project no.327 thunder bay. ontario senior geologist · group 400 meters southwest along strike...

52P08NW0010 W9640 00547 PETAWANGA LAKE 010

NORANDA MINING AND EXPLORATION INC.

DIAMOND DRILLING REPORT

PETAWANGA PROJECT

N.T.S. 52P/8

WESTERN CANADA REGION

PROJECT NO.327 THUNDER BAY. ONTARIO

JUNE, 1996

REG FELIX SENIOR GEOLOGIST

52P08NW0010 W9640 00547 PETAWANGA LAKE

Table of Contents

PAGE

SUMMARY .... ............. . ... .....................................................................................................................1

1 O INTRODUCTION................................................................................................................................^

2 O LOCATION AND ACCESS ............. ....................................................................................................2

3.0 PROPERTY DESCRIPTION....................... ........................................................................................2

40 REGIONAL GEOLOGY .......................................................................................................................3

5.0 PREVIOUS WORK..............................................................................................................................3

6.0 DIAMOND DRILLING ..........................................................................................................................4

7.0 DISCUSSION OF RESULTS ...............................................................................................................4

8.0 CONCLUSIONS AND RECOMMENDATIONS....................................................................................^

STATEMENT OF EXPENDITURES (MARCH 1 - JUNE 30, 1996)............................................................8

REFERENCES..................................... ....................................................................................................9

List of AttachmentsScale

Figure 1 Location and Regional Geology Map ................................................................ 1:300,000

Figure 2 Claim Map - Petawanga Lake .............................................................. (approx.) 1:80,000

Figure 3a Attwood Lake Area Compilation Map................................................... (approx.) 1:75,000

Figure 3b Disco Lake Area Compilation Map....................................................... (approx.) 1:10,000

Figure 4 Stacked Profile - L5500W...................................................................................... 1:2500



List of Appendices

Appendix l Diamond Drill Logs

Appendix II Geochemical Analyses, Analytical Procedures

Appendix III Petrographic Reports

List of Maps (In Back Pockets)

Map 1 Drill Hole Location - Discovery Lake (West) Grid................................................... 1:5000

Map 2 Section 55+OOW - DDH PO96-13 ..........................................................................1:1000

Map 3 Section 22+OOW - DDH PO96-14 ................................ ...........................................1:500

Map 4 Section 31+OOW- DDH PO96-15 ..........................................................................1:1000

010C

SUMMARY

In late March, April and early May, 1996, three holes totalling 496,6 meters were drilled on the

Petawanga property. Two holes tested the North Central HLEM conductor, a strong northeast-southwest

trending anomaly located at the top of the Central Felsic Volcanic Group, at vertical depths of 30, 75 and

175 meters. The North Central HLEM conductor has been traced with ground geophysical and surface

geological surveying over a strike length of 4 kilometers on the Petawanga property and another 3.5

kilometers across the adjacent Attwood property. Only three drill holes, PO-1, PO-95-10, and PO-95-11,

previously tested this anomaly.

A third hole tested the South Main HLEM anomaly located near the top of the Cormac Volcanic

Group 400 meters southwest along strike from DDH PO-6 at a vertical depth of 70 meters. Previous drilling

(PO-3 to 9, PO-95-12) in the Cormac Volcanics concentrated on the Goldfields and Ryley Cormac showings

(5 holes) and the South Main HLEM anomaly (3 holes).

The 1996 drill holes covered in this report varied from 134 meters to 210 meters in length and tested

anomalies down to a maximum vertical depth of 175 meters. Banded to massive pyrrhotite with lesser

pyrite mineralization and moderate to intense metamorphosed equivalents of hydrothermal alteration of the

felsic metavolcanic stratigraphy was intersected in each of the 1996 drill holes. No economic Cu-Zn

mineralization was intersected in either of the drill holes on the North Central HLEM anomaly and a similar

but narrow local section of fractured felsic tuff mineralized with 5-10 070 chalcopyrite over 0.5 meters was

intersected in the drill hole which further tested the South Main HLEM anomaly.

1.0 INTRODUCTION

A diamond drilling program was carried out on the Petawanga property between March 19 and May 15, 1996 The object was to test two HLEM conductive horizons with associated strong magnetics. The first anomaly (North Central HLEM Anomaly) which was located at the stratigraphic top of favourable Central Felsic Group metavolcanics was tested at depth for potential volcanic massive sulphide mineralization. The HLEM conductive horizon occurs within a zone of intense garnet-chlorite, chlorite-amphibole- garnettmagnetite, and garnet-staurolite alteration. Drill hole PO-10 which was previously drilled near geologically mapped pyroclastic breccia had intersected 4 pyrrhotite-pyrite zones hosted by interbedded moderately to intensely altered (chlorite-garnetimagnetite) felsic lapilli/quartz-eye tuffs and banded argillites. The sulphide zones range in width from 5 meters up to 60 meters in core width and host semi- massive to massive units that vary from l meter core thickness to 13 meters. The second anomaly South Mam HLEM Anomaly) tested is located near the top of the Cormac Volcanic Group. Previous drilling (1991) had intersected 2.09 07o Cu, 32 g/t Ag, 2gH Au over 1.27 meters hosted within a geochemically copper enriched zone in PO-6. An AEM/AMAG survey in 1995 delineated the South Main HLEM anomaly a further 500 meters west of DDH PO-6. In 1995, DDH PO-12 was drilled 200 meters east and along strike from PO- 6. The 45 meters of S-5% disseminated to banded pyrrhotite pyrite mineralization with local concentrations of 30-40 07o and a 0.5 meter section mineralized with S-5% chalcopyrite that was intersected m PO-12 , in conjunction with remobilized massive sulphide intersections and the copper and zinc enrichments intersected in drill holes PO-3 to 9 indicate that there are active Cu and Zn rich hydrothermal systems in the Cormac Volcanic Domain.

2.0 LOCATION AND ACCESS

The property is located in the Thunder Bay Mining District approximately 100 kilometers north of Armstrong and 25 kilometers west of Fort Hope. The property is situated about 5 kilometers south of Petawanga Lake on the Albany River. The Discovery Lake grid is accessible from Armstrong, Nakina or Pickle Lake via float or ski-equipped plane charter to a tent camp on Disco Lake. The lake is shallow and small allowing fixed wing aircraft to exit with only partial cargo loads. Another tent camp was erected in 1995 on Auger Lake which is located l kilometers to the southwest of Disco Lake. Auger Lake is a much larger lake and will accommodate full cargo loads. Diamond drilling programs require helicopter support. Landing strips for wheel based aircraft near the property include Fort Hope and Miminiska Lake (20 kilometers northwest (Figure 1).

3.0 PROPERTY DESCRIPTION

The property encompasses 193 unpatented mining claims (193 units) totalling 3088 hectares. The claims are situated within claim map areas G-378 (Petawanga Lake) and G-287 (Kawitos Lake) of the Thunder Bay Mining Division and are listed below (Figure 2).

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PETAWANGA

LOCATION MAP

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Table 1: Petawanga Claims

Claim NumbersTB 1,040,631TB 1,120,975-978TB 1,122,020TB 1,122,021-022TB 1,122,023-024TB 1,122,025-026TB 1,122,027TB 1,122,029TB 1,138,336TB 1,138,337TB 1,138,338-339

Recorded |Claim Numbers7/17/897/17/897/17/899/20/898/23/899/20/898/23/898/23/899/20/89

3/8/909/20/89

TB 1,138,389TB 1,138,392TB 1,139,667TB 1,142,048-061TB 1,142,072-075TB 1,142,353-364TB 1,147,544-571TB 1,148,726-727TB 1,149,125-129TB 1,165,210-213TB 1,165,214-230

Recorded |ciaim Numbers3/8/903/8/903/8/903/8/903/8/903/8/909/6/90

8/24/908/24/908/24/90

9/7/90

TB 1,165,231-233TB 1,165,234-242TB 1,165,258TB 1,165,260-287TB 1,165,288TB 1,165,290-300TB 1,165,801-803TB 1,165,856-865TB 1,165,931-940TB 1,166,065-073

Recorded9/24/90

9/7/909/24/908/24/90

9/7/908/24/908/24/908/24/90

9/7/909/7/90

The project area is covered by an option agreement between Falconbridge Limited/Shaun Parent/Michael Smith and Noranda Mining and Exploration Inc. The claims were staked by S. Parent and M. Smith who together hold a 25 07o interest. Noranda has the right to earn 5007o (37.5 07o) of Falconbridge's 75 07o interest subject to an NSR by spending 3900,000 over four years and 100 07o of Parent/Smith's total 2507o interest by making cash payments totalling 550,000 to Parent/Smith. Noranda is the operator.

4.0 REGIONAL GEOLOGY

The property is located within an "underexplored" northeast-trending belt of metavolcanics and metasediments along the southern margin of the Uchi Subprovince, part of the Superior Province of the Canadian Shield (Figures 1 and 3a and 3b). This belt connects with the main regional greenstone belt of the Uchi Subprovince about 16 kilometers north of Attwood Lake. According to Wallace (1977), the older metavolcanics are predominantly pillowed and massive mafic flows intermixed with units of andesitic to rhyolitic pyroclastic rocks. The metavolcanics are conformably overlain by clastic metasedimentary rocks consisting mainly of polymictic conglomerate rocks rich in metavolcanic clasts. Ferruginous chemical metasediments occur in several places close to the metavolcanic-metasedimentary interface. The supracrustal sequence is surrounded by granitoid rocks, predominantly trondhjemitic to granodioritic in composition. The rocks have been metamorphosed under amphibolite facies conditions. The property has been interpreted by Falconbridge to consist of five distinct geological domains, the Cormac Volcanics, Central Felsic Volcanics, Western Volcanics, and the Northern and Southern Granite Domains. A number of small localized Cu ± Zn occurrences occur within the Cormac Volcanics and have been previously trenched and/or drill tested. The Central Felsic Domain contains "brickwork" style chlorite-amphibolite-garnet alteration within "lahar-type" deposits where lapilli to block sized fragments occur infrequently.

5.0 PREVIOUS WORK

Throughout the years, geological mapping and exploration in the Petawanga Lake-Kawitos Lake areas has been limited by their remote location and poor accessibility. Geological maps published by government agencies (Geological Survey of Canada-1960 and the Ontario Department of Mines -1969 ) which encompassed the current property were the result of reconnaissance surveys that were part of much larger areas. These maps provide a very generalized geological data base. In 1973 the Ontario Geological Survey initiated a program of detailed geological mapping in the eastern part of the Uchi Subprovince. Included in this program were the Attwood Lake area (Wallace 1977) situated immediately to the southwest

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of the Petawanga property, and the Miminiska Lake and Opikeigen Lake areas (Wallace 1978) situated immediately to the north. In the past 35 years four companies are known to have directed mineral exploration activity on the Petawanga property toward the location of base metal sulphide or gold deposits.

In 1961, Boylen Engineering Offices followed up a previous airborne reconnaissance survey with ground magnetic and magniphase EM surveys, geological mapping, trenching and 11 diamond drill holes totalling 1276 meters.

In 1976, New Jersey Zinc Exploration Company Limited undertook geological mapping and prospecting and completed 9 diamond drill holes totalling 317 meters following an AEM survey of the region.

During 1986 Goldfields followed up a Mag, VLF, EM airborne survey with linecutting, outcrop stripping and 1 drill hole totalling 245 meters.

Falconbridge Limited obtained an option on the property in 1990 and conducted linecutting, geological mapping, ground Mag, VLF and HLEM geophysical surveying and mechanical stripping. In the summer of 1991, nine drill holes totalling 1723.5 meters tested a number of geological and geophysical anomalies.

Noranda obtained an option on the property in 1994. Geophysical surveying, geologic mapping and lithogeochemical sampling were completed in 1994. During March-April, 1995 an AEM/AMAG survey was flown over the adjacent Attwood claim group. In June, 1995 downhole pulse electromagnetic surveying was carried out on four holes previously drilled by Falconbridge on the Petawanga property. A diamond drilling program with three holes totalling 692 meters was also completed in June, 1995. Linecutting, ground magnetics and HLEM surveying were done on extensions of the Disco Lake grid in conjunction with similar surveys on the adjacent Attwood property in the early winter of 1996.

