GM 53062 1995 DIAMOND DRILLING REPORT ON THE NORMETAL COMINCO PROPERTY, PROJECT 08-731 1995 DIAMOND DRILLING REPORT ON THE NORMÉTAL COMINCO PROPERTY PROJECT 08-731 N.T.S. 32D/14

FALCONBRIDGE LIMITED I79

MRN - S.I.S.E.M. 1995/07 GM 53062

ROUYN-NORANDA MARC L'HEUREUX QUÉBEC, CANADA SR. FIELD GEOLOGIST FEBRUARY 1995 NORMAND DUPRAS PROJECT GEOLOGIST

95 066 007 .44 fi

SUMMARY

A 206-meter diamond drill hole has been completed by Falconbridge Limited on the Cominco Property, Project 08-731 on February 22 and 23, 1995. The program was undertaken to further define and delineate a mineralized intersection drilled by Utah Mines Limited in 1975

The exploration hole was targeted on a weak UTEM anomaly as well as on a 3-channel INPUT anomaly. These anomalies are the western lateral extension of a mineralized intersection (0.15% Cu, 0.40% Zn over 3 feet) encountered by Utah Mine in hole CN-3. The hole 95-31-01 drilled by Falconbridge Limited intersected traces to locally 1% small stringers of chalcopyrite associated mainly with carbonate-quartz veinlets within a quartz- eyed rhyolitic unit. This unit is weakly to moderately sericitized.

The expected mineralized contact between the rhyolite and the intermediate units was successfully intersected by the bore hole, but unfortunately no economic sulphide mineralization was returned. Nevertheless, the hole has allowed to corroborate the geological interpretation of the northern portion of the property. Pulse EM survey will be completed next month.

Additional exploration activities such as surface diamond drilling and bore hole geophysics are recommended to investigate the lateral extension of this historical mineralized intersection. 111

TABLE OF CONTENTS

SUMMARY ii

SECTION 1 Introduction 1.1 Scope of Work 1 1.2 Location and Access 1

SECTION 2 Geology 2.1 Regional Geology 5 2.2 Local Geology 5

SECTION 3 Diamond Drilling 3.1 Background of Program 8 3.2 Falconbridge Drilling Procedure 9

SECTION 4 Conclusion and Recommendations 11

REFERENCES 12

APPENDIX A : Diamond Drill Log

MAP POCKETS: Geology Map 1:5,000 Cross Section 1:1,000

LIST OF TABLES

TABLE 1 Legal Description of the Normétal Cominco Property 1 TABLE 2 Diamond Drill Hole Collar Location 9

LIST OF FIGURES

FIGURE 1 Normétal Cominco Property Location Map 3 FIGURE 2 Normétal Cominco Claim Map 4 FIGURE 3 Regional Geology Map of Abitibi 6 FIGURE 4 Normétal Cominco (Geology) 7 1

SECTION 1 - INTRODUCTION

1.1 Scope of work

The following report covers the diamond drilling results returned from the 1995 Falconbridge Limited drilling program carried out on the Normétal Cominco property, project 08-731.

1.2 Location and Access

The Normétal Cominco property consist of 34 claims totaling 1,360 hectares. The claim groups are located in the Perron township, range II, lots 37 to 43 inclusively, Rousseau township, range I, lots 1 to 16 inclusively, Clermont township range VII lots 49 to 57 inclusively and in range VIII, lots 46 to 49 inclusively, in Abitibi county, Québec. The claims are registered in the name of Falconbridge Limited under the following licenses:

Table 1

Legal Description of the Normétal Cominco Property

CLERMONT TOWNSHIP

CLAIM RANGE LOT AREA 5015400 VII 49 40 5015399 VII 50 40 5015398 VII 51 40 5015385 VII 52 40 5015386 VII 53 40 5015387 VII 54 40 5015388 VII 55 40 5015389 VII 56 40 5015390 VII 57 40

5016913 VIII 46 40 5016912 VIII 47 40 5016911 VIII 48 40 5016908 VIII 49 40 2

ROUSSEAU TOWNSHIP

CLAIM RANGE LOT AREA 5051200 2 40 5051201 3 40 5051202 4 40 5051203 5 40 5051204 6 40 5051205 7 40 5051206 8 40 5051207 9 40 5051208 10 40 5051209 11 40 5051210 12 40 5051211 13 40 5051212 14 40 5051213 15 40 5051214 16 40

