lOPU-OMHAGEY 010

GEOLOGY OF BAGGEOPHYSICAL

PROSPECTING AND WITH OPAP

OUTGRANT OP92-064

by: CLAUDE LAROUCHE, P. ENGINEEROVALBAY GEOLOGICAL SERVICES INC.1070 Lithium Drive, Unit liTHUNDER BAY ONTARIOP7B 6K2Tel: (807) 623-3770Fax: (807) 623-2335

JANUARY 1993

TABUS OF CO aBOWEoouoraMM HAGEY 01OC

- Introduction ...................................... 3

- Location and access ............................... 7

- Claims ............................................ 9

- Previous work ..................................... 11

- Regional geology .................................. 13

- Mineralization .................................... 15

- Recent work:

- Geophysical test survey ...................... 16- Prospecting napping .......................... 16

- Conclusions ....................................... 19

- Cost of work ...................................... 20

- Certificate of qualifications ..................... 21

LIST OF FIGURES

Figure 1: Location nap ........................ 8Figure 2: Sketch of clains .................... 10Figure 3: Regional geology .................... 14

LIST OF MAPS (in pocket)

Map 1: Compilation East partMap 2: Compilation West partMap 3: Magnetic surveyMap 4: VLF-Em 16 survey (Cutler)Map 5: VLF-Em 16 survey (Jim Creek)Map 6: VLF-Em 16 survey (Seatle)

INTRODUCTION

The following report presents the results of a prospecting mapping programme along with a geophysical test survey, completed with the help of an OPAP Grant to Henri Lavoie. A compilation of all pertinent information was also completed outside the scope of the field investigation in order to better orientate the prospecting mapping activities. The purpose of the programme is to assess the potential for auriferous porphyries and for base metal mineralization in the felsic volcanics.

The area in Conacher and Hagey Townships has been prospected in the past by numerous companies, and deposits of economic interest are known, such as: Bandore Zone fi, 650,000 tons grading 0.25 opt Au; Bandore Zone f 4, 1,200,000 tons grading 0.12 opt Au; and Frank West property, estimated 200,000 tons grading 0.10 opt Au.

Geological setting of gold mineralization in the western part of Shebandowan Greenstone belt has been summarized by L. Charlton in an Open File Report f 5636, published by the O.S.G. in 1987.

"...investigation of the setting of gold mineralization in this part of the belt has shown that the gold is structurally controlled, and for the most part associated with brittle structures (veins and fractures) developed at a moderately late stage in the deformation and alteration history. From examination of the displacement history and timing of structures in the area, it has been concluded that the early sinistral shear zones which provided the main fluid conduits enabling metasomatic iron carbonate and sericite alteration considered favourable gold exploration targets in other greenstone belts, are flexed, reactivated, and overprinted by subordinate dextral shear and fracture zones under the influence of a dextral deformation regime. The carbonatization process may have overlapped the onset of this imprint, and the ensuing quartz veining and gold related sulphide mineralization were even more likely to have occurred under the influence of the dextral regime.

The main effects of the change from one deformation regime to the other are:

(1) flexing of pre-existing shear zones, and minor vein filling within these zones, either as discontinuous, multiple veins along the pre-existing strong foliations or shear planes (e.g. Bandore trenches and outcrop) or as extension veins occupying former normal" fractures at high angles to these foliations (e.g. the main Ray Smith vein) ;

(2) refocussing of carbonothermal to hydrothermal fluids, already utilizing some of the early shear zones as conduits, towards major structural intersections or along later, more brittle fault zones, e.g., the northwest-trending faults and many subsidiary structures.

(3) possible brittle failure of entire, relatively competent masses, strained to the ductile limit during the earlier sinistral regime, and the emplacement of quartz stockworks, which may be barren if the rocks are not accessible to the main hydrothermal conduits, or may be auriferous if accessible to auriferous hydrothermal fluids, and if conditions are suitable for precipitation of gold and pyrite (e.g., the carbonatized Pistol Lake stock, at least to a limited extent).

Thus, mineralization in many cases will probably not correspond geometrically to the ankerite-sericite schist alteration zones established during the earlier sinistral deformation regime, although it is suggested that they are likely to have intersected them.

Recommendations tor ExDlora.iii.on

It is therefore suggested that a sound exploration tactic in the Highway f 11 area would be to start with a ground investigation of any sericite-ankerite schist zones, particularly as these present an easily recognized target.

