32EI2SW8065 St HOBLITZELL 010

DIAMOND DRILLING

TOWNSHIP: HOBLITZELL TWP. REPORT NO: 20

WORK PERFORMED FOR: Cogema Canada Ltd.

RECORDED HOLDER: Same as Above [xx]

p Claim No.

fefe L 789332

p L 789335

fe L 789318

Hi. L 789S26/ |: ' L 789329

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: Other

Hole No.

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Footage

BUR-01 200m BUR-03 149m

BUR-04 200m

BUR-09 257m

BUR-10 244m

BUR-11 217m

BUR-12 191m

BUR-13 188m

date filed April 89

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Date Note

Feb/88 (1)C.2) Feb/88 (!)C2J

Feb/88 (l)C^)

Mar/88 ( 1 ) (2)

Mar/88 ( 1 ) C"^)

Mar/88 ( 1 ) #2)

Mar/88 ( 1 ) C2)

Mar/88 0)^-2)

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I.

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

FINAL REPORT 1988 "DIAMOND DRILL RESULTS"

VOLUME l of 3

Ref. No. 88-CND-47-03A (Document: #0135U)

By: R. St-Jean J. Learn Nov. 1988

aaeiesweaes 20 HOBLITZELL 010C

TABLE OF CONTENTS

page

1. INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

1.1 General Statement . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ll . 2 Location and Access . . . . , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ll . 3 Summary of Work Performed to Date . . . . . . . . . . . . . . . . . . . . . l1.4 Bedrock Geology of the Project Area . . . . . . . . . . . . . . . . . . . 31.5 Objectives of the Drilling Program . . . . . . . . . . . . . . . . . . . . 4

2. OVERVIEW OF FIELD WORK . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

2 . l Line-cutting . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 52 . 2 Ground Geophysics . . . . . . . . . . . . . . . . . . . . . . \ . . . . . . . . . . . . . . 5

2.2.1 VLF and Magnetics .............................. 52.2.2 Induced Polarization . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

2 . 3 Reverse Circulation Drilling . . . . . . . . . . . . . . . . . . . . . . . . . . 62 . 4 Diamond Drilling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

3. DIAMOND DRILL RESULTS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 10

3 . l General Outline . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 103 . 2 Blue Lake Area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 103 . 3 Burntbush Grid Area . . . . . . . . . , . . . , , . . . . . . . . . . . . . . . . . . . . 14

3.3.1 Section 350E ..... .................,............ 143.3.2 Section 900W . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 223.3.3 Section 2000W .................................. 28

3 . 4 Spade Lake Area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32

4 . DISCUSSION OF RESULTS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35

4 . l Blue Lake Area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 354 . 2 Burntbush Grid Area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35

4.2.1 Rock Types . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 354.2.2 Structure and Deformation . . . . . . . . . . . . . . . . . . . . . . 364.2.3 Magnetics as a Mapping Tool . . . . . . . . . . . . . . . . . . . . 384.2.4 Alterations and Gold Geochemistry . . . . . . . . . . . . . . 40

4 . 3 Spade Lake Area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 43

TABLE OF CONTENTS

5. SUMMARY AND CONCLUSIONS

5.1 Recommendations for Further Work

page

44

47

6. REFERENCES 49

LIST OF APPENDICES

Volume 2 of 3;

APPENDIX I : DIAMOND DRILL HOLE DESCRIPTIONS

1. Summary Logs2. Field Logs

Volume 3 of 3;

APPENDIX II : SAMPLE RESULTS

1. Chemistry Results2. Thin Section Descriptions

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LIST OF FIGURES

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Figure l : Location of the Burntbush River Property, Northeastern Ontario, Scale 1:250 000 ...

Figure 2 : Progressive alteration assemblages in the East South "C" ore zone at the Dickenson Hine, Red Lake District ....... 42

LIST OF TABLES

Table l : Diamond Drill Statistics 11

Table 2 : Summary of Gold Results - BUR-12 34

if

LIST OF MAPS

Map l : Diamond Drill Hole Locations Scale: 1:20 000

Map 2 : L5050E, Diamond Drill Hole BUR-08, Cross-Section Scale: 1:500

Hap 3 : L4900E, Diamond Drill Hole BUR-02, Cross-Section Scale: 1:500

Map A : L350E (south), Diamond Drill Holes BUR-05, BUR-06, Cross-Section Scale: 1:500

Map 5 : L350E (north), Diamond Drill Hole BUR-07, Cross-Section Scale: 1:500

Map 6 : L900W (south), Diamond Drill Holes BUR-01, BUR-03,Cross Section Scale: 1:500

Map 7 : L900W (north), Diamond Drill Holes BUR-04, BUR-10,Cross-Section Scale: 1:500

Map 8 : L2000W (south), Diamond Drill Holes BUR-09, BUR-13,Cross Section Scale: 1:500

Map 9 : L2000W (north), Diamond Drill Hole BUR-11, Cross-Section Scale: 1:500

Hap 10 : L5900W, Diamond Drill Hole BUR-12, Cross-Section Scale: 1:500

Map 11 : Burntbush Grid Geologic Interpretation Scale: 1:5000

1. INTRODUCTION

1.1 General Statement

The Burntbush River project is a joint venture gold exploration program between COGEHA Canada Limited and AMERITEX Resources Limited, The property comprises 312 contiguous mining claims. The joint venture agreement was signed in May 1986.

1.2 Location and Access

The Burntbush River property covers about 50 km* in the townships of Hoblitzell and Noseworthy, northeastern Ontario (see Fig. 1). It is located approximately 90 km northwest of La Sarre and 20 km west of the Quebec-Ontario border (latitude 49'30'N, longitude 79 050'W, NTS 32E and 42H).

During the winter program, access to the area was by winter road via Tomlinson Road, which connects to a main E-W maintained gravel road joining La Sarre, Que. and Iroquois Falls, Ont.

1.3 Summary of Work Performed to Date

Most of the project area (300 claims) was staked for AMERITEX in January, 1984. The only work performed by them on the claims was an airborne VLF-EM and magnetics surveyi which was contracted to Aerodat Ltd (Ameritex, 1984).

In May 1986, COGEMA and AMERITEX signed a joint venture agreement naming COGEMA operator of the exploration program and all subsequent work has been performed by ourselves. At this time, a block of 12 claims (previously held by DOME Explorations Ltd) was added to the property.

The first field program was performed in the summer of 1986, and comprised geologic traverses aimed at locating, mapping and sampling outcrops. Traverse spacing ranged from 50 to 100 m and numerous undocumented outcrops were found and described (COGEMA Reference No. 86-CND-47-02).

l

t 1 . Figure l Location of the Burntbush River Property, Northeastern Ontario. Scale 1:250 000

1 Tomlinson Road— — — Winter road to camp

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Later, in the fall of 1986, five of the larger outcrops were stripped and detailed mapping was performed in order to better understand the geology. These outcrops are fairly well distributed across the property and represent an important step in understanding the property geology at a broader scale (COGEMA Ref. No. 87-CND-47-01).

In December 1986, a second airborne survey was commissioned, this time to DIGHEM Surveys Ltd, mostly because the previous airborne survey did not include low frequency or time domain EM instrumen tation (COGEMA Ref. No. 87-CND-47-02).

The winter 1987 program consisted of reverse circulation (overburden) drilling at ~400 m x 400 m spacing and was planned to cover the southern one third of the property. Unfortunately, 23 of the planned drill holes could not be completed due to mild weather which made it necessary to abandon work on the east side of the Burntbush River.

Reverse circulation drilling was therefore resumed during the summer 1987 program. This program was designed to complete the reconnais sance holes not yet drilled, and also to perform some detailed follow-up drilling (~200 m x 200 m spacing) in areas of interest interpreted from the results of the winter program (see COGEMA Ref. No. 87-CND-47-02).

Work performed during 1988 includes:

* line cutting of two grids (Burntbush and Blue Lake grids);

* ground magnetics and VLF surveys over these grids and along two profiles of particular interest;

* IP surveys over selected lines;

* reverse circulation drilling of 40 additional sites;

* 13 diamond drill holes for a total of 2904.5 m.

1.4 Bedrock Geology of the Project Area

The bedrock geology of the area was first studied by Thomson (1936) and more recently by Johns (1982). The following brief summary serves only as an introduction; the reader is referred to our earlier reports for more background information.

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The property has been informally subdivided into a "northern low magnetic terrane" and "southern high magnetic terrane":

Very few outcrops occur in the north part of the property, and from these it is interpreted that the area is underlain by predominantly high grade metasedimentary rocks (turbidites), with lesser predominantly mafic, metavolcanic rocks, A few intrusive metagabbros are present and there are numerous late dykes and veins of various compositions.

The southern part of the property may be less strongly metamorphosed than the northern part, and outcrop exposure is somewhat better. Tuffs and flows of mostly intermediate compositions have been mapped. These rocks have been intruded by various others, including metagabbro and diabase, but veining seems to be less common than in the north.

It is believed that one or more major east-west structures transect the property and this is supported to some extent by our surface mapping.

1.5 Objectives of the Drilling Program

The main objective of the drilling program was to evaluate the gold potential of the property. Thus, 10 of the holes were drilled along three fences in the south-central part of the property (Burntbush grid) where reverse circulation drilling indicated variable rock types and weakly anomalous gold values (up to 31 ppb) and where airborne magnetics results suggested probable structural (but also possibly stratigraphic) contacts of potential interest.

The remaining three holes were more widely distributed across the property. Two holes were drilled in the metasediments: the first to test the strong E-W magnetic anomaly of the northeastern portion of the property (L4900E), the second to test an IP anomaly to the south of reverse circulation holes BOB-12 and BOB-114, where abundant gold grains were detected in pre-Wisconsinan gravels (Blue Lake grid). Finally, one hole was drilled west of Spade Lake (L5900W) to test a magnetic contact where reverse circulation drilling had again indicated weakly anomalous gold values (up to 28 ppb).

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2. DESCRIPTION OF FIELD WORK

2.1 Line-cutting

During winter 1987, widely spaced lines were cut for the purpose of surveying reverse circulation holes. For this program (1988), approximately 200 km were cut and picketed to permit ground geophysical surveys, and correct positioning of reverse circulation and diamond drill holes.

Two grids and two profiles were cut or rechained by EM Exploration Services Inc. (of Rouyn-Noranda, Que.): the Burntbush grid (line cutting 137 km, rechaining 5.4 km), the Blue Lake grid (line cutting 61 km, rechaining 3.3 km), the Blue Lake profile (L4900E, included in above) and the Spade Lake profile (L5900W, rechaining 0.9 km). Lines were cut 50 m apart and picketed every 25 m.

2.2 Ground Geophysics

2.2.1 VLF and Magnetics

These two surveys were carried out simultaneously by EM Explo ration Services Inc. on the grids and profiles. Readings were taken on all lines at 25 m spacing (50 x 25 m lattice). The surveys were undertaken to aid in ground positioning of the drill holes, and to evaluate the usefulness of a more detailed survey compared to the airborne results, which were flown at 100 m spacing.

The VLF survey was done using a Geonic's "VLF-EM 16" instrument using the Cutler, Maine (NAA, 24,0 KHz) station. In-phase and quadrature components were read and hand drawn profiles were produced on-site. In all cases, readings were taken with the operator facing north.

The magnetics survey was done using an EDA "Omni IV proton magnetometer" while a base station monitored the diurnal variation. Every day, data were "dumped" through the base station and corrected readings were printed. A hand-contoured map was then produced.

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At the end of the program, the VLF and magnetics data were digitized and computer drawn maps were supplied to us by the contractor.

The contractor's report covering these surveys has been compiled and is presented in COGEMA Ref. No. 88-CND-47-02 (volume 2).

2.2.2 Induced Polarization

A limited amount of IP work was performed to aid in drill hole positioning and to evaluate the usefulness of this method in the project area.

This survey was done on 6 lines (lines 3+50E, 51+OOE, 56tOOE, 64+OOE, 68+OOE, 71+OOE) and also along the camp road (which approximately follows line 900W) by JVX, Ltd. (of Thomhill, Ont.). A total of 8.225 km was surveyed in five days. The contractor used a Scintrex IPR-11 multichannel time domain receiver and a Scintrex IPC-7 2.5 kW time domain IP/resistivity transmitter with an 8 hp motor generator. Each day, results were downloaded from the field instruments to a micro-computer and pseudosections were produced.

The contractor's report is presented in COGEMA Ref. No. 88-CND-47-02 (volume 1).

2.3 Reverse Circulation Drilling

Reverse circulation drilling was performed by Heath and Sherwood Drilling Inc. (of Kirkland Lake, Ont.); logging and sampling was performed by Overburden Drilling Management Limited (of Nepean, Ont.),

A total of 40 sites were drilled and these were distributed acrqss 4 areas within the property: along the E-W magnetic anomaly in the northeast part (18 holes), in the area between the Burntbush River and Nedlog Lake (6 holes), in the southernmost part of the property west of the Burntbush River (5 holes) and along an E-W line located between the western property boundary and the large sheared metagabbro outcrop (11 holes).

A fully interpreted report has been prepared (COGEMA Ref. No. 88-CND-47-01) which describes this program.

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l

2.4 Diamond Dellling

The diamond drilling contract was awarded to Les Forages Foranord Inc. (of Rouyn-Noranda, Que.) while drill hole surveying, core logging and core sampling were realized by Cogema's personnel.

A total of 13 holes were drilled for a cumulative total of 2904.5 m.

Dri.lJ.ing.Jiechnique

The material used by Foranord consisted of:

. two Longyear 38 unitized diamond coring drills equipped with BQ rodsand BW and NW casing;

. two unitized pump shacks equipped with sufficient water lines;

. one Timber Jack tractor for drill moves and water hauling;

. one bulldozer (D5 or D6) for trail maintenance and drillmoves;

. one propane heated water tank (5000 imp. gals) that was used wherewater supply was too remote.

Foranord directed the operations from their own base camp located at the old Newmont camp on the Burntbush River. The drills were run on two 12 hour shifts.

Drill. hojLe—survexing

All holes were carefully spotted on the grid before the arrival of the machinery. After the site was cleaned, the drill was positioned and levelled with the assistance of a Cogema geologist. Hole inclination was verified when the drill was in place.

During drilling, hole inclination was checked every 60 m using the acid etched tube method.

Core-logRing

All holes were logged and described in the field at 1:100 scale. Each box, once logged, was clearly identified with metallic embossing tape (hole No., box No., depth) and properly stored.

Core—sam2ljLna and analysis

Core sampling was performed with several objectives in mind:

* to analyze for gold in areas of interest;

* to analyze for major elements in the "typical" rock units;

* to analyze also for minor elements in the "typical" rock types since bedrock chips from the reverse circulation program are analyzed in this manner, and since the minor element package which we use includes a gold analysis;

* to sample for thin sections to help understand the rock types and alterations present.

Sampling for "gold only" was done in two stages. At first, the core was sampled for gold at the discretion of the logging geologist; 50 cm long, half core samples were taken. After discussion, it was decided that larger samples (1.5 m long, half core) over more continuous zones would be preferable to smaller "punctual" samples. The drill core was then resampled using these new criteria.

A total of 669 samples were sent for "gold only" analysis; of these, 175 were sent to the assay laboratory of "Mine Yvan Vdzina" in Destor, Que., and 494 samples were sent to Chimitec Ltee, in Ste-Foy, Que.

Other samples, taken are as follows:

- 89 samples analysed for both major and minor elements 11 samples analysed for major elements only 2 samples analysed for minor elements only

- 110 thin sections

Major and minor element analyses were done by Chimitec. See Appendix II for the analytical procedures and detection limits. Thin sections were made at Ecole Polytechnique in Montreal.

Control, sampl.es and r e JLi ability of

During the sampling, quartzite control samples were inserted at intervals of approximately 25 samples, to help detect possible problems of contamination which might cause false gold anomalies.

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COGEMA Canada purchased one ton of this material and It is used on all gold projects. Preliminary analyses of the quartzite done by Chimitec all gave ^ ppb Au (by neutron activation).

Twenty-one control samples were inserted into the "gold only" samples sent to Chimitec; twenty gave ^ ppb while one gave 20 ppb Au. Although one sample appears to be weakly contaminated, we feel confident that Chimitec has provided us with reliable results.

Ten controls were sent to Mine Yvan Vezina, and nine gave below detection limit results; the tenth sample gave 0.8 g/t which indicates the possibility of occasional strongly contaminated samples from this lab. Thus, any important anomalies should be rechecked by sampling the remaining half core (NOT the pulp or reject) before conclusions can be drawn.

Eight control samples were also introduced with the minor elements samples sent to Chimitec. The results show no evidence of contamination in any elements.

i 4,,

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3. DIAMOND DRILL RESULTS

3.1 General Outline

Thirteen diamond drill holes were performed; a total of 2904.5 m were drilled. Drill hole locations are given on HAP l, and a drilling summary is presented in Table 1.

Two of the holes were drilled in the eastern part of the property (Blue Lake area; BUR-02, 08), ten holes were drilled in the central part (Burntbush grid area; BUR-05, 06, 07 on L350E, BUR-01, 03, 04, 10 on L900W and BUR-09, 13, 11 on L2000W) and one hole was drilled in the western part of the property (Spade Lake area; BUR-12).

Results will be presented from east to west across the property (rather than in the order drilled) to facilitate discussion of the results.

Results presented are mainly a summary of the diamond drill (1/100) |- logs (see Appendix I), chemistry results and thin section studies

(see Appendix II), but reference is also made to the various exploration results described in earlier reports (eg outcrop studies, reverse circulation drilling, airborne and ground geophysical work).

3.2 Blue Lake Area

BUR-08-(see MAP 2)

BUR-08 was drilled on the west shore of Blue Lake to test a weak IP response. The VLF profile also shows an in-phase inflection and corresponding reverse quadrature crossover; both of these are weak, low amplitude features.

No outcrop is exposed in this eastern part of the property, but the results of reverse circulation drilling suggested that metamorphosed greywackes (biotite ± amphibole ± garnet schists) would be inter sected.

* - 10 -a...

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Table l : DIAMOND DRILL STATISTICS

HOLE #DRILL #

BUR-01 #01

BUR-02 #02

BUR-03 #01

BUR-04 #01

BUR-05 #01

BUR-06 #02

BUR-07 #02

BUR-08 #01

BUR-09 #02

BUR- 10 #01

BUR- 11 #02

BUR- 12 #01

BUR- 13 #02

STARTEDCOMPLETED

22/02/88 25/02/88

25/02/88 02/03/88

25/02/88 26/02/88

26/02/88 29/02/88

29/02/88 11/03/88

03/03/88 09/03/88

09/03/88 14/03/88

12/03/88 15/03/88

15/03/88 18/03/88

16/03/88 19/03/88

18/03/88 22/03/88

20/03/88 23/03/88

22/03/88 24/03/88

COLLARCO-ORDINATES

X: 900W Y: 1340S

X: 4900E Y: 2025N

X: 900W Y: 1175S

X: 900W Y: 775S

X: 350E Y: 850S

X: 350E Y: 500S

X: 350E Y: 160S

X: 5045E Y: 705N

X: 2000W Y: 325S

X: 900W Y: 350S

X: 2000W Y: 775N

X: 5900W Y: 050N

X: 2000W Y: 200N

AZIMUTHINCLINATION

180e -45.5*

180 e -50.5*

180 0 -45. 5 0

178* -45.5*

181 0 -50 0

180' -50 0

179 C -SO 0

174 0 -50 e

180 e -45.5*

ISO 0 ' -45 0

180 0 -45. S0

180e -45*

180" -45*

OVERBURDEN BEDROCK

7.3 192.7

46.1 198.9

6.5 142.5

7.3 192.7

52.4 225.6

40 207.2

44.9 215.1

37 191.3

20.8 236.2

16.2 227.8

19.3 197.7

41 150

27.7 160.3

TOTAL DEPTH

200

245

149

200

278

247.2

260

228.3

257

244

217

191

188

CUMULATIVE TOTALS; 0/B : 366.5 Bedrock : 2538

Total : 2904.5

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S*-''

The main purpose of the drill hole was to see if there might be a relation between this and other IP anomalies to the east (within the Blue Lake grid area) and the presence of abundant gold grains in pre-Wisconsinan gravels preserved in a topographic "hole" to the immediate northeast of Blue Lake.

The principal rock type logged is greywacke. Foliation measures are mostly in the 60 to 80 degrees to core axis (tea) range, with a few readings of 50 to 60* tea. We interpret these results to mean that the rocks dip north at 55 to 75*, with local more steeply dipping sections. The greywackes are locally cut by thin (*C1 m) porphyritic and mafic dykes.

The greywackes are fine grained quartz-feldspar-biotite schists. Minor garnet and/or amphibole porphyroblasts are locally present. The rocks are generally fresh and unaltered: calcite is present in variable amounts but is generally only a minor constituent.

Sulfide content of the rocks is very low. Pyrite was, however, smeared together with chlorite on many fracture planes. Where fracture density is significant, this pyrite could conceivably cause an IP response, for example at 110 to 125 m. This fracture zone would conceivably also explain the VLF anomaly.

The hole was not extensively sampled, due to the fresh appearance of the rocks, and due to the lack of structural deformation. The best gold value was 9 ppb, taken in a mafic dyke near the top of the fracture zone mentioned above.

BUR-02-(see MAP 3)

BUR-02 was drilled into the strong linear coincident high magnetic-EM anomaly which extends east-west across the northeastern part of the claim group. A ground geophysical profile (magnetics and VLF) was performed to facilitate hole positioning. The magnetics profile shows a well-defined peak anomaly with subsidiary magnetic features on the north flank. The VLF results show a low amplitude in-phase inflection with corresponding reverse quadrature crossover on this flank, which probably correlates with the northernmost of two parallel airborne EM anomalies detected with the DIGHEM survey.

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No outcrop is exposed in this eastern part of the property, and at the time of drilling, no reverse circulation holes had been completed in this area. We concluded, though, from later reverse circulation drilling that the high magnetic response was due to the occurrence of mafic metavolcanic rocks of limited thickness, within the metasedi- mentary pile. This situation resembles the setting at outcrop exposures in the north-central part of the property (trench 1).

The field description of the core can be subdivided into two main units. Predominantly micaschists are logged down to about 95 m, and afterwards, mostly argillites are described. Foliation measures range from 40 to 45* tea down to about 105 m, from 105 to 120 m they gradually change to 60 to 70" tea, and they remain in this range to the end of the hole, except for the interval 195 to 206.5 tn, where meter scale folds were observed. Acid tests indicate that between 120 and 180 m, the inclination of the drill hole changed from -47 to -33*, so we interpret these results to indicate mainly vertical to subvertical dipping units. The stratigraphy also includes minor quartzite, and has been locally cut by porphyry dykes.

The contact zone between the two main units is of particular interest since substantial sulfide mineralization is present. Both pyrite and pyrrhotite are present, mostly as coarse segregations in brecciated quartz-calcite clots. From 94.7 to 95.2 m the sulfide mineralization is described as "massive" and "earthy". Also, just below the interval of sulfide mineralization, at 98.3 to 100.6 m, the argillite is weakly graphitic and faulted. There is no obvious relationship between the sulfide mineralization and the fault.

Note that the position of the strongest magnetic peak does not correlate well with the location of the sulfide mineralization. Instead, it appears that the sulfides and graphite have caused the VLF response and subsidiary magnetic features on the north flank of the main peak (magnetic) anomaly.

The poor correlation between the main magnetic peak and the sulfide mineralization may be explained by the results of thin section studies and major element geochemistry. Although one sample, taken at 113 m, is clearly the same argillaceous greywacke that is predominant in BUR-08, the remaining samples have very high amphibole contents (up to 5(W and major element geochemistry more characteristic of tholeiitic basalt.

Textures observed in thin section are not typical of massive flow units, but show mineralogic banding at mm scale (which explains the metasedimentary interpretation given in the field). It is possible

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that this indicates incipient migmatization, or that these are metatuffs or volcanic derived immature metasediment s. In order to

l better understand the details of this drill hole, we should relog and* more extensively sample it.

The rocks are generally fresh and unaltered (with the exception of the sulfide interval and graphitic fault) although minor calcite occurs, which decreases in abundance with depth.

Pyrite and pyrrhotite occur everywhere throughout the hole in minor quantities. Occasional thin intervals of quartz-calcite veining with coarse pyrite and/or pyrrhotite resembling the sulfide interval occur elsewhere in the hole over short (say -20 cm) intervals. In general, though, sulfide content is ^H, and decreases with depth.

The principal sulfide interval was sampled, and two of these gave results of 0.2 g/t Au; a few samples were tested for Cu and Zn, the best values received were 0.0581 Cu and Q.264% Zn.

3.3 Burntbush Grid Area

3.3.1 Section 350E

Drilling along this section was performed mainly to investigate the geology and structure of the metavolcanic terrane east of the Burntbush River. We interpret from airborne geophysics and from bedrock elevation contouring that a northwest trending fault approximately follows the riverbed. The results of this profile were therefore also intended to test continuity of the stratigraphy and deformation across the fault.

Magnetics contouring in this part of the property is of low amplitude, in contrast with the variable susceptibilities encountered to the west, so a test IP line was performed here to aid in positioning of the holes.

BUg-05-(see MAP A)

BUR- 05 is the southernmost hole on the profile, and was drilled into a broad zone of weakly anomalous IP response. Coincident with the IP anomaly, the magnetics data show a transition from uniform (low) susceptibility to gently

- 14 -

increasing values towards the south. The VLF data are flat, but overburden thickness is considerable (*32 m in the nearest reverse circulation hole).

No outcrops occur in the immediate vicinity, but numerous exposures of metavolcanic rocks have been mapped in the southernmost part of the property. These are all greater than 0.5 km away from the collar location. One large outcrop occurs at about 0.5 km to the southwest, west of the Burntbush River (trench 3), and it deserves mention since it is located along a high magnetic trend which passes just south of the drill hole.

The outcrop consists of two main rock units: a mixed tuff unit is intruded by metagabbro. The tuffs include a dacitic lapilli tuff sub-unit and an iron-rich tholeiitic sub-unit characterized by abundant magnetite, garnet and hornblende. They are thinly interbedded and folded at cm scale. The beds are nearly horizontal and fold axes plunge gently to the east. We have interpreted that the outcrop may indicate the presence of a parasitic anticline located on the north flank of a major anticlinal axis somewhere further south. A few weakly anomalous gold values were obtained from grab samples here, the maximum value was 30 ppb.

Most of the reverse circulation bedrock chip samples from this area are interpreted as intermediate metavolcanics, but the nearest sample is a sheared felsic tuff (BOB-101), which assayed ^ ppb Au.

BUR-05 drill core can be subdivided into two main units. These are both mafic to intermediate metavolcanic units, but they are separated by a brittle fault zone at 206 to 238 m. The fault consists mostly of unconsolidated gouge and rock fragments locally cemented together with calcite. Associated with the fault, fracture related hematization extends into the adjacent units. Whereas foliations of the metavolcanics are generally near perpendicular to the core axis (eg 75 to 90* tea, suggesting north dips of about 45*), the main fracture trends in and adjacent to the fault are near parallel to the core axis. We have therefore intersected the fault at low angle, implying that the true thickness of the gouge zone may be less than ^5 m.

