med green ± hom leuco gabbro w finer zone, 3% mm qz-cal veining 40 to CA195,8 226,4 30,6 pillow and fg to mg loc gabbroic text, ± hom andesite w cm chlo-cal chill margins, loc fol 40 to CA

226,4 235,4 9 alt andsame unit, more alt, loc chlo schist over 100 cm w 5% diss py 50 to CA, w 4% qz-cal mm-2cm v, loc cm leucocratic epi zone possibly alt chill margins

235,4 251 15,6 pillow andfg loc mg med green and w cm pl-chlo-py chill margins (see photos), w cm alt pl phX in the last 3 m

251 EOH

Second Lithology

From To L Id rock types, grain size, etc. CA Photo

8 10,4 2,4 pil andpaler green zone w 5% well dev chill margins & mm euh porphyric quartz phX inside pillows

18,5 18,9 0,4 int dyke hom fg-mg pale purplish bo int dyke

36,4 37,4 SZ 5% of ultramafic material assimilated in this section

39,7 40,1 0,4 int dyke hom fg-mg med grey chl-pl int dyke

48,6 48,8 0,2 qz v fol qz v w assimilated chl-py mm stringers 45

83,2 -83,2 qz-cal bx 10 cm ang bx w mm-cm frag & 40% qz-cal 40

95,2 95,4 0,2 qz-Si v 80% qz veining in silicified zone 40

123,8 124,6 0,8 Si zonepale green hom fg silicified zone w fuzzy & sharp contacts w 7% mm qz phX, could be a dyke 15-30

148,4 -148,4 qz v 3 cm qz-cal v 40 to CA 40

149,05 -149,05

151,3 151,45 0,15 int dykehetero fg-mg purplish-grey dyke w mm spherules, 3% diss py & 2-3 cm chill margins on both contact (see photo) 90

156,3 162,7 6,4 bx 3% ang mm qz-cal brecciation w mm-1-2 cm veining 40 to CA 40184,15 185,7 1,55 bx 3% ang mm qz-cal brecciation w mm-1-2 cm veining 40 to CA 40

187,7 188 0,3 SZmm banding w chlo-cal-qz SZ w few 1 cm qz v 40 to CA, loc brecciated w mm-1 2cm ± ang fragments 40

188,9 190,8 1,9mm banding w chlo-cal-qz SZ w few 1 cm qz v 40 to CA, loc brecciated w mm-1 2cm ± ang fragments 40

195,8 198,4 2,6 qz v 5% mm-3cm qz v, 20 to CA 20200,9 201,05 0,15 qz-epi SZ 60202,2 202,6 0,4 qz-epi SZ 80% 40218,7 219,4 0,7 qz-pl v + int dyke40 cm brecciated qz-pl v at upper contact 20227,8 229,2 1,4 int dyke 70% dark grey hom fg int dyke

Depth

Alteration (1-5) Pervasive Alteration (%) Frac-control

From To L Id Description CA Qz Cal Epi Si Chl Epi Alb Qtz-Cal

48,8 52,6 3,8 epi andepidote sheared & brecciated andesite 30 2 2 3 5 4

Depth

Mineralization (% sulfides)

From To L Id Py Cpy Po

6 17 11 pillow and 2% (diluted) sub-mm py in .5 mm wide qz chill margins 2,00%

No. From To L Description

38236 std 6Pc

38237 std 15 Pa

38238 diabase 20 cm sample @ 111-111.5m

38239 5,4 6,15 0,75 Si-py 1 cm chill margin








38247 26,75 28 1,25 SZ

38248 28 28,8 0,8 Si zone

38249 28,8 33 1,2 Si zone 3 m missing

38250 33 34,15 1,15 SZ

38251 34,15 34,6 0,45 Qz vein

38252 34,6 35,5 0,9 Si zone

38253 35,5 36,4 0,9 SZ

38254 36,4 37,4 1 SZ

38255 37,4 38,25 0,85 Si zone

38256 38,25 39,8 1,55 SZ

38257 40,1 41 0,9 SZ

38258 41 42 1 SZ

38259 42 43 1 SZ

38260 43 44 1 SZ38261 44 45 1 SZ38262 45 46,4 1,4 SZ38263 46,4 47,4 1 sheared and38264 47,4 48,8 1,4 sheared and38265 std 6Pc38266 std 15Pa38267 diabase 20 cm 111-111.538268 48,8 50 1,2 epi sheard and38269 50 51 1 epi sheard and38270 51 52,1 1,1 epi sheard and

Sample results

Logged by : AC Sheet of

Box # From To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 5 9 4 3,9 98% 3,75 94% 18,2 19,22 9 13,2 4,2 4,2 100% 4,2 100% 24 24,43 13,2 17 3,8 3,7 97% 2,4 63% 46,7 474 17 21 4 3,9 98% 3,1 78% 56,7 57,35 21 24,9 3,9 3,8 97% 3,3 85% 59 63,46 24,9 29,1 4,2 4,2 100% 3,95 94%7 29,1 36,4 4,3 4,3 100% 4,15 97% 3 m error8 36,4 40,5 4,1 4,1 100% 3,45 84%9 40,5 44,6 4,1 4 98% 3 73%10 44,6 48,8 4,2 4,1 98% 3,65 87%11 48,8 53 4,2 4,2 100% 3,9 93%12 53 56,7 3,7 3,6 97% 3 81%13 56,7 60,7 4 3,8 95% 1,9 48%14 60,7 63,9 3,2 2,7 84% 0,1 3%15 63,9 67,6 3,7 3,7 100% 3,55 96%16 67,6 71,7 4,1 4,1 100% 3,6 88%17 71,7 75,8 4,1 4,1 100% 3,65 89%18 75,8 80,05 4,25 4,25 100% 3,95 93%19 80,05 84,2 4,15 4,15 100% 4,15 100%20 84,2 88,6 4,4 4,4 100% 4,1 93%21 88,6 92,55 3,95 3,95 100% 3,8 96%22 92,55 96,5 3,95 3,95 100% 2,95 75%23 96,5 100,75 4,25 4,25 100% 4,25 100%24 100,75 104,65 3,9 3,9 100% 3,7 95%25 104,65 108,8 4,15 4,15 100% 4,05 98%26 108,8 113 4,2 4,2 100% 4,2 100%27 113 117,25 4,25 4,25 100% 4,25 100%28 117,25 121,45 4,2 4,2 100% 4,15 99%29 121,45 125,65 4,2 4,2 100% 4,13 98%30 125,65 129,95 4,3 4,3 100% 3,85 90%31 129,95 134,2 4,25 4,25 100% 3,95 93%32 134,2 138,5 4,3 4,3 100% 4,2 98%33 138,5 142,6 4,1 4,1 100% 3,85 94%34 142,6 146,65 4,05 4,05 100% 3,85 95%35 146,65 151 4,35 4,35 100% 4,3 99%36 151 155,1 4,1 4 98% 3,55 87%37 155,1 159,1 4 3,8 95% 2,55 64%38 159,1 163,1 4 3,9 98% 3,3 83%39 163,1 167,4 4,3 4,3 100% 3,8 88%40 167,4 171,7 4,3 4,3 100% 3 70%41 171,7 176 4,3 4,3 100% 4,25 99%42 176 180,2 4,2 4,2 100% 4,2 100%43 180,2 184,6 4,4 4,4 100% 4,15 94%44 184,6 188,7 4,1 4,1 100% 3,65 89%45 188,7 193 4,3 4,3 100% 4,25 99%46 193 197 4 4 100% 3 75%47 197 201 4 3,95 99% 2,8 70%48 201 205,35 4,35 4,35 100% 4,35 100%49 205,35 209,6 4,25 4,25 100% 4,15 98%50 209,6 213,8 4,2 4,2 100% 4 95%

Geotechnical Log Hole No. :C08-19Date : Feb 1 10


51 213,8 218,2 4,4 4,4 100% 4,2 95%52 218,2 222,45 4,25 4,25 100% 3,85 91%53 222,45 226,5 4,05 4,05 100% 4,05 100%54 226,5 230,6 4,1 4,1 100% 3,9 95%55 230,6 234,8 4,2 4,2 100% 4 95%56 234,8 -234,8 0% 0%57 0 0 #DIV/0! #DIV/0!58 0 0 #DIV/0! #DIV/0!59 0 0 #DIV/0! #DIV/0!60 0 0 #DIV/0! #DIV/0!61 0 0 #DIV/0! #DIV/0!62 0 0 #DIV/0! #DIV/0!63 0 0 #DIV/0! #DIV/0!64 0 0 #DIV/0! #DIV/0!65 0 EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-08-17 L-2000E 2050N 300 0 -50 293,4 17/02/09 23/02/09 MV 10/05/29-31

Princ Lithology

From To L Id rock type Photo0,00 33,00 33,00 OB Casing

33,00 87,00 54,00 TufGray dacitic lapilli and bomb tuff. Strongly deformed and well foliated at 20° c.a. Fragments are mostly of felsic nature, with a few basaltic ones.

87,00 95,00 8,00 MAnGray fine-grained dacite. Contact with upper unit is progressive: disappearance of foliation and of fragments. Very weakly foliated at 40° c.a.

95,00 126,00 31,00 BAn

Localized breccia in dacite. Gray angular dacitic fragments in a black aphanitic matrix. Matrix is about 10% of the whole rock, and is associated with up to 10% pyrrhotite and pyrite mineralization.

126,00 139,90 13,90 MAn Gray fine-grained dacite. Weakly foliated at about 50° c.a.

139,90 199,90 60,00 BAn

Green very fine-grained andesite. Well foliated at 30° c.a. Pervasive silica alteration in bands, giving them a pale green aspect with green fragments (unaltered rock). Alteration decreases in depth.

199,90 248,00 48,10 MAnGreen fine-grained andesite. Weakly foliated at 30° c.a. Change in lithology is marked by reduction in foliation and disappearance of pervasive alteration

248,00 256,30 8,30 BAn Green fine-grained andesite. Moderately foliated at 40°. Pervasive silica alteration taking a breccia-like form.

256,30 279,80 23,50 MAn Green fine-grained andesite. Weakly foliated at 30°.

279,80 291,60 11,80 DiDDark gray medium-grained diabase dyke. Granulometry is smaller towards the contacts. Contacts are at 50° c.a. Strong foliation in the proximity of large quartz veins.

291,60 293,40 1,80 MAn Gray-green fine-grained andesite.293,40 EOH End Of Hole.

DDH Depth

Second Lithology From To L Id rock types, grain size, etc. Photo

76,70 78,50 1,80 InDGray fine to medium grained intermediate dyke. Granulometry is coarser near the center. Well foliated, with sharp contacts, both at 20° c.a.

132,00 135,60 3,60 PoDGray-brown intermediate porphyry dyke. 5 to 30% centimetric feldspar porphyrs, most in the center and least at the contacts. Contacts are sharp at 30° c.a.

160,90 166,10 5,20 InD

Reddish brown fine to medium grained intermediate dyke. About 20% biotite crystals are present, their size increasing towards the center. Contacts are sharp at 25° c.a.

170,60 170,90 0,30 DiD Black diabase dyke with irregular shape.

172,90 174,10 1,20 PoDGray-brown intermediate porphyry dyke. 30% feldspar porphyrs. Contacts are sharp at 50° c.a.

175,90 183,60 7,70 DiD

Several black diabase dykes, the smallest with irregular shapes, cutting into andesite, forming about 10% of this zone. The largest is 30cm, and their contacts is between 30 and 60° c.a.

233,20 234,20 1,00 InDBrown fine-grained intermediate dyke. Sharp contacts at 30°.

244,00 245,40 1,40 InD Brown fine-grained intermediate dyke. Contacts at 30° c.a.

Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal Chl Alb

41,40 42,20 0,80 QCaPossible quartz-carbonate vein (or bomb), with associated albite alteration of the wall rock and very weak pyrite mineralization.

- 20% 8%

115,00 116,10 1,10 QtzPinch and swell 3cm quartz vein with pyrrhotite and chalcopyrite mineralization.

10° 15%

146,00 169,00 23,00 QAlbSmall, early and highly deformed quartz-albite vein associated with possible visible gold mineralization. Only in andesite.

1% 1%

176,10 177,20 1,10 QCChlAt least 5cm wide quartz-carbonate-chlorite vein with strong epidote and hematite alteration and weak pyrite mineralization.

20° 50% 6% 4%

181,50 182,20 0,70 QtzFolded very small quartz veins (<5mm) associated with strong albite alteration of the wall rock. Very weak pyrite mineralization. Fold axis 70° c.a.

203,40 204,50 1,10 QCAlbQuartz-albite and quartz-carbonate veins with very weak pyrite mineralization. Angle is for quartz-albite.

40° 10% 6% 10%

209,30 210,00 0,70 QCalbA few quartz-carbonate veins, 1-5cm large, striking 20-40° c.a. Very weak pyrite mineralization.

20-40° 10% 15%

215,00 215,60 0,60 Brc Carbonate filled localized breccia. 20°

217,50 218,00 0,50 QtzVery small quartz veins with strong, localized albite alteration of the wall rock. Weak pyrite mineralization.

30° 2%

219,40 220,20 0,80 QtzSmall quartz veins with strong albite alteration and weak pyrite.

40° 4%

222,00 227,00 5,00 QtzSeveral small quartz veins with strong albite alteration. No visible mineralization. Largest alteration zones are at 222.15 (5cm) and at 224.25 (12cm).

50° 1%

227,00 227,50 0,50 QtzLarge (4cm) grey quartz vein. No visible alteration or mineralization.

50° 5%

230,00 230,50 0,50 Qtz Large (4cm) quartz vein with weak albite alteration. 70° 5%

237,30 238,00 0,70 QtzA 3cm quartz vein in a silicified zone of the rock. Weak pyrite mineralization.

40° 3%

238,00 240,75 2,75 QCalbVery large carbonate-quartz veins, possibly breccia. Moderate pyrite mineralization in the wall rock only.

40° 4% 20%

240,75 241,50 0,75 QtzMany small grey quartz veins in a small zone. Strong pyrite mineralization.

40-50° 25%

244,00 245,40 1,40 Brc Calcite filled breccia in a dyke. 15%

246,40 246,60 0,20 QtzSmall quartz veins with large albite alteration border. Moderate pyrite mineralization.

50° 5%

258,70 259,20 0,50 Qtz 2cm grey quartz vein. No alteration or mineralization. 20° 5%

Depth Veins(%)

260,00 260,50 0,50 QCAlbQuartz-carbonate veins and a quartz-albite veins. Both are at 60° c.a. but in opposite directions.

60° 5% 4% 1%

262,20 262,40 0,20 QtzOne 7cm grey quartz vein. No visible alteration or mineralization.

60° 10%

265,20 265,80 0,60 QtzOne 6cm quartz vein. No visible mineralization or alteration.

20° 20%

275,80 277,00 1,20 QAlbA few sub-parallel quartz-albite veins. Largest is 3cm. Very weak pyrite mineralization.

60° 3% 8%

283,70 284,30 0,60 QtzLarge (12cm) quartz vein with a few smaller ones. No visible mineralization.

40° 20%

291,60 292,10 0,50 QtzTwo quartz veins in the andesite near the contact with diabase. No mineralization.

30° 5%

From To L Id Description Serp Asb Chl Epi Alb Hem Sil Serp Asb Chl Epi Alb Sil

41,40 42,20 0,80 Alb Possible albite alteration of the wall rock near a quartz-carbonate vein.

1

139,90 176,10 36,20 SilAlb

Silica and albite alteration in a foliated andesite. Alteration appears in bands, following foliation, and appear as green unaltered fragments in a pale green, altered matrix. This alteration does not affect the dykes.

3 3

176,10 177,20 1,10 EpiHem Strong epidote and hematite alteration both in a large quartz vein and in the wall rock

4 4

177,20 199,90 22,70 SilAlb

Weak silica and albite alteration in a foliated andesite. Alteration appears in bands, following foliation, and appear as green unaltered fragments in a pale green, altered matrix. This alteration does not affect the dykes.

1 1

203,40 204,50 1,10 Alb Strong but limited albite alteration around quartz veins. 10%217,50 218,00 0,50 Alb Moderate albite alteration around quartz veins. 10%219,40 220,20 0,80 Alb Strong albite alteration around quartz veins. 20%

220,20 221,10 0,90 Sil Strong silica alteration in bands. Breccia-like texture, with green fragments in a pale green matrix.

3

222,00 227,50 5,50 Alb Strong albite alteration of the wall rock near small quartz veins

5%

230,00 230,50 0,50 Alb Weak albite alteration around a quartz vein. 5%

237,30 238,00 0,70 SilPervasive silicification of the rock. May or may not be associated with either the quartz vein or the pyrite mineralization.

2

246,40 246,60 0,20 Alb Albite alteration around quartz veins. 20%

248,00 256,30 8,30 Sil Pervasive silicification of the rock, taking a breccia-like form, similar to 177.20 - 199.90.

1


From To L Id Py Cpy Ars Cpy Po VG

41,40 42,20 0,80 PyVery weak and very fine grained pyrite mineralization in a possible quartz vein with albite alteration.

1%

59,00 59,60 0,60 PyStrong centimetric euhedral pyrite mineralization in a felsic fragment. Pyrite is rusted.

8%

90,00 90,05 0,05 PoChunk of very weakly magnetic pyrrhotite with a few euhedral pyrite crystals.

1% 10%

95,00 115,00 20,00 PoAnhedral pyrrhotite masses and euhedral pyrite crystals in the cinder matrix of the volcanoclastic breccia.

2% 3%

115,00 116,10 1,10 PoCpy Pyrrhotite and chalcopyrite in a boudinaged quartz vein. 1% 7%

116,10 126,00 9,90 PoAnhedral pyrrhotite masses and euhedral pyrite crystals in the ash matrix of the volcanoclastic breccia.

2% 3%

146,00 169,00 23,00 VG

Possible visible gold mineralization, some are associated with small early quartz-albite veins, some not. Only in andesite. The limits of this zone are the first and the last seen occurrences.

Tr

176,10 177,20 1,10 PyWeak pyrite mineralization associated with large quartz vein and epidote and hematite alterations.

2%

181,50 182,20 0,70 PyVery weak pyrite mineralization associated with very small quartz veins and albite alteration.

1%

203,40 204,50 1,10 PyVery weak pyrite mineralization associated with quartz veins and albite alteration.

1%

209,30 210,00 0,70 Py Very weak pyrite mineralization in quartz-carbonate veins. 1%

217,50 218,00 0,50 PyWeak pyrite mineralization in the wall rock of quartz veins with albite alteration.

2%

219,40 220,20 0,80 PyWeak pyrite mineralization around quartz veins with albite alteration.

2%

237,30 238,00 0,70 PyWeak pyrite mineralization associated with a quartz vein in a silicified zone.

1%

238,00 240,75 2,75 PyModerate pyrite mineralization only in the wall rock of very large carbonate-quartz veins.

4%

240,75 241,50 0,75 PyStrong euhedral to subhedral pyrite mineralization associated with grey quartz veins.

8%

246,40 246,60 0,20 PyModerate pyrite mineralization associated with quartz vein and albite alteration.

3%

262,40 263,00 0,60 Py Pyrite veinlets. 7%275,80 277,00 1,20 Py very weak pyrite mineralization in quartz-albite veins. 1%


Sample Number From To Length Comments Id Au Ag

38302 41,40 42,20 0,80Possible quartz vein with albite alteration and very weak pyrite mineralization.

38303 59,00 59,60 0,60 8% pyrite in felsic fragment.

38304 104,10 104,80 0,705% pyrite and 5% pyrrhotite in a ash-rich portion of the volcanoclastic breccia.

38305 115,00 116,10 1,107% pyrrhotite and 1% chalcopyrite in a quartz vein.

38306 0,00 Blank 238307 0,00 Standard 6Pc38308 139,90 140,90 1,00 Possible visible gold in altered andesite.38309 140,90 141,90 1,00 Possible visible gold in altered andesite.38310 141,90 142,90 1,00 Possible visible gold in altered andesite.38311 142,90 143,90 1,00 Possible visible gold in altered andesite.38312 143,90 144,90 1,00 Possible visible gold in altered andesite.38313 144,90 145,90 1,00 Possible visible gold in altered andesite.38314 145,90 146,90 1,00 Possible visible gold in altered andesite.38315 146,90 147,90 1,00 Possible visible gold in altered andesite.38316 147,90 148,90 1,00 Possible visible gold in altered andesite.38317 148,90 149,90 1,00 Possible visible gold in altered andesite.38318 149,90 150,90 1,00 Possible visible gold in altered andesite.38319 150,90 151,90 1,00 Possible visible gold in altered andesite.38320 151,90 152,90 1,00 Possible visible gold in altered andesite.38321 152,90 153,90 1,00 Possible visible gold in altered andesite.38322 153,90 154,90 1,00 Possible visible gold in altered andesite.38323 154,90 155,90 1,00 Possible visible gold in altered andesite.38324 155,90 156,90 1,00 Possible visible gold in altered andesite.38325 156,90 157,90 1,00 Possible visible gold in altered andesite.38326 157,90 158,90 1,00 Possible visible gold in altered andesite.38327 158,90 159,90 1,00 Possible visible gold in altered andesite.38328 159,90 160,90 1,00 Possible visible gold in altered andesite.38329 0,00 Blank 338330 0,00 Standard 15Pa38331 166,10 167,10 1,00 Possible visible gold in altered andesite.38332 167,10 168,10 1,00 Possible visible gold in altered andesite.38333 168,10 169,10 1,00 Possible visible gold in altered andesite.38334 169,10 170,10 1,00 Possible visible gold in altered andesite.38335 170,10 171,10 1,00 Possible visible gold in altered andesite.

Assays

38336 171,10 172,10 1,00 Possible visible gold in altered andesite.38337 172,10 172,90 0,80 Possible visible gold in altered andesite.38338 172,90 174,10 1,20 Porphyry dyke.38339 174,10 175,10 1,00 Possible visible gold in altered andesite.38340 175,10 176,10 1,00 Possible visible gold in altered andesite.

38341 176,10 177,20 1,10Large quartz vein with epidote and hematite alteration.

38342 177,20 178,20 1,00 Possible visible gold in altered andesite.38343 178,20 179,20 1,00 Possible visible gold in altered andesite.38344 179,20 180,20 1,00 Possible visible gold in altered andesite.38345 180,20 181,20 1,00 Possible visible gold in altered andesite.

38346 181,20 182,20 1,00Small quartz veins with strong albite alteration.

38347 182,20 183,20 1,00 Possible visible gold in altered andesite.38348 183,20 184,20 1,00 Possible visible gold in altered andesite.38349 184,20 185,20 1,00 Possible visible gold in altered andesite.38350 185,20 186,20 1,00 Possible visible gold in altered andesite.38351 0,00 Blank 238352 0,00 Standard 6Pc38353 186,20 187,20 1,00 Possible visible gold in altered andesite.38354 187,20 188,20 1,00 Possible visible gold in altered andesite.38355 188,20 189,20 1,00 Possible visible gold in altered andesite.38356 189,20 190,20 1,00 Possible visible gold in altered andesite.38357 190,20 191,20 1,00 Possible visible gold in altered andesite.38358 191,20 192,20 1,00 Possible visible gold in altered andesite.38359 192,20 193,20 1,00 Possible visible gold in altered andesite.38360 193,20 194,20 1,00 Possible visible gold in altered andesite.38361 194,20 195,20 1,00 Possible visible gold in altered andesite.38362 195,20 196,20 1,00 Possible visible gold in altered andesite.38363 196,20 197,20 1,00 Possible visible gold in altered andesite.38364 197,20 198,20 1,00 Possible visible gold in altered andesite.38365 198,20 199,20 1,00 Possible visible gold in altered andesite.38366 199,20 199,90 0,70 Possible visible gold in altered andesite.38367 199,90 200,90 1,00 Possible visible gold in altered andesite.38368 209,30 210,00 0,70 Quartz-carbonate veins with weak pyrite.38369 217,50 218,00 0,50 Quartz veins with albite and pyrite.38370 219,40 220,20 0,80 Quartz veins with albite and pyrite.38371 220,20 221,10 0,90 Breccia-like silica alteration.

38372 0,00 Blank 338373 0,00 Standard 6Pc38374 222,00 222,50 0,50 Large quartz-albite vein.38375 223,10 224,40 1,30 Large quartz-albite veins.38376 227,00 227,50 0,50 Grey quartz vein.38377 237,30 238,00 0,70 Silicified zone with quartz vein.38378 238,00 239,00 1,00 Very large quartz-carbonate vein.38379 239,00 240,00 1,00 Very large quartz-carbonate vein.38380 240,00 240,75 0,75 Very large quartz-carbonate vein.38381 240,75 241,50 0,75 Many small grey quartz veins.38382 246,20 246,70 0,50 Quartz-albite veins.38383 258,70 259,20 0,50 Small grey quartz vein.

38384 260,00 260,50 0,50 Quartz-carbonate veins and quartz-albite vein.

38385 262,00 263,00 1,00 Grey quartz veins and pyrite veins.38386 265,20 265,80 0,60 Large quartz vein.38387 275,80 277,00 1,20 Several quartz-albite veins.38388 283,70 284,40 0,70 Large quartz vein in diabase.38389 291,60 292,10 0,50 Two quartz veins at lithological contact.

Hole No. : C-08-17Date : 2010/05/29-31Logged by : MV Sheet of

Box # From To Length Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 33,10 36,80 3,70 3,70 100% 3,20 86%2* 36,80 43,40 6,60 3,20 48% 2,07 31%3 43,40 47,00 3,60 2,80 78% 0,95 26%4 47,00 51,10 4,10 3,30 80% 1,50 37%5 51,10 53,20 2,10 2,10 100% 0,90 43%6 53,20 56,50 3,30 3,00 91% 0,66 20%7 56,50 59,80 3,30 3,00 91% 0,32 10%8 59,80 63,80 4,00 4,00 100% 3,90 98%9 63,80 68,10 4,30 4,10 95% 3,90 91%10 68,10 72,40 4,30 4,30 100% 4,24 99%11 72,40 76,70 4,30 4,30 100% 4,00 93%12 76,70 80,80 4,10 3,60 88% 3,13 76%13 80,80 84,50 3,70 3,90 105% 3,41 92%14 84,50 88,60 4,10 4,00 98% 3,50 85%15 88,60 92,60 4,00 4,00 100% 3,53 88%16 92,60 96,70 4,10 4,10 100% 3,65 89%17 96,70 100,90 4,20 4,20 100% 3,82 91%18 100,90 104,80 3,90 3,90 100% 3,15 81%19 104,80 108,30 3,50 3,50 100% 2,42 69%20 108,30 112,50 4,20 4,20 100% 4,00 95%21 112,50 116,80 4,30 4,30 100% 4,12 96%22 116,80 121,20 4,40 4,40 100% 4,22 96%23 121,20 125,50 4,30 4,30 100% 3,70 86%24 125,50 129,70 4,20 4,20 100% 3,52 84%25 129,70 134,00 4,30 4,30 100% 3,86 90%26 134,00 138,20 4,20 4,20 100% 3,90 93%27 138,20 142,40 4,20 4,20 100% 3,81 91%28 142,40 146,30 3,90 3,80 97% 3,50 90%29 146,30 150,50 4,20 4,10 98% 3,41 81%30 150,50 154,40 3,90 3,90 100% 3,60 92%31 154,40 158,20 3,80 3,80 100% 3,42 90%32 158,20 162,40 4,20 4,20 100% 3,86 92%33 162,40 166,30 3,90 3,90 100% 3,35 86%34 166,30 170,40 4,10 4,00 98% 3,50 85%35 170,40 174,50 4,10 4,10 100% 3,47 85%36 174,50 178,60 4,10 4,10 100% 3,64 89%37 178,60 182,90 4,30 4,30 100% 3,93 91%38 182,90 187,10 4,20 4,20 100% 3,88 92%39 187,10 191,40 4,30 4,30 100% 4,10 95%40 191,40 195,70 4,30 4,20 98% 3,87 90%41 195,70 200,00 4,30 4,30 100% 4,11 96%42 200,00 204,20 4,20 4,20 100% 3,59 85%43 204,20 208,50 4,30 4,30 100% 3,90 91%44 208,50 212,70 4,20 4,20 100% 3,70 88%45 212,70 216,80 4,10 4,10 100% 3,95 96%46 216,80 221,00 4,20 4,20 100% 3,90 93%47 221,00 225,10 4,10 4,10 100% 3,93 96%48 225,10 229,30 4,20 4,20 100% 3,73 89%49 229,30 233,50 4,20 4,20 100% 3,73 89%50 233,50 237,60 4,10 4,10 100% 3,99 97%51 237,60 241,70 4,10 3,90 95% 3,39 83%52 241,70 245,10 3,40 3,20 94% 2,04 60%

Geotechnical Log


53 245,10 249,30 4,20 4,30 102% 4,05 96%54 249,30 253,60 4,30 4,30 100% 4,24 99%55 253,60 257,90 4,30 4,20 98% 3,89 90%56 257,90 262,20 4,30 4,30 100% 4,00 93%57 262,20 266,40 4,20 4,10 98% 3,63 86%58 266,40 270,70 4,30 4,30 100% 4,06 94%59 270,70 275,00 4,30 4,30 100% 4,14 96%60 275,00 279,10 4,10 4,10 100% 3,66 89%61 279,10 283,20 4,10 4,00 98% 3,59 88%62 283,20 287,30 4,10 4,10 100% 3,60 88%63 287,30 291,50 4,20 4,20 100% 4,13 98%64 291,50 293,40 1,90 1,90 100% 1,55 82%* 3 meters missing between box 1 and 2, either a missing box or, more likely, a mistake with length blocks.