Parts of these zones where significant normal extensional fractures, dextral fractures or shear zones, flexing, dilating, or crosscutting the earlier structures, are either exposed, or suggested by a prominent presence of related minor structures in existing outcrops, should be thoroughly investigated as zones where hydrothermal activity and perhaps precipitation might be enhanced; as it is likely that many of the more significant structures will be poorly exposed, geophysical techniques may be of assistance in defining these zones.

Attention should meanwhile be paid to any occurrences of pyrite or other sulphides in the carbonatized zones, particularly those that are associated with shear planes, fracture or breccia zones, and the occurrence and geometry of quartz veining connected to the carbonatized zones.

The latite/quartz syenite dykes might also be worthy of independent investigation, particularly those that are highly carbonatized and/or contain pyrite.

The numerous sericite-ankerite schist zones traversing the Shebandowan Lake pluton, which commonly contain showings of sulphide, particularly chalcopyrite and molybdenite, are also worthy of serious investigation. Much of the north part of the pluton is affected by incipient carbonatization even where not penetratively foliated (although to a much lesser degree than the Pistol Lake stock). Given the greater dispersal (and possibly less focusing) of the early alteration, it is even more important to seek structural situations such as the contact zone itself, and late brittle faults and dilational environments affecting the early shear zones which might have enhanced the focusing of fluids.

Although the Shebandowan Lakes pluton is relatively young (Corfu and Stott 1986), it was undoubtedly affected by the sinistral shear zones and associated carbonatization. It may therefore have acted as a competent "augen" within this shear system, the relatively deformed east-projecting tail through Lower Shebandowan Lake representing one of the deformed "tails" or "wings" of the augen. The contact zone along the northeastern edge of the pluton may have been located in the "pressure shadow" during the sinistral regime, and was therefore carbonatized and sericitized even between the ankerite-sericite schist zones.

The abundance of fractures in the J.F. West area of possible "Timiskaming" age (i.e. slightly younger than the Shebandowan Pluton: Corfu and Stott 1986), may also have developed in this pressure shadow environment. Because the latter structural environment might have been modified during the subsequent dextral regime, when most of the auriferous quartz veining is thought to have been deposited, areas where shear zones and contacts appear disrupted due to the latter event may be worth examining more closely, e.g., the island in Middle Shebandowan Lake, southeast of Amp Lake, on which a molybdenum occurrence has been reported. Unfortunately, this promising area is occupied by a major lake.

However, the analogous situation might be found on the southwestern side of the Shebandowan Lake pluton, near the northwest-trending, dextral Crayfish Creek Fault, a fault which was probably active during the mineralization interval and thus itself may be important in focusing mineralization. In the area west of the contact, and extensive, differentiated mafic intrusion should perhaps be considered as part of the competent. Shebandowan Lake pluton "augen," the effects of which might therefore have extended to the rocks from upper Greenwater Lake to the west of Upper Shebandowan Lake, considering the dextral offset along the Crayfish Creek Fault."

LOC&TIOH

The claims are located on the north shore of Lover Shebandowan Lake, in Conacher and Hagey Townships, Thunder Bay Mining Division. The village of Shebandowan is approximately 5 kilometres to the east.

The Trans-Canada Highway f 11 transects the southern part of the claims. Numerous logging and hydro service roads provide interior access. A major hydro transmission lane runs east- west across the central portion of the claims and a second one just north of the claim block.

The property is centred on the Hagey-Conacher Townships line and adjoins the west boundary of the Bandore property.

8

J

Ho? La k* Property

O MM MO

SCALE ha,COO.aoo

400 ka

REBAGLIATI GEOLOGICAL CONSULTING L

North Coast Jndustri es Lf d. Voacainur, Brlriah Columbia

LOCATION MAP

Hag Lake PropertyCONACHER a HAGEY TOWNSHIP Thunder Bay Mining Division. Onrcric

January. 1988 | NTS:Oar*:

The property under study Includes many claim blocks optioned from different holders.

Hag Lake Block (Consolidated North Coast Industries Ltd.)

Claim f:

TB 557097 557101 557105 557109 557113 557119 557123 557127 557134 557143 557147 557152 557156 557922

TB 557098 557102 557106 557110 557114 557120 557124 557131 557135 557144 557115 557153 557118 886673

TB 557099 557103 557107 557111 557117 557121 557125 557132 557136 557145 557116 557154 557119 886676

TB 557100 557104 557108 557112 557118 557122 557126 557133 557142 557146 557151 557155 557917 886677

Claim i (Dan Calvert)

Block 1188031 (2 claims)

TB 1195497 TB 1195496 1183250

Claim f (Mike Fogen)

Block TB 1196232 (9 claims) 1193969 (5 claims) 1193966 (4 claims)

TB 1183248 TB 1183249

HAGEY TWP

CONACHER TWP l 4 S CONA

OT

11EVIOU8 WORK

Halverson claims

Detailed geological mapping was carried out in October 1983 on the Halverson claims by GLE Resources Ltd. IP/Resistivity, VLF-Em and Magnetometer surveys were carried out by Mattagami Lake Exploration Ltd in October and November 1980.