- 15 -

The upper metavolcanic unit consists mostly of weakly foliated to massive rocks which fall in the calcalkaline basalt and andesite fields on a Jensen cation plot (see Appendix I). Variable amounts of amphibole poikiloblasts and/or biotite flakes are set in a very fine grained groundmass of recrystallized feldspar and quartz. Microscopic textures are indicative of shearing of moderate to strong intensity, which was not apparent at mesoscopic scale.

Within this upper unit, there are several 2 to 7 m sections with abundant (10 to 207,) garnet poikiloblasts. These intervals are characterized by high total iron and MnO contents and plot as tholeiites.

Below the fault, the metavolcanics are slightly more felsic, plotting in the calcalkaline andesite and dacite fields. Biotite is generally abundant, and amphibole occurs only locally over short intervals. The feldspar-quartz groundmass is very fine grained and completely recrystallized, and shearing is judged to be of moderate intensity.

The most extensive alteration in the drill hole is an elevated calcite abundance, mostly in the form of tiny dispersed grains and as fracture fillings. It is difficult to evaluate the significance of this calcite since it is also present as a late cement in the brittle fault. A one meter strongly sericitized band located at about 8 m below the fault gave the highest C0 2 value (^77o). Chloritization is locally strong, but is not widespread. Finally, it should be added that the first 15 m of bedrock drilled was strongly fractured.

Sulfide content of the rocks is generally low. Minor disseminated pyrite generally accounts for <0.5% of the rock. In a 2.2 m band of altered, sheared felsic quartz eye tuff near the top of the hole, pyrite content may reach li*. In the last 15 m drilled, pyrite abundance seems to have been increasing (up to ^Q.5%), where it was associated with occasional thin quartz veinlets. Pyrite content in the core seems insufficient to explain the IP data.

Most sampling for gold analysis was concentrated in and adjacent to the main brittle fault. A few weakly anomalous values were received immediately above (12, 40 ppb), within (10, 20 ppb), and below (15 ppb) this zone.

- 16 -

p-

The best analytical value of 643 ppb Au was taken in the last 50 cm of core drilled (277.5 to 278.0 m). This result surprised us, as the core seemed fresh and unaltered. The closest sample taken is only 3.5 m uphole and gave ^ ppb; a weakly anomalous value of 10 ppb Au was received at 262.5 to 263.0 m. The pulp of the strongly anomalous sample was retested and gave 540 ppb. Further confirmation of this result is required, and it is suggested that the retained split core be sent for analysis, and that the last 10 to 20 m of the drill hole also be fully sampled.

Other weakly anomalous results received include values of 10 ppb and 37 ppb from weakly sheared garnet-rich tholeiites, and a 33 ppb result from the thin, strongly sheared felsic quartz eye tuff {near the top of the hole).

BUR-06-(see HAP 4)

BUR-06 was drilled into a much better defined IP anomaly than was BUR-05. The magnetics profile is relatively flat; the VLF profile shows a very subtle in-phase inflection coincident with the IP response.

The outcrops described previously (see BUR-05 introduction) are the only exposures close to BUR-06. Nearby reverse circulation bedrock chip samples are mostly of mafic to intermediate metavolcanic rocks; the closest sample (BOB-103) gave a gold value of 7 ppb.

In BUR-06, the predominant rock type encountered is a mafic to intermediate metavolcanic which strongly resembles those drilled in BUR-05. However, this hole is much less monotonous, since intercalations of several different units occur:

two thin (-5 m) sections of quartz eye tuff are present near the top of the hole;

two thin (*10 m) sections of feldspar porphyry are described;

. a 20 m thick crenulated schist unit occurs at 120 to 140 m;

a 7 m thick aphanitic rhyolite occurs just below the crenulated schist unit.

- 17 -

R'i'

Additionally, a few garnet-rich intervale, equivalent to those described in BUR-05 are present, and a brittle fault occurs at 183.5 to 195.7 m. Foliations are relatively uniform at 60 to 80" tea at the top and bottom of the hole, Which we interpret to indicate north dips of 55 to 75 0 . In the interval 90 to 170 m though, local variations suggest less uniform dips and evidence of minor meter-scale folds.

The principal mafic to intermediate calcalkaline metavolcanic unit differs from those described in BUR-05 in that the amphibole porphyroblasts are smaller, and recrystallization of the feldspar-quartz groundmass is less advanced; relict plagioclase phenocrysts are only partially recrystallized. These rocks are only very weakly sheared.

Brief descriptions of the minor rock units are given below:

. the quartz-eye tuff plots as a calcalkaline dacite and contains *lQf, quartz phenocrysts set in a fine grained groundmass of recrystallized feldspar and quartz. The quartz eyes are weakly strained and exhibit pressure shadows. The only ferromagnesian mineral is biotite;

the feldspar porphyry plots as a calcalkaline andesite and contains abundant sericitized plagioclase phenocrysts, along with minor coarse amphibole, set in a fine grained groundmass of recrystallized feldspar and quartz. Minor biotite flakes are present;

the crenulated schist unit is composed mainly of very fine grained recrystallized quartz and feldspar and with abundant coarse muscovite flakes which bend around relict plagioclase phenocrysts. In thin section, it is difficult to see a well defined, continuous crenulation cleavage, the mica flakes appear to be wrapped around phenocrysts, some of which are completely recrystallized. This rock plots in the calcalkaline dacite field;

the aphanitic rhyolite also plots in the calcalkaline field, and is composed mainly of very fine grained quartz and feldspar. Minor quartz eyes and relict plagioclase phenocrysts are preserved. The ferromagnesian minerals have altered to chlorite, and muscovite flakes are abundant (note: the high Na 20 analysis may indicate that the muscovite is in fact paragonite).

- 18 -

Shearing in hole BUR-06 is strongest in and adjacent to the crenulated schist unit. Elsewhere it is of weak intensity, but the degree of recrystallization suggests that minor widespread structural deformation is present.

The brittle fault zone consists mostly of unconsolidated gouge, and associated fracture orientations are again near parallel to the core axis. There is no apparent mineral alteration directly related to the fault.

Alterations include the widespread presence of minor sericite but this may be related to the greater abundance of felsic rocks relative to BUR-05. It is not clear whether the paragonite (?) seen in the aphanitic rhyolite is due to alteration or whether the original rock was sodium-rich. Chlorite is abundant in the crenulated schist, but in most other samples appears to be retrograde (see below). Calcite is never abundant (eg ^D and is commonly not present. The first 25 m of core is strongly fractured.

Of interest is the occurrence of coarse chloritoid flakes and prismatic crystals in the metavolcanics below the brittle fault. These samples are strongly chloritized (no biotite or amphibole remains) and also strongly sericitized. One thin section showed about 3* tiny euhedral elongate tourmaline crystals. This part of the hole is strongly altered, and although the rocks plot as tholeiitic dacite to rhyolite, this does not reflect a primary bulk composition.

Sulfide content of the rocks is generally low. Pyrite concentrations of up to about ITo are present in the crenulated schist and aphanitic rhyolite units. The pyrite is extremely fine grained in these units and uniformly disseminated. Although the concentration is estimated to be relatively low, the number of individual sulfide grains is quite high. It is not improbable that these units are the cause of the IP anomaly.

But, this mineralization does not.account for the VLF anomaly which alternatively, might be due to the brittle fault zone. If this is true, the fault might dip south and strike east-west (VLF profiles on adjacent lines to the east show a similar VLF response).

Continuous sampling for gold analysis was carried out in three separate parts of BUR-06: in fractured rock close to the bedrock surface, in the area of the crenulated schist and aphanitic rhyolite units and in and adjacent to the brittle fault. Punctual samples were taken elsewhere.

- 19 -

JSSY"

|; "

Near the top of the hole, in and adjacent to the uppermost quartz eye tuff unit, weakly anomalous values of 35, 21 and 10 ppb Au were received. Very local pyrite concentrations of up to 5X occur in this area. Further up, one result of 0.3 g/t (over 0.5 m) was also received, but the sample is bounded on either side by low gold values of 5 ppb or less.

Most samples taken in the crenulated schist and aphanitic rhyolite give background values; one sample shows 15 ppb. Just above these units, in altered feldspar porphyry, two samples gave 30 and 25 ppb Au.

Similarly, sampling in the vicinity of the brittle fault shows low gold values; one sample gave 10 ppb Au.

Deeper in the hole, a punctual sample of chloritoid-bearing rock gave 0.2 g/t Au. It is recommended that this part of the hole be further sampled, and a careful relogging of this part of the hole with particular emphasis on chloritoid abundance should also be done.

BUR-07-(see MAP 5)

The strongest IP response detected on section 350E was tested with BUR-07. The magnetics and VLF profiles are flat.

There is no outcrop near this drill hole. Reverse circulation bedrock chips to the south and west are predominantly mafic metavolcanics, but at 400 to 500 m away, to the north and east, biotite schists characteristic of the vast northern metasedimentary terrane are encountered.

The drill hole intersected a thick, well foliated and relatively uniform rock type over most of its length. In the field, there was disagreement as to whether this unit was metasediment or metatuff, and whether the sub-unit at 206.4 to 218.9 m contained pebbles or lapilli. The monotony of the drill hole is interrupted only by thin intervals of: a very fine grained graphitic unit (79.8 to 86.5 m), and a felsic tuff (at 91.8 to 108.6 m). Foliation measures in the first 45 m of core generally range from 60 to 70* tea, suggesting dips of 65 to 75* north. Below 90 m, foliations range from 70 to 85* tea, suggesting slightly gentler north dips of 55 to 70*.

- 20 -

The main rock type drilled is now interpreted to be a calcalkaline mafic to intermediate metavolcanic unit. Amphibole poikiloblasts and/or biotite flakes are set in a fine to medium grained feldspar-quartz groundmass. The foliation is generally defined by alternating ferromagnesian rich and poor domains at mm scale. Host thin sections appear to be only weakly deformed.

The graphitic unit is faulted and sheared and is composed mostly of very fine grained quartz and feldspar. Euhedral garnets are undeformed but inclusions within the poikiloblasts are well aligned. Presence of amphibole suggests the rock is tuffaceous.

The felsic tuff is conspicuously lacking in ferromagnesian minerals; chlorite and corroded garnet are present. Abundant relict sericitized plagioclase phenocrysts and lesser quartz eyes are set in a variably recrystallized quartz-feldspar groundmass. Samples taken from this unit plot as tholeiitic rhyolites.

Alterations are generally weak and are not widespread. Abundant dispersed calcite is present near the top of the hole, but elsewhere it was not present, or occurred as veinlets. Sericite alteration was evident in the felsic tuff, but is moderate to very weak in the more mafic rocks. Retrograde chloritization of biotite and/or amphibole is generally present, and is locally strong. The first 20 m of core is strongly fractured.

Pyrite occurs sporadically, but not uncommonly accounts for about IJt of the rock. The highest pyrite contents (*3X) were recorded in and adjacent to the graphitic tuff. This unit accounts for the strong IP response.

Sampling for gold analysis was not extensive due to the fresh, uniform appearance of the main rock type. Two samples taken near the bedrock surface gave 0.2 g/t Au. Other weakly anomalous results include a value of 17 ppb in felsic tuff, 14 ppb in the metavolcanic unit, and values of 13 and 21 ppb in the lapilli tuff sub-unit.

- 21 -

3.3.2 Section 900W

Four holes were drilled along this section located west of the Burntbush River primarily to ascertain whether or not the contrasting magnetics were due to structural features or due to normal (stratigraphic) rock unit boundaries. A test IP line was done along the camp's access road (which closely follows this section) and these results were used to aid in drill positioning.

BUR-01-(see HAP 6)

BUR-01 is the southernmost hole of this profile and is located near the southern border of the property. This hole, along with hole BUR-03 (to the north), was drilled to test the contact zone between low, uniform magnetics to the north, and high, variable magnetics to the south. BUR-01 was positioned to intersect an IP conductor coinciding with a well defined, but relatively weak VLF in-phase crossover with parallel quadrature response.

Nearby outcrops include trench 3, located at about 700 metres due east (see section 3.3.1), and a small outcrop of intermediate metavolcanic rock at 300 m to the west. This small outcrop is structurally similar to the layered rocks at trench 3 in that cm-scale open folds plunging gently to the east are abundant and the beds are near horizontal. Calcite alteration here is quite strong; the only sample taken gave 5 ppb Au.

Reverse circulation holes in this area are all classed as intermediate metavolcanics. Gold values range from ^ ppb to 7 ppb for most samples, but one sample, from BOB-158, which contains abundant free quartz and coarse pyrite (associated with the quartz but occurring also in the wall rock) gave 323 ppb Au. A second analysis gave 265 ppb. (Note that a result of 363 ppb was incorrectly reported in COGEMA Ref. No. 88-CND-47-01),

The hole is subdivided into two main units which alternate downhole. Mafic to intermediate flows (similar to those described in BUR-05 and BUR-06) predominate, and 5 m to 45 m thick intervals of lapilli tuff occur. Foliations range generally from 50 to 80 e tea, but there is a gradual trend towards greater angles with depth. The units probably dip north at 60 to 80*.

~ 22 -

i.

The flow rocks are composed of poikiloblastic amphibole and lesser garnet set in a very fine grained recrystallized feldspar-quartz groundmass. Relict plagioclase phenocrysts are common and only weakly recrystallized. The only "fresh" sample analyzed (it shows, in fact, moderate chlorite and calcite alteration) plots as a calcalkaline basalt; on the Jensen diagram.

The flow rocks become moderately magnetic with depth, and the increase in magnetite content may indicate that a mafic tholeiitic unit can be mapped using the magnetics contouring. This should be tested with additional sampling and analyses.

The lapilli tuff unit is characterized by rounded, elongate very fine grained felsic (to intermediate ?) clasts with mafic matrix identical to the flow unit. Contacts between this unit and the flow rocks are abrupt, and may be marked by late brittle fracture zones of limited depth extent.

Alteration of the mafic rocks includes extensive generally strong, pervasive calcite as interstitial dispersed grains and microfractures. Moderate chloritization of the amphiboles is also fairly extensive, but strongest in the first 100 m. At one of the brecciated contacts (between flow and lapilli tuff), sericitization was noted in addition to extreme calcite alteration.

Pyrite is the main sulfide mineral noted, and is everywhere present in minor amounts. In lapilli tuffs at 30-38 m, pyrite is more abundant (up to 5*) and this probably explains the IP response. The pyrite in this interval appears to be related to a small fracture/fault zone and is interpreted to be a mineralization rather than a primary feature. A second pyritic zone in the flow rocks at 156-166 m (up to 3*) was also seen. The VLF response may be related to the upper pyritic zone, or the fractured rock adjacent to it.

The two pyritic zones were sampled and most samples were sent to the Hine Yvan Vezina lab for analysis. In the upper interval (30-38 m), three values of 0.2 g/t were received and weakly pyritic hangingwall rocks gave weakly anomalous results up to 45 ppb Au (from Chimltec). The lower interval (156-166 m) also gave interesting gold values (up to 0.3 g/t). Both of these intervals should be resampled and sent for geochemistry analyses.

- 23 -

BUR-OS.Csee MAP 6)

BUR-03 was collared 165 m north of BUR-01 and was drilled to test whether or not the fracture zone at 30-38 m in BUR-01 was part of a larger structure. The magnetic profile shows low magnetics to the north, and higher magnetics (resembling the profile at BUR-01) to the south. VLF data are not flat, but no bedrock anomaly is interpreted.

Nearby outcrops and reverse circulation holes are as described for BUR-01.

The drill hole cut a monotonous mafic to intermediate metavolcanic flow rock, the same unit as has been described in previous holes. We recognize, however, two sub-units, one porphyroblastic unit (amphibole ± garnet) and one fine-grained "massive" unit. Foliations are mostly in the 50 to 65* tea range, suggesting subvertical north-dipping units.

The porphyroblastic sub-unit most strongly resembles that described in BUR-06 in that relict feldspar phenocrysts have been well preserved. One such sample falls in the calcalkaline andesite field on a Jensen plot, but local thin intervals rich in garnet (eg 25H at 54-58 m) suggest minor tholeiitic flows are present.

We interpret the fine grained "massive" sub-unit to be the strongly sheared equivalent of the porphyroblastic rock. Microscopic textures are clearly indicative of this and include: discrete grain size variations of the recrystallized feldspar-quartz groundmass, near total destruction of amphiboles replaced by newly crystallized flaky to fibrous chlorite, and the presence of two subparallel foliations which may occur together, or which may truncate one another. The drill log also indicates that minor faulting/brecciation is commonly observed in the "massive" sub-unit.

In addition to the chloritization, we observe local pervasive calcite alteration and local minor sericitization. Sericite generally occurs in fractured zones.

Sulfide content of these rocks is quite low, but, pyrite was more commonly observed in the "massive" sub-unit.

Only a few "punctual" samples were taken in this hole. One sample gave 0.2 g/t but this is not considered to be of particular interest.

- 24 -

BUR-04-(see MAP JO

BUR-04 is located 400 m north of BUR-03. It was drilled to investigate a strong magnetic-electromagnetic trend, and the southern contact of this trend.

There are no outcrops in this part of the property. Reverse circulation holes to the east gave weak Au values of 6 and 12 ppb in intermediate metavolcanics, to the southwest, Au values ^ ppb were received in a felsic metavolcanic.

The drill hole is subdivided into four units:

* from 7.3-74.1 m: very fine grained tholeiitic dacitewith abundant sulfides (pyrite ^ pyrrhotite, up to ion over significant lengths), may be thinly laminated or flow banded, i.e. probably a mixture of flows and tuffs, local minor amphibole and/or garnet poikiloblasts;

* from 74.1-124.9 m: stretched feldspar porphyry, strongly serlcitized elongate feldspars set in a very fine grained feldspar-quartz groundmass, falls in tholeiitic rhyolite field on Jensen plot;

* from 124199-200 m: mafic to intermediate porphyroblasticflow rocks similar to the main rock types described in BUR-01, BUR-03, except that here they plot in the tholeiitic andesite field on the Jensen diagram;

* from 178.0-193.5 m: 15 m unit within the flows, above, of thinly bedded mixed mafic and felsic tuffs (or stretched lapilli tuff), strongly reminiscent of the layered rocks at trench 3 (see section 3.3.1).

Contacts between the units are abrupt, and strongly fractured. The first 25 m of sulfidic rock is also strongly fractured. The felsic porphyry is sheared, as are the adjacent units within about 5 m of the upper and lower contacts. Foliations are somewhat variable, ranging from 60 to 85* tea, suggesting north dips of about 50 to 75*.

Extensive moderate calcite and sericite alteration is observed in the sheared rocks, and a weak to moderate chloritization is observed in all units.

- 25 -

Sulfide content of this hole is quite spectacular in the uppermost dacitlc unit, but pyrite is also quite abundant (average about 3fc) in the first 20 m of the feldspar porphyry unit. Deeper in the drill hole, pyrite is common but rarely attains IT,,

BUR-04 was sampled continuously from the bedrock surface to 131 m, this includes the suIfidle dacite unit, the sheared feldspar porphyry and the sheared part of the mafic to intermediate flow unit. Most samples give trace (Mine Yvan Vezina results) or very low (eg *(10 ppb) gold values. But, from 14-28 m, 5 of 12 samples gave results ranging from 24 to 60 ppb Au and two isolated samples in the feldspar porphyry gave 20 and 25 ppb Au.

Sampling below 131 m was punctual, but three relatively fresh-looking samples taken in the flow rocks gave 0.2 g/t Au.

BUR-10-(see MAP l)

BUR-10 was collared at 425 m north of BUR-04, and is the northernmost hole of section 900W. The hole was drilled to test magnetic contacts suggestive of an east-west structure, and an east-northeast trending stratigraphic and/or structural contact. In profile, the east-west feature appears as a trough between two magnetic peaks, with an associated VLF in-phase inflection, the east-northeast feature coincides with the southern limit of the southern magnetic peak. In this area, the IP test line (camp road) has veered northeast towards the river, and the data suggest anomalous conductivity "off-line".

There is no outcrop near here; reverse circulation drilling in nearby holes indicated intermediate metavolcanle bedrock. The nearest hole gave 6 ppb Au, results at 400 m to the east and west gave 8 and 11 ppb Au, respectively. Note that these three reverse circulation holes fall on section E-E', which consistently gave weakly anomalous gold values.

In this hole, we drilled a non-uniform sequence of mixed tuffaceous rocks, along with a 40 m thick blue quartz porphyritic unit. In general, the tuffs are more felsic uphole, more mafic downhole. Foliations in the upper part of the hole range mostly from 50 to 80* tea, but are characterized commonly by 30* changes over short intervals.

- 26 -

Thereafter, foliations are more uniform, gradually changing from 60 to 70* tea (in the quartz porphyry) to 65 to 80 e tea in the last 100 m drilled. This suggests that folding is common, but that with depth, units more consistently dip to the north at 60 to 80*.

In the interval 16.2-91.4 m (above the blue quartz porphyry), the rocks are mostly composed of fine grained biotite, feldspar and quartz with local intervals showing quartz eyes and/or altered feldspar phenocrysts. They are thinly laminated and weakly to moderately well sheared. Host samples analyzed for major elements fall in the calcalkaline dacite to rhyolite fields on the Jensen plot. One sample which plots as a calcalkaline basalt in fact carries 60% Si0 2 and is very strongly altered; another plots as a tholeiitic dacite: probably this is due to a local concentration of pyrrhotite.

The quartz porphyry could probably be included with the mixed tuffs of felsic tendency described above, but it does represent a uniform 40 m thick unit. It is moderately sheared.

In the interval 130.4-244 m, most thin sections show poikiloblastic amphibole, thus the tendency towards more mafic (calcalkaline basalt to andesite) compositions. The one sample which gives a tholeiitic chemistry trend contains significant garnet poikiloblasts and has an MnO analytical result of Q.46%, and was taken from a distinct 3 m thick unit. These more mafic rocks are generally only very weakly sheared.

This hole is mostly strongly altered, particularly in the more felsic rock types where calcite and sericite are abundant. Chlorite and epidote are also commonly observed along with very minor tourmaline and possibly also fuchsite. The mafic rocks are strongly altered in the same manner but slightly less so.

Pyrite is the main sulfide mineral, but pyrrhotite is commonly present in minor quantities. Sulfide abundance consistently approaches 0.5 to 11* in the more felsic rocks (i.e. down to about 130 m), and thereafter it decreases quite dramatically. At 87-90 ra, pyrite content attains lOH over short intervals, and these local concentrations are coincident with sections where the foliations parallel the core axis.

- 27 -

We sampled this hole continuously in the first 50 m and in shorter sections (eg up to 15 m) in various other intervals, as well as punctually throughout. In the short section of abundant pyrite at 87.2-88.2 m, two adjacent samples gave 300 and 75 ppb Au. At 23.0-30.5 m a weakly anomalous zone (eg 10 to 25 ppb Au in 6 samples and 95 ppb Au in a seventh) occurs and just below this at 43.5-45.5, two adjacent samples gave 64 and 50 ppb Au.

3.3.3 Section 2000W

In effect, this section can be considered the northern extension of section 900W, since the magnetic contours suggest an east-northeast striking stratigraphy in these areas. Drill hole positions were chosen based on magnetics and/or geologic interpretations; no induced polarization was performed here.

BUR-09-(see MAP 8)

BUR-09 is the southernmost hole on this profile and was drilled across a strong magnetic anomaly. Magnetics contouring suggests that we may have drilled the north limb of a fold whose axial trace trends east-northeast. But, we also interpreted a possible east-west structure extending from this hole directly towards hole BUR-10.

No outcrops occur in this area; reverse circulation holes nearby include one hole at *150 m to the west in an area of low magnetics, and one hole at -250 m to the east in an area of high magnetics. The former drilled into an intermediate metavolcanic which gave 14 ppb Au, the latter was a felsic metavolcanic which gave 8 ppb Au.

The drill hole is subdivided into two main units. In the upper part of the hole (from 20.9-130.8 m), quartz ± feldspar crystal tuffs were intersected. In the lower part (130.8-257.0 m), biotite rich tuffs with abundant felsic lapilli occur, along with a relatively coarse grained, massive feldspar porphyry unit which we interpret to be a late felsic dyke. Foliations in the first 75 m are generally 45 to 55* tea, suggesting vertical orientations. Thereafter, foliations are generally 60 to 75* tea, suggesting north dips of 65 to 80*.

i?,,- 28 -

!!*r,;

The upper crystal tuff unit is composed of feldspar phehocrysts and quartz eyes up to several mm in size set in a very fine to fine grained recrystallized quartz-feldspar groundmass with minor biotite flakes. Locally, the quartz eyes become slightly stretched and partially recrystallized, and in these intervals the feldspar phenocrysts are also partially to completely recrystallized and may be totally lost in the groundmass. Thus, this unit can be subdivided into two sub-units, one of which is the sheared equivalent of the other. Most of these samples fall in the calcalkaline dacite field on a Jensen cation plot; one sample plots in the tholeiitic field but this sample carries significant pyrite.

The lapilli tuff in the lower part of the hole is composed of felsic, weakly porphyritic, rounded, locally elongate lapilli (fragments reach a maximum of about 20 cm) set in a fine grained groundmass of feldspar-quartz-biotite which is also weakly porphyritic. Two samples from this unit also plot as calcalkaline dacites.

Within the lapilli tuff unit, we observed two intervals of feldspar porphyry which we interpret to be dyke material. However, the contacts are concordant so they may alternatively be sills, flows or tuffs. The feldspar phenocrysts are pinkish and are generally about l cm in size, and the groundmass is massive to only weakly foliated, thus this unit is clearly distinct from the thinly laminated tuffs in the upper part of the hole. One sample analyzed for major elements plots as a calcalkaline rhyolite.

Alterations in the rock units' are generally weak, most evident is the abundance of calcite in all rock types except the sheared tuffs in the upper part of the hole. Sericite/muscovite is also relatively common, but in quantities which are not unusual for felsic rocks.

Sulfide content of the drill hole is somewhat anomalous. The crystal tuffs generally contain l to 3X disseminated pyrite, and from 54 to 85 m, pyrite content is estimated at 5J,. The lapilli tuffs also have a pyrite content of l to 3fc, but no pyrite was observed in the feldspar porphyry dykes. The strong magnetic peak does not obviously correlate with any particular rock unit or mineralization, and seems to reflect an increased magnetite content recorded in the lapilli tuffs at 140 to 185 m.

- 29 -

Sampling for gold analysis is quite extensive in the upper laminated tuffs, whereas mostly punctual sampling was performed in the lapilli tuffs and feldspar porphyry dykes. A number of samples gave weakly anomalous gold values, the most significant being the interval 131.5 to 137.5 m (the top of the lapilli tuff where it is in contact with sheared crystal tuffs) where three of five samples gave 95, 70 and 55 ppb Au.