PERRON TOWNSHIP

CLAIM RANGE LOT AREA 5051369 II 37 40 5051368 II 38 40 5051367 II 39 40 5051366 II 40 40 5051365 II 41 40 5051364 II 42 40 5051363 II 43 40

The Normétal Cominco property is situated one hundred and ten (110) kilometres North of the town of Rouyn-Noranda. Located in the NormétaVVal St-Gilles area, it is readily accessible by Highway 101 from Rouyn-Noranda to La Sane and by the Highway 393 from to Val St-Gilles. A network of ATV and snow-mobile trails cross most of the property. NORMETAL COMINCO PROPERTY LOCATION MAP

a aL~.w... ~.~.~... .. ..

VAL ST-GILLES

NORMETAL

LA SARRE

L. Macamic

MACAMIC

DUPARQUET

48°30'

L. Duparquet

L. Dass=rat

ROUYN-NORANDA

NORLOC.cdr (PN-108) FIG. 1 00163FW1.CDR (PN-128) 5

SECTION 2 - GEOLOGY

2.1 Regional Geology

The Normétal area is located in the Gale Group volcanics (Latulippe 1976), in the Archean Abitibi Greenstone belt of Northwestern . The Gale Group volcanics forms lozenge-shaped volcano-sedimentary terrain, bounded in the North and South by the Casa-Berardi and Chicobi structural breaks, respectively (Daigneault and Archambault 1990). Regional stratigraphy of the Gale Group is poorly defined: volcanic rocks are both abundant and lithologically diverse. These include mafic, intermediate and felsic volcanic lavas and volcanoclastic rocks, epiclastic volcanics, various sediments and iron formations (Gilman 1961, Tolman 1951). The Gale Group volcanic rocks are regionally metamorphosed to the greenschist facies.

2.2 Local Geology

The Normétal-Cominco Option property consists of a complex, alternating series of slightly overturned, south and north facing mafic and intermediate to felsic volcanic units, forming a thick volcanic pile trending roughly SE-NW. Volcanic rocks are cut by various intrusive rhyolite stocks and dykes, and younger NE-SW trending diabase dykes. A laterally extensive sedimentary horizon occurs near the top of the volcanic sequence.

The Normétal Mine Sequence is located near the southern portion of the property, forming the immediate stratigraphic hangingwall of the sedimentary unit, and consists of a series of mafic to felsic volcanoclastic rocks. Intermediate to felsic, coarse epiclastic breccias and fine to medium tuffs form the immediate Mine Horizon. Alteration effects range from weak to pervasive, with locally developed zones of abundant chloritoid. Local intense compressive deformation is attributed to strongly schistose rocks near the Normétal Mine, and the strongly attenuated shape of the original Normétal Orebody. Metamorphic conditions in the mine increased with depth from greenschist grade to amphibolite grade, as documented by Bertrand. Mine Sequence rocks are immediately overlain by a relatively fresh metabasalt. REGIONAL GEOLOGY MAP OF ABITIBI Witinatti

OPATICA SUBPROVINCE

. ~ \ `~ I'' '. I ~ f .~ I ~ ~ ALLARD GROUP MATAGAMI ,~~

TAIBI GROUP

GALE GROUP + + + + ++++++- ++++++----- ++_++++*-

CASTAGNIER ++ -. + +++ + + + + + + - + + + + + + + + + +++++++++++ KINOJEVIS GROUP + + + + + + + + + + +++++++++++ + + ++++++++ + + + +++++++ + + + + + + + + + + + + + + + + + + + + + ++++++++ + GNEISSIC ROCKS BLAKE R. GROUP + + + + + + + + + 1 + + + + + + + + + + + + + + + + + + + + GRANITIC INTRUSIONS + + COBALT GROUP STRATIFORM INTRUSIONS ~ \ l i I~ 1 ULTRAMAFIC ROCKS L-~ / 77° N ,; , ,~ I ~,~ . ~ \ \ . VOLCANOSEDIMENTARY l ~i _/I ~ l 2-' _ 1 ROCKS \ 1 =-,~ ~ \~~~~ PROTEROZOIC ROCKS / I PONTIAC A SUBPROVINCE MAJOR FAULTS CC 100Km Q BELLECÔMBE 1~ o v GNEISSES 179 (FROM LATULIPPE 1976)