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC08-18 L-2200E 2200N 300 0 -50 302m 24/02/2009 28/02/2009 AC Feb1-7 10

DDH Depth Princ Lithology

From To L Id rock type CA Photo

39 93,2 54,2 bx and

fg brecciated pale green andesite, w var content of black apha matrix, mostly silica, w loc cm zones of mm py, loc cm and dykes. Intensity & % of brecciarion var w mm to decim cm and ang to rounded frag. Loc and is massive over cm to decim scale

93,2 97,7 4,5 and massive fg-mg pale green grey andesite w loc fg heterogeneities

97,7 99,9 2,2 porphyry mg ± hetero porphyry pale grey dyke

99,9 102,55 2,65 and fg-mg hom pale green and

102,55 105,3 2,75 bx andfg-mg pale grey-green hetero bx and w 2-3% leuco matrix, mm fragmentation of unit, w 1-2% diss mm py, w 1 cm qz-hem v 15 to CA

105,3 106,4 1,1 dyke meso-melano int fg-mg hom dyke106,4 106,9 0,5 ctcl mg epi ctcl zone, 30 to

106,9 110,1 3,2 andprob fg hetero and w colour var from pale green to med grey, w minor mm qz v 20 to CA & cm silicified zone w minor epi & sub-mm py 30

110,1 114,55 4,45 int dyke pale green fg hom massive int dyke114,55 117,1 2,55 int dyke idem prev unit, grey-yellowish, w 5% diss mm epi117,1 118,25 1,15 porphyry fg grey-yellow hom epi-porphyry dyke118,25 121,15 2,9 dyke fol hom pale grey-green fg dyke 40121,15 123,2 2,05 dyke fol more hetero fg med-grey green dyke 20

123,2 127,7 4,5 bx & massive andfg to mg pale green bx (20%) & massive (80%) and w much less brecciation than upper unit, mx only 2% of unit dark to meg grey, apha, loc cm assimil and fragments, loc fol 40 to CA 40

127,7 138,75 11,05 massive and massive, fg hom pale to med green and w 3% sub-mm to mm chlo phX138,75 140,35 1,6 fol and idem , fg-mg fol and same comp as prev unit, 40 to CA 40140,35 142,3 1,95 massive and idem 138.75 w no chlo142,3 145,6 3,3 fol and fg-mg fol and, 40 to CA, w loc cm massive zones, loc mm pl-epi banding 40

145,6 149,1 3,5 mafic tufffg & mg dark grey hetero mafic tuff or volcanogenic sed w loc sed textures & loc cm zones w 10% chlo phX

149,1 151,3 2,2 int tuff same kind of volc sed unit int comp w 5% mm chlo phX & .5% sub-m,m diss py, loc cm fol zones 50

151,3 166 14,7 wek fol andweak fol fg to mg pale green hetero and w loc .5% mm euh py, w loc massive cm zones, w cm pl-epi-rich zones 45

166 181,4 15,4 bx massive and

fg to mg hetero pale green massive and w loc bx w decim sub-rounded frag in dark green fg matrix showing litho copntinuity w paler massive and (photos), loc decim fol zones (169-170m), w 3 1-2 cm qz-pl submyl qz v 40-60 to CA 40

181,4 198 16,6 massive andsame and unit continuous into pale green fg hom and, loc fol over decim zones, tr of brecciation, loc mg hom text, w sub-mm chlo phX 40

198 205 7 massive & bx andsame unit w diffuse brecciation, cm frag of same litho w % matrix, 2% of sub-mm qz sw, loc fol anmd finely transposed over decim zones 40

205 271,35 66,35 massive and

same and unit pale green, loc mesocratic fg hom & hetero and, loc fol over decim zones, loc decim brecciation w mm & cm rounded frag of pale to med green colour, loc mg hom text, w sub-mm chlo phX & loc mm white pl phX 35

271,35 274,9 3,55 int porphyrymg hom pale purple chlo porphyry w diss py -.5%, w vfg chill margin at upper contact & mm chlo phX 10%

274,9 277 2,1 SZ SZ in mg hom pale green and w 2% mm qz-clo v // SZ 40277 294 17 massive and more massive mg pale green and w loc decim paler zones (increase of pl conc)

294 302 massive & bx and

same and unit pale green, loc mesocratic fg hom & hetero and, loc fol over decim zones, loc decim brecciation w mm & cm rounded frag of pale to med green colour, loc mg hom text, w sub-mm chlo phX & loc mm white pl phX

302 EOH

Second Lithology

From To L Id rock types, grain size, etc. CA Photo

39 43,8 4,8 bx and high brecc and w 20% aph black mx, mm to cm rouded to sud-ang frag

45,9 46,3 0,4 and dyke fg, hom int dyke

50,5 50,8 0,3 dyke fg, hom int dyke 1

51,45 51,85 0,4 SZ mm shear zone in and w 5 cm breecia zone w 40% aph mx

68 69 1 bx and sub-mm diss py, .2%

74,8 75,65 0,85 bx andbreccia w 5% aph black Si matrix, 35% mm pl-qz sub-rounded fraction & 50% med gret rounded 1-2 cm fragments

73,4 bx photo bx crosscutting andesite 1

70,6 bx photo bx crosscutting andesite 195,35 95,6 0,25 mafic dyke fg hom dark grey dyke96,4 96,7 0,3 felsic dyke fg hom pale grey felsic dyke w 2% mm white phX84,5 bx and photos breccia 3166 mafic dyke 2 cm wide fg hom mafic dyke 50170 mafic dyke 3 cm wide fg hom mafic dyke 40219,2 219,5 mg-cg and mg yto cg pale green massive and w 5% mm pl white phX245 bx photo bx ds hetero fg-mg pale green and285 285,2 int porph idem main unit contact 40 to CA289,15 289,35 int porph idem main unit contact 30 to CA

Depth

Structure Photo

From To L Id % fractures, shear, ctcl, mylt CA Qz Cal Epi Ser Py

51,45 51,85 0,4 bx andmm shear zone in and w 5 cm breecia zone w 40% aph mx, w 4 cm qz v at upper contact, ser alt in the first 15 cm of sz 35 3 5 1

63,1 bx and 20 cm of sheared andesite 40

68,8 69,65 bx and 3% mm-1 cm qz v CA 15-40, w minor epi 15-40 3 1

73 74 bx and 5% mm- 5cm qz v 0-40 5

90,5 91,5 2 2cm qz-pl v 10 2

100,9 101 dyke hom int f dyke

103,9 v qz 2 cm 50

104,5 v qz-pl 2 cm 50

110,1 114,55 3-1 cm pl-qz v w 1 cm alt halo 15

114,5 115,1 qz v 30% massive qz v loc 1 cm vein 20 to CA 20123 123,2 pl-qz 50% veining fg to vfg ctcl pl-qz-epi v 50138,75 139,5 qz-cal v 5% mm qz-cal v // to fol & 50-60 40144,75 144,9 qz sz 50% protomyl qz-pl veining w mm chlo 60146,1 146,3 qz-pl 3 cm real w qz-pl v w sub myl text 20150,7 151,05 qz v 30% qz-chlo-pl veining w var ang to CA161,8 162,25 qz v 60% qz-chlo v // to CA & 1 cm wide SZ 30 to CA 0

182 183,05fol zone 40 to CA w 1 2 cm qz-pl v // to fol w 3 cm wide pale grey hom aph Si-zone 40

191,2 191,5 qz v 20% qz v (2 cm) w some chlo conc 0210,35 210,8 qz v 20% qz v (1-3 cm) w mm chlo conc 25211,3 qz v 2-4 cm qz v & conc w chlo 20222,7 223 SZ fine lam sz or transposed zone w 2 mm qz v at contact 35228,1 229 pl-qz zone in the first 30 cm & mm qz v // to main fol 40233,6 aph Si 5 cm aph pale grey Si-zone w mm qz-pl v at lower contact 35235,6 237,5 SZ mm banded sz in ± hom pale green and 35248,75 qz v 2 cm qz v w chlo conc 20 to CA cutting a 2 cm qz-pl SZ 40 to CA 20250 qz v 3 cm qz v 20250,9 251,05 pl conc 5 cm pl-qz-chlo v w 2 cm qz v at lower contact 40 to CA 25256,2 pl conc 4 cm pl-qz v 40260,85 261,45 cal-qz sw cal-qz sw w mm veining 15% in brecciated and fol zone w 2% mm euh py 40262,4 262,6 pl-qz v 2 cm pl-qz v 30% w mm cal v 30269,1 3 cm cm ang breccia w qz-cal mx293,2 pl v 7 cm pl-qz v w chlo, 60 to CA 60293,6 pl v 7 cm pl-qz v w chlo, 60 to CA w sub-myl text 60293,8 295,5 qz & pl v 7% cm qz v 20 to CA, w 5 & 15 cm pl-qz v ± brecciated or protomyl299,4 pl v 2 cm vfg aph pl-qz v 50300,55 pl v 2 cm sub-myl pl-qz v 80300,7 pl v 2 cm sub-myl pl-qz v 80

Depth Veins(%)

Alteration (1-5) Pervasive Alteration (%) Frac-control

From To L Id Description Chl Epi Ser Alb Si Chl Epi Alb Qtz-Cal

39 57,9 18,9 bx and brecc and w limited chlo-ser alt

Depth


From To L Id Py Cpy Po

149,1 151,3 2,2 int tuff sub-mm diss py 0,50%

Sample resultsNo. From To L Au Ag38233 102,55 103,6 1,0538234 149,15 150,4 1,2538235 150,4 157,3 6,9

Logged by : AC Sheet of

Box# From To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 39 42,7 3,7 3,4 92% 1,75 47% 39 41,82 42,7 46,5 3,8 3,6 95% 2,6 68% 42,8 43,553 46,5 50,3 3,8 3,6 95% 3,25 86% 53 53,854 50,3 53,85 3,55 3,35 94% 2,45 69% 63,9 64,25 53,85 57,9 4,05 4,05 100% 3,85 95% 156 56,26 57,9 62 4,1 4,1 100% 3,7 90% 156,6 156,87 62 66,15 4,15 4,1 99% 3,25 78% 212,4 212,758 66,15 69,9 3,75 3,7 99% 3,2 85%9 69,9 74,3 4,4 4,4 100% 4,2 95%10 74,3 78,25 3,95 3,9 99% 3,6 91%11 78,25 82,6 4,35 4,35 100% 4,25 98%12 82,6 86,3 3,7 3,7 100% 3,5 95%13 86,3 90,4 4,1 4,1 100% 3,85 94%14 90,4 94,7 4,3 4,3 100% 4,2 98%15 94,7 98,8 4,1 4,1 100% 3,9 95%16 98,8 102,1 3,3 3 91% 1,7 52%17 102,1 106,1 4 4 100% 3,95 99%18 106,1 110,4 4,3 4,2 98% 3,25 76%19 110,4 114,55 4,15 4,1 99% 3,75 90%20 114,55 118,5 3,95 3,95 100% 3,5 89%21 118,5 122,6 4,1 4,1 100% 3,7 90%22 122,6 127 4,4 4,4 100% 4,3 98%23 127 131,2 4,2 4,15 99% 3,9 93%24 131,2 135,3 4,1 4,1 100% 3,95 96%25 135,3 139,7 4,4 4,4 100% 4,35 99%26 139,7 143,75 4,05 4,05 100% 3,95 98%27 143,75 147,8 4,05 4,05 100% 3,8 94%28 147,8 151,9 4,1 4,1 100% 4 98%29 151,9 156 4,1 4,1 100% 3,75 91%30 156 160,25 4,25 4,15 98% 3,65 86%31 160,25 164,6 4,35 4,35 100% 4,25 98%32 164,6 168,6 4 4 100% 3,85 96%33 168,6 172,8 4,2 4,2 100% 3,95 94%34 172,8 177 4,2 4,2 100% 4 95%35 177 181,4 4,4 4,4 100% 3,6 82%36 181,4 185,25 3,85 3,8 99% 2,7 70%37 185,25 189,5 4,25 4,25 100% 4,05 95%38 189,5 193,7 4,2 4,2 100% 4,2 100%39 193,7 197,85 4,15 4,15 100% 3,85 93%40 197,85 202,2 4,35 4,35 100% 4,05 93%41 202,2 206,2 4 4 100% 3,8 95%42 206,2 210,2 4 4 100% 3,3 83%43 210,2 214,3 4,1 3,9 95% 2,9 71%44 214,3 218,4 4,1 4,1 100% 3,85 94%45 218,4 222,6 4,2 4,2 100% 4 95%46 222,6 226,9 4,3 4,3 100% 4,2 98%47 226,9 231,25 4,35 4,35 100% 4,25 98%48 231,25 235,2 3,95 3,95 100% 3,85 97%49 235,2 239,3 4,1 4,1 100% 3,55 87%50 239,3 243,6 4,3 4,3 100% 4,2 98%

Geotechnical Log Hole No. :C08-19Date : Feb 1 10


51 243,6 246,3 2,7 2,7 100% 2,55 94%52 246,3 251,1 4,8 4,8 100% 4,8 100%53 251,1 256,3 5,2 5,2 100% 5,2 100%54 256,3 260,5 4,2 4,2 100% 4,2 100%55 260,5 264,65 4,15 4,15 100% 4,15 100%56 264,65 268,85 4,2 4,2 100% 3,95 94%57 268,85 273,05 4,2 4,1 98% 4 95%58 273,05 277,1 4,05 4,05 100% 3,2 79%59 277,1 281,2 4,1 4,1 100% 3,7 90%60 281,2 285,6 4,4 4,4 100% 4,35 99%61 285,6 290 4,4 4,4 100% 4,2 95%62 290 293,8 3,8 3,8 100% 3,5 92%63 293,8 297,9 4,1 4,1 100% 3,8 93%64 297,9 302 4,1 4,1 100% 4,1 100%65 302 EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC08-19 L-2200E 2050N 300 0 -50 302m 24/02/2009 28/02/2009 MP 01/02/2010

Princ LithologyFrom To L Id rock type Photo

39 101,7 62,7 bx and fg brecciated pale green andesite, w var content of black apha matrix, mostly silica, w loc cm zones of mm py, loc cm and dykes. Intensity of brecciarion var w mm to cm and ang to rounded frag

101,7 107 5,3 lost description

107 136,7 29,7

136,7 140,7 4

140,7 143,55 2,85

143,6 298,1 154,5297,5 302 4,5

302 302 0 E.O.H End Of Hole

DDH Depth


39 43,8 bx and high brecc and w 20% aph black mx, mm to cm rouded to sud-ang frag

45,9 46,3 and dyke fg hom int dyke

50,8 50,5 dyke fg, hom int dyke 1

51,45 51,85 SZ mm shear zone in and w 5 cm breecia zone w 40% aph mx

lost description

Depth

Depth Structure Veins(%) PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal

40,7 101,7 61 Black Schist Some crushed core. Poorly fractured. Most of the fx are filled by clear cal. Locally banding.

1--2 1--2

101,7 107 5,3 Feldspar porphyry

Feldspar porphyry. Light grey. Highly crushed core. Porphyritic texture. 30-40% coarse plagioclase fld. Some of the fld are slightly epidotized(light greenish). Very fine matrix. Some tiny holes and cavities.

0 0

108,8 111,4 2,6 Int vol dyke Int volc dyke. Gradual upper contact, sharp lower contact(40*). Dark grey. Fine grained. Moderately silicified in the upper part. Porphyritic texture. A few coarser(med grained) mafic minerals. Some filled fractures(mostly by cal with qz traces). Some small py cubes

1 1

113,6 113,8 0,2 Int vol dyke Altered volc dyke. Clear color. Light greenish-grey. Sharp upper and lower contacts of 30*. Porphyritic texture; 10% mafic fine grains partially turned into chlorite. Aphanitic altered groundmass(epidotized). Numerous small py grains.(up to 10%)

0 0

114,2 114,3 0,1 Qz-cal vein 10cm thick amophous qz vein. Cuts the host schist sharply(30*). Some calcite filling tiny fx. Some py at the margins of the vein. The margins are slightly sheared.

97 3

114,4 114,6 0,2 Int vol dyke Altered volc dyke. Clear color. Light greenish-grey. Sharp upper and lower contacts of 40*. Aphanitic texture. Silicified and epidotized matrix. A white cm amorphous qz vein and a cm light greyish qz vein with some cal traces. A few tiny fx filled by cal. Some py small cubes at the margins of the vn.

5 15

119,75 119,95 0,2 Int vol dyke Altered and sheared int volc dyke. Cuts the host rock sharply(40* upper and lower contacts). Epidotized fine grained matrix. Dark altered minerals forming fabics. A few filled fx(by clear cal-qz). Some py small cubes.

0 2

120 121,3 1,3 Black Schist Highly fractured zone. Numerous mm fx filled by clear cal. Some crushed core.

0 10

121,4 124,3 2,9 Int vol dyke Int volc dyke. Gradual upper contact, sharp lower contact(40*). Dark grey. Fine grained. Locally porphyritic texture. Some filled mm fractures(by cal with qz traces). Some small py cubes. A few small py patches. Calcified matrix where level of fracturation is higher.

1 1--2

125,5 125,6 0,1 Int vol dyke Altered and sheared int volc dyke. Cuts the host rock sharply(50* upper and lower contacts). Epidotized fine grained matrix. Dark altered(chloritized) minerals forming foliations(50*/ca). A mm fx filled by cal. A few py small cubes.

0 0

184,4 191 6,6 Int Volc Brecciated zone showing some sulphides. Dark color. Numerous coarse angular clasts. Altered aphanitic dark matrix. Py po patches. Silicified groundmass. A few fx filled by clear cal-qz.

1--2 2--3

204,2 205,1 0,9 Int Volc Brecciated zone. A few py patches and small grains. Dark aphanitic chloritized matrix. A few filled fx.

1 1--2

248,5 259,6 11,1 Int Volc Altered, locally brecciated and sheared zone. Greenish grey aphanitic chloritized matrix. Locally moderately silicified and calcified. Poorly fractured. A few cal-qz veinlets and filled fx.

1 1

277 285 8 Int volc Sheared and locally brecciated int volcanics cut by a few volc dykes (most of the contacts of the dykes are sharp, the thickest dyke is less than half a meter). Silicified and chloritized greenish aphanitic matrix. Fabrics

1 1

From To L Id Description Serp Asb Chl Epi Alb Si Serp Asb Chl Epi Alb Qtz-Cal40,7 107 66,3 Schist Nearly unaltered black shist. A few fractures filled by clear cal with

some qz locally. 0-1 1--2

113,6 113,8 0,2 Int vol dyke

Altered volc dyke. Clear color. Light greenish-grey. Sharp upper and lower contacts of 30*. Porphyritic texture; 10% mafic fine grains partially turned into chlorite. Aphanitic altered groundmass(epidotized). Numerous small py grains.(up to 10%)

1 1 1 0

114,4 114,6 0,2 Int vol dyke

Altered volc dyke. Clear color. Light greenish-grey. Sharp upper and lower contacts of 40*. Aphanitic texture. Silicified and epidotized matrix. A white cm amorphous qz vein and a cm light greyish qz vein with some cal traces. A few tiny fx filled by cal. Some py small cubes at the margins of the vn.

1--2 1--2 1 1--2

119,75 119,95 0,2 Int vol dyke

Altered and sheared int volc dyke. Cuts the host rock sharply(40* upper and lower contacts). Epidotized fine grained matrix. Dark altered minerals forming fabics. A few filled fx(by clear cal-qz). Some py small cubes.

1 1 1

120 121,3 1,3 Black Schist

Highly fractured zone. Numerous mm fx filled by clear cal. Some crushed core.

0 1--2

125,5 125,6 0,1 Int vol dyke

Altered and sheared int volc dyke. Cuts the host rock sharply(50* upper and lower contacts). Epidotized fine grained matrix. Dark altered(chloritized) minerals forming foliations(50*/ca). A mm fx filled by cal. A few py small cubes.

1 1--2

134,3 135 0,7 Int vol dyke

Intermed volc dyke. Sharp upper and lower contacts(45*). Light grey color. Poorly fractured. Fine grained. Aphanitic matrix. Porphyritic texture: some fine mafic minerals(a few percent). Some mm fx filled by cal, dark chlorite. The margin of the dyke is sheared and highly

1 1--2

143,3 158,7 15,4 Int Volc Altered and mineralized zone. Sulphides rich. The rock is mod-strongly silicified and show numerous coarse py patches. Massive py zones (up to 30cm thick). Some coarse pyrrhotite patches. Fractured and brecciated zones. Most of the fx are filled by clear cal. A few filled by sulphides.

1--2 3--4 1--2

248,5 259,6 11,1 Int Volc Altered and locally sheared zone. Greenish grey aphanitic chloritized matrix. Locally moderately silicified and calcified. Poorly fractured. A few cal-qz veinlets showing locally some sulphides

2--3 1--2 1

277 285 8 Int volc Altered sheared and locally brecciated int volcanics cut by a few volc dykes (most of the contacts of the dykes are sharp, the thickest dyke is less than half a meter). Silicified and chloritized greenish aphanitic matrix.

1--2 2--3 0.5-1


No. From To L Au Ag Co Cu Ni Pb Zn38169 43,8 44,8 1 < 0.01 0,2 0,002 0,006 0,009 0,001 0,02238170 44,8 46,1 1,3 < 0.01 0,2 0,003 0,008 0,008 0,001 0,02638171 49,6 50,9 1,3 < 0.01 0,2 0,003 0,003 0,013 < 0.001 0,00938172 53,2 54 0,8 < 0.01 0,2 0,002 0,004 0,008 < 0.001 0,01638173 55,6 56,5 0,9 < 0.01 0,2 0,002 0,005 0,006 0,001 0,02238174 59,1 60,1 1 < 0.01 0,2 0,002 0,007 0,007 0,001 0,02238175 62,5 63,1 0,6 < 0.01 0,2 0,001 0,002 0,003 < 0.001 0,00838176 82,7 83,6 0,9 < 0.01 0,2 0,002 0,005 0,009 < 0.001 0,01738177 83,6 84,9 1,3 < 0.01 0,2 0,002 0,006 0,007 < 0.001 0,02238178 91,8 92,8 1 < 0.01 0,2 0,003 0,005 0,011 0,001 0,02538179 92,8 93,8 1 < 0.01 0,2 0,003 0,006 0,011 0,001 0,02638180 93,8 95 1,2 < 0.01 0,2 0,002 0,005 0,008 < 0.001 0,01938181 113,4 113,9 0,5 < 0.01 0,2 0,002 0,005 0,008 < 0.001 0,00938182 113,9 115 1,1 < 0.01 0,3 0,002 0,009 0,01 0,003 0,03438183 116 117 1 0,07 0,4 0,004 0,021 0,015 0,005 0,11738184 118 119 1 0,07 0,4 0,003 0,014 0,011 0,004 0,06538185 119 119,9 0,9 0,07 0,3 0,003 0,016 0,015 0,004 0,08138186 122,1 123,5 1,4 0,02 0,2 0,001 0,002 0,002 < 0.001 0,01238187 123,5 124,9 1,4 0,05 0,2 0,001 0,006 0,005 0,002 0,0338188 124,9 126,2 1,3 0,07 0,2 0,002 0,008 0,008 0,002 0,04338189 126,2 127,5 1,3 0,04 0,2 0,001 0,003 0,004 0,002 0,02338190 127,5 128,8 1,3 0,09 0,4 0,003 0,013 0,01 0,004 0,05838191 Stand 15Pa 1,05 0,2 0,003 0,005 0,012 < 0.001 0,00838192 Stand 6Pc 1,53 0,2 < 0.001 0,003 0,003 0,002 0,00538193 Blank sample 0,02 0,2 0,003 0,015 0,003 < 0.001 0,0138194 143,3 143,8 0,5 0,31 2 0,007 0,006 0,007 0,005 0,00638195 143,8 145 1,2 0,05 0,2 0,004 0,003 0,01 0,001 0,00538196 145 146 1 0,04 0,2 0,006 0,002 0,011 0,001 0,00738197 146 147,4 1,4 0,05 0,2 0,003 0,001 0,009 < 0.001 0,00738198 147,4 148,8 1,4 0,13 0,2 0,007 0,003 0,01 0,002 0,00638199 148,8 150,2 1,4 0,06 0,2 0,003 0,003 0,011 < 0.001 0,00538200 150,2 151,6 1,4 0,03 0,2 0,002 0,005 0,011 < 0.001 0,00638201 151,6 153 1,4 0,03 0,2 0,002 0,003 0,01 0,001 0,00538202 153 154,4 1,4 < 0.01 0,2 0,006 0,005 0,013 0,003 0,00638203 154,4 155,8 1,4 0,06 0,2 0,007 0,002 0,013 0,003 0,00538204 155,8 157,2 1,4 0,06 0,2 0,007 0,004 0,015 0,005 0,00638205 157,2 158,6 1,4 0,05 0,2 0,003 0,004 0,011 0,001 0,00638206 158,6 160 1,4 0,05 0,7 0,005 0,042 0,036 0,002 0,00538207 160 160,8 0,8 0,02 0,2 < 0.001 0,002 0,017 < 0.001 0,00838208 165 165,9 0,9 0,03 0,2 0,002 0,002 0,015 < 0.001 0,00538209 165,9 166,9 1 0,03 0,2 0,002 0,002 0,013 0,001 0,00438210 169,7 171 1,3 0,06 0,2 0,004 0,006 0,012 0,002 0,00838211 171 172,1 1,1 < 0.01 0,2 0,004 0,005 0,012 0,001 0,01238212 172,1 173,4 1,3 < 0.01 0,2 0,003 0,007 0,012 < 0.001 0,01438213 173,4 174,8 1,4 < 0.01 0,2 0,002 0,005 0,012 < 0.001 0,011

Sample results

38214 Stand 15Pa 0,96 0,2 0,003 0,006 0,011 < 0.001 0,00838215 Stand 6Pc 1,57 0,2 < 0.001 0,004 0,003 0,002 0,00538216 Blank sample 0,04 0,2 0,002 0,014 0,003 < 0.001 0,0138217 174,8 176,2 1,4 0,04 0,2 0,002 0,005 0,011 < 0.001 0,0138218 176,2 177,4 1,2 0,04 0,2 0,003 0,005 0,012 < 0.001 0,0138219 177,4 178,4 1 0,04 0,2 0,003 0,005 0,011 < 0.001 0,01538220 179,7 181,1 1,4 0,04 0,2 0,003 0,005 0,012 < 0.001 0,01538221 181,1 181,6 0,5 0,04 0,2 0,002 0,004 0,012 < 0.001 0,01238222 184,1 185,4 1,3 0,04 0,2 0,002 0,005 0,012 < 0.001 0,0238223 185,4 186,4 1 0,03 0,2 0,002 0,004 0,011 < 0.001 0,0138224 186,4 187,6 1,2 0,04 0,2 0,002 0,005 0,011 < 0.001 0,01138225 187,6 188,3 0,7 0,04 0,2 0,002 0,003 0,011 < 0.001 0,00938226 188,3 189,2 0,9 0,04 0,2 0,002 0,004 0,011 < 0.001 0,01138227 189,2 190,6 1,4 0,03 0,2 0,002 0,005 0,012 < 0.001 0,01538228 190,6 191,2 0,6 0,03 0,2 0,002 0,006 0,012 < 0.001 0,01338229 192,5 193,5 1 0,02 0,2 0,003 0,005 0,012 < 0.001 0,01238230 204,2 205,1 0,9 0,02 0,2 0,002 0,006 0,011 < 0.001 0,0138231 242,8 243,3 0,5 0,01 0,2 0,002 0,001 0,013 < 0.001 0,00638232 262,7 263,2 0,5 < 0.01 0,2 0,002 0,003 0,013 0,003 0,012

Geotechnical LogDate :27-01-10Logged by : MP Sheet of

Box number From To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 40,7 44,1 3,4 3,34 98% 2,6 76%2 44,1 47,9 3,8 3,7 97% 3,3 87%3 47,9 51,6 3,7 3,59 97% 3,5 95%4 51,6 55,6 4 3,9 98% 3,84 96%5 55,6 59 3,4 3,2 94% 3,2 94%6 59 63,1 4,1 3,97 97% 3,77 92%7 63,1 67,4 4,3 4,12 96% 4,02 93%8 67,4 71,1 3,7 3,5 95% 3,4 92%9 71,1 74,9 3,8 3,7 97% 3 79%10 74,9 78,6 3,7 3,56 96% 2,6 70%11 78,6 81,2 2,6 2,3 88% 1,5 58%12 81,2 85,2 4 3,8 95% 3,6 90%13 85,2 89 3,8 3,7 97% 3,5 92%14 89 93 4 3,9 98% 3,8 95%15 93 96,9 3,9 3,83 98% 3,7 95%16 96,9 100 3,1 3,01 97% 2,6 84%17 100 103 3 3 100% 0,25 8%18 103 106 3 2,9 97% 0,36 12%19 106 109,75 3,75 3,6 96% 1,6 43%20 109,75 113,2 3,45 3,34 97% 3,2 93%21 113,2 117,5 4,3 4,21 98% 3,92 91%22 117,5 121,3 3,8 3,75 99% 3,63 96%23 121,3 125,4 4,1 4,02 98% 3,87 94%24 125,4 129,2 3,8 3,8 100% 3,6 95%25 129,2 133 3,8 3,76 99% 3,56 94%26 133 137 4 4 100% 2,7 68%27 137 141,3 4,3 4,32 100% 4,3 100%28 141,3 144,9 3,6 3,45 96% 2,07 58%29 144,9 149 4,1 4,15 101% 4,15 101%30 149 153,2 4,2 4,2 100% 4,2 100%31 153,2 157,3 4,1 4 98% 4 98%32 157,3 161,5 4,2 4,2 100% 4,2 100%33 161,5 165,8 4,3 4,23 98% 4,1 95%34 165,8 170 4,2 4,2 100% 4,2 100%35 170 174,2 4,2 4,2 100% 4,18 100%36 174,2 178,6 4,4 4,38 100% 4,38 100%37 178,6 182,8 4,2 4,2 100% 4,2 100%38 182,8 187,1 4,3 4,27 99% 4,27 99%39 187,1 191,3 4,2 4,2 100% 4,2 100%40 191,3 195,3 4 4 100% 3,98 100%41 195,3 199,4 4,1 4 98% 3,67 90%42 199,4 203,3 3,9 3,87 99% 3,7 95%43 203,3 207,6 4,3 4,27 99% 4,24 99%44 207,6 211,8 4,2 4,2 100% 4,14 99%45 211,8 215,7 3,9 3,9 100% 3,9 100%46 215,7 219 3,3 3,2 97% 2,9 88%47 219 223 4 4 100% 4 100%48 223 227,2 4,2 4,2 100% 4,2 100%49 227,2 231,5 4,3 4,3 100% 4,3 100%50 231,5 235,75 4,25 4,23 100% 4,23 100%51 235,75 239,7 3,95 3,9 99% 3,67 93%52 239,7 243,4 3,7 3,7 100% 3,6 97%

Hole No. :C08-19


53 243,4 247,3 3,9 3,87 99% 3,87 99%54 247,3 251,3 4 4 100% 4 100%55 251,3 255,75 4,45 4,3 97% 4,25 96%56 255,75 259,8 4,05 4 99% 4 99%57 259,8 263,55 3,75 3,73 99% 3,56 95%58 263,55 268 4,45 4,3 97% 4,3 97%59 268 272,2 4,2 4,2 100% 4,2 100%60 272,2 276,4 4,2 4,2 100% 4,17 99%61 276,4 280,6 4,2 4,2 100% 4,17 99%62 280,6 284,8 4,2 4,2 100% 4,2 100%63 284,8 289,2 4,4 4,3 98% 4,3 98%64 289,2 293,5 4,3 4,3 100% 4,3 100%65 293,5 298,2 4,7 4,7 100% 4,7 100%66 298,2 302 3,8 3,8 100% 3,8 100%

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC08-20 L-2100E 1850N 300 0 -50 300m 03/03/2009 10/03/2009 MP 17-22 Jan 2010

Princ LithologyFrom To L Id rock type Photo22 86,5 64,5 And Intermed volcanics. Light grey locally darker grey. Locally

brecciated. Aphanitic matrix. Locally porphyritic texture with some clear pl fld. Weakly fractured (filled by cal-qz). Altered: chloritized dark groundmass. Some dark chl stringers. Silicified. Some pyrite. A few po patches.

86,5 121,5 35 And Intermed volcanics. Dark greenish-grey. Locally brecciated and mod sheared. Aphanitic matrix. Locally porphyritic texture with some clear pl fld. Weakly fractured (filled by cal-qz). Altered: chloritized dark groundmass. Locally some med to coarse angular qz grains, some a smaller and flat(fabrics). Silicified. Some sulphides as py cubes and a few po patches located in the brecciated and more fractured zones.

121,5 149 27,5 And Intermed vocanic. Light grey. Altered. Locally mod fractured. Aphanitic matrix. Locally silicified. Weakly sheared on some spots. Quite homogenous in terms of grain size. Some sulfides forming patches.

149 161,7 12,7 Schist Black shist. Locally graphitic. Very dark grey to black. Very fine grained. Locally sheared. Some sulfides following foliations(40*). A few fx filled by cal-qz. Gradual contact with the volcanics above. Py nodules and cubes. Some crushed core around 161m deep.

161,7 166,5 4,8 And Intermed volcanics dyke. Light grey. Fine grained. Gradual upper contact. Sharp lower contact(40*). Poorly fractured. Fx filled by cal-qz. Some mm to cm py cubes (2--3%). Locally bleached and weakly altered. Slightly sheared close to the contacts.

166,5 217,3 50,8 Schist Black shist. Locally graphitic. Very dark grey to black. Very fine grained. Aphanitic texture. Locally sheared and highly fractured. Some sulfides locally forming beds and following banding. Fx filled by cal-qz. Gradual contact with the volcanics above. Py nodules and cubes. Some crushed core from 167 to 171m deep. Some altered vol dykes containing some py cubes cutting the host rock sharply.

217,3 220 2,7 Int-felsic VolcIntermed to felsic volcanic dyke. Light grey. Fine grained. Gradual upper contact. Sharp lower contact(40*). Poorly fractured. Fx filled by cal-qz. Some mm to cm py cubes (2--3%). Locally bleached and weakly altered. Slightly sheared close to the contacts.

DDH Depth

220 234,5 14,5 Schist Black shist. Locally graphitic. Very dark grey to black. Very fine grained. Aphanitic texture. Locally sheared and highly fractured. Some sulfides locally forming beds and following foliations. Fx filled by cal-qz. Gradual contact with the volcanics above. Py nodules and cubes.

234,5 299 64,5 And Intermed volcanics. Grey to dark grey. Aphanitic matrix. Locally weakly altered by chl. Poorly fractured. Some fx filled by chl, cal-qz. Mm to cm qz veins. Clear cal-qz vnl. Locally porphyritic texture with some clear pl fld. Some silicified parts. 1-3% py.

299 299 0 E.O.H End Of Hole.

Second Lithology From To L Id rock types, grain size, etc. Photo23,8 28,8 5 And Volc altered breccia. Chloritized and silicified.Upper part: aphanitic dark

matrix dark greyish coarse angular clasts. Some py stringers. Po small patch. Lower part: clearer greyish chloritized matrix coarse angular altered clasts. Some clasts are flat Flow pattern. Some py po

39,8 49,4 9,6 And Volc altered breccia. Chloritized and silicified. Coarse greyish chloritized clasts in a very dark grey aphanitic matrix. Fx filled by cal-qz. A few py grains in the groundmass.

97 121,5 24,5 And Altered volcanics. Locally brecciated. Mod fractured. Most of the fx are filled by clear cal-qz. Some sulphides. Py cubes, forming patches, filling fx or located at the margins of some vn. Mod chloritized fine matrix. Silicified.

161,7 166,5 4,8 And Intermed volcanics. Light grey. Fine grained. Gradual upper contact. Sharp lower contact(40*). Poorly fractured. Fx filled by cal-qz. Some mm to cm py cubes (2--3%). Locally bleached and weakly altered. Slightly sheared close to the contacts.

194 196,6 2,6 And Intermed volc dyke. Grey. Fine grained. 25-35% clear pl fld. Fx filled by cal-qz. Slightly altered matrix by chlorite. Some py cubes. Sharp upper and lower contacts of 35*. Weakly sheared close to the contacts.

217,3 220 2,7 Int-felsic VolcIntermed to felsic volcanic dyke. Light grey. Fine grained. Gradual upper contact. Sharp lower contact(40*). Poorly fractured. Fx filled by cal-qz. Some mm to cm py cubes (2--3%). Locally bleached and weakly altered. Slightly sheared close to the contacts.

234,5 284 49,5 And Intermed volcanics. Grey to dark grey. Aphanitic matrix. Locally moderately altered by chl. Poorly fractured. Locally brecciated. Some fx filled by chl, cal-qz. Mm to cm qz veins. Clear cal-qz vnl. Locally porphyritic texture with some clear pl fld. Some silicified parts. 1-2% py.

284 299 15 And Intermed volcanics. Grey to dark grey. Aphanitic altered matrix. Weakly altered by chl. Silicified. Poorly fractured. Some fx filled by chl, cal-qz. Mm to cm qz veins. Clear cal-qz vnl. A cal-qz vnl with some moly at 295.2m deep.

299 299 0 E.O.H End Of Hole

Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal22 35 13 And 3-5% Fx. Slightly sheared and brecciated from 24.2

to 29m deep.3 3--5

35 50 15 And A few fx filled by clear cal-qz 2--3 2--350 62 12 And Some fx filled by cal-qz. Mm to cm. Some crushed

core around 59 and 62m deep.2 2

62 71 9 And A very few fx filled by clear cal-qz 1 197,2 123 25,8 And 2-3% fx. Local small sheared zones (fabrics) 2--3 2--3

125,3 128,45 3,15 And Fractured zone. Mm to cm Fx filled by clear cal-qz 5--7 5--7

149 161,7 12,7 Schist 1--2% Fx. 40* foliations 1--2 1--2

161,7 166,5 4,8 And 1% fx filled by cal-qz. Slighly sheared at the contacts with the host rock.