BUR-13-(see MAP 8)

BUR-13 was drilled into a low magnetic area in the north part of the "high magnetic terrane" to investigate the geology, and to test for the presence of a northwest trending fault interpreted from regional airborne magnetics. The VLF is flat.

Again, no outcrop is exposed near here; reverse circulation drilling results show mafic to intermediate metavolcanic bedrock. Hole BOB-58, at *200 m to the southwest, gave 31 ppb Au.

We intersected a monotonous sequence of mafic to intermediate calcalkaline metavolcanics. Foliations range from 55 to 75* tea, suggesting north dips of about 60 to 800 .

These are composed of amphibole poikiloblasts and occasional relict plagioclase phenocrysts set in a fine grained, weakly recrystallized feldspar-quartz groundmass. Very minor, thin dykes of similar composition were also observed.

Alterations are weak and mostly restricted to sericitization of the relict plagioclase. The first 25 m of core is very strongly fractured, but it is difficult to conjecture whether or not this is a manifestation of a regional structure.

Sulfide content is low, but up to 51* pyrite was observed very locally.

Sampling for gold was very punctual due to the fresh, unaltered appearance of the core. One sample gave 260 ppb Au; it was taken adjacent to a pyritic interval and justifies some additional sampling in this hole. (A reanalysis of the pulp gave 290 ppb).

- 30 -

F;:-

BUR-U^see MAP 9)

BUR-11 was drilled at 300 m east of an outcrop of strongly sheared metagabbro (trench 2), which we interpret to lie approximately along the contact between the vast metasedi- mentary terrane to the north, and the metavolcanic. terrane which lies to the south. Whereas the outcrops show a strong magnetic signature, the area drilled shows low, uniform magnetics. The purpose of this hole, then, was to investigate this deformation zone outside the intrusive body.

Other, undeformed metagabbro exposures occur to the northwest of trench 2, thus limiting the width of the shear zone to the north, but no other similar outcrops occur south of it. Much sampling was done in these gabbros, and a small percentage of the samples gave anomalous gold values up to 110 ppb, commonly related to local silicification.

Reverse circulation holes to south intersected mostly mafic metavolcanic rocks, but these are several hundred metres away. Perhaps of significance was the discovery of irregular gold grains in the basal till of BOB-94, although drilling at 200 m further north yielded no anomaly.

Host of the hole intersected sheared metagabbro. The magnetic expression of the outcrops may therefore be largely due to their proximity to surface (although overburden depth here is only 14 m). Schistosity is generally at 55 to 75* tea and shows truncations and minor folding. The hole ended in a weakly foliated to massive felsic intrusive.

Sheared metagabbro strongly resembles surface samples described in earlier reports: amphibole and feldspar are the chief constituents, and the well developed schistosity is mostly due to grain size variations and thin shear planes. In drill core though, we observe more biotite than we reported from the surface samples. Significant widths of barren white quartz vein are reported at 71 to 78 m.

The weakly deformed felsic rock is composed mainly of plagioclase phenocrysts. These are set in a weakly to moderately sheared quartz-feldspar groundmass which clearly comprises only about 20 to 301 of the rock. Garnet porphyroblasts are not uncommon.

- 31 -

Although the metagabbro is strongly deformed, it is only weakly altered.

Sulfide content is low, but short intervals of core may contain up to 5% coarse pyrite and/or pyrrhotite.

This hole was sampled continuously from 19.3 to 161 m (and punctually thereafter), but most results are low. Isolated weak anomalous values, eg 20-80 ppb Au are common, but are mostly bounded by adjacent background samples. One result of 480 ppb Au was received from a sample of sheared metagabbro right at the contact with the felsic rock. It too, is bounded by adjacent samples which give low values.

3.4 Spade Lake Area

One hole was drilled along section 5900W (BUR-12, see MAP 10) to investigate a magnetic boundary with a corresponding VLF response best described as a transition between low quadrature readings (to the south) and high quadrature readings (to the north).

No outcrop was found in this part of the property. But, at &800 m south of our claim boundary, Newmont has trenched to bedrock and exposed mostly felsic to intermediate crystal tuffs. There are very weakly sheared to strongly sheared; intensity of shearing in the trenches is stronger to the north. Subsequent drilling by Newmont intersected the following lithologies from north to south: a pink sodic granite, intermediate tuffs, a tholeiitic basalt, more tuffs, argillites. Shearing is described only in the southern tuffs, and erratic economic gold values were obtained over narrow widths, mostly in quartz-pyrite veins. Anomalous gold values are widespread (see COGEMA Ref. No. 87-CND-47-04).

Reverse circulation holes in this area intersected mainly a red coloured "felsic crystal tuff" which we later re-interpreted as the sheared equivalent of the pink sodic granite described by Newmont. Some holes intersected felsic to intermediate metavolcanic rocks as well, and overall, most holes gave weakly anomalous gold values ranging up to 28 ppb. Thus, the drill hole was positioned not solely on the basis of geophysical results.

BUR-12 intersected the reddish sodic granite over most of its length. We have chosen to call it a granodiorite porphyry. In the first 100 m, it is strongly sheared and fractured, and less extensive

- 32 -

IV' lv'

sheared intervals also occur deeper in the hole. The shear fabric (foliation) is mostly oriented at 75 to 85 e tea, indicating northerly dips of 50 to 60". Near the end of the hole, we drilled two intervals of a felsic quartz eye tuff (xenoliths ?).

The "fresh" granodiorite porphyry is composed of weakly sericitlzed plagioclase phenocrysts and lesser quartz eyes up to about l cm large, set in a sheared groundmass of recrystallized quartz and feldspar, along with some biotite, sericite, calcite, chlorite and opaques. Although the core appeared massive, the groundmass is incredibly well oriented in thin section, wrapping around and between the abundant phenocrysts.

The felsic crystal tuffs are similarly weakly sheared, but few phenocrysts are present, mostly of quartz.

The major sheared interval (eg from 40 to 100 m), shows typical development of mylonite. In most cases, the rock cannot safely be identified as the sheared equivalent of the porphyry, it is very fine grained, may be grey or pink, and is strongly fractured (and oxidation related to the fracturing has stained much of the rock to a dirty yellowish colour). However, locally, where the rock is pink, even though it is well foliated and fine grained it closely resembles thinner, less intensely sheared intervals deeper in the hole.

Alterations in the main sheared interval are strong and include abundant chlorite, sericite, calcite and the development of uncommon minerals, one of which has been tentatively identified as vivianite. Alterations are weaker in the "fresh" granodiorite porphyry and the crystal tuff units.

Sulfide mineralization in the shear includes disseminations of fine grained pyrite up to about 10% of the rock over short intervals, and as coarser pyrite grains in thin quartz ± tourmaline veins. We also observed trace amounts of chalcopyrite and galena. Fine grained disseminations of arsenopyrite may be present; we have requested As analyses to confirm this, but results have not yet been received.

Gold values in the main shear are clearly at anomalous levels. These are summarized in Table 2.

- 33 -

Table 2 : SUMMARY OF GOLD RESULTS - BUR-12(41.0 - 107.0 m)

Depth Weighted Average Range It samples (m) (Au ppb) (Au ppb)

41.0- 45.5

45.5- 56.0

56.0- 65.0

65.0- 68.0

68.0- 77.0

77.0- 84.5

84.5- 86.0

86.0- 89.0

89.0- 95.0

95.0-107.0

rt

44

282

35

187

7

150

30

. 308

12

3

20- 65 5

130-550 4

1

160-230 3

tf- 20 5

1

1

135-480 2

rt- 45 8

Recovery (*)

100

75

55

40

60

90

90

80

70

98

- 34 -

4. DISCUSSION OF RESULTS

4.1 Blue Lake Area

The main rock type of the "northern low magnetic terrane", is confirmed to be (argillaceous) greywacke. These have been metamorphosed to amphibolite facies, so that the term quartz- feldspar-biotite ± garnet schist better describes the rock.

Linear high magnetic trends within the metasediments are due to rocks of mafic metavolcanic affinity, generally carrying ^QJ, amphibole with abundant calcic plagioclase (andesine-labradorite).

We interpret the greywackes to be a thick sequence of turbidite sediments, within which occur minor thin, but laterally extensive tholeiitic mafic volcanic units.

Although we drilled only two holes in this part of the property, one zone of possible interest was intersected in hole BUR-02. In this hole, at *92 to 98 m, a thin interval of sulfide mineralization occurs adjacent to a weakly graphitic fault zone. Unfortunately, core analyses gave low results for Au, Cu and Zn.

Elsewhere, the rocks were fresh and unaltered, and Au geochemistry results show low background values.

4.2 Burntbush Grid Area

4.2.1 Rock Types

The most common single rock type drilled on the Burntbush grid is a mafic to intermediate weakly foliated metavolcanic containing poikoloblastic amphibole ± garnet set in a finer grained mostly recrystallized groundmass of plagioclase, biotite and quartz ± relict plagioclase phenocrysts. We interpret these to be basalt and andesite flows which have been metamorphosed to lower amphibolite facies. This is the predominant rock type in holes BUR-01, BUR-03, BUR-05, BUR-06 and BUR-13, and is a subsidiary rock type in BUR-04.

Most of these show calcalkaline chemistry, but a few samples rich in garnet (high FeO) are tholeiites, and we suspect that BUR-01, which has anomalous magnetite content, may also be largely tholeiitic.

- 35 -

Pyroclastic rocks of similar composition also occur, Lapilli tuffs in BUR-01 have a matrix which is identical to the above rock type, but ashfall tuffs in BUR-07 and the last 100 m of BUR-10 contain more abundant biotite, and therefore show a better defined foliation. BUR-07 also contains minor lapilli tuff, and crystal tuffs occur in BUR-10.

Truly felsic metavolcanic rocks were drilled in only three holes. The stretched feldspar porphyry from BUR-04 (74.1-124.9 m) and a silicic quartz eye tuff from BUR-07 (91.8-108.6 m) plot as tholeiitic rhyolites, while the aphanitic (porphyritic) rhyolite in BUR-06 (143.4-150.7 m) plots in the calcalkaline field.

The remaining, intermediate metavolcanic rocks are variable in appearance. These include pyritic dacite tuffs and flows from BUR-04 (7.3-74.1 m), ash tuffs from BUR-05 (238-278 m), various units in BUR-06 (including quartz eye tuffs, ash tuff, feldspar porphyry, crenulated schist; all are of limited depth extent), crystal and lapilli tuffs in BUR-09, and ash and crystal tuffs in the first 130 m of BUR-10. For mapping purposes, we distinguish an intermediate subdivision only when a distinctive unit has a substantial thickness; in all other cases, we include these intermediate rocks together with the mafic or felsic units with which they occur (see logging summaries, Appendix I).

The intermediate metavolcanics are predominantly calcalkaline; but, the pyritic dacites from BUR-04 plot as tholeiites.

Intrusive rocks were drilled in hole BUR-11. Sheared metagabbro was logged in the first 140 m of core, and a more felsic, weakly sheared intrusive occurs afterwards.

4.2.2 Structure and Deformation

We have interpreted many of the rocks drilled in the Burntbush grid area to be sheared. It should, however, be emphasized that nowhere does the intensity of this shearing approach that observed in the metagabbro drilled in hole BUR-11. The drill core is easily compared with the outcrops exposed to the west, and for this reason, no detailed discussion is presented.

In hole BUR-09, we interpreted from mesoscopic observations that parts of the feldspar-quartz porphyritic schist were sheared based on textural relations. These sheared intervals show a better schistosity, stretching of quartz-eyes and destruction of feldspar phenocrysts.

- 36 -

In hole BUR-04, we interpreted the stretched feldspar porphyry to be sheared, mainly due to the highly elongate feldspar phenocrysts. But, further support for this interpretation was found in the form of dislocation of garnet porphyroblast^ in the mafic to intermediate rocks immediately adjacent to the unit.

Finally, we suggested that the crenulated schist unit of BUR-06 was sheared, but we recognize that micaceous rocks need not be sheared to display a strong crenulation fabric.

Our field descriptions contain occasional references to shearing elsewhere, but we now interpret shearing to be more widespread than previously thought. This is due to microscopic examination of the mafic to intermediate amphibole schists which display the following:

- the groundmass in which amphibole ± garnet occurs is strongly recrystallized. Plagioclase and quartz are so fine grained that they cannot be distinguished in thin section. Furthermore, grain size variations within this groundmass, along with oriented biotite flakes, show the presence of two subparallel foliations which may occur together, and which also commonly truncate each other.

- samples in which these textures are poorly developed show relict plagioclase phenocrysts and a gradation between these and more strongly sheared examples can be described. As intensity of shearing increases, plagioclase phenocrysts become more strongly recrystallized, to the point where none remain. The more strongly deformed samples show stretched and dislocated amphiboles and/or garnets, and finally, amphibole may be completely destroyed and replaced by chlorite flakes. The strongest shearing is exhibited by the "massive" intervals in BUR-03. Note that the field log for BUR-03 shows a good correlation between minor faults and "massive" texture, and that this hole (along with the stretched quartz crystal tuffs in BUR-09) also shows more vertical dipping units, relative to the others.

Widespread shearing in this area might also explain why all of the clasts in the lapilli tuffs are so well rounded, flattened and elongate. Alternatively, these may be epiclastic deposits,

- 37 -

i:

Using such widely spaced drill holes, combined with the paucity of outcrop exposure, it is difficult to map where deformation is most intense, or to speculate on the orientation of the strongest "shears". However, it is our interpretation that local areas within the grid are very strongly sheared, and that others are more or less, completely undeformed, and that the remainder shows weak to moderate shear fabric.

In addition to shearing, we observed two brittle faults of possible regional significance. The fault in hole BUR-06 may trend east-west and dip south (based on fracture orientations and a weak VLF response) . Orientation of the fault in hole BUR-05 is more speculative; we suggest that it may trend northwest and be part of a larger fault system which approximately follows the Burntbush River in this area (based on fracture orientations, regional magnetics interpretation, and the observation that the VLF response interpreted to correlate with the fault in BUR-06 continues east of the line, but disappears west of the line) .

4.2.3 Magnetics as a Mapping Tool

Before beginning this drilling program, we postulated that the boundary zones between high and low magnetic trends within the "southern high magnetic terrane" represented stratigraphic and/or structural boundaries between different rock units. The results of our drilling support this interpretation, but detailed mapping using the available drill holes and the magnetics map is not possible.

For example, drill holes which intersected predominantly mafic to intermediate calcalkaline metavolcanics (flows and tuffs taken together, BUR-03, 05, 06, 07, 13) ail fall in areas of low magnetics. Hole BUR-01 may be the only exception, since magnetics contouring shows an east-northeast trending zone of moderately high values. But, we suspect that additional sampling will show that magnetite content in this hole will substantially increase the iron content relative to the others, and that this represents a tholeiitic unit.

But, within these holes, different units of limited depth extent occur which have no apparent magnetic signature (for example, thin (*3m) tholeiitic basalt flows, or a 30 m unit in BUR-06 containing crenulated schist and aphanitic

- 38 -

fe"

rhyolite). Note that a change from mafic to intermediate flows, to intermediate tuffs in BUR-OS appears to correlate with a transition to higher magnetics.

Hole BUR-11, which drilled sheared metagabbro and a felsic intrusive is also located in low magnetics. Previously, we had interpreted that circular high magnetic anomalies located to the west and northwest of the drill hole defined the limits of the metagabbro, but now it seems possible that they are related to the bedrock topography. Thus, the true extent of this unit can only be guessed at.

The remaining three drill holes are all located along high magnetic trends. The southernmost of these, BUR-04, intersected ^67 m of dacites, followed by *51 m of felsic stretched feldspar porphyry. The last 75 m of core is mostly mafic to intermediate metavolcanics, which correlates well with the decrease in magnetics towards the south. However, these have tholeiitic chemistry and so they differ somewhat from BUR-01, where magnetics is higher.

BUR-09 and BUR-10 appear from the magnetics map to occur on a fold; BUR-09 on the north limb and BUR-10 very close to the hinge, and on the south limb. It is interesting that foliations measures in the upper part of BUR-10 suggest that folding is common; this may support the interpretation that this magnetic feature really is a fold hinge.

BUR-10 intersected a mixed section of pyroclastics. These plot mostly as calcalkaline dacites down to 130 m and afterwards they become somewhat more mafic, plotting as calcalkaline basalt and andesite. This change in composition approximately correlates with a decrease in magnetics, we therefore place the last 100 m of this hole in the same (regional) unit as the flows and tuffs in BUR-03, 05, 06, 07 and 13.

BUR-09 intersected feldspar-quartz crystal tuffs down to 130 m, and these are followed by mainly lapilli tuff. Both units show calcalkaline dacite compositions, but only part of the lapilli tuffs correlate with high magnetic values.

Hap 11 shows our geologic interpretation of the Burntbush grid. We have considered all of the available geologic data (from outcrop, reverse circulation and diamond drilling) along with the magnetics, and to a lesser extent, VLF and IP results.

- 39 -

IF

It

l* f

This interpretation is necessarily somewhat preliminary, and the relationship of rock units across the interpreted structures is difficult to ascertain. The internal symmetry within each of these blocks is also not well defined.

It is, though, of interest that magnetics suggests that rock units strike east-northeast. Since we interpret the main shear in the north part of the grid area to strike east-west, and since we suggest that much of the foliations developed in the "massive" rocks to be a shear fabric, it can be postulated that the entire grid lies within a large east-west trending structural deformation corridor.

This also suggests that drill holes should have been oriented more southeast. This is not a major problem since the angular difference is small, but it indicates that the foliations dip more steeply than indicated in section 3.2.

4.2.4 Alterations and Gold Geochemistry

Section 3.50E

Alterations in BUR-05 and BUR-07 are more or less restricted to anomalous calcite abundance. In BUR-05 this may be more due to the late brittle fault which shows a calcite cement; in BUR-07, this calcite is present mainly in the first 50 m drilled.

Gold geochemistry in these two holes show mostly background to very weakly anomalous results. The best value of 643 ppb Au was taken in the last 50 cm of core from BUR-05. It is perhaps significant that the intensity of shearing seemed to be decreasing towards the end of the hole, and that thin quartz-pyrlte veins become more abundant.

Alterations in BUR-06 are variable, due in part to the diversity of rock types. Sericite and paragonite (?) may be related to alteration (paragonite may be metamorphic derivative of pyrophyllite). We also consider that the chloritoid in the mafic metavolcanics towards the end of the hole is an alteration mineral. A brief review of the literature shows that:

- 40 -

i) bleached wall rocks adjacent to ore at the CasaBerardi deposits commonly show a sericite-ankerite- chlorite-quartz ± chloritoid 4; chromian mica assemblage (Pattison et al. 1986). Whereas chloritoid in BUR-06 is coarse and euhedral, chloritoid at Casa Berardi occurs as minute, usually microscopic grains. Sericite, chlorite, quartz and tourmaline are also present in the altered rocks in BUR-06, but ankerite and chromian mica have not been identified.

ii) a progressive alteration package including chloritoid has been documented from the East South "C" ore zone at the Dickenson Mine (Red Lake district). Mathieson and Hodgson (1984) have shown that as intensity of alteration increases, hornblende content decreases rapidly and eventually disappears. Newly formed minerals include biotite, chlorite, chloritoid, staurolite, andalusite, and in the most strongly altered rocks, garnet (see Fig. 2). The analogy with BUR-06 is most pertinent since this part of the Dickenson Hine is within the metamorphic aureole of an intrusive body and is at amphibolite facies. Note that co-existing hornblende and chloritoid has not been found in these altered rocks in BUR-06.

iii) at the Bousquet property, in the western part of the no. 6 mineralized zone, sheared and altered basalts locally contain up to 25H chloritoid crystals that cut across all tectonic fabrics (Tourigny and Hubert, 1986). This texture is remarkably similar to that observed in BUR-06.

Gold geochemistry results from BUR-06 show background to weakly anomalous results. However, the chloritoid-bearing rocks were inadequately sampled.

Section 900W

Chlorite alteration is moderate to strong and is extensive in holes BUR-01, 03 and 04. It is most evident in BUR-03 and the upper parts of BUR-01. Calcite and sericite alteration are also commonly observed in all of the drill holes.

- 41 -

UMTB Hb

lncr*oiing intensity of oltirotion

FIG. 7. Schematic representation of the variation in abundance of minerals indicative of alteration in mafic mctavolcanic rocks in the ESC ore zone. Symbols: UMTB - unaltered metamorphosed tholeiitic basalt: Hb * hornblende or weakly altered facies: Bi-Chl * biotite-chlorite or moderately altered facies; Gt " garnet or strongly altered facies.

Figure 2 : Progressive alteration assemblages in the East South ore zone at the Dickenson Hine, Red Lake district (from Mathieson and Hodgson, 1984)

- 42 -

Gold geochemistry results from 'drill core along 900W show mostly low background to weakly anomalous values. The pyritic intervals in BUR-01 should be resampled (eg 30-38 m, 150-165 m), Elevated results in BUR-04 (up to 60 ppb Au) are probably related more to anomalous pyrite abundance than to a gold mineralization event. Finally, in BUR-10, we interpret anomalous gold values (up to 95 ppb Au) to be of possible significance, but we suggest that two adjacent samples which give 300 and 75 ppb Au are related to a minor local zone of enriched pyrite content.

Section 2000W

Alterations along this profile are generally of weak intensity.

Gold geochemistry results give mostly low background to weakly anomalous results. A maximum result of 480 ppb Au, and other values up to 80 ppb Au in BUR- 11 suggest that there is some Au mineralization to be found associated with the shear zone. Although one sample from BUR-13 gave 260 ppb Au, it is difficult to explain its importance. In BUR-09, anomalous results up to 95 ppb Au in lapilli tuff adjacent to sheared crystal tuff should be further Investigated.

4.3 Spade Lake Area

In hole BUR-12, we drilled a shear zone which shows anomalous gold values (up to 550 ppb Au) over significant lengths. This shear zone approximately follows the northern contact of a sodic granodiorite porphyry intrusive. Undeformed rock north of the shear was not intersected.

This is considered to be the most important result of the 1988 exploration program. Problematic is the fact that fracture density is high and there was much core loss, making analytical results difficult to evaluate. But, the shear has a clear geophysical signature and should be fairly well delineated using surface methods.

- 43 -1 '

'i'-.': ••f\ SiS "

5. SUMMARY AND CONCLUSIONS

Two holes were drilled in the eastern part of the property and we believe that the results obtained are applicable to all of the "northern low magnetic terrane".

We interpret the northern part of the property to be underlain by a thick turbidite sequence, within which occur minor thin, but laterally extensive tholeiitic mafic metavolcanic units. These metavolcanics can be mapped using magnetic contours since they have higher susceptibilities.

In hole BUR-02, a thin sulfide rich interval occurs adjacent to a weakly graphitic fault zone. Although Au, Cu and Zn analyses gave low values, this zone could have polymetallic base metal potential along strike. Till samples taken from reverse circulation holes do not, however, show any anomalous Cu or Zn values.

Elsewhere within the "northern low magnetic terrane", exploration work has not provided us with any indication of potential economic mineralization. But, it should not be forgotten that drilling by Dome Exploration Ltd in 1982, along a northwest trending EM conductor in the central part of the property, intersected quartz veining which gave a few values of 0.4 dwt/ton Au (*0.7 g/t) over short (^ m) intervals.

Within the Burntbush grid area, ten holes were drilled, and these have greatly improved over ability to interpret the geology in this part of the property.

Low magnetic areas are underlain by a calcalkaline mafic to intermediate metavolcanic sequence. These are mostly flows; but pyroclastics are not uncommon. The low magnetic band joining the area south of BUR-10 and drill hole BUR-07 may, for example, be dominated by tuffs. Within this sequence we also observe minor thin intervals of tholeiitic basalt and felsic to intermediate lithologies which have no apparent magnetic signature.

The main exception to this generalization is the northern part of the grid, which is characterized by low magnetic values where BUR-11 was drilled. The large mass of metagabbro which we intersected, and which outcrops to the west and northwest cannot be mapped by outlining the circular magnetic features as previously thought; these may alternatively be related to bedrock topographic highs.

- 44 -

l*:'

Three main east-northeast trending high magnetic zones cross the central and western parts of the grid. The southernmost band is believed to represent a 100 to 200 m thick tholeiitic basalt unit, the central band represents sulfide-rich tholeiitic dacites in contact with a felsic feldspar porphyry unit, while the northern zone has the shape of a fold. This zone appears to be composed of a mixed succession of mostly intermediate calcalkaline (dacitic) pyroclastics.

These rocks have been metamorphosed to lower amphibolite facies, the predominant mineral assemblage in the mafic rocks, for example, is hornblende, biotite, plagioclase, quartz ± garnet with minor retrograde chlorite.

All of the rocks are interpreted to be weakly to moderately sheared, and locally shearing is very well developed. It is strongest in the metagabbro of BUR-11, but is also well displayed in crystal tuffs in BUR-09, in the stretched feldspar porphyry in BUR-04, and in the mafic rocks in BUR-03.

Whereas foliations are interpreted to be mostly oriented east-northeast, with steep northerly dips, we suspect that these discrete "shears" trend east-west. Although we have suggested this to be evidence of a wide structural deformation "corridor", magnetics contouring to the west indicates foliations trend east-west there.

Our evaluation of alterations observed in the drill core, and of gold geochemistry results, suggest that this area holds good potential for economic gold mineralization. As a first observation we point to isolated strongly anomalous gold values which have been found in various parts of the grid:

- a value of 643 ppb Au in BUR-05, at the end of the drill hole where intensity of shearing drops off, and where thin quartz-pyrite veins start to appear;

- a value of 480 ppb Au in BUR-11, in sheared metagabbro at the contact with weakly sheared felsic rocks;

- a value of 323 ppb Au in reverse circulation hole BOB-158, close to BUR-01, in metavolcanics with abundant quartz veining and coarse pyrite;

- A value of 260 ppb Au in seemingly fresh, unaltered mafic rocks adjacent to a pyritic zone of limited depth extent.

- 45 -

l?:,'"

i'.'..'. N"

As a second observation, we point to weakly to moderately anomalous gold values which occur over more significant lengths:

- in BUR-01, results of 15 to 45 ppb Au at 24-30 m, followed by apyritic interval from 30-38 m within which 3 of 4 samples from 32-34 m gave 0.2 g/t Au;

- also in BUR-01, apparently isolated values of 0.2 to 0.3 g/t Au in a pyritic interval from 150-165 m;

- in BUR-09, results of 55 to 95 ppb Au in lapilli tuffs adjacent to sheared feldspar-quartz crystal tuffs;

- in BUR-10, results of 15 to 95 ppb Au at 24.5-31.5 m and 50 to 64 ppb Au at 43.5-45.5 m in weakly fractured mixed (intermediate) tuffs.

As a third observation, we suggest that chlorite and calcite alteration along profile 900W, and that chloritoid-bearing altered mafic metavolcanics in BUR-06 may have a relationship with Au mineralization nearby.