6.0 DIAMOND DRILLING

The diamond drilling was contracted to W.G. Langley Ltd. of Brampton, Ontario. The holes were drilled utilizing a JKS 300 diamond drill with BDBGM thin wall size drill rods. Core was logged in metric units. Sampling was done on geologic controlled intervals from 0.4 meters to 2.2 meters but generally averaged 1.5 meters over areas of sulphide mineralization. A total of 118 drill core samples were submitted to Accurassay Labs Ltd. for Cu-Zn-Ag±Au analyses. In addition, a suite of 8 core samples from the three holes was analyzed for whole rock determinations by Chemex Labs of Mississauga, Ont. These data will aid in the evaluation of the varying intensities of hydrothermal alteration observed to date and will help focus future drill targeting. Thin section and petrography examinations were done on 3 core specimens of intense alteration. Analytical procedures and results are appended to this report.

Drill hole locations are plotted on Figure 3 and Map 1. Stacked profiles of each of the drill hole targets are provided on Figures 4-6. The drill logs and cross sections are appended.

7.0 DISCUSSION OF RESULTS

Three diamond drill holes totalling 496.6 meters were completed. The first and third holes were designed to test the Main HLEM conductive horizon which has been delineated for 7.0 kilometers of strike length and occurs at the top of the felsic volcanic group. The North Central HLEM anomaly varies in expression along strike from multiple conductive sources to a single conductive feature.

The first hole, PO-13, intersected the target conductive zone between 90.6-111.5m at a vertical depth between 60-80m. The HLEM anomaly at this section is comprised of a graphitic-pyritic argillite- exhalite zone at the top of the Central Felsic Metavolcanic Group in contact with the overlying Western

Mafic Metavolcanic Group. Sulphide mineralization consists mainly of 20-2507o blebs and bands of pyrite with lessor pyrrhotite including two narrow (10 cm) bands of massive pyrite-pyrrhotite. No significant copper-zinc mineralization was noted; traces of chalcopyrite and sphalerite were noted in the exhalite unit as well as the overlying altered felsic tuffs. Values up to 110 ppm copper and 1112 ppm zinc occur within the upper sulphidized felsic tuffs, and a very weak geochemical zinc enrichment (up to 512 ppm zinc) occurs within the banded argillites hosting the semi-massive to massive sulphide intersections. The semi-massive to massive pyrite-pyrrhotite bands themselves were relatively depleted in copper and zinc suggesting that they occur laterally distal to BM deposition. The footwall felsics exhibit striking porphyroblastic staurolite and garnet alteration within a moderately sericitized and chloritized aphanitic finely bedded felsic tuff. The hole was shut down within a porphyroblastic staurolite biotite felsic schist. The stratigraphy intersected in DDH PO-96-13 correlates well with the first or top conductive zone of PO-95-10 where an interbanded pyritic argillite and massive sulphide exhalite unit overlies an intensely altered (staurolite-garnet porphyroblasts) bedded felsic tuff. In PO-95-10 the hole was drilled further to intersect a second massive sulphide (13 meters of po-py) zone located at the contact of altered felsic lapilli tuffs and felsic bedded tuffs approximately 80 meters down stratigraphy from the first exhalite. It would have taken another 100 meters of drilling of PO-96-13 to test this horizon with no HLEM anomaly to target on this section.

The second drill hole, PO-96-14, targeted the South Main HLEM anomaly at 75 meters vertical depth, 400 meters west of drill hole PO-6. Airborne AEM/AMAG carried out in 1995 and ground geophysics completed in April, 1996, extended the South Main HLEM anomaly another 500 meters to the southeast of drill hole PO-6. PO-96-14 intersected the target conductive zone between 68-122 meters downhole at a vertical depth between 55-85m. The HLEM anomaly at this section is comprised of 2-3 07o pyrrhotite and trace chalcopyrite with local 20-30 07o pyrrhotite bands over 0.4 meters hosted by altered mafic and felsic tuffs within the Cormac Volcanic Group. Alteration is intense throughout the drilled section and is comprised mainly of porphyroblastic garnetistaurolite and fine-grained chlorite and biotite. A local section of fractured felsic tuff was mineralized with S-5% chalcopyrite over 0.5 meters. Assays of this section returned a value of 1.2 07o copper, 257 ppm zinc and 18 grams per tonne silver. Assays also indicate that the sulphidized units throughout the entire hole are geochemically enriched in copper up to 1720 ppm copper. This section is very similar in morphology, alteration and sulphide mineralization to that previously intersected in PO-12 and PO-6 along strike to the northeast. PO-12 was collared 300 meters east of PO-6. Assay results of drill core from PO-95-12 indicated a geochemical enrichment of Q.1% copper, 346 ppm zinc and 17.7 grams per tonne silver over 23.3 meters including D.22% copper and 27.8 grams per tonne silver over 8.5 meters. The zone has been tested by 7 drill holes over a strike length of nearly 2 kilometers and a best intersection of 2.09 07o Cu, 32gA Ag over 1.27 meters has been reported from PO-6. No other conductive features remain untested on this horizon and no further drilling is warranted at this time. Downhole PEM surveying is recommended for PO-96-14.

The third drill hole, PO-96-15, was targeted to test multiple conductors within the North Central HLEM anomaly 200 meters northeast along strike from PO-1 at vertical depths of 50, 75 and 175 meters. The first target conductive zone was intersected between 40.8-45 meters downhole at a vertical depth between 30-34m. The HLEM anomaly at this section is comprised of 20-3007o pyrite-pyrrhotite hosted by altered mafic tuffs within the Western Volcanic Group. The second conductive zone was intersected between 62.0-91.1 meters at a vertical depth of 45-70 meters. This zone is comprised of a mixed zone of mineralized felsic tuffs and exhalite near the top of the Central Felsic Group. The unit is very siliceous and is mineralized with 20-30 07o pyrrhotite and lessor pyrite. Three 40 cm. massive sulphide bands are included in this section. The third conductive zone was intersected between 130-176 meters at a vertical depth between 100-130 meters. A number of narrow units of strongly altered (chlorite-amphibole-garnet) felsic crystal tuffs are mineralized with 10-15 07o pyrrhotite±pyrite. Assay results indicate very little copper-zinc geochemical enrichment associated with any of these conductive horizons.

Petrography examinations of thin sections of drill core from PO-96-13 confirm that the rocks are intensely altered and composed essentially of quartz and muscovite with coarse porphyroblasts of staurolite and altered biotite, the latter in places almost completely replaced by chlorite. The presence of 10 07o cordierite was also noted.

There is some definite alkali enrichment (K 2 O*MgO)- depletion (Na 2O-*-CaO) trends from major oxide geochemistry of drill core samples from PO-96-13 and PO-96-14. The sample analysed from PO-96- 14 is near the collar above the target zone between 68-122 meters and is similar to a sample analyzed in PO-95-12 with a high Ishikawa index of 82, both suggesting proximity to massive sulphide mineralization to the north or up-stratigraphy from the South Main HLEM anomaly. Little alteration is indicated from major oxide geochemistry of samples from PO-96-15.

8.0 CONCLUSIONS AND RECOMMENDATIONS

Three drill holes intersected intense chlorite-garnet-staurolitetbiotite alteration mineral assemblages and sulphide zones which range in width from 11 meters up to 66 meters in core width and host semi- massive to massive pyrite-pyrrhotite units that vary from 0.1 meter core thickness to 0.4 meters. No significant copper-zinc mineralization was intersected.

The North Central HLEM anomaly which has a strike length in excess of 8 km has now been drilled tested with 5 DDH's on the Petawanga property spaced approximately 1 km apart on lines 2200W, 3100W, 3300W, 4400W and 5500W. Only DDH PO95-10 on line 4400W has tested a zone of multiple conductive features. The second or central massive sulphide intersection in hole PO-95-10 was the most impressive in terms of VMS textures and morphology. PO-1 on line 3300W was collared within altered felsic stratigraphy and probably overshot the top or first conductive zone. It intersected a 1 meter band of fractured controlled semi massive pyrrhotite hosted by an altered felsic tuff and may also have overshot the second or central massive sulphide horizon. The strongest alteration was intersected on lines 4400W and 5500W and appears that the most intense alteration is spatially associated with the apparent felsic center which lies between lines 3800W and 5700W. Further drill testing is recommended to test this zone on lines 5000W and 3800W on the Petawanga property. HLEM surveying has previously delineated three untested conductive features to the east and along strike with the North Central Exhalite horizon. Drill testing is also recommended for each of these targets on the Discovery Lake Grid (West)-north of the NYLA occurrence, Central Grid Zone, and the T-Bone Lake Grid Zone.

A persistent copper-zinc±silver geochemical enrichment exists within most of the altered stratigraphy intersected along the South Main HLEM anomaly.. The zone has been tested by 7 drill holes over a strike length of nearly 2 kilometers and a best intersection of 2.09 07o Cu, 32g7t Ag over 1.27 meters has been reported from PO-6. No other conductive features remain untested on this horizon and no further drilling is warranted at this time. Proximity to massive sulphide mineralization to the north or up stratigraphy from the South Main HLEM anomaly is suggested from an alkalic enrichment - depletion alteration index of the major oxide geochemistry ((K^O+MgO) l (K 2 CHMgCHNa 2 CHCaO) *100)) for a sample analyzed from PO-96-14

The North Central HLEM conductor has been traced geophysically for over 8 kilometers across the Attwood and adjacent Petawanga properties. A total of seven drill holes have tested this sulphide iron formation/exhalite horizon within the upper portions of the felsic volcanic rocks and intersected massive sulphide zones up to 13 meters in core length with only geochemical zinc enrichment detected to date. Iron formations are spatially and temporally related to several massive sulphide deposits in the world including the "Tetsusekiei" (red chert) at the Fukazawa Mine, a Kuroko - type deposit in Hokuroku, Japan, the Main Contact Tuff at the Millenbach deposit in Noranda and the Key Tuffite at the Matagami deposit, Quebec. These hydrothermal sediments are thought to be analogues of modern metaliferous sediments which were deposited from hydrothermal fluids which vented into a submarine basin. Studies of modern sediments reveal that their bulk geochemical composition vary with distance from the source of the hydrothermal fluids. Geochemical variations (e.g. Au, As, Hg, Bi, Sb, Ba/Ti, Cu+Pb+Zn, Fe/Mn), sulphur and carbon isotope analyses as well as mineral presence or absence (e.g. carbonates) in iron formations can be used to guide exploration by providing effective discriminants to massive sulphide mineralization. It is recommended that future drill hole targeting include the application of iron formation and related hydrothermal sediments geochemistry studies

Respectfully submitted,

NORANDA MINING AMD EXPLORATION INC.

Reg FelixThunder Bay, Ontario Senior Geologist June 4,1996 Western Canada Region

STATEMENT OF EXPENDITURES (MARCH 1 - JUNE 30, 1996)

Drilling Contract Costs———————————————-————-———-S 56,010.97

Assay Costs — -————————————————-————-—~—~— 775.40

Engineering Labour————-—————-———————.—.....—..—— 15,806.53

Mob-Demob —————————————-———-—-—-————.—————-0.00

Transportation (Air, Helicopter, Ground) ————————————————————— 18,851.29

Supplies —————....—.-----—-————---——---.————————4 652 74

Equipment Rental————————————————————————————————————0.00

Food Z Lodging ———————————————————————————2,100.88

GRAND TOTAL———————————————————S 98,197.81

REFERENCES

Felix, R.A.1994: Report of Work, Petawanga Lake Project, N.T.S. 52P/8, For Noranda Mining and Exploration Inc.,

Assessment Work Report, MNDM Thunder Bay, Ontario.

Felix, R.A.1995: Diamond Drilling Report, Petawanga Project, N.T.S. 52P/8, For Noranda Mining and Exploration

Inc., Assessment Work Report, MNDM Thunder Bay, Ontario.

Felix, R.A.1995: Report of Work-1994; Attwood Project, N.T.S. 52P/8, For Noranda Mining and Exploration Inc.,

Assessment Work Report, MNDM Thunder Bay, Ontario.

Felix, R.A. and Petrie L.1995: Report of Geophysical Surveying-1995; Attwood Project, N.T.S. 52P/8, For Noranda Mining and

Exploration Inc., Assessment Work Report, MNDM Thunder Bay, Ontario.

Franklin, J.M.1984. Characteristics of alteration associated with Precambrian massive sulphide deposits. In Volcanic

Rocks, Hydrothermal Alteration, and Associated Massive Sulphide and Gold Deposits: University of Minnesota-Duluth Short Course Notes. Edited by R.L. Morton and D.A. Groves, Duluth, p. 92-105.

Hodges, D.1991: Magnetometer and VLF surveys, Kawitos Lake Area. Falconbridge Internal report, 52/P8 1-3-1.

Hodges, D., and Fournier, J.D.1991: Geology and Geophysical Programs, Ryley Cormac area, August to September, 1990. Falconbridge

Limited Internal Report 52/P8 1-2-1.