1 1

166,5 217,3 50,8 Schist 1-3% fx filled by clear cal. 30-40* foliations. Some py beds following the foliations.

1--3 1--3

217,3 220 2,7 Int-felsic Volc

5-7% fx filled by clear cal-qz. 3--5 3--5

220 234,5 14,5 Schist 2--3% fx filled by clear cal-qz. 2--3 2--3234,5 299 64,5 And 1--2% fx filled by clear cal-qz. 1--2 1--2

Depth Veins(%)

From To L Id Description Serp Asb Chl Epi Alb Si Serp Asb Chl Epi Alb Qtz-Cal22 73,1 51,1 And Locally chloritized aphanitic matrix. Some epidotized

fld. Locally moderately silicified and calcified groundmass. 1--2 2 2--3

73,1 122 48,9 And Mod chloritized groundmass. Silicified locally where the core is more fractured and brecciated.

2--3 2--3121,5 149 27,5 And Intermed vocanics. Light grey. Altered. Locally mod

fractured. Aphanitic matrix. Locally silicified. Weakly sheared on some spots. Some sulfides forming patches.

2

1--2161,7 166,5 4,8 And Intermed volcanics dyke. Light grey. Fine grained.

Gradual upper contact. Sharp lower contact(40*). Poorly fractured. Fx filled by cal-qz. Some mm to cm py cubes (2--3%). Locally bleached and weakly altered. Slightly sheared close to the contacts.

1 1

166,5 217,3 50,8 Schist cal-qz filling mm to cm Fx 2217,3 220 2,7 Int-

felsic Volc

Chloritized and silicified groundmass. Cal-qz filling numerous mm-cm fx.

2 2 2--3 5234,5 284 49,5 And Weakly silicified groundmass locally. A few fx filled by

clear cal-qz. 1 1--2284 299 15 And W-mod chloritized aphanitic matrix 1--2 1 1


From To L Id Py Cpy Ars Cpy Pyrrh24,5 26 1,5 And Altered breccia showing some py patches. A few small po

patches3--5 0,1

63,7 66,5 2,8 And Altered zone. Locally brecciated. Silicified aphanitic matrix. Some pyr cubes and a few po patches.

1--2 0,1

97,2 102,7 5,5 And Py and po patches and locally filling fx. 2 1--2

109,4 121,5 12,1 And Py patches and cubes. Some po patches and locally filling fx or forming stringers.

1--2 1--2

130,6 132 1,4 And Py patche. Small po nudules or fillin some fx. 3--4 0,5134,7 136,8 2,1 And Py stingers. Po traces 1--2 0,1140,1 141 0,9 And Py 1--2144 145 1 And Py 1--3145,4 146,1 0,7 And Py 1--2147,6 149 1,4 And Py 1--3

150,3 151,1 0,8 ShistPy patches and small rounded nodules. Py forming foliations or filling with cal-qz

1--2

151,1 152 0,9 ShistPy patches and small rounded nodules. Py forming foliations or filling with cal-qz

1--2

152 153,2 1,2 ShistPy patches and small rounded nodules. Py forming foliations or filling with cal-qz

1--3

161,7 166,5 4,8 Shist Py cubes. Mm-cm. 2--3197 217 20 Shist py stringers and forming well rounded coarse stains with

clear cal traces around. Some py forming beds and parallel to the foliations. Some py inside the fx filled by cal-qz.

2--3

222 224,3 2,3 Shist Nods of py. Py bands. 3--4231 235,5 4,5 Shist Py coarse patches 3--4236,8 237,8 1 And Mm py cubes. 2248 249,3 1,3 And Py 1--2252,4 253,1 0,7 And Py 1266,4 267,8 1,4 And Py 1--2267,8 269 1,2 And Py 1270,8 271,9 1,1 And Py 1274,3 274,9 0,6 And Py 0,5294,6 295,3 0,7 And Py traces. Mo 0,5


No. From To L Id Au Ag Co Cu Ni Pb Zn38056 24,5 25,1 0,6 And < 0.01 0,2 0,002 0,004 0,011 < 0.001 0,01138057 25,1 26 0,9 And < 0.01 0,2 < 0.001 0,005 0,009 0,001 0,0138058 63,7 65,1 1,4 And < 0.01 0,2 < 0.001 0,005 0,011 0,002 0,00838059 65,1 66,5 1,4 And 0,01 0,2 0,002 0,005 0,011 < 0.001 0,00738060 97,2 98,2 1 And < 0.01 0,2 0,003 0,008 0,017 0,001 0,0138061 98,2 99 0,8 And < 0.01 0,2 0,002 0,005 0,013 < 0.001 0,0138062 99 100 1 And < 0.01 0,2 < 0.001 0,003 0,011 0,001 0,00938063 100 101,4 1,4 And < 0.01 0,2 0,001 0,005 0,012 < 0.001 0,00838064 101,4 102,7 1,3 And < 0.01 0,2 0,002 0,006 0,013 < 0.001 0,01138065 109,4 110,8 1,4 And 0,01 0,2 0,001 0,004 0,01 < 0.001 0,01138066 110,8 112 1,2 And < 0.01 0,2 0,002 0,005 0,011 < 0.001 0,0138067 112 113 1 And < 0.01 0,2 < 0.001 0,004 0,011 < 0.001 0,0138068 113 114,4 1,4 And < 0.01 0,2 < 0.001 0,004 0,011 < 0.001 0,0138069 114,4 115,4 1 And < 0.01 0,2 < 0.001 0,003 0,011 < 0.001 0,0138070 115,4 116,8 1,4 And 0,01 0,2 < 0.001 0,004 0,012 0,001 0,0138071 116,8 117,3 0,5 And 0,02 0,2 0,002 0,011 0,015 < 0.001 0,01138072 117,3 118,7 1,4 And 0,01 0,2 0,001 0,004 0,011 < 0.001 0,0138073 118,7 120,1 1,4 And < 0.01 0,2 0,002 0,006 0,012 0,001 0,00938074 120,1 121,5 1,4 And 0,01 0,2 0,002 0,005 0,012 0,001 0,0138075 130,6 132 1,4 And < 0.01 0,2 0,007 0,008 0,016 < 0.001 0,00838076 134,7 135,5 0,8 And < 0.01 0,2 0,004 0,008 0,014 0,001 0,02338077 135,5 136,8 1,3 And < 0.01 0,2 0,003 0,003 0,012 < 0.001 0,0138078 Stand 15Pa 1,02 0,2 0,003 0,006 0,011 < 0.001 0,00738079 Stand 6Pc 1,55 0,2 < 0.001 0,004 0,003 0,001 0,005

38080 Blank sample < 0.01 0,2 0,003 0,015 0,003 < 0.001 0,0138081 140,1 141 0,9 And < 0.01 0,2 0,003 0,005 0,011 < 0.001 0,01138082 144 145 1 And < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00838083 145,4 146,1 0,7 And < 0.01 0,2 0,003 0,006 0,012 < 0.001 0,0138084 147,6 149 1,4 And < 0.01 0,2 0,003 0,003 0,008 < 0.001 0,00838085 150,3 151,1 0,8 And < 0.01 1,2 0,005 0,025 0,014 0,006 0,13338086 151,1 152 0,9 Schist 0,01 0,6 0,005 0,037 0,016 0,004 0,21138087 152 153,2 1,2 Schist < 0.01 0,5 0,005 0,045 0,018 0,004 0,2538088 177,3 178,5 1,2 Schist < 0.01 0,3 0,003 0,011 0,013 0,002 0,02838089 211,7 213 1,3 Schist 0,08 0,3 0,002 0,01 0,008 0,005 0,0338090 213 214 1 Schist 0,02 0,3 0,003 0,005 0,01 0,001 0,01738091 214 215 1 Schist 0,01 0,3 0,003 0,005 0,011 0,002 0,01438092 215 216 1 Schist 0,01 1 0,003 0,004 0,011 0,001 0,01338093 216 217 1 Schist 0,09 0,9 0,003 0,011 0,008 0,004 0,05738094 222 222,7 0,7 Schist 0,12 1,1 0,005 0,043 0,019 0,006 0,20138095 223,3 224,3 1 Schist 0,05 0,8 0,006 0,048 0,02 0,005 0,19638096 231 232 1 Schist 0,05 0,6 0,005 0,033 0,015 0,003 0,19738097 232 233,2 1,2 Schist 0,22 1,2 0,005 0,012 0,011 0,005 0,07538098 233,2 234,3 1,1 Schist 0,04 0,4 0,004 0,004 0,011 0,002 0,017

Sample results

38099 234,3 235,5 1,2 And 0,05 0,5 0,004 0,004 0,011 0,002 0,01938100 236,8 237,8 1 And < 0.01 0,3 0,003 0,005 0,012 < 0.001 0,0138101 Stand 15Pa 1,01 0,2 0,003 0,006 0,011 < 0.001 0,00838102 Stand 6Pc 1,56 0,2 < 0.001 0,004 0,002 0,002 0,00538103 Blank sample < 0.01 0,2 0,003 0,015 0,003 < 0.001 0,0138104 248 249,3 1,3 And < 0.01 0,2 0,004 0,006 0,013 0,001 0,01538105 252,4 253,1 0,7 And < 0.01 0,3 0,003 0,005 0,011 < 0.001 0,01438106 266,4 267,8 1,4 And < 0.01 0,2 0,005 0,008 0,013 0,001 0,01538107 267,8 269 1,2 And < 0.01 0,2 0,003 0,006 0,014 0,001 0,01338108 270,8 271,9 1,1 And < 0.01 0,3 0,004 0,006 0,013 0,001 0,01438109 274,3 274,9 0,6 And < 0.01 0,2 0,004 0,007 0,014 < 0.001 0,01738110 294,6 295,3 0,7 And < 0.01 20,8 0,006 0,006 0,032 3,616 0,422

Logged by : MP Sheet of


1 22 26,8 4,8 4,1 85% 4 83%2 26,8 30,6 3,8 4,2 111% 3,8 100%3 30,6 34,8 4,2 4,1 98% 4,01 95%4 34,8 39,15 4,35 4,3 99% 4,27 98%5 39,15 43,25 4,1 4,1 100% 4,1 100%6 43,25 47,4 4,15 4,12 99% 4,1 99%7 47,4 51,7 4,3 4,3 100% 4,21 98%8 51,7 56 4,3 4,2 98% 4,2 98%9 56 60,2 4,2 4,1 98% 3,7 88%10 60,2 64,3 4,1 4,1 100% 4,01 98%11 64,3 68,5 4,2 4,15 99% 4,15 99%12 68,5 72,8 4,3 4,25 99% 4,25 99%13 72,8 77,05 4,25 4,3 101% 4,25 100%14 77,05 81,3 4,25 4,3 101% 4,15 98%15 81,3 85,6 4,3 4,3 100% 4,3 100%16 85,6 89,7 4,1 4,1 100% 4,1 100%17 89,7 93,9 4,2 4,15 99% 4,15 99%18 93,9 98 4,1 4,1 100% 4,01 98%19 98 102,2 4,2 4,2 100% 4,2 100%20 102,2 106,5 4,3 4,35 101% 4,35 101%21 106,5 110,7 4,2 4,2 100% 4,2 100%22 110,7 115 4,3 4,3 100% 4,3 100%23 115 119,25 4,25 4,2 99% 4,2 99%24 119,25 123,45 4,2 4,2 100% 4,2 100%25 123,45 127,8 4,35 4,33 100% 4,33 100%26 127,8 132 4,2 4,18 100% 4,18 100%27 132 136,5 4,5 4,3 96% 4,3 96%28 136,5 140,7 4,2 4,21 100% 4,21 100%29 140,7 145,1 4,4 4,28 97% 4,2 95%30 145,1 149 3,9 4 103% 4 103%31 149 153,25 4,25 4,27 100% 4,27 100%32 153,25 157,6 4,35 4,2 97% 4,2 97%33 157,6 161,3 3,7 3,72 101% 3,3 89%34 161,3 164,9 3,6 3,3 92% 2,5 69%35 164,9 168,5 3,6 3,2 89% 2,3 64%36 168,5 171,7 3,2 3,1 97% 2,8 88%37 171,7 175,2 3,5 4,1 117% 3,5 100%38 175,2 179,2 4 4,05 101% 4,05 101%39 179,2 183,5 4,3 4,2 98% 4,2 98%40 183,5 187,3 3,8 4,25 112% 4,05 107%41 187,3 191,15 3,85 3,9 101% 3,75 97%42 191,15 195,15 4 4 100% 3,85 96%43 195,15 198,5 3,35 3,3 99% 3,25 97%44 198,5 202,5 4 3,9 98% 3,84 96%45 202,5 206,2 3,7 3,6 97% 3,55 96%46 206,2 209,8 3,6 3,53 98% 3,25 90%47 209,8 213,8 4 3,98 100% 3,95 99%48 213,8 218,05 4,25 4,23 100% 4,23 100%



49 218,05 222,2 4,15 4,13 100% 4,1 99%50 222,2 225,6 3,4 3,35 99% 3,3 97%51 225,6 229,9 4,3 4,27 99% 4,27 99%52 229,9 234,1 4,2 4,2 100% 4,2 100%53 234,1 238,4 4,3 4,34 101% 4,29 100%54 238,4 242,5 4,1 4,1 100% 4,05 99%55 242,5 246,85 4,35 4,34 100% 4,34 100%56 246,85 250,4 3,55 3,5 99% 3,5 99%57 250,4 254,4 4 4 100% 4 100%58 254,4 258,4 4 3,95 99% 3,95 99%59 258,4 262,7 4,3 4,2 98% 4,2 98%60 262,7 266,4 3,7 3,67 99% 3,67 99%61 266,4 270,6 4,2 4,18 100% 4,18 100%62 270,6 274,9 4,3 4,31 100% 4,31 100%63 274,9 279,2 4,3 4,27 99% 4,27 99%64 279,2 283,5 4,3 4,3 100% 4,3 100%65 283,5 287,6 4,1 4,05 99% 4,05 99%66 287,6 291,8 4,2 4,2 100% 4,2 100%67 291,8 296 4,2 4,2 100% 4,2 100%68 296 299 3 3 100% 3 100%

DDH X Y Elevation Azimuth Inclination Depth Started Completed Logged by Date NAD83 E NAD83 NC08-21 L-2100E 1850N 300 0 -50 299m 06/03/09 12/03/09 MP 10/01/2010

Princ LithologyFrom To L Id rock type Photo9,5 41,9 32,4 And Intermed volcanics. Light to locally dark grey. Fine grained.

Locally fractured and brecciated. Slightly to mod altered by cal. Cal-Qtz vnlets and filled frcatures. Some mineralized zones. Sulfid patches, nodules and stringers. Some pyr, pyrrhotite (mgn)

41,9 57,5 15,6 Arg Argilite. Very dark grey to black. Very fine grained. Fractures filled by clear cal-Qtz. Locally some Pyrrh-pyr stingers. Some pyr cubes

57,5 113,3 55,8 And Intermed volcanics. Grey. Fine to v fine grain. Aphanitic and locally porphyric texture. Locally some angular coarse clasts. Fractures filled by clear cal-Qtz. Some pyr grains. Cpy and Po traces, mostly filling some fract. Some light greenish material filling some fct associated with Qtz-cal.

113,3 135,4 22,1 Porph And Porphyritic andesite. 25-30% coarse clear pg feldspars. Porphyritic texture. Light grey Vf grained groundmass. Some py traces. Poorly fractured. Homogenous in terms of grain size and composition. Light greenish epidotized feldspars. A few fx filled by cal-qz.

135,4 137,4 2 Arg Argilite. Very dark grey to black. Very fine grained. 30* sharp upper contact. Gradual lower contact. Fractures filled by clear cal-Qtz. 5% qz-cal veinlets. Sulfid traces.

137,4 172,9 35,5 And Intermed volcanics. Grey to greenish grey. Vf to fg. Mostly aphanitic with locally porphyritic texture. Slightly altered: epidotized fld and silicified matrix on some spots. Locally highly fractured. Brecciated with some sulfids. Py and po patches or forming stringers and filling some fx. Some cal-qz vts. Close to the upper contact with the argilite above some dark material is filling most of the fx.

DDH Depth

172,9 224 51,1 And Slightly to moderately altered intermed volcanics cut by aphanitic and porphyritic mafic to intermed dykes. Grey, light grey, light greenish grey. Chloritized-epidotized calcified and silicified vfg matrix. Cal-qz forming stringers, vn and vts, filling mm to cm fx. Some sulfides : py cubes, locally some small po patches.

224 299 75 And Weakly altered indermed volcanics. Grey. Light grey and locally greenish grey. Aphanitic to locally porphyritic texture.Fine to Vfg groundmass. Poorly fractured. Some clear cal-qz filling some of the fx. Locally chloritized matrix. Locally bleached. Some clear coarse pl fld(a few percent) locally a very few black angular well crystallized pyroxenes. Local shearing. Local silicification. Brecciated on some spots. A few qz vn, vts and small patches. Some ind to mafic vol small dykes cut the host rock sharply. Locally a very few py cubes.

299 299 0 E.O.H

Second Lithology From To L Id rock types, grain size, etc. Photo9,5 15,1 5,6 And Int volc. Dark grey. Fine grained. Poorly fractured. Some coarse

angular clasts. A well rounded felsic xenolith. A few small pyr grains

15,1 25 9,9 And Int volc. Light grey. Very fine grained. Aphanitic texture. Numerous fract filled by clar cal-Qtz. A few med size clear feldspar grains. Locally brecciated. Some mineralized zones showing some Pyr-pyrrh stringers and veinlets.

25,9 33,4 7,5 And Inter volc. Altered sheared and brecciated zones showing some pyr-pyrrh mineralization.

33,4 35,2 1,8 And Int volc. Very light grey. Qtz-cal veins and patches. Mylonitic. Brecciated and fractured. Cal into the matrix. Silicified.

41,9 42,4 0,5 Arg Argilite. Very fine grained. Very dark grey to black. Highly fractured zone showing numerous filled frc. Some clear patches with some greenish alteration material.

49 49,5 0,5 And Int volc dyke. Very fine grained. Sharp contacts(45*). Some coarse argilite clasts

64 70 6 And Inter volc. Numerous Qtz veinlets. Qtz-cal filling tiny fct

90,2 91,4 1,2 And Inter volc dyke. Some pyr

108,1 108,4 0,3 And Intermed volc dyke. Darker grey. Fg. Homogenous. Sharp upper and lower contacts 40*. 1% mm Fx filled by clear cal-qz

110,7 110,95 0,25 And Fresh andesitic dyke. Dark grey. Vfg. Homogenous. 0.5% mm Fx. Sharp upper and lower contacts of 50*

113,2 114,2 1 Por And Porphyritic Andesitic dyke. 30% coarse clear unaltered angular fld. Unfractured. Sharp lower and upper contacts of 30*.

Depth

114,25 116,1 1,85 And Intermed volc dyke. Darker grey. Fg. Homogenous. Sharp upper and lower contacts 40*. 1% mm Fx filled by clear cal-qz. Locally brecciated.

144 147 3 And Altered andesite. Sil and epidotized groundmass. Some dark material is filling most of the fx

156,6 175 18,4 And Brecciated and altered volcanics showing locally some sulphides patches, filling some fx or forming small nodules. Some qz vn and vts, cal-qz filling mm fx.

175 178,5 3,5 And Nearly unaltered mafic dyke. Dark grey. Poorly fractured. Aphanitic dark matrix. Shows a few black mm-cm grains of augite(1%). Clear cal-qz filling mm and cm fx. 30* sharp upper contact. Gradual lower contact.

190,7 191,15 0,45 And Intermed volcanic dyke. Unaltered and unfractured. Grey. Vf grained. Aphanitic groundmass with 20% of fg clear pl fld. Sharp upper and lower contacts of 45*. A few py grains.

193,35 194,6 1,25 And Dark grey vfg volc dyke. Nearly unaltered. Some mm--cm fx filled by clear cal-qz. Sharp upper and lower contacts of 10 and 20*.

196,2 197,15 0,95 And Nearly unaltered Volc dyke. Vfg. 2-3% mm fx filled by clear cal-qz. A cm angular clast with some med to coarse pl fld. Upper and lower sharp contacts.

200,7 202,3 1,6 Por And Feldspar porphyry. Dark grey. Porphyritic texture. 20-25% of clear angular pl fld. Aphanitic to vfg groundmass. Nearly unaltered. 1--2% mm-cm fx filled by cal-qz. A few py cubes. Sharp contacts (0-10*). The host rock is moderately sheared close to the contacts with the dyke

209,3 210,9 1,6 And Vfg altered volc dyke. Grey, greenish grey. A few altered (chloritized) med size mafic grains(1%). A coarse well rounded felsic xenolith showing some coarse clear pl fld. A few mm fx filled by cal-qz. A qz vein with some cal traces close to the lower contact. Some cal-qz patches at the contact. Slightly sheared and chloritized margins.

258,8 260,3 1,5 And Fg intermed volc dyke. Dark grey. Unaltered and nearly unfracured. 20*upper sharp contact. A very few fx filled by clear cal-qz. Sharp lower contact.

266,4 267,1 0,7 And Fg volc dyke. Nearly unaltered and unfractured. Very sharp 15* upper contact. 40* very sharp lower contact. A few small py grains close the lower contact inside or related to qz veining. A few small qz-cal patches. Qz-cal also filling a few fx.

276,8 277,7 0,9 And Fg nearly unaltered volc dyke. Dark grey. Sharp upper and lower contacts of 25*. Chloritized margins, fractured with some clear cal-qz filling them. A coarse well rounded altered clast from the host rock.

279,2 279,7 0,5 And Light grey silicified vfg vol dyke. Sharp upper contact 30*. Gradual lower contact. Brecciated and fractured margins showing some alteration(chloritized matrix). A few py cubes. Poorly fractured.

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal9,5 41,9 32,4 And 2-5% fractures 2--3 241,9 42,4 0,5 Arg 5% fractures 5 544 53,9 9,9 Arg Mod sheared. Flat pyr grains. 50*clearer Qtz-cal veinlets 2 369 70 1 And

Fractured and brecciated zone. Sheared. 30*foliations. Partially mylonitic. Filled fct. Qtz veinlets 2 1

77,5 78,9 1,4 And Fractured zone. Stockwerk. 4 5

95,4 96,8 1,4 And Qtz veins 20 396,8 101,3 4,5 And Brecciated and sheared zone. 30* foliations 5 3105,5 113,3 7,8

And

Sheared, brecciated and fractured zone showing qtz veins and veinlets. Qtz stringers and forming mm foliations of 40*. Twisted qz-cal vts.

3--4 2--3

140,2 148,7 8,5 And Brecciated and fractured zone showing veins and veinlets. Some fx filled by dark alteration materials. Chl qz ep into the matrix. Relicts of pg fld.

2 2

156 173 17 And Sheared and brecciated numerous small zones showing some sulphides patches, nodules and filling some mm fx. Qz vn and vts. Some of the sulphides are surrounding altered clasts, some at the margins of vn and vts.

3 0,5

175 178,5 3,5 And Nearly unaltered mafic dyke. Dark grey. Poorly fractured. Aphanitic dark matrix. Shows a few black mm-cm grains of augite(1%). Clear cal-qz filling mm and cm fx. 30* sharp upper contact. Gradual lower contact.

2 2

190,7 191,15 0,45 And Aphanitic groundmass with 20% of fg clear pl fld. Sharp upper and lower contacts of 45*. A few py grains.

2 3

193,35 194,6 1,25 And Dark grey vfg volc dyke. Nearly unaltered. Some mm--cm fx filled by clear cal-qz. Sharp upper and lower contacts of 10 and 20*.

3 2

196,2 197,15 0,95 And 2-3% mm fx filled by clear cal-qz. A cm angular clast with some med to coarse pl fld. Upper and lower sharp contacts.

3 2

200,7 202,3 1,6 Por And1--2% mm-cm fx filled by cal-qz. A few py cubes. Sharp contacts (0-10*). The host rock is moderately sheared close to the contacts with the dyke

1 2

202,3 276 73,7 And 1% mm-cm fx filled by clear cal-qz. 2-3% sheared 1 1276,8 277,7 0,9 And Two mm fx filled by cal-qz. 0,1 0,1

Depth Veins(%)

From To L Id Description Serp Asb Chl Epi Alb Si Serp Asb Chl Epi Alb Qtz-Cal9,5 41,9 32,4 And Fract filled by cal-Qtz 241,9 56,8 14,9 And mm-cm Fract filled by cal-Qtz 3

56,8 113 56,2 And Fract filled by cal-Qtz. Cal-qz patches. 5

113 135,4 22,4 Por And 25-35% of coarse angular epidotized plag feldspars 2 1145 161 16 And Altered ground mass. Slightly to

moderately epidotized and silicified. Some cal-qz patches and filling fx

2--3 2 3 0,5

173 202,3 29,3 And

Slightly to moderately altered. Greenish grey. Locally moderate amount of chlorite into the aphanitic matrix. 2 2 3 1 0,5 0,5 2--3

202 276 74 And

Locally slightly altered. The matrix is locally bleached and chloritized (light greenish). Silicified and calcified on some spots. Most of the fx are filled by clear cal-qz. 2--3 1

276 299 23 And Weakly chloritized groundmass. Locally silicified. 2 1--2


From To L Id Py Cpy Ars Cpy Pyrrh16,6 19,1 2,5 And Pyrite-Pyrrhotite veins and patches 3 2--3

25,7 33,4 7,7 And Brecciated and fractured zone. Sulfids veins, stringers and patches

2 2

45,4 55,8 10,4 Arg Pyr cubes, pyrrhotite stringers and veinlets. Fct filled by sulfids

1 2

69 69,6 0,6 And Some pyr 1

72,9 75,1 2,2 And Some pyr. Some po 1--2 174,1 75,2 1,1 And Some pyr. Some po 1 0,579,9 81,3 1,4 And Some pyr. Some po 1 0,581,3 82,7 1,4 And Some pyr. Some po 2 182,7 83,2 0,5 And Some pyr. Some po 0,5 184,4 85,3 0,9 And Some pyr. Some po 1 189,6 90,6 1 And Some pyr 1,590,6 91,8 1,2 And Some pyr. Some po 1 0,591,8 92,6 0,8 And Some pyr. Some po 0,5 0,5135,5 135,7 0,2 And Pyr traces 0,2156,6 158 1,4 And Po small patches. Py cubes. Py filling mm fx 0,5 0.5-1159 159,8 0,8 And Po filling a few mm fx. Py traces 0,25 0.5-1161 161,5 0,5 And cm Po vn 0,1 0,5163,1 164,5 1,4 And Po small patches. A few py grains 0,25 0,3167,6 172,3 4,7 And Po patches, filling fx or forming stringers. Some py 0.5-1 0,5178,5 185,7 7,2 And Disseminated py. Cpy and po traces 1 0,1 0,1204,1 206,7 2,6 And Some py cubes. A few small po patches 0.5--1 0,1208 209,3 1,3 And Py cubes 0,5 0210,2 211,2 1 And Qz vein showing some py inclusions 0,2 0215,15 215,7 0,55 And Some py. Po and Cp traces. 0,5 0,1 0,1263,4 268,5 5,1 And A few small py cubes. Small py patches. 0,2277 279,4 2,4 And A few py cubes. 0,1


No. From To L Id Au Ag Co Cu Ni Pb Zn38001 15,4 16,5 1,1 And < 0.01 0,2 0,002 0,007 0,011 < 0.001 0,02538002 16,5 17 0,5 And < 0.01 0,4 0,008 0,011 0,013 0,003 0,03438003 19,3 20 0,7 And < 0.01 0,2 0,004 0,011 0,015 < 0.001 0,0138004 22,9 24,3 1,4 And < 0.01 0,2 0,002 0,008 0,012 < 0.001 0,02138005 25,9 26,4 0,5 And < 0.01 0,5 < 0.001 0,018 0,018 < 0.001 0,04138006 27,4 28,7 1,3 And < 0.01 0,3 0,004 0,007 0,012 < 0.001 0,04638007 28,7 30,2 1,5 And < 0.01 1,3 0,015 0,006 0,01 0,003 0,14138008 30,2 31,5 1,3 And < 0.01 0,2 0,002 0,004 0,012 < 0.001 0,01238009 31,5 32,4 0,9 And < 0.01 1,6 0,006 0,005 0,008 0,001 0,02438010 32,4 33,4 1 And < 0.01 0,4 0,007 0,004 0,008 < 0.001 0,02738011 35,9 36,8 0,9 And < 0.01 0,2 0,007 0,007 0,01 < 0.001 0,02338012 45,3 45,8 0,5 Arg < 0.01 0,2 0,003 0,005 0,011 < 0.001 0,01238013 47,8 49 1,2 Arg < 0.01 0,2 0,002 0,007 0,008 < 0.001 0,02438014 49,8 50,3 0,5 Arg < 0.01 0,4 0,002 0,008 0,007 < 0.001 0,02938015 50,3 51,2 0,9 Arg < 0.01 0,3 0,003 0,004 0,007 < 0.001 0,00638016 51,2 51,8 0,6 Arg < 0.01 0,2 0,004 0,004 0,012 < 0.001 0,02838017 55,4 56 0,6 Arg < 0.01 0,2 0,002 0,003 0,006 < 0.001 0,0138018 69 69,7 0,7 And < 0.01 0,2 0,002 0,005 0,01 < 0.001 0,00838019 74,1 75,2 1,1 And < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00738020 79,9 81,3 1,4 And < 0.01 0,2 0,003 0,004 0,011 < 0.001 0,00738021 81,3 82,7 1,4 And < 0.01 0,3 0,003 0,006 0,013 < 0.001 0,00938022 82,7 83,2 0,5 And < 0.01 0,2 0,002 0,006 0,013 < 0.001 0,0138023 Stand 15Pa 0,99 0,2 0,003 0,006 0,011 < 0.001 0,00738024 Stand 6Pc 1,47 0,2 < 0.001 0,004 0,003 0,002 0,00538025 Blank sample < 0.01 0,2 0,002 0,015 0,002 < 0.001 0,01138026 84,4 85,3 0,9 And < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00838027 89,6 90,6 1 And < 0.01 0,2 0,002 0,003 0,012 < 0.001 0,00838028 90,6 91,8 1,2 And < 0.01 0,3 0,003 0,006 0,015 < 0.001 0,00838029 91,8 92,6 0,8 And < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00738030 156,6 158 1,4 And < 0.01 0,2 0,003 0,005 0,012 < 0.001 0,0138031 159 159,8 0,8 And < 0.01 0,2 0,003 0,005 0,012 < 0.001 0,00638032 161 161,5 0,5 And < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00738033 163,1 163,9 0,8 And < 0.01 0,2 0,002 0,005 0,012 < 0.001 0,00638034 163,9 164,5 0,6 And < 0.01 0,2 0,003 0,005 0,013 < 0.001 0,00738035 167,6 169 1,4 And < 0.01 0,2 0,003 0,005 0,013 < 0.001 0,00738036 169 169,6 0,6 And < 0.01 0,2 0,003 0,005 0,015 < 0.001 0,01938037 169,6 171 1,4 And < 0.01 0,2 0,002 0,004 0,012 < 0.001 0,00738038 171 172,3 1,3 And < 0.01 0,2 0,001 0,006 0,012 < 0.001 0,00838039 178,5 179,6 1,1 And < 0.01 0,2 < 0.001 0,005 0,01 < 0.001 0,00838040 179,6 181 1,4 And < 0.01 0,2 < 0.001 0,004 0,01 < 0.001 0,00738041 181 182,4 1,4 And < 0.01 0,2 0,001 0,004 0,011 < 0.001 0,008

Sample results

38042 182,4 183,4 1 And < 0.01 0,2 < 0.001 0,005 0,011 < 0.001 0,00738043 183,4 184,5 1,1 And < 0.01 0,2 < 0.001 0,004 0,012 < 0.001 0,00738044 184,5 185,7 1,2 And < 0.01 0,2 0,001 0,006 0,012 0,001 0,00938045 204,1 204,9 0,8 And < 0.01 0,2 0,002 0,007 0,014 < 0.001 0,00938046 Stand 15Pa 0,95 0,2 0,002 0,006 0,011 < 0.001 0,00738047 Stand 6Pc 1,51 0,2 < 0.001 0,004 0,002 0,002 0,00538048 Blank sample < 0.01 0,2 < 0.001 0,016 0,003 < 0.001 0,01138049 204,9 205,5 0,6 And < 0.01 0,2 < 0.001 0,004 0,011 < 0.001 0,00938050 205,5 206,7 1,2 And < 0.01 0,2 < 0.001 0,004 0,011 < 0.001 0,00838051 208 209,3 1,3 And 0,02 0,2 < 0.001 0,005 0,01 0,001 0,00838052 210,2 211,2 1 And < 0.01 0,2 < 0.001 0,003 0,009 0,001 0,00738053 215,15 215,7 0,55 And < 0.01 0,2 < 0.001 0,005 0,011 < 0.001 0,00838054 266,6 267,1 0,5 And < 0.01 0,2 0,001 0,006 0,016 0,001 0,00738055 271,4 272 0,6 And < 0.01 0,2 0,001 0,005 0,011 0,001 0,009



1 9,5 13,2 3,7 2,9 78% 1,93 52%2 13,2 17,4 4,2 4,1 98% 3,9 93%3 17,4 21,6 4,2 4,2 100% 4,1 98%4 21,6 25,7 4,1 3,9 95% 3,8 93%5 25,7 29,8 4,1 4 98% 4 98%6 29,8 34,1 4,3 4,2 98% 4,2 98%7 34,1 38,3 4,2 3,8 90% 4,1 98%8 38,3 42,4 4,1 4,05 99% 3,6 88%9 42,4 46,4 4 4 100% 4 100%10 46,4 50,6 4,2 4,15 99% 4,15 99%11 50,6 54,8 4,2 4,15 99% 4,1 98%12 54,8 59 4,2 4 95% 3,5 83%13 59 63 4 3,9 98% 3,82 96%14 63 67,1 4,1 4 98% 4 98%15 67,1 71,2 4,1 4,1 100% 4,1 100%16 71,2 75,5 4,3 4,2 98% 4,2 98%17 75,5 79,8 4,3 4,3 100% 4,2 98%18 79,8 84,2 4,4 4,2 95% 4,2 95%19 84,2 88,2 4 4,3 108% 4,3 108%20 88,2 92,2 4 3,4 85% 3,4 85%21 92,2 96,5 4,3 4,2 98% 4,2 98%22 96,5 100,8 4,3 4,3 100% 4,3 100%23 100,8 105,05 4,25 4,2 99% 4,2 99%24 105,05 109,2 4,15 4,1 99% 4,1 99%25 109,2 113,2 4 4 100% 4 100%26 113,2 117,7 4,5 4,25 94% 4,2 93%27 117,7 122 4,3 4,2 98% 4,2 98%28 122 126,35 4,35 4,37 100% 0%29 126,35 130,75 4,4 4,35 99% 4,35 99%30 130,75 134,9 4,15 4,15 100% 4,15 100%31 134,9 139,2 4,3 4,3 100% 4,3 100%32 139,2 143,45 4,25 4,23 100% 4,23 100%33 143,45 147,8 4,35 4,25 98% 4,19 96%34 147,8 152 4,2 4,2 100% 4,2 100%35 152 156,25 4,25 4,15 98% 4,15 98%36 156,25 160,5 4,25 4,17 98% 4,05 95%37 160,5 164,7 4,2 4,25 101% 4,1 98%38 164,7 169 4,3 4,3 100% 4,3 100%39 169 173,3 4,3 4,3 100% 4,21 98%40 173,3 177,55 4,25 4,2 99% 4,2 99%41 177,55 181,7 4,15 4,2 101% 4 96%42 181,7 186 4,3 4,25 99% 4,25 99%43 186 190,2 4,2 4,25 101% 4,2 100%44 190,2 194,4 4,2 4,2 100% 4,2 100%45 194,4 198,8 4,4 4,38 100% 4,38 100%



46 198,8 203 4,2 4,2 100% 4,2 100%47 203 207,3 4,3 4,3 100% 4,3 100%48 207,3 211,65 4,35 4,35 100% 4,35 100%49 211,65 215,9 4,25 4,2 99% 4,2 99%50 215,9 220,2 4,3 4,3 100% 4,3 100%51 220,2 224,55 4,35 4,3 99% 4,3 99%52 224,55 228,9 4,35 4,35 100% 4,35 100%53 228,9 233,2 4,3 4,26 99% 4,26 99%54 233,2 237,6 4,4 4,32 98% 4,32 98%55 237,6 242 4,4 4,37 99% 4,37 99%56 242 246,2 4,2 4,19 100% 4,19 100%57 246,2 250,6 4,4 4,29 97% 4,29 97%58 250,6 254,85 4,25 4,19 99% 4,19 99%59 254,85 259,1 4,25 4,26 100% 4,26 100%60 259,1 263,3 4,2 4,2 100% 4,2 100%61 263,3 267,6 4,3 4,3 100% 4,3 100%62 267,6 271,9 4,3 4,32 100% 4,32 100%63 271,9 276,3 4,4 4,3 98% 4,3 98%64 276,3 280,5 4,2 4,19 100% 4,19 100%65 280,5 284,75 4,25 4,22 99% 4,22 99%66 284,75 289,1 4,35 4,31 99% 4,31 99%67 289,1 293,4 4,3 4,25 99% 4,25 99%68 293,4 297,55 4,15 4,2 101% 4,2 101%69 297,55 299 1,45 1,45 100% 1,45 100%

DDH X Y Elevation Azimuth Inclination Depth Started Completed Logged by Date NAD83 E NAD83 NC08-22 L-1900E 1775N 300 0 -50 290m 13/03/2009 16/03/09 MP 22-27/01/2010

Princ LithologyFrom To L Id rock type Photo20,5 209 188,5 And Interm volcanics. Dark to light grey. Aphanitic texture. Weakly to

mod altered : locally silicified and chloritized. Some cal qz vn vnlt and filling most of the fx. Locally brecciated and highly fractured with numerous qz-cal vnlt, some aphanitic dark chl is forming most of the matrix. Locally some disseminated py. Some po traces.