When these results are combined with the clear evidence of locally intense shearing, obtained from only ten drill holes, in an area of very poor outcrop exposure, the only problem which arises is where to spot the next generation of drill holes.

Finally, one drill hole was collared in the western part of the property, and here we intersected a granodiorite porphyry which is strongly sheared at its northern boundary. The true width of the shear is not known since we collared into it; no undeformed core was recovered north of the zone. Within this shear, disseminated pyrite and minor quartz ± tourmaline veining with coarse pyrite was observed; also fracture density was high and this resulted in substantial core loss. Gold geochemistry results are very encouraging: nine samples gave greater than 100 ppb Au in two 9 m sections and one 6 m section, all between 56-95 m.

This hole represents the most encouraging result of the 1988 exploration program.

Ifr

5.1 Recontmendations For Further Work

At the present time, the proposed program for 1989 on the Burntbush River project is directed towards further evaluation of the western part of the property, in the vicinity of Spade Lake. We plan to: .

i) extend the Burntbush grid west. Depending on cost ofline-cutting and ground geophysics we may extend the grid all the way to the western boundary of the property, or, alternatively, we may chose to select a specific portion of this part of the property for follow-up work. Line spacing will be 100 m. Note that the change from 50 m to 100 m spacing should not compromise our interpretive capabilities since there appears from detailed airborne studies, to be more uniform, east-west trending magnetics in this part of the property relative to the Burntbush grid area;

ii) perform ground geophysics, including magnetics and an EH method. We will evaluate the possibility of replacing the VLF-EH method used in 1988, perhaps with a horizontal loop instrumentation which has a wider range of frequency options;

iii) perform diamond drilling with three objectives:

to test east and/or west the shear zone intersected in BUR-12, probably at intervals of 400 m;

to drill a more or less continuous profile north from BUR-12 into the vast metasedimentary terrane in the vicinity of reverse circulation hole BOB-170;

to test, also at 400 m intervals, the contact between the metasedimentary and metavolcanic terrenes if this contact is determined from the profile drilling (above) to be sheared, as is suggested by our results in the Burntbush grid area.

We also plan to resample drill core stored in the field to further evaluate targets defined from our interpretation of the 1988 program. The main areas of interest are in holes BUR-01, BUR-05 and BUR-06, but additional major element analyses from these and other holes will also be requested.

- 47 -

fer

But, we recommend also that the following work be done, either during 1989 or at a later date, depending on the availability of exploration funds. These are listed below in order of priority.

i) humus sampling should be performed at relatively close spacing (eg 25 m) along the new cut lines in the vicinity of Spade Lake, to see if the gold mineralization encountered in BUR-12 has a related expression in the surficial organics. If such an association can be confirmed, a survey should be conducted over the Burntbush grid also;

ii) the Burntbush grid should be extended east, to better place in regional context the results received from holes BUR-05 and BUR-06. Of particular interest is the area southeast of BUR-05, where bedrock conductors are interpreted to be present;

iii) additional drilling on the Burntbush grid should be performed after results of the resampling program are received. We should follow-up the anomalous bedrock geochemistry from reverse circulation hole BOB-158, and we should do more work near holes BUR-05 and BUR-06. Additional work east and/or west of BUR-09 is also warranted;

iv) finally, we propose that a careful profile by profile evaluation of the airborne electromagnetic and magnetic results be undertaken along the linear east-west trend north of Blue Lake. Based on quality of the anomalies, two widely spaced profiles might be chosen for drilling, to test the polymetallic base metal potential of the conductor.

- 48 -

'•l

6. REFERENCES

IRVINE, T.N. and BARAGAR, W.R.A. 1971, A Guide to the Chemical Classifi cation of the Common Volcanic Rocks, Can. J. Earth Sci, v.8, p.523-548

JENSEN, L. S. 1976, A New Cation Plot for Classifying Subalkalic Volcanic Rocks, Ont. Div. Mines MP 66, 22p.

JOHNS, G.W. 1982, Geology of the Burntbush-Detour Lakes Area, District of Cochrane, Ont. Geol. Surv. Rept 199, 82p.

MATHIESON, N.A. and HODGSON, C.J. 1984, Alteration, mineralization, andmetamorphism in the area of the East South "C" ore zone, 24th level of the Dickenson mine, Red Lake, northwestern Ontario, Can. J. Earth Sci., v.21, p.35-52

PATTISON, E.F., SAUERBREI, J.A., HANNILA, J.J. and CHURCH, J.F. 1986,Gold Mineralization in the Casa-Berardi Area, Quebec, Canada, in Macdonald J.A. (ed.), Proceedings of Gold '86, an International Symposium on the Geology of Gold: Toronto, 1986, p.170-183

THOMSON, R. 1936, Geology of the Burntbush River Area; Ont. Dept. Mines, Annual Rept v.45, Pt.6, p.49-63

TOURIGNY, G. and HUBERT, C. 1986, The Bousquet Property, in Hubert, C. and Robert F. (eds.), Structure and Gold, Rouyn to Val d'Or, Quebec; Geol. Assoc. Can., Mineral. Assoc. Can., Can. Geophys. Union, Joint Ann. Meeting: Ottawa, 1986, p.12-26

Various assessment files, Hoblitzell and Noseworthy townships, Office of the Resident Geologist, Kirkland Lake, Ontario:

AMERITEX COGEHA DOME NEWHONT

19841987, 198819821986, 1987

- 49 -

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

FINAL REPORT 1988

"DIAMOND DRILL RESULTS"

VOLUME 2 Of 3

APPENDIX I

DIAMOND DRILL HOLE DESCRIPTIONS

1. SUMMARY LOGS

2. FIELD LOGS

Ref. No. 88-CND-47-03 (Document: //0149U)

By: R. St-Jean J. Learn S. Ball R. Mousseau

Compiled: November, 1988

1. SUMMARY LOGS

NOTES; The Summary Logs are intended to summarize the fieldlogs in concise form and were prepared after reception of all chemistry data and after examination of thin sections.

Jensen cation plots (Jensen, 1976) are given for all samples on which major element geochemistry was performed. Sample numbers are given on the summary log to aid the reader in determining from which lithology samples were taken.

FeO and Fe203 components of the FejOs totaliron analytical results were calculated using theprocedure recommended by Irvine and Barager (1971).

SUMMARY LOG

BUR-01;

O - 7.3 OVERBURDEN

7.3-200.0 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

7.3- 28.5 amphibole ± garnet schist; flow28.5- 38.8 amphibole ± garnet volcaniclastic schist; lapilli tuff38.8- 55.6 amphibole schist; flow (5018, 5019)55.6- 89.9 amphibole ± garnet volcaniclastic schits; lapilli tuff (5020)89.9- 97.3 amphibole schist; flow97.3-102.3 amphibole volcaniclastic schist; lapilli tuff102.3-200.0 amphibole ± garnet schist; flow (5026)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 12.5-13.0: 0.2 g/t; relatively fresh, punctual sample

2) at 24-30 m: 20, 40, 15, 45 ppb; fractured, weakly pyritic zone; at 32-34 m: 3 of 4 samples give 0.2 g/t; 2-5% pyrite

3) at 150.1-150.6: 0.2 g/t; weakly pyritic healed breccia;at 156.0-157.0: 0.3, 0.2 g/t; L-3% pyrite;at 163.0-165.5: 2 of 5 samples give 0.2 g/t; weakly pyritic

I'cO i lc;Oj ' tiOj

Rock umplt colour(ippraiimiu) ) . High-Iron

\** \TholcliiieOMiliB"ek

BUR-01

JENSEN CATION PLOTS

Al,0, MgO

5018 mafic flow

t 5020 volcaniclastic

A 5026probably volcaniclastic

(clast: matrix not recordedF.O*rtJOJ*TlOJ

I*,ICO

RI 203

5019 altered contact zone

m 203

SUMMARY LOG

BUR-02;

O -46.1 OVERBURDEN

46.1-132.3 METASEDIMENTARY ROCKS

46.1- 91.8 biotite ± amphibole * garnet schist; greywacke and/orash tuff (5088, 5093J

91.8- 97.8 strongly sulfidized schist (pyrrhotite * pyrite) 97.8-132.3 biotite ± garnet schist; argillaceous greywacke (5105)

122.5-127.2: feldspar porphyry dyke

132.3-245.0 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

132.3-195.0 amphibole-garnet schist; flow or ash tuff (5108, 5109)195.0-206.5 interbedded quartzite and schist206.5-229.7 feldspar porphyry dyke229.7-245.0 amphibole ± garnet schist; flow or ash tuff

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 75.0-75.5: 0.2 g/t; quartz-calcite-pyrite-pyrrhotite veining

2) at 91.5-92.0: 0.2 g/t; lQ1o pyrrhotite, minor pyrite as breccia cement

leo i r.,o,,' no

{\ High-Iron t* \Thol4llileOJHli

'""'p&t'" vf \ x ^•^^——

Rock umplt colour liaproiimtul

BUR-02

JENSEN CATION PLOTS

M,0,

F.O.f.203'Il02

5088, 5093 greywacke and/or ash tuff

R1203

5 S Z E TIB

5105 argillaceous greywacke

5108, 5109 flow or ash tuff

B1J03

BUR-03;

SUMMARY LOG

O - 6.5 OVERBURDEN

6.5-149.0

6.5-149.0

MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

amphibole ± garnet schist; flow (5049, 5050, 5055, 5057)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 61.0-61.5: 0.2 g/t; weakly pyritic healed breccia, punctual sample

BUR-03

JENSEN CATION PLOTS

Al,0,

5049, 5050 flows

R) 203

•0*f.JOJ.7lOJ

5055, 5057 altered flows

01303

BUR-04 i

SUMMARY LOG

O - 7.3 OVERBURDEN

7.3- 74.1 INTERMEDIATE METAVOLCANIC ROCKS

7.3- 74.1 sulfide-rich schist (pyrite < pyrrhotite); flow (5062, 5068, 5067)

74.1-124.9 FELSIC HETAVOLCANIC ROCKS

74.1-124.9 stretched feldspar porphyry; porphyritic flow or sill (5074, 5075)

124.9-200.0 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

124.9-178.0 178.0-193.5

193.5-200.0

amphibole ± garnet schist; flow (5082, 5084) amphibole ± garnet volcaniclastic schist; thinly interbedded mafic and felsic tuffs or stretched lapilli tuff (5086) amphibole-garnet schist; flow

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 14.0-15.5: 40 ppb; up to 10* pyrite—pyrrhotite, quartz veinlets at 17.5-25.5: 15, 60, 10, 15, 45, 24 ppb; up to 101 pyrite-pyrrhotite,

quartz-pyrite veinlets at 26.5-31.0: 25, 15, 15 ppb: S-10% pyrite

2) at 81.0-82.5: 25 ppb; 3* pyriteat 108.5-110.0: 20 ppb; relatively fresh sample

3) at 146.5-147.0, 157.5-158.0, 194.0-194.5: 0.2 g/t; weakly fractured,relatively fresh, punctual samples

BUR-04

JENSEN CATION PLOTS

•0*NJ03*TI02

5062 (*10H py)5067, 5068 (O* py)

pyritic flows

Al,0,

F.O'F.203*Tl02

RI 209

5074, 5075 stretched feldspar porphyry

At 203

FtO*F*203*Tl02

SI 203

S ft I C i

5082, 5084 flows

5086volcaniclastic

(clast: matrix not recorded)

RI203

BUR-05;

SUMMARY LOG

O - 52.4 OVERBURDEN

52.4-206.1 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

52.4- 67.0 67.0- 69.2 69.2-206.1

amphibole schist; flow (5148)quartz-calcite-sericite schist; quartz-eye tuff (5149) amphibole ± garnet schist; flow (5150, 5151, 5152, 5153, 51547 5156, 5157)

206.1-238.0 FAULT GOUGE

238.0-278.0 INTERMEDIATE METAVOLCANIC ROCKS

238.0-278.0 biotite schist; ash tuff (5178, 5179, 5180, 5181, 5182)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 67.5-68.0: 33 ppb; thin, altered quartz-eye tuff, punctual sample

2) at 188.2-188.7: 37 ppb; relatively fresh, garnet-rich schist, punctualsample

3) at 205.0-206.0: 12, 40 ppb; hematite alteration adjacent to fault gouge

4) at 221.0-224.0: 20 ppb; fault gouge

5) at 277.5-278.0: 643 ppb; relatively fresh, punctual sample taken atend of hole

BUR-05

JENSEN CATIOM PLOTSF.OF.J03.TI02

5148, 5152, 5153, 5156, 5157 flows

01203

ftO'F.ZOS'TlOJ

RISC&

t 5149 quartz-eye tuff

5150, 5154 garnet-rich flows

A 5151 flow adjacent to quartz vein

FtO'ftJOJ.TlOJ

5179, 5181 ash tuff

BIJOJ

* 5178 sericitized ash tuff

A 5180amphibole-bearlng ash tuff

(thin el m intervals not typical of unit

RI303 it fi lea

l!'

BUR-06;

SUMMARY LOG

O - 40.0 OVERBURDEN

40.0-121.6 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

40.0- 52.8 52.8- 57.5 57.5- 62.2 62.2- 68.1 68.1- 87.4 87.4- 92.0 92.0-108.0 108.0-121.6

amphibole schist; flowbiotite-quartz eye schist; quartz eye tuff (5115)amphibole ± garnet schist; flowbiotite-quartz eye schist; quartz eye tuffamphibole ± garnet schist; flowbiotite schist; ash tuffamphibole schist; flowfeldspar porphyry; porphyritic flow (5118)

121.6-150.7 FELSIC to INTERMEDIATE METAVOLCANIC ROCKS

i-fiff: 121.6-140.1

140.1-143.4 143.4-150.7

crenulated quartz-sericite schist; deformed crystaltuff (5123, 5129)amphibole-garnet schist; flowsilicic aphanitic schist; porphyritic rhyolite (5135)

150.7-247.2 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

It;150.7-156.3 156.3-164.6 164.6-183.5 183.5-195.7 195.7-223.0 223.0-247.2

amphibole schist; flowfeldspar porphyry; porphyritic flow or dykeamphibole ± garnet schist; flow (5145)fault gougeamphibole-garnet schist; flowchloritoid ± garnet schist; altered flow (5162, 5164)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 46.0-46.5 m: 0.3 g/t; spike anomaly in fractured amphibole schist

2) at 51.0-53.0 m: 35 ppb; fractured contactat 56.0-56.5 m: 21 ppb; fractured quartz-eye tuff, weakly pyritic

3) at 115.0-116.5: 25 ppb; bleached section in feldspar porphyry at 119.5-121.0: 30 ppb; chloritized section in feldspar porphyry,

weakly pyritic

4) at 232.0-232.5: 0.2 g/t; chloritoid-gamet schist, weakly pyritic

BUR-06

JENSEN CATION PLOTSIcO

It';

5118, 5145 flows

5115 quartz-eye tuff

A 5123 feldspar porphyry

5129 Granulated schist

A 5135 porphyritic rhyolite

5162, 5164 chloritoid schist

RI303

BUR-07:

SUMMARY LOG

O - 44.9 OVERBURDEN

44.9- 91.8 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

44.9- 79.8

79.8- 86.5

86.5- 91.8

laminated amphibole ± feldspar ± garnet schist;ash and crystal tuffs (5170)graphitic schist; argillaceous sediment or tuffaceoussediment (5172)laminated amphibole ± garnet schist; ash tuff

91.8-108.6 FELSIC METAVOLCANIC ROCKS

91.8-108.6 quartz eye * garnet schist; quartz eye tuff (5174, 5175)

108.6-260.0 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

108.6-148.0

148.0-206.4

206.4-218.9

218.9-260.0

laminated biotite 4- amphibole 4- garnet schist; ash tuff(5184, 5186, 5187)"laminated amphibole 4- biotite schist; ash tuff(5191, 5194)amphibole-biotite volcaniclastic schist; lapilli tuff(5201, 5202)laminated amphibole ± biotite schist; ash tuff(5204, 5209)

tefe

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 63.0-63.5: 0.2 g/t; weakly pyritic punctual sample in fractured schist at 73.5-74.0: 0.2 g/t; weakly pyritic, relatively fresh, punctual sample

2) at 218.3-218.8: 21 ppb; chloritized lapilli tuff, punctual sample

rton*,o,

BUR-07

JENSEN CATION PLOTS

Rock urnpl* wtouf (ippionimlH)

tlxk

5170, 5184, 5186, 5187, 51915194, 5204, 5209

ash tuffsAl,0,

RIMS

5172 graphitic schist

BIJ035174, 5175

quartz eye tuffs

RI 203

5201 , 5202 lapilli tuffs

RI303

BUR-08;

SUMMARY LOG

O - 47.0 OVERBURDEN

47.0-228.3 METASEDIMENTARY ROCKS

47.0-228.3 biotite -t- garnet schist; greywacke (5210, 5211, 5212, 5213, 5214, 5215, 5216, 5217)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) maximum result is 9 ppb

t*..'

...~- W;.

RoekumplltOlOUf , f,v- (wp.onlnuul if No\ HljMrOB

/\ v \TheWHIe DmH Slick A 4 A* ^

Ouk •rMB-OHV/A

BUR-08

JENSEN CATION PLOTS

5210, 5212, 5213, 52145215, 5217greywacke

BI203

5211, 5216 dykes

fl)303

BUR-09;

SUMMARY LOG

O - 20.9 OVERBURDEN

20.9-257.0 INTERMEDIATE (DACITIC) METAVOLCANIC ROCKS

20.9-130.8

130.8-195.4 195.4-214.5 214.5-238.7 238.7-257.0

feldspar-quartz porphyritic schist; crystal tuff (5218, 5221, 5226, 5229, 5232, 5237) biotite-volcaniclastic schist; lapilli tuff (5243) feldspar-quartz porphyry; dyke or sill biotite-volcaniclastic schist; lapilli tuff (5248) feldspar-quartz porphyry; dyke or sill (5249)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 83.5-85.0 m: 20 ppb; 5% pyrite in sheared crystal tuff

2) at 101.5-102.0 m: 0.2 g/t; 1 weakly sheared crystal tuff

3) at 124.0-124.5: 21 ppb; 3% pyrite in crystal tuff

4) at 133.0-137.5: 70 ppb, trace, 95, 55 ppb; lapilli tuff adjacent tosheared crystal tuff

5) at 148.5-149.0: 0.2 g/t; 3% pyrite in lapilli tuff, punctual sampleat 157.0-157.5: 69 ppb; 21, pyrite in lapilli tuff, punctual sampleat 161.5-162.0: 0.3 g/t; 51 pyrite in lapilli tuff, punctual sample

6) at 214.5-215.0: 0.2 g/t; 2% pyrite in lapilli tuff at contact withfeldspar-quartz porphyry dyke, punctual sample

Rock Mmplt Mlwn lappnulmiul

BUR-09

JENSEN CATION PLOTS

M|0,

5218, 5221, 5226, 52295232, 5237

crystal tuffs

AI303

no:

1)1203

FtO*f.}OJ.TlOJ

5243, 5248 lapilli tuffs

5249 porphyry dyke or sill

RI303

BUR-10;

SUMMARY LOG

O -16.2 OVERBURDEN

16.2-130.4 INTERMEDIATE METAVOLCANIC ROCKS

16.2- 91.4

91.4-130.4

mixed biotite-muscovite schist; ash and crystal tuff (5250, 5251, 5252, 5253, 5254, 5255, 5256, 5257) quartz porphyry; quartz-eye tuff or sill (5260)

130.4-244.0

130.4-244.0

MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

mixed amphibole-biotite schist; ash and crystal tuff (5261, 5262, 5263, 5264, 5265, 5682, 5683)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 24.5-31.5 m: 15, 95, 25, 15, 19, 15 ppb; weakly fractured mixed tuffs

2) at 43.5-45.5 m: 64, 50 ppb; 2m thick quartz-eye tuff, minor py, po

3) at 87.2-88.2 m: 300, 75 ppb; up to 10% pyrite in 20 cm open fold hinge

Black

BUR-10

JENSEN CATION PLOTS

M,0j

5250, 5251, 5252, 5253, 52545255, 5256, 5257, 5260intermediate mixed tuffs

RI203

5261, 5262, 5263, 52645265, 5682, 5683

mafic to intermediate mixed tuffs

HI 203

SUMMARY LOG

BUR-11 i

O -19.3 OVERBURDEN

19.3-159.2 MAFIC INTRUSIVE ROCKS

19.3-159.2 feldspar-amphibole schist; sheared metagabbro(5266, 5273, 5282) 71.1-77.7 mostly White quartz vein

159.2-217.0 FELSIC INTRUSIVE ROCKS

159.2-217.0 equigranular felsic granitoid (5290, 5294, 5297)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 105.5-106.0 m: 20 ppb; sheared metagabbroat 113.0-113.5 m: 70 ppb; sheared metagabbro, brown alterationat 119.0-119.5 m: 80 ppb; sheared metagabbro, S-5% pyrite-pyrrhotiteat 129.0-129.5 m: 60 ppb; fracture zone in sheared metagabbroat 131.0-132.5 m: 30 ppb; fracture zone in sheared metagabbro

2) at 150.0-150.5 m: 25 ppb; felsic dyke in sheared metagabbro

3) at 153.5-159.5 m: 20, 5, 480, 15 ppb; sheared metagabbro at contactwith felsic granitoid

4) at 165.0-165.5 m: 26 ppb; felsic granitoid, punctual sampleat 170.0-170.5 m: 65 ppb; quartz vein in felsic granitoid, punctual sampleat 174.5-175.0 m: 20 ppb; quartz vein in felsic granitoid, punctual sampleat 180.0-180.5 m: 53 ppb; quartz vein in felsic granitoid, punctual sample

nock umpli colour lipproximllel

Black

BUR-11

JENSEN CATION PLOTS

AC,Oj

5266, 5273, 5282 sheared metagabbro

Bl 3035290, 5294

felsic granitoid

01MJ

5297 porphyry dyke

S tt It

\(

Jo\it J* t

L ——— j—— Xit iir b yla

8,0

SUMMARY LOG

BUR-12;

O - 41.0 OVERBURDEN

41.0-191.0 FELSIC INTRUSIVE ROCKS

41.0-147.4 granodiorite porphyry (5301)147.4-158.2 quartz-eye schist; quartz-eye tuff (5309)158.2-181.6 granodiorite porphyry (5311)181.6-191.0 quartz-eye schist; quartz-eye tuff

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 45.5-78.5 m: 45, 20, 30, 40, 65, 140, 550, 180, 130, 35, 160, 230, 170,20 ppb; sheared pyritic granodiorite porphyry

at 84.5-96.5 m: 150, 30, 480, 135, 15 ppb; sheared pyritic granodioriteporphyry

at 102.5-104.0 m: 45 ppb; sheared granodiorite porphyry

2) at 147.5-148.0 m: 25 ppb; pyritic quartz-eye tuff at contact withporphyry, punctual sample

3) at 173.3-173.8 m: 160 ppb; quartz vein with galena in fresh granodioriteporphyry, punctual sample

luO i li!,Oj ' MOj

Rock l*npl* colour lipproxlmitcl

Black

BUR-12

JENSEN CATION PLOTS

Al,0j

5301 fresh granodiorite porphyry

B1303

35 S 37 S Tio

5309 quartz-eye tuff

RI203

SUMMARY LOG

BUR-13;

O -27.7 OVERBURDEN

27.7-188.0 MAFIC to INTERMEDIATE METAVOLCANIC ROCKS

27.7-188.0 amphibole schist; flow(5404, 5406, 5407, 5411)

SUMMARY OF GOLD ANALYTICAL RESULTS

1) at 83.5-84.0 m: 260 ppb; relatively fresh schist, minor pyrite, punctualsample

2) at 187.5-188.0 m: 21 ppb; relatively fresh schist, minor pyrite, punctualsample at end of hole

ife

•JWMfags*^"'^"^'*^'

BUR-13

JENSEN CATION PLOTS

Al,0j

5404, 5406, 5407, 5411 flows

RI203

2. FIELD LOGS

The following notes should help the reader understand the manner in which core was logged, and also includes an explanation of information which is given in the logs in abbreviated form:

COLUMN TITLE

DESCRIPTIONEXPLANATION OF ABBREVIATIONS

BOX: core box number as received from drillers

DEPTH: depth in metres (from drill floor)

7. REG: 7o recovery; generally given in 3 m intervals, i.e. measured length of core between driller tags expressed as %. However, if drill core can be fitted across drill tag, zone of core loss can be more precisely determined, and we have made every effort to do so

LOG: graphic representation of drill log; the legend we use is still at a preliminary stage and will be presented in full at a later time

GRAIN SIZE: visual estimate of grain size; where porphyro blastic or porphyritic rock types occur, grain size of groundmass and coarser minerals given, separately

TEXTURE: macroscopic rock texture

STRUCTURES: foliations measures in degrees to core axis, folds and other features also reported here

FRACTURES AND F * fracture VEINS: V - vein

- Density: where fracture or vein density prohibitsindividual description (eg where 10 or more fractures of same orientation occur in limited depth interval), density of fractures (or veins) are given: number of fractures (or veins) per metre

- Angle: angle of fracture (F) or vein (V) to core axis as suffix to feature eg. F40 is a fracture at 40 e to core axis; in some cases where more than one identical fracture occurs in restricted interval, we prefix with the number of fractures eg 2F40, rather than report in density column

2. FIELD LOGS (cont'd)

COLUMN DESCRIPTIONTITLE EXPLANATION OF ABBREVIATIONS

- Nature: abbreviated description of fractures and veins including description of fracture eg

RO, R0: roughSH: smoothSS: striations, slickens l idesV: vuggyH, HE: healed, recemented

and also including description of minerals associated with fractures or veins, eg

cb : carbonatecc: calciteeh, chl: chloriteci: claycpy: chalcopyriteep: epidotefs, fspr: feldsparhem: hematitekaol: kaolinitelim: limonitemt: magnetitemu, muse: muscoviteox: oxides eg limonite, or generally rusty surfacespeg: pegmatoidpo: pyrrhotitepy: pyriteQ, q: quartzser: sericiteSi: very fine silica cementtm: tourmaline

other common abbreviations used:

Bl, bl: bleachingbkn: zones of broken core, probably natural but

perhaps locally due to drillers bx: brecciation; dense fracturation of no apparent

regular orientation ft: minor fault

finally, we emphasize that fractures appearing on log are interpreted to be fractures; breaks parallel to foliation are generally not recorded (unless they are interpreted to be fractures) and places where the core has been broken by drillers to fit into core box are not recorded.