Hodges, D.J. and Manojlovic, P.M.1993: Application of lithogeochemistry to exploration for deep VMS deposits in high grade metamorphic

rocks, Snow Lake, Manitoba. Journal of Geochemical Exploration, 48 (1993) 201-224 ElsevierScience Publishers B.V., Amsterdam.

Ishikawa, Y. and Yanagisawa, Y.1974. Geology of the Ainai mine, with special reference to syngenetic origin of the Daikoku deposits. Soc.

Min. Geol. Jpn., Spec. Iss., 6:79-88.

Kalogeropoulos, S. I., and Scott, S. D.1983: Mineralogy and Geochemistry of Tuffaceous Exhalites (Tetsusekiei) of the Fukazawa Mine ,

Hokuroku District , Japan: Econ. Geol. Mon., v.5, p. 412 - 432.

Kalogeropoulos, S. I., and Scott, S. D.1989: Mineralogy and geochemistry of an Archean tuffaceous exhalite: the Main Contact Tuff,

Millenbach mine area, Noranda, Quebec: Can. Jour. Earth Sci. v. 26, p. 88 - 105.

Liaghat, S., and MacLean, W.H.1992: The Key Tuffite, Matagami mining district: Origin of the tuff components and mass changes: Explor.

Mining Jour., v. 1, p. 197-207.

Riverin, G. and Hodgson, C.J. 1980 : Wall rock alteration at the Millenbach Cu-Zn Mine, Noranda, Quebec. Econ. Geol., 75: 424-444.

Severin, P.W.A., and Balint, F.

1985: Geological Setting of the Winston Lake Massive Sulphide Deposit; p. 6-15 in Gold and Copper-Zinc Metallogeny Hemlo-Manitouwadge-Winston Lake, Ontario, Canada, edited by R.H. McMillan and D.J. Robinson, a joint publication of the Geological Association of Canada and the Canadian Institute of Mining and Metallurgy.

Thurston P.C., and Carter M.W.1970 : Operation Fort Hope. Ontario Department of Mines and Northern Affairs, Miscellaneous Paper 42.

Wallace1981 : Geology of the Attwood Lake Area. Ontario Geological Survey Report 203

10

APPENDIX l

Diamond Drill Logs

PROPERTY: PETAWANGAHOLE No.: P096-13Collar Eastings: -5500.00Collar Northings: -250.00Collar Elevation: 0.00Grid: AUGER LAKEBASELINE AZIMUTH IS AT 030 DEGREES

NORANDA MINING St EXPLORATION INC.

DIAMOND DRILL LOG

Collar Inclination: -50.00 Logged by: R FELIX Grid Bearing: 180.00 Date: MARCH,1996 ' '- ' Final Depth: 134.00 metres Down-hole Survey: ACID TO TEST HLEM ANOMALY AT 50-75 M VERT.DEPTHCORE SIZE BGBDM: DRILLED BY W.G. CLAIM NUMBER: 1173499; CORE STORED AT AUGER LAKE

LANG

FROM TO UTHOLOGICAL DESCRIPTION

O 9.1 (LAKEWATER)

FROM TO

ASSAYS WIDTH Cu(ppm) Zn(pcm) Ag(ppm)

9.1 19.4 (OVERBURDEN)

19.4 76.0 (MAFIC METAVOLCANIC)

- very fine grained to medium grained- grey green to green- massive to finely banded- comprised essentially of hornblende and feldspar- massive pillowed flows at: 24-26.5m, 29.5-37.8m, 41-53.7m- finely foliated to banded mafic tuffs at 19.4-24.Om, 26.5-29.5m, 37.8-41m, 53.7-56.1m, 69-76m- core samples: 21m - 40 deg to CA- 29m - 10 deg to CA- 40m - 40 deg to CA- 54m - 35 deg to CA- 58m - 45 deg to CA- characteristic weak to moderate chlorite alteration with intense chlorite- garnet alteration between 69-76m; porphroblastic garnet clusters and bands up to 3cm in size- moderate biotite alteration occurring as 1-2cm biotite-rich bands between 19.4-20m- frequent anastomising quartz-feldsparV-carbonate veining/fracture

HOLE No: PO96-13

NORANDA MINING S EXPLORATION INC.

DIAMOND DRILL LOGPROPERTY: PETAWANGA HOLE No.: P096-13 Page 2

FROM TO LITHOLOGICAL DESCRIPTION

filling- intense carbonate-chlorite alteration near end of section- bull quartz veining at 46.9-47.0, 59.3-60.0; nonmineralized except for occasional specks of pyrite- intense fracturing noted between 19.4-24.0; 69.8-76.0; possible fault gouge tt 71.4m- medium to coarse grained mafic tuffs noted at 56.1-59.3 and 60-69; very finely foliated at 40-45 deg to CA with characteristic 1-2im lithic fragments- mineralized with trace of 1-2mm blebs of pyrite, occasional specks of chalcopyrite- at 69-76m section is mineralized with 3-5X fine disseminations and bands of pyrite locally up to 5-10X over narrow intersections

76.0 90.6 (FELSIC METAVOLCANICS)

Altered Felsic Tuff76.0-79.2 - very fine grained, grey-white to grey to grey-green in colour

- finely foliated at 45 deg to CA- weakly garnetiferous with 3-5X pinhead garnetsoccasional coarse grained quartz-feldspar-garnet-cMoritesegregationsnear top of sectionweakly mineralized with 1-2X fine wisps and hairline bandsof pyrite

Chlorite Schist/Breccia79.2-81.5 - very fine grained, black, with frequent bull white quartz veining

TOASSAYS

WIDTH Cu(ppm) Zn(ppm) Ag(ppm)

7677788081838486878981

.00

.00

.50

.00

.50

.00

.50

.00

.50

.00

.50

7778808183848687899090

.00

.50

.00

.50

.00

.50

.00

.50

.00

.60

.60 S

.00

.50

.50

.50

.50

.50

.50

.50

.50

.60(.10

3461488010210185941109697

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.978

628219626

3272022923683391112447

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.385

11222222222

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

HOLE Mo: P096-13




and breccia fragments- finely foliated at 45-50 deg to CA- characteristic bands and siliceous 'cherty' fragments ^lcm wide- mineralized with 10-15X bands and blebs of pyrite

Banded Felsic Tuff- 81.5-90.6 - very fine grained, grey-green- finely foliated at 45 deg to CA- moderate chlorite alteration- frequent bull white to greenish white quartz bandingV-pyrite ^3cm thick parallel to foliation- local section of intense brecciation with quartz-chlorite*7-graphite in anastomising style fractures- mineralized with 10-15X pyrite and occasional blebs, 1-3mm, and narrow veinlets of chalcopyrite+X-sphalerite between 88.1-90.6m

90.6 105.0 (INTERBANDED ARGILLITES/CHLORITE-GRAPHITE SCHISTS)

- unit is very fine grained, well banded and black and grey; locallygraph i t i c90.6-100.3 - section is mainly banded argillite* at 40 deg to CA- frequent anastomsing hairline fractures mineralized with quartz- mineralized with 20-25X blebs and bands <-1cm wide of pyrite 100.3-105.0 - section is strongly graphitic and rock is extremely soft, fault gouge- approximately 1.5-Z.Om of lost core

105.0 111.5 (EXHALITE)

FROMASSAYS


90919294959798100

102105

.60

.30

.80

.30

.80

.30

.80

.30

.00

.70

91.92.94.95.97.98.100.102.

105.106.

308030BO30803000

70 :40

).70.50.50.50.50.50.50.70

1.70).70

64.90.90.72.79.58.23.47.

26.125.

000000000000000000000000

000000

723380

2442761395563

17864

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000'.000.000.000.000.000.000'.000

'.000'.000

HOLE No: P096-13

NORANDA MINING S, EXPLORATION INC.

DIAMOND DRILL LOG

APROPERTY: PETAWANGA HOLE No.: P096-13 Page 4

FROM LITHOLOGICAl DESCRIPTION FROM

section is a mixed zone of interbanded argillites with 106.40 chlorite-pyrite 108.00 schists, chert, felsic tuff breccia and narrow massive sulphide 109.50 bands 110.50 105.0-108.0 - section is mineralized with 20-25X pyrite- pyrrhotite as sulphide clasts and balls, ^cm, and wisps- occasional blebs and wisps of chalcopyrite e.g. 106.4 with massive pyrite-pyrrhotite band between 105.7-105.8108.0-111.5 - section is grey-white, very fine grained and very siliceous becoming more chloritic and black near end of section- mineralized with 25X bands and blebs to semi-massive pyrite-pyrrhotite; local massive pyrite-pyrrhotite band at 110.4-110.5

TO

108.00109.50110.50111.50

ASSAYS WIDTH Cu(ppm) Zn(ppm) Ag(ppm)

1.601.501.001.00

58.00067.00072.00058.000

512.00061.00094.000323.000

2.0002.0001.0002.000

111.5 112.7 (ALTERED FELSIC TUFF) 111.50 112.50 1.00 39.000 88.000 1.000

- orey to grey-green, strongly foliated with weak to moderate chlorite alteration- fine beds, 1-2mm thick- mineralized with 3-5X finely disseminated pyrite-pyrrhotite

112.7 116.7 (BIOTITE-STAUROLITE SCHIST/FELSIC TUFF)

- very fine grained, grey, finely foliated and banded at 50 deg to CA- characteristic porphroblastic subhedral staurolite crystals ^0.5 cm in size and black biotite clumps ^O.Scm- section is very siliceous and typical of a felsic tuff

HOLE Mo: PO96-13

PROPERTY: PETAWANGA HOLE No.: PO96-13


DIAMOND DRILL LOG

Page 5

FROM TO LITHOLOG1CAL DESCRIPTION FROM

116.7 121.7 (GARNET-STAUROLITE SCHIST/FELSIC TUFF)

- very fin* grained, grey, finely foliated, porphroblastic, very siliceous- characteristic porphroblasts •M.Scm in size of euhedral to subhedralgreenish-grey garnet?? crystals and ^O.Scm yellow-brown staurolitecrystals116.7-117.3 - finely bedded felsic tuff

121.7 134.0 (STAUROLITE-BIOTITE-GARNET QUARTZ EYE TUFF)

- very fine grained, grey, finely foliated at 50 deg to CA, very s i l i ceous- characteristic black subhedral to euhedral biotite and yellow-brown staurolite porphroblasts ^3mm is size- some faint "ghost-like" garnet pseudomorphic porphroblasts- occasional specks and blebs of pyrite

TOASSAYS

WIDTH Cu(ppm) Zn(ppm) AgCppm)

134.0 EOH

DOWN-HOLE SURVEY DATA

DEPTH INCLINATION BEARING

134.00 -40.00 180.00

HOLE Mo: P096-13

PROPERTY: PETAWANGAHOLE No.: PO96-14Collar Eastings: -5100.00Collar Northings: -1575.00Collar Elevation: 0.00Grid: SOUTH AUGERCORE SIZE : BGBDM; DRILLED BY W.G LANGLEY


DIAMOND DRILL LOG

Collar Inclination: -50.00 Logged by: R FELIX . ,Grid Bearing: 180.00 Date: MARCHll996 ''"^ '"Final Depth: 152.10 metres Down-hole Sdrvey: ACIDTO TEST HLEM ANOMALY AT 50 -75M VERT.DEPTHBASELINE AZIMUTH IS 020 DEGREESCLAIM NUMBER:1165269: CORE STORED AT AUGER LAKE

FROM TO LITHOLOGICAL DESCRIPTION FROM TOASSAYS



2.5 21.3 (MAFIC METAVOLCANIC FLOUS)

- fine grained to medium grained, green, finely foliated to banded at 50 deg to CA- frequent chlorite-epidote banding at 30 deg to CA- mainly flows with lessor tuffs- localized sections of intense chlorite-garnet alteration; garnets are porphroblastic up to 1cm in size; typical light green fibrous actinolite crystals noted e.g. 13- 18m- occasional weak pyV-po mineralization up to 3X- occasional narrow felsic bands with 3-5X wisps and blebs of pyrrhotite e.g. 5.5m

21.3 35.4 (FELSIC QUARTZ EYE TUFF)

-fine grained to medium grained, grey to grey-green to pink and green-comprised essentially of quartz feldspar, biotite, garnet and chlorite- finely foliated, occasionally banded at 40 deg to CA- characteristic 2-4mm size smoky grey to blue subhedral to euhedral quartz eyes