00101 F_1.CDR (PN-001) FIG. 3 N FALCONBRIDGE LIMITED RHYOLITE SEDIMENTS Exploration Timmins, Ontario ~ ANDESITE ""I FAULT NORMETAL COMINCO GRANITE IJ INTERPRETED MINE HORIZON (GEOLOGY) GABBRO SHOWING DIABASE Traced: J . Date. 12/08/94 NTS:32D14.32FJ03 8731 0 5 Km Drawn: Date Map No ~ QUARTZ-FELDSPAR PORPHYRY II Supervised. N.D. Date: 12/08/94 Date Fig.4 8

SECTION 3 - DIAMOND DRILLING

3.1 Background of Program

Recent work by Cominco Limited between 1990 to 1992 on the Cominco property area includes geological mapping and a total of eleven (11) diamond drill holes (NC-90-4, NC- 91-11, 12, 14, 16, 18, 20, 22, 23, 26 and 32) covering a strike length of six (6) kilometres along the Mine Sequence on the western extension of the property. This work allowed to outline the following:

- A comprehensive stratigraphy sequence similar to the Normétal Mine area.

- Recognition on the property of the Mine Sequence as well as the Mine Horizon that hosts the Normétal Mine (11 Mt at 5.12%Zn, 2.15% Cu).

Considering the above results, the historical data review of the Cominco property area and the lack of bedrock exposure, it was recommended that one (1) diamond drill hole totaling 200 metres be executed. 9

3.2 Falconbridge Drilling Procedure

One (1) diamond drill hole totaling 206 metres of BQ sized core was drilled on February 22 and 23, 1995 by Benoît Diamond Drilling of Val D'Or, Québec. The core logging was executed at the Falconbridge Limited core shack located in Normétal, Québec. Since the diamond drill hole collar location have not been surveyed, the co-ordinate presented on the cross-section is based on a grid centered on L0+00 and BLO+00. Drilling data was standardized to a scale of 1:1,000 and produced as a cross section. Hole deflections in course of the bore hole were recorded by using acid test at forty (40) metre intervals. The following drill hole collar location refer to the geological surface plan produced by Cominco Limited during the course of mapping surveys, done in the summers of 1990 and 1991.

TABLE 2

DIAMOND DRILL HOLE COLLAR LOCATION

HOLE # COORDINATES AZIMUTH DIP LENGTH TARGET

95-31-01 L68+00E / 1+50S N 360 -55 206m UTEM/INPUT (P-1)

Total 206m

The following is a description of the diamond drilling objectives and results encountered in the bore hole of the 1995 Falconbridge Limited winter drilling campaign. For more details, please refer to the drilling cross section in the back pocket. io

D.D.H. 95-31 01 (P-1)

This hole was recommended to test the mineralized intersection (0.15% Cu, 0.40% Zn over 3 feet) encountered in hole CN-3 drilled in 1975 by Utah Mine. The mineralized zone is hosted at the interface between a rhyolite unit and a thick sequence of intermediate composition. The proposed hole was planned to test the western lateral extension of this intersection at some 200 metres on a target which also correlates to a weak INPUT / UTEM anomaly. Based on the historical drill section of hole CN-3, it was interpreted that the geology was dipping to the south, which allowed us to drill test the target at about 70 meters from the property boundary and 100 meters below the surface.

P 95-31-01: - Test a weak UTEM anomaly - Test a 3-channel INPUT anomaly. - Test the west extension of the mineralization intersected in hole CN-3 (0.15% Cu, 0.40% Zn over 3 feet)

The hole successfully intersected the inferred mineralized geological contact between the rhyolite and intermediate units. In the present hole, no significant alteration or mineralization were observed along the geological contact. In fact, only few pyrite bleeds and very rare chalcopyrite specks and veinlets were noted. Nevertheless, the hole drilled in the western extension of hole CN-3 has allowed to corroborate the geological interpretation expected in this portion of the property. It should be noted that the property is characterized by a major lack of bedrock exposure. The geological interpretation of the property is based on the historical diamond drill holes that were drilled entirely by Utah Mines between 1975 and 1978. 11

SECTION 4 - CONCLUSION and RECOMMENDATIONS

The exploration hole was targeted on a weak UTEM anomaly as well as on a 3-Channel INPUT anomaly. These anomalies were the western lateral extension of the mineralized intersection (0.15% Cu, 0.40% Zn over 3 feet) accoutered by Utah Mine in hole CN-3. The expected mineralized contact between the rhyolite and the intermediate units was successfully intersected by the bore hole, but unfortunately, no economic sulphide mineralization was observed. Nevertheless, the hole has allowed to corroborate the geological interpretation of the northern portion of the property.