209 246,5 37,5 And Interm volcanics. Dark to very dark grey. Aphanitic texture. Slightly chloritized matrix. Locally silicified. Some fractured and brecciated zones showing some disseminated sulphides. A few mm fx filled by clear cal-qz. Py and Po small patches, filling some of the fx.

246,5 261,65 15,15 Black shist

Black schist. Very fine grained. Aphanitic texture. Locally slightly sheared (fabrics) and altered. Poorly fractured. A few fx filled by clear cal-qz. Some well rounded py nodules often surrounded by cal. Py also filling mm fx. Crossed by volc altered dykes(small sheared, chloritized, silicified and calcified). Most of the volc dykes cut the host rock sharply. Homogenous in terms of color and texture. A few coarse well rounded and altered vol clasts. Locally the py is forming small beds. Locally graphitic(2-5%).

261,7 290 28,3 And Altered and fractured andesite. Grey. Very fine grained. Aphanitic texture. Weakly to moderately chloritized. Locally highly silicified. Numerous mm-cm fx filled mostly by clear cal. Locally sheared. Some py patches, forming bands, disseminated and filling some fx. Locally some crushed core. Locally strongly bleached. Fabrics: dark minerals are forming bands and stringers locally some mafic minerals are flat and partially turned into greenish chl. Cal-clay-chl filling numerous tiny fx

290 290 E.O.H End Of Hole

DDH Depth

Second Lithology From To L Id rock types, grain size, etc. Photo20,5 35 14,5 And Brecciated and altered zone. Chl stringers and surrounding clasts.

Locally silicified and calcified groundmass. Qz-cal vn vnlt and filling the fx.

35 36,2 1,2 And Mod sheared. Chloritized. Fabrics. Flat mafic grains forming small flat stains or small bands

63,5 64 0,5 And Brecciated. Some coarse rounded clasts. Chloritized dark aphanitic matrix.

73,5 79,1 5,6 And Brecciated. Some coarse rounded clasts. Some mm to cm clear qz vn and vnlt. Chloritized dark aphanitic matrix.

89 96 7 And Breccia. Numerous mm fx filled by dark aphanitic chl112,7 121 8,3 And Fractured zone showing some sulfide traces. Mm to cm cal-qz veins and

vnlts.125 133 8 And Mod fractured. Some fx are filled by clear cal-qz show cm greenish

epidotized margin133 145,5 12,5 And Poorly fractured weakly silicified and chloritized andesite. A few clear

cal-qz vnlts. Locally some sulfides.145,5 152 6,5 And Nearly unfractured and unaltered andesite. A few fx filled by cal-qz.

Locally some well rounded qz grains of a fe mm152 169 17 And Altered andesite. Chloritized and silicified aphanitic matrix. Fx filled

mostly by dark chl. Some po-py traces. 204,8 206,8 2 felsic dyke Felsic dyke. Cream color. Aphanitic texture. High amount of aphanitic

qz grains. Very homogenous in terms of compostion, color and texture. Nearly unfractured (0.5% fx filled by cal-qz). Very sharp upper and lower contacts. (0*/CA) A few very fine mafic grains are partially chloritized.

228,5 240 11,5 And Mod altered and bleached. High amount of chlorite and greenish epidote into the matrix. Higher porosity. Softer. A few fx filled by clear cal. A few nodules of py. Po traces.

261 275,5 14,5 And Altered and fractured zone. Mod-stongly silicified and calcified zones. Numerous mm-cm fx filled by clear cal some by dark chl. Locally sheared. The py forms bands and coarse patches.

275,5 290 14,5 And Fractured zone showing some py. Numerous mm-cm fx filled by clear cal-qz. Locally sheared. The py forms small patches

Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal23,5 34,7 11,2 And Stockwerk. Brecciated and fractured. A few fx filled by

clear cal-qz. Mm to cm qz vn, qz-cal vn5--7 2--3

35 36,2 1,2 And Mod sheared. Chloritized. Fabrics. Flat mafic grains forming small flat stains or small bands

1 1

63,5 64 0,5 And Brecciated. Some coarse rounded clasts. Chloritized dark aphanitic matrix.

0 0

73,5 79,1 5,6 And Brecciated. Some coarse rounded clasts. Some mm to cm clear qz vn and vnlt. Chloritized dark aphanitic matrix.

2 1

89 96 7 And Breccia. Numerous mm fx filled by dark aphanitic chl 1 1

112,7 121 8,3 And Fractured zone showing some sulfide traces. Mm to cm cal-qz veins and vnlts.

1--2 1--2

125 133 8 And Mod fractured. Some fx are filled by clear cal-qz show cm greenish epidotized margin

2--3 2--3145,5 152 6,5 And Nearly unfractured and slightly altered andesite. A few fx

filled by cal-qz. Locally some well rounded qz grains of a fe mm

0,5 1

152 177,3 25,3 And A few fractured and brecciated zones. Most of the fx are filled by clear cal-qz. A few qz vnlets. Locally small qz patches.

1 0,5

177,3 204,8 27,5 And Small slightly sheared zones. Some mm fx filled by clear cal-qz. Bleached more porous core around 190m deep in a brecciated zone.

0,5 0,5

236 239 3 And Sheared zone. Fabrics and chl stringers. Py beds. A few clear cal-qz twisted vnlets.

1 1--2

261 290 29 And Fractured zone showing some py. Numerous mm-cm fx filled by clear cal-qz. Locally sheared. The py forms bands and coarse patches in these zones.

1 3--7

Depth Veins(%)

From To L Id Description Serp Asb Chl Epi Alb Si Serp Asb Chl Epi Alb Qtz-Cal20,5 42,5 22 And Altered fractured and brecciated zone. 10-20% dark chl.

Silicified zones. Some cal into the matrix where silicification is weaker.

2--3 1--2 1--2

42,5 68 25,5 And Mod silicified matrix. 2--3

73,5 79,1 5,6 And Dark aphanitic chloritized matrix. Weakly-mod silicified. 3--4 1--2 1

97 101 4 And Slightly chloritized/epidotized. Locally mod silicified. Some med well rounded qz grains

1 1 2 1--2

101 116 15 And Silicified. Slightly chloritized and calcified fine grained matrix

1 1--2 1

152 169 17 And Altered andesite. Chloritized and silicified aphanitic matrix. Fx filled mostly by dark chl. Some po-py traces.

2 2--3 5 0,5 2--3

172,3 204,8 32,5 And Chloritized silicified aphanitic matrix. Locally some fx show cm epidotized margins.

1--2 1--2 1--2

228,5 240 11,5 And Mod altered and bleached. High amount of chlorite and greenish epidote into the matrix. Higher porosity. Softer. A few fx filled by clear cal. A few nodules of py. Po traces.

2--3 1 1

261 290 29 And Altered and fractured zone. Mod-stongly silicified and calcified zones. Numerous mm-cm fx filled by clear cal some by dark chl. Locally sheared. The py forms bands and coarse patches.

1 2--3 5--10


From To L Id Py Cpy Ars Cpy Pyrrh29,1 30,1 1 And Some disseminated py. 0,5

33,2 34,1 0,9 And Py 0,5

66,8 67,5 0,7 And Some disseminated py. 1

69,1 69,6 0,5 And py traces. Po traces 0,1 0,178,1 79 0,9 And Py traces. 0,1116,2 117,6 1,4 And Py and po traces 0,1 0,1131,6 132,3 0,7 And Py Po 0,5 0,1158,6 159,2 0,6 And Py Po very small patches. 0,5 0,2162,2 162,7 0,5 And Py Po 0,2 0,2164 165,1 1,1 And Py Po 0,5 0,1186,4 187,8 1,4 And Py filling a few mm fx. Py-Po patch 0,5 0,2195 196,1 1,1 And Py-Po patches 1 1200,05 201,3 1,25 And Py 0,5202,7 203,3 0,6 And Po-Py patch 1 1--2206,8 223,05 16,25 And Disseminated py (cubes and filling some fx) Some po small

patches, associated with py or concentrated in the fratured and brecciated zones.

1--2 0.5--1

227,4 228,4 1 And Disseminated py (cubes and filling some fx). A very few po small patches.

1-1.5 0,1

235,7 236,8 1,1 And Some disseminated py. 1236,8 238 1,2 And A few small pyr cubes. A few py beds. 0.5-1238 239,4 1,4 And Some py filling mm fractures. 0.5-1239,4 240,8 1,4 And Py filling a few mm fx. Py-Po small patches. 0.5-1 0,5241,2 242,2 1 And Disseminated py. 1242,2 243,2 1 And Some py filling mm fractures, forming mm beds and small

patches.1

245,4 251,2 5,8 And-Schist

Some py beds, py filling mm fx. Py patches surrounded by clear cal.

1--2

254 254,7 0,7 Shist Py small nodules forming well rounded or flat eyes. Some py forming mm beds. A few mm fx filled by py.

1

256,7 257,9 1,2 Shist Pyr nodules 1259,5 260,5 1 And

dykeDisseminated py. 1-1.5

260,5 261,9 1,4 And A few very small pyr grains 0,1

261,9 263,3 1,4Schist Pyr nodules, patches, forming beds and a few filling mm

fx. 2--3

263,3 264,4 1,1 And Py bands and filling some mm to cm fx with clear cal. 1--2

264,4 265,2 0,8And Py patches. Py bands and filling some mm to cm fx with

clear cal. 1--2

265,2 266,55 1,35 And Py coarse patches. 2--3272 272,7 0,7 And Py small patches and grains 1--2273,3 274,1 0,8 And Disseminated 1


278,1 278,8 0,7 And Py small patches and filling a few mm fx 0,5286,7 287,7 1 And Diss py 1287,7 289,1 1,4 And A few small pyr cubes. A few py small patches 1

No. From To L Au Ag Co Cu Ni Pb Zn38111 29,1 30,1 1 0,01 0,2 0,003 0,006 0,011 < 0.001 0,01438112 33,2 34,1 0,9 0,01 0,2 0,004 0,007 0,015 < 0.001 0,02438113 66,8 67,5 0,7 0,02 0,3 0,004 0,006 0,015 < 0.001 0,01738114 69,1 69,6 0,5 0,01 0,3 0,004 0,009 0,015 0,009 0,01638115 78,1 79 0,9 < 0.01 0,3 0,003 0,005 0,013 < 0.001 0,0138116 116,2 117,6 1,4 < 0.01 0,2 0,003 0,005 0,013 < 0.001 0,00938117 131,6 132,3 0,7 0,02 0,2 0,004 0,007 0,014 < 0.001 0,00938118 158,6 159,2 0,6 < 0.01 0,2 0,004 0,005 0,015 < 0.001 0,01438119 162,2 162,7 0,5 < 0.01 0,2 0,004 0,006 0,013 < 0.001 0,01638120 164 165,1 1,1 < 0.01 0,3 0,003 0,006 0,014 < 0.001 0,01438121 186,4 187,8 1,4 < 0.01 0,2 0,004 0,006 0,014 < 0.001 0,02138122 195 196,1 1,1 < 0.01 0,2 0,005 0,007 0,016 < 0.001 0,02538123 200,05 201,3 1,25 < 0.01 0,2 0,004 0,005 0,016 < 0.001 0,0238124 202,7 203,3 0,6 < 0.01 0,2 0,005 0,013 0,019 < 0.001 0,01738125 206,8 208 1,2 < 0.01 0,2 0,004 0,004 0,015 < 0.001 0,01438126 208 209,4 1,4 < 0.01 0,2 0,004 0,005 0,016 < 0.001 0,02138127 209,4 210,5 1,1 < 0.01 0,2 0,004 0,004 0,015 < 0.001 0,02238128 210,5 211,6 1,1 < 0.01 0,2 0,003 0,005 0,015 < 0.001 0,01538129 211,6 213 1,4 < 0.01 0,2 0,003 0,005 0,014 < 0.001 0,01438130 213 214,4 1,4 < 0.01 0,2 0,003 0,004 0,014 < 0.001 0,01438131 214,4 215,6 1,2 < 0.01 0,2 0,003 0,004 0,014 < 0.001 0,01338132 215,6 217 1,4 < 0.01 0,2 0,003 0,004 0,015 < 0.001 0,01938133 Stand 15Pa 1 0,2 0,003 0,006 0,012 < 0.001 0,00738134 Stand 6Pc 1,6 0,2 < 0.001 0,004 0,003 0,002 0,00538135 Blank sample < 0.01 0,2 0,003 0,015 0,003 < 0.001 0,0138136 217 218,4 1,4 < 0.01 0,2 0,003 0,005 0,013 < 0.001 0,01538137 218,4 219,6 1,2 < 0.01 0,2 0,003 0,004 0,013 < 0.001 0,01838138 219,6 221 1,4 < 0.01 0,2 0,003 0,004 0,013 < 0.001 0,01338139 221 222 1 < 0.01 0,2 0,003 0,005 0,014 < 0.001 0,03138140 222 223,05 1,05 < 0.01 0,2 0,003 0,004 0,013 < 0.001 0,01338141 227,4 228,4 1 < 0.01 0,2 0,002 0,005 0,007 < 0.001 0,00638142 235,7 236,8 1,1 < 0.01 0,2 0,003 0,005 0,013 < 0.001 0,00838143 236,8 238 1,2 0,01 0,2 0,003 0,005 0,012 < 0.001 0,00938144 238 239,4 1,4 < 0.01 0,2 0,003 0,005 0,014 < 0.001 0,00838145 239,4 240,8 1,4 0,01 0,2 0,003 0,004 0,012 < 0.001 0,00938146 241,2 242,2 1 < 0.01 0,2 0,003 0,004 0,012 < 0.001 0,00938147 242,2 243,2 1 < 0.01 0,2 0,002 0,004 0,013 < 0.001 0,00938148 245,4 246,2 0,8 < 0.01 0,2 0,003 0,004 0,015 < 0.001 0,00838149 246,2 247,3 1,1 0,02 0,2 0,002 0,005 0,011 0,001 0,01138150 247,3 248,5 1,2 < 0.01 0,3 0,004 0,016 0,015 0,002 0,08238151 248,5 249,9 1,4 0,03 0,4 0,005 0,021 0,018 0,002 0,12638152 249,9 251,2 1,3 < 0.01 0,7 0,006 0,033 0,016 0,005 0,15638153 254 254,7 0,7 0,04 0,8 0,006 0,04 0,019 0,006 0,179

Sample results

38154 256,7 257,9 1,2 0,14 1 0,006 0,049 0,018 0,007 0,27738155 259,5 260,5 1 0,02 0,2 0,004 0,022 0,025 < 0.001 0,02938156 Stand 15Pa 1,1 0,2 0,003 0,006 0,012 < 0.001 0,00838157 Stand 6Pc 1,5 0,2 < 0.001 0,003 0,003 0,002 0,00538158 Blank sample < 0.01 0,2 0,003 0,014 0,003 < 0.001 0,01138159 260,5 261,9 1,4 0,03 0,7 0,005 0,019 0,018 0,003 0,10538160 261,9 263,3 1,4 0,02 0,2 0,003 0,005 0,013 0,001 0,01838161 263,3 264,4 1,1 0,05 0,5 0,003 0,006 0,01 0,002 0,0238162 264,4 265,2 0,8 0,15 1,1 0,003 0,007 0,011 0,004 0,02538163 265,2 266,55 1,35 < 0.01 0,4 0,004 0,007 0,011 0,003 0,05338164 272 272,7 0,7 < 0.01 0,3 0,004 0,007 0,024 0,001 0,01138165 273,3 274,1 0,8 0,01 0,2 0,003 0,009 0,016 0,003 0,0138166 278,1 278,8 0,7 0,01 0,2 0,003 0,008 0,011 0,004 0,01838167 286,7 287,7 1 < 0.01 0,2 0,003 0,006 0,014 0,001 0,00938168 287,7 289,1 1,4 < 0.01 0,2 0,003 0,006 0,012 0,001 0,009



1 20,5 24,6 4,1 3,9 95% 1,83 45%2 24,6 28,6 4 4 100% 3,62 91%3 28,6 32,7 4,1 4,12 100% 3,9 95%4 32,7 36,8 4,1 4 98% 3,7 90%5 36,8 41 4,2 4,2 100% 4,2 100%6 41 45,3 4,3 4,25 99% 4,27 99%7 45,3 49,4 4,1 3,9 95% 3,6 88%8 49,4 53,5 4,1 4,05 99% 3,8 93%9 53,5 57,4 3,9 3,92 101% 3,4 87%10 57,4 61,5 4,1 4,1 100% 4,1 100%11 61,5 65,6 4,1 4,1 100% 4 98%12 65,6 69,9 4,3 4,3 100% 4,3 100%13 69,9 74,2 4,3 4,27 99% 4,27 99%14 74,2 78,6 4,4 4,3 98% 4,3 98%15 78,6 82,85 4,25 4,3 101% 4,19 99%16 82,85 87,1 4,25 4,2 99% 4,13 97%17 87,1 91,1 4 3,98 100% 3,78 95%18 91,1 95,4 4,3 4,07 95% 4,05 94%19 95,4 99,7 4,3 4,31 100% 4,24 99%20 99,7 104 4,3 4,28 100% 4,28 100%21 104 108,2 4,2 4,1 98% 4,1 98%22 108,2 112,5 4,3 4,3 100% 4,25 99%23 112,5 116,6 4,1 4,05 99% 4,05 99%24 116,6 121 4,4 4,2 95% 3,97 90%25 121 125 4 3,98 100% 3,98 100%26 125 129,3 4,3 4,26 99% 4,26 99%27 129,3 133,4 4,1 4,05 99% 4,05 99%28 133,4 137,6 4,2 4,17 99% 4,17 99%29 137,6 141,8 4,2 4,2 100% 4,2 100%30 141,8 146 4,2 4,13 98% 4,11 98%31 146 150,4 4,4 4,3 98% 4,22 96%32 150,4 154,6 4,2 4,2 100% 4,2 100%33 154,6 158,9 4,3 4,33 101% 4,27 99%34 158,9 163,2 4,3 4,26 99% 4,24 99%35 163,2 167,4 4,2 4,2 100% 4,2 100%36 167,4 171,6 4,2 4,2 100% 4,2 100%37 171,6 175,9 4,3 4,25 99% 4,25 99%38 175,9 180,15 4,25 4,23 100% 4,23 100%39 180,15 184,4 4,25 4,25 100% 4,22 99%40 184,4 188,7 4,3 4,3 100% 4,17 97%41 188,7 193 4,3 4,27 99% 4,27 99%42 193 197,4 4,4 4,33 98% 4,33 98%43 197,4 201,75 4,35 4,32 99% 4,32 99%44 201,75 206 4,25 4,23 100% 4,23 100%45 206 210,3 4,3 4,3 100% 4,3 100%46 210,3 214,6 4,3 4,28 100% 4,28 100%



47 214,6 218,85 4,25 4,23 100% 4,23 100%48 218,85 223,05 4,2 4,17 99% 4,17 99%49 223,05 227,3 4,25 4,25 100% 4,22 99%50 227,3 231,2 3,9 3,89 100% 3,84 98%51 231,2 235,5 4,3 4,27 99% 4,27 99%52 235,5 239,7 4,2 4,15 99% 4,12 98%53 239,7 243,9 4,2 4,21 100% 4,21 100%54 243,9 248 4,1 4,05 99% 4,05 99%55 248 252,1 4,1 4,1 100% 4,1 100%56 252,1 256 3,9 3,9 100% 3,9 100%57 256 260,05 4,05 4 99% 4 99%58 260,05 264,2 4,15 4,1 99% 4 96%59 264,2 267,7 3,5 3,4 97% 3,01 86%60 267,7 271,85 4,15 4,1 99% 3,92 94%61 271,85 275,7 3,85 3,8 99% 3,75 97%62 275,7 279,5 3,8 3,7 97% 3,6 95%63 279,5 283 3,5 3,3 94% 3 86%64 283 286,6 3,6 3,5 97% 2,6 72%65 286,6 290 3,4 3,4 100% 3,4 100%


C-10-24 L-4500E 1050N 300 Grid Noth -50 300m 06-janv-10 10-janv-10 AC & GV May 27-28 2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 40,00 40,00 OB Overburden casing40,00 44,60 4,60 MAn grey fg hom bo monzonite

44,60 58,90 14,30 MAn

hom, fg felsic volc w limited chlorite content, loc mm phX up to 3%, cm internal structures marked by var in alt some epi, loc cm brecciation suscept in the .5-1.5 range

58,90 62,85 3,95 MAn idem

62,85 64,70 1,85 MAnmg hom chlo felsic-intermediate ?? Volcanics in continuity w previous unit

64,70 80,3 15,60 MAn

hom, fg felsic volc w limited chlorite content, loc mm phX up to 3%, cm internal structures marked by var in alt some epi, loc cm brecciation suscept in the .5-1.5 range

80,30 110,2 29,90 MAn idem

110,20 110,8 0,60 SyDhom vfg to fg dark pruplish syenite w shears upper & lower contacts 45 to CA

110,80 124,35 13,55 MAnhom, fg felsic volc w limited chlorite content, loc mm phX up to 3%, cm internal structures marked by var in alt some epi,

124,35 129,2 4,85 SyD fg-mg hom chlo syenite or monzonite129,20 129,5 0,30 SyD vfg hom purplish syenite

129,50 129,9 0,40 MAnfg hom chlo metavolcanic unit w mm qz-cal v 45 to CA at upper & lower contacts

129,90 131,2 1,30 SyD vfg hom purplish syenite w grad continuity w next unit131,20 132,7 1,50 SyD fg-mg hom chlo syenite or monzonite w grad continuity w next unit

132,70 135,5 2,80 SyDvfg hom purplish syenite w minor 2% loc white mm phX, w grad continuity w next unit

135,50 138,1 2,60 SyD fg-mg hom chlo syenite or monzonite138,1 139,5 1,40 SyD idem well developed finely banded schistosity, 45 to CA139,50 140,8 1,30 MaV fg ± hom chlo schist, 40 to CA w 1% diss py140,80 141,15 0,35 MaV hom fg chlo monzonite141,15 141,8 0,65 MaV fg ± hom finely banded chlo schist, 40 to CA

141,80 142,6 0,80 MAnalt & chlo vfg felsic to int dark green metavolc idem previous major volc unit

142,60 143,2 0,60 MAn fg chl- qz-cal sw-2% diss py SZ, 25 to CA

143,20 146,2 3,00 MaVfg med green ± hom chlo monzonite w darker and finer gr lower 20 cm prob chill margin, 45 to CA

146,20 147 0,80 MaV idem unit in SZ finely banded schistosity 45 to CA147,00 153,4 6,40 MaV fg med green ± hom chlo monzonite153,40 155,9 2,50 SyD vfg to fg hom purplish syenite w 3% mm white phX

DDH Depth

155,90 163,1 7,20 MaV fg med green ± hom chlo monzonite

163,10 163,4 0,30 MAnalt & chlo vfg felsic to int dark green metavolc idem previous major volc unit

163,40 167,95 4,55 MaVfg med green ± hom chlo massive monzonite, w tr py & contamination up to 20 cm at the upper contact

167,95 169,3 1,35 MAnalt & chlo vfg massive felsic to int dark green metavolc idem previous major volc unit

169,30 173,5 4,20 MAn pale green felsic volc idem prev unit w high chlo alt173,50 173,9 0,40 MAn transirion zone

173,90 184,7 10,80 MAnalt & chlo vfg massive felsic to int dark green metavolc idem previous major volc unit

184,70 185,7 1,00 MAnbrecciated zone idem prev unit w cm fragments w first half meter highy brecciated w vfg chlo matrix 60% w tr mm py

185,70 199,5 13,80 MAnvfg dark green w loc light green epi alt w loc SZ 45 to CA w loc cm Qz+Ca v 45 to CA

199,50 201 1,50 MAn var fg medium green w loc reddish v prob transition zone199,50 214,2 14,70 MAn var fg to mg medium greem w dark phX & loc white phX

214,20 299,3 85,10 MAnfg-mg var w mg light green w dark mineral w SZ & loc epi alt w loc qz v, And massive

EOH

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP

40,60 41,00 0,40 hom med grey feisc volc, possibly dacite44,45 44,6 0,15 quartz v 45

49,4 49,55 qz-fpK v w some brecciation // to CA 049,9 50,05 0,15 idem w mm fugs 4054,3 54,45 0,15 assimilated monzonite v 80

57,85 58,50 0,65SZ w mm qz-cal v & micro CTCL structure + 2% diss py over 15 cm in center of zone 40

very weak suscept

55,55 55,70 0,15 monzonite v 8068,40 10 cm zone w 40% brecciated qz-fpK cluster65,10 5 cm chlo breccia w elongated alt mm elements 3583,50 10 cm qz-fpK cluster related to weak epi alt // CA 5101,85 101,95 0,10 50% qz-epi-pl ± cal in alt zone w diss py less .5% 80

114,35 114,5 0,15 2 cm qz-pl-cal v in alt zone w low diss py 45148,50 5 cm qz v 50

186,10 10 cm SZ w mm qz-cal v w 2-3% Py w tr Cpy w 45 to CA188,70 cm qz-cal v w 3% py w 45 to 50 to CA

190,2 190,5 0,3030 cm zone w mm to cm qz-cal v w 3 % py w loc Cpy in v w 60 to CA

193,70 194,15 0,45 Hom red brown syenite 5% diss py dyke?195,4 qz-cal v w elongated epi alt w 3% py198,3 199,5 1,20 mm qz-cal v w var 10 to 60 to CA w 3% diss py199,5 201 fg var green to red w 3-5% diss py203,4 204,25 0,85 fg dark w orange phX w orange alt at top, prob dyke?205,8 206,2 0,40 qz-cal v w white phX w 3% py & purple mineral in v207,3 207,8 0,50 fg dark 30 to CA prob dyke? 210,8 211,6 0,80 mg w dark foliation 45 to CA w 2% diss py & near v

211,8 214,2 2,40white phX w 60 cm zone w mm qz-cal v w fault w low py at 212.7

214,5 qz-cal v 45 to CA217,1 5 cm qz-cal v w py and tr Cpy 45 to CA219,4 15 cm zone w epi alt223,7 qz-cal v w epi alt w 2% py 30 to CA224,4 224,75 0,35 qz-cal v 20 to CA w 2% py228,7 230,9 2,20 fg greyish w white phX

DDH Depth

235,6 236,7red brown fg w low diss py except in 10 cm transition zone at bottom 5 %

238,4 20 cm deformed zone w 5% py241,6 243,2 1,60 SZ 90 to CA w 5% py w vugs in qz-cal v247,35 20 cm zone w qz-cal v & epi alt & chlo253,8 255,75 1,95 fg dark w white phX w loc mm qz-cal v260,5 10 cm qz-cal v

266,1 266,5 0,4040 cm zone w qz-cal v w epi alt & vugs w unidentified black metallic mineral

267,35 5 cm qz-cal v268,8 5 cm qz-cal v275,2 10 cm zone 276,65 277,8 1,15 qz- cal vein // to CA w 2% py & v 45 to CA286,7 5 cm qz-cal v291,4 296,45 qz-cal v // to CA w mm v & 80 to CA w 3% py

296,45 298,7fg reddish brown w breccia w K alt & qz-cal v 90 to CA w vugs w 2 % py

From To Length Id Description CA Py Po Cpy Sph Gal Mag57,45 57,60 0,15 2% diss py fg CTCL 267,95 A 10 cm w 2% diss py w 1 cm qz-cal v in center 35 272,10 72,4 0,30 B 2 5 diss py w 2 1cm v qz-cal 35 277,35 C 10 cm w 2% diss py w 1 cm qz-cal v in center 35 2

98,10 98,50 0,40 D 4% diss py in fg CTCL w 5 cm qz v in center of zone 30 4100,90 101,20 0,30 E 1 % diss py in alt zone w 2 cm qz-cal v in center 30 1

176,857 cm fg qz-chlo sheared zone w 2% py w 1 cm qz-cal v 45 2

178,6015 cm fg qz-chlo sheared zone w 2% py w 1-2 cm qz-cal v 45 2

179,00 179,20 0,20sheared 2% py w 1 cm qz-cal v w late fg 1 cm chlo-epi vi n opposite direction 45 2

180,85 181,05 0,20 idem 5% diss py w 1 cm qz-cal v 70 5236,70 F 10 cm zone transition w syenite dyke 5% py 90 5238,35 G 15 cm deformed zone w 4% py 80 4239,75 239,90 0,15 H qz-cal v w 3% py 30 3241,60 242,90 1,30 SZ w low py & cm qz-cal v 90

0,00296,50 296,75 0,25 I brecciated zone w 3 % py 3

297,35 297,55 0,20 Jqz-cal v w brecciated zone w 3% py & unidentified black mineral 3

297,70 297,85 0,15 K reddish fg w breccia & cal v w 3 % py 3298,60 298,70 0,10 L qz-cal v 50 to CA w breccia & vugs & 2% py & tr Cpy 2 tr


Sample Id From To Length Comments Id Au Ag46060 57,85 58,55 0,70 SZ w 15 cm 2% diss py fg CTCL

46061 65,10 66,60 1,505 composite sample A-E (see mineralization) alt & CTCL zones w qz & qz-cal v