21.3023.0024.5026.0027.5029.0030.5032.0033.50

23.0024.5026.0027.5029.0030.5032.0033.5035.40

.70 1760.000

.50 1184.000

.50 664.000

.50 480.000

.50 880.000

.50 18.000

.50 504.000

.50 400.000

.90 343.000

143.00071.00050.00014.00010.0008.000

20.0009.000

67.000

5.0004.0002.0002.0003.0002.0004.0002.0003.000

HOLE No: P096-14




-frequent intensely altered sections with typical green chlorite and pink porphroblastic garnets up to 2cm in size- intense garnet-chlorite sections at 21.3-24.5, 30.3--occasional blebs and wisps of chalcopyrite at: 22.6m, 23.3m, 23.5m, 25.3m,25.6m, 27.7m, 28.2m, 28.5m, 30.7m, 32.0m, 33.2m chalcopyrite frequently occurs in fractures and associated with narrow quartz veinlets

35.4 38.2 (MAFIC METAVOLCANIC FLOWS)

- very fine grained, dark green, and frequently banded at 40 deg to CA; top meter exhibits strong chl-biotite alt.- probably a pillowed flow unit- minor disseminated py-po

38.2 41.0 (QUARTZ FELDSPAR PORPHYRY)

- white, very fine grained, siliceous, with 2-4mm subhedral to euhedral feldspar phenocrysts; composed of qtz-feldspar-biotite- massive to weakly foliated, conformable contacts suggest synvolcanic high level Intrusion

41.0 46.8 (MAFIC TUFF/DYKE)

- medium grained, dark green to greenish black, massive to weakly foliated- weak banding at 40 deg to CA- mottled texture comprised essentially of white fine grained feldspar

ASSAYS FROM TO WIDTH Cu(ppm) Zn(ppm) Ag(ppm)

21.30 35.40 14.10 697.780 45.631 3.028

HOLE No: TO96-14


DIAMOND DRILL LOG PROPERTY: PETAWANGA HOLE No.: PO96-14 Page

ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION FROM TO WIDTH Cu(ppnt) Zn(ppm) Ag(ppm)

and medium grained phyric amphibole and very fine grained amorphous chlorite


- very fine grained, green, massive to banded at 50 deg to CA- characteristic brownish fine grained biotite-rich bands/selvages

53.6 56.8 (MODERATELY ALTERED FELSIC TUFF)

- fine grained, grey-green to grey to brown- comprised essentially of biotite-feldspar and 1-2mn siie quartz eyes- characteristically banded with brown biotite-rich bands and lapilli ^1cm thick by 4cm long and green chlorite bands- banding it 60 deg to CA- altered with epidote, chlorite and pink garnet prophroblasts, 20-25X, becoming larger to 2cm down sections

56.8 63.2 (MAFIC TUFF/DYKE)

- same as 41-46.8- phyric amphibole 'blasts' in a green chloritic matrix- trace to 1X disseminated pyV-po

63.2 68.0 (INTENSELY ALTERED FELSIC TUFF) 63.20 65.00 1.80 576.000 86.000 3.00065.00 66.50 1.50 408.000 74.000 2.000

- similar to 21.3-35.4 and 53.6-56.8 66.50 63.00 1.50 656.000 70.000 3.000-very fine grained, grey-green to pink and green nith 63.20 68.00 4.80 548.500 77.250 2.688

HOLE No: P096-14




porphroblasticgarnetsVskeletal staurolite pseudomorphs <-2cm in size- some sections with phyric 'actinolite?' crystals ^5mm long within an epidote rich matrix- minor specks and blebs of chalcopyriteV-pyrite noted in more siliceous bands/veinlets at 54.0, 64.3, 64.7, 67.0, 67.5, 67.7 and 68 meters 67.5-68.0 - 2-3X blebs and wisps of pyrrhotite


- massive to pillowed, very fine grained, green with biotite-rich tuffs/ epiclastic tuffs at 70.7-71.3- spotted mafic tuffs/dyke like before 71.3-72.0

73.2 78.8 (INTENSELY ALTERED FELSIC TUFF)

- fine grained, grey, finely foliated at 60 deg to CA- similar to previous section between 63.2-68.0 with fine 1-2mm anhedral quartz eyes, but more biotitic; intense garnet, 30-40X ^1.5cm porphroblasts-chlorite alteration between 73.5-78.0 77.7-78.7 - 3-5X finely disseminated pyrrhotite; minor alcopyrite at 78.4

78.8 96.3 (ALTERED MAFIC TUFF)

very fine grained, green to grey-green with frequent brownish biotitic bands at 60 deg to CA- local blebs and narrow veinlets of pyrrhotite OX

FROM

73.2074.7076.2077.70

74.7076.2077.7078.80


1.50 22Z.OOO 45.000 2.0001.50 14.000 24.000 2.0001.50 904.000 148.000 4.0001.10 608.000 210.000 4.000

7880818386

.80

.30

.80

.30

.60

BO.81.83.84.87.

3080308000

11110

.50

.50

.50

.50

.40

240248104176912

.000

.000

.000

.000

.000

64.46.52.44.

192.

.000

.000

.000

.000

.000

33227

.000

.000

.000

.000

.000

HOLE No: P096-14


DIAMOND DRILL LOG PROPERTY: PETAWANGA HOLE No.: P096-14 Page 5

ASSAYS

FROM TO UTHOLOGICAl DESCRIPTION FROM TO WIDTH Cu(ppm) Zn(ppm) Ag(ppm)

80.3-84.8 - 3-5X disseminated pyrrhotite; local wisps and blebs 73.20 87.00 13.80 282.290 68.283 2.478 of 5-10X pyrrhotiteV-pyrite along siliceous fractures and 92.10 93.60 1.50 224.000 116.000 2.000 veinlets, trace chalcopyrite 93.60 94.00 0.40 688.000 286.000 3.000- two narrow banded pyrrhotite sections noted at 86.6-87.0 and 94.00 95.50 1.50 114.000 183.000 2.000 93.6-94.Om comprised of 20-30X pyrrhotite+X-pyrite and minor 92.10 95.50 3.40 230.059 165.559 2.118 chalcopyrite-intense biotite-chlorite-porphroblastic garnet sections exhibited between 87.2-88.5 and 91.8-96.3m

96.3 98.7 (MAFIC HETAVOLCANICS)

- very fine grained, green, massive to pillow flows

98.7 100.6 (WEAKLY ALTERED FELSIC TUFFS)

- fine grained, grey, banded at 30-40 deg to CA- characteristic biotite-rich bands- irregular contact with overlying mafic metavolcanics- probably speclastic- weakly mineralized with 2-3X finely disseminated pyrrhotite

100.6 101.2 (MAFIC METAVOLCAMIC)

- very fine grained, green and finely banded at 30 deg to CA

101.2 104.3 (QUARTZ FELDSPAR PORPHYRY)

- same as section higher up in the hole between 38.2-41.0

HOLE No: P096-14



ASSAYS


104.3 116.6 (ALTERED MAFIC TUFFS)

- fine grained to medium grained, characteristically banded withbiotite-rlch layers at 60 deg to CA- Intense porphroblast ic garnet alteration between 105. 5-115. 7m- local 15-20X pyrrhotite-rich sections between 111.0-111.1 and1U.5-W.8m- 15-20X pyrrhotite with 2-3X chalcopyrite noted between 115.2-115.5m

116.6 120.0 (INTENSELY ALTERED FELSIC TUFF)

very fine grained, grey, very siliceous with characteristicbiotite-rlch lapilli and bands- banding at 60-70 deg to CA- intensely porphroblast ic garnet alteration <•\cm In size Vstaurolite, mineralized with 2-3X disseminated pyrrhotite.trace chalcopyritebetween 118.6-119.1 including a fracture controlled band ofmassive chalcopyrite between 118. 6- 118. 9m

120.0 124.4 (ALTERED MAFIC TUFF)

- same as before, green with brownish-black biotite banding at60 deg to CA120.8-123.0 - Intense garnet-chlorite altered section with garnet

FROM

110.

111.

113.1U.115.

116.

117.

118.119.

120.120.122.21.123.

00

50005050

6060

6010

0080103000

TO

111.50113.00114.50115.50116.60

117.60118.60119.10120.00

120.80122.10123.00123.00124.40

WIDTH

1

1

1

1

1

1

1

00

010

1011

.50

.50

.50

.00

.10

.00

.00

Cu(ppm)

260156109

1192

.000

.000

.000

.000

171.000

78260

.5012000

.90

.80

.30

.90

.70

.40

337

148324nw270173

.000

.000

.000

.000

.000

.000

.000

.319

.000

Zn(ppm)

113.35.45.95.172.

58.112.257.101.

77.78.92.36.48.

000000

000

000000

000000000000

000000000660000

Ag(ppni)

22232

.000

.000

.000

.000

.000

2.000

218

2

22312

.000

.000

.000

.000

.000

.000

.307

.000'blasts' ^3cm in size122.1-122.2 - patchy 3-5X pyrrhotite and 1-2X chalcopyritemineralization

HOLE No: P096-14

NORANDA MINING S EXPLORATION INC. S \

DIAMOND DRILL LOG PROPERTY: PETAWANGA HOLE No.: PO96-14 Page 7

^ ——— ....... ——— .v^..^———..——— -.~ ——— —————— ——— ..——— ——— -. VH ..~ ——— —————— ... Hnv ——— . ——— .. ——— v.......——— ——— ...WVH WW——— ——— ——— -.~——— ̂ ™ ——— ——— MM.——— ——— ——— ——— ™^M.. ——— ———™^——.-. —— ——— ™——— ——— ——, ——— ——— ™. ——— ——— ^.—— ——— ——— ——— ——— ——— ——— ——— ——— .^ —— ——— ——— —— ——— ——— ——— —— —————— ——— ——— ——— —— ——— —— ——— ——— —— ——— ——— ———

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION FROM TO WIDTH Cu(ppm) Zn(ppm) Ag(ppm)

124.4 132.4 (OUARTZ EYE FELSIC TUFF)

- very fine grained, grey, siliceous, comprised of finely foliated quartz-feldspar-biotite at 60 deg to CA- characteristic occasional blue quartz eyes 2-3mm in size- also occasional garnet 'blasts' and 1X pyrrhotite


- interbanded very fine grained, massive to pillowed flows and fine grained to medium grained tuffs and biotite-rich and tuffs as before- porphroblastic garnets from 139.4 to end of section

152.1 EOH



100.00 -43.00 180.00

152.10 -39.00 180.00

HOLE Mo: P096-14

PROPERTY: PETAWANGAHOLE No.: P096-15Collar Eastings: -3100.00Collar Northings: 525.00Collar Elevation: o.ooGrid: DISCO LAKECORE SIZE :BGBDM; DRILLED BY W.G. IANGLEY

NORANDA MINING d EXPLORATION INC.

DIAMOND DRILL LOG

Collar Inclination: -50.00 Logged by: R FELIX Grid Bearing: 180.00 Date: MAY,, 1966 Final Depth: 200.00 metres Down-hole Survey: ACID To test HLEM cond. at a vert.depth from 25 to 125mBaseline Azimuth is 070 degre Claim Numbers: 1165263, 1149125

FROM TO UTHOLOGICAL DESCRIPTION


1.5 56.0 (MAFIC METAVOLCANICS)

FROM

40.80

42.30

43.801.5-36.0 - fine grained to very fine grained, green to dark green,composed essentially of hornblende and feldspar, well bandedat 60 deg to CA,

frequent white quartz banding e.g. at 6.7-7.7, 9.2-9.5, 10.5-10.6,H. 9-15.3m36.0-56.0 - fine foliated mafic tuffs, fine grained, grey-green with frequentpatchy brownish biotite alteration; includes a banded sulphide iron formationwith 20-30X pyrite-pyrrhotite with siliceous fragments ^2cm between40.8-45.Om

- foliation at 50 deg to CA

56.0 62.0 (BEDDED FELSIC TUFFS)

fine grained, grey-black to greenish-grey, characteristically siliceous and chloritic with 2-3X pinhead garnets; bedded at 50 deg to CA; occasional quartz-feldspar pegmatoids

62.0 91.1 (MINERALIZED FELSIC TUFFS/EXHALITE)

-mixed lone of felsic tuff breccias felsic flows, cherty felsic

59.0060.50

62.0063.5065.00

42.3043.8045.30

60.5062.00

63.5065.0065.40


154.000144.000126.000

1.501.50

1.501.500.40

100.000161.000114.000

25.000 74.00037.000 118.000

100.00034.000

304.000

704.000261.00059.000

4.0003.0003.000

1.0002.000

2.0002.0006.000

HOLE No: P096-15



FROM TO L1THOLOGICAL DESCRIPTION

tuffs end banded pyrrhotite with local massive pyrrhotite* pyrite bands; also characteristic frequent dark green magnetite-amphibole-chlorite bands up to 4cm wide throughout; bandingat 50 deg to CA-unit is very siliceous composed mainly of phyric quartz with20-30X pyrrhotite, minor pyrite, also 10-15X garnets occurringas banded clusters up to Urn wide with dark green chlorite-amphibole bands-massive pyrite bands at 65-65.4, 67.8-68.2 and 72. 7-73. 1m at50 deg to CA