Additional exploration activities such as surface diamond drilling and bore hole geophysics are recommended to investigate the lateral extension of this historical mineralized intersection.

Respectfully submitted,

~

Marc L'Heureux Senior Field Geologist Falconbridge Limited

Normand Dupras Project Geologist Falconbridge Limited 12

REFERENCES

Bertrand , C., (1969). Metamorphism of the Normétal Mine. University of Western Ontario, PhD these, unpublished.

Bertrand, C., and Hutchinson, R.W., (1973). Metamorphism at the Normétal Mine, Northwestern Québec. CIMM Bull., 76, pp. 226-234.

Brown, W. L., (1948). Normétal Mine, In: Structural Geology of Canadian Ore Deposits. CIMM Special Volume, pp. 683-693.

Catallani, S., and Bambic, P., (1991). Lithogeochemistry and Alteration, Perron and Des Méloizes Townships. Québec., Submitted to Cominco Ltd.

Daigneault, R., and Archanbault. G., (1990). Les grands couloirs de déformation de la sous-province de l'Abitibi. In The Northwestern Québec Polymetallic Belt. Edited by: M. Rive, P. Verpaelst, Y. Gagnon, J.M. Lulin, G. Riverin and A. Simard. Canadian Institue of Mining and Metallurgy, Special Volume 43, pp. 43- 64.

Gilman, W. F., (1961). Rapport préliminaire sur la canton de Des Méloizes, comté d'Abitibi-Ouest, Québec, Ministère des richesses naturelles du Québec, RR-462, 15p.

Latulippe, M., (1976). Excursion géologique, Val d'Or-Malartic., MRNQ, DP-367, 124p.

Tessier, A. C., (1991). The Norcom/Normétal Projects, May 1990 to May 1991 Progress Report, NTS: 32D/14, 32E/3.

Tessier, A. C., (1991). The Norcom Project. Report of Summer 1991 Drilling Program, NTS: 32E/3.

Tolman, C., (1951). Normétal Mine Area. Department of Mines, Mineral Deposits Branch. Province of Québec. GR-34. pp.34. APPENDIX A

FALCONBRIDGE LIMITED DATE: 03/01/1995 HOLE NUM03ER: 95-31-01 DRILL HOLE RECORD IMPERIAL UNITS: METRIC UNITS: X PROJECT NAME: 8733 PLOTTING COORDS GRID: UTM ALTERNATE COORDS GRID: COMINCO COLLAR DIP: -55° 0' 0" PROJECT NUMBER: 8733 NORTH: 150.000 NORTH: 1+50S LENGTH OF THE HOLE: 206.00M CLAIM NUMBER: 5015399 EAST: 6800.00E EAST: 68+ OE START DEPTH: 0.00M LOCATION: NORMETAL AREA ELEV: 3000.00 ELEV: 0.00 FINAL DEPTH: 206.00M COLLAR ASTRONOMIC AZIMUTH: 360° 0' 0" GRID ASTRONOMIC AZIMUTH: 360° 0' 0" DATE STARTED: 02/21/1995 COLLAR SURVEY: NO PULSE EM SURVEY: NO CONTRACTOR: BENOIT DATE COMPLETED: 02/22/1995 RQD LOG: NO PLUGGED: NO CASING: YES DATE II11'ED: 02/24/1995 HOLE MAKES WATER: NO HOLE SIZE: BQ CORE STORAGE: NORMETAL UTM COOED.:

COMMENTS : WEDGES AT:

DIRECTIONAL DATA:

Depth Astronomic Dip Type of FLAG Comments Depth Astronomic Dip Type of FLAG Comments (MI Azimuth degrees Test (M) Azimuth degrees Test

40.00 -54° 0' 0" A OK 80.00 -53° 0' 0" A OK 120.00 A OK 160.00 -51°30' 0" A OK 190.00 -52° 0' 0" A OK

HOLE NUMBER: 95-31-01 DRILL HOLE RECORD LOGGED BY: MARC L'HEUREUX PAGE: 1 HOLE NUMBER: 95-31-01 DRILL HOLE RECORD DATE: 03/01/1995