GEOT: Geotechnical parameters

-F: friability - a qualitative measure of rock competence [ F - friable eg core can be broken with bare hands l VF s very friable eg core easily broken

EF o extremely friable eg clay where this column is not filled out, hammer is needed to break core

2. FIELD LOGS (cont'd)

COLUMN TITLE

DESCRIPTIONEXPLANATION OF ABBREVIATIONS

- R: rock quality designation (RQD); a measure of fracture density commonly used in rock mechanics studies Where the length of core in box in lengths of 10 cm or greater is expressed as 1, of one 3 m run in very fractured rock, RQD value is low, in non-fractured rock, RQD is 100; where this column is not filled out, RQD is

COLOUR: colour of core When wet

lower case letters are tones: l * light m s medium d s dark

capital letters are colours:B ^ blackBL s blueBN s brownG a greyGG s greyish green/greenish greyGN s greenO ~ orangeP s pinkPG * pinkish greyR s redW s white

* s two colours which alternate repeatedly- - colour transitional between two colours

MINERALS AND ALTERATIONS: a representation of occurrence of minerals of

specific interest, abbreviations as for fractures and veins

SAMPLE //: location and number of sample

TS #: location and number of thin section

DESCRIPTION: description given by logging geologist, we have also recorded Au analytical results here

Form SDG-45

kCOGEMA.DIAMOND DRILL HOLE RECORD

BURN T BUSH RIVER PROJECT

DRILL HOLE NO . : BUR- 01

Hoblitzell

CLAIM NO(S).: L789332

TOWNSHIP

DATE BEGUN

COMPLETED

LOGGED BY

CONTRACTOR : Les ForaRes Foranord

CORE SIZE ! BQ_______"______22/02/88 DRILL FLUIDS: HaO25/02/88

i. St-Jean

COLLAR CO-ORDINATES

GRID UTM X; 900W______*581250E

Y:

Z:

1340S -5481900N~288

180DEPARTURE; AZIMUTH: ' —

INCLINATION: -——————

CHECKED BY: J. Learn

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DEPTH

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DEVIATION RECORD

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CHECKED BY: J. Learn, R. St-Jean, S. Ball

DEPTHS: OVERBURDEN: 7.3m

END OF HOLE: 200m

HORIZONTAL COMPONENT:

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REMARKS; ground to drill floor 0.7m, casing pulled

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Form SDG-45

COGEMA. LteT/Ltd.

DIAMOND DRILL HOLE RECORD

BURNTBUSH RIVER PROJECT

DRILL HOLE NO.: BUR- 03

Hoblitzell

CLAIM NO(S).: 1789332

TOWNSHIP

DATE BEGUN

COMPLETED

LOGGED BY

CONTRACTOR : Les Forages Foranord

CORE SIZE 5 BQ_______________25/02/88 DRILL FLUIDS: H 2026/02/88

COLLAR CO-ORDINATES

GRID

X; 900W_____

Y:

Z:

UTM

*581250E

H75S *5482050N*287

DEPARTURE: AZIMUTH: ISO

INCLINATION: -45.5

DEPTHS :

CHECKED BY: J. Learn

6 ' 5m

DEPTH

60m

120m

DEVIATION RECORD

AZIMUTH DIP METHOD

,

450

430HF 47.

HF 47,

CHECKED BY: J, Learn, R.St-Jean, S. Ball

OVERBURDEN:

END OF HOLE:

HORIZONTAL COMPONENT: 107m

VERTICAL COMPONENT 104m

REMARKS: drill floor to ground level 0.5m, casing pulled

LOCATION SKETCH 1:5000:

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Form SDO-45

DIAMOND DRILL HOLE RECORD

BURNTBUSH RIVER PROJECT

DRILL HOLE NO.; BUR-04

CLAIM NO(S).: L789335

TOWNSHIP : Hoblitzell

DATE BEGUN : 26/02/88

COMPLETED ; 29/02/88

CONTRACTOR : Les Forages Foranord

CORE SIZE : BQ---—-—-.-———-...

DRILL FLUIDS:

LOGGED BY : R. St-Jean

COLLAR CO-ORDINATES

GRID UTM X. 900W______*581250E

Y:

Z:

775S '*5482450N*282

DEPARTURE: AZIMUTH:178'

INCLINATION: -A5.5

CHECKED BY: J. Learn

DEPTH

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120m

180m

DEVIATION RECORD

AZIMUTH DIP METHOD450

440

430

HF 47,

HF 47.

HF 47.

DHECKED BY; J. Learn, R. St-Jean, S. Ball

DEPTHS; 7.3mOVERBURDEN:END OF HOLE! 200.0m

HORIZONTAL COMPONENT: 143m

VERTICAL COMPONENT : 140m

REMARKS: drill floor to ground level 0.4m, casing pulled

LOCATION SKETCH 1:5000;'

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DIAMOND DRILL HOLE RECORD

BURNTBUSH RIVER PROJECT

DRILL HOLE NO.; BUR-09

Hoblitzell

CLAIM NO(S).: L789318

TOWNSHIP

DATE BEGUN

COMPLETED

LOGGED BY

15/03/88

CONTRACTOR : Les Forages Foranord

CORE SIZE ! BQ--—---———1————

DRILL FLUIDS:

18/03/88

R. St-Jean

COLLAR CO-ORDINATES

GRID UTM X: 2000W______gSSOlSOE

325S *5482900N

Z: *288

DEPARTURE; AZIMUTH:

INCLINATION:.

CHECKED BY:

18 Ow-45.

DEPTHS; OVERBURDEN:

R. St-Jean

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DEPTH60m

120m

180m

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DEVIATION RECORD

AZIMUTH DIP METHOD430

420

390

370

HF 45J

HF 4%

HF 47.

HF 455

3HECKED BY: J. Learn, R. St-Jean, S. Ball

END OF HOLE: 257.00mHORIZONTAL COMPONENT:

VERTICAL COMPONENT :

194m

169m

REMARKS; drill floor to ground level 0.3m, casing pulled

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COGEMA LtleVtd.

DIAMOND DRILL HOLE RECORD

BURNTBUSH RIVER PROJECT

DRILL HOLE NO.: BUR-10

CLAIM NO(S).

TOWNSHIP

DATE BEGUN

COMPLETED

LOGGED BY

L789326 l L789329

Hoblitzell—--——

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J. Learn

CONTRACTOR : Les Forages Foranord

CORE SIZE : BQ_________,______

DRILL FLUIDS:

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390

370

HF 4%

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CHECKED BY: J. Learn, R. S t- Jean, S. Ball

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DRILL HOLE NO.; BUR-11

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CLAIM NO(S).: L789304

TOWNSHIP

DATE BEGUN

COMPLETED

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CONTRACTOR : Les Forages Foranord

CORE SIZE J BO-————————————18/03/88 DRILL FLUIDS; HgO

22/03/88

R. St-Jean

COLLAR CO-ORDINATES

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DEPARTURE; AZIMUTH: 180

INCLINATION: -45.5

CHECKED BY: J- Learn

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DEVIATION RECORD

AZIMUTH DIP METHOD410

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HP 47,

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HF 47.

CHECKED BY: J. Learn, R. St-Jean, S. Ball

DEPTHS: 19.3mOVERBURDEN:END OF HOLE: 217.0m

HORIZONTAL COMPONENT:

VERTICAL COMPONENT :

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143m

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DIAMOND DRILL HOLE RECORD

BURNTBUSH RIVER PROJECT

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CLAIM NO(S).: L789316 l L789317

TOWNSHIP : Hoblitzell_____

DATE BEGUN : 22/03/88—————

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COGEHA CANADA LIMITED

BURNTBUSH RIVER PROJECT

FINAL REPORT 1988 "DIAMOND DRILL RESULTS"

VOLUME 3 of 3

1.

2.

APPENDIX II

SAMPLE RESULTS

CHEMISTRY RESULTS

THIN SECTION DESCRIPTIONS

Ref. No. 88-CND-47-03 (Document: #0149U)

^\By: R. St-Jean

J. Learn Compiled: November, 1988

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1. CHEMISTRY RESULTS

REMARKS

i) there are four sets of tables

. "gold only" results

. Cu, Zn from BUR-02

. major elements

. minor elements

ii) for "gold only" results:

. MYV refers to samples sent to Mine Yvan Vezina TEC refers to samples sent to Chimitec

iii) sample numbers prefixed with the letter "C" or referred to as "CTL" are quartzite control samples and are presented in the tables in the sequence that they were inserted and analyzed

iv) negative results indicate results below the detection limit, i.e. "-" really means "-C"

ll

i i i i i i

PROCEDURES and DETECTION LIMITS

A) Mine Yvan Vezina:

FractionExtractionMethod

-150 mesh (two stage crushing, grinding) 3 parts HC1: l part HN03 - aqua regia atomic absorption

Detection limit for Au : 0.2 g/t for Cu, Zn : 0.0011

B) Chimitec;

Au ("gold only"):

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i

Fraction Extraction Method Detection

limit

-150 mesh (two stage crushing, grinding) 3 parts HC1: l part HN03 - aqua regia fire assay - atomic absorption

5 ppb

Note: normal Chimitec procedure is to crush entire sample, then pulverize 250 g, then analyze 10 g; for these samples, 500 g were pulverized and 30 g were analyzed (to increase precision of analyses)

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MAJOR ELEMENTS

CaO, Na20:

fraction

extractionmethod detection limit

K20, P205 :

fraction extractionmethoddetection limit

LOI:

fractionmethod detection limit

C02 :

fraction extractionmethoddetection limit

(total iron), MnO, MgO,

: -150 mesh (two stage crushing, grinding)

: metaborate fusion: emission - plasma : 0.01*

: -150 mesh : metaborate fusion: emission - plasma: 0.03*

: -150 mesh: gravimetry : 0.01*

: -150 mesh : H3P04: gravimetry: D.05%

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MINOR ELEMENTS

fraction method

detection limits :

AuSmSbSe, Th, U, LuAs, Os, Ta, Tb, BrEu, Hf, Mo, WLa, Ag, YbCd, Co, Rb, Se, CeTeGr, NiBa, IrZn, SnZrFe, Na

-150 meshneutron activation

2 ppb 0.05 ppm 0.1 ppm 0.2 ppm 0.5 ppm1 ppm2 ppm 5 ppm 10 ppm 20 ppm 50 ppm 100 ppm 200 ppm 0.02*

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Page

Line

t3456789

1011121314151617181920212223242526272829303132333435363738394041424344454647484950515253545556

1 of BURNTBUSH

Hole no

BUR- 01 BUR- 01BUR- 01BUR- 01BUR-01BUR-01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR-01BUR-01BUR- 01BUR- 01BUR- 01BUR-01BUR- 01BUR- 01BUR- 01BUR- 01BUR-01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR-01BUR-01BUR- 01BUR-01BUR- 01BUR- 01BUR-01BUR- 01BUR-01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR-01BUR- 01BUR- 01BUR-01

Sample

C5000 50015444544554465447500250035004500550065007500850095010501150125013501450155016501750215022502350245025C50255027544854495450C545050285451545254535454502950305031503250335034503550365037503850395040504150425043504450455046

DIAMOND

From

12.50 12.5124.0025.5027.0028.5030.0030.5031.0031.5032.0032.5033.0033.5034.0034.5035.0035.5036.0036.5037.0037.5075.5076.0093.00

103.50113.60126.90138.50146.00147.50149.00149.00150.10150.60151.50153.00154.50156.00156.50157.00157.50158.00158.50159.00159.50160.00160.50161.00161.50162.00162.50163.00163.50164.00164.50

DRILLING ^GOLD RESULTS^ [88/09/15]

To

12.50 13.0025.5027.0028.5030.0030.5031.0031.5032.0032.5033.0033.5034.0034.5035.0035.5036.0036.5037.0037.5038.0076.0076.5093.50

104.00114.10126.90139.00147.50149.00150.10149.00150.60151.50153.00154.50156.00156.50157.00157.50158.00158.50159.00159.50160.00160.50161.00161.50162.00162.50163.00163.50164.00164.50165.00

Au ppb

0 0

20401545

00000000000000000000000

-510-5-5

0-5-5-5-5

000000000000000000

Au g/t

-0.20 0.200.000.000.000.00

-0.20-0.20-0.20-0.200.200.20

-0.200.20

-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.200.000.000.000.000.200.000.000.000.000.300.20

-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.200.20

-0.20-0.20-0.20

Lab.

MYV MYVTECTECTECTECMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVTECTECTECTECMYVTECTECTECTECMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYV

ai1! : "

1-' B

1

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1r- B

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I'*'

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: 1I'B4'"'

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Iii.

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Page

Line

II5960616263646566676869707172737475767778798081828384858687888990919293949596979899

100101102103104105106107108109110111112

2 of

Hole ne

BUR- 01 BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR- 01BUR-01BUR-01BUR- 01BUR- 01BUR- 02BUR- 02BUR-02BUR- 02BUR-02BUR-02BUR- 02BUR-02BUR-02BUR-02BUR-02BUR-02BUR-02BUR-02BUR-02BUR-02BUR- 02BUR- 03BUR-03BUR- 03BUR- 03BUR-03BUR-03BUR-03BUR-03BUR-04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR-04

BURNTBUSH

? Sample

5047 545554565457545854595460546154625463546454655466546754685048546950895090509150925094509550965097509850995100C510051015102510351065107C5050505150525053505450565058505953515352535350605355535653575358506153595360536153625363

DIAMOND

From

165.00 165.50167.00168.50178.00179.50181.00182.50184.00188.50190.00191.50193.00194.50196.00197.50198.0074.0074.5075.0075.5091.5092.0092.5094.5095.0095.5096.0096.0096.5097.0097.50

129.00129.5032.0042.5052.4061.0076.0092.60

133.00145.50

7.308.009.50

11.0011.5012.5014.0015.5017.0017.5019.0020.5022.0023.50

DRILL]

To

165.50 167.00168.50170.00179.50181.00182.50184.00185.50190.00191.50193.00194.50196.00197.50198.00200.0074.5075.0075.5076.0092.0092.5093.0095.0095.5096.0096.5096.0097.0097.5098.00

129.50130.0032.0043.0052.9061.5076.5093.10

133.50146.00

8.009.50

11.0011.5012.5014.0015.5017.0017.5019.0020.5022.0023.5025.00

[88/09/15]

Au ppb Au g/t Lab,

010-5-5-5-5-55

-5-5-5-5-5-5-50

-50000000000000000000000000

-5-5-505

1040100

1560101545

0.200.000.000.000.000.000.000.000.000.000.000.000.000.000.00

-0.200.00

-0.20-0.200.20

-0.200.20

-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.200.20

-0.20-0.20-0.20-0.200.000,000.00

-0.200.000.000.000.00

-0.200.000.000.000.000.00

MYVTECTECTECTECTECTECTECTECTECTECTECTECTECTECMYVTECMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVTECTECTECMYVTECTECTECTECMYVTECTECTECTECTEC

1If

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If: g.

' -1y' H'

1V M

if., gm

1-,,: fjSt-

1=1

I' —1ri, 'P

l.filv, a .ri

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1.1

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sS-'

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1f -S *: m

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Page

Line

m115116117118119120121122123124125126127128129130131132133134135136137138139140141142143144145146147148149150151152153154155156157158159160161162163164165166167168

3 of BURNTBUSH

Hole no

BUR-04 BUR-04BUR-04BUR- 04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR-04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR-04BUR- 04BUR- 04BUR- 04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR- 04BUR-04

Sample

5364 50635365536653675064536853695370506553715372537353745375C5375506653765377537853795380538153825383506953845385538653875070538853895390539150715392539353945395539650725397539853995400C5400541250735413541454155416541754185419

DIAMOND

From

25.50 26.0026.5028.0029.5031.0031.5033.0035.0036.5037.0038.0039.5041.0042.5042.5043.5044.0045.5047.5048.5050.0051.5053.0054.5056.4056.9058.0059.5061.0061.0063.0064.5066.0067.5068.5069.0070.5072.0073.5075.0076.0076.5078.0079.5081.0081.0082.5084.0084.5085.5087.0088.5090.0091.5093.00

DRILLING ^GOLD RESULTS^

To

26.00 26.5028.0029.5031.0031.5033.0035.0036.5037.0038.0039.5041.0042.5043.5042.5044.0045.5047.0048.5050.0051.5052.5054.5056.4056.9058.0059.5061.0063.0061.5064.5066.0067.5068.5069.0070.5072.0073.5075.0076.0076.5078.0079.5081.0082.5081.0083.5084.5085.5087.0088.5090.0091.5093.0094.50

Au ppb

5 0

25151505

15-50

-555

-5-5-505

-5-5-5-5-5-5-50

-5-5-5-50

-5-5-5-50

-5-5-5-5-50

-5-5-525-5-50

-5-5-5-55

-5-5

Au g/t

0.00 -0.200.000.000.00

-0.200.000.000.00

-0.200.000.000.000.000.000.00

-0.200.000.000.000.000.000.000.000.00

-0.200.000.000.000.00

-0.200.000.000.000.00

-0.200.000.000.000.000.00

-0.200.000.000.000.000.000.00

-0.200.000.000.000.000.000.000.00

Lab

TEC MYVTECTECTECMYVTECTECTECMYVTECTECTECTECTECTECMYVTECTECTECTECTECTECTECTECMYVTECTECTECTECMYVTECTECTECTECMYVTECTECTECTECTECMYVTECTECTECTECTECTECMYVTECTECTECTECTECTECTEC

[88/09/153

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m171172173174175176177178179180181182183184185186187188189190191192193194195196197198199200201202203204205206207208209210211212213214215216217218219220221222223224

4 of BURNTBUSH

Hole no

BUR-04 BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR- 04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR- 04BUR-04BUR-04BUR- 04BUR- 04BUR-04BUR- 04BUR- 04BUR-04BUR- 04BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR- 05BUR-05BUR-05BUR- 05BUR-05BUR- 05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05

Sample

5420 54215422542354245425C542554265427542854295430543154325433C50755076543454355436543754385077543950785440544154425443507950805081508350855087547054715472547354745475C54755476547754785155C5155548254835484548554865487548854895490

DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15

From

94.50 96.0097.5099.00100.50102.00102.00103.50105.00107.00108.50110.00111.50113.00114.50115.99116.00116.50118.00119.50121.00122.50123.90124.40125.00125.50127.00128.50130.00131.00146.50157.50174.00179.00194.00126.50128.00129.50153.50155.00156.50156.50177.50179.00180.50191.50191.50200.00201.50203.00205.50206.00209.00212.00215.00218.00

To

96.00 97.5099.00100.50102.00103.50102.00105.00107.00108.50110.00111.50113.00114.50116.00115.99116.50118.00119.50121.00122.50123.90124.40125.00125.50127.00128.50130.00131.00131.50147.00158.00174.50179.50194.50128.00129.50131.00155.00156.50158.00156.50179.00180.50182.00192.00191.50201.50203.00205.00206.00209.00212.00215.00218.00221.00

Au ppb-5 -5™"Q

-5™" JJ

-5-5-5-5-520-5-5-5-500

-5-5— J)

550

100

-5-5-5-5000000

-5-5-5-5-5-5-55

-5-500

~* Z?

5-5405

-510-5-5

Au g/t

0.00 0.000.000.000.000.000.000.000.000.000.000.000.000.000.00

-0.20-0.200.000.000.000.000.00

-0.200.00

-0.200.000.000.000.00

-0.200.200.20

-0.20-0.200.200.000.000.000.000.000.000.000.000.000.00

-0.20-0.200.000.000.000.000.000.000.000.000.00

Lab.

TEC TECTECTECTECTECTECTECTECTECTECTECTECTECTECMYVMYVTECTECTECTECTECMYVTECMYVTECTECTECTECMYVMYVMYVMYVMYVMYVTECTECTECTECTECTECTECTECTECTECMYVMYVTECTECTECTECTECTECTECTECTEC

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3Ain227228229230231232233234235236237238239240241242243244245246247248249250251252253254255256257258259260261262263264265266267268269270271272273274275276277278279280

5 of BURNTBUSH

Hole no

BUR-05BUR-05BUR-05BUR-05BUR- 05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR-05BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR- 06BUR-06BUR- 06BUR- 06BUR- 06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06

Sample

5491549254935494549554965497549854995500C550055015502550355045505550651105507511155085112550955105113511455115512551355145515551655175518551951165117511951205121512255205521552255235524512451255525C5525512655265527552851275529

DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15

From

221.00224.00227.00230.00233.00234.50236.00237.50239.00240.50240.50242.00243.5040.0041.0042.5044.0046.0046.5047.5048.0050.5051.0053.0055.0055.5056.5058.0059.5061.0062.5064.0065.5067.0068.5080.0080.5095.00101.00101.50103.00113.50115.00116.50118.00119.50121.00121.50122.00122.00122.50123.00125.00126.50128.00128.50

To

224.00227.00230.00233.00234.50236.00237.50239.00240.50242.00240.50243.50245.0041.0042.5044.0046.0046.5047.5048.0050.5051.0053.0055.0055.5056.0058.0059.5061.0062.5064.0065.5067.0068.5070.0080.5081.0095.50101.50102.00103.50115.00116.50118.00119.50121.00121.50122.00122.50122.00123.00125.00126.50128.00128.50130.00

Au ppb

20-55

-5-5-5-5-5-55

-515-5-5-5-5-505050

351000

-5-5-5-5•"Q

-5-5-5-5000000

-525-5-53000

-5-50

-5-5-50

-5

Au g/t

0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.300.00

-0.200.00

-0.200.000.00

-0.20-0.200.000.000.000.000.000.000.000.000.00

-0.20-0.20-0.20-0.20-0.20-0.200.000.000.000.000.00

-0.20-0.200.000.00

-0.200.000.000.00

-0.200.00

Lab.

TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECMYVTECMYVTECMYVTECTECMYVMYVTECTECTECTECTECTECTECTECTECMYVMYVMYVMYVMYVMYVTECTECTECTECTECMYVMYVTECTECMYVTECTECTECMYVTEC

11I

i-'

,.

1"

'•-j.'-

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If 1

I'

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1'

11: mm

•i 1

r

1r B1

1

1"

.,, .

1,, ; , .

1,

as-

1

Page

Line

1283284285286287288289290291292293294295296297298299300301302303304305306307308309310311312313314315316317318319320321322323324325326327328329330331332333334335336

6 of BURNTBUSH

Hole no

BUR-06 BUR-06BUR- 06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR- 06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-06BUR- 06BUR-06BUR-06BUR-06BUR-06BUR-06BUR-07BUR- 07

Sample

5530 512855315532553351305534553551315536553751325538513355395134513655405137554151385542513955435140554451415545514255465143514455475548514655495550C5550555155525553555451475555555655575558515851595160516151635165516651675168

DIAMOND DRILLING J^GOLD RESULTS^ [88/09/15

From

130.00 131.00131.50132.50134.50136.50137.00138.50140.00140.50142.00143.50144.00145.00145.50146.00147.00147.50148.00148.50149.00149.50150.00150.50151.00151.50152.00152.50153.00153.50161.00163.50181.00182.50184.00184.50185.00185.00188.00191.00194.00195.50197.00197.50198.50200.00201.50203.00207.50209.00222.50232.00237.50244.0047.5057.50

To

131.00 131.50132.50134.00136.50137.00138.50140.00140.50142.00143.50144.00145.00145.50146.00146.50147.50148.00148.50149.00149.50150.00150.50151.00151.50152.00152.50153.00153.50155.00161.50164.00182.50184.00184.50185.00188.00185.00191.00194.00195.50197.00197.50198.50200.00201.50203.00203.50208.00209.50223.00232.50238.00244.5048.0058.00

Au ppb

-5 0

-51550

-5-50

-5-50

-50

-500

-50

-50

-50

-50

-50

-50

-500

-5-50

-5-5-5-5-5-5100

-5-5-5-5000000000

Au g/t

0.00 -0.200.000.000.00

-0.200.000.00

-0.200.000.00

-0.200.00

-0.200.00

-0.20-0.200.00

-0.200.00

-0.200.00

-0.200.00

-0.200.00

-0.200.00

-0.200.00

-0.20-0.200.000.00

-0.200.000.000.000.000.000.000.00

-0.200.000.000.000.00

-0.20-0.20-0.20-0.200.20

-0.20-0.20-0.20-0.20

Lab.

TEC MYVTECTECTECMYVTECTECMYVTECTECMYVTECMYVTECMYVMYVTECMYVTECMYVTECMYVTECMYVTECMYVTECMYVTECMYVMYVTECTECMYVTECTECTECTECTECTECTECMYVTECTECTECTECMYVMYVMYVMYVMYVMYVMYVMYVMYV

fi1

ne 'Hl

f*"V

1si"; - -

1- m

1li'M1 1li B

1-1.1liI.,-*f - 1 #..-.fjm11' "i-liJ-*-':; M

t1- ' ^

fifir- .

Ht:ri 1 - 'k-, -m•- mli^, ' ..

t —

IIV

m;: 1

Page

Line

t^^B339340341342343344 345346347 348349350351 352353354 355356357358359360361 362363364 365366367368369370371 372373374375376377378 379380381 382383384385386387388 389390391392

7 of

Hole n(

BUR- 07 BUR-07BUR-07BUR-07BUR-07BUR- 07BUR-07BUR-07 BUR-07BUR-07BUR-07 BUR- 07BUR-07BUR-07BUR- 07 BUR-07BUR-07BUR-07 BUR-07BUR-07BUR- 07BUR- 07BUR- 07BUR-07BUR- 07 BUR- 07BUR-07BUR-07 BUR-07BUR-07BUR-07BUR- 07BUR- 07BUR- 07BUR-07 BUR-07BUR- 07BUR- 09BUR- 09BUR-09BUR-09BUR-09 BUR-09BUR-09BUR-09 BUR-09BUR-09BUR-09BUR-09BUR- 09BUR- 09BUR-09 BUR-09BUR-09BUR-09BUR-09

7 of BURNTBUSH DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15]

Sample

5169517155595560556155625563 5173 C51755176517751835185518851895564556555665567556855695570519051925193519551965197519851995200C5200520352055206520752085219557155725573557452205575 C557555765577522255785579558052235581558255835224

From

63.0073.5078.0079.5081.0083.0086.0087.0098.0098.50101.00109.00119.00125.50141.50142.00143.00144.50146.00147.50149.00150.50152.00169.50172.00182.00184.00188.00191.00196.50200.50200.50219.00227.00231.50244.00247.0031.0031.5032.5034.0035.5037.0037.5037.5039.0040.5041.0041.5042.5044.0045.0045.5051.0052.5054.00

To

63.5074.0079.5080.5083.0086.0087.0087.5098.0099.00101.50109.50119.50126.00142.00143.00144.50146.00147,50149.00150.50152.00152.50170.00172.50182.50184.50188.50191.50197.00201.00200.50219.50227.50232.00244.50247.5031.5032.5034.0035.5037.0037.5039.0037.5040.0041.0041.5042.5044.0045.0045.5047.0052.5054.0054.50

Au ppb Au g/t Lab.

00

-5-5-5-5-500000000

-5-5-5-5-5-5-50000000000000000

-5-5-5-50

-5-55

-50

-5-5-50

-5-5-50

0.200.200.000.000.000.000.00

-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.200.000.000,000.000.000.000.00

-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.20-0.200.000.000.000.00

-0.200.000.000.000.00

-0.200.000.000.00

-0.200.000.000.00

-0.20

MYVMYVTECTECTECTECTECMYVMYVMYVMYVMYVMYVMYVMYVTECTECTECTECTECTECTECMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVMYVTECTECTECTECMYVTECTECTECTECMYVTECTECTECMYVTECTECTECMYV

l

Page 8 of BURNTBUSH DIAMOND DRILLING ^GOLD RESULTS^lilif~

IIIf

lifi' ™ftv .