91.1 112.5 (STRONGLY ALTERED FELSIC TUFFS)

•quartz, phyric rock, grey-blue, very fine grained, shows weakclastic texture and lapilli sized to tuff breccia sized quartzphenocrysts/fragments-groundmass of least altered section of the unit are quartzo-

FROM

65.40 66.906768697172737476777980828385868889

919294959798

.80

.20

.70

.20

.70

.10

.60

.10

.60

.10

.60

.10

.60

.10

.60

.10

.60

.10

.50

.00

.50

.00

.50

TO

66.90 67.806869717273747677798082838586888991

9294959798100

.20

.70

.20

.70

.10

.60

.10

.60

.10

.60

.10

.60

.10

.60

.10

.60

.10

.50

.00

.50

.00

.50

.00

WIDTH

1.50 0.900.401.501.501.500.401.501.501.501.501.501.501.501.501.501.501.501.50

1.401.501.501.501.501.50

ASSAYS Cu(ppm)

84.000 86.000294.000645214213493449366943848965863228102

7241492314932

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

Zn(ppm)

74.000 64.0005022182964597577677072384434283334

5646663989106

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

Ag(ppm)

3.000 3.00062447434343333244

323232

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000feldspathic with 20-25X biotiteV-chlorite; biotite and chloritedefine the foliation at 70-75 deg to CA-unit is similar to above except not as strongly mineralized

HOLE Ho: P096-15



FROM TO L1THOLOGICAL DESCRIPTION

with sulphides 5-10X pyrrhotite with local blebs and bands and narrow streaks from 91.1-100m generally associated with chlorite- garnet altered section- alteration Is moderate to locally intense banded, mm up to 30mm, pervasive chlorite, 20-45X, garnet 5-35X, and magnetite •OX; the bands make up 25-30X of unit and sometimes exhibit an anastomosing character. Chlorite Is probably retrograde hornblende. Garnet is porphroblastic and found within the chlorite sections- occasional pegmatite veins, course grained, white to orange, eg. 105-105.5m

112.5 210.0 (ALTERED FELSIC CRYSTAL TUFF)

quartz+feldspar phyric, very siliceous, light grey to grey- green, very fine grained with characteristic 5-10X, 2-3mn white feldspar phenocrystsunit is still chlorite-garnet banded with 30-40X of the unit as patchy and banded chlorite-garnet alteration the groundmass still quartzo feldspathic with biotite 15-20X; alterationis similar in character and intensity to the above unit strongly chlorite-amphibole-flarnet section are as follows: 112.5-122.38, 130.5-133.5, 137.5-K3.3, H9.3-168.0, 173.5-182.6- foliation varies as follows: 115m - 50 deg to CA 120m - 50 deg to CA 130m - 45-50 deg to CA HOm - 75-80 des to CA

FROMASSAYS


129.80131.30132.80138.50HO. 00142.70U9.50151.00152.50154.00155.50157.00158.50160.00161.50163.00164.50166.00

131.30132.80134.30140.00141.50144.20151.00152.50154.00155.50157.00158.50160.00161.50163.00164.50166.00167.50

1.501.501.501.501.501.501.501.501.501.501.501.501.501.501.501.501.501.50

123.00097.00087.00064.00050.00018.00076.00051.00073.00039.00016.00053.00035.00034.00026.00011.00027.00015.000

40.00047.00037.00036.00036.00037.00067.00039.00055.00054.00042.00044.00031.00036.00042.00044.00035.00033.000

3.0003.0003.0003.0002.0002.0003.0002.0003.0002.0002.0003.0002.0002.0002.0002.0002.0002.000

HOLE Mo: PO96-15



FROM LITHOLOGICAL DESCRIPTION

150m - 55 deg to CA160m - 55 deg to CA200m - 50 deg to CAoccasional coarse grained pegmatite veins it 113.8-115.4m,126.5-126.9m, 135.2-135.7m, 144.7-145.5mpyrrhotfte+X-pyrite occurs as scattered blebs bands and itreaksthroughout, but becomes more concentrated up to 10-15X in thedark green chlorite-oarnet-amphibole bands at: 130.8-131.8,132.8-133.5, 138.3-H1.8, 142.7-158.5, 164.5-16735, 174.0-175.5

210.0 EON



100.00 -43.00 180.00

150.00 -42.00 180.00

200.00 -40.00 180.00

TOASSAYS


167169170172174

.50

.00

.50

.00

.00

169170172174175

.00

.50

.00

.00

.50

1.501.501.502.001.50

54222010

103

.000

.000

.000

.000

.000

28.00033,25,55.25.

.000

.000

.000

.000

3.0002.0002.0002.0003.000

HOLE No: P096-15

APPENDIX II Geochemical Analyses, Analytical Procedures

Chemex Labs Ltd,Analytical Chemists * Geochemists * Registered Assayers

5175 Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: NORANDA MINING AND EXPLORATION INC.

960 ALLOY DRIVE THUNDER BAY, ONTARIO P7B 6A4

Comments: ATTN: REG FELIX

A9619717

CERTIFICATE A9619717

(BUF ) - NORANDA MINING AND EXPLORATION INC.

Project: 327 P.O. #:

Samples submitted to our lab in Vancouver, BC. This report was printed on 17-JUN-96.

SAMPLE PREPARATION

CHEMEXCODE

208226

3202238

NUMBERSAMPLES

8888

DESCRIPTION

Assay ring to approx 150 mesh0-3 Kg crush and splitRock - save entire rejectNitric-acjua-regia digestion

CHEMEXCODE

902906

2590903908905

1989907909901904910

2540289120672898297329782974

25

NUMBERSAMPLES

888888888888888888888

ANALYTICAL

DESCRIPTION

A1203 Hi XRFCaO Hi XRFCr2O3 Hi XRFFe203 Hi XRFK20 Hi XRFHgO Hi XRFMnO Hi XRFNa20 Hi XRFP205 Hi XRFSiO2 Hi XRFTiO2 Hi XRFLOI Hi XRFTotal HBa ppmt XRFRb ppmi XRFSr ppmt XRFMb ppmt XRFZr ppmi XRFY ppmi XRFCu ppmi HNO3-aqua regia digestZn ppmi HHO3-aqua regia digest

PROCEDURES

METHOD

XRFXRFXRFXRFXRFXRFXRFXRFXRFXRFXRFXRFCALCULATIONXRFXRFXRFXRFXRFXRFAASAAS

DETECTIONLIMIT

0.010.010.010.010.010.010.010.010.010.010.010.010.01

s1223211

UPPERLIMIT

100.00100.00100.00100.00100.00100.00100.00100.00100.00100.00100.00100.00105.0050000500005000050000soooo500001000010000

Chemex Labs LtdAnalytical Chemists" Geochemists * Registered Assayers

5175Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163



Project: 327Comments: ATTN: REG FELIX

Page Number : 1-A Total Pages : 1 Certificate Date: 17-JUN-9G Invoice No. : 19619717 P.O. Number : Account : BUF

CERTIFICATE OF ANALYSIS A961 971 7

SAMPLE

P096-13-112.5P096-13-115.5P096-13-119P096-13-133P096-14-14

P096-15-60P096-15-160P096-15-120

PREPCODE

208208208208208

208208208

226226226226226

226226226

A1203 *,XRF

19.6220.7219.5322.3014.70

14.6213.3213.89

CaO \XRF

0.681.260.690.731.44

3.464.435.04

Cr203 \XRF

0.030.030.040.030.04

0.030.030.04

Fe203 \XRF

4.425.745.575.76

20.44

3.9614.7713.09

K20 \XRF

4.293.11-3.433.390.96

2.302.191.20

MgO \XRF

1.912.332.442.666.54

1.251.541.49

MnO \XRF

0.050.070.070.070.08

0.090.750.65

Na20 \XRF

2.371.902.231.330.25

3.042.303.22

P205 \XRF

0.110.120.120.120.10

0.090.080.10

Si02 \XRF

61.3761.3761.2159.6651.17

69.1958.9459.98

Ti02 *.XRF

0.630.710.650.761.43

0.370.510.55

LOI *XRF

3.752.043.762.302.07

0.760.180.15

TOTAL*

99.2399.4099.7499.1199.22

99.1699.0499.40

Bappm

605685540580100

360410330

CERTIFICATION:

Chemex Labs Ltd,Analytical Chemists' Geocheinists" Registered Assayers

5175 Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163



Project: 327Comments: ATTN: REG FELIX

Page Number : 1-B Total Pages : 1 Certificate Date: 17-JUN-96 Invoice No. : 19619717 P.O. Number : Account : BUF

| CERTIFICATE OF ANALYSIS A9619717

SAMPLE

P096-13-112.5P096-13-115.5P096-13-119P096-13-133P096-14-14

P096-15-60P096-15-160P096-1S-120

PREPCODE

208208208208208

208208208

226226226226226

226226226

RbPpm

14010813611424

926032

Srppm

132182152134< 2

96146216

Nbppm

810

810

2

846

Zrppm

144141135147

87

129120120

yppm

2222202212

81414

CUppm

40464941

125

188017

Znppm

99189673

310

405938

CERTIFICATION:

5 1996

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448FAX (807) 623-6820

Page l

NORANDA MINING AND EXPLORATION INC, 960 ALLOY DRIVE THUNDER BAY, ONTARIO P7B 6A4

ATTENTION: R. FELIX

Accurasssa\f#123456789

10111213141516171819202122232425

SAMPLE #r Customer96- 13-

76.0 to 77.077.0 to 78.578.5 to 80.080.0 to 81.581.5 to 83.083.0 to 84.584.5 to 86.086.0 to 87.587.5 to 89.089.0 to 90.690.6 to 91.391.3 to 92.892.8 to 94.394.3 to 95.895.8 to 97.397.3 to 98.898.8 to 100.3100.3 to 102102 to 105.7105.7 to 106.4106.4 to 108.0108.0 to 109.5109.5 to 110.5110.5 to 111.5111.5 to 112.5

Zincppm

6282

19626

327202292368339

1112723380

2442761395563

17864

5126194

32388

Silverppm

1122222222121111

^122222121

March 26, 1996

Job* 964376

Project* 327P.O. # TB No. 11050

Copper ppm

1122222222121111:122222121

34614880

1021018594

11096649090727958234726

1255867725839

Certified By:

f l 1996



PHONE (807) 623-6448p eFAf( (807) 623-6820

NORANDA MINING AND EXPLORATION 960 ALLOY DRIVE THUNDER BAY, ONTARIO P7B 6A4

ATTENTION: R. FELIX

SAMPLE # Accurassay Customer

123456789

1011121314151617181920212223242526272829

P096-14-21. 3-23.0P096-14-23.0-24.5PO96-14-24. 5-26.0P096-14-26.0-27.5PO96-14-27. 5-29.0PO96-14-29.0-30.5P096-14-30. 5-32.0P096-14-32.0-33.5PO96-14-33.5-35.4PO96-14-63. 2-65.0P096-14-65.0-66.5PO96-14-66. 5-68.0PO96-14-73.2-74.7PO96-14-74.7-76.2PO96-14-76.2-77.7PO96-14-77.7-78.8PO96-14-78.8-80.3P096-14-80.3-81.8P096-14-81.8-83.3P096-14-83.3-84.8P096-14-86. 6-87.0PO96-14-92.1-93.6P096-14-93. 6-94.0P096-14-94.0-95.5P096-14-110. 0-111.PO9 6 -14 -111. 5 -113.P096-14-113. 0-114.P096-14-114. 5-115.PO96-14-115. 5-116.