FROM ROCK ANGLE TO TYPE TEXTURE AND STRUCTURE TO CA ALTERATION MINERALIZATION REMARKS

0.00 CASING TO sj oh F. 21.00

21.00 INTER- Medium to light greenish grey. Coarse grained General alteration in iron-carbonate Trace - 1% coarse to fine grained Good ROD. TO MEDIATE (1-15mm) to locally aphyric. of porphyries. Local moderate pyrite with local specks of 80.82 PORPHYRITIC chloritization of groundmass. chalcopyrite associated with veinlets. VOLCANIC 40-50% feldspar porphyries of different shapes ROCKS and densities in a fine grained intermediate 63.24-65.50 - Moderately silicified sTr to 1% Py,Cp. .3, D, G, Ch,F groundmass. The distribution of porphyries is and weakly sericitized. irregular and may be coalescent due to alteration. 1-2% fine grained leucoxene. Weak foliation 0 55° CA. 1-2% carbonate-quartz veinlets oriented parallel to foliation. Very monotonous sequence. Sharp lower contact 0 65° CA.

80.82 FELSIC Yellowish grey. Fine to medium grained General weak pervasive Good RQD. TO INTRUSIVE (1-2mm). sericitization. 84.88 ROCKS .4,m, a, b. Massive, homogeneous medium-grained rhyolite I1-2mm1. May be a dike, but no sharp contacts. 2-3% fine graine (

84.88 QUARTZ- Medium grey. Aphyric groundmass, 1-3mm quartz General weak to locally moderate Trace - 1% pyrite and chalcopyrite Good ROD. TO EYED eyes. sericitization. associated with sericitized fractures 124.46 RHYOLITE and quartz veins and veinlets. .4,q,m,Se. Massive with 2-3% quartz eyes (1-3mm). Sericite filled fractures oriented mainly parallel to sTr to 1% Py,Cp. foliation a 60° CA. Fractures represent 5t of rock volume. Presence of hornblende is observed locally. 1-2t quartz-carbonate veinlets. Sharp lower contact a 70° CA.

99.15-99.25 - 10-15t quartz veins and veinlets containing 5% cp.

124.46 INTER- Medium grey. Aphyric to fine grained (<1mm). Weak pervasive chloritization. 1-2% coarse grained pyrite with Good RQD. TO MEDIATE trace of chalcopyrite associated with 201.00 VOLCANIC Generally massive with some micro feldspar carbonate-quartz veinlets. ROCK porphyritic zones. Monotonous sequence. 2-3% s3,m,a. quartz-carbonate veins and veinlets oriented subparallel to weak foliation a 65-70° CA.

HOLE NUMBER: 95-31-01 DRILL HOLE RECORD LOGGED BY: MARC L'HEUREUX PAGE: 2

HOLE NUMBER: 95-31-01 DRILL HOLE RECORD DATE: 03/01/1995

FROM ROCK ANGLE TO TYPE TEXTURE AND STRUCTURE TO CA ALTERATION MINERALIZATION REMARKS

41126.48-126.704Qt,Chls - quartz vein with Trace pyrite. chlorite. 1126.48-126.70lkTr Py.

033.20-133.700.Qt,Chls - quartz veins with chlorite.

41148.10-148.10.9?,c. - felsic dyke, coarse grained m 65° CA.

4152.05-152.69.4,m. - rhyolitic dyke, aphyric Weak sericitization. 1% chalcopyrite stringers within and massive. 5% fractures (sericitized) oriented fractures. parallel to weak foliation 0 65-70° CA. Sharp ;152.05-152.651}.1% Cps upper and lower contact 0 65° CA.

i1160.00-190.001.3,bx,Ch. - locally brecciated Increase in chloritization 1-2t coarse-grained pyrite (tectonic) with sulphide in matrix. 2-3% (moderate). associated with groundmass and cubic carbonate-quartz injections and veinlets parallel pyrite (2-5mm) in groundmass. to moderate foliation 0 50° CA. 41160.00-190.001k1-2t Py. 4161.70-162.001k3,°p,Chs - gouge. Strong chloritization.