Hag Lake Property

1939-1961

Rochon-Maney or Ourgold Mining Company Ltd carried out significant trenching and pitting in the middle of claim TB 557151.

1945

14 drill holes were drilled by Lobanor Gold Mines Limited on the Hagey-Conacher Township boundary, south of Hag Lake. The drilling covered 1,100 feet across the metavolcanic-feldspar porphyry contacts. Lenticular shear zones in the porphyry are reported to be silicified and mineralized with some pyrite and minor chalcopyrite. Three (3) holes for which, the locations are not known, are reported to contain significant gold values.

Hole 2: 13.9 feet of 0.10 opt AuHole 6: 3.4 feet of 0.148 opt AuHole 7: 1.1 feet of 0.08 opt Au

1980

Property was staked by Greenwhich Lake Exploration Limited.

1980 December

A group of 53 contiguous claims, west of the Bandore property, were optioned by Mattagami Lake Exploration.

1981-1982

Mattagami Lake Exploration Limited carried out diamond drilling on the property controlled by Greenwhich Lake Exploration Ltd.

12

1981

Line cutting, detailed geological mapping, magnetometer, resistivity and I.P. surveys were completed prior to a diamond drilling program in the fall of 1981.

1982-1988

Lincoln Resources carried out geophysics and completed drilling, mainly on the Hag Lake zone.

1988

North Coast Industries Ltd carried out an eight (8) hole diamond drilling programme on the Hag Lake zone.

13

BEGIOHAL GEOLOGY

The Shebandowan Lakes area has been mapped by the Ontario Department of Mines, Map No. 2267.

This map sheet, at a scale of one inch to one-half mile, accompanies Geological Report 110 entitled "Geology of the Lower Shebandowan Lake Area, District of Thunder Bay" by J.A. Morin.

The area is underlain by east-west trenching metavolcanics and metasediments of Archean age, the latter principally to the north of the Postam Lake Fault. The volcanic sequence is composed dominantly of andesitic to basaltic flows with tuffaceous interbeds, but dacites, rhyolites, tuffs and metasedimentary horizons are also recorded. The grade of regional metamorphism ranges from greenschist facies in the south to amphibolite facies in the north. The volcanic sequence is cut by a number of later intrusions, the largest of which is the Shebandowan Lake quartz-diorite stock. Minor intrusives include gabbro and peridotite sills, lamprophyre and quartz-feldspar porphyry dykes.

14

ENGLISH RIVER yi

SU8PROVWCEV.

m PROTEROZOICSHEBANDOWAN

(——l SUNBAR-BATWMG LAKES COUPLEX

Ifamty volcanic Md svdlnwntarT recks

PROTEROZOIC SEDIMENTARY and MTRUSIVE ROCKS

TDMSKAMNG-TYPE* VOLCAMC and SEOMENTARY ROCKS

GRANITE. SYEMTE. MONZONTTE.DIORITE. Son* ofatona complex, and —--—awn* Inctud* mafte to ultranwllc pitas** | j'OLOER* METAVOLCANIC ROCKSMaaaiv* to foliated, yndlfforamiatad ZZZT mM METAOIA8ASE - -- FELSC

METAGREYWACKES p..s

Figure ^: Generalized geological nap of the western part of the Shebandowan Greenstone Belt. General tectonic setting shown In inset.

15

IiISATIQM

In order to carry on a systematic exploration program on the claim group adjacent zones of economic mineralization are described. The area surrounding the Bandore zone l l trenches, just east of the present study area, is underlain by mafic metavolcanic rocks cut by metadiabase and a relatively large body of feldspar porphyry. These rocks are affected by several easterly to east-northeasterly striking sinistral shear zones which have been flexed and locally intersected by slightly younger, east-southeastern striking dextral shear and fracture zones. Locally the exposed feldspar porphyry has been overprinted by a broad east- striking, sericite-carbonate-chlorite schist zone, one of the carbonatized shear zones. The mineralized zones which occur as seams along the foliation and as lenses accompanied by chlorite.