1i. m

1i.s*.1fi

.11' w .

liBi11* B•i* BB*f!

IBit B1

t*'

..,.1

I™"

|aft—

fif1:.

: H

fi

li

Line

m395396397398399400401402403404405406407408

- 409410411412413414415416417418419420421422423424425426427428429430431432433434435436437438439440441442443444445446447448

Hole no

BUR-09 BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR- 09BUR- 09BUR-09BUR-09BUR-09BUR- 09BUR- 09BUR-09BUR- 09BUR-09BUR- 09BUR- 09BUR-09BUR-09BUR-09BUR- 09BUR- 09BUR-09BUR-09BUR-09BUR- 09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR-09BUR- 09BUR- 09BUR-09BUR-09BUR- 09BUR-09BUR- 09BUR-09BUR-09BUR-09BUR-09

Sample

5584 558555865225C5225558755885589559052275591522855925593559455955230559655975231559855995600C560056015233560252345603560456055606560756085609561052355611561256135614561552365616561756185238561956205239562156225240562356245625

•*" -*, ** *f -^ *1 *NT

From

54.50 56.0057.5058.5058.5059.0060.5062.0064.0066.0072.5074.0074.5075.5077.0078.5080.0080.5082.0083.0083.5085.0086.5086.5088.0091.50

100.00101.50102.00103.50105.00106.50108.00109.50111.00112.50113.50114.00115.50117.00118.50120.00121.50122.00124.50126.00128.00128.50130.00131.00131.50133.00134.00134.50136.00137.50

*^ ** Wb 4kX *^ *

To56.00 57.5058.5059.0058.5060.5061.5064.0066.0066.5074.0074.5075.5076.5078.5080.0080.5082.0083.0083.5085.0086.5088.0086.5089.0092.00

101.50102.00103.50105.00106.50108.00109.50111.00112.50113.50114.00115.50117.00118.50120.00121.50122.00124,00126.00128.00128.50130.00131.00131.50133.00134.00134.50136.00137.50139.00

[88/09/15

Au ppb Au g/t Lab,-5-5-5005

105

-5050

-5-5-5-50

-5-50

20-5-5-5-50

-50

-5-5-5-5-5-5-5100

1015105

150

10550

-550

10700

9555-5

0.000.000.00

-0.20-0.200.000.000.000.00

-0.200.00

-0.200.000.000.000.00

-0.200.000.00

-0.200.000.000.000.000.00

-0.200.000.200.000.000.000.000.000.000.000.00

-0.200.000.000.000.000.00

-0.200.000.000.00

-0.200.000.00

-0.200.000.00

-0.200.000.000.00

TECTECTECMYVMYVTECTECTECTECMYVTECMYVTECTECTECTECMYVTECTECMYVTECTECTECTECTECMYVTECMYVTECTECTECTECTECTECTECTECMYVTECTECTECTECTECMYVTECTECTECMYVTECTECMYVTECTECMYVTECTECTEC

Jl1

*

1? B

1"

[riis'

fi.f1 '!. -

.J-

If

tk; lt*

1"

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P M1fi

iiiji'L

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r-l. .

1I; -lr -jjqjjjj , B^l]*Ju""^BJ1' 1"V

i.lii.

Page

Line

^^4W451452453454455456457458459460461462463464465466467468469470471472473474475476477478479480481482483464485486487488489490491492493494495496497498499500501502503504

9 of BURNTBUSH

Hole no

BUR-09BUR-09BUR-09BUR- 09BUR-09BUR- 09BUR-09BUR- 09BUR-09BUR-09BUR-09BUR- 09BUR-09BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR-10BUR- 10BUR- 10BUR-10BUR- 10BUR- 10BUR- 10BUR- 10BUR-10BUR- 10BUR-10BUR- 10BUR- 10BUR-10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR-10BUR- 10BUR- 10

Sample

C562552415242524456265627562852455629563056315246524756325633C525056345635563656375638563956405641564256435644564556465647564856495650C56505651565256535654565556565657565856595660566152585259566256635664566556665667566856695670

DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15J

From

137.50149.50152.50161.50162.00163.50165.00182.00188.00189.50191.00214.00214.50

16.2018.0019.5020.0021.5023.0024.5027.0028.0030.0031.5033.0034.5036.0037.5039.0040.5042.0044.0045.5045.5047.0049.0050.5052.0053.5055.0056.5058.0059.5061.0062.5087.2087.7097.5099.00

100.50131.50133.00134.50136.00137.50139.00

To

137.50150.00153.00162.00163.50165.00166.50182.50189.50191.00192.50214.50215.00

18.0019.5019.5021.5023.0024.5026.5028.0029.5031.5033.0034.5036.0037.5039.0040.5042.0043.5045.5047.0045.5048.5050.5052.0053.5055.0056.5058.0059.5061.0062.5064.0087.7088.2099.00

100.50102.00133.00134.50136.00137.50139.00140.50

Au ppb-5

0005

-5-5

0-5-5

500

-5-5

0-5-51015251515-5

55

** D-5-5-5

550

5"~ 0-5-5-5-5-5-5-5-5-5-5-5

30075-5-5-5-5-5-5

' -5-5

5

Au g/t

0.000.20

-0.200.300.000.000.00

-0.200.000.000.00

-0.200.200.000.000.800.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000,000.000.000.000.000.000.000.000.000.000.000.000.000.000.00

Lab.TECMYVMYVMYVTECTECTECMYVTECTECTECMYVMYVTECTECMYVTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC

1•F L

1r "

1,

tf*-|1f : '

1'

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far

fi;'.."

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1iI li1it'.'n

Page

Line

507508509510511512513514515516517518519520521522523524525526527528529530531532533534535536537538539540541542543544545546547548549550551552553554555556557558559560

10 of BURNTBUSH

Hole no

BUR- 10BUR-10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR-10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 10BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11

Sample

56715672567356745675C56755676567756785679568056815684568556865687568856895690569156925693569452675695569652685697569856995700C5700570157025703570457055706570757085709571057115269527057125713527157145715527257165717571857195720

DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15]

From

140.50142.00143.50145.00168.00168.00169.50171.50173.00174.50195.00196.50228.50242.5019.3021.0022.5024.7026.0027.5029.0030.5032.0034.0034.5036.5038.0038.5040.0041.5043.0043.0044.5046.0047.5049.0050.5052.0053.5055.0056.5058.0059.5060.5061.0061.5063.0064.5065.0066.0067.5068.0069.0070.5072.0073.50

To

142.00143.50145.00146.00169.50168.00171.00173.00174.50176.00196.50198.00230.00244.0021.0022.5024.2026.0027.5029.0030.5032.0034.0034.5036.5038.0038.5040.0041.5043.0044.5043.0046.0047.5049.0050.5052.0053.5055.0056.5058.0059.5060.5061.0061.5063.0064.5065.0066.0067.5068.0068.5070.5072.0073.5075.00

Au ppb

-5-5-5-5-5-5-5-5-5-5-5-510-5-5-5-5-5-5-5-5-5-55

-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-515-510-510-5-5-5-5-5-5-5-5

Au g/t

0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.00

Lab.

TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC

1m1"•••m

1'

is

1

1i 1

1

1,

,1""1r ti

1

1

1

i,l"""mt

t-

,i

1i'-:-

II

Page

Line

50562563564565566567568569570571572573574575576577578579580581582583584585586587588589590591592593594595596597598599600601602603604605606607608609610611612613614615616

11 of

Hole ne

BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11

BURNTBUSH

) Sample

57215722572357245725C5725572657275274572857295730573157325275C52755733527657345735573652775737573852785739574052795741574257435744574552805746574752815748574952835750C575057515752575357545755528457565285575757585759528657605761

DIAMOND

From

75.0076.5078.0079.5081.0081.0082.5084.0085.5086.0087.5089.0090.5092.0093.0093.0093.5094.0094.5096.0097.5098.5099.00100.50102.00102.50104.00105.50106.00107.50109.00110.50112.00113.00113.50115.00116.00116.50117.50119.00119.50119.50121.00122.50124.00125.50127.00127.90128.50129.00129.50131.00132.50134.00134.50136.00

DRILL:To

76.5078.0079.5081.0082.5081.0084.0085.5086.0087.5089.0090.5092.0093.0093.5093.0094.0094.5096.0097.5098.5099.00100.50102.00102.50104.00105.50106.00107.50109.00110.50112.00113.00113.50115.00116.00116.50117.00119.00119.50121.00119.50122.50124.00125.50127.00128.00128.40129.00129.50131.00132.50134.00134.50136.00137.50

[88/09/15 j

Au ppb Au g/t Lab.-5-555

10-5-51510-5-5™" V

-5-5-520-5-5-5-5-5-5-5"* J)

-5-5-520-5-5-5-5-570-5-55

-5-580-5-5-5-5-5-5-515-560-530— y

-5-5-5

0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.00

TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC

11•i

•s-

1i.

V

1|

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11

::

,4;- .

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Page

LineA618619620621622623624625626627628629630631632633634635636637638639640641642643644 645646647648649650651652653654655656657658659660661662663664665666667668669670671672

12 of BURNTBUSH

Hole no

BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR-11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR- 11BUR-12BUR- 12 BUR- 12BUR- 12BUR-12BUR- 12BUR-12BUR- 12BUR- 12BUR- 12BUR-12BUR- 12BUR-12BUR- 12BUR- 12BUR- 12BUR-12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR-12BUR-12BUR- 12

Sample

57625287576357645765576652885767576857695289577057715772577357745775C57755776529152925293529552965298529953155316 531753185319532053215322532353245325C5325532653275328532953305331533253335334533553365337533853395340534153425343

DIAMOND DRILLING ^GOLD RESULTS^

From

137.50139.00139.50141.00142.50144.00145.50146.00147.50149.00150.00150.50152.00153.50155.00156.50158.00158.00159.50170.00174.50177.00187.50197.50205.50214.5041.0042.50 44.0045.5047.0048.5050.0053.0056.0059.0062.0062.0063.5065.0068.0071.0074.0077.0078.5080.0081.5083.0084.5086.0089.0092.0095.0096.5098.0099.50

To

139.00139.50141.00142.50144.00145.00146.00147.50149.00150.00150.50152.00153.50155.00156.50158.00159.50158.00161.00170.50175.00177.50188.00198.00206.00215.0042.5044.00 45.5047.0048.5050.0053.0056.0059.0062.0063.5062.0065.0068.0071.0074.0077.0078.5080.0081.5083.0084.5086.0089.0092.0095.0096.5098.0099.50101.00

Au ppb-5-5-5-5-5-5-5-55

1025-5-5205

48015-5""O

65205

-5-5-5-5-5-5 -54520304065140550180-513035

16023017020-5-5-55

15030

48013515-5155

Au g/t

0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.00 0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.00

Lab

TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC

[88/09/15

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Linem674675676 677678679680681682683684685686687688689690691692693 694695696697698699700

t

13 of BURNTBUSH

Hole no

BUR- 12BUR- 12BUR- 12BUR- 12 BUR- 12BUR-12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR- 12BUR-12BUR- 12BUR-12 BUR- 12BUR-12BUR- 12BUR- 13BUR- 13BUR- 13BUR- 13

Sample

5344534553465347 5300C5300534853495350C535054015302530354025403530453055306530753085310 5312531353145405540854095410

DIAMOND DRILLING ^GOLD RESULTS^ [88/09/15

From

101.00102.50104.00105.50 122.00122.00122.50125.00127.00127.00128.50130.00130.50131.00132.00133.50144.50145.00147.00147.50158.00 174.50181.50190.5083.50132.50147.50149.00

To

102.50104.00105.50107.00 122.50122.00124.50127.00128.50127.00130.00130.50131.00132.00133.50134.00145.00145.50147.50148.00158.50 175.00182.00191.00

- 84.00134.00148.00150.50

Au ppb-5455

-5 -5-5-5-5-5-5-5-5-5-5-5-555

10255

-5-5-5

260-5-5-5

Au g/t

0.000.000.000.00 0.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.000.00 0.000.000.000.000.000.000.00

Lab.

TECTECTECTEC TECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTECTEC TECTECTECTECTECTECTEC

li l l l l l l l i i im

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Page l of BURNTBUSH DIAMOND DRILLING >> BASE METALS ASSAYS << [88/11/223

Line Hole no Sample From To Au g/t Cu '/. Zn V. Lab.

'81 BUR-O2 5O97 94.5O 95.OO -0.20 O.058 O.264 MYV82 BUR-O2 5O9B 95.OO 95.50 -O.2O O.026 O.O56 MYV83 BUR-02 5099 95.50 96.00 -0.20 0.020 0.052 MYV84 BUR-02 5100 96.OO 96.5O -0.20 O.017 O.l16 MYV86 BUR-O2 51O1 96.5O 97.OO -0.20 O.O1O O.O40 MYV87 BUR-02 5102 97.OO 97.50 -0.20 0.018 0.164 MYV88 BUR-O2 51O3 97.5O 98.OO -O.2O O.O14 O.184 MYV

ll l ll PlBt l of BURNTBUSH BIMKMB DRILLING )) HMOR ELEMENTS U [68/09/13)

lint Molt no Suplt Frot To Si02 I 1102 I A1203I Ft203I HnO l HtO l do l Nt201 K20 l P205 l LOI X TOTAL! C02 l

1111111m

1

1

1

1

1

1

l

1234S67S9

101112IS14ISU17IBIf2*21222J2425U27282930313233343536373839404142434445464748495051CItH.

535455

MM 01MM 01MM 01MM 01BUR 02BUR 02BUR 02BUR 02MM 02MM 03MM 03MM 03BUR 03BUR 04MM 04MM 04MM 04MM 04MM 04MM 04MM 04BUR 05BUR 05BUR 05MM 05MM 05MM 05MM 05BUR 05MM 05BUR 05BUR 05BUR 05BUR 05BUR 06BUR 06BUR 06BUR 06BUR 06BUR 06MM 06BUR 06MM 07BUR 07MM 07MM 07BUR 07BUR 07BUR 07BUR 07tUR 07B'JR 07BUR 07BUR 07BUR 07

501850195020502650885093510551085109504950505055505750625068506750745075508250845086514851495150515151525153515451565157517851795180518151155118512351295135514551625164517051725174517551B451B651B7519151545101520252045209

40.5055.5071.50

127.0061.5080.00

113.00143.00179.5014.0032.0083.00

130.5025.0047.0052.5083.50

105.00169.50176.00182.0061.5067.5087.0094.00

106.50134.00188.20194.00205.00247.70249.00262.50273.5056.0094.00

113.00134.00146.50175.50724.00232.5068.0080.5094.0098.00

114.50123.00124.3016B.40175.00210.5021B.30225.70254.00

41.0056.0072.00

127.5062.0080.50

113.50143.50180.0014.5032.5083.50

131.0025.5047.5053.0084.00

105.50170.00176.50182.5062.0068.0087.5094.50

107.00134.50188.70194.50205.50248.20249.50263.00274.0056.5094.50

113.50134.50147.00176.00224.50233.0066.5081.0094.5098.50

115.00123.50124.80168.90175.50211.00218.80226.00254.50

51.0452.1167.4250.7254.6752.9862.7148.9852.0757.1552.8057.B650.8252.6857.0958.4972.5771.6653.9555.7158.8761.2260.1155.6359.2459.9856.9947.7049.2258.1948.4155.4550.3660.1564.6858.7153.7668.9665.0255.0861.6054.1444.3557.6772.8975.7159.3453.4961.2846.0851.1556.2254.3245.9257.04

1.140.830.550.581.020.840.630.951.051.261.371.080.970.971.070.910.500.532.700.81

.86

.97

.36

.75

.84

.200.940.440.990.591.061.060.980.530.520.790.800.930.492.631.191.130.420.880.200.410.980.681.471.531.571.010.780.76O.B6

15.6515.1915.6414.1015.5414.6116.3314.9815.9415.9014.2819.5517.4916.2018.6116.7512.9113.1914.6615.6616.6016.7216.4B13.1320.2618.4117.3013.8115.6316.0218.4217.8116.5718.3117.0316.1520.7615.2617.5315.1419.2821.4113.9815.8813.1211.8016.2015.1416.0415.90!t.3515.7215.2716.8015.63

9.856.596.367.047.B56.887.79

16.1813.466.248.786.598.08

15.6510.099.082.624.02

11.3115.977.678.204.10

13.596.197.89

10.0621.209.549.384.368.04

10.726.906.008.068.234.973.40

10.056.91

13.828.22

10.095.564.71

10.006.218.29

14.3710.588.559.313.688.59

0.140.140.170.150.200.140.090.480.390.150.220.170.110.140.170.160.110.080.220.730.240.190.110.570.130.110.261.020.080.370.100.070.160.150.090.110.150.060.030.230.170.350.120.340.060.040.380.080.120.220.180.130.170.090.13

5.331.251.361.713.634.94 -3.533.544.274.065.042.471.771.921.481.830.350.543.842.272.422.771.352.441.712.893.683.206.112.862.213.234.952.002.006.213.761.541.043.681.691.964.653.040.790.595.172.723.227.794.474.088.341.4B5.34

8.9311.034.48

13.2410.309.462.38

10.5112.167.636.973.51B.153.644.605.292.992.939.266.406.565.217.097.145.214.135.937.277.985.989.306.31

10.656.183.755.056.861.772.868.711.940.71

15.672.441.541.412.906.044.479.529.997.495.104.426.01

3.162.533.062.373.363.602.331.691.443.731.932.223.652.633.223.513.083.342.820.523.332.251.971.133.662.351.891.032.022.242.062.561.061.432.213.103.451.317.433.331.711.452.482.243.343.792.141.974.671.782.B43.162.394.403.37

0.051.461.591.47O.B31.053.740.930.390.991.021.851.730.910.690.902.012.240.040.880.691.132.020.820.630.700.510.471.491.264.242.430.711.612.461.161.071.610.790.182.041.360.771.471.140.761.321.450.550.260.271.041.231.460.73

0.210.230.120.160.200.640.290.210.150.380.280.300.270.260.330.360.280.300.540.310.420.260.330.270.190.200.240.280.330.100.380.270.220.260.280.250.160.170.380.580.400.330.100.220.110.140.330.120.390.240.140.420.270.170.33

4.307.900.606.402.801.901.001.801.001.706.402.304.705.702.001.501.601.201.301.102.101.506.402.201.402.402.501.604.303.609.204.302.902.103.202.703.002.202.700.802.402.708.00

.40

.90

.60

.40

.40

.20

.60

.30

.50

.90

.20

.80

99.8199.26

101.5597.95

100.4299.03

100.82100.25102.3399.1999.0997.9097.73

100.7299.3598.7899.02

100.05100.66102.3699.96

100.42101.3397.6799.47

100.26100.3298.0297.70

100.5899.73

101.5399.2799.62

102.22102.28102.0098.98

101.87100.4099.3499.3698.7698.67

100.67100.95101.1689.51

101.7099.2899.0699.33

100.08100.3899.B3

2.525.740.436.412.041.100.111.751.001.353.360.072.730.210.200.521.080.551.030.761.000.133.081.650.150.110.561.142.411.617.023.111.450.690.101.041.110.591.270.580.200.176.036.210.730.600.160.600.180.221.040.500.390.560.52

l l l l

l m Pi'* 2 of mmm DIMIOHD DRILLING n HAJOR ELEMENTS *X [88/07/13]

LiM Holt no SaipU Froi TD Si02 l Ti02 I A1203I Ft2031 HrtO l HgO I C*o I M201 KM I WOS I L01 I TOTAL! C02 ll

l

l

l

l

ii ii i i iii i

5657585960M62aM65tta68a7071727374757k7778798081828384858687888990919293949596979899100

MR 08MM 08BUR 08IUR08BUR 08BUR 08BUR 08BUR 08BUR 09BUR 09BUR 09BUR 09BUR 09BUR 09BUR 09BUR 09BUR 09BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 10BUR 11BUR 11BUR 11BUR ItBUR 11BUR 11BUR 12BUR 12BUR 13BUR 13BUR 13BUR 13

521052115212521352145215521652175218522152245229523252375243524852495250525152525253525452555254525752405261526252635264526556825683526652735282529052945297530153095404540654075411

77.00110.00110.50145.50176.00194.85203.00218.0025.5040.0062.0076.5089.00124.00157.00224.00246.0019.5026.5029.5043.5048.5064.0069.0081.00113.00131.00146.00161.00171.00185.00200.00217.5024.2068.50117.00165.00180.00198.50124.50154.0047.5095.00115.50187.50

77.50110.40111.00146.00176.50195.30203.50218.5026.0040.5062.5077.0089.50124.50157.50224.50246.5020.0027.0030.0044.0049.0064.5069.5081.50113.50131.50146.50161.50171.50185.50200.50218.0024.7069.00117.50165.50180.50199.00125.00154.5048.0095.50116.00189.00

62.5049.7264.1959.7758.0258.5451.1863.2164.3464.7363.6562.4466.1466.3964.3169.4165.1060.3466.8463.2464.1464.2862.5859.1467.1466.6054.4858.6758.8959.1454.2961.1848.8350.1446.8852.3875.9475.9162.6447.4370.4857.0358.2554.5852.98

0.570.470.580.630.690.560.870.610.400.440.390.570.390.460.570.480.400.840.590.540.720.500.430.880.770.471.101.050.960.990.910.830.860.781.681.080.080.090.700.370.710.831.121.131.23

16.4219.8816.3616.4117.3116.0713.9316.4015.6615.8014.7817.6215.8816.1215.2114.0815.8916.3716.7714.7413.8717.0117.0517.0815.4516.4115.0816.9516.3516.5815.5016.3414.8214.7016.2515.4811.9712.0016.3415.8814.4216.2116.2815.6316.46

5.667.466.287.288.034.5411.426.363.043.293.826.372.864.735.964.382.668.482.555.199.263.293.40

. 5.615.583.3415.304.796.585.0410.464.8110.3711.2614.9412.191.271.354.442.062.108.138.2410.1810.32

0.090.130.090.090.090.080.220.080.130.050.220.020.080.050.100.060.030.130.050.090.110.050.060.110.080.060.460.200.160.130.260.190.180.190.230.200.020.020.080.030.040.140.110.150.15

2.856.463.023.503.853.639.45 '3.301.542.321.771.351.522.171.801.231.264.141.131.822.081.531.752.571.762.013.921.943.643.254.471.894.288.816.686.200.330.362.370.900.474.863.365.463.64

4.509.752.751.971.897.08

10.373.065.014.315.151.254.701.103.161.852.684.162.425.003.524.145.576.473.444.137.067.146.436.066.615.92

12.548.948.086.951.041.064.122.362.796.444.747.628.62

3.462.844.233.773.085.002.234.312.385.021.671.994.842.373.332.145.721.330.671.070.670.721.430.740.962.070.81'1.923.213.062.832.051.392.953.203.095.875.625.375.290.333.333.853.172.08

2.541.602.153.043.742.191.352.462.931.733.323.731.852.572.392.932.683.264.073.402.714.052.933.293.012.661.201.731.471.951.051.660.630.431.010.400.460.572.442.433.790.701.030.581.52

0.230.284.160.230.250.590.400.220.270.360.330.270.230.290.290.210.230.310.250.300.250.250.210.190.270.190.190.260.160.250.290.260.270.100.410.210.050.130.300.280.290.260.310.260.27

1.301.501.001.401.503.400.800.602.601.705.104.202.502.300.601.801.801.003.803.801.603.604.003.101.801.902.305.601.602.501.403.305.101.401.301.601.501.002.302.103.701.902.600.802.30

100.12100.10100.8198.1098.44101.69102.21100.5198.3199.75100.2199.81100.9998.5597.7299.5798.44100.3699.1499.1998.9399.4299.4899.18100.2699.84101.90100.2599.4598.9698.0698.4299.2799.70100.6699.7898.5498.10101.0999.1399.1299.8399.8999.5699.57

0.870.240.160.050.132.250.10-0.051.511.452.550.061.660.200.600.991.340.110.932.390.521.411.631.860.641.041.143.351.111.300.880.894.210.260.460.230.690.120.721.481.130.200.320.491.84

11

1V1•lJ111i1l

1- -',11

1;1

Page i of BURNTBUSH DIAMOND DRILLING >> MINOR

Line

1234567e9

10H12131415161718192021 2223242526272829 30313233 34353637 38394041 42434445464748*9 505152t-.1

5455

Hole Saiple

010152020203030303030404040404040405050505 0505050505050505 05050506 06060606 06070707 07070707070707070308OS,IC

oe08

50185020510551085109504950505055CTL505750625067507450755082508450865148514951505151 51525153515451565157517851795180 51815182CTL5115 CTL511851235129 51355170CTL5172 5174518651875191 520152025204520? 521052115212521352145215

Froi

40.5071.50113.00143.00179.5014.0032.0083.00-9.00

130.5025.0052.5083.50105.00169.50176.00182.0061.5067.5087.0094.00 106.50134.00188.20194.00205.00247.70249.00262.50 273.50277.50-9.0056.00 -9.0094.00113.00134.00 146.5068.00-9.0080.50 94.00123.00124.30168.40 210.50218.30225.70254.00 77.00110.00110.50145.50176.00194.85

ELEMENTS << [88

TD Au ppb As ppi Sb ppi Ba ppi Cd ppi Cs ppi Cr ppi Co ppi Eu ppi Hf ppi Ir ppi

41.0072.00113.50143.50180.0014.5032.5083.50-9.00131.0025.5053.0084.00

105.50170.00176.50182.5062.0068.0087.5094.50 107.00134.50188.70194.50205.50248.20249.50263.00 274.00278.00.-9.0056.50 -9.0094.50113.50134.50 147.0068.50-9.0081.00 94.50123.50124.80168.90 211.00218.80226.00254,50 77.50110.40111.0014i.OG176.50195.30

-25

-2-2-26-25

-2-224B3

-2-2-2-2-23310333

37912-2-210 -2

643-221 -2-23

-2 -2-2-25

17-2-214 132198 7964

*" 'i.

-2

0.6 0.2 -50-0.5 -0.1-0.5 -0.1-0.5 -0.1-0.5 0.1-0.5 -0.1-0.5 0.1-0.5 -0.1-0.5 -0.10.9 -0.1

300720160-5026063

290-50290

14.0 0.4 561.0 0.310.0 0.3-0.5 -0.1-0.5 0.2-0.5 0.1-0.5 0.1-0.5 0.10.8 0.1-0.5 -0.1-0.5 -0.1 -0.5 -0.1-0.5 -0.1

110260310-50180210220450300210 140120

-0.5 0.3 200-0.5 0.2-0.5 -0.-0.5 0.-0.5 -0.-0.5 0. -0.5 -0.-0.5 -0.-0.5 -0.1.5 -0.