50556

Copper ppm

1720118466448088018

50440034357640865622214

904608240248104176912224688114260156109

1192171

April 12, 1996

Job# 964459

Project # 327-111 P.O. # 10893

Silver

54223242332322443322723222232

Certified By: JLJPA



PHONE (807) 623-6448(807) 623-6820


ATTENTION: R. FELIX


3031323334353637

PO96-14- P096-14- PO96-14- PO96-14- PO96-14- PO96-14- PO96-14- PO96-14-

116.6117.6118.6119.1120.0120.8122.1123.0

•117.6•118.6•119.1•120.0•120.8•122.1•123.0•124.4

Copper ppm

78 260

;*10,000 337 148 324

1104 173

April 12, 1996

Job* 964459

Project # 327-111 P.O. # 10893

Silver ppm

22

1822232

Zinc ppm

5811225710177789248

Certified By:

J(JL l l 1936

ACCURASSAY LABORATORIES1070 LITHIUM DRIVE, UNIT 2

THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 623-6448

FAX (807) 623-6820

Page l


ATTENTION: R. FELIX


123456789

1011 Check12131415161718192021 Check2223242526272829

PO96-15 PO96-15 PO96-15 PO96-15 PO96-15 PO96-15 PO96-15 P096-15 PO96-15 PO96-15 P096-15 PO96-15 P096-15 PO96-,15 PO96-15 PO96-15 PO96-15 P096-15 PO96-15 PO96-15 PO96-15 PO96-15 P096-15 PO96-15 P096-15 PO96-15 PO96-15 P096-15 P096-15

5-

0-

9-

40.842.3•43.8•59.0•60•62.0•63.5•65•65.4•66.9•66•67.8•68.2•69.7•71.2•72•73.1•74.6•76.•77.6•77.6•79•80.6•82.1•83.6•85.1•86.6•88.1

7-

1-

1-

42.343.845.360.562.063.565.065.466.967.867.868.269.771.272.773.174.676.177.679.179.180.682.183.685.1

May 21, 1996

Job* 964637

Project # 327-111 P.O. # 11652

86.61-88,

-89.6 -89.6-91.1

Goldppb

<56

c5^^8^10<56878

19349

101262873^21^<5<56

<5^^^

GoldOz/t

^.001*:0.001^.001•sO.OOl^.001•cO.OOllO.OOl^.001*:0.001^.001^.001.cO.OOl^.0010.0060.0010.003^.001^.0010.002

.cO.OOl^.001^.001^.001^.001^.001*:0.001*:0.001^.001<0.001

Certified By:

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES /\'C.


PHONE (807) 623-6448FAX (807) 623-6820

Page 2


ATTENTION: R. FELIX


303132333435363738394041424344454647484950515253545556575859606162

P096Check PO96

PO96PO96PO96PO96P096P096P096PO96P096

Check PO96P096P096P096PO96PO96PO96PO96PO96PO96

Check P096PO96P096P096P096PO96P096PO96P096P096

Check P096PQ96

•15-91.•15-91.•15-92.•15-94.•15-95.•15-97.•15-98.•15-129•15-131•15-132•15-138•15-138•15-140•15-142•15-149•15-151•15-152•15-154•15-155•15-157•15-158•15-158•15-160•15-161•15-163•15-164•15-166•15-167•15-169•15-170•15-172•15-172•15-174

,0 ,5

1-92.51-92.55-94.00-95.55-970-985-100.0.8-131.3.3-132.8.8-134.3.5-140.0.5-140.0.0-141.5.7-144.2.5-151.0.0-152.5.5-154.0.0-155.5.5-157-0.0-158.5.5-160.0.5-160.0.0-161.5.5-163.0.0-164.5.5-166.0.0-167.5.5-169.0.0-170.5.5-172.0.0-174.0.0-174.0.0-175.5

May 21, 1996

Job# 964637

Project # 327-111 P.O. # 11652

Goldppb

2422<584<55

^5<5^<5<5<5<5<5<525<5<55

<5<5<528<5<5<5<5<5^<5<5<5

GoldOz/t

^.001<0.001<0.0010.002

•cO.OOl<0.001

<0.001<0.001<0.001^.001<0.001<0.001<0.001cO.OOl-CO. 001•iO.OOl<0.001<0.001<0.001•cO.OOl<0.001<0.001<0.001<0.001*:0.001<0.001<0.001<0.001<0.001•cO.OOl<0.001<0.001

Certified By:



PHONE (807) 623-6448FAX (807) 623-6820

Page l


ATTENTION: R. FELIX


123456789

1011121314151617181920212223242526272829

PO96-15-40.8-42.3PO96-15-42.3-43.8P096-15-43.8-45.3P096-15-59.0-60.5P096-15-60. 5-62.0P096-15-62.0-63.5P096-15-63. 5-65.0P096-15-65.0-65.4P096-15-65.4-66.9P096-15-66.9-67.8PO96-15-67.8-68.2P096-15-68.2-69.7P096-15-69.7-71.2P096-15-71.2-72.7P096-15-72. 7-73.1P096-15-73.1-74.6P096-15-74. 6-76.1PO96-15-76.1-77.6PO96-15-77. 6-79.1PO96-15-79.1-80.6PO96-15-80. 6-82.1P096-15-82.1-83.6P096-15-83. 6-85.1PO96-15-85.1-86.6P096-15-86. 6-88.1P096-15-88.1-89.6P096-15-89. 6-91.1P096-15-91.1-92.5PO96-15-92. 5-94.0

May 21, 1996

Job# 964637

Project # 327-111 P.O. # 11652

Copperppm

1541441262537

10034

3048486

2946452

14213493449366943848965863

2281027241

Zincppm

10016111474

11870426159746450221829645975776770723844342833345646

Silver ppm

43312226336244743434333324432

Certified By:


1070 LITHIUM DRIVE, UNIT 2THUNDER BAY. ONTARIO P7B 6G3

PHONE (807) 623-6448FAX (807) 623-6820Page 2


ATTENTION: R. FELIX


303132333435363738394041424344454647484950515253545556

P096-15-94.0-95.5P096-15-95. 5-97.0PO96-15-97.0-98.5PO96-15-98. 5-100.0P096-15-129.8-131.3PO96-15-131.3-132.8P096-15-132.8-134.3P096-15-138. 5-140.0PO9 6 -15-140. 0-141. 5P09 6 -15 -142. 7 -144. 2P09 6 -15 -149. 5 -151.0P096-15-151.0-152.5P096-15-152. 5-154.0P096-15-154.0-155.5PO9 6 -15-155. 5 -157-0PO96-15-157.0-158.5P096-15-158. 5-160.0P096-15-160.0-161.5PO96-15-161. 5-163.0P09 6 -15 -163. 0-164. 5PO96-15-164. 5-166.0P096-15-166.0-167.5PO96-15-167. 5-169.0PO96-15-169 .0-170.5P096-15-170. 5-172.0P096-15-172. 0-174.0PO96-15-174.0-175.5

May 21, 1996

Job# 964637

Project # 327-111 P.O. # 11652

Copperppm

4923

14932

123978764501876517339165335342611271554222010

103

Zincppm

663989

1064047373636376739555442443136424435332833255525

Silver ppm

323233332232322322222232223

Certified By;

APPENDIX III Petrographic Reports

Vancouver Petrographies Ltd.JAMES VINNELL,JOHN G. PAYNE, Ph DCRAIG LEITCH, Ph o Geoiog.xJEFF HARRIS, Ph o GootogisiKEN E. NORTHCOTE, Pn.D 0*0100*

P.O. BOX 396080 GLOVER ROAD,FORT LANG LE Y, B.C.VOX 1JOPHONE (604) 888-1323FAX. (604) 888-3642

PETROGRAPHIC REPORT ON SIX THIN SECTIONS

Report for: R. FelixNor anda Mining and Exploration Inc.9&O All oy Dri veThunder Bay, Ontario P7B SA4.

Invoice 9&0322 P.O.tt 11655 Projects 322/327 June 24, 'l986.

AT96-1 91m: AMPHIBOLITE; LAYERS OF PLA6IOCLASE-BIOTITE-QUARTZ-ZOISITE- SPHENE, CALCITE-CHLORITE

Foliated, fine- to medium-grained, dark green to red—brown and white, gneissic rock; only traces of stain for K—feldspar, trace magnetism, minor reaction to HC1 in places. Modal mineralogy in polished thin section is approximately:

Amphibole ( h or n b l en d e? ) BO"/.Biotite 15/1?P1 ag i oc l ase (. c a l c i c ) l OXQuartz 57.Carbonate t'"'mainly calcite) 57.Chlorite 27.Z o i s i t e f c l i n z o i s i t e 27.Sericite 17.Sphene, ilmenite -:'-. 1 7.Pyrrhotite, trace chaicopyri t e tr

Amphibole forms subhedral crystals rarely over l mm long, commonly in irregular aggregates up to several mm across. Pleochroism is olive to blue-green, extinction angle c •'''•Z' about 15 degrees. It is mostly intergrown with carbonate or biotite. Biotite forms subhedral to euhedral flakes up to 0.6 mm in diameter, with colourless to red-brown pleoc h r o i sm; mi n or alt erat i on t o c hl or i t e is c ommon in pi ac es, e s pie c: i all y near car b on a t e—r i eh layers. The chlorite is mainly length- fast, with moderate to high birefringence for chlorite, suggesting a h g--r l c h variety; it forms subhedral flakes of similar size to biotite.

Carbonate forms subhedral crystals, likely mainly calcite, up to O.S mm diameter and concentrated in certain layers intergrown with amphibole. Other layers (red-brown in hand specimen) are rich in sub- to anhedral, rounded domains of '"'calcic plagioclase up to 0.5 mm in diameter (slightly elongate parallel to foliation and full of fine, 1O- 50 micron rounded inclusions of quartz) intergrown with biotite and minor zoisite and sphene. Relief well above quartz suggests a calcic plagioclase; in places, there is minor to moderate alteration to fine sericite (subhedral flakes of 25-35 microns diameter) axnd a fuzzy alteration product that forms between it and zoisite, and on a larger scale between the biotite-rich and amphibole-ri eh layers.

Zoisite i: or clinozoisite) forms sub— to euhedral crystals to 0.25 mm size, with anomalous blue and yellow-green interference colours and no pleochroism. It is intergrown with a fine-grained, fuzzy and poorly crystallized mineral that could be ?epidote-cl inozoisi t e after plagioclase (associated with other calcic minerals such as sericitized plagioclase, sphene and calcite). Sphene forms subhedral crystals to 0.3 mm, elongate parallel to foliation, cored by minor ilmenite.

Traces of pyrrhotite form subhedral crystals to O.15 mm, mixed in places with chalcopyrite of similar size and containing tiny 10-20 micron flames of ?pyrite or pentlandite (too small to identify positively). Bulfides are most commonly intergrown with amphibole.

ATSG-1 14Sm: MUSCOVITE-QUARTZ-MI NOR CHLORITE SCHIST WITH PORPHYROBLASTS OF "'STAUROLITE, ALTERED TD MUSCOVITE-QUARTZ-CHLORITE-SULFIDES

Dark grey to blackish, well foliated schist containing about 10- 157. prominent O. 5 cm por phyr obi ast s, minor pyrite and pyrrhotite (rock is moderately magnetic, but shows no reaction to cold dilute HC1 or stain for K- f el dspar '.i . Modal mineralogy in polished thin section is ap pr o x i mat el y:

Muscovite 607.Quarts 207.'"'Staurolite (por phyr obi ast s) 107.Chlorite 57.Pyrite 27.Pyrrhotite 27.Rut i l e, sp h en e ^^ 17.

This rock consists of fine-grained, wel l-fol i ated muscovite-minor quartz schist hosting large subhedral altered porphyroblast relics and clots of chl or i te-sulfi de; other chlorite crystals are randomly oriented. Muscovite forms sub- to euhedral flakes up to about 0.25 mm in diameter, but is commonly semi—massive, containing only minor quartz; there is a gradation to layers of almost pure quartz with minor muscovite. Quartz occurs as subhedral, mainly annealed crystals generally less than O.15 mm in diameter, but in coarse "clots" with chlorite and sulfides, quartz forms sub- to anhedral crystals to 0.7 mm size and traces of lamellar structure, likely indicating strain. Chlorite forms euhedral length—fast crystals to 1.25 mm, bent in places, with first-order grey birefringence and very pale colour indicating Mg-rich composition.

The relict porphyrobiasts are mainly composed of a massive, optically continuous, olive-green to yellowish—brown!sh mineral with low to moderate birefringence, weak pleochroism, and full of inclusions of fine rounded quartz (10-5O microns) and muscovite (to O. 2 mm!) and chlorite (to 0.5 mm); the mineral seems likely to be staurolite, by comparison to other samples in this suite, but could be a hydrous (partly altered) biotite. Core areas of the porphyrobiasts are replaced by muscovite, or muscovite and quartz. In other examples, patches up to 0.3 mm across of very fine-grained brown material could be '"'sphene and/or rutile mixed with leucoxene. If they are not staurolite, it would be difficult to speculate as to the original i d en t i t y o f t h s p or p h y r ob l a st s .