46062 176,60 176,85 3 composite178,60 179,20180,85 181,10 1,10

46063 205,80 206,20 0,40 qz-cal v w white phX & 3% py 46064 224,40 224,75 0,35 qz-cal v w epi alt w py

46065 236,703 composite sample F-H (see mineralization) alt & deformation zone

238,35239,75 239,90 0,40

46066 241,60 242,90 1,30 SZ w low py & cm qz-cal v

46067 266,1 266,5 0,4040 cm zone w qz-cal v w epi alt & vugs w unidentified black metallic mineral

46068 296,50 296,754 composite sample I-L (see mineralization) breccia & qz-cal v & K alt

46069 291,4 292,7 1,3 qz-cal v // to CA w mm v & 80 to CA w 3% py46070 292,70 294,25 1,55 idem46071 294,25 295,40 1,15 idem

Assays

Hole C-10-24DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge Comments

Box no. From To Length % Length % Comments % % From To1 40 43 3 2,4 80% 0,85 28% 50 contains 5% cm quaternary pebbles 2 43 46,3 3,3 4,15 126% 2,40 73% 60 contains 1% cm quaternary pebbles 3 46,3 50,6 4,3 4,35 101% 3,90 91% 304 50,6 54,7 4,1 4,1 100% 3,60 88% 35 54,7 58,9 4,2 4,2 100% 4,05 96% 06 58,9 63,3 4,4 4,3 98% 3,85 88% 07 63,3 67,5 4,2 4,3 102% 3,60 86% 08 67,5 71,8 4,3 4,25 99% 3,70 86% 09 71,8 76,1 4,3 4,25 99% 3,95 92% 010 76,1 80,3 4,2 4,15 99% 4,00 95% 011 80,3 84,4 4,1 4,2 102% 3,65 89% 012 84,4 88,7 4,3 4,4 102% 3,65 85% 113 88,7 93,05 4,35 4,35 100% 3,85 89% 014 93,05 97,4 4,35 4,35 100% 3,95 91% 015 97,4 101,1 3,7 4,15 112% 3,35 91% 016 101,1 105,6 4,5 4,17 93% 3,90 87% 017 105,6 109,75 4,15 4,14 100% 3,45 83% 018 109,75 114 4,25 4,2 99% 3,75 88% 019 114 118,1 4,1 4,18 102% 3,45 84% 020 118,1 122,2 4,1 4,00 98% 2,37 58% 421 122,2 126,3 4,1 4,10 100% 3,20 78% 022 126,3 130,3 4 4,15 104% 3,34 83% 023 130,3 134,35 4,05 4,10 101% 2,54 63% 024 134,35 138,5 4,15 4,15 100% 2,41 58% 125 138,5 142,5 4 4,30 108% 2,71 68% 326 142,5 146,8 4,3 4,35 101% 4,15 97% 027 146,8 151,15 4,35 4,30 99% 3,95 91% 028 151,15 155,4 4,25 4,35 102% 3,70 87% 029 155,4 159,8 4,4 4,25 97% 4,00 91% 030 159,8 164,05 4,25 4,35 102% 3,60 85% 031 164,05 168,45 4,4 4,43 101% 4,20 95% 032 168,45 172,66 4,21 4,07 97% 2,21 52% 133 172,66 176,84 4,18 4,23 101% 3,58 86% 034 176,84 181,07 4,23 4,25 100% 3,57 84% 035 181,07 185,35 4,28 4,10 96% 1,60 37% 036 185,35 189,52 4,17 4,21 101% 1,21 29% 037 189,52 193,7 4,18 4,21 101% 3,45 83% 038 193,7 197,8 4,1 4,31 105% 3,76 92% 039 197,8 201,81 4,01 4,20 105% 3,20 80%40 201,81 206 4,19 4,20 100% 2,24 53%41 206 210,1 4,1 4,31 105% 4,05 99%42 210,1 214,5 4,4 4,20 95% 3,27 74%43 214,5 218,7 4,2 4,17 99% 3,28 78%44 218,7 223,9 5,2 4,27 82% 2,74 53%45 223,9 227,1 3,2 4,27 133% 3,72 116%

46 227,1 231,5 4,4 4,33 98% 3,50 80%47 231,5 235,75 4,25 4,35 102% 3,65 86%48 235,75 239,8 4,05 4,03 100% 3,10 77%49 239,8 244,9 5,1 4,20 82% 4,78 94%50 244,9 248,25 3,35 4,22 126% 3,11 93%51 248,25 252,6 4,35 4,32 99% 4,13 95%52 252,6 256,8 4,2 4,28 102% 3,55 85%53 256,8 261 4,2 4,04 96% 3,85 92%54 261 265,3 4,3 4,32 100% 4,00 93%55 265,3 269,5 4,2 4,17 99% 3,88 92%56 269,5 273,7 4,2 4,30 102% 3,84 91%57 273,7 278 4,3 4,22 98% 3,36 78%58 278 283,3 5,3 4,24 80% 5,06 95%59 283,3 286,6 3,3 4,27 129% 2,66 81%60 286,6 290,9 4,3 4,26 99% 3,96 92%61 290,9 295,1 4,2 4,20 100% 2,99 71%62 295,1 299 3,9 4,10 105% 2,88 74%63 299 299,3 0,3 0,20 67% 0,25 83%

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC10-25 L-4700E 4075N 300 Grid North -50 300m 11/01/10 15/01/10 GV May 28-31 2010

Princ Lithology

From To L Id rock type Photo0,00 44,60 44,60 OB overburden44,60 47,10 2,50 MAn vfg dark w 2% py

47,10 89,00 41,90 Tufvfg medium green matrix w up to 70% clasts prob lapili/bomb tuff? W 2% py & 1% Po (diss & mm elongated) w progressive diminution in % of chlo in matrix

89,00 112,60 23,60 Tuffg light green w unfocused(???) clasts w loc qz-cal v w loc foliation 45 to CA w loc SZ

112,60 117,50 4,90 Tuf fg greyish w black minerals w 2-3% py & breccia w Fd

117,50 126,40 8,90 Tuffg light green w unfocused(???) clasts w loc qz-cal v w loc foliation 45 to CA w loc SZ

126,40 128,45 2,05 Tuflight to dark green w color var w elongated clasts 60 to CA prob transition zone? W 3% diss Py

128,45 129,20 0,75 GSisvfg black w elongated & deformed Py & cal 45 to CA w siltstone w graphite

129,20 133,00 3,80 Tuf fg greyish qz-cal w black minerals w 2-3% py

133,00 133,90 0,90 GSisvfg black w elongated & deformed Py, qz-cal v 45 to CA w chlo siltstone w graphite

133,90 135,60 1,70 InD fg dark matrix w 5% white phX w 2% diss py & biotite135,60 138,60 3,00 Tuf fg greyish qz-cal w black minerals w 2-3% py138,60 139,15 0,55 InD fg dark matrix w 5% white phX w 5% diss py

139,15 145,45 6,30 Tuffg dark matrix w 50% clasts w 7% diss py & elongated fragments of Po, w progressive change in matrix color to light green ( diminution of Chlo %) , bomb tuff?

145,45 166,20 20,75 Tuffg dark matrix w 50% clasts w 2% diss py & more elongated fragments of Po, w progressive change in matrix color to light green ( diminution of Chlo %) , bomb tuff?

166,20 171,75 5,55 Tuf idem Tuff w var in graphite content and qz-graphite zone at top171,75 172,90 1,15 Tuf fg greyish qz-cal w black minerals172,90 176,00 3,10 Tuf idem Tuff w net contact w next unit between light & dark matrix176,00 184,60 8,60 Tuf idem Tuff 184,60 187,35 2,75 Tuf fg matrix w elongated clasts 45 to CA, idem Tuff?

187,35 243,80 56,45 Tuffg greyish qz-cal matrix w black mineral w var in qz-chlo content w qz-cal v

260 30242,00

MAnfg medium green w mm qz-cal v & epi alt w loc 5% white phX & loc cm qz-cal v, And mass?

DDH Depth

Second Lithology

From To L Id rock types, grain size, etc. Photo51,85 52,15 0,30 InD fg dark w net contacts dyke?54,60 55,05 0,45 InD fg dark w net contacts dyke?67,75 qz-cal v 10 to CA w 1% Po77,45 80,20 2,75 highly foliated zone with 2% py & 2% Po87,50 88,40 0,90 qz-cal v w breccia 3% py 89,10 89,30 0,20 idem96,70 97,10 0,40 qz-cal v 30 to CA w 3% py103,50 104,00 0,50 fg dark green w 1% py112,60 113,60 1,00 fg dark foliated w 5% mm cal v & Fd114,25 10 cm qz v w chlo115,10 115,30 0,20 20 cm qz-cal v w Py, Po, Chlo & unidentified silver mineral Mo?122,20 124,00 1,80 fg qz-chlo w 2% py160,40 160,90 0,50 fg qz-chlo164,25 164,70 0,45 fg greyish qz-cal w black minerals w 1% py164,70 165,10 0,40 qz-cal breccia & v 20 to CA

0,00171,30 171,75 0,45 fg black w clasts prob Tuff? W 5% Po and 5% Py176,80 10 cm qz-cal & epi? V 45 to CA179,45 20 cm zone w cal v 30 to CA184,20 10 cm zone w qz v 30 to CA185,1 185,6 0,50 fg dark matrix no clasts186,4 186,5 0,10 idem190,4 190,7 0,30 fg dark matrix no clasts w 1% py191,6 192,2 0,60 qz-cal v w 3% diss py193,2 193,6 0,40 fg dark matrix no clasts w vfg diss py199,35 200,45 1,10 qz-cal v 45 to CA201,9 202,7 0,80 qz-cal v zone w Mo?203,3 203,7 0,40 qz-cal v zone w SZ204,3 204,45 0,15 qz-cal v 45 to CA212,25 212,4 0,15 qz-cal v 45 to CA219,2 219,65 0,45 K-qz alt zone w mm qz-cal v w 3% py222,2 5 cm qz-cal v223 223,2 0,20 5 cm qz-cal v 40 to CA w unidentified reddish brown mineral240,05 240,25 0,20 5 cm qz-cal v 30 to CA241,4 242,7 1,30 fg greyish w 25% white phX dyke?

242,75 243,30,55

5 cm qz-cal vein w deformation and foliation 45 to CA w 5-7% py

243,8 255,812,00

fg reddish brown matrix w 35 % white phX & 15% black mineral w chlo fragments & diss py, dyke?

Depth

260,1 260,45 0,35 15 cm qz-cal v w pinkish color & chlo 45 to CA260,9 261,35 0,45 5 cm pinkish qz-cal v 30 to CA

266,8 267,050,25

15 cm qz-cal v w 1% py, chlo, epi alt & black mineral in v tourmaline?

267,25 268 0,75 fg black w biotite, one contact dyke?268,1 268,5 0,40 mm qz-cal v zone w epi alt269 269,25 0,25 fg black w dark mineral, biotite?270,7 271,4 0,70 2 qz-cal v w black mineral, tourmaline? Chlo & epi alt272,8 273,2 0,40 pinkish qz-cal v 60 to CA cut by qz-cal v 30 to CA275,25 275,45 0,20 2 cm qz-cal v w black mineral & epi alt278 278,25 0,25 2cm qz-cal v w epi alt278,6 279 0,40 mm v w high epi alt281,4 282 0,60 fg black w foliation 45 to CA w 1% py, dyke?284 284,1 0,10 5 cm qz-cal v w high epi alt289,3 290,7 1,40 zone w mm-cm qz-cal v w red mineral, SZ w 3% py, 45 to CA

291,1 10 cm qz-cal v with red mineral & epi alt, w 1% py, 60 to CA292,7 10 cm qz-cal v w chlo & SZ w 1-2% py, 60 to CA293,3 5 cm qz-cal w epi alt & 1% py, 60 to CA294,8 295,7 0,90 vfg reddish-brown-grey w small phX, dyke? 45 to CA296 2 cm pinkish qz-cal v w epi alt, 45 to CA296,8 297,35 0,55 zone w cm pinkish qz-cal v w chlo & epi alt, 80 to CA298,5 300,15 1,65 fg grey-black w 5% white phX dyke? 45 to CA300,7 302 1,30 zone w high epi alt in holes?

From To L Id Py Cpy Po Ars67,75 30 cm qz-cal v 10 to CA w 1% Po 177,45 80,20 2,75 highly foliated zone with 2% py & 2% Po 2 287,50 88,40 0,90 qz-cal v w breccia 3% py 389,10 89,30 0,20 idem 396,70 97,10 0,40 qz-cal v 30 to CA w 3% py 3103,50 104,00 0,50 fg dark green w 1% py 1114,25 A 10 cm qz v w chlo

115,10 115,30 0,20 B20 cm qz-cal v w Py, Po, Chlo & unidentified silver mineral Mo?

126,40 128,45 2,05light to dark green w color var w elongated clasts 60 to CA prob transition zone? W 3% diss Py

128,45 129,20 0,75 Cvfg black w elongated & deformed Py & cal 45 to CA w graphite? Volcanic ash?

133,00 133,90 0,90 Dvfg black w elongated & deformed Py, qz-cal v 45 to CA w chlo & graphite? Volcanic ash?

138,60 139,15 0,55 fg dark matrix w 5% white phX w 5% diss py

139,15 145,45 6,30fg dark matrix w 50% clasts w 7% diss py & elongated fragments of Po, w progressive change in matrix color to light green ( diminution of Chlo %) , bomb tuff?

145,45 166,20 20,75fg dark matrix w 50% clasts w 2% diss py & more elongated fragments of Po, w progressive change in matrix color to light green ( diminution of Chlo %) , bomb tuff?

171,30 171,75 0,45 fg black w clasts prob Tuff? W 5% Po and 5% Py201,9 202,7 0,80 qz-cal v zone w Mo?219,2 219,65 0,45 K-qz alt zone w mm qz-cal v w 3% py

242,75 243,30,55


266,8 267,050,25

15 cm qz-cal v w 1% py, chlo, epi alt & black mineral in v tourmaline?

0,00


Sample Id From To Length Comments Id Au Ag46072 67,55 67,90 0,35 30 cm qz-cal v 10 to CA w 1% Po46073 87,50 87,80

88,10 88,4089,10 89,45 0,95

46074 87,80 88,0588,40 89,00 0,85

46075 89,45 90,35 0,90 SZ w 3% py46076 96,70 97,10 0,40 qz-cal 30 to CA w 3% py46077 114,20 114,35

115,10 115,35 0,40

46078 116,60 117,50 0,90 qz-cal v w breccia & alt46079 127,4 128,45 1,05 transition zone w 2-3% py46080 128,45 129,20

133,00 133,90 1,65

46082 141,9 142,5143,2 143,65144,6 144,9 1,35

46081 163,55 164,25164,7 165,1 1,1

46085 171,30 171,75 0,45 fg black w clasts prob Tuff? W 5% Po and 5% Py46086 201,9 202,7 0,80 qz-cal v zone w Mo?46087 219,2 219,65 0,45 K-qz alt zone w mm qz-cal v w 3% py

46088 242,75 243,30,55


46089 245,75 246,45251 251,45254,2 254,5 1,45

46090 266,8 267,05270,7 271,4 0,95

46091 289,3 290,7292,65 292,75 1,5

2 composite fg light matrix w 50% clasts w 5% diss py & more elongated fragments of Po, Tuff?

test 3 composite reddish dyke? Py, tr Cpy?

2 composite of qz-cal v w black mineral, tourmaline? W epi alt

2 composite qz-cal v & SZ

Assays

3 composite qz-cal-plagio v w silica alt 3% py

2 composite fg w foliation 45 to CA & 3% py

2 composite qz-cal v sample A-B (see mineralization)

2 composite sample C-D (see mineralization)

3 composite fg light matrix w 50% clasts w 5% diss py & more elongated fragments of Po, Tuff?

Logged by : Genevieve Vautour Sheet of


1 44,60 47,10 2,50 2,32 93% 1,91 76%2 47,10 51,20 4,10 4,15 101% 3,94 96%3 51,20 55,60 4,40 4,32 98% 4,24 96%4 55,60 59,80 4,20 4,17 99% 3,58 85%5 59,80 64,10 4,30 4,36 101% 3,75 87%6 64,10 68,10 4,00 4,06 102% 3,07 77%7 68,10 72,40 4,30 4,32 100% 4,09 95%8 72,40 76,80 4,40 4,28 97% 3,84 87%9 76,80 80,90 4,10 4,24 103% 3,68 90%10 80,90 85,30 4,40 4,27 97% 4,13 94%11 85,30 89,90 4,60 4,18 91% 4,28 93%12 89,90 93,50 3,60 4,16 116% 2,92 81%13 93,50 97,90 4,40 4,37 99% 4,16 95%14 97,90 102,00 4,10 4,12 100% 3,95 96%15 102,00 106,10 4,10 4,09 100% 3,89 95%16 106,10 110,40 4,30 4,27 99% 4,15 97%17 110,40 114,70 4,30 4,23 98% 4,06 94%18 114,70 119,00 4,30 4,17 97% 3,70 86%19 119,00 123,30 4,30 4,30 100% 4,10 95%20 123,30 127,70 4,40 4,36 99% 4,05 92%21 127,70 131,90 4,20 4,08 97% 3,34 80%22 131,90 135,90 4,00 4,05 101% 3,45 86%23 135,90 140,30 4,40 4,29 97% 3,76 85%24 140,30 144,60 4,30 4,25 99% 4,08 95%25 144,60 148,90 4,30 4,37 102% 3,59 83%26 148,90 153,10 4,20 4,10 98% 3,92 93%27 153,10 157,30 4,20 4,20 100% 4,08 97%28 157,30 161,4 4,10 4,00 98% 3,70 90%29 161,40 165,5 4,10 4,17 102% 3,87 94%30 165,50 169,9 4,40 4,36 99% 3,94 90%31 169,90 174,2 4,30 4,26 99% 3,91 91%32 174,20 178,4 4,20 4,17 99% 4,16 99%33 178,40 182,7 4,30 4,17 97% 4,02 93%34 182,70 186,9 4,20 4,28 102% 3,96 94%35 186,90 191,3 4,40 4,23 96% 3,98 90%36 191,30 195,6 4,30 4,26 99% 3,53 82%37 195,60 199,9 4,30 4,25 99% 4,07 95%38 199,90 204,2 4,30 4,26 99% 4,16 97%39 204,20 208,4 4,20 4,28 102% 3,72 89%40 208,40 212,7 4,30 4,18 97% 3,81 89%41 212,70 217 4,30 4,27 99% 4,04 94%42 217,00 221,3 4,30 4,29 100% 4,29 100%43 221,30 225,5 4,20 4,30 102% 3,92 93%44 225,50 230 4,50 4,32 96% 4,43 98%45 230,00 234,2 4,20 4,16 99% 3,79 90%46 234,20 238,5 4,30 4,23 98% 3,90 91%47 238,50 242,7 4,20 4,20 100% 3,47 83%48 242,70 246,7 4,00 4,14 104% 3,06 77%49 246,70 250,9 4,20 4,34 103% 3,12 74%

Geotechnical Log Hole No. : C-10-25Date : May 28 2010


50 250,90 255,2 4,30 4,17 97% 2,80 65%51 255,20 259,4 4,20 4,09 97% 2,79 66%52 259,40 263,7 4,30 4,23 98% 4,06 94%53 263,70 268 4,30 4,23 98% 3,60 84%54 268,00 272,1 4,10 4,17 102% 3,67 90%55 272,10 276,5 4,40 4,29 98% 3,45 78%56 276,50 280,7 4,20 4,27 102% 3,47 83%57 280,70 285 4,30 4,18 97% 4,05 94%58 285,00 289,3 4,30 4,31 100% 3,35 78%59 289,30 293,5 4,20 4,11 98% 2,78 66%60 293,50 297,7 4,20 4,23 101% 3,57 85%61 297,70 302 4,30 4,32 100% 3,56 83%

EOH


C-10-26 L-5000E 1900N 300 Grid North-50 300m 16-janv-10 20-janv-10 GV May 31-June 2 2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 39,00 39,00 OB overburden casing

39,00 106,10 67,10 Tuf

vfg medium green matrix w up to 70% elongated clasts 45 to CA, prob lapili/bomb tuff? W 2% py & 1% Po (diss & mm elongated) w progressive diminution in % of chlo in matrix & loc high density of small clasts

Tuff seem lighter when near contact w qz-cal v

106,10 125,90 19,80 Tuf fg black to light grey matrix w var in clasts content, w 2-3% py & po py & po often in nodula where po seems replaced by cubic py

125,90 127,00 1,10 Tuf transition zone var from black to grey w disparition of clasts127,00 128,50 1,50 STuf fg greyish tuff w 3% diss py

128,50 129,2 0,70 GSis vfg black w graphite-qz-cal-py & po w foliation 45 to CApy in nodula & often associated w cal

129,20 133,5 4,30 STuf idem prev tuff unit133,50 151,9 18,40 GSis idem prev graphite unit w var w tuff unit151,90 152,4 0,50 STuf idem prev tuff unit w var w graphite unit152,40 173,6 21,20 GSis idem prev graphite unit173,60 178,8 5,20 Tuf var of graphite siltstone and grey tuff178,80 193,35 14,55 Tuf fg medium green matrix undefined clasts, tuff w 3% py & 2% po

193,35 301 107,65 MAnfg medium green w epi alt w loc mm-cm qz-cal v & dyke w 2% py & 2% po, silicification

var in unit color when in contact w qz-cal v

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP47,20 5 cm qz-cal v w 2% py & epi alt 45 to CA50,8 2 cm qz-cal v w 2% py 30 to CA57,05 57,7 0,65 zone w cm qz-cal v & high silica content58,2 58,75 0,55 zone w cm qz-cal v & high silica content60,2 0,20 2 cm qz-cal v w 80 to CA w 10 cm zone of high silica61,1 61,20 0,10 InD fg dark, dyke?62,10 63,50 1,40 mm-cm qz-cal v w light matrix, silica?

76,05 76,50 0,45 TufTuff w fg matrix & highly elongated clasts 45 to CA (clasts mostly black and white)

79,10 79,20 0,10 InD fg dark, dyke?

79,50 79,90 0,40zone w cm qz-cal 30-80 to CA v & high silica content, w 2% py & Po

86,60 88,60 2,00 mm-cm qz-cal v w 3% py88,6 89,3 0,70 zone w small clasts, lineation 45 to CA w py & po92,10 92,90 0,80 zone w mm-cm qz-cal v w alt

93,60 96,45 2,85reddish zone w mm-cm qz-cal v w alt w 3% py w greenish v 10 to CA

121,25 2 cm qz-cal v 30 to CA w chlo & 1% py121,80 122,20 0,40 zone w mm qz-cal v 10 to CA w 1% py124,00 2 cm qz-cal v 30 to CA w 2% py124,30 124,60 0,30 zone of blackish tuff w mm qz-cal v 80 to CA

136,7 150,8 14,10 SyDfg reddish brown matrix w 30% white phX w a greyish color near both ends, cal & unidentified metallic grey mineral

157,20 157,50 0,30 Tuf zone of grey tuff160,1 160,4 0,30 Tuf idem165,7 166,4 0,70 GSis graphite siltstone zone w 35% py

173,6 175,9 2,30 Tufgrey high silica content tuff w 3% py & yellowish mineral (alt?) w 7% mm black v?

175,9 178 2,10 GSis graphite siltstone zone w 20% py & po180,8 5 cm qz-cal v w chlo181 182,1 1,10 And? fg green w black & white mineral, dyke?182,1 183 0,90 cm qz-cal v w py zone183,5 184,3 0,80 brecciated tuff in black matrix, dyke?184,3 184,9 0,60 DiD fg black with black minerals w 2% py186,4 187,6 1,20 DiD fg black with black minerals w 2% py 30 to CA200,1 deep red-purple clasts w high epi alt

DDH Depth

201,8 202,4 0,60 InD fg black w 1% py and biotite, dyke

208,8 211,2 2,40zone w 3 qz-cal v >20 cm w py, po, chlo, tourmaline & epi alt & SZ

212 221,8 9,80mm-cm qz-cal v w py & po 20-80 to CA, 5 cm v w diss small black minerals at 213.8 m

213,1 qz-cal clast? In SZ218 20cm zone w qz-cal v226,1 226,6 0,50 2 cm qz-cal v 10 to CA w py & chlo227,1 227,25 0,15 qz-cal v w 3% py concentrated in epi alt230,85 231,45 0,60 qz-cal v zone 10-80 to CA w py & po, w epi alt & tourmaline?234,4 234,55 0,15 qz-cal v w epi alt w3% py237,5 237,75 0,25 2 qz-cal v 30 to CA

238,35 239 0,65qz-cal v zone w chlo & reddish-brown mineral in v w low py, 30 to CA

244,6 245,2 0,60 2 cm qz-cal v 10 to CA246,4 246,6 0,20 qz-cal v w po & Cpy251,6 252,1 0,50 qz-cal tourmaline nodula w deformation & po254,25 255,95 1,70 vfg black matrix w white qz nodula261,6 262,2 0,60 2 cm qz-cal v 10 to CA w tourmaline269 270,1 1,10 InD fg black w black minerals & 1% py, dyke?270,1 270,4 0,30 3 cm qz-cal v w zone w 3% py274,8 275,2 0,40 2 cm qz-cal v 30 to CA w 2% py276,2 277 0,80 cm qz-cal v w foliation 45 to CA w 2% py277,25 277,8 0,55 cm qz-cal v w epi alt and foliation 45 to CA277,8 279,9 2,10 fg greyish, silica? W 5% diss py282,8 285,5 2,70 InD fg black w black minerals & 1% py, dyke?285,5 288,4 2,90 zone w fragment "& foliation 45 to CA291 291,6 0,60 40 cm qz-cal v w alt & 3% py

297,5 302 4,50zone w fragment "& foliation 45 to CA w loc cm qz-cal v & qz-cal nodula

From To Length Id Description CA Py Po Cpy Sph Gal Mag47,20 5 cm qz-cal v w 2% py & epi alt 45 to CA 250,8 2 cm qz-cal v w 2% py 30 to CA 2

79,50 79,90 0,40zone w cm qz-cal 30-80 to CA v & high silica content, w 2% py & Po 2 2

86,60 88,60 2,00 mm-cm qz-cal v w 3% py 3

93,60 96,45 2,85reddish zone w mm-cm qz-cal v w alt w 3% py w greenish v 10 to CA 3

121,25 2 cm qz-cal v 30 to CA w chlo & 1% py 1121,80 122,20 0,40 zone w mm qz-cal v 10 to CA w 1% py 1124,00 2 cm qz-cal v 30 to CA w 2% py 2127,00 128,50 1,50 STuf 3% diss py 3128,50 129,2 0,70 GSis py & po 45129,20 133,5 4,30 STuf idem prev tuff unit133,50 151,9 18,40 GSis idem prev graphite unit w var w tuff unit151,90 152,4 0,50 STuf idem prev tuff unit w var w graphite unit165,7 166,4 0,70 GSis graphite siltstone zone w 35% py 35

173,6 175,9 2,30 Tufgrey high silica content tuff w 3% py & yellowish mineral (alt?) w 7% mm black v? 3

175,9 178 2,10 GSis graphite siltstone zone w 20% py & po 20184,3 184,9 0,60 DiD fg black with black minerals w 2% py 2186,4 187,6 1,20 DiD fg black with black minerals w 2% py 30 to CA 2201,8 202,4 0,60 InD fg black w 1% py and biotite, dyke 1227,1 227,25 0,15 qz-cal v w 3% py concentrated in epi alt 3234,4 234,55 0,15 qz-cal v w epi alt w3% py 3246,4 246,6 0,20 qz-cal v w po & Cpy tr269 270,1 1,10 InD fg black w black minerals & 1% py, dyke? 1270,1 270,4 0,30 3 cm qz-cal v w zone w 3% py 3274,8 275,2 0,40 2 cm qz-cal v 30 to CA w 2% py 2276,2 277 0,80 cm qz-cal v w foliation 45 to CA w 2% py 2277,8 279,9 2,10 fg greyish, silica? W 5% diss py 5282,8 285,5 2,70 InD fg black w black minerals & 1% py, dyke? 1291 291,6 0,60 40 cm qz-cal v w alt & 3% py 3

291,60 301 9,40 MAnfg medium green w epi alt w loc mm-cm qz-cal v & dyke w 2% py & 2% po, silicification 2 2


Sample Id From To Length Id Comments Au Ag

46092 208,80 210,20 1,4030 cm qz-cal v w smaller v & SZ w py,po & Cpy?

46093 210,20 211,20 1,0025 cm qz-cal v w tourmaline w py & po

46094 246,30 246,80 0,50 qz-cal v w po & Cpy46095 270,1 270,7 0,60 3 cm qz-cal v w zone w 3% py46096 291 291,6 0,60 40 cm qz-cal v w alt & 3% py

Assays


Box no. From To Length % Length % Comments % % From To1 39,00 42,60 3,60 3,38 94% 2,75 76% 02 42,60 46,70 4,10 4,08 100% 2,99 73% 03 46,70 51,00 4,30 4,14 96% 3,66 85% 04 51,00 55,30 4,30 4,23 98% 4,09 95% 05 55,30 59,5 4,20 4,2 100% 3,70 88% 06 59,50 63,8 4,30 4,29 100% 3,90 91% 07 63,80 68,1 4,30 4,11 96% 3,90 91% 08 68,10 72,3 4,20 4,13 98% 3,70 88% 09 72,30 76,6 4,30 4,26 99% 3,73 87% 010 76,60 81 4,40 4,21 96% 3,71 84% 011 81,00 85,2 4,20 4,22 100% 4,22 100% 012 85,20 89,6 4,40 4,13 94% 3,64 83% 013 89,60 93,9 4,30 4,26 99% 3,99 93% 014 93,90 98,2 4,30 4,18 97% 3,68 86% 015 98,20 102,5 4,30 4,33 101% 4,08 95% 016 102,5 106,8 4,3 4,26 99% 3,86 90% 017 106,8 111,1 4,3 4,16 97% 3,81 89% 018 111,1 115,5 4,4 4,27 97% 3,78 86% 019 115,5 119,8 4,3 4,22 98% 3,93 91% 020 119,8 124 4,2 4,15 99% 3,69 88% 021 124 128,3 4,3 4,21 98% 3,98 93% 022 128,3 132,6 4,3 4,26 99% 3,35 78% 023 132,6 136,8 4,2 4,21 100% 3,50 83% 024 136,8 141,1 4,3 4,23 98% 2,48 58% 025 141,1 145,4 4,3 4,27 99% 4,01 93% 026 145,4 149,8 4,4 4,35 99% 3,26 74% 027 149,8 153,8 4 4,08 102% 2,53 63% 028 153,8 158 4,2 4,19 100% 2,63 63% 029 158 162,6 4,6 4,31 94% 2,46 53% 030 162,6 166,8 4,2 4,32 103% 3,71 88% 031 166,8 170,9 4,1 4,27 104% 4,13 101% 032 170,9 175 4,1 4,12 100% 2,43 59% 033 175 179 4 4,16 104% 2,67 67% 034 179 183,3 4,3 4,29 100% 3,70 86% 035 183,3 187,7 4,4 4,30 98% 4,08 93% 036 187,7 191,9 4,2 4,24 101% 3,41 81% 037 191,9 196,1 4,2 4,22 100% 2,96 70% 038 196,1 200,9 4,8 4,27 89% 3,67 76% 039 200,9 205,6 4,7 4,25 90% 3,54 75%40 205,6 209 3,4 4,23 124% 3,77 111%41 209 213,2 4,2 4,33 103% 4,12 98%42 213,2 217,5 4,3 4,28 100% 3,92 91%43 217,5 221,8 4,3 4,20 98% 3,86 90%44 221,8 226,2 4,4 4,30 98% 3,95 90%45 226,2 230,5 4,3 4,24 99% 3,61 84%

46 230,5 234,6 4,1 3,98 97% 2,90 71%47 234,6 239 4,4 4,27 97% 3,43 78%48 239 243,1 4,1 4,15 101% 3,45 84%49 243,1 247,4 4,3 4,23 98% 3,85 90%50 247,4 251,7 4,3 4,18 97% 3,89 90%51 251,7 255,9 4,2 4,15 99% 3,89 93%52 255,9 260,2 4,3 4,25 99% 3,70 86%53 260,2 264,4 4,2 4,17 99% 3,84 91%54 264,4 268,7 4,3 4,31 100% 3,80 88%55 268,7 272,9 4,2 4,13 98% 3,53 84%56 272,9 277,2 4,3 4,24 99% 4,00 93%57 277,2 280,7 3,5 3,25 93% 1,27 36%58 280,7 285 4,3 4,24 99% 3,88 90%59 285 289,2 4,2 4,32 103% 3,45 82%60 289,2 293,4 4,2 4,15 99% 3,71 88%61 293,4 297,7 4,3 4,18 97% 4,10 95%62 297,7 301 3,3 3,12 95% 2,62 79%

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-27 L-5300E 2900N 300 Grid North -50 300m 21/01/10 25/01/10 MV 2010/06/01 - 03


0,00 33,00 33,00 OB Casing.

33,00 61,25 28,25 TufDark gray intermediate lapilli and bomb tuff. Moderately foliated at 40° c.a. Most fragments are of a more felsic nature. The matrix sometimes reaches a light gray colour.

61,25 75,30 14,05 PoD

Brown to reddish brown quartz-feldspar porphyry dyke. Porphyrs form up to 70% in the center, and diminish towards the borders. Borders are green. About 5% very small vacuoles. Contacts are sharp at 80° c.a.

75,30 93,60 18,30 Tuf

Lapilli and bomb tuff. Well foliated at 30° c.a. Starts light gray with large fragments, ends nearly black with no visible fragments. Either contamination by graphite (following unit) or decreasing granulometry (indicating possible reversed polarity).