-0.5 -0.1.0 -0.

-0.5 -0.0.6 -0. 0.6 0.-0.5 -0.-0.5 -0.-0.5 -0. -0.5 -0.-0.5 -0.0.7 -0.-0.5 -0. -0.5 -0.-0.5 -0.-0.5 -0.-0.5 0. 1.4 -0.

-0.5 -0.-0.5 -0.-0.5 -0.-0.5 -0.0.6 0.

\ 460300470350110 370430-50750 -50140240

1200 200160-50360 200170220-50 23021025077

390390450830

1 11001 1200

-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5 -5-5-5-5 -5-5-5-5 -5-5-5-5-5-5-5-5-5-5-5-5 -5-5-5-5-5-5

-0.53.85.21.0

-0.51.81.11.4

-0.5-0.50.93.03.75.6-0.51.21.61.73.30.90.51.01.50.84.32.62.84.91.6 4.13.9

-0.52.3

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13077

23027029038042077

29061

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28018019023022095170 11012011019011050

110150 12088

270160 360320130140 120620350150 190210110270 230610120230 210250250250280140

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Page 2 of BURNTBUSH DIAMOND DRILLING ^ MINOR ELEMENTS << [88/O9/13]r*ye (uic?ur\i^iiDLJon u j. n ri u i* L/ isr\j,L.i~xwu s s riiwun t^L-c.ncnii*3 NX LOO

'H Line Hole Saiple Froi To Au ppb As ppi Sb ppi Ba ppi Cd ppi Cs ppi Cr ppi Co ppi Eu ppi Hf ppi Ir ppi

M. AD PTl -Q AA -O AA -*) -A ^ -A l -4A -( -A t T1A .4 -t t -KA

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La ppi

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>> MINOR ELEMENTS <<

Rb ppi

-555

12028-5141143-53410284045-5222339SB262525131946338651206089-560-51530633025-5422753141425255013888376170 14060-5

Se ppi

27.410.019.043.849.927.027.320.60.220,920.320.39.210.030.419.022.01B.O15.020.019.023.619.010.027.613.018.020.029.011.08.90.47.1-0.218.016.015.06.3

27.2-0.222.96.516.024.541.622.633.316.022.314.022.216.021.1 24.59.00.5

Se ppi

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Ag ppi

-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-22

-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2 -2-2-2

Ti ppi

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Tb ppi

0.8-0.50.60.90.7O.BO.B0.7

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[88/O9/13]

Thppi

0.71.66.9

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13.02.8

H ppi

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l l l Page 2 of BURNTBUSH DIAMOND DRILLING >> MINOR ELEMENTS << [88/O9/13]

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203.00218.0025.5040.0062.0076.5089.00-9.00124.00157.00224.00246.0019.5026.5029.5043.5048.5064.0069.0081.00113.00-9.00131.00146.00161.00171.00185.00200.00217.5024.2068.50117.00165.00180.00198.50124.50-9.00154.00173.3047.5095.00115.50187.50

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Pig* l of BURNTBUSH DIAMOND DRILLING >> MINOR ELEMENTS << [B8/O9/133

Lint Hole Saiple Froi To U ppi Yb ppi In ppi te ppi Na l Sn ppi Te ppi Zr ppi Br ppi Lu ppi Si ppi

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40.5071.50113.00143.00179.5014.0032.0083.00-9.00130.5025.0052.5083.50105.00169.50176.00182.0061.5067.5087.0094.00106.50134.00188.20194.00205.00247.70249.00262.50273.50274.00-9.0056.00-9.0094.00113.00134.00146.5068.00-9.0080.5094.00123.00124.30168.40210.50218.30225.70254.0077.00110.00110.50llf.'-?176.00194.85-9.00

41.0072.00113.50143.50180.0014.5032.5083.50-9.00131.0025.5053.0084.00105.50170.00176.50182.5062.0068.0087.5094.50107.00134.50188.70194.50205.50248.20249.50263.00274.00274.50-9.0056.50-9.0094.50113.50134.50147.0068.50-9.0081.0094.50123.50124.80168.90211.00218.80226.00254.5077.50110.40111.00' ' t f''

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2.002.442.001.401.202.971.802.00-0.023.352.062.852.562.682.340.512.971.701.300.862.731.801.400.891.601.701.502.000.881.100.55-0.021.70

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-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-10C-100-100-100-100-100-100-100-100

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260-200270

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0.30.30.20.40.40.40.40.3-0.20.30.40.30.30.40.30.40.30.30.20.50.30.40.40.30.40.30.20.30.40.20.2-0.2-0.2-0.20.20.20.4-0.2-0.2-0.20.51.60.40.50.50.40.30.30.40.2-0.20.30.?0.3-0.2-0.2

4.703.304.902.803.005.506.044.502.904.204.104.005.305.7010.004.904.904.205.005.043.504.704.903.004.303.804.404.603.902.803.005.545.803.003,303.204.505.101.401.604.0015.045.646.204.904.202.204.102.903.002.003.904.204.60

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57 OB58 0859 0960 0961 0962 0963 0964 0965 0966 0917 0968 0969 1070 1071 1072 1073 1074 1075 1076 1077 1078 1079 1080 1081 1082 1083 1084 1085 1086 1187 1188 1189 1190 1191 1192 1293 1294 1295 1296 1397 1398 1399 13

BURNTBUSH DIAMOND DRILLING

Saiple

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203.00218.0025.5040.0062.0076.5089.00-9.00124.00157.00224.00246.0019.5026.5029.5043.5048.5064.0069.0081.00113.00-9.00131.00146.00161.00171.00185.00200.00217.5024.2068.50117.00165.00180.00198.50124.50-9.00154.00173.3047.5095.00115.50187.50

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203.50218.5026.0040.5062.5077.0089.50-9.00124.50157.50224.50246.5020.0027.0030.0044.0049.0064.5069.5081.50113.50-9.00131.50146.50161.50171.50185.50200.50218.0024.7069.00117.50165.50180.50199.00125.00-9.00154.50173.8048.0095.50116.00188.00

D ppi

0.51.91.21.11.01.21.10.21.42.01.41.00.31.01.11.11.52.23.90.91.10.40.30.2-0.20.20.30.4-0.2-0.20.4-0.20.61.91.20.90.21.10.80.20.4

-0.2-0.2

Yb ppi

-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2*2-2-2-2-2-23

-2-2-2-2-22

-2335

10-2-2-2-2-2-23

-22

Zn ppi

200130380170910230210

-100230180230120340-100170200150200270240240

-100360470130610190180150190190180

-100160

-100130

-100180

4900-100240170210

Ce ppi

3551484446515522636361762264644086715947604730332423232924-55720641201006938566321302835

>> MINOR ELEMENTS << [81

N) I

1.803.021.903.841.301.403.74

-0.021.902.591.704.281.000.440.790.520.561.100.590.671.50

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Sit ppi

-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100-100

Te ppi

-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10-10

Zr ppi

-200-200-200270-200-200-200-200250350270370320-200-200-200-200-200-200-200-200-200-200-200-200-200-200-200-200-200-200-200720-200-200360-200-200-200-200560

-200-200

Br ppi

-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0-2.0

Lu ppi

0.30.2-0.2-0.2-0.2-0.2-0.2-0.2-0.20.2-0.2-0.20.3-0.2-0.20.2-0.2-0.2-0.20.2-0.2-0.20.40.2-0.20.20.30.30.30.20.30.50.71.3-0.2-0.2-0.2-0.2-0.20.30.40.30.3

Si ppi

4.103.803.804.003.604.703.801.904.904.504.005.002.905.405.003.706.504.904.603.804.303.103.603.703.403.503.303.603.001.805.602.906.9012.007.104.602.904.503.602.703.903.604.20

[8B/O9/13D c)

i l l l

lri i ili iii ii li i ii

2. THIN SECTION DESCRIPTIONS

m

- .

1,.

i

'-.'^^l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; B (JR.-Q i Sample No.; S~^ (8

Depth : *tO, S"

Field Rock Name:

Major Minerals: (It - habit, srain size):

1 62^ ) 4 y "/o 9A^^. ——^—————f 7 ^ "————^^F p——-——\—^—^^—

/A^wUJvJ^ 3 S 0/*II lliP'' /T) l -5 c'/j U A^^gxJ____________-O /a—-———--————^—i—---—-—i-—

I r O 't j /c~ o/ L^CuJf^C^^*-___________O /O....^.^^^.^^—,^-^——-,----—-

g ^ Jv^u^u-_____l^L*________________ll ———:—————————il Veins. Fractures; ^——————,———-—,—^—.^^^—^^^t B ' /x/vX-vv C-f^-^t^i /v-C^^~-*^*-t^ t-o s5il '^^li

Minor Minerals:

Alterations:7 ^^ ; -^ ^V tX^Cxt^- ^3. t^^it^Z^C^**^_____^rf^*^^. X^^^^V-^^^^i^^^^**^*^1*!___ ^^^.J ^

l ———^Rock Texture; o

———————————Sit-^ i^D^JC.

l

l

i

Rock Name:

(Doc. 00005U - 11.05.88)

1111,1

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; 6UR- OlDepth : 5"S~, "?-

sample No.: 5"O / 3

Field Rock Name: -O j^Jjjff cJLe^+y—~ir^—zr——Major Minerals: (1 - habit, grain size):

C/ Xl^KC-d^t-/

xO^ipfi LA

30

Minor Minerals:O Ofo

"o

f\

Veins. Fractures:

1 '/ Xi i #~ cUr*-o-a^

Alterations :

i'r--

Jt :-

i1

Rock Texture:

iZJt L&si

y

Rock Name: X? J?. Uu.* Ji

(Doc. S0005U - 11.05.88)

ill

i

COGEMA CANADA LIMITED

B U RNTBUSH R I V ER PROJECT

THIN SECTION DESCRIPTION Hole No.; O O K -O ' Sample No.;

Depth : T"/. 9

Field Rock Name:— rieio KOCK name; '-e^xu^e /^-^^^o^^^C'^^'^^c f*^^t**x~^i ^^^~^^m B^^MBBa*M^*H^**Bi*BB.^^^^^.nB ^•~~~———^i**~—m^^^^————^^^^*^^^^^^^^p^^-^^^^—^^~t^*~il^*^mii r*m^^^^,

l ———————^j)^<s^1U^ */ Afa* ^^^^i

Minor Minerals:

Veins, Fractures:

Alterations :

Rock Name:

5" 0/*

_____7 y*———————o———————————— —

l

l

l

KOCK Texture: i~vLas-^ ctsm^sm. ^Lx^7" ^

B __________________' ________

T4--l, IT-—.. **t? t O "T-

l

1(Doc. #0005U - 11.05.88)

V r cr Major Minerals; (X - habit, grain size); _________'

I /O-, -s 9n 0A . A a " e J)l*C Z-________________ l J U /*——^————— S^fjLM /~*^~* Qsl4L*~JLf' .———————————————————————————p y ^-Q y

J -

Rock Texture: t-^&s^ c/jms^o. SUUS\JL. ts. cxca s***~~^ aj 2T 7^ ^ ^, ,^ ; f

ll

l l l ll lli

COGEMA CANADA LIMITED

B URNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No.;

Depth :

Sample No .; 5 O 3.

il ^o f*tf*r—

Major Minerals; (X - habit, grain size);40SlmjO^/ \JdAAs 2

3 -b /0

tc y.Minor Minerals;

(9; SLj's&'LA** .^^Cc^y) fti^t/JLJL^ S^tf

Veins. Fractures;

l lll ll

Alterations;

Rock Texture;

Rock Name;

(Doc. 00005U - 11.05.88)

l ll

i

i

COGEHA CANADA LIMITED

BUR N T B U S H R I V E R P R O 3 E C T

li tl THIN SECTION DESCRIPTION BOfc-03 ft-3^ Sample No.;

I t ffi Field Rock Name; M^KXU/V-*——^AVWI/UC jAxs^j—

ll '~^0 "~"S

Major Minerals; (X - habit, grain size):

Veins. Fractures

Alterations

Rock Name: ____T~^

l :====:(Ooc. I0029U - 19.11.86)

f

"^

H1nor Minerals;5

Rock Texture: /^Cyc^n/^o cZf - /^^yiaA^^^^Li^ , /JLut^jtM f ±c&X+^^o***____ ,^— . 'j'1— / *-* j.. _ r-1 i i ' —t-*j f . f\vttf-

ll 9lllll

l l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.: g^/V -C/J? Sample No.;

Depth : 33 3, C

Field Rock Name:

Major Minerals: (H - habit, grain size):

i_____________/O 0/.

, A J

__________3P^

l Minor Minerals:

o ht^ijAj 3. y*

Veins. Fractures:

l l

Rock Texture:

(Doc. 00005U - 11.05.88)

Alterations: 6-^VJ^V^JL Xs-^o-i*?-^ x^w^ GO^\ d** jfasLaJLsv^^^-ft

I Rock Name; T^teZ^JLJt /t t/ ' "/t i .li r / ,'/ (j

_________________________ ___ t n^txOg^t^C/UA 7 ^7? /^l f A^u^o t**i C^~~af

l

l

ll 9llI Field Rock Name; _____/tfa/*^ pctw— ______ ^ F*—

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; OUKi~O2) Sample No.; S^OSSDepth : 33.f

Major Minerals; (X - habit, grain size); —l Q-?- ) 4s 0Jo___(o.os-^ o.o?

CLdtruL tre) 3 y VQ

*7 oy•| ^J o^^e^c-*-C4 O /o

Minor Minerals:

3

l

l

l....^•n

ll l l

< i Ve.

Veins, Fractures:

Alterations:

Rock Texture:

Rock Name:

(Doc. S0005U - 11.05.88)

COGEHA CANADA LIMITED

B U R N T B U S H R I V E R P R O J E C Tl C __________l THIN SECTION DESCRIPTION BOfc-fi? \30.8* Sample No.; 5&S7

l

ii

Field Rock Name:

Major Minerals: (X - habit, grain size):

I *———————————- _________c^ffovcU^ (Ft- i

/c ' - f- ?_____________________________ f -JgAx^ftcLc*_______gr

-l ——————————————————

n 111 w i n 111 c i Q id* L^" ^fl\jfl-^'h*iiit*-j^,^J

____________________h^^i.d-o TLo_____f ^

.__________________ /x?A^Uw^ia-^Oc^^g___^

Minor Minerals: fi 'vt-^x? ^3 0X

Veins. Fractures:

Alterations:

Rock Texture:

l

l

l

l Rock Name; /T^dif^tJ^ .^ ti^tuJl^A^ ^^ij ^ *^ /bv*~

™ (DOC. *0029U - 19.11.86)

i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l l l l l

_______________l~jelfflA4*.

l r.UR^k.t^wr,) i-z

l li i

THIN SECTION DESCRIPTION Hole No.; CfisK-CJ'f Sample No.Depth : PS^ *is^

Field Rock Name:

Major Minerals; Ck - habit, grain size); ________________^ xO 7 O/

______/Ir-'

Minor Minerals;

i

Veins. Fractures; ____/xVytx- /^ ~V

M __________________________________

Alterations:i ——E i Rock Texture; *~

x0 ' - * -p——— —————^2^. ^ O^————_______L? gx^^A-tT^--^_____.'.^,

il i

l* AsRock Name;

(Doc. #0005U - 11.05.88)

l i i i i i ii l l lll

-m

v-iI l l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

Sample No.;THIN SECTION DESCRIPTION Hole No.;Depth : 6~o?. O

Field Rock Name;

Major Minerals; (X - habit, grain size);

Tc

V /o

Minor Minerals:

Veins. Fractures; ~~ C

Alterations; H -ww/ L'rp .

l /M J LXJ~*JL

Rock Texture; Id br-La T-u

Rock Name; JZ~-y, ——————— —————

(Doc. #0005U - 11.05.88)

tc*

t i l l i l l l li liEi ii ii

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No.

Depth

Sample No.; O

QJL#

Major Minerals; (% - habit, grain size);

Minor Minerals;

Veins. Fractures;

Alterations:

Rock Texture;

V ORock Name;

7 V.

o

&Z

,SI- T- 3s

(Doc. #0005U - 11.05.88)

lll i li

ir. "

i

l

COGEMA CANADA LIMITED

BURNTBUS H RI V E R PR O J E C T

THIN SECTION DESCRIPTION Hole No.; BU/Z ~^^

Depth : P O , r

Sample No.

Field Rock Name;

Major Minerals; (H - habit, grain size);0/0

+/0 0/*

V.Vo

o

Minor Minerals;3 "/o

A^J2h

Veins. Fractures:

iU~

i

I;

1

i

Alterations; (^b&ri^tt.

Rock Texture:

Rock Name:

l

(Doc. 00005U - 11.05.88)

i i i i i iill l i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No. Depth

Sample No . ; 5^ ? S~/^

Malor Minerals; (X - habit, grain size)

? (o O gxLgK^

/O y

~f~

r^JL' -

'/o

Minor Minerals;

Veins. Fractures;

l

i i

Alterations; f 4 CKeL^Lt^J

Rock Texture; XLxA-xvv-^ ^-J^JLfL^^^t basHjLAstjtf v y u -4- Cvvf-*ii ^^ \Mv***JMr*~C\AA4^—tt—(f-^ 3 I/A,

ii

Rock Name;

(Doc. #0005U - 11.05.88)

l 1 l l l

lS'"ll il

l;-.il[l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; pOfc -&1 Sample No.; 5O~t^) ODepth : IOSt-3t t**-

Field Rock Name; ..————.^-^——.——————^^-——

Major Minerals; (l - habit, grain size); _______________________________

50 7-S' A

Minor Minerals;

Veins. Fractures;

Alterations;

Rock Texture;

Rock Name;v r

(Doc. #0005U - 11.05.88)

i i i i

i i i i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name;i /ta-Ztxe

Major Minerals; (J. - habit, grain size);

H

Minor Minerals;

Veins. Fractures;

S

Sample No.

'si*O L0uL*L~te df

/Q—

^facL'tr L-.

i i i iii

Alterations:

#j^fjis- st^tisi^t. Lt .

Rock Texture: —

Rock Name;

(Doc. #0005U - 11.05.88)

l

l l l l l l l l l i l ll

l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; O OR"O^ Sample No.:

Depth : __

Field Rock Name;

3—— 4~JJt~, v v 3

0 DO -t--ixxxw -^-"-^^-ft'

Major Minerals; (H - habit, grain size):y el /t,

3 -i-A 30

^ fe)V

( v

Minor Minerals:

L*s

Veins. Fractures;

Alterations: 5-5

l

c?-/-^ l/

Rock Texture:

Rock Name:

(Doc. #0005U - 11.05.88)

il l l l l l l lfi llm

'

11ii.l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

.* Depth :

Sample No.;* /x**t

Field Rock Name: j ujty^o 6-\J

a- 7 ,^-w, Le^ s*-0i*\v-

Major Minerals: (1 - habit, grain size):C/

3Minor Minerals: f

V

Veins, Fractures:

Alterations:

c*/.

Rock Texture:

Rock Name:(j o

(Doc. 00005U - 11.05.88)

li-

l

l

l

l

l

COGEMA CANADA LIMITED

B U R N T B U S H RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name;

Major Minerals; (^ - habit, grain size);

sample No.;

l

l

l

I

II

.

Minor Minerals; /"A

fc

Veins. Fractures;

Alterations: 7

Rock Texture; tM T-

l

l

l

Rock Name;

(Doc. //0005U - 11.05.88)

i i i i i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.: Sample No .: S2/S

Field Rock Name:

Depth : Q S- S"

4Major Minerals; (Tt, - habit, grain size);

T tt-

Minor Minerals:

i17*

Veins, Fractures:

Alterations: L^.13^ Ct^-^OVl tJU&VvCt. frdLi*A**VtC

hRock Texture:

Rock Name:

/)(* Li4A~

JLi^L

i (Doc. #0005U - 11.05.88)

il t1

ii i isi;

111i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name:

Sample No.O, 12.

Major Minerals: (X - habit, grain size):so '3

/o

3 v.Vo

Minor Minerals:

0/*

Veins. Fractures:

Ut 3)

^?fW

fa--

Alterations: - r*JL.-Lv g

'- -t.

11

Rock Texture: r\ /ix-^^u.

Rock Name: TZ /t^. — t/Co* U -^

(Doc. #0005U - 11.05.88)

lj*'

l

l

i l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; ——————-—

Depth : k l -9Q

Sample No.: 5" P

Field Rock Name;

Major Minerals; (T* - habit, grain size);

5 /O

j- JA^y

^*j'. _ tdfD Ofo

11

Minor Minerals;3/0-A(j\, .

Veins, Fractures:

Alterations:

Rock Texture:

Rock Name:

(Doc. #0005U - 11.05.88)

C/

uLK

l(i; -i i i i i ii ii ii l l l i l l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

- 03 Sample No.; Sg)

Field Rock Name; (L^u

Major Minerals; (H - habit, grain size);i o 33 aa Ve

350/*

Minor Minerals;

Veins. Fractures;

Alterations;-tA^-C*

V O

Rock Texture; Ze m oLf

Rock Name;

(Doc. #0005U - 11.05.88)

.t T

l

"

m

ll

l

l i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name;

Sample No.: S (P 3 SL

tr

Major Minerals; (l - habit, grain size);

.

v^^ k 0*0*

Minor Minerals;

a^LLJ

Veins. Fractures;

l A pitt

l l l l l

y 7o

Alterations;

Rock Texture; X? *

Rock Name; c (^I^CQ (f

(Doc. #0005U - 11.05.88)

l i l l l i i i i i i i i ii ii i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No. :

Depth :

Field Rock Name;

- 09 Sample No.; 37"

Major Minerals; (* - habit, grain size);

t? 0/*

Minor Minerals;

Veins. Fractures;

Alterations:c? -* .

Rock Texture;

Rock Name; 2T

(Doc. #0005U - 11.05.88)

4 "ALtjJ) jJL

r t/Laf A

LA^

4*

A^t^i*^X

LAX

l l l l l l ll

l l 1 i l i i i

i i

COGEMA CANADA LIMITED

BUR NTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; BUR '

Depth ; f 5?

Sample No. V3

Field Rock Name:

Major Minerals; (X - habit, grain size);

Fp 3 ZS'h 55 7.O SvOlv*.

S e^J 7*

Minor Minerals:

r/*4-

tc. .

Veins. Fractures;

Alterations:

Rock Texture;

Rock Name;

(Doc. 00005U - 11.05.88)

(j D ii QFtp LUv

Uv^XI-f

Pis

. B"' |

™*

'-

.

1*B

1

I

l

l

i i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; 6OR.~Q" Sample No.

Depth : 199.02-

Field Rock Name;

Major Minerals; (X - habit, grain size);

f \^U^*A

^T.- .^ 7.

Minor Minerals:

Veins. Fractures;

Alterations :TT

Rock Texture: n A*-4u-^ sG c. \**s3 T

."

. ^1f. 'W

II ^^B w

B

^H •H

Rock Name:

(Doc. tfOOOSU - 11.05.88)

ll 9

COGEMA CANADA LIMITED

BUR N T B USH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No. : 0" Sample No.

- Depth : 3OH. BO

lField Rock Name;

Major Minerals; (X - habit, grain size):

/. 38

:|h (Doc. ffOOOSU - 11.05.88); IFi

10 '/.

l 1

. /g r,

Minor Minerals;l

a jj < f

l Veins. Fractures;

Alterations; S

:9 Rock Texture; /l/u-q/^ /^ g KXX?I./u-q/

Rock Name;~

l l l l l l l l l l l l ll

i ii il

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name:

Sample No.:

Major Minerals; (l - habit, grain size)iy.

ul 3.0 'A tfr g~ff^20 y**/'

y.

Minor Minerals:

(y ; y*

Veins. Fractures:

Alterations :

Rock Texture: K^l* T.

Rock Name:

(Doc. 00005U - 11.05.88)

(7

l l COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l THIN SECTION DESCRIPTION Hole No.: B(J^- 3 Sample No.; S 'L V 3

Depth : P N ^. l O

Field Rock Name;

lMajor Minerals; (X - habit, grain size);

1^1, G?o*-autXs f id /f-———-—./i6A*M0 CtJL^fJJ "y*0**—^^—*^*~'___ r^flL^Uj f 3 3 7* J7y* Jtidt'JiiLjJL, FpfiL* ffi*,)iL^*L

l

Minor Minerals:

Veins. Fractures:

l cJUt'L

ll -Z__________™ (\ JL^jfcu__________fc

l l l l•av

m Rock Texture; n

l 1=1

l

l

l

Alterations; ___jzu^a.fLTT

"/.•'••••j-

Rock Name;

(Doc. 00005U - 11.05.88)

l l l l l l l i i i i i i i

COGEMA CANADA LIMITED

B URNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :

Field Rock Name:

Sample No.: 53 So

Major Minerals: (1, - habit, grain size):CL^JE j) sg?r^LuiL 15*y*

ID '/o

Minor Minerals: rV* *-

Veins, Fractures:

jjff /QJiAsifa

T* fjnn^t^^t

* J

ffi

Alterations: tjt

Rock Texture:

1i

Rock Name: a^ L*Jf

(Doc. #0005U - 11.05.88)** (ei•QCm ''

li l

1"

1

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; GUfc-10 Sample No.: 53Depth : __^4. i

Field Rock Name: "

Major Minerals; (ft - habit, grain size);lI dAwuxt^ X ^6*A ^t^e^-tt/a U-c^r^y '/- g^cT^~-^--*~w*^a.______/w^*^ •fr^*- -*A* Q^v*"^

JT^ ^ L i^.. ^ ^ " , ^.. ^L O S .-f-.-frP.O 7 I ~*t /y?. .. ^T

3-0

l ——————————

l zzl —————————l Minor Minerals; ———^..^—.—.——^^

l . 04**.."*__________^ l aA

ii,r*

Veins. Fractures:

Alterations; f^d Jla Ac***?, a^t ccri*~0JLe*cXI /vo-^ *^^1 *^^___^cxt-^—

Rock Texture:

Rock Name:JL fiUJt

l (Doc. #0005U - 11.05.88)

I II 7 T*V7fc"tM KxUwt^w , - i-J.O C

i l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l THIN SECTION DESCRIPTION Hole No. : S o ^ ~ltf Sample No.: 5^3 Sol m Depth : ;Z9,5"

•T Field Rock Name; gfA^k cj^ie^ Zts^e^ji^ ' ————-——^^—.^-^————————.

lMajor Minerals; (X - habit, grain size);

l (S^gouAt 7 -33 A xfrn^oJ't'M *Vx^gnxtA.^a6^t^,K^tyO

l 7:

Minor Minerals;

l*- h

~*

*,.

Veins. Fractures;

Alterations; S

Rock Texture;

(Doc. #0005U - 11.05.88)

va

Rock Name; T~ ^y^^ — e^^U CL*4\ U*.

illllll

COGEMA CANADA LIMITED

BURNTBUSH RIVER P R O J EOT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No.;

Depth : 3*1. 9

- (0 Sample No.