Pyrite forms euhedral crystals to about l mm diameter, commonly containing fine (2O — 3O micron) rounded to irregu.liu" inclusions of chalcopyrite, and intergrown in places with subhedral to lath-like pyrrhotite up to 0.5 mm in size, elongate parallel to foliation. In places there are traces of rutile (euhedral crystiUs to 5'0 microns) associated with the sulfides.

F' a g e 4

AT36-1 22Om: QUARTZ-MUSCOVITE SCHIST WITH PDRPHYROBLASTS OF STAUROLITE AND CHLORITE-KSPAR ALTERED BIOTITE; MINOR DUARTZ-PYRRHOTITE VEIN ING

Dark grey to blackish, ma f i c -l ooki ng rock characterized- by 2.07. euhedral dark crystals to 3 mm long and l O'/, black "'biotite books interleaved with a mineral that stains for potassium. The rock is slightly magnetic but shows no reaction to cold dilute HC1; modtU mineralogy in polished thin section is approximately:

Quarts 457.Muscovite 3O7.Biotite (chl or i t i zed ) l O"/.'"'Staurolite 1O7.Chlorite 2-37.K-feldspar 17.Pyrrhotite, trace chalcopyrite, pyrite l*/.Sphene, rutile -t!'/.

This rock consists of porphyr obi ast s of altered biotite and '''staurolite in a quartz-muscovite matrix. The matrix varies from quartz-rich and coarse (sub— to anhedral crystals to 0.5 mm) to muscovite-ri eh and finer (muscovite forming eu— to subhedral flakes to 0.25 mm; quartz to O.I mm). The euhedral porphyrobiasts appear to be staurolite (high relief, low first-order grey birefringence, parallel extinction, length-slow, optically positive, pale yellow pleochroism, full of fine rounded quartz inclusions to 25 microns). The crystals are mainly less than 3 mm in length and in places form crossed (penetration) twins.

Biotite porphyrobiasts are euhedral to somewhat rounded in outline, up to 3 mm in diameter, and are partly interleaved by K- feldspar (relief below that of quartz; yellow stain in etched slab) as subhedral, in places twinned, crystals up to 0.15 mm long; elsewhere, the biotite is replaced by '"'chlorite (very low birefringence, pale colour, length—slow; essentially a hydration of the biotite). Muscovite commonly coats the outer margins of the biotite crystals. Rare sphene as euhedral crystals to 5O microns are associated with pyrrhotite in the biotite crystals, and euhedral rutile to 0.3 mm long are found at their margins. Rare pleochroic haloes are formed around minute (10 micron) crystals of '"'allanite in the chlorite.

The rock is crossed by a 1-2 mm thick quartz-sulfi de veincontaining subhedral pyrrhotite to O.5 mm with very fine (!1O—25 micron!) flame—like inclusions of pyrite and surrounded by minor chalcopyrite to 0.1 mm. Minor rutile, as euhedral crystals to 0.3 mm, is associated withi the vein margins.

PS96-13 115 m: QUARTZ-MUSCOVITE SCHIST WITH COARSE PORPHYROBLASTS OF STAUROLITE AND CHLORITE-KSPAR ALTERED BIOTITE; TRACE GARNET

D au" l: grey, finely foliated to laminated rock containing about 25X small dark por phyr obi ast s to 2 mm size. The rock shows traces of magnetism, but no reaction to cold dilute HC1; the same minor stain for K-feldspar occurs in biotite crystals. Modal mineralogy in polished thin section is approximately:

Quartz 357.Muse ov i t e 257.Staurolite 2O7.Biotite ''partly c h l or i t i zed ) 157.Chlorite C after biotite!) 1-27.Pyrrhotite, trace chalcopyrite, pyrite 1-271K-feldspar 17.Ilmenite \1~/.Garnet -^17.

This slide consists of large to very large porphyrobiasts of staurolite and smaller biotite in a matrix of quartz and muscovite. The matrix varies from fine (mainly 50—1OO micron subhedral, annealed quartz and lesser, euhedral 75—1OO micron flakes of muscovite) to coarse, irregular lensey areas of quartz (sub- to anhedral, to 0.3 mm diameter) that form around and cut across staurolite porphyrobiasts. In some elongate areas subparallel to foliation the matrix is rich in very fine (2—5 micron) opaque inclusions, too fine to ideintify with certainty, but possibly pyrrhotite.

The staurolite porphyrobiasts are euhedral to subhedral in outline, up to l cm in length, and appear to be both clear (free of inclusions) and highly crowded by characteristic rounded quartz inclusions, in the same crystal or penetrating twinned crystals; it almost looks as if the i ne lusion-free areas are remnants of an alteration process that has produced the areas of inclusion-rich material (commonly both areas are optically continuous). Only in at few cases can the typical yellow pleochroism be seen. It is possible that the inclusion-rich portions are overgrowths on cores of clear staurolite; the clear portions do in places almost look like a separate mineral. There is very rare garnet (euhedral, to O.2 mm, colourless; no an omalous an i sot r op i sm).

Biotite forms euhedral crystals or books up to 2: mm in diameter (."3. mm where aggregated), containinq common minute radioactive crystals surrounded by pleochroic haloes. In places the biotite is interleaved to almost completely replaced by chlorite (length-slow, pale green) as subhedral flakes to 0.35 mm, and minor K-feldspar as subhedral, elongate crystals to 0.15 mm.

Pyrrhotite forms elongate lath-like to subhedral crystals up te al most l mm long, commonly inter gr own or associated with finer tabular' euhedral ilmenite crysta-ils to 0.15 mm (ilmenite also occurs separate from pyrrhotite). There are traces of chalcopyrite (to O.1mm) and very fine flame-like '"'pyrite (3O microns) in the coarsest pyrrhotite blebs.

F'age 6

PS9E.--13 l17ni:QUARTZ-MUBCOVITE-"CORDIERITE SCHIST, COARSE PORRHVRDBLASTE STAUROLITE, SMALLER CHLORITE-K5RAR-- ''SILLIMANITE ALTERED BIOTITE

Dark grey, foJ iated quar t r. --mi c a schist containing 10-15/1 large darker grey to black porphyrobiasts up to centimeter size as well as f i rier black biotite crystals and common pyrrhotite blebs t roc k is magnetic, but shows no reaction to cold dilute HC1 and only trace stain for K--f el dspar ) . Modal mineralogy in polished thin section is a p p r o x i m a t e l y:

Quartz 4O7.Muscovite 307.Biotite (small porphyrobiasts) 107.'"'Cordierite or plagioclase feldspar 107.?St aur o l i t e (l ar ge por phyr ob l ast s ) 57.Chlorite 27.Pyrrhotite 1-27."'Sillimanite 17.Rut ile -^ 17.K-feldspar 07.

This rock is essentially composed of a matrix of quartz, muscovite and "'cordierite or plagioclase that hosts scattered large por phyr obi asts of ?c h l or i t i zed biotite, possibly after some former prograde mineral, arid abundant finer, partly chl or it i zed biotite crystals.

The matrix varies from quartz—rich to muscovi te-'?cor di er i te rich. Quartz forms subhedral crystals to 50 microns, mainly annealed, except in quartz-rich "sweats" or lenses that are up to 2 mm thick and contain sub- to anhedral j, also mainly annealed, quartz up to O.S mm in diameter. '"'Cordierite or '"'plagioclase is chiefly distinguished by its- partial alteration to fine c l ay —seri c i t e (10-2Q micron flakes); rare subhedral '"'hexagonal outlines and apparently small negative 2V, together with low birefringence and relief close to that of quartz, are suggestive of cordierite. If however it is plagioclase, the lack of yellow stain in the etched slab axnd relief close to that of quartz would suggest an intermediate composition, perhaps '"'andesine, but this cannot be confirmed optically due to the small grain size (subhedral, to O.I mm; no twinning visible). Muscovite forms euhedral flakes rarely over O.25 mm in diameter. Minor fine pyrrhotite as subhedral laths to 0.2 mm is common in the host rock also, coarsening to 0.5 mm in the quartz-rich "sweats", and fine rutile forms euhedral crystals to 50 microns l cm g.

B i o t i t e f or m s e u h e ci r s. l t o s u b h e ci r a l c r y s t a l s t o 1.5 rn m d i a m c: t e. r Pin places partly to almost completely replaced by c hi or i t B, and rarely interleaved ei t the coves by a fibrous, fine-grained mineral that could be '"'sillimanite (subhedral, moderate birefringence, length-slow, high relief; to 0.2 mm), and minor K-feldspar (subhedral, to 0.1 mm. It j s not clear whether biotite is altering to or from the "'sillimanite. The large porphyrobiasts are pale yellowish-brown in colour with abundant f i n e q u a r t z i n c l u s i o ri s, cores o f m u s c o v i t e, a n d c r o s s e d by o r surrounded by muscovite; they appear to be staurolite, as in the previous samples, and are most similar to the very large porphyrob]asts in AT36-1 at 143m, but in this sample contain crystals of the partly altered biotite. Chlorite forms euhedral flakes to 0.5 mm diameter with first-order birefringence, pale colour, and length-fast character suggesting Mg-rich composition.

F'age 7

PQ96-13 133m: QUARTZ-MUSCOVITE SCHIST WITH LARGE PDRPHYROBLASTS OF ^-'STAUROLITE AND SMALLER BIOTITE; TRACE TOURMALINE, ?GARMET

Grey, porphyroblastic rock largely without foliation containing about 15-207. small dark biotite crystals to 2.5 mm and scattered large porphyrobiasts to over l cm C some of which contain a reddish mineral). The rock is weakly magnetic, probably due to fine '"'pyrrhotite, and contains traces of yellow-stained K-feldspar in the biotite (see etched slab). Modal mineralogy in thin section is approximately:

Quartz 35X Muscovite 30"/. Staurolite C?) 15"/. Biotite ' 157. Chlorite 27. Opaque ('"'pyrrhotite, '"'ilmenite) IX Tourmaline C?schor l i t i c ) 17. K-feldspar <l"/. Garnet C?) -••. IX

This is a quartz-mica schist containing large porphyrobiasts of '"'staurolite and smaller biotite crystals. The matrix consists of quartz and muscovite in variable proportions, with quartz forming subhedral, commonly somewhat elongated (2:1) crystals to 0.1 mm (except adjacent to biotite crystals, where subhedral equant quartz is up toO.7 mm diameter). Muscovite forms euhedral flakes commonly less than O.25 mm in di ameter.

Biotite forms generally euhedral crystals or books to about 2 mm in diameter, containing abundant fine pleochroic haloes around some fine mineral containing a radioactive material. The pleochroism is generally in shades of medium brown, with only minor alteration to chlorite, and minor inclusions of fine (1OO micron) elongate K— feldspar. Chlorite is length-fast and has moderate (first-order white) birefringence, indicating Mg—rich composition; euhedral crystals are up t o 0. 3 mrn d i amet er .

The large porphyrobiasts are characterized by moderately high relief, very abundant fine quartz inclusions, low (grey) birefringence and very pale yellowish to pinkish colour; they may be '"'staurolite or '"'andalusite, but comparison to the similar mineral in other sections suggests the former is more likely. Crystals of biotite are rarely included in the large porphyrobiasts; oriented quartz inclusions show swirls and folds in the crystals ('?syn — met amor phi c growth or 'T'post — metamorphic crenulation cleavage; appears to line up with crenulation in muscovite and areas of fine shreddy brownish '"'hydrobiotite).

Minor tourmaline with greenish-brown pleochroism ('"'schor l i t i c composition) forms slender euhedral prisms to 0.35 mm lonq in certain layers of the rock. Rare si eve—textured crystals (inclusions of quartz, muscovite, tourmaline; veined by quartz and '"'altered to chlorite or '"'cordierite) that are close to isotropic, with euhedral hexagonal outlines under l mm in diameter and high relief, suggest 'T'garneb (with anomalous ani sot r opi sm) .

Craig H. B. Lei t eh ,-THY. D. , P.Eng C 604) 653-9158 492 Isabella Point Road, Salt Spring Island, B.C. VSK lV4

Ministry ofNorthern Developmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street. Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.

Instructions:

52P08NW0010 W9640.00547 PETAWANGA LAKE

- Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for req

Recorder.- A separate copy of this form must be completec- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

900

327-dd-96Recorded Holder(s)

Noranda Mining and Exploration Inc. fyn,eotuB#*DG.e L,^ t Te^ ft AAddress "" c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A4Mining Division Thunder Bay

Dates Work From: Performed March 1, 1996

Township/Area Q Petawanga Lake I^A^S /~fo ) Lrff\^

Client No. ^ g

Telephone No. (807) 623-4339

M or G Plan No.