Although the extent of the surface mineralization in not great, the gold values clearly indicate that the porphyry was accessible to, and provided a depositional environment for highly auriferous fluids during or after deformation.

On the Hag Lake property hole f GW-81-1 drilled by Mattagami Lake Exploration, who had the property under option from Greenwich, intersected 0.798 oz Au/ton (uncut) and 4.01 oz Au/ton over a width of 4.03 metres on IP anomaly f 8. Subsequent drilling failed to cut similar values but numerous anomalous to economic intersections were returned, the highest being 0.42 oz Au/ton and 1.37 oz Ag/ton over 0.62 metres in hole GW-82-5. Disseminated pyrite in pillowed andesite explain the IP anomaly and gold mineralization consists of disseminated and streaky pyrite in quartz-carbonate-sericite schists. Recent holes returned the following values:

Hole 88-7: 0.122 opt Au for 1.05 metres Hole 88-8: 0.132 opt Au for 1.00 metres

0.340 opt Au for 1.01 metres0.104 opt Au for 0.75 metres

Hole 88-10: 0.260 opt Au for 0.68 metres Hole 88-12: 0.180 opt Au for 1.24 metres

16

GEOPHYSICAL TEST SURVEY

Prospecting mapping

A geophysical test survey was carried in the south central portion of the property in order to locate and detail a north- south magnetic anonaly which appears on the airborne survey flew a few years earlier by the Ministry. A total of 4.5 km of north-south lines 100 metres apart with Tielines at IS and 4+25N and Baseline O were surveyed with an OMNI IV type instruments. A base station was used to correct diurnal variations and three (3) VLF-Em 16 stations were used.

The results are presented on a series of 4 Maps at the scale of 1=2,500 in pocket.

The magnetic survey did not pick up any significant anomaly in the surveyed area. The Em surveys located numerous strong conductors which are locally displaced.

The geological mapping was conducted along the roads and zones of outcrops in order to determine the local geology. The program was carried out to aid in assessing the potential of the property for gold mineralization particularly in view of the known gold values from the Bandore property to the east.

The Halverson claims appear to be entirely underlain by the Shebandowan Lake Stock, a major quartz-diorite intrusive. Outcrop are very limited and present in the southwest part of Conacher Township and around a group of pits and trenches around line L-32S station 45+OON.

Much of the ground within the study area is low-lying and swampy, with coarse gravel to sand occasionally exposed on higher ground. Tree cover is mixed, alders black spruces in the wetter areas and re-forestation of Jack pine in the drier ground. The vertical relief rarely exceeds fifty feet. Drainage in the area is not well developed, streams being dispersed to form muskey swamps. The area is characterized by abundant glacial drift obscuring the bedrock.

17

The Hag Lake area is underlain by a succession of mafic to intermediate Archean metavolcanic with minor rhyolitic and metasedimentary horizons. For the most part, the units trend east-vest and dip steeply north. The metavolcanics include fragmentals and flows; the former predominates in the southern half of the property and are overlain by an extensive andesite to basaltic flow unit to the north which are intruded by gabbro sills, peridotite sill and minor feldspar porphyries.

Near the middle of claim TB 557151 a heavily mineralized east- west zone of blocks of massive pyrite with minor pyrrhotite was located while prospecting. In the last trench to the east a zone of shearing over 30 feet wide within the fragmentals has been intruded by a porphyry and lenticular quartz veins. Five (5) trenches, a pit and several outcrops were located in the area. The trenches exposed sheared fragmentals containing sub-rounded rhyolite clasts and pyrite clasts, only some of which may be the remains of boudinaged pyrite beds. The pyrite clasts are up to 20 cm in diameter and are quite weathered. Reading the description of the diamond drill holes on the Bandore zone f 4, it appears that this fragmented horizon may be the same intersected just north of the ore body.

A brief description of the different geological units follows:

Mafic metavolcanics

Andesite to basalt fairly massive, green colour. Flows typically pillowed comprise the majority of the sequence. Flow breccia with minor tuff and tuff breccia are present in the central part of the property close to the assume contact between mafic volcanic and felsic fragmentals.

Andesitic tuffs

Andesite tuffs are fine-grained to aphanitic green and well foliated. Minor fine lapillis and felsic to intermediate clasts are common. Slight shearing is evident, essentially parallel to the schistosity (090 degrees steep dip to the north).

18

Quartz diorite

Quartz diorite is a massive coarse grained equigranular rock of buff to grey colour, weathering light grey. Locally, chlorite and epidote alteration of mafic minerals give a greenish tinge. Close to the margin, small partly assimilated xenoliths of metavolcanics are present. The iron-stained quartz diorite becomes slightly to moderately sheared in an east-west direction with X-4% pyrite. Fine quartz veins parallel the shearing. East-west fault zones are also present.