93,60 107,60 14,00 GrS

Black graphite siltstone. Schistose at 20° c.a. About 5% pyrite in bands and large rounded masses. A few felsic units are present: very light gray with small green crystals.

107,60 114,00 6,40 MAnGray-green very fine-grained andesite. Well foliated at 40° c.a. Several bands of graphite siltstone up to 110m.

114,00 115,00 1,00 Tuf Green andesitic lapilli tuff. Foliated at 50° c.a.

115,00 144,00 29,00 MAnGreen fine-grained andesite. Rarely medium-grained. Foliation generally weak, if present.

144,00 169,60 25,60 BAnGreen or brown fine-grained andesite. Strong alteration of this unit, by the silicification of the matrix of localized breccia.

169,60 175,20 5,60 BAnBorder between the preceding and following units, showing either texture alternatively.

175,20 189,00 13,80 BAnBreccia in the andesite. Gray-green to brown fine-grained andesite, often as fragments in a black aphanitic matrix. Foliation marked by fragments at about 30° c.a.

189,00 232,40 43,40 MAnGray-green to brown fine-grained andesite. Weakly foliated at 45° c.a.

232,40 239,80 7,40 InD

Brown aphanitic intermediate rock. Strongly silicified near the top. Well foliated at 40° c.a. Several bands of green andesite. Contacts with the green andesite are sharp, but unit may be either extrusive or intrusive.

239,80 251,00 11,20 MAnGreen to brown very fine-grained andesite. Very well foliated at 40° c.a.

251,00 276,10 25,10 MAnGreen fine to medium-grained andesite. Often, up to 15% of fine to large quartz fragments. Foliation at 45° c.a.

276,10 280,70 4,60 TufBrown lapilli tuff with green andesite fragments. Matrix is fine-grained. Foliation at 45° c.a.

DDH Depth

280,70 285,40 4,70 MAnGreen fine to medium-grained andesite. Often, up to 15% of fine to large quartz fragments. Foliation at 45° c.a.

285,40 302,00 16,60 TufBrown lapilli tuff with green andesite fragments. Matrix is fine-grained. Foliation at 45° c.a.

EOH


54,40 55,40 1,00 PoDGreen quartz-feldspar porphyry dyke. Porphyrs make up 10% of the rock. Contacts are sharp at 30° c.a. Probably related to following dyke (lithology 1).

113,00 114,00 1,00 DiDA few dykes of diabase in the andesite. Contacts are not linear.

115,50 117,10 1,60 DiDOne large and two small black diabase dykes (largest is 30-60 cm). Contacts are not linear.

153,50 154,20 0,70 DiDBlack fine-grained diabase dyke. Contacts are sharp at 70° c.a.

192,20 195,70 3,50 InDDark gray, fine-grained intermediate dyke. 10% biotite crystals.

246,70 249,00 2,30 InDBrown medium-grained intermediate dyke. Rare vacuoles. Contacts are sharp at 45° c.a.

253,40 254,70 1,30 SyD Beige medium-grained syenite dyke.

Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal Alb Chl Tour

127,30 128,30 1,00 SZShear zone with grey quartz, quartz and quartz-albite veins, as well as pyrite and pyrrhotite bands. Very strong foliation at 60° c.a.

60° 10% 2%

131,80 134,00 2,20 QtzMedium, 2-3cm large, quartz veins. Sometimes associated with large masses of pyrite and pyrrhotite. Random orientations.

134,00 143,10 9,10 QAlbSmall albite veins and medium quartz veins. No alteration or mineralization.

2% 2%

144,00 163,00 19,00 BrcLocalized breccias with silicified matrix, characteristic to this andesitic unite.

5%

163,00 164,00 1,00 QAlbA few medium quartz-albite veins with a silky appearance. No visible mineralization.

5% 5%

164,00 169,60 5,60 Brc Rare localized breccias with silicified matrix. 1%

170,50 175,20 4,70 QAlbA few medium quartz veins and small quartz-albite veins, striking randomly. Not associated with mineralization.

175,20 189,00 13,80 Brc

Localized breccia. Angular to sub-angular andesite fragments in a black aphanitic matrix. Strongest between 175.2 and 179.2. Very weak pyrite mineralization in the matrix.

191,35 191,50 0,15 Qtz2 gray quartz veins, 4cm and 1cm. No visible mineralization.

4%

209,30 209,90 0,60 QAlb4cm quartz vein, striking 20° c.a. No visible mineralization.

20° 15% 1%

207,20 207,70 0,50 QAlbEarly quartz-albite stockwork. Strong sphalerite and rare chalcopyrite mineralization in the veins and in nearby fractures.

5% 3%

207,70 208,00 0,30 QCa 2 medium quartz-carbonate veins. No mineralization. 10% 5%

208,60 209,00 0,40 QAlbA few sub-parallel quartz and quartz-albite veins with weak pyrrhotite and chalcopyrite mineralization.

30° 4% 1%

209,00 210,30 1,30 BrcFaded breccia with weak but pervasive silicification of the matrix. Well foliated at 30°.

30°

210,30 210,80 0,50 QChl1 medium and 1 large quartz-chlorite veins with moderate pyrrhotite mineralization, mostly in the wall rock.

10% 1%

221,50 222,50 1,00 QCaA few quartz-carbonate veins, the largest being 4cm wide, with no visible mineralization.

5% 1%

224,60 225,30 0,70 QtzSeveral small quartz sub-parallel quartz veins. No visible mineralization.

40° 10%

225,30 226,00 0,70 QTOne large grey quartz-tourmaline vein, with fragments of a quartz-albite-tourmaline vein, similar to those of the following structure.

30° 20% 2%

226,90 229,00 2,10 QTAlbA few medium quartz-albite-tourmaline veins. The tourmaline appears as very small crystals. No visible mineralization.

Depth Veins(%)

231,50 231,60 0,10 Ca 5cm wide carbonate vein. No mineralization. 45° 30%

262,80 263,90 1,10 QT3 medium quartz-tourmaline veins, one striking near c.a., the others at 30° c.a. No visible mineralization or alteration.

30° 10% 2%

266,00 267,40 1,40 QTAlbA few small quartz-carbonate veins and one quartz-albite-tourmaline vein. No visible mineralization.

269,00 269,40 0,40 QtzOne 6cm grey quartz vein, with very weak pyrite mineralization.

50° 10%

274,80 275,10 0,30 Qtz Two 2cm quartz veins, no mineralization. 10%292,00 292,10 0,10 QAlb One 3cm quartz-albite vein, no visible mineralization. 50° 4% 10%

293,80 294,80 1,00 SZShear zone with several small parallel quartz-carbonate veins. Pervasive silicification of the rock. No visible mineralization.

40° 5% 5%

From To L Id Description Serp Asb Chl Epi Alb Sil Serp Asb Chl Epi Alb61,00 61,25 0,25 Sil

Silicified border near quartz-feldspar porphyry dyke.

5

144,00 169,60 25,60 SilSilicified matrix in localized breccias in this whole unit. Not associated with any particular mineralization.

2

209,00 210,30 1,30 SilFaded breccia with weak but pervasive silicification of the matrix. Well foliated at 30°.

1

232,40 234,80 2,40 SilStrong silicification of the brown aphanitic intermediate unit. No visible mineralization.

3

244,80 245,30 0,50 EpiStrong epidotization of the wall rock around small fractures filled with quartz or calcite. Associated with weak pyrite mineralization.

70%

293,80 294,80 1,00 Sil Pervasive silicification in a shear zone. 3


From To L Id Py Cpy Ars Po Sph52,00 53,60 1,60 Py 10% disseminated pyrite euhedral crystals. 10%

55,40 60,00 4,60 Po0-20% euhedral pyrite in pyrrhotite fragments in the tuff. Quantity decreases with depth. Probable replacement of pyrrhotite by pyrite.

5% 2%

127,30 128,30 1,00 PoStrong pyrite mineralization associated with grey quartz veins in a shear zone, as well as pyrite and pyrrhotite bands.

10% 3%

129,60 131,80 2,20 Py Large masses of pyrite. 8%

131,80 134,00 2,20 PoLarge masses of pyrite and pyrrhotite associated with quartz veins.

3% 3%

135,70 135,90 0,20 Po Rounded and deformed chunks of pyrrhotite. 10%

143,10 144,00 0,90 PyDeformed veinlets and chunks of pyrite. Near the contact with lower lithology.

6%

207,20 207,70 0,50 CPySphStrong sphalerite and rare chalcopyrite in an early quartz-albite stockwork and nearby fractures.

1% 6%

208,60 209,00 0,40 PoCpyWeak pyrrhotite and chalcopyrite mineralization in quartz and quartz-albite veins.

1% 2%

210,30 210,80 0,50 PoModerate pyrrhotite mineralization in quartz-chlorite veins.

4%

244,80 245,30 0,50 PyWeak pyrite mineralization associated with epidote alteration around fractures.

1%

269,00 269,40 0,40 PyVery weak pyrite mineralization in a grey quartz vein.

1%


Sample Id From To Length Comments Id Au Ag Co Cu Ni Pb Zn

38390 127,30 128,30 1,00Shear zone with grey quartz veins and strong pyrite and pyrrhotite mineralization.

38391 129,60 130,70 1,10 Strong pyrite mineralization.38392 130,70 131,80 1,10 Strong pyrite mineralization.38393 0,00 Blank 238394 0,00 Standard 6Pc

38395 131,80 132,90 1,10Strong pyrite and pyrrhotite mineralization with quartz veins.

38396 132,90 134,00 1,10Strong pyrite and pyrrhotite mineralization with quartz veins.

38397 143,10 144,00 0,90 Strong pyrite mineralization.38398 163,00 164,00 1,00 Silky quartz-albite veins.

38399 207,20 207,70 0,50Strong sphalerite and rare chalcopyrite mineralization in a quartz-albite stockwork.

38400 207,70 208,60 0,90 Quartz-carbonate veins.

38401 208,60 209,00 0,40Pyrrhotite with sub-parallel quartz and quartz-albite veins.

38402 209,00 210,30 1,30Pervasive silicification of the matrix in breccias.

38403 210,30 210,80 0,50Strong pyrrhotite mineralization with quartz veins. < 0.01 < 0.2 0,003 0,006 0,007 < 0.001 0,007

38404 224,60 225,30 0,70 Concentration of quartz veins. 0,01 0,2 0,003 0,007 0,009 < 0.001 0,009

38405 225,30 226,00 0,70Large quartz-tourmaline vein with fragments of previous vein. 0,01 < 0.2 0,002 0,004 0,007 < 0.001 0,007

38406 232,40 233,60 1,20 Pervasive silicification. < 0.01 < 0.2 < 0.001 0,003 0,001 < 0.001 0,00538407 233,60 234,80 1,20 Pervasive silicification. < 0.01 < 0.2 < 0.001 0,002 0,002 < 0.001 0,011

38408 244,80 245,30 0,50Strong epidotization around fractures and weak pyrite mineralization. 0,01 < 0.2 0,002 0,004 0,009 < 0.001 0,006

38409 262,80 263,90 1,10 Quartz-tourmaline veins. < 0.01 < 0.2 0,003 0,005 0,012 < 0.001 0,00938410 269,00 269,40 0,40 Grey quartz vein. 0,01 < 0.2 0,003 0,006 0,01 < 0.001 0,00738411 293,80 294,80 1,00 Silicification and veins in shear zone. 0,01 < 0.2 0,003 0,007 0,01 < 0.001 0,009

Assays

Hole No. : C-10-27Date : 2010/06/01 - 03Logged by : Matthieu Vallée Sheet of


1 33,00 36,90 3,90 3,90 100% 2,88 74%2 36,90 41,10 4,20 4,20 100% 3,62 86%3 41,10 45,30 4,20 4,20 100% 3,76 90%4 45,30 49,60 4,30 4,30 100% 3,60 84%5 49,60 53,80 4,20 4,20 100% 3,64 87%6 53,80 58,10 4,30 4,30 100% 3,50 81%7 58,10 62,40 4,30 4,30 100% 3,58 83%8 62,40 66,60 4,20 4,00 95% 2,80 67%9 66,60 70,80 4,20 4,20 100% 3,28 78%10 70,80 74,90 4,10 3,90 95% 3,17 77%11 74,90 79,20 4,30 4,20 98% 2,64 61%12 79,20 83,40 4,20 4,20 100% 3,51 84%13 83,40 87,60 4,20 4,10 98% 3,84 91%14 87,60 91,90 4,30 4,30 100% 4,12 96%15 91,90 96,10 4,20 4,20 100% 3,75 89%16 96,10 99,90 3,80 3,20 84% 1,88 49%17 99,90 103,50 3,60 3,50 97% 1,65 46%18 103,50 106,80 3,30 3,00 91% 1,11 34%19 106,80 110,90 4,10 3,80 93% 1,75 43%20 110,90 114,90 4,00 4,00 100% 2,97 74%21 114,90 119,00 4,10 4,10 100% 3,63 89%22 119,00 123,30 4,30 4,30 100% 3,97 92%23 123,30 127,50 4,20 4,20 100% 3,45 82%24 127,50 131,70 4,20 4,20 100% 3,08 73%25 131,70 135,90 4,20 4,20 100% 3,71 88%26 135,90 140,20 4,30 4,30 100% 3,90 91%27 140,20 144,50 4,30 4,30 100% 3,25 76%28 144,50 148,70 4,20 4,10 98% 3,47 83%29 148,70 152,80 4,10 4,10 100% 3,35 82%30 152,80 157,10 4,30 4,20 98% 3,80 88%31 157,10 161,20 4,10 4,10 100% 3,51 86%32 161,20 165,50 4,30 4,30 100% 3,91 91%33 165,50 169,80 4,30 4,30 100% 3,78 88%34 169,80 174,00 4,20 4,20 100% 3,80 90%35 174,00 178,30 4,30 4,30 100% 3,90 91%36 178,30 182,70 4,40 4,30 98% 3,90 89%37 182,70 187,00 4,30 4,30 100% 4,10 95%38 187,00 191,20 4,20 4,20 100% 3,83 91%39 191,20 195,50 4,30 4,30 100% 4,04 94%40 195,50 199,90 4,40 4,40 100% 4,22 96%41 199,90 204,00 4,10 4,10 100% 3,65 89%42 204,00 208,30 4,30 4,30 100% 3,64 85%43 208,30 212,60 4,30 4,30 100% 3,80 88%44 212,60 216,80 4,20 4,10 98% 3,52 84%45 216,80 221,10 4,30 4,30 100% 3,88 90%46 221,10 225,40 4,30 4,20 98% 3,62 84%47 225,40 229,80 4,40 4,40 100% 3,94 90%48 229,80 234,10 4,30 4,30 100% 3,68 86%49 234,10 238,20 4,10 4,10 100% 3,67 90%

Geotechnical Log


50 238,20 242,50 4,30 4,30 100% 4,10 95%51 242,50 246,70 4,20 4,20 100% 3,63 86%52 246,70 250,90 4,20 4,10 98% 3,02 72%53 250,90 254,70 3,80 3,50 92% 2,64 69%54 254,70 258,90 4,20 4,00 95% 3,32 79%55 258,90 263,00 4,10 4,10 100% 3,35 82%56 263,00 267,40 4,40 4,40 100% 4,27 97%57 267,40 271,80 4,40 4,40 100% 4,23 96%58 271,80 276,10 4,30 4,30 100% 4,17 97%59 276,10 280,40 4,30 4,30 100% 3,94 92%60 280,40 284,80 4,40 4,40 100% 3,71 84%61 284,80 288,90 4,10 4,10 100% 3,82 93%62 288,90 293,00 4,10 4,10 100% 3,65 89%63 293,00 297,40 4,40 4,40 100% 3,94 90%64 297,40 301,70 4,30 4,30 100% 4,23 98%65 301,70 302,00 0,30 0,30 100% 0,30 100%

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-28A L-5500E 2855N 300 Grid North-50 83m 02-févr-10 03-févr-10 GV 02/06/10

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 61,50 61,50 OB overburden casing61,50 74,00 12,50 Tuf fg green matrix w 30 % elongated white clasts74,00 83,00 9,00 STuf vfg greyish tuff w 3% mm cal v

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments70,00 fg black & white bloc, dyke????

DDH Depth

Hole C-10-28-ADDH Depth Recovery RQD Blocky core Crumbly core Fault gouge Comments

Box no. From To Length % Length % Comments % % From To1 61,5 64,7 3,2 2,43 76% 0 0% 252 64,7 68,5 3,8 2,66 70% 0,43 11% 503 68,5 74 5,5 1,83 33% 0,24 4% 754 74 83 9 1,76 20% 0,77 9% 50

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-28B L-5500E 2850N 300 Grid North-50 77m 03-févr-10 05-févr-10 GV 02/06/10


54,00 77,00 23,00 Tuffg medium green to dark w 5-20% mostly pale clasts w 1% py & loc mm-cm qz-cal v w loc cal breccia

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments58,60 58,90 0,30 cm qz-cal v 10 to CA w low py61,1 61,3 0,20 breccia zone w cal64,35 64,45 0,10 mm qz-cal v65,05 65,25 0,20 faulting65,6 contact between dark tuff and medium green72,8 73,40 0,60 cm qz-cal v 10 to CA w 2% Cpy75,20 75,40 0,20 cm qz-cal v 10 to CA w 2% Cpy & 1% py

DDH Depth

Sample Id From To Length Id Comments Au Ag46097 68,45 68,60

72,8 73,4075,20 75,40 0,90

Assays

3 Composite mm-cm qz-cal v w Cpy

Hole C-10-28-BDDH Depth Recovery RQD Blocky core Crumbly core Fault gouge Comments

Box no. From To Length % Length % Comments % % From To1 54 57,8 3,8 3,83 101% 2,93 77% 02 57,8 62,6 4,8 4,01 84% 3,08 64% 53 62,6 66,8 4,2 4,24 101% 3,90 93% 04 66,8 71 4,2 4,17 99% 3,59 85% 05 71 75,3 4,3 4,23 98% 4,01 93% 06 75,3 77 1,7 1,6 94% 1,47 86% 0

EOH


0,00 40,30 40,30 OB Casing40,30 43,50 3,20 GrS Black graphite siltstone. Very well foliated at 45° c.a. Many pyrite masses, 2-20% of the rock.43,50 72,70 29,20 Tuf Grey lapilli tuff. Fragments are mostly of felsic nature. Well foliated at 30° c.a.

72,70 77,10 4,40 GrSBlack graphite siltstone. Very well foliated at 30° c.a. Many pyrite crystals and masses, 1-10% of the rock.

77,10 82,70 5,60 Tuf Gray-green lapilli and bomb tuff. Large rounded fragments of felsic rock. Foliated at 30° c.a.

82,70 136,20 53,50 DiDDark gray to greenish and black medium-grained diabase dyke. Lightly to strongly magnetic. Fine-grained and darker near the contacts. Very few fractures and veins, with rare chlorite ones. Contacts are sharp at 30° c.a.

136,20 137,90 1,70 GrSBlack graphite siltstone. 5% pyrite. Well-foliated at 30° c.a. Sharp contact with subsequent lithology at 30° c.a.

138,50 151,30 12,80 AAnStrong shear zone in what probably used to be andesite. Moderate to very strong foliation at 20° c.a. Strong silicification and, in places, albitization.

151,30 170,30 19,00 MAn Green fine-grained andesite. Moderate to strong foliation at 45° c.a.

170,30 184,70 14,40 PoDReddish brown quartz-feldspar porphyry. Red colour appears to be linked with iron oxides rather than k-feldspars. Porphyrs are mostly feldspars, and form up to 60% of the rock in the center of the dyke, and as low as 5% in the margins. Sharp contacts at 80° c.a. upper and 30° c.a. lower.

184,70 223,60 38,90 MAnGreen fine-grained andesite. Well foliated at 30° c.a., often with small veinlets of calcite parallel to foliation. Later quartz veins sometimes cut through the foliation. Both veins are mostly barren.

223,60 245,50 21,90 DiDBlack fine to medium grained diabase dyke. No fractures or veins. Upper contact is blocky, lower is sharp at 30° c.a. Chill margins: lighter colour and nearly aphanitic.

245,50 249,90 4,40 MAnBlack and light green very fine grained (mylonitic?) andesite. Highly foliated at 30° c.a. Several pinch and swell orange calcite veins.

249,90 253,30 3,40 MAnGreen fine-grained andesite. Moderately foliated at 20° c.a. with many small bands of calcite parallel to foliation.

253,30 261,30 8,00 InDLight brown fine-grained intermediate dyke. Many large (largest at least 10cm) angular fragments of what seems to be either granite or pegmatite. Contacts are sharp at 20° c.a.

261,30 270,20 8,90 MAnDark green fine-grained andesite. Well foliated at 10° c.a. with many small bands of calcite parallel to foliation.

270,20 282,80 12,60 SyDDeep pink, medium-grained syenite? dyke. Grains are very fine in the margins and grow towards the center. Sharp contacts at 20° c.a.

282,80 338,00 55,20 SyD Red fine-grained to aphanitic syenite dyke. Upper contact is sharp, but not visible due to sampling.338,00 EOH

DDH Depth

Second Lithology From To L Id rock types, grain size, etc. Photo138,70 139,40 0,70 InD Dark gray fine-grained intermediate dyke. Unaltered and unfoliated.

151,30 151,50 0,20 InDDark gray fine-grained intermediate dyke. Unaltered and unfoliated. Contacts at 20° c.a.

159,70 160,50 0,80 InDDark gray fine-grained intermediate dyke. Weakly foliated parallel to contacts at 40° c.a.

194,15 194,20 0,05 InD Dark gray, fine-grained intermediate dyke. Contacts at 40° c.a.

196,80 197,40 0,60 InDDark gray fine-grained intermediate dyke. Upper contact is sharp at 45° c.a. Lower is blocky, possible fault gouge.

266,90 269,60 2,70 FeD

Pale orange near aphanitic, possibly granitic, dyke. Made primarily of silica and k-feldspar, it could also be a vein, striking near parallel to c.a. Contacts are sharp, but wavy: upper is sub-parallel to c.a., with a sharp cut-off, lower is a sharp cut-off at 90° c.a. Andesite is altered to a light green colour near the margins.

276,30 279,60 3,30 PoDLight brown to greenish-brown intermediate porphyry dykes. Later event than syenite, which it cuts. Feldspar porphyrs form up to 30% of the rock in the center, 5% in the margins. Sharp contacts at 20° c.a.

284,80 285,20 0,40 MaDDark green and red fine-grained mafic dyke. Inclusions of the syenite in the margins. Very well foliated at 20° c.a.



298,40 305,00 6,60 MaDDark green fine-grained mafic dyke. Inclusions of the syenite in the margins. Very well foliated at 20-40° c.a.

316,50 323,10 6,60 MaDDark green and red fine-grained mafic dyke. Inclusions of the syenite in the margins. Very well foliated at 10-30° c.a.



Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal Alb

137,90 151,30 13,40 SZ

Strong shear zone, with silicification, albitization and very strong pyrite mineralization. Many grey quartz veins. Foliation decreases with depth, going from very strong to moderate, at about 30-45° c.a. Unless noted otherwise in mineralization, rock contains about 2-5% pyrite.

45° 25% 2%

151,50 161,00 9,50 QtzMany small quartz veins, bearing little to no visible mineralization, following the foliation of the rock. Localized breccia filled with calcite at 152.6.

45° 8%

161,00 165,10 4,10 QAlbSeveral quartz-albite veins, bearing little to no visible mineralization. Veins are discontinuous and deformed, probably early.

45° 2% 2%

208,80 210,90 2,10 QCa2 medium carbonate-quartz veins, striking at 20° c.a. The first (1cm) has chalcopyrite on its contacts with the rock. The second has moderate pyrite mineralization in and around the vein.

20° 1% 2%

218,60 219,60 1,00 StkA possible stockwork of pink-gray calcite veins, associated with strong pyrite mineralization of the wall rock and possible traces of sphalerite.

282,90 284,50 1,60 QtzSeveral small quartz veins with moderate to strong pyrite mineralization. Weak epidote alteration of the wall rock.

3%

324,30 328,20 3,90 QtzA few small quartz veins with very weak pyrite mineralization. Associated with an aphanitic zone from 325.9 to 328.0.

2%

Depth Veins(%)

From To L Id Description Serp Asb Chl Epi Alb Sil Serp Asb Chl Epi Alb Sil

137,90 138,50 0,60 AlbStrong albitization of the wall rock, giving it a beige colour. Associated with very small quartz veins and moderate pyrite mineralization.

3

138,50 144,30 5,80 SilStrong silicification of the rock in a shear zone, sometimes completely replace by quartz. Some strong pyrite mineralization.

4

144,30 145,80 1,50 Alb

Strong albitization of the wall rock, giving it a beige colour. In the center a quartz-chlorite vein with very strong pyrite mineralization. Elsewhere, moderate to strong pyrite mineralization associated with grey quartz veins.

4

145,80 151,30 5,50 SilStrong silicification of the rock in a shear zone, sometimes completely replace by quartz. Some strong pyrite mineralization.

3

282,90 284,50 1,60 EpiWeak and limited epidote alteration near small quartz veins.

3%


From To L Id Py Cpy Ars Sph40,30 43,50 3,20 Py 2-20% pyrite masses in graphite siltstone. 10%72,70 77,10 4,40 Py 1-10% pyrite crystals and masses in graphite siltstone. 5%

136,20 137,90 1,70 Py 5% pyrite in graphite siltstone. 5%

137,90 138,50 0,60 Py5% pyrite associated with strong albitization and small quartz veins.

5%

139,60 140,90 1,30 Py20% pyrite mineralization in a very strong shear zone. Associated with grey quartz veins and near complete silicification of the rock.

20%

144,90 145,30 0,40 Py15% pyrite, mostly as a vein cutting in the center of a 10cm quartz-chlorite vein.

15%

208,80 209,90 1,10 CPyChalcopyrite plaque in the contacts between a carbonate-quartz vein and the wall rock.

1%

209,90 210,90 1,00 PyModerate pyrite mineralization in and around a quartz-carbonate vein.

3%

218,60 219,60 1,00 SphStrong pyrite mineralization and possible traces of sphalerite in a stockwork of pink-gray calcite veins.

5% 1%

266,90 269,60 2,70 Py Very weak pyrite mineralization in a granitic dyke or vein. 1%282,90 284,50 1,60 Py 5% pyrite mineralization near small quartz veins. 5%

324,30 328,20 3,90 PyVery weak pyrite mineralization associated with small quartz veins.

1%


Sample Id From To Length Comments Id Au Ag

38412 208,80 209,90 1,10Chalcopyrite plaque in a carbonate-quartz vein.

38413 209,90 210,90 1,00 Moderate pyrite in a carbonate-quartz vein.

38414 218,60 219,60 1,00Strong pyrite mineralization around a possible calcite vein stockwork. Possible traces of sphalerite as well.

Assays


Box# From To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 40,30 43,65 3,35 3,35 100% 2,16 64%2 43,65 47,90 4,25 4,20 99% 3,36 79%3 47,90 52,10 4,20 4,20 100% 3,57 85%4 52,10 56,30 4,20 4,20 100% 3,55 85%5 56,30 60,50 4,20 4,20 100% 2,70 64%6 60,50 64,70 4,20 4,20 100% 3,23 77%7 64,70 68,90 4,20 4,10 98% 3,00 71%8 68,90 73,05 4,15 4,15 100% 2,95 71%9 73,05 77,25 4,20 4,10 98% 2,16 51%10 77,25 81,40 4,15 4,15 100% 3,25 78%11 81,40 85,60 4,20 4,20 100% 3,06 73%12 85,60 89,80 4,20 4,20 100% 3,48 83%13 89,80 93,80 4,00 4,00 100% 3,12 78%14 93,80 98,00 4,20 4,20 100% 3,30 79%15 98,00 101,20 3,20 3,20 100% 2,03 63%16 101,20 105,20 4,00 4,00 100% 3,68 92%17 105,20 109,40 4,20 4,20 100% 3,37 80%18 109,40 113,40 4,00 3,80 95% 2,30 58%19 113,40 117,60 4,20 4,20 100% 3,25 77%20 117,60 121,80 4,20 4,20 100% 3,30 79%21 121,80 126,00 4,20 4,20 100% 3,40 81%22 126,00 130,30 4,30 4,30 100% 3,70 86%23 130,30 134,40 4,10 4,10 100% 3,50 85%24 134,40 138,60 4,20 4,20 100% 2,62 62%25 138,60 143,00 4,40 4,30 98% 3,20 73%26 143,00 146,80 3,80 3,80 100% 2,90 76%27 146,80 150,70 3,90 3,90 100% 3,05 78%28 150,70 154,70 4,00 4,00 100% 3,00 75%29 154,70 158,50 3,80 3,60 95% 2,30 61%30 158,50 162,80 4,30 4,10 95% 3,08 72%31 162,80 166,80 4,00 4,00 100% 3,19 80%32 166,80 170,90 4,10 4,10 100% 3,10 76%33 170,90 175,10 4,20 4,20 100% 3,24 77%34 175,10 179,20 4,10 4,10 100% 3,28 80%35 179,20 183,30 4,10 4,10 100% 3,20 78%36 183,30 187,50 4,20 4,10 98% 3,07 73%37 187,50 191,70 4,20 4,20 100% 3,95 94%38 191,70 196,10 4,40 4,30 98% 4,30 98%39 196,10 200,40 4,30 4,10 95% 4,00 93% 197,2 197,440 200,40 204,50 4,10 4,10 100% 3,20 78%41 204,50 208,70 4,20 4,20 100% 3,38 80%42 208,70 212,90 4,20 4,20 100% 4,12 98%

Geotechnical Log

Fracture Angle/Frequency TallyHighly Broken Fault Gouge

43 212,90 217,10 4,20 4,20 100% 3,67 87%44 217,10 221,40 4,30 4,30 100% 3,75 87%45 221,40 225,30 3,90 3,70 95% 2,56 66%46 225,30 229,40 4,10 4,10 100% 3,47 85%47 229,40 233,80 4,40 4,30 98% 3,84 87%48 233,80 238,20 4,40 4,30 98% 3,70 84%49 238,20 242,40 4,20 4,20 100% 3,90 93%50 242,40 246,60 4,20 4,20 100% 3,50 83%51 246,60 250,90 4,30 4,20 98% 3,96 92%52 250,90 255,00 4,10 4,10 100% 3,64 89%53 255,00 259,00 4,00 4,00 100% 2,81 70%54 259,00 263,10 4,10 4,10 100% 3,36 82%55 263,10 267,50 4,40 4,40 100% 3,17 72%56 267,50 271,70 4,20 4,20 100% 3,10 74%57 271,70 275,40 3,70 3,70 100% 3,10 84%58 275,40 279,80 4,40 4,20 95% 2,48 56%59 279,80 283,90 4,10 4,10 100% 3,41 83%60 283,90 287,90 4,00 3,90 98% 2,73 68%61 287,90 292,20 4,30 4,30 100% 3,32 77%62 292,20 296,40 4,20 4,20 100% 3,84 91%63 296,40 300,70 4,30 4,30 100% 3,98 93%64 300,70 305,00 4,30 4,30 100% 3,88 90%65 305,00 309,30 4,30 4,30 100% 3,90 91%66 309,30 313,60 4,30 4,30 100% 3,66 85%67 313,60 317,30 3,70 3,70 100% 2,60 70%68 317,30 321,60 4,30 4,30 100% 3,58 83%69 321,60 325,90 4,30 4,30 100% 4,13 96%70 325,90 329,90 4,00 3,90 98% 2,18 55%71 329,90 334,00 4,10 4,10 100% 3,97 97%72 334,00 338,00 4,00 3,80 95% 3,44 86%

EOH Note: Already sampled, recuperation and RQD values could be very different from original ones.

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-30 L-5900E 2775N 300 Grid North-50 300m 22-févr-10 26-févr-10 GV June 3-5 2010


49,00 59,30 10,30 MAnfg medium green w loc epi alt w mm-cm qz-cal v & v clusters, w py & po reddish-brown alt

59,30 69,40 10,10 Tuf fg medium green, greyish w loc foliation 45 to CA

69,40 92,70 23,30 Tuf

fg matrix var from black t grey, foliation 45 to CA w deformation, bedded & diss py & po?, mm-cm qz-cal v w loc black matrix w pale clasts

92,70 117,60 24,90 Tuffg medium green, greyish w loc epi alt w mm-cm qz-cal v & v clusters, w py & po, loc silicification, tr Cpy

119,20 123,6 4,40 GSis vfg black w qz-cal and 3% py

123,60 143,8 20,20 Tuffg medium green w loc mm-cm qz-cal v w alt & 3% py and loc 3% Cpy, loc foliation 30 to CA

143,80 180,2 36,40 Tuf fg black w loc foliation, loc mm-cm qz-cal v w py & po

180,20 192,5 12,30 Tuffg medium green w var in % clasts & aspect (rounded or elongated, w loc qz-cal v & silicified zone

192,50 213,5 21,00 Tuf

fg black w foliation 45 to CA w var in graphite content w 5% py elongated fragments, nodula or bedded w loc qz-cal beds // to foliation

213,50 249,3 35,80 Tuf

fg medium green w var in % clasts & aspect (rounded or elongated ( w var in matrix color, pale to dark, and in % of clasts and silica) important alt

249,30 287 37,70 Tuf fg grey to black (w var in graphite content & % of clasts)287,00 300 13,00 STuf Tuff w high silica & potassic alt (no graphite)

EOH

DDH Depth

Lithology of Sub-units

From To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments54,60 55,70 1,10 InD fg black w 5 cm qz-cal v at 55.2m65,85 2 cm qz-cal v 60 to CA67,7 68,7 1,00 zone w 3-4% py & vugs in bedded py 30 to CA75,9 76,2 1 cm qz-cal v 10 to CA79,2 79,80 0,60 InD fg black w black mineral83,6 84,00 1 cm qz-cal v 10 to CA85,1 2 cm qz-cal v 45 to CA w 2% py89,2 89,60 qz-cal v 10 to CA94,4 2 cm qz-cal v 50 to CA w chlo & 1% py95 1 cm qz-cal v 45 to CA w 1% py altered98,1 98,15 0,05 InD fg black w black mineral

101,8 103,80 2,00zone w black matrix & high silica content?? & 3 cm qz-cal v at 103.5 m

103,50 5 cm qz-cal v 20 to CA v py & <1% Cpy ???104,20 104,60 0,40 cm qz-cal v w alt & 3% py106,00 2 cm qz-cal v 30 to CA106,90 1 cm qz-cal v w 3% py109,10 2 cm qz-cal v 30 to CA110,60 2 cm qz-cal v 25 to CA w 2% py113,40 114,15 0,75 zone w cm qz-cal v & alt117,60 119,20 1,60 fg medium green w 45% white phX128,45 129,00 0,55 GSis vfg black w foliation 45 to CA w qz-cal, graphite129,35 130,60 1,25 GSis vfg black w foliation 45 to CA w qz-cal, graphite130,60 132,80 2,20 cm qz-cal v w high alt & >5% py137,90 139,30 1,40 5 cm qz-cal v 10 to CA w alt w 3% py142,5 2 cm qz-cal v w py & 5-7% Cpy143,35 2 cm qz-cal v w py & black mineral in v

147,852 cm qz-ca v 90 to CA w unidentified brown mineral (sheets) biotite?