To: June 30, 1996

Work Performed (Check One Work Group Only)Work Group

X

Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

Diamond Drilling (Holes P096-13, 14, 15)

Total Assessment Work Claimed on the Attached Statement of Costs98,198

Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name

R. Felix W. G. Langley (Drilling)

Chemex Labs

Accurassay Labs

Midwest Helicopters

AddressC/O 960 Alloy Drive, Thunder Bay, Ontario P7B 6A4 Brampton, Ontario

5175 Timberlea Blvd, Mississauga, Ont.

1070 Lithium Drive, Thunder Bay, Ont.

L4W 2S3

P7B 6G3

Thunder Bay

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.

Date Recorded Holder or Agent (Signature)

Certification of Work Report1 certify that 1 have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true.

Name and Address of Person Certifying

Cecilia M. Barrett, 960 Alloy Drive, Thunder Bay, Ontario P7B 6A4Telepone No.

(807) 623-4339

Date o 7 c, As

1

Certified By (Signature)

For Office Use OnlyTotal Value Cr. Recorded Date Recorded

Deemed Approval Date

Mining Recover

^~- /j U~s\A^frwJDate Approved

Date Notice for Amendments Sent

Received Stamp

CIHAJ3DHtf9661 - 1 130UOISIAIQ Suiuiji\;

XBQ japunni.

0241 (03/91)

Details for Work Report # 327-dd-96 Page 1

Work Report* for Applying Reserve

Claim Number (see note 2)

TB 1,138,337

TB 1,138,389

TB 1,138,392

TB 1,139,667

TB 1,142,048

TB 1,142,049

TB 1,142,050

TB 1,142,051

TB 1,142,052

TB 1,142,053

TB 1,142,054

TB 1,142,055

TB 1,142,056

TB 1,142,057

TB 1,142,058

TB 1,142,059

TB 1,142,060

TB 1,142,061

TB 1,142,072

TB 1,142,073

TB 1,142,074

TB 1,142,075

TB 1,142,353

TB 1,142,354

TB 1,142,355

TB 1,142,356

TB 1,142,357

TB 1,142,358

TB 1,142,359

TB 1,142,360

TB 1,142,361

TB 1,142,362

TB 1,142,363

TB 1,142,364

TB 1,149,125

TB 1,165,263

TB 1,165,269

TB 1,173,498

TB 1,173,499

TB 1,173,500

TB 1,173,501

TB 1,173,502

TB 1,173,503

# of Claim Units

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

Value of Assesment Work Done

on this Claim

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.00

20,000.00

19,550.00

30,000.00

0.00

28,648.00

0.00

0.00

0.00

0.00

Value Applied to this Claim

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

369.00

369.00

369.00

37.00

37.00

37.00

400.00

37.00

37.00

37.00

37.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

Values Assigned from this Claim

10,966.00

2,000.00

Reserve:Work to be Claimed at

a Future Date

9,034.00

19,550.00

30,000.00

26,248.00

Details-for Work Report # 327-dd-96 Page

Work Report* for Applying Reserve

Claim Number (see note 2)

43

Total Number of Claims

# of Claim Units

Value of Assesment Work Done

on this Claim

Value Applied to this Claim

98,198.00 13,366.00

Total Value Work Total Value Done Work Applied

Values Assigned from this Claim

Reserve:Work to be Claimed at

a Future Date

12,966.00 84,832.00

Total Assigned Total Reserve From

Credits you are claiming in this report may be cut back. In order to minimize the adverse affects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (x) one of the following:

1. Credits are to be cut back starting with the claims listed last, working backwards.

2. Credits are to be cut back equally over all claims contained in this report of work.

3. Credits are to be cut back as priorized on the attatched appendix.

4. x Credits are to be cut back starting with the claims that have reserve credits.

In the event that you have not specified your choice of priority, option one will be implemented.

Note 1: Examples of beneficial Interest are unrecorded transfers, option payments, memorandum of agreements, etc.,with respect to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

I certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Date

12/16/96 10:53 O807 623 0452Ministry ofNorthern Development

NORANDA TBAYStatement of Costs for Assessment Credit

MR TB 002/002_________ Tttniactkxi Number (ofllc4 UM)

Personal Information collected on thlt form It obtained under the authority of subsection 8(1) of the Assessment Worts Regulation WM. Under •action 8 of the Mining Act, Ihe Information to a public record. This Information w(l be used to review Ihe assessment work and correspond wllh the mining land holder. Questions about thin collection ihould be directed lo the Chtof Mining Record*, MInlslry of Northern Devefop'iml and Mln**. filh Floor, 033 Hummv Lake Rond. Sudbury, Ontario. ME OBS.

PROJECT #327-dd-96

Work Type

Diamond Drilling

Assays/Thin Sections

Labour

-

,

Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo- metres of arid fine, number of samples, etc.

496.6 meters

126

59 mandays

Associated Costs (e.g. supplies, mobilization and demobilization).

( Supplies (Core Boxes, gas, maps)

.... ,

Transportation Costs

Air (Helicopter S6.184 -f Fixed Wing S1 0,271)

Ground

Food and Lodging costs

Cost Per Unit

8112.80

S6. 16

^7.**^**

Total Value of Assessment Work

Total Cost

56,011

776

15,807

4,653

16,455

2,396

2,100

98,198

Calculations of Filing Discounts:

1. Work filed within two years of performance Is claimed at 100^ of the above Total Value of Assessment Work.2. If work Is filed after two years and up lo five yeans after performance, it can only be claimed at 50*H) of the Total

Value of Assessment Work. If this situation applies to your claims, use Ihe calculation below:Total 3 value of worked claimed.TOTAL VALUE OF ASSESSMENT WORK x 0.60

Note:- Work older than 5 years Is not eligible for credit.- A recorded holder may be required to verify expenditures claimed In this statement of costs within AS days of a request for verification and/or correction/clarification. If verification and/or correction/clarification Is not made, the Minister may reject all or part of the assessment work submitted,

Certification verifying costs;dfi '

l, LJfe-"./*. Stf. ^jtrfSfTf , do hereby; certify, that the amounts shown are aa accurate as may(plane prlni fuH mm*) ' ' j

reasonably be determined and the costs were Incurred while condubling assessment work on the lands Indicated onreasonay e etermne an e coss were nure we

the accompanying Declaration of Work form as rfyfT*/ ^ ^f^Zr ' * (rocordod^eftder. agent; or ttut* oompwiy pmilfen wfth

to make this certification.

am authorized

SigjiaiijMjuw #S

-*

H C F E R EN C E 6

NOT OPEN FOR STAKING (PROV. PARK)Thunder fi*y

Mining Division

RECEIVED

ALBANY PROVINCIAL PARK

Petawanga

LEGENDHIGHWAY AND ROUTE No. OTHER ROADS

TRAILS SURVEYED LINES

TOWNSHIPS. BASE LINES. ETC- L ----LOTS, MINfNG CLAIMS, PARCELS. ETC

UNSURVEYED LIMES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINEMARSH OR MUSKEG ^*~* MINES TRAVERSE MONUMENT

DISPOSITION OF GROWN LANDS"~~~

TYPE OF DOCUMENTL - - J293 , 1165292 [ iroocaa- ( ( , |1BgSEB

PATENT, SURFACE fc MINING RIGHTS

.SURFACE RIGHTS ONLY

.MINING RIGHTS ONLY LEASE, SURFACE ft MINING RIGHTS

" , SURFACE RIGHTS ONLY

" .MINING RIGHTS dNLY LICENCE OF OCCUPATION .. __ ... __ ........,i __ . TORDER-IN-COUNCIL .. .. __ ......—— _ 1......... __ 'OC

RESERVATION ___ ...... ___ ..,...— ... _ .-...—— — 0CANCELLED

SAND 8. GRAVEL .. _ .... _ ........... .....—— ....... .. 0 xPERMITS FOR COMMERCIAL TOURaMgDLrtPCBT CAMPS y

: MINING RIGHTS IN PARCELS PATfWTED PRIOR TO MAY 6,

11165291 11^727

j 1165279 l 1165276 \ 116

- -JTB-—Fl 1138392 J H22020 j- - - -f- - - -

l T^W l ^** l l II1&WHW II l

'3a 336 . |Ma?t .^ M^ '^ k- - -f TBM-B ' " l . l I

1913. VESTED IN ORIGINAL PATENTEE BY THE PUBLIC LANDS ACT. R S O 1970, CHAP. 3BO. SEC. 83, SUBSEC 1.

SCALE: 1 INCH = 40 CHAINS

AREA *

PETAWANGA LAKEM. N. R. ADMINISTRATIVE DISTRICT

GERALDTONMINING DIVISION

THUNDER BAYLAND TITLES/ REGISTRY DIVISION

THUNDER BAY/?206737Ministry of Natural

- Resources

Land Mpnag ament

JULY 14,1981G-272HURST AND FELSIA LAKES G-378

O O CM

!i

~ 7 o~•^-Q^

; r^ *c

6: S ^

/^ ;Lr^ /"^O,S n" w <̂

^6.^^

Scale 1:500050 O 50 100 150 200

(meters)

DISCOVERY WEST

DISCOVERY WEST PETAWANGA NUMBERBASELINE AZIMUTH : 7G de

DATE : MARCH/1995 NTS : 52P/8 SURVEY B v : NORANDA MIMING k EXPLORATION

FILE : M327DSW

Mining and Exploration Inc.

52P08NW0010 W9640.00S47 PETAWANGA LAKE 210

en inC\J T

eno3

ftr*. m

en ISm en0

SenROJ

eno uoC\J

13C\J

en

l

P096-13NORTH

-25

-50

-75

MAFI C METAVOLCANICS

l CHLOfilTE-a APHITE SCHISTS

TER

OVERBURIEN

CLAIM 173499

-25

-50!

-75

-100

/CH.-f1 SCH/OBJVFELSIC TU F BX/MS)

i DUST l FELSIC TIFFS FELSIC TUFFS- STAUROLITE SCHIST

BIOTITE BARNET QUAR' Z EYE TUFFS

134.(O f.——605=13-

-100

-125 -125

-150 -150

-175

-200

en inOJ

C/)

-200

eninCMm

NORANDA MINING AND EXPLORATION

327-PETAWAN6A

SECTION 5500W

P096-13

BAR 6RAPH l CM. * 200 PPM COPPER. 600 PPM ZINC

BATE: 96/06/07 l SCALE; 1/1000

MAP52P08NWD010 W9640.00S47 PETAWANGA LAKE 220

on o oCOin to oin

(D

enin en oS ID

P096-14NORTH

-25

CLAIM 1165269

IVEHBURDEN

— MAFIC NET* OLCANIC FLOWS

FELSIC QUARTZ EYE TUFFS

-25,

-50 V

t MAFIC METAVOLCANIC FLOMS

OU; RTZ FELDSPAR PORPHYRY

MAFIC TIFF/DYKE

I MAFIC NETAVOLCANIC

MODERATELY ALTERED

MAFIC TUFF/DYKE

INTENSELY ALTERED FELSIC TUFFS

FELSIC TUFFS

-50

-75

ALTERED MAFIC

MAFIC METAVOLCANIC FLOWS

PEU9FAR E9RFIIVRV

MAFIC METAWJLCANIC FLOWS

INTENSELY ALTERED FELSIC TUFFS

TUFFS

-75

ALTERED MAFIC TUFFS

ALTERED FELSIC TUFFS

ALTERED MAFIC TU FS

OUAP.TZ EYE FELSIC TUFF i

-100 -100


327-PETAWANGA

SECTION 5100W

PO36-14

BAR GRAPH l CM. - 200 PPM COPPER 500 PPM ZINC

OATE: 96/OB/07 l SCALE: 1/500

MAP 3

52P08NW0010 W9&40.00547 PETAWANGA LAKE 230

o o m moin m i 0

0^

gOJ TT

1T

IT) f^ T

•zOs

P096-15NORTH

-25

OVERBURDEN

\ HAFCC METAVOL MICS

CLAIM tt 1165263

-25

-50CLAIM f 1149125 t BEDOED FEI SIC TUFFS

-50

-75

MINERALIZED FELSIC l JFFS/EXHALITE

-75

-100 -100

-125

.TEBED FELSIC CRYSTAL TUFFS

-125 i

-150

TO BE OfilL SO

200 00 l.p ts-a-150

-175 -175

-200 -200

in l r-Iool


327-PETAWANGA

SECTION 3100W

P096-15

BAR GRAPH l CM. - 200 PPM COPPER, 500 PPM ZINC

DATE: 96/08/07______ l SCALE: 1/1000

52P08NW0010W9640.00547 PETAWANGA LAKE 240MAP 4

project no.327 thunder bay. ontario senior geologist · group 400 meters southwest along strike...

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