It appears that the eastern and northeastern parts of the Shebandowan Lake pluton are affected by both ductile and brittle structures, including discrete ductile shear zones generally composite or conjugate and large and/or small scale fractures. Both brittle and ductile structures are accompanied by intense carbonate alteration and associated locally with sulphide mineralization, most commonly chalcopyrite with or without pyrite, arsenopyrite and molybdenite. Even outside these altered zones much of the northeast part of the pluton is affected by some degree of sericitization and carbonatization.

Fragmental

A thick lens of felsic fragmental with minor brecciated horizons outcrops in the central part of claim TB 557151. Clasts of rhyolite (?) with pyrite fragments are set in an andesitic matrix which is often sheared.

Quartz porphvrv

Locally cuts the quartz-diorite of the Shebandowan Lake Stock. Porphyry is pale buff and contains up to 5* pyrite.

Gabbro

Gabbroic sills are the main mafic intrusives encountered on the property along with minor lamprophyre.

The gabbro is medium grained, massive. Quartz veining is common in most of the gabbro outcrops. In places large blocks of andesite are found rafted into the gabbro near the contacts.

19

The early cycle of metavolcanic rocks and subsequent Igneous Intrusions were affected by a series of northeasterly to easterly striking, sinistral ductile shear zones, followed by the westerly to northwesterly striking dextral shear zones and minor faults. -Carbonate sericite alteration are developed along the shear zones. Quartz veining is directly correlated with gold mineralization at Bandore zone f l and Hag Lake zone.

Of the 12 IP anomalies which occurred on the property, five (f l, 2, 6, 8, 9) were drilled and returned anomalous to economic gold intersections. Anomalies f 5, 7, 10 and 11 represent good targets for drilling. Three of the anomalies (f 4, 12 and 13) have a low priority rating.

Anomaly f lo lies on strike with the Bandore feldspar porphyry which contains significant gold values over narrow width. Anomaly f li is at least 2000 meters in length and has a weak to moderate metal factor expression.

20

COST OF WORK

Line cutting and chaining

4.5 km C SSSO.OO/km .. . ..... . .... . ... . $ 1,575.00

Magnetic test survey

4.5 km 0 $175.00/kn . . ... .... . ... . . ... $ 787.50

VLF-Em 16 survey (3 stations)

4.5 km C S250.007km . . . .. . ... . .... . .. . S 1,125.00

Prospecting

15 days e $100.00/day . . . . . . . . . . . . . . . . O 1,500.00

Mapping

9 days e $350.00/day . ... . ... . . ... . . .. $ 3,150.00

Travelling 3,800 km 8 OO.SO/km ......... $ 1,140.00

Food .................................... $ 100.00

Report and drafting ..................... $ 750 . 00

Photocopies and Reproduction ............ 5 ___ 92.00

TOTAL: S io.2iQ.gn

21

CERTIFICATE OF QUALIFICATIOH8

THIS IS TO CERTIFY THAT:

I am a resident of Thunder Bay, province of Ontario, Canada (385 Riviera Drive, Box H-9, Thunder Bay, Ontario, P7B 6K2).

I have been engaged in mining exploration since 1974 and have been consulting as a professional geological engineer since 1980.

I am a graduate of Quebec University, Chicoutimi (B.Se. Eng., 1974) and Carleton University (M.Se. Geol., 1979).

I am a member of the Order of Engineers of the Province of Quebec and also a member of Prospectors and Developers Association and of the Canadian Institute of Mining and Metallurgy.

This report is based on pertinent informations from previous data and the author personal supervision of the project. The author conducted a large part of the survey.

Signed in Thunder Bay, January 29th, 1993

CLAUDE LAROUCHE, P. Eng.

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CONACHER TOWNSHIPVLF-EM16 SEATLE 21.4KHZ

( SCALE 1 - 2,500 Drafting Claude Larouche

DATE JANUARY 1933

OVALBAY GEOLOGICAL SERVICES INC.

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DATE JANUARY 1993

OVALBAY GEOLOGICAL SERVICES INC.

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DATE JANUARY 1993

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DATE JANUARY 1993

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EXECUTED BY

INTERPRETED BY

APPROVED BY

DRAWN BY

S2B09NE0003 OP92-0&* HAGEY 240

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52B09NE0003 OP92-064 HAGEY 250 i