Major Minerals; (X - habit, grain size);) /S 7*

Minor Minerals;

(9 3 lol

i Veins. Fractures;

Alterations;

Rock Texture; vQ g ^^* '-

iRock Name; o

(Doc. S0005U - 11.05.88)

h

i i i i i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.;

Depth :Sample No.: 5^53

Field Rock Name: ^p-tj ULVV

Major Minerals: (% - habit, grain size):

I /^t^^xxU-______1C7 /O 'SvLJ^ti. IP Yo

z y*

fP

:

1'' "

i

1

Minor Minerals:

Veins, Fractures: —fT^^C A — T"

Alterations; ^ -C^±4±f2t^4±l±.

1~ MV*

1

Rock Texture; twJa AC/

Rock Name:

(Doc. ffOOOSU - 11.05.88)

li 9ii i iil iiP ilii"- tli li l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name: /•vt

Hole No.: Depth :

L^*-X~-f JL**LS\t

T o. 5"Sample No. S f

Major Minerals; ^ - habit, grain size);

? 1^ 'o'/o

0qSl^US^&l *

b-* //o3 "A

***^***-**!!-rv*

Minor Minerals:Qfa^

Veins, Fractures:

Alterations : rf

/LiJls ' i^ 6, fJUiltl ^0————

Rock Texture:

Rock Name:

tx-

a~^

"CL/

ii

(Doc. #0005U - 11.05.88)

l lll l l l

l l l l l l i ll

l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; J? UP - l d

Depth : tt a . 8Sample No.

Field Rock Name: ***~

Major Minerals: (It - habit, grain size):

Minor Minerals:

Veins, Fractures:

A1:-.

Alterations: tf**8-

Rock Texture: ri

Rock Name: ^—c^ ~teJl

(Doc. 00005U - 11.05.88)

l l COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l THIN SECTION DESCRIPTION Hole No.; B O R. ~ \# Sample No.: S~3. S~ S'

Depth : o ' -@

Field Rock Name; 7~^n^^j(^Ce^^ TA^C^JL^-—^———.^——-——————.^———.———.—.—

II ———————————————————————————————Major Minerals; (X - habit, grain size); ___^__^_^^___^______^__^______

l AL*~xL 7 9 *A/^^cLaJLec^.}

l —————,) P /0 "

cr - - f— v-) gAXX^t LC

C) V

i 1

"

1

Minor Minerals;

t'

li

Veins. Fractures:

(Doc. #0005U - 11.05.88)

Alterations; Q M^vvg ^LZAA^A, U X^

Rock Texture; N ki^a^-c^ ,___C q^ciju^ )____x?^ 4xx? T^

l IZRock Name; IZ~ ^Jbi^^jtJLL,jtil mi————

llB

—

l

l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

Sample No.;THIN SECTION DESCRIPTION Hole No. :

Depth : 4 3,

Field Rock Name;

Major Minerals; (* - habit, grain size);

l 9

xH^oa^TU.

/o

La^J tf*~ K^-xrz^vdT . - kg d*CT14J-&

i Minor Minerals;

3 /o-

l

l

l

l

Veins. Fractures i

Alterations;

i iP i

Rock Texture;

Rock Name: f^^w

(Doc. #0005U - 11.05.88)

Q&'Ob-OZ

l l l l i l l l l

f- - -

l

(lF

l

l

li

l

i

l

li*- '

i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Ho le No.: Sample No.: S~P 5

Depth : &I.O

Field Rock Name: 4 U

Major Minerals: (* - habit, grain size):

/IP

r c

6 J? /O

) < 1 V*3

Minor Minerals:/a

Veins, Fractures:

-J— *xu*t^U3

Alterations:

3- iA' o-^L G^oA*^-, 4-Rock Texture: VS

Rock Name: t^Jl

(Doc. tfOOOSU - 11.05.88)

j^* 6*X-O

lL- '

l

lL ,,

l

l(T

l5,

l

i

COGEMA CANADA LIMITED

BUR N T B USH RIVER P R O J E C T

THIN SECTION DESCRIPTION Hole No. :

Depth :

Sample No.; S

Field Rock Name;

Major Minerals: (l - habit, grain size)

U*X*~d-tA-^ wix^-'v

l —. Minor Minerals;1.

i 1

</% fc"Z /

\A-

r i?KjC^T~^oXx. —— ' \S\^ .

Veins, Fractures:

•iXV^Tutw Cx^

rAlterations : ~ C d-

l

l

iRock Texture: /^./^ eLrl-UK u3g JU^J^, tL**i sO

Rock Name; Ouv fcx

(Doc. 00005U - 11.05.88)

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

f- '

l ll THIN SECTION DESCRIPTION Hole No.: Bofe-*(0 Sample No.; S~*3^/

Depth : 131,0'f

Field Rock Name; -f ^

i C7

Major Minerals; (J, - habit, grain size):

I rM^L^^ IB*/* ^^tL Jfcj ' /T TT y /7y**-, o/ ]

l ^^,,

I ^tXxg^tx ._____y ^0 7*

Minor Minerals:

Veins. Fractures;l ll Alterations; So——-a- o^ctx-Q *- c-LJLo\*^t. oJc-d*^AXw* o/; - ————— ——————————————— A. ,, .—————r-

lt. n

l l l

Rock Texture: f f&^MM ± ^Lg^J/. ^

Rock Name:

|g ———————————^L^^ ?ff

(Doc. 00005U - 11.05.88)

*-:

l 9i l i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.: 13u(2- If? Sample No.; tT 3 4

Depth

ILfc* Field Rock Name;

Major Minerals: (11 - habit, grain size)

_______ ________ ^, B ^ /) J ;0 [ 7 T

•V_________________./'g A

________Ji;i —————Minor Minerals:I njmvi. ni.iicLaj.ai ______________

(9/^^_____J7 /^

l ll

Veins. Fractures:

——————————————————.. .———-———————o -/— ^ f) "f~ s* y i — /~- { ""^ . i Alterations: —3 cxo-*-^___cccJ^cx-- U. ox. ic*'t*i-xvxtxr'Q ^ \ y j^>^x^at><>^>^< l

——————————————^^7 K^^-X ^r^A.——————————————™ '•****X' "fr^t^Ky ~~^Xr-j eLl^^r** f**~

I Rock Texture; S^tt^w^i/ti oJ^JL^JI - -f^t^AJltL ————^ ^ ~

l Rock Name: -J&

l zzzzz^zzzizzl (Doc. ffOOOSU - 11.05.88)

lll l i

COGEMA CANADA LIMITED

BURNTBUSH RIVE R PROJECT

THIN SECTION DESCRIPTION

Field Rock Name:

Hole No.; Depth :

~ 1 0 Sample No.: ,5~c2 (o 3

l Major Minerals; (l - habit, grain size)Op /o T~ ***~JP •JxwoL—t ci

i i

^^-^^^>t^^^^wu<^vc>c3

Minor Minerals:

l Veins, Fractures:i i ii i'f Bi i

Alterations:

Rock Texture: *e* , d* ~ Ut!**'/}'

S3 C Kxt-a T

Rock Name:

(Doc. tfOOOSU - 11.05.88)

l

ll i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; BuR.-

Depth : l 71. 0

Samp le No.

Field Rock Name;

Major Minerals; (X - habit, grain size);

i irif-ii Minor Minerals:

HiiXA^x

Z'lX A —— Al

fi.

i i

Veins, Fractures:

Alterations :

iRock Texture:

i - C

Rock Name:(Sis

i (Doc. tfOOOSU - 11.05.88)

-t-ffC*. Li*, .

i l t COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l l i

THIN SECTION DESCRIPTION Hole No

Depth

Field Rock Name;

.; 3

Major Minerals; ^ - habit, grain size);

/o

Sample No.; S P S"

4A

Minor Minerals;

k

Veins. Fractures;

Alterations;

Rock Texture; T /i—————————l~*--O l

Rock Name;i

|rV*yt^^"^1i A.C/ ^ T,

(Doc. #0005U - 11.05.88)

4.

kCOGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIH SECTION DESCRIPTION Hole No.; B u Sample Ho.;

Depth ; 200,

Field Rock Name;

i Major Minerals; (51 - habit, grain size)

h 3S~AA, QJ^JL^- JtiL.fi JL^L^

l S

Minor Minerals;

t'

i* iit:l

J

Veins. Fractures; - c

i l

Alterations;

v

II Rock Texture:Im

Rock Name; fe/I/IS

l

i (Doc. #0005U - 11.05.88)

l llr -iy ^

i l iife :

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.; Q

Depth :Sample No.: 5~ 2 8

, 5~

Field Rock Name:

Major Minerals: (* - habit, grain size)

3 y.

Minor Minerals:

/o

Veins. Fractures:

Alterations:

^ 4- f e

Rock Texture: ~t^H^^l^c foew j^&vti

l

l

(Jijti^

Rock Name:

Jrf, a. .

(Doc. #0005U - 11.05.88)

iCOGEMA CANADA LIMITED

BUR NTS U S H RI V E R P R O J E C TiDepth : 2V.

THIN SECTION DESCRIPTION Hole No.; BuR' l f Sample No.; O ^ 4* b

. " Field Rock Name; "Skjg^L^

Major Minerals; (l - habit, grain size)

6L*J^ ), *v.2CLe/'

,._______^ f.

Minor Minerals;

li . . f . . —— ^^—— - ^ //./~7~

^ (^C^c^^O__________________1/V '______-^^^ C*"—^/^ frt*. L^i-C^CUl y -Veins. Fractures;

Ir:.'p;*

l ______l —B Alterations; ______JJ^L^ f c L*^*, aJ-uU^LA^m 0{

l

l

l

Rock Texture;

Rock Name;

____________f

l(Doc. tfOOOSU - 11.05.88)

ll m

.t...

l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.: BUf^- l l Sample No.;

Depth : ^ /'

, ft j v *j /fOField Rock Name; ^ \^jtf^-t^i o^^^Jy ^v^^^y . cHJ ax^ti^JL .

J 3 ^J

l Major Minerals; (% - habit, grain size);___________________o T ^ J /rmrfU*i *±A4s~0~Tr\4tA 6*^e eiA4ns*dL*.—a-*^a——————————-—.-~ ^~.p*—*,1 —ri . jT —™~-™""

f^cLa-figt^ (^Li^ift^e) l O

..___________/5"*/————n—^^—————————————————

l

lMinor Minerals;

iI Veins. Fractures; C^&^L aJLLc^f^f qj^0v:^xi y^ue^w-1 ^ e^^ 7^

l :

l Alterations: /^g^ygxuo^-^ ^ txtf nJ^Le^LA^r^ afy XVOT* /c, ^ vfc^XH' gt#T. )CTiX^VTH^ it-^-V

Rock Texture:

1i

l

Rock Name:

(Doc. #0005U - 11.05.88)

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

l *

lB THIN SECTION DESCRIPTION Hole No.: B^^' 'l Sample No.; S o)^?3

" Depth

l

l

Field Rock Name;

Major Minerals; (t, - habit, grain size);T^/O /o________ XWtXysM^^A ^xv^UC^^o LH..CXXU/ - ^LfegV\-^i

,- n i ^i -W Q 7 Q " *

,__________/3^ f-j- ^- -^

l lom "ScL/ixi/e-^K-,^————^———-4 0/*

Minor Minerals:

V

J . CV A^c^^L- .____;____3 Vo

T?

l

i i

Veins. Fractures:

g Alterations; ___rJcc^c^^^c, kcJL&^A^ gjisfriAs^cX

Rock Texture:

_____________________o—-^JkJi-dlt^Li

l

l

l

l

Rock Name:

(Doc. #0005U - 11.05.88)

lir l

I THIN SECTION DESCRIPTION Hole No.; Q \Jft~' (( Sample No.;

Depth : H3.?g

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

Field Rock Name; OJUv * - /- tt*^ ftx*-JCrVTCT ttj /Yna.-A^*j~* /yvi&t-^i i^ur^-^,u^———— ——— T^ r—Major Minerals; (ti - habit, grain size);C^-*-*^Axt^- f: , C/

33r^A

iC c^J^Jt^ -T Vo 1

Minor MineralsI VlAtft^b LA^IL^l. O JLO *

C^AA^^-C^ _____ i? /o

_____[______S V*l =Veins , Fractures :

Alterations : ^p. w

i l il -——m ————™ Rock Name; ___-S

i

l

Rock Texture:

(Doc. tfOOOSU - 11.05.88)

l:: t-

l

l

i i

l

l:,

l ll

i": -

L,nElil[l l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No.

Depth

Field Rock Name:

Sample No.: S 2. Q 2-

Major Minerals: (1. - habit, grain size)

A 3 3 "1 "

Minor Minerals:3

Veins, Fractures: jp-t*t~{ylt4sUL4J

Alterations: U?

Rock Texture:

Rock Name: O kjta^ju

(Doc. tfOOOSU - 11.05.88)

lll ll l

COGEMA CANADA LIMITED

BURNT BUSH RIVER P R O J EOT

THIN SECTION DESCRIPTION Hole No. : G^R-'H Sample No.; 5"2 BO

Depth : l k . 10

Field Rock Name:

Major Minerals; (* - habit, grain size);

s

(r*) /e*/.m*

e

Minor Minerals;

m

i Veins. Fractures;

i..

,.. — (Doc. #0005U - 11.05.88)

t l

•m p A i .^ ,. ^ /V"0 ., /i ., . 7 0cT

Alterations : r S-^^vr^^tUL^ /5 lv gyp- g*-

•j Rock Texture; j: G

bL^-f^i^ e^^UJ^a, yt^^ "xv-fc^ — vcX^ " Aj^6-,*r~ *x xvvi^To^ ;Cc^ttZU-g . C /N^--T •

a MJu ovJ''t*.L

•i-

iCOGEMA CANADA LIMITED

BURN TBUSH RIVER P R O J E C T

THIN SECTION DESCRIPTION Hole No. :

Depth :

Field Rock Name;

Sample No .; b 2- J

l Major Minerals; (To - habit. Rrain size);

i

f

l l l Minor Minerals;

l l l l l l l l

Veins. Fractures;

Alterations;

Rock Texture;

Rock Name;

(Doc. 00005U - 11.05.88)

itK

i i i i i iii

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No.

Depth

t Vf i

Major Minerals; (1* - habit, grain size);

Minor Minerals;

(9

to,

Veins. Fractures;

1m Alterations;

l

i

Rock Texture;

Rock Name; ^A

(Doc. 00005U - 11.05.88)

Sample No.;

f

iiiVl1- ii ll

ii i i i i i i i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No. Depth

Bud- liJ33.0

Sample No.

Field Rock Name: X)o

Major Minerals; (t, - habit, grain size);

•f.' Minor Minerals;

i {o

Vo

,y.-B Veins. Fractures;ir

Alterations : JtLJJg^^i i^tyijf

si ~j 27 fi

Rock Texture:

Rock Name: .^t* J^b*. ?

(Doc. #0005U - 11.05.88)

l i i iiiiii i i i i

COGEHA CANADA LIMITED

BURNTBUSH RIVER PR O J E C T

THIM SECTION DESCRIPTION Hole No.;

Depth ;

Field Rock Name;

(2~ Sample No.;

sdJL*-4iJt^A-\S* jQ

Major Minerals; (% - habit, grain size);

A—^ g_g

r i.

' 10 '

Minor Minerals; /••y/a

Vo xuJ-tL.

Veins. Fractures; S—^ Z-~X Cv-^-t^f

—f d

Alterations;

i i

Rock Texture;

Rock Name;

(Doc. #0005U - 11.05.88)

ll ll

l l

IIIlli

llil

! l Rock Texture;

l

COGEMA CANADA LIMITED

BURNTBUSH RIVE R PROJECT

THIH SECTION DESCRIPTION Hole Ho. : B V fc - \ 2.

Depth : l 5" j. 80Sample No.;

Field Rock Marne;

Major Minerals; (* - habit, grain size)

y.

Minor Minerals;3 J

Afajcti

Veins. Fractures;

Alterations ; utj

Rock Name;

&L

l (Doc. tfOOOSU - 11.05.88)

(S:?""

i

l

l

a"~''i

illilL,

i iii-ii

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION

Field Rock Name;

Hole No.; B (J {? - \7-

Depth : 769. 95"

Sample No.;

G -2. 'P

Major Minerals; (X - habit, grain size);

S"-l-.'. 1

Minor Minerals;

Veins. Fractures

Alterations i

l l l l l

Rock Texture;

775. S 30 f(Doc. 00005U - 11.05.88)

ii i i ik -iii*i

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

THIN SECTION DESCRIPTION Hole No. Depth

~ 1 3 Sample No.; S^ O*1

4?.

Field Rock Name; /^CoX^g Lo

- Major Minerals; (H - habit, grain size);

y3 y*

Minor Minerals;

i 9/.Cfo

t\ m Veins. Fractures;l

l

I

l

l

l

l

Alterations;

Rock Texture;

Rock Name;.

(Doc. #0005U - 11.05.88)

lCOGEMA CANADA LIMITED

BUR N T B U S H R I VER PROJECT

THIN SECTION DESCRIPTION Hole No. : 6 K- 13 Sample No.; fT

Depth : 5* S. O

Major Minerals; (H - habit, grain size)

1 ^^^ Field Rock Name; Ax&A^e w s**^AJL*™*-*~db-eiJJi——-— j^&w-"

4T A/^ut^ 7 ^Y,^1^ A . . ^ f M f

l3 7o

^ Minor Minerals;

*.--,. ^~-^—18 ™ Rock Name;

(Doc. #0005U - 11.05.88)t

Veins. Fractures;

B Rock Texture; A/g^v^ /Jto UIAX) fcg___^l^c^uejl LuaV jM^Le^ xigK^r-

l

l

l

COGEMA CANADA LIMITED

BURNTBUSH RIVER PROJECT

— THIN SECTION DESCRIPTION Hole No.: 6 Ufc- l 3 Sample No.; S^OT"

l Depth : It 5*. 3

l Field Rock Name;

Major Minerals; (l - habit, grain size);lW^ uLwM.'ts ? So "A

ifl ret k f*** J—2JZi!-fm # 7^7 jy o/T. W /S^~*U. u-____c? A?

C^-MX^V"^(-/^___X /oi ———Minor Minerals;

i'rM Veins. Fractures; (txJLc^t. U. /vCt^v Lg fa

fli

P M -. . , , j- "^* " * ' ' * /^ /l II T— -f— , l J A — f^ ^ t7* J^Lv^Alterations:

t*- ^—^————

I Rock Texture: /v^wa^ u? ^*^o 6^*____^d^tJUf* ^o g Axx?/

____________________!________

l

i

i

Rock Name:

(Doc. tfOOOSU - 11.05.88)

ii i i i j

COGEMA CANADA LIMITED

BURNTBUSH RIVER PR 0 J E C T

THIN SECTION DESCRIPTION Hole No.; BUR.~\^ Depth : 181 .

Sample No.: S 4///

Field Rock Name: f\

Major Minerals; Ck - habit, grain size);

i S'/o

1 ii lil i

Minor Minerals:

3

Veins. Fractures:

Alterations:

itI Rock Texture:ii

Rock Name:

l(Doc. tfOOOSU - 11.05.88)

Ministry ofNorthern Developmentand Mines

/y foofRicorNeme and Poste^AdcTress or Recorded Xoldei

COGEMA CANADA LIMITED

32E12SWae6S 20 HOBLITZELL 900

T-4677

2000 Mansfield, Suite 400, Montreal, Quebec, H3A 2Z1Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

8576for Performance of the following work. (Check one only)

Manual Work

S ha f t Sinking Drifting or other Lateral Work.

] Compressed Air, other Power driven or mechanical equip.

Power Stripping

J Diamond or other Core drilling

J Land Survey

All the work was performed on Mining Claim!!): gee attached list

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Diamond Drill Contractor: Les Forages Foranord Inc.920 boulevard Rideau C.P. 307Rouyn-Noranda, Quebec J9X 5C3

Equipment: 2 unitized drill shacks with super 38 Longyear core drills with hydraulic tower, hydraulic chuck, hydraulic mud mixer,

pressure pumps: Beam 435 with hydraulic motor,

supply pumps: Beam pump with AC l diesel motor in unitized shack,

BQ core barrels, rods, BW and NW casing,

bulldozer, timberjack, sloops, portable heated water tank (for transporting water to holes remote from river, lakes)

one full camp with kitchen, workshop, sleeping facilities.

Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth In the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report Is true.

Name and Postal Address of Person Certifying

John Learn, 2000 Mansfield, Suite 400, Montreal, Quebec, H3Z 2Z1Date Certified ,IWt Certified b* (Signature)

Table of Information l Attachments Required by the Mining Recorder JKfhn LearnType of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

Specific information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost mutt be submitted within 30 days of recording.

Signed core log showing; footage, diameter of core, number and angles of holes.

Name and address of Ontario land surveyer.

Other information (Common to 2 or more types)

Names end addresses of men who performed manual work /operated equipment, together with dates and hours of employment.

Names and addresses of owner or operator together with dates when drilling/stripping done.

Nil

Attachments

Work Sketch: these are required to show the location and extent of work in relation to the nearest claim post.

9Work Sketch (as above) in duplicate

Nil

768 (86/12)

MINING LANDS; PLEASE COMPLETE THIS FORM S. RETURN IT WITH REPORT ——— TO THE ASSK&SMIW FJI.KS OFF1CK

DATE REMOVED: . fj] (from AFO)

REPORT f

PICHE NO. :

DATE RETURNED: (to AKI)')

(whore applicable)

REASON FOR REQUESTING REPORT (complete 11-4 below):

1. INFORMATION ADDED TO EXISTING PAGES OF REPORT: Q

IF YES, SPECIFY PAGES: ____

2. a) PAGES/MAPS ADDED TO THIS REPORT: TOTAL PAGES ADDED

b) TYPE OF PCS ADDED:

3. a) REMOVAL OF PGS FROM REPORT:

b) TYPE OF PAGES REMOVED :

J ___ TOTAL MAPS ADDED

CORRESPONDENCE

WORK REPORTS (AMENDED)

WORK RPTS (NEW)

MISSING PAGES OF TEXT

OTHER (PLEASE SPECIFY)

TOTAL PGS REMOVED

CORRESPONDENCE

WORK REPORTS

PGS OF TEXT

OTHER (PLEASE SPECIFY)

4. REPORT NEEDED FOR REFERENCE ONLY:

NO INFORMATION ALTERED :

NO INFORMATION ADDED :

NO INFORMATION DELETED :

DISTRIBUTION OF CRBDITS Doe.: 1608c

L789211

L789212

L789213

L789214

L789215

L789216

L789217

L789218

L789219

L789220

L789221

L789222

L789223

L789224

L789225

L789226

L789227

L789228

L789229

L789230

L789231

L789232

L789233

L789234

L789235

L789236

L789237

L789238

L789239

L789240

L789241

L789242

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

L789243

L789244

L789245

L789246

L789247

L789248

L789249

L789250

L789251

L789252

L789253

L789254

L789255

L789256

L789257

L789258

L789259

L789260

L789261

L789262

L789263

L789264

L789265

L789266

L789267

L789268

L789269

L789270

L789271

L789272

L789273

L789274

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

25

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25

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L789275

L789276

L789277

L789278

L789279

L789280

L789281

L789282

L789283

L789284

L789285

L789286

L789287

L789288

L789289

L789290

L789291

L789292

L789293

L789294

L789295

L789296

L789297

L789298

L789299

L789300

L789301

L789302

L789303

L789304

L789305

L789306

25

25

25

25

25

25

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25

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25

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25

25

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15

25

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25

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25

25

25

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25

25

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25

15

15

L789307

L789308

L789309

L789310

L789311

L789312

L789313

L789314

L789315

L789316

L789317

L789318

L789319

L789320

L789321

L789322

L789323

L789324

L789325

L789326

L789327

L789328

L789329

L789330

L789331

L789332

L789333

L789334

L789335

L789336

L789337

L789338

25

25

25

25

25

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25

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25

25

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25

25

25

25

25

25

25

25

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25

25

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25

25

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25

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L789339

L789340

L789341

L789342

L789343

L789344

L789345

L789346

L789347

L789348

L789349

L789350

L789351

L789352

L789353

L789354

L789355

L789356

L789357

L789358

L789359

L789360

L789361

L789362

L789363

L789364

L789365

L789366

L789367

L789368

L789369

L789370

25

25

25

25

25

25

25

21

21

21

21

21

21

21

18

21

21

21

21

21

21

21

21

21

21

21

21

21

21

21

21

21

Pag* 2Doe . : 1608c

L789371L789372

L789373

L789374

L789375

L789376

L789377

L789378

L789379

L789380

L789381

L789382

L789383

L789384

L789385

L789386

L789387

L789388

L789389

L789390

L789391

L789392

L789393

L789394

L789395

L789396

L789397

L789398

L789399

L789400

L789401

L789402

21

21

21

21

21

21

18

21

21

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21

21

21

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21

21

21

28

28

28

28

28

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28

28

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18

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- r . •••--

L789403

L789404

L789405

L789406

L789407

L789408

L789409

L789410

L789411

L789412

L789413

L789414

L789415

L789416

L789417

L789418

L789419

L789420

L789421

L789422

L789423

L789424

L789425

L789426

L789427

L789428

L789429

L789430

L789431

L789432

L789433

L789434

28

28

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28

28

28

28

28

28

28

28

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28

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L789435L789436

L789437

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L789451

L789452

L789453

L789454

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L789462

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L789464

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28

28

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28

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L789474

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L789494

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28

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L789499L789500L789501

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282828

282828282828

36

38

38

75

75

75

75

75

75

75

75

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75

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i

WORK WAS PERFORMED OM THE FOLLOtflMG CLAIMS;

L789239

L789304

L789316

L789317

L789318

L789326

L789329

L789332

L789332

L789335

L789357

L789358

L789358

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L789467

L789468

BUR-12

BUR-11

BUR-13

BUR-13

BUR-09

BUR-10

BUR-10

BUR-01

BUR-03

BUR-04

BUR-05

BUR-06

BUR-07

BUR-07

BUR-02

BUR-02

BUR-08

BUR-08

0-191

0-2170-71

71-188

0-2570-14

14-244

0-200

0-149

0-200

0-278

0-247.2

203-260

0-203

0-154

154-245

147-228

0-147

metersmetersmetersmetersmetersmetersmetersmetersmetersmetersmetersmetersmetersmetersmetersmeters.3 metersmeters

626.6 feet711.9 feet232.9 feet383.9 feet843.2 feet45.9 feet754.6 feet656.2 feet488.8 feet656.2 feet912.1 feet811.0 feet187.0 feet666.0 feet505.2 feet298.6 feet

266.7 feet482.3 feet

Total: 2904.5 meters 9529 feet * 9529 days

Note: Also included in the report on drilling are analytical results and thin sections descriptions which would add an additional 920 days work; however, only 8576 days are needed to bring the total assessment credits over all 312 claims which comprise the Burntbush River property to the required amount of 200 days. Thus, the full five years' work has been performed and reported.

(Doc.: 1608c)

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