201.00 MASSIVE Light grey, aphyric to fine-grained. Weak pervasive sericitization. Good ROD. TO RHYOLITE 206.00 a4,m, a, qs Massive with less than 1% blue quartz eyes (1-4 mm). Weak sericitization. 1% quartz-carbonate veins (4-5mm) oriented parallel to schistosity 0 65° CA.

HOLE NUMBER: 95-31-01 DRILL HOLE RECORD LOGGED BY: MARC L'HEUREUX PAGE:

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HOLE NUMBER : 95-31-01 ASSAYS SHEET DATE: 01/03/1995

Sample From To Leng. H Cu Zn Au Ag Pb Co Cu/Zn Ni Comments (M) (M) (M) H PPm PPm PPb PPm ppm PPm PPm PPm

1 34.00 35.00 1.00 2 76.50 77.00 0.50 3 78.00 79.00 1.00 4 83.00 84.00 1.00 5 99.00 100.00 1.00 SANtnL~ tr\~ric~c'. Ç c~ ~r~c -~~i~v~ (0 i(c `t~ J 6 126.00 127.00 1.00 7 133.00 134.00 1.00 8 134.00 135.50 1.50 9 135.50 137.00 1.50 10 152.00 153.00 1.00 11 161.50 162.50 1.00 12 197.00 198.00 1.00

HOLE NUMBER: 95-31-01 ASSAYS SHEET PAGE: 4

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sIGXE6 . :^S1./95

HOLE NUMBER 95-31-01 GEOCHEMICAL ASSAY DATE: 01/03/1995 Sample From To Leng. SIO2 AL2O3 CAO MOO NA2O 520 FE2O3 TIO2 P2O5 MNO CR2O3 LOI SUM Y ZR BA CU ZN NI CR FIELD CHEM ALUM (M) (M) } t } } } k k t } t } k t PPM PPM PPM PPM PPM PPM PPM NAME ID 1 38.00 38.20 0.20 3,D,C> 2 41.00 41.20 0.20 3,m 3 64.00 64.20 0.20 4,3,m,Si,Se 4 81.10 81.30 0.20 4,m,(9),5e 5 89.00 89.20 0.20 tJ(;) ~ At'tb AgE- U'~ ~r."~3 (~(~ 4,m,q,Se 6 119.00 119.20 0.20 4,m,q 7 131.00 131.20 0.20 3,m 8 159.80 160.00 0.20 3,m 9 176.80 177.00 0.20 3,m,Ch 10 200.00 200.20 0.20 3,m,Ch 11 205.80 206.00 0.20 4,m,Se

HOLE NUMBER: 95-31-01 GEOCHEMICAL ASSAY PAGE: 5 HOLE NUMBER 95-31-01 GEOCHEMICAL ASSAYS DATE: 01/03/1995 Sample From To Leng. RB SR CO2 AG AU CO PB V AS SN CD SH BI SE HF TA {i MO TH U B CS LA CE ND (M) (M) (M) PPM PPM t PPM PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM 1 38.00 38.20 0.20 2 41.00 41.20 0.20 3 64.00 64.20 0.20 4 81.10 81.30 0.20 5 89.00 89.20 0.20 6 119.00 119.20 0.20 7 131.00 131.20 0.20 8 159.80 160.00 0.20 9 176.80 177.00 0.20 10 200.00 200.20 0.20 11 205.80 206.00 0.20

HOLE NUMBER: 95-31-01 GEOCHEMICAL ASSAYS PAGE: 6 HOLE NUMBER : 95-31-01 GEOCHEMICAL ASSAYS DATE: 01/03/1995

Sample From To Leng. SM EU GD DY ER LU OS IR RU RH PT PD LI BE MN GA GE IN TL SC BR YE MGOp CA/AL NI/MgO ISHIKW ZN/NA (M) (M) (M) PPM PPM PPM PPM PPM PPM PPB PPB PPB PPB PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM

1 38.00 38.20 0.20 2 41.00 41.20 0.20 3 64.00 64.20 0.20 4 81.10 81.30 0.20 5 89.00 89.20 0.20 6 119.00 119.20 0.20 7 131.00 131.20 0.20 8 159.80 160.00 0.20 9 176.80 177.00 0.20 10 200.00 200.20 0.20 11 205.80 206.00 0.20

HOLE NUMBER: 95-31-01 GEOCHEMICAL ASSAYS PAGE, 7