151,4 1 cm qz-cal v w py and po154,8 154,95 0,15 5 cm qz-cal v 30 to CA156 2 cm qz-cal v w 5% po159,4 2 cm qz-cal v 30 to CA165,95 166,3 0,35 qz-cal v w 3% po w chlo168,2 1cm qz-cal v w po & brownish mineral (sticks??) 45 to CA168,5 1 cm qz-cal v w py & po w unidentified brown mineral 45 to CA169,7 mm qz-cal v w 2% po177,4 178,2 0,80 zone w mm qz-cal v 3% po & foliation 45 to CA

DDH Depth

180,1 180,15 0,05 2 cm qz-cal v 45 to CA w 2% po190,85 2 cm qz-cal 50 to CA w po & Cpy (green qz)191,7 192,5 0,80 zone w mm-cm qz-cal v w 3% py & 2% po203,3 203,8 0,50 var in tuff, fg grey w diss py213,6 213,75 0,15 zone w qz alt w py and small reddish crystals, sphalerite216,3 216,45 0,15 py in v w vug219,7 220,4 0,70 zone w qz-cal v w green foliation 45 to CA w py & po221,25 221,3 0,05 mm qz-cal v w sphalerite w py222,6 223 0,40 zone w mm-cm qz-cal v w py & po, w epi alt224,2 224,3 0,10 5 cm qz-cal v w py, po & small crystals sphalerite222,6 226,2 3,60 zone w 5% diss py232,5 232,6 0,10 qz-cal v 45 to CA233,5 234,2 0,70 InD fg dark green w low diss py239 244,3 5,30 zone w high silica & Fd alt w 5cm qz-cal at 241.1m245 245,7 0,70 2 cm qz-cal v at 10 to CA w diss py250,50 265,3 14,80 InD fg grey-reddish w 50 % white phX270,8 271,4 0,60 fg black w 50% py bedded273,6 274,7 1,10 fg grey bedded w 5% py & 1% po, no clasts274,7 279,3 4,60 zone fg black w white cm clasts, high silica content279,3 279,7 0,40 fg black w 25% bedded py280,55 280,65 0,10 fg black w py v w vugs285,8 286,1 0,30 fg black zone w spider's web texture w mm white v287,25 291,25 4,00 zone w high alt w py, po & sphalerite294,2 296,2 2,00 fg dark green w high chlo content299,8 300 0,20 zone w mm qz-cal v w py & tr Cpy & alt

From To Length Id Description CA Py Po Cpy Sph Gal Mag67,7 68,7 1,00 zone w 3-4% py & vugs in bedded py 30 to CA 30 385,1 2 cm qz-cal v 45 to CA w 2% py 45 294,4 2 cm qz-cal v 50 to CA w chlo & 1% py 50 195 1 cm qz-cal v 45 to CA w 1% py altered 45 1103,50 5 cm qz-cal v 20 to CA v py & <1% Cpy ??? 20 tr104,20 104,60 0,40 cm qz-cal v w alt & 3% py 3106,90 1 cm qz-cal v w 3% py 3110,60 2 cm qz-cal v 25 to CA w 2% py 25 2130,60 132,80 2,20 cm qz-cal v w high alt & >5% py 5137,90 139,30 1,40 5 cm qz-cal v 10 to CA w alt w 3% py 10 3142,5 2 cm qz-cal v w py & 5-7% Cpy 5156 2 cm qz-cal v w 5% po 5165,95 166,3 0,35 qz-cal v w 3% po w chlo 3169,7 mm qz-cal v w 2% po 2177,4 178,2 0,80 zone w mm qz-cal v 3% po & foliation 45 to CA 45 3180,1 180,15 0,05 2 cm qz-cal v 45 to CA w 2% po 45 2190,85 2 cm qz-cal 50 to CA w po & Cpy (green qz) 50191,7 192,5 0,80 zone w mm-cm qz-cal v w 3% py & 2% po 3 2203,3 203,8 0,50 var in tuff, fg grey w 5% diss py 5219,7 220,4 0,70 zone w qz-cal v w green foliation 45 to CA w py & po 45221,25 221,3 0,05 mm qz-cal v w sphalerite w py tr222,6 223 0,40 zone w mm-cm qz-cal v w py & po, w epi alt222,6 226,2 3,60 zone w 5% diss py 5270,8 271,4 0,60 fg black w 50% py bedded 50273,6 274,7 1,10 fg grey bedded w 5% py & 1% po, no clasts 5 1279,3 279,7 0,40 fg black w 25% bedded py 25287,25 291,25 4,00 zone w high alt w py, po & sphalerite tr299,8 300 0,20 zone w mm qz-cal v w py & tr Cpy & alt tr


Sample Id From To Length Id Comments Au Ag46098 113,25 114,15 0,90 SZ w py & reddish mineral46099 130,60 131,65 1,05 qz-cal v with alt w py46100 131,65 133,00 1,35 idem

46101 138,10 139,35142,40 142,55 1,40

46102 191,7 192,5 0,80 zone w mm-cm qz-cal v w 3% py & 2% po46103 213,6 213,75

216,3 216,45221,25 221,3224,2 224,3 0,45

46104 219,7 220,4222,6 223 1,10

46105 226,45 226,75227,20 227,50 0,60

46106 270,8 271,4279,3 279,7280,55 280,65 1,10

46107 287,75 288,10290,45 291,25 1,15

2 composite

3 composite

2 composite

Assays

2 composite SZ w py & qz-cal v w Cpy

4 composite w sphalerite & py

2 composite SZ w py & qz-cal v


Box no. From To Length % Length % Comments % % From To1 49 53 4 3,81 95% 0,9 23% 502 53 57,3 4,3 4,32 100% 2,65 62% 03 57,3 61,3 4 3,87 97% 2,45 61% 04 61,3 65,2 3,9 3,97 102% 3,47 89% 05 65,2 69,4 4,2 4,21 100% 4,13 98% 06 69,4 73,6 4,2 4,16 99% 3,81 91% 07 73,6 77,7 4,1 3,9 95% 1,91 47% 258 77,7 80,6 2,9 2,91 100% 1,20 41% 30

9 80,6 84,8 4,2 4,05 96% 3,75 89%few bloc dropped from the box, mixed 0

10 84,8 88,8 4 4,12 103% 3,61 90% 011 88,8 93 4,2 4,1 98% 3,47 83% 012 93 97,1 4,1 4,18 102% 2,41 59% 013 97,1 100,9 3,8 3,64 96% 1,46 38% 1014 100,9 104,2 3,3 3,9 118% 0,45 14% 2515 104,2 108,7 4,5 3,99 89% 2,64 59% 1016 108,7 113 4,3 4,2 98% 3,79 88% 017 113 117,2 4,2 4,1 98% 3,22 77% 018 117,2 121,4 4,2 4,2 100% 2,83 67% 019 121,4 125 3,6 4,22 117% 2,07 58% 020 125 129,1 4,1 4,09 100% 3,06 75% 021 129,1 133 3,9 4,02 103% 3,68 94% 022 133 137,2 4,2 4,26 101% 4,24 101% 023 137,2 141,4 4,2 4,22 100% 4,02 96% 024 141,4 145,7 4,3 4,23 98% 3,51 82% 025 145,7 149,9 4,2 4,17 99% 3,33 79% 026 149,9 154,2 4,3 4,25 99% 3,66 85% 027 154,2 158,6 4,4 4,25 97% 4,05 92% 028 158,6 162,9 4,3 4,25 99% 3,89 90% 029 162,9 167,1 4,2 4,17 99% 3,79 90% 030 167,1 171,5 4,4 4,20 95% 3,59 82% 031 171,5 175,8 4,3 4,32 100% 3,90 91% 032 175,8 180 4,2 4,08 97% 3,78 90% 033 180 184,2 4,2 4,13 98% 3,47 83% 034 184,2 188,6 4,4 4,24 96% 3,59 82% 035 188,6 192,9 4,3 4,22 98% 3,90 91% 036 192,9 197,2 4,3 4,20 98% 3,48 81% 037 197,2 201,4 4,2 4,26 101% 3,67 87% 038 201,4 205,7 4,3 4,05 94% 3,35 78% 039 205,7 209,2 3,5 3,70 106% 3,34 95%40 209,2 213,4 4,2 4,16 99% 3,42 81%41 213,4 217,6 4,2 4,16 99% 3,84 91%42 217,6 221,8 4,2 4,14 99% 3,55 85%43 221,8 226,1 4,3 4,17 97% 3,90 91%44 226,1 230,3 4,2 4,13 98% 3,67 87%

45 230,3 234,6 4,3 4,21 98% 3,41 79%46 234,6 238,8 4,2 4,16 99% 3,15 75%47 238,8 243,1 4,3 4,19 97% 3,62 84%48 243,1 247,3 4,2 4,23 101% 3,50 83%49 247,3 251,5 4,2 4,16 99% 3,90 93%50 251,5 255,7 4,2 4,14 99% 3,14 75%51 255,7 259,9 4,2 4,18 100% 3,93 94%52 259,9 264,1 4,2 4,22 100% 3,54 84%53 264,1 268,4 4,3 4,20 98% 3,62 84%54 268,4 272,7 4,3 4,22 98% 3,63 84%55 272,7 277,1 4,4 4,33 98% 3,87 88%56 277,1 281,4 4,3 4,16 97% 3,67 85%57 281,4 286,1 4,7 4,24 90% 3,60 77%58 286,1 289,8 3,7 4,06 110% 3,36 91%59 289,8 294 4,2 4,20 100% 3,16 75%60 294 298,2 4,2 4,08 97% 2,07 49%61 298,2 300 1,8 2,22 123% 1,67 93%

EOH


C-10-31 L-6100E 2650N 300m Grid North-50 236 04-mars-10 10-mars-10 GV June 5-6 2010


11,00 184,50 173,50 SyDfg grey to red matrix w 50 % white phX w black mineral & rock fragment, w loc dyke & qz-cal v, w 2% diss py

184,50 236,00 51,50 DiD vfg black-dark green, magnetic w 1% pyEOH

DDH Depth

Lithology of Sub-units

From To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments11,45 11,75 0,30 zone w cm qz-cal v w 3% py & red alt, 90 to CA13,9 14,65 0,75 zone w cm qz-cal v 10 to CA27,3 -27,30 3 cm qz-cal v w slivery mineral & py27,5 28,10 0,6029,3 31,50 2,2033 33,75 0,75 zone w cm qz-cal v w purple mineral???46,30 48,80 2,50 zone v qz-cal v 15-30 to CA w py & chlo50,00 50,90 0,90 fg red-black matrix w black mineral (sticks)60,30 63,45 3,15 fg reddish matrix w var in % white phX (0-25%)

70,30 70,80 0,50 zone w qz-cal v w black mineral in v & silvery mineral, 45 to CA57,20 71,50 14,30 mg grey-black matrix w 60% white phX w low py81,55 81,75 0,20 fg reddish matrix w black minerals

84,75 85,30 0,5520 cm qz-cal v w black bedded minerals Mo? in v w py & sphalerite

90,90 91,10 0,20 2 qz-cal v w black bedded mineral w py-Cpy & sphalerite95,25 95,80 0,55 zone w mm qz-cal v w py96,70 5 cm qz-cal v w high epi alt100,15 100,3 0,15 fg reddish w black mineral & greenish alt102,50 103,10 0,60 mm qz-cal v w mm epi v 45-90 to CA104 104,5 0,50 mm qz-cal v w mm epi v, 30 to CA118,15 120,8 2,65127,1 130,6 3,50134,4 134,75 0,35 20 cm qz-cal v w chlo143,4 143,9 0,50 zone w qz-cal v w intense & large epi alt153,1 2 cm qz-cal v w high epi alt154,25 154,6 0,35 zone w cm qz-cal v w chlo & <1 % py157 160 3,00 fg reddish & black w 2% py & epi alt160,8 162,3 1,50 zone w mm qz-cal v w epi alt162,75 163,05 0,30 fg reddish-black w 1% small phX169 170,2 1,20 fg reddish-black w 1% small phX180,2 182,7 2,50 DiD vfg dark green, magnetic

182,7 183,4 0,70transition zone, fg red-green-black w fibrous mineral, chrysotile & talc at top, ultramafic layer??

200,3 202,15 1,85 zone w qz-cal v & large epi alt207,2 207,8 0,60 qz-cal v w chlo & <1 % py219,9 220,25 0,35220,9 222,15 1,25

DDH Depth

fg reddish matrix w small black minerals

mm qz-cal v w epi v & alt 90 to CA

zone w epi alt & red mineral

From To Length Id Description CA Py Po Cpy Sph Gal Mag11,45 11,75 0,30 zone w cm qz-cal v w 3% py & red alt, 90 to CA27,3 -27,30 3 cm qz-cal v w slivery mineral & py46,30 48,80 2,50 zone v qz-cal v 15-30 to CA w py & chlo

84,75 85,30 0,5520 cm qz-cal v w black bedded minerals Mo? in v w py & sphalerite

90,90 91,10 0,20 2 qz-cal v w black bedded mineral w py-Cpy & sphalerite95,25 95,80 0,55 zone w mm qz-cal v w py154,25 154,6 0,35 zone w cm qz-cal v w chlo & <1 % py157 160 3,00 fg reddish & black w 2% py & epi alt207,2 207,8 0,60 qz-cal v w chlo & <1 % py



17,90 18,1527,25 27,35 0,55

46109 33,10 33,80 0,70 qz-cal v w purple mineral46110 46,25 46,75

47,35 48,1048,40 48,60 1,45

46111 70,30 70,85 0,55 qz-cal v w black mineral

46112 84,75 85,30 0,5520 cm qz-cal v w black bedded minerals Mo? in v w py & sphalerite

46113 90,95 91,15103,60 104,50 1,10

46114 118,15 118,70119,65 120,30127,20 127,45129,55 129,75 1,65

46115 143,4 144,2 0,80 zone w qz-cal v w intense & large epi alt4 composites, qz-cal v w epi alt

Assays

3 composite - qz-cal v

3 composite qz-cal v

2 composite, qz-cal v

Hole DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge Comments

Box no. From To Length % Length % Comments % % From To1 11 13,8 2,8 2,9 104% 1,57 56% 02 13,8 17,9 4,1 4,13 101% 3,20 78% 03 17,9 22,1 4,2 4,22 100% 3,26 78% 04 22,1 26,3 4,2 4,15 99% 3,70 88% 05 26,3 30,6 4,3 4,31 100% 2,82 66% 06 30,6 34,6 4 4 100% 1,72 43% 07 34,6 38,7 4,1 4,08 100% 2,83 69% 08 38,7 42,8 4,1 4,06 99% 3,19 78% 09 42,8 47 4,2 4,08 97% 3,20 76% 010 47 50,9 3,9 3,85 99% 2,37 61% 011 50,9 54,7 3,8 3,6 95% 1,37 36% 012 54,7 58,8 4,1 4,1 100% 2,80 68% 013 58,8 63 4,2 4,24 101% 1,99 47% 014 63 67,3 4,3 4,12 96% 2,30 53% 015 67,3 71,5 4,2 4,21 100% 3,24 77% 016 71,5 75,7 4,2 4,14 99% 2,61 62% 017 75,7 80 4,3 4,16 97% 3,26 76% 018 80 84,2 4,2 4,16 99% 2,01 48% 019 84,2 88,2 4 4,08 102% 2,39 60% 020 88,2 92,2 4 3,83 96% 1,70 43% 021 92,2 96,3 4,1 4,10 100% 3,16 77% 022 96,3 100,7 4,4 4,20 95% 2,88 65% 023 100,7 104,7 4 4,12 103% 3,50 88% 024 104,7 109,1 4,4 4,37 99% 3,78 86% 025 109,1 113,4 4,3 4,25 99% 3,40 79% 026 113,4 117,7 4,3 4,26 99% 3,39 79% 027 117,7 122 4,3 4,19 97% 3,29 77% 028 122 126,2 4,2 4,18 100% 3,56 85% 029 126,2 130,6 4,4 4,22 96% 3,45 78% 030 130,6 134,8 4,2 3,94 94% 3,18 76% 031 134,8 138,8 4 4,11 103% 3,67 92% 032 138,8 143,2 4,4 4,20 95% 3,95 90% 033 143,2 147,1 3,9 3,91 100% 2,60 67% 034 147,1 151,2 4,1 3,96 97% 3,15 77% 035 151,2 155,4 4,2 4,18 100% 3,60 86% 036 155,4 159,8 4,4 4,31 98% 3,91 89% 037 159,8 164,1 4,3 4,26 99% 3,32 77% 038 164,1 168,4 4,3 4,26 99% 3,54 82% 0

39 168,4 172,8 4,4 4,23 96% 3,62 82%40 172,8 177,1 4,3 4,27 99% 3,72 87%41 177,1 181,3 4,2 4,08 97% 3,23 77%42 181,3 185,5 4,2 4,10 98% 2,74 65%43 185,5 189,8 4,3 4,18 97% 3,00 70%44 189,8 194 4,2 4,11 98% 3,14 75%45 194 198,3 4,3 4,13 96% 3,81 89%46 198,3 202,5 4,2 4,13 98% 2,50 60%47 202,5 206,6 4,1 4,05 99% 2,77 68%48 206,6 210,9 4,3 4,19 97% 3,38 79%49 210,9 215,1 4,2 4,14 99% 3,62 86%50 215,1 219,4 4,3 4,24 99% 3,93 91%51 219,4 223,6 4,2 4,12 98% 2,67 64%52 223,6 227,8 4,2 4,10 98% 3,02 72%53 227,8 231,9 4,1 4,13 101% 2,92 71%54 231,9 236 4,1 4,00 98% 3,04 74%

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-32 L-6200E 2400N 300 Grid North-50 300m 11-mars-10 14-mars-10 GV June 7-8 2010


46,00 78,60 32,60 MAnfg medium green w loc mm qz-cal v, loc mm cal mm phX, w py, Cpy & po

78,60 228,60 150,00 PAnfg medium green w mm qz-cal v, loc brecciated zone, w py w pillow borders

228,60 247,20 18,60 MAn idem And247,20 274,75 27,55 PAn idem pillow274,75 288,4 13,65 SyD fg red matrix w elongated black minerals, dyke?288,40 302 13,60 MAn fg-mg green w mm cal v, w loc mg matrix w black phXEOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments46,35 47,00 0,65 10 cm qz-cal v 60 to CA w Cpy53,9 54,1 0,20 cm qz-cal v 60-70 to CA w py, Cpy68,65 69,8 1,15 InD fg pinkish71,15 71,30 0,15 InD fg pinkish, alt?77,25 77,80 0,55 fg green w mm qz-cal v w chlo 45 to CA w py78,6 79,30 0,70 fg green w cm qz-cal v w deformation, py95,65 95,95 0,30 zone w 15 cm qz-cal w py, cpy & chlo98,5 5 cm qz-cal zone w 2% py, po98,55 98,80 0,25 InD fg dark, dyke?101,15 101,55 0,40 idem101,95 102,60 0,65 idem117,70 10 cm qz-cal v 45 to CA123,90 124,75 qz-cal v 10 to CA w tr cpy124,75 125,25 0,50 qz-cal v179,5 179,9 0,40 pillow border w qz181,50 181,75 0,25 idem w py & vugs185,55 187,10 1,55 InD fg grey w 2% py187,10 187,25 0,15 zone w qz-chlo & py19,80 1 cm pink qz-cal v208,75 208,85 0,10 pillow border w qz & py223,10 223,50 0,40 qz-cal v 10 to CA229,25 230,45 1,20 InD fg-mg red 236,5 236,75 0,25 2 cm qz-cal v w py & sphalerite238,55 5 cm qz-cal v w py243,7 243,9 0,20 qz-cal v w pink & green alt245,65 246 0,35 zone w qz-cal v & and 90 to CA248 250,3 2,30 zone w cm qz-cal v 10 to CA257,4 4 cm qz-al v266,45 272 5,55 And zone w mm qz-cal v clusters273,2 274,1 0,90 mg green SZ? Foliation // to CA274,1 274,75 0,65 pink qz-cal v w py 10 to CA274,75 277,4 2,65 transition zone, fg green-red279 279,25 0,25 mm qz-cal v 10 to CA w 3% Cpy & 2% py

284,1 284,75 0,65 InDfg green w 20% black phX, w pink-yellow cal v w cubic silvery minerals

285,8 286,2 0,40 40 cm qz-cal v w 2% py

DDH Depth

288,4 289,8 1,40 transition zone, fg green-red, w qz-cal v

From To Length Id Description CA Py Po Cpy Sph Gal Mag46,35 47,00 0,65 10 cm qz-cal v 60 to CA w Cpy 60 tr53,9 54,1 0,20 cm qz-cal v 60-70 to CA w py, Cpy 60 tr77,25 77,80 0,55 fg green w mm qz-cal v w chlo 45 to CA w py 4578,6 79,30 0,70 fg green w cm qz-cal v w deformation, py95,65 95,95 0,30 zone w 15 cm qz-cal w py, cpy & chlo tr98,5 5 cm qz-cal zone w 2% py, po 2123,90 124,75 qz-cal v 10 to CA w tr cpy 10 tr181,50 181,75 0,25 idem w py & vugs185,55 187,10 1,55 InD fg grey w 2% py 2187,10 187,25 0,15 zone w qz-chlo & py208,75 208,85 0,10 pillow border w qz & py236,5 236,75 0,25 2 cm qz-cal v w py & sphalerite tr238,55 5 cm qz-cal v w py274,1 274,75 0,65 pink qz-cal v w py 10 to CA 10 2 3279 279,25 0,25 mm qz-cal v 10 to CA w 3% Cpy & 2% py 10284,1 284,75 0,65 InD fg green w 20% black phX, w pink-yellow cal v w cubic silvery minerals285,8 286,2 0,40 40 cm qz-cal v w 2% py 2


Sample Id From To Length Id Comments Au Ag

46118 50,95 51,4553,90 54,1056,10 56,20 0,80

46119 236,5 236,75237,65 238,00243,70 243,90 0,70

46120 273,15 274,70 1,55 SZ & qz-cal v46121 279,00 279,25

285,8 286,2 0,6546122 284,1 284,75 0,65 dyke w py & alt cal v

Assays

3 Composite w qz-cal v w py, cpy, po & sphalerite?

3 composite w qz-cal v w sphalerite & alt

2 composite, Qz-cal v w py & cpy


Box no. From To Length % Length % Comments % % From To1 46 48,2 2,2 1,91 87% 1,85 84% 02 48,2 52,7 4,5 4,32 96% 3,54 79% 03 52,7 56,9 4,2 4,1 98% 3,83 91% 04 56,9 61,1 4,2 4,2 100% 4,05 96% 05 61,1 65,3 4,2 4,07 97% 3,95 94% 06 65,3 69,6 4,3 4,23 98% 3,70 86% 07 69,6 74 4,4 4,35 99% 3,70 84% 08 74 78,2 4,2 4,27 102% 3,90 93% 09 78,2 82,4 4,2 4,17 99% 3,50 83% 010 82,4 86,7 4,3 4,2 98% 3,27 76% 011 86,7 91 4,3 4,25 99% 3,54 82% 012 91 95,4 4,4 4,26 97% 3,98 90% 013 95,4 99,7 4,3 4,22 98% 3,73 87% 014 99,7 104 4,3 4,31 100% 4,07 95% 015 104 108,3 4,3 4,21 98% 3,98 93% 016 108,3 112,5 4,2 4,22 100% 3,86 92% 017 112,5 117 4,5 4,26 95% 4,09 91% 018 117 121,3 4,3 4,27 99% 4,05 94% 019 121,3 125,6 4,3 4,25 99% 3,91 91% 020 125,6 129,9 4,3 4,23 98% 3,81 89% 021 129,9 134,2 4,3 4,16 97% 3,71 86% 022 134,2 138,4 4,2 4,24 101% 3,95 94% 023 138,4 142,7 4,3 4,12 96% 3,52 82% 1024 142,7 146,9 4,2 4,26 101% 3,58 85% 025 146,9 151,2 4,3 4,25 99% 3,98 93% 026 151,2 155,4 4,2 4,09 97% 3,40 81% 027 155,4 159,6 4,2 4,03 96% 3,43 82% 028 159,6 163,9 4,3 4,27 99% 3,99 93% 029 163,9 168,1 4,2 4,10 98% 3,50 83% 030 168,1 172,4 4,3 4,22 98% 3,85 90% 031 172,4 176,6 4,2 4,16 99% 3,68 88% 032 176,6 180,9 4,3 4,25 99% 4,02 93% 033 180,9 185,3 4,4 4,27 97% 3,90 89% 034 185,3 189,5 4,2 4,16 99% 3,13 75% 035 189,5 193,8 4,3 4,20 98% 4,08 95% 036 193,8 198,1 4,3 4,22 98% 3,64 85% 037 198,1 202,4 4,3 4,30 100% 4,30 100% 038 202,4 206,6 4,2 4,20 100% 3,65 87% 0

39 206,6 211 4,4 4,30 98% 4,07 92%40 211 215,2 4,2 4,12 98% 3,38 80%41 215,2 219,6 4,4 4,16 95% 3,71 84%42 219,6 223,8 4,2 4,15 99% 3,63 86%43 223,8 228 4,2 4,10 98% 3,34 80%44 228 232,1 4,1 4,09 100% 3,86 94%45 232,1 236,4 4,3 4,13 96% 3,79 88%46 236,4 240,7 4,3 4,23 98% 3,95 92%47 240,7 245 4,3 4,25 99% 3,26 76%48 245 249,3 4,3 4,22 98% 2,77 64%49 249,3 253,6 4,3 4,09 95% 3,63 84%50 253,6 257,9 4,3 4,13 96% 3,40 79%51 257,9 262 4,1 4,06 99% 3,21 78%52 262 266,2 4,2 4,11 98% 3,67 87%53 266,2 270,4 4,2 4,10 98% 3,56 85%54 270,4 274,7 4,3 4,19 97% 3,83 89%55 274,7 278,9 4,2 3,80 90% 2,33 55%56 278,9 283 4,1 3,90 95% 3,03 74%57 283 286,5 3,5 3,47 99% 2,09 60%58 286,5 290,5 4 3,58 90% 2,30 58%59 290,5 294,9 4,4 4,25 97% 4,01 91%60 294,9 299,1 4,2 4,20 100% 3,48 83%61 299,1 302 2,9 2,90 100% 2,40 83%

EOH

DDH X Y Elevation Azimuth Inclination EOH Started Completed Logged by Date NAD83 E NAD83 NC-10-33 L-6500E 2300N 300 Grid North-50 350m 15-mars-10 20-mars-10 GV June 8-10 2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 40,50 40,50 OB overburden casing stops at 29m

40,50 52,20 11,70 PAnvfg-fg non hom, green w black & white, pillow borders & mm black-green spots

52,20 71,30 19,10 MAn fg hom green w mm cal v & white spots71,30 217,70 146,40 PAn idem last pillow217,70 248,40 30,70 MAn fg dark green w qz-cal v highly deformed

248,40 347,25 98,85 PAnidem last pillow w proto-pillow w 3 loc cm qz-cal v w Cpy at 256.25m, 265.3m, 276.4m, w loc cm qz-cal v

347,25 350 2,75 ??? fg black-dark green, w red bed/alt w mm qz-cal v EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments53,25 54,75 1,50 MAn And w intense epi alt60,05 60,5 0,45 mg green And w epi alt in v, w py cpy70,75 71,3 0,55 cm qz-cal v w py74,1 74,40 0,30 20 cm qz-cal v 45 to CA w py & Cpy102 102,15 0,15 5 cm qz-cal v w py114,75 115,75 1,00 zone w mm cal v117,7 118,50 0,80 zone w mm cal v & cal breccia119 124,00 5,00 InD fg black w mm cal v119,95 120,15 0,20 fg green zone in dyke124,90 126,90 2,00 pillow border zone w cal v 2% py135,2 135,3 0,10 5 cm qz-cal v 45 to CA w epi136,30 136,50 0,20 10 cm qz-cal v w epi158,25 158,40 0,15 qz-cal v w diss py 30 to CA169,70 170,20 0,50 InD fg black 173,3 173,6 0,30 zone w qz-cal v 45 to CA w py & Cpy193,50 196,60 3,10 MAn fg green And mass200,90 201,30 0,40 qz-cal v w py & Cpy 60 to CA206,00 207,00 1,00 zone w qz-cal w py202,00 217,70 15,70 highly deformed zone w mm cal v 45 to CA230,7 239 8,30 zone w qz-cal v highly deformed234,1 tr Cpy243,00 245,00 2,00 qz-cal v 246,65 246,90 0,25 mm qz-cal v w 3% py and reddish mineral277,05 277,35 0,30 qz-cal v w reddish alt & tr Cpy303,1 310,5 7,40 InD fg grey w black elongated mineral & mm white phX306,2 5 cm qz-cal v w chlo & py309,5 309,7 0,20 2 qz-cal v w chlo, py and Cpy320,65 321,35 0,70 SZ 60 to CA w qz-cal v & epi alt327,3 328,6 1,30 InD fg dark w mm white phX w py & mm cal v

DDH Depth


74,10 74,40 1,0046124 93,25 93,40

99,80 100,05102,00 102,15 0,55

46125 200,90 201,30 0,40 qz-cal v w Cpy46126 246,65 246,90

249,70 249,85256,2 256,4 0,60

46127 265,20 265,40268,40 268,70276,30 276,65291,70 291,90 1,05

46128 306 306,45309,45 309,95 0,95

3 composite qz-cal in And w py & cpy

2 composite qz-cal v w Cpy in dyke

Assays

2 composite qz-cal v

3 composite qz-cal v in And

3 composite qz-cal v in And w py & cpy


Box no. From To Length % Length % Comments % % From To1 overburden2 overburden3 40,5 42,1 1,6 1,45 91% 1,08 67% 04 42,1 48,2 6,1 3,71 61% 2,72 45% 255 48,2 52,5 4,3 4,14 96% 3,70 86% 06 52,5 56,6 4,1 4,03 98% 3,03 74% 07 56,6 61 4,4 4,23 96% 3,86 88% 08 61 65,2 4,2 4,17 99% 3,48 83% 09 65,2 69,5 4,3 4,22 98% 3,10 72% 010 69,5 73,5 4 4,03 101% 3,48 87% 011 73,5 77,7 4,2 4,14 99% 3,64 87% 012 77,7 82 4,3 4,2 98% 3,70 86% 013 82 86,2 4,2 4,09 97% 3,49 83% 014 86,2 90,5 4,3 4,06 94% 3,82 89% 015 90,5 94,7 4,2 4,1 98% 3,30 79% 016 94,7 98,9 4,2 4,14 99% 3,73 89% 017 98,9 103,2 4,3 4,32 100% 4,03 94% 018 103,2 107,4 4,2 4,02 96% 3,55 85% 019 107,4 111,7 4,3 4,04 94% 3,70 86% 020 111,7 116,1 4,4 4,33 98% 4,20 95% 021 116,1 120,5 4,4 4,25 97% 3,74 85% 022 120,5 124,7 4,2 4,26 101% 3,67 87% 023 124,7 128,9 4,2 4,20 100% 3,88 92% 024 128,9 133,2 4,3 4,16 97% 3,74 87% 025 133,2 137,6 4,4 4,28 97% 4,04 92% 026 137,6 141,9 4,3 4,36 101% 3,90 91% 027 141,9 146,2 4,3 4,23 98% 3,83 89% 028 146,2 150,5 4,3 4,30 100% 3,87 90% 029 150,5 154,8 4,3 4,21 98% 4,10 95% 030 154,8 158,9 4,1 4,13 101% 3,69 90% 031 158,9 163,1 4,2 4,09 97% 3,64 87% 032 163,1 167,5 4,4 4,14 94% 3,90 89% 033 167,5 171,8 4,3 4,15 97% 3,60 84% 034 171,8 176 4,2 4,20 100% 2,73 65% 035 176 180,3 4,3 4,29 100% 3,86 90% 036 180,3 184,5 4,2 4,09 97% 4,00 95% 037 184,5 188,6 4,1 3,98 97% 3,23 79% 038 188,6 192,8 4,2 4,11 98% 3,35 80% 0

39 192,8 197 4,2 4,02 96% 2,95 70% 040 197 201,2 4,2 4,04 96% 3,32 79% 041 201,2 205,3 4,1 4,09 100% 3,61 88%42 205,3 209,4 4,1 3,96 97% 3,23 79%43 209,4 213,6 4,2 4,02 96% 3,54 84%44 213,6 217,9 4,3 4,25 99% 3,43 80%45 217,9 221,7 3,8 3,88 102% 1,91 50%46 221,7 225,7 4 4,04 101% 2,46 62%47 225,7 230 4,3 4,08 95% 3,59 83%48 230 234,2 4,2 4,07 97% 3,27 78%49 234,2 238,3 4,1 4,06 99% 3,70 90%50 238,3 242,2 3,9 3,82 98% 3,08 79%51 242,2 246,2 4 3,72 93% 1,93 48%52 246,2 250 3,8 3,74 98% 3,28 86%53 250 254,4 4,4 4,20 95% 3,91 89%54 254,4 258,7 4,3 4,20 98% 3,75 87%55 258,7 263 4,3 4,09 95% 3,61 84%56 263 267,3 4,3 4,24 99% 3,98 93%57 267,3 271,5 4,2 4,16 99% 3,72 89%58 271,5 275,8 4,3 4,20 98% 3,52 82%59 275,8 280 4,2 4,18 100% 3,75 89%60 280 284,3 4,3 4,06 94% 3,30 77%61 284,3 288,6 4,3 4,21 98% 4,03 94%62 288,6 293,1 4,5 4,25 94% 3,87 86%63 293,1 297,2 4,1 4,23 103% 3,77 92%64 297,2 301,5 4,3 4,19 97% 3,66 85%65 301,5 305,7 4,2 4,06 97% 3,98 95%66 305,7 310 4,3 4,28 100% 4,13 96%67 310 314,3 4,3 4,12 96% 3,60 84%68 314,3 318,6 4,3 4,28 100% 4,03 94%69 318,6 322,9 4,3 4,21 98% 4,12 96%70 322,9 327,2 4,3 4,15 97% 3,91 91%71 327,2 331,5 4,3 4,22 98% 3,69 86%72 331,5 335,7 4,2 4,08 97% 3,79 90%73 335,7 340,1 4,4 4,28 97% 3,75 85%74 340,1 344,4 4,3 4,23 98% 4,05 94%75 344,4 348,8 4,4 4,33 98% 3,68 84%76 348,8 350 1,2 1,16 97% 1,00 83%EOH

DDH X Y El Az Incl EOH Started Completed Logged by Date NAD83 E NAD83 N

C10-34 L-6200E 2400N 300 Grid North-50 350m 20/03/10 24-mars-10 AC and MV 05/28/2010 and 06/07-09/2010

Main Unit LithologyFrom To Length Id Rock type Photo Comments & scpt0,00 28,10 28,10 OB Overburden casing

28,10 41,25 13,15 PAnmgreen, fg, loc coarser pillow andesite w mm to cm chlo-cal, loc breciated chill margins 5%, w loc cm brecciated trile points, cm zone of white mm phX nil

41,25 67,00 25,75 Gabmg hom massie pale to med green and or leuco gabbro, w mm chlo cristals 2% w finer first 50 cm, loc decimetric gr size var from mg to mg-fg, last m is hom fg nil

67,00 78,00 11,00 PAnidem previous unit, pillow andesite, 4 photos 73.4 m cm chill margin w stratified inner pillow and proto pillow in the margin

78,00 123,20 45,20 PAnGreen aphanitic andesite pillows. Chill margins sometimes show quartz and/or carbonate filling, little to no mineralization unless noted.

123,20 136,3 13,10 DiDDark gray fine-grained diabase dyke. Upper contact is sharp at 20° c.a. Lower is difficult to discern.

136,30 157,7 21,40 PAnGreen aphanititc to fine-grained andesite pillows. Sometimes calcite and/or quartz filling of pillow chill margins, with no associated mineralization.

157,70 163,2 5,50 MAnGreen fine-grained andesite. Contacts are sharp with upper at 10° c.a. and lower at 40° c.a.

163,20 350 186,80 PAnGreen aphanititc to fine-grained andesite pillows. Sometimes calcite and/or quartz filling of pillow chill margins, with no associated mineralization.

EOH

DDH Depth

Lithology of Sub-unitsFrom To Length Id Rock types, Change in grain size, colour, etc. CA Photo MPP From To L Comments34,00 34,50 0,50 SZ cm SZ w bx chlo-cal chill margin 2036,55 36,75 0,20 Alt pale green massive qz-pl-ser alt zone

35,7 41,25 5,55MAn

fg and w 2%, loc 5% over 50 cm of mm cal veining & sw & tr py 45

51,35Gab

contact betwen vfg gabbro & mg gabbro w upper 50 cm gr size going from mg to fg & last 10 cm vfg 40

61 61,15 0,15 QCa cal-qz v w weak bx 8568,35 68,8 0,45 SZ weak shear zone in fg ± hom andesite, 2 cm cal-qz v @ 68.7 50

73,8 76,60 2,80Gab

hom mg gabbro dyke w 30 cm chill margins goimg from fg to aphanitic near contact 50

101,90 107,10 5,20

DiD

Gray-brown medium-grained diabase dyke. Becomes finer grained near upper contact and gradually becomes red and very-fine grained about 2m from the lower contact. Sharp contacts at 40° c.a. 40

111,50 112,10 0,60DiD

Dark gray fine-grained diabase dyke. Sharp contacts at 40° c.a. 40

117,90 119,10 1,20 DiD Gray fine-grained diabase dyke. Contacts are sharp at 30° c.a. 30

176,70 179,00 2,30InD

Dark gray fine-grained intermediate dyke. Contacts are sharp at 30° c.a. 30

179,70 180,30 0,60InD

Dark gray fine-grained intermediate dyke. Contacts are sharp and marked by quartz veins with pyrite mineralization, orientations at 45° c.a. 45

196,4 201,3 4,90MAn

Gray-green fine-grained andesite. Progressive contacts with the pillow andesite.

207,40 208,10 0,70DiD

Dark gray fine-grained diabase dyke. Sharp contacts at 20° c.a. 20

231,10 244,90 13,80

AAn

Dark green, fine-grained, altered andesite. From the margins to the center (236-240m): weakly to moderately foliated, 60° c.a. to sub-parallel to c.a. Also an increase in quartz-carbonate veinlets towards the center.

280,50 298,50 18,00PoD

Reddish brown quartz-feldspar porphyry dyke. Porphyrs make up to 20% of the rock. The margins become light brown. Sharp contacts, but non-linear, at about 30° c.a.

DDH Depth

303,70 310,35 6,65

PoD

Gray to light brown quartz-feldspar porphyry dyke. Porphyrs make up to 20% of the rock. Sharp contacts at 70° c.a. Andesite pillows are highly foliated for 1m near the lower contact.

331,90 333,40 1,50DiD

Dark gray fine-grained diabase dyke. Contacts are sharp at 40° c.a.

DDH Depth Structure (Intensity 1-5) Veining (%)From To Length Id comments BD CA SH CA FOL CA BX Q/C CA Q/A CA QZ CA CAL Q/Chl Q/Epi CA STW Photo

89,40 89,70 0,30QCa

Quartz-carbonate blocks, probably filling of breccia. No mineralization in the veins.

40 20

91,50 92,00 0,50QCa

Large carbonate vein with a few quartz-carbonate ones. Very weak pyritemineralization in the quartz-carbonate veins.

40 10 30

127,80 127,90 0,10QCa

1cm quartz-carbonate vein with epidotization of the wall rock. No visible mineralization.

45 10

128,80 129,40 0,60QCa

One 4cm wide quartz-carbonate vein, striking at 20° c.a. No mineralization.

20 10

178,40 178,60 0,20Qtz

Discontinuous 1cm wide quartz vein with moderate chalcopyrite mineralization.

30 10

179,70 180,30 0,60Qtz

Two 2cm wide quartz veins marking the borders of an intermediate dyke. Associated with moderate pyrite mineralization, mostly in the upper one.

30 20

182,50 183,20 0,70

QCa

Large pillow chill margin with quartz-carbonate and carbonate veins (filling?). Large euhderal pyrite crystals outside the veins. Upper orientation is 80° c.a., lower 45° c.a. in the other direction.

10 10

200,30 200,60 0,30QCa

One 3cm quartz-carbonate vein, striking 30° c.a. No mineralization.

30 20

206,70 206,90 0,20QCa

One 3cm quartz-carbonate vein, striking 40° c.a. No mineralization.

40 20

236,00 242,00 6,00QCa

Many small quartz-carbonate and carbonate veins and veinlets. Most are between 70-90° c.a. Generally little to no mineralization.

80 5 5

246,70 247,00 0,30QCa

One 1cm quartz-carbonate vein with strong pyrite mineralization, striking 20° c.a.

20 10

256,30 256,50 0,20Qtz

One 3cm wide quartz vein, striking 45° c.a. No visible mineralization.

45 20

257,00 257,20 0,20QAlb

Three medium quartz and quartz-albite veins, striking at 70° c.a. No visible mineralization.

70 25 10

262,60 262,90 0,30Ca

One 4cm wide carbonate vein, striking at 30° c.a. in a pillow chill margin. No mineralization.

30 20

280,80 280,90 0,10Ca

One 3cm wide carbonate vein, striking at 70° c.a. No visible mineralization.

70 20

303,90 308,50 4,60

QChl

Small to large quartz-chlorite veins, striking 60-90° c.a., with very weak pyrite mineralization. Largest are at 305.1m (10cm @ 60° c.a.) and at 306.9 (6cm @ 70° c.a.). A few with some red hematite.

70 5

324,00 324,20 0,20QCa

A 7cm wide carbonate-quartz vein, striking at 40° c.a. No visible mineralization.

40 30

325,60 326,80 1,20QCa

One 1cm wide grey quartz and carbonate vein, striking near parallel to c.a. Weak pyrite mineralization.

0 5

327,90 331,90 4,00QEpi

A few medium sized quartz-epidote veins. Very weak chalcopyrite mineralization.

8

333,80 338,30 4,50QEpi

A few medium sized quartz-epidote veins. No visible mineralization.

30 5

From To Length Id Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Cal Ank Tal Srp Chl SI Bio Fel Epi Lim Comments

127,80 127,90 0,10 Epi 10Epidotization of the wall rock extending by 1cm around vein.

231,10244,90 13,80 ChlTal 1 3

Pervasive alteration in chlorite and possibly talc. Strongest in the center.


From To Length Id Description CA Py Po Cpy Sph Gal Mag57,45 57,60 0,15 2% diss py fg CTCL 267,95 A 10 cm w 2% diss py w 1 cm qz-cal v in center 35 272,10 72,4 0,30 B 2 5 diss py w 2 1cm v qz-cal 35 277,35 C 10 cm w 2% diss py w 1 cm qz-cal v in center 35 2

91,50 92,00 0,50Py 1% pyrite in quartz-carbonate veins. 1

178,40 178,60 0,20 CPy 2% chalcopyrite in a small quartz vein. 30 2

179,70 180,30 0,60Py

4% pyrite in 2 quartz veins marking the borders of an intermediate dyke. 30 4

182,50 183,20 0,70Py

10% large euhedral pyrite in a large pillow chill margin. 10

236,80 236,90 0,10Py

5% pyrite in and aroun a 1cm quartz-carbonate vein striking sub-perpendicular to c.a. 90 5

237,70 237,90 0,20 Py 5% pyrite in a large carbonate "chunk". 5246,70 247,00 0,30 Py 4% pyrite in a small quartz-carbonate vein. 20 4303,90 308,50 4,60 Py 1% pyrite in euhedral crystals in quartz-chlorite veins. 70 1

325,60 326,80 1,20Py

2% pyrite mineralization in a grey quartz and carbonate vein. 0 1

327,90 331,90 4,00 CPy 1% chalcopyrite in quartz-epidote veins. 1


Sample Id From To Length Comments Id Au Ag38428 178,50 179,00 0,50 2% chalcopyrite in a small quartz vein.

38429 179,70 180,30 0,604% pyrite in 2 quartz veins marking the borders of an intermediate dyke.

38430 182,50 183,20 0,70 10% pyrite in a pillow chill margin.38431 236,00 237,00 1,00 Altered andesite with many veins.38432 237,00 238,00 1,00 Altered andesite with many veins.38433 238,00 239,00 1,00 Altered andesite with many veins.38434 239,00 240,00 1,00 Altered andesite with many veins.38435 240,00 241,00 1,00 Altered andesite with many veins.38436 241,00 242,00 1,00 Altered andesite with many veins.38437 0,00 Blank 338438 0,00 Standard 6Pc38439 246,70 247,00 0,30 4% pyrite in a small quartz-carbonate vein.38440 303,90 304,90 1,00 1% pyrite in quartz-chlorite veins.38441 304,90 305,90 1,00 1% pyrite in quartz-chlorite veins.38442 305,90 306,60 0,70 1% pyrite in quartz-chlorite veins.38443 306,60 307,50 0,90 1% pyrite in quartz-chlorite veins.38444 307,50 308,50 1,00 1% pyrite in quartz-chlorite veins.38445 325,60 326,80 1,20 2% pyrite mineralization in a grey quartz and 38446 327,90 328,90 1,00 1% chalcopyrite in quartz-epidote veins.38447 328,90 329,90 1,00 1% chalcopyrite in quartz-epidote veins.38448 329,90 330,90 1,00 1% chalcopyrite in quartz-epidote veins.38449 330,90 331,90 1,00 1% chalcopyrite in quartz-epidote veins.

Assays

Hole: C-10-34 Logged by: Matthieu Vallée Date: 2010/06/07 - 09

DDH Depth Recovery RQD Blocky core Crumbly core Fault gouge CommentsBox no. From To Length % Length % Comments % % From To1 28,10 32,20 4,10 4,05 99% 2,95 72% 52 32,20 36,75 4,55 4,35 96% 4,30 95% -3 36,75 41,10 4,35 4,20 97% 4,15 95% -4 41,10 45,20 4,10 4,25 104% 3,95 96% -5 45,20 49,45 4,25 4,25 100% 3,95 93% -6 49,45 53,55 4,10 4,15 101% 3,85 94% -7 53,55 57,75 4,20 4,20 100% 4,20 100% -8 57,75 62,00 4,25 4,35 102% 4,00 94% -9 62,00 66,20 4,20 4,25 101% 4,20 100% -10 66,20 70,35 4,15 4,20 101% 3,60 87%11 70,35 74,70 4,35 4,25 98% 4,15 95%12 74,70 78,80 4,10 4,20 102% 3,80 93%13 78,80 83,10 4,30 4,20 98% 3,68 86%14 83,10 87,50 4,40 4,40 100% 4,33 98%15 87,50 92,00 4,50 4,50 100% 4,35 97%16 92,00 96,20 4,20 4,20 100% 3,94 94%17 96,20 100,50 4,30 4,30 100% 4,10 95%18 100,50 104,80 4,30 4,30 100% 3,34 78%19 104,80 108,90 4,10 4,00 98% 3,43 84%20 108,90 112,90 4,00 3,90 98% 3,20 80%21 112,90 117,10 4,20 4,20 100% 3,40 81%22 117,10 121,30 4,20 4,20 100% 3,99 95%23 121,30 125,60 4,30 4,30 100% 4,11 96%24 125,60 130,00 4,40 4,30 98% 4,02 91%25 130,00 134,20 4,20 4,20 100% 3,70 88%26 134,20 138,50 4,30 4,20 98% 3,71 86%27 138,50 142,80 4,30 4,30 100% 4,03 94%28 142,80 147,00 4,20 4,20 100% 3,63 86%29 147,00 151,20 4,20 4,20 100% 3,89 93%30 151,20 155,40 4,20 4,20 100% 3,40 81%31 155,40 159,70 4,30 4,30 100% 3,97 92%32 159,70 163,90 4,20 4,20 100% 3,44 82%33 163,90 168,20 4,30 4,30 100% 3,96 92%34 168,20 172,40 4,20 4,20 100% 3,80 90%35 172,40 176,60 4,20 4,20 100% 3,69 88%36 176,60 180,90 4,30 4,30 100% 3,99 93%37 180,90 185,10 4,20 4,20 100% 3,97 95%

38 185,10 189,40 4,30 4,30 100% 4,25 99%39 189,40 193,80 4,40 4,40 100% 4,17 95%40 193,80 198,10 4,30 4,30 100% 3,92 91%41 198,10 202,30 4,20 4,20 100% 3,71 88%42 202,30 206,60 4,30 4,30 100% 3,71 86%43 206,60 210,90 4,30 4,30 100% 4,05 94%44 210,90 215,00 4,10 4,10 100% 3,77 92%45 215,00 219,30 4,30 4,30 100% 3,90 91%46 219,30 223,60 4,30 4,30 100% 4,07 95%47 223,60 227,80 4,20 4,20 100% 3,94 94%48 227,80 232,20 4,40 4,30 98% 4,00 91%49 232,20 236,30 4,10 4,10 100% 3,96 97%50 236,30 240,20 3,90 3,80 97% 2,60 67%51 240,20 244,50 4,30 4,30 100% 4,08 95%52 244,50 248,70 4,20 4,20 100% 4,00 95%53 248,70 253,00 4,30 4,20 98% 3,40 79%54 253,00 257,20 4,20 4,20 100% 3,79 90%55 257,20 261,60 4,40 4,40 100% 4,04 92%56 261,60 265,90 4,30 4,30 100% 4,18 97%57 265,90 270,10 4,20 4,20 100% 3,89 93%58 270,10 274,40 4,30 4,30 100% 4,00 93%59 274,40 278,70 4,30 4,30 100% 4,12 96%60 278,70 282,90 4,20 4,20 100% 3,35 80%61 282,90 287,00 4,10 4,10 100% 3,70 90%62 287,00 291,00 4,00 4,00 100% 3,67 92%63 291,00 295,10 4,10 4,10 100% 3,63 89%64 295,10 299,30 4,20 4,20 100% 3,97 95%65 299,30 303,70 4,40 4,40 100% 4,17 95%66 303,70 308,00 4,30 4,30 100% 4,22 98%67 308,00 312,20 4,20 4,20 100% 3,87 92%68 312,20 316,50 4,30 4,30 100% 4,00 93%69 316,50 320,60 4,10 4,10 100% 3,35 82%70 320,60 324,90 4,30 4,20 98% 3,96 92%71 324,90 329,10 4,20 4,10 98% 3,57 85%72 329,10 333,30 4,20 4,20 100% 3,82 91%73 333,30 337,50 4,20 4,20 100% 3,96 94%74 337,50 341,60 4,10 4,10 100% 3,68 90%75 341,60 345,80 4,20 4,20 100% 3,96 94%76 345,80 350,00 4,20 4,20 100% 3,98 95%EOH


0,00 23,00 23,00 OB Casing

23,00 40,70 17,70 PAnLight green aphanitic andesite pillows. One "pedoncule" pointing towards the top.

40,70 53,70 13,00 MAnGreen fine-grained andesite. Often with up to 20% light green or black "spots", possibly old vacuoles.

53,70 88,85 35,15 MAn

Green-gray medium-grained andesite. Finer grains in the margins. Sharp contacts at 30° c.a. Granulometry decreases until aphanitic towards 63.8, where it becomes large, with a sharp contact at 30° c.a. Possibly a contact between flows.

88,85 112,30 23,45 PAnLight green aphanitic andesite pillows. Lower contact with andesite is non-linear, with a part that is sub-parallel to c.a.

112,30 128,70 16,40 MAnGreen-gray medium-grained andesite. Sometimes carbonate and quartz form in the chill margins, but are not mineralized. Finer grains in the margins. Upper contact is non-linear, and strikes sub-parallel to perpendicular to c.a.

128,70 353,00 224,30 PAnGreen aphanitic to fine-grained andesite pillows. Often some quartz and/or carbonate filling in the pillow chill margin. Unless noted otherwise, they are barren.

EOH

p

DDH Depth

Second Lithology From To L Id rock types, grain size, etc. Photo115,50 115,80 0,30 AnD Green aphanitic andesite dyke. Sharp contacts at 70° c.a.144,00 144,20 0,20 InD Dark gray fine-grained intermediate dyke. Sharp contacts at 45° c.a.169,90 170,60 0,70 InD Dark gray fine-grained intermediate dyke. Sharp contacts at 30° c.a.

200,70 203,60 2,90 MAnGray with green spots, fine-grained andesite. Sharp upper contact at 40° c.a., with parallel foliation in the margin.

203,60 206,60 3,00 SyD Red fine-grained syenite dyke. Contacts at 50° c.a.217,40 219,70 2,30 MAn Gray-green fine-grained andesite. Well foliated at 60° c.a. 227,80 232,70 4,90 MAn Gray-green fine-grained andesite. Sharp contacts at 40° c.a.

248,40 249,70 1,30 AAnGray large-grained rock, possibly altered andesite. Mafic crystals in a mostly plagioclase matrix. Upper contact is quartz vein, lower is sharp at 70° c.a.

323,60 323,80 0,20 InDDark gray fine-grained intermediate dyke. Sharp contacts at 45° c.a. Associated with alteration and carbonate veins.

326,10 326,40 0,30 InDDark gray fine-grained intermediate dyke. Contacts follow pillow chill margins, with upper at 30° c.a. and lower at 10° c.a.

Depth

Structure PhotoFrom To L Id % fractures, shear, ctcl, mylt CA Qz Cal Alb Chl

39,10 40,10 1,00 QCaSeveral small to medium quartz-carbonate and carbonate veins. Very weak pyrite mineralization.

1% 5%

40,10 40,70 0,60 BrcLocalized breccia. Moderate pyrite mineralization, but no visible associated alteration.

44,00 47,10 3,10 QAlbA few small quartz-albite veins and veinlets. Several are very deformed. No visible mineralization.

1% 2%

51,40 53,00 1,60 QtzThree 2cm quartz veins with weak to moderate epidote alteration in and out of the vein. No visible mineralization.

30 2%

58,00 58,40 0,40 QChlOne folded 2cm quartz-chlorite vein, going in and out the same side of the rock, at 20° c.a.

3% 1%

59,80 60,10 0,30 SZSmall shear zone, filled with quartz and carbonate veins. No alteration, no visible mineralization.

70 25% 10%

70,70 71,70 1,00 QCaSeveral quartz-carbonate veins and quartz veins, the second with strong epidote alteration of the wall rock. Weak pyrite mineralization.

70 10% 5%

71,90 72,10 0,20 QCa One 2cm carbonate-quartz vein, no mineralization. 20 1% 5%

113,80 114,00 0,20 QCaOne quartz-carbonate vein, closing and opening in the core, striking at 30° c.a. No visible mineralization.

30 10% 5%

124,80 125,00 0,20 QCaOne 2cm quartz-carbonate vein, striking 30° c.a. No visible mineralization.

30 5% 10%

133,30 134,00 0,70 Brc Localized breccia filled with calcite. No mineralization. 10%

150,50 150,70 0,20 QtzOne 0.5cm wide quartz vein with strong pyrite mineralization in the vein itself, striking at 40° c.a.

40 1%

155,80 156,20 0,40 QCaOne 6cm quartz-carbonate vein in a chill margin of a pillow. No visible mineralization.

50 5% 15%

167,50 167,70 0,20 CaOn 10cm carbonate vein, striking at 50° c.a. No visible mineralization.

50 60%

182,00 184,00 2,00 QCaPossible shear zone, with several carbonate-quartz veins and foliation of the wall rock, at 70-80° c.a. No visible mineralization.

70 5% 20%

195,00 195,20 0,20 QtzOne 0.5cm quartz vein, with large yellow epidote alteration of the wall rock, extending up to 4cm on either side. No visible mineralization.

30 5%

219,20 219,70 0,50 QCaA few small quartz-carbonate veins near and parallel to a 4cm one. Moderate pyrite mineralization in the smaller veins.

60 10% 5%

227,60 227,80 0,20 Qtz Two small quartz veins, no visible mineralization. 60 20%229,30 229,50 0,20 QCa One 4cm quartz-carbonate vein, no mineralization. 40 20% 10%

Depth Veins(%)

248,40 248,70 0,30 QtzA 2cm wide quartz vein, with moderate pyrite mineralization. Forms border of what is possibly an altered andesite.

20 20%

249,00 249,30 0,30 Qtz

One 20cm wide quartz vein with weak pyrite and galena? mineralization. Forms the center of a large grained intermediate lithology, and associated with extreme alteration of the foot wall.

50 60%

264,20 264,60 0,40 QtzOne 4cm quartz vein, striking twice across the vein (probably folded). No mineralization.

30%

272,40 272,90 0,50 QCa

One 4cm quartz vein, striking at about 30° c.a., with weak pyrite mineralization in its margins. A few smaller quartz and quartz-carbonate veins, with no mineralization, are associated with it.

30 20% 4%

291,80 292,30 0,50 QCaSeveral small grey quartz and quartz-carbonate veins, sub-parallel at 30° c.a. Very weak pyrite and pyrrhotite mineralization.

30 20% 10%

299,30 299,60 0,30 QCaOne 10cm wide quartz-carbonate vein. No visible mineralization.

40 20% 20%

323,30 324,00 0,70 CaA few small parallel calcite veins, associated with weak silicification of the andesite and moderate pyrite mineralization.

45 1% 6%

From To L Id Description Serp Asb Chl Epi Sil Seri Serp Asb Chl Epi Alb

33,60 36,10 2,50 Oth Black minerals being replaced by chlorite in what appears to be pillow margins. Possibly volcanic glass.

51,40 53,00 1,60 Epi Weak to moderate epidote alteration in and around quartz veins.

2%

70,70 71,70 1,00 Epi Strong epidote alteration around 2 quartz veins. 4%195,00 195,20 0,20 Epi Strong epidote alteration around one quartz vein. 10%

249,30 249,50 0,20 SeriExtreme sericitization and transformation of the mafic minerals into diopside? (bright green crystals), in the foot wall pof a large quartz vein.

5

323,30 324,00 0,70 SilWeak silicification of the andesite pillows near an intermediate dyke. Associated with carbonate veins and moderate pyrite mineralization.

1


From To L Id Py Cpy Ars Gal Po40,10 40,70 0,60 Py 4% pyrite in a localized breccia. 4%

70,70 71,70 1,00 Py2% pyrite mineralization associated with quartz-carbonate and quartz veins, the latter with epidote alteration.

2%

150,50 150,70 0,20 Py 4% pyrite in a very small quartz vein. 4%219,20 219,70 0,50 Py 3% pyrite associated with quartz-carbonate veins. 3%195,00 195,20 0,20 Py 4% pyrite in large euhedral crystals in the quartz vein. 4%

249,00 249,30 0,30 Gal2% pyrite and 2% galena? in small euhedral crystals in a large quartz vein.

2% 2%

272,40 272,90 0,50 Py 2% pyrite in the margins of a medium quartz vein. 2%

291,80 292,30 0,50 Po2% pyrite and 1% pyrrhotite associated with small grey quartz and quartz-carbonate veins.

2% 1%

323,30 324,00 0,70 Py5% pyrite mineralization in a weakly silicified andesite, associated with intermediate dyke and calcite veins.

5%


Sample Id From To Length Comments Id Au Ag38415 0,00 Blank 338416 0,00 Standard 15Pa38417 40,10 40,70 0,60 4% pyrite in a localized breccia.

38418 70,70 71,70 1,002% pyrite associated with quartz-carbonate veins and quartz veins with epidote alteration.

38419 150,40 150,80 0,40Small quartz vein with strong pyrite mineralization.

38420 182,00 183,00 1,00 Possible shear zone.38421 183,00 184,00 1,00 Possible shear zone.38422 219,20 219,70 0,50 3% pyrite in several quartz-carbonate veins.

38423 248,40 249,00 0,604% pyrite in medium quartz vein, in the margin of what is possibly an altered andesite.

38424 249,00 249,70 0,702% pyrite and 2% galena? in a large quartz vein, with extreme sericitization of the foot wall.

38425 272,40 272,90 0,502% pyrite in the margins of a medium quartz vein.

38426 291,80 292,30 0,502% pyrite and 1% pyrrhotite associated with small grey quartz and quartz-carbonate veins.

38427 323,30 324,00 0,705% pyrite mineralization in a weakly silicified andesite, associated with intermediate dyke and calcite veins.

Assays


Box numberFrom To Lenght Recovery Recovery RQD RQD% CSm m m m % m % 0-30 30-60 60-90 from to from to

1 23,00 24,80 1,80 1,50 83% 1,50 83%2 24,80 29,00 4,20 4,20 100% 3,80 90%3 29,00 33,20 4,20 4,20 100% 3,90 93%4 33,20 37,60 4,40 4,40 100% 4,03 92%5 37,60 41,70 4,10 4,10 100% 3,83 93%6 41,70 46,00 4,30 4,30 100% 3,93 91%7 46,00 50,20 4,20 4,20 100% 3,91 93%8 50,20 54,40 4,20 4,20 100% 3,84 91%9 54,40 58,75 4,35 4,35 100% 3,69 85%10 58,75 62,90 4,15 4,15 100% 3,20 77%11 62,90 67,30 4,40 4,30 98% 4,08 93%12 67,30 71,50 4,20 4,20 100% 3,77 90%13 71,50 75,80 4,30 4,30 100% 3,51 82%14 75,80 79,90 4,10 4,10 100% 3,30 80%15 79,90 83,70 3,80 3,70 97% 2,23 59%16 83,70 87,60 3,90 3,80 97% 3,06 78%17 87,60 91,90 4,30 4,30 100% 3,91 91%18 91,90 96,30 4,40 4,40 100% 4,18 95%19 96,30 100,50 4,20 4,20 100% 3,65 87%20 100,50 104,70 4,20 4,20 100% 3,62 86%21 104,70 109,00 4,30 4,30 100% 4,19 97%22 109,00 113,10 4,10 4,10 100% 3,70 90%23 113,10 117,50 4,40 4,40 100% 3,96 90%24 117,50 121,80 4,30 4,30 100% 3,90 91%25 121,80 126,00 4,20 4,20 100% 3,88 92%26 126,00 130,30 4,30 4,30 100% 3,87 90%27 130,30 134,60 4,30 4,10 95% 3,54 82%28 134,60 138,90 4,30 4,30 100% 3,17 74%29 138,90 143,00 4,10 4,10 100% 3,70 90%30 143,00 147,20 4,20 4,20 100% 3,72 89%31 147,20 151,60 4,40 4,40 100% 4,27 97%32 151,60 155,80 4,20 4,20 100% 4,08 97%33 155,80 160,20 4,40 4,40 100% 4,19 95%34 160,20 164,50 4,30 4,30 100% 4,10 95%35 164,50 168,80 4,30 4,30 100% 3,95 92%36 168,80 173,10 4,30 4,30 100% 4,02 93%37 173,10 177,40 4,30 4,30 100% 3,94 92%38 177,40 181,60 4,20 4,20 100% 3,83 91%39 181,60 185,90 4,30 4,30 100% 3,79 88%40 185,90 190,30 4,40 4,40 100% 4,16 95%41 190,30 194,50 4,20 4,20 100% 3,85 92%42 194,50 198,80 4,30 4,30 100% 4,06 94%43 198,80 203,00 4,20 4,10 98% 3,35 80%44 203,00 207,20 4,20 4,20 100% 3,67 87%45 207,20 211,50 4,30 4,30 100% 3,92 91%46 211,50 215,70 4,20 4,10 98% 2,80 67%47 215,70 220,00 4,30 4,30 100% 3,25 76%48 220,00 224,30 4,30 4,20 98% 3,75 87%

Geotechnical Log

Fracture Angle/Frequency TallyHighly Broken Fault Gouge

49 224,30 228,70 4,40 4,40 100% 4,20 95%50 228,70 233,00 4,30 4,30 100% 3,85 90%51 233,00 237,30 4,30 4,30 100% 3,83 89%52 237,30 241,80 4,50 4,40 98% 3,76 84%53 241,80 246,10 4,30 4,30 100% 3,53 82%54 246,10 250,20 4,10 4,00 98% 3,28 80%55 250,20 254,30 4,10 4,10 100% 3,36 82%56 254,30 258,50 4,20 4,20 100% 3,72 89%57 258,50 262,70 4,20 4,20 100% 3,56 85%58 262,70 267,00 4,30 4,30 100% 3,85 90%59 267,00 271,20 4,20 4,20 100% 3,97 95%60 271,20 275,50 4,30 4,30 100% 3,57 83%61 275,50 279,70 4,20 4,20 100% 3,60 86%62 279,70 283,90 4,20 4,20 100% 3,64 87%63 283,90 288,20 4,30 4,20 98% 3,50 81%64 288,20 292,50 4,30 4,30 100% 4,01 93%65 292,50 296,80 4,30 4,30 100% 3,77 88%66 296,80 301,00 4,20 4,20 100% 4,00 95%67 301,00 305,40 4,40 4,40 100% 4,10 93%68 305,40 309,80 4,40 4,40 100% 4,00 91%69 309,80 314,10 4,30 4,30 100% 3,83 89%70 314,10 318,40 4,30 4,30 100% 3,77 88%71 318,40 322,70 4,30 4,30 100% 4,13 96%72 322,70 326,90 4,20 4,20 100% 3,65 87%73 326,90 331,30 4,40 4,40 100% 3,98 90%74 331,30 335,50 4,20 4,20 100% 3,26 78%75 335,50 339,80 4,30 4,30 100% 3,96 92%76 339,80 344,10 4,30 4,30 100% 3,82 89%77 344,10 348,20 4,10 4,10 100% 3,90 95%78 348,20 352,50 4,30 4,30 100% 4,17 97%79 352,50 353,00 0,50 0,50 100% 0,41 82%

EOH

diamond drilling report of the cleaver property - Geology Ontario

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