41015SE8111 8.7716 DORE010

GEOLOGICAL SURVEY

SWAYZE PROJECT

SWAYZE, DENYES, AND DORE TOWNSHIPS,

ONTARIO

NTS: 41 O 15

RECEIVED

j AN 29 1985

MINING LANDS SECTION

Robert BellGeologistCanadian Nickel Company Ltd.Copper Cliff, OntarioDecember, 1984

i 2- ri i

SUMMARY AND CONCLUSIONS

The property consists of 359 contiguous claims, of which 237 are covered in this report, located in parts of Swayze, Denyes and Dore townships, approximately 240 km northwest of Sudbury.

A total of approximately 400 kilometres of line was cut and detail mapped at a scale of 1:2500. The claims are underlain by a synclinally folded sequence of volcanics, ranging in composition from ultramafic to felsic, and metasedi- ments. Several areas of pervasive carbonate alteration were outlined. Gold values are very low to weakly anomalous.

In many parts of the property outcrop exposure is very poor, hence prospecting by conventional methods has not upgraded or downgraded the potential for economic deposits.

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Woman Rlv*r i

FIGURE l Canadian Nickel Company Limited

SWAYZE PROJECT, ONTARIO Location MapSCALE t' 250 000

4101SSE0H1 2.7716 DORE

TABLE OF CONTENTS010C

SUMMARY AND CONCLUSIONS

I.0 INTRODUCTION

2.0 LOCATION AND ACCESS

3.0 PROPERTY

4.0 PREVIOUS WORK

5.0 REGIONAL GEOLOGY

6.0 GEOLOGICAL SURVEY

6.1 Ultramafic Rocks6.2 Mafic Volcanics6.3 Intermediate Volcanics6.4 Acid Volcanics6.5 Metasedimentary Rocks6.6 Intrusive Rocks

7.0 MINERALIZATION

8.0 STRUCTURE AND ALTERATION

9.0 CONCLUSIONS AND RECOMMENDATIONS

10.0 REFERENCES

II.0 CERTIFICATE OF QUALIFICATIONS

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666778

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FIGURES

Figure Number Scale

1 General Location Map 1:250,000

2 Claim Map . 1:50,000

3 Geology (Sheets 1-23) 1:2500

Table Number Page

l Geological Legend 5

1.0 INTRODUCTION

As a result of a study made to identify the most promising gold belts with unexplored potential, Canadian Nickel Company Limited (Canico) staked 560 contiguous claims in the Swayze township area in 1981. The present survey covers 237 contiguous claims located in parts of Swayze, Denyes and Dore townships.

The horseshoe shaped claim block covers a synclinally folded sequence of ultra mafic to felsic flows and intrusives, and metasediments. The claims were evalu ated for their gold potential by gridding and detail mapping. Any altered outcrops (carbonatized, sericitized, silicified, pyritized, quartz veins, etc.) were sampled and assayed for gold.

Favourable stratigraphy and alteration were encountered, but gold values were typically very low to only weakly anomalous.

2.0 LOCATION AND ACCESS

The property consists of 237 contiguous claims located in parts of Denyes, Dore and Swayze townships, approximately 240 km northwest of Sudbury, Ontario, and 55 km east of Chapleau, Ontario (Figure 1). The property lies within the Porcupine Mining Division. The NTS is 41-0-15.

Access is by float plane, utilizing numerous lakes located within the claim block. Airbases are located in Sudbury, Gogama, Folyet, and Chapleau.

The northeast corner of the property can now be accessed via a new gravel road, established by Heron Resources, originating in the Ivanhoe Provincial Park near Folyet, and leading to the former Kenty Mine.

3.0 PROPERTY

The property consists of 359 contiguous claims owned by Canico {Figure 2), of which 237 are covered in this report. The claims in Dore township, although contiguous with those in Swayze township, form an isolated block as the connecting claims are not gridded or included in the 237 claims under discussion.

Two years assessment work derived from a 1981 airborne geophysical survey kept the claims in good standing until April, 1984. The claims were then put under extension. Four additional claims in Denyes township were staked in 1984 to close open fractions found within the existing claim block.

The claims are as follows:

P606312.313 Recorded April 14, 1981; currently under extension to Dec. 14, 1984P606317P606320.321P606324.325P607075-080P607100-102 " " "

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Claims recorded April 14, 1981 and currently under extension to April 12, 1985:

P574149P574150P574151P574154P576194P576195P588859P588860P588861P588862P588863P588864P588997P588998P588999P589000P605017P605077P605078P605125P605126P605127P605128P605129P605130P605131P605132P605135P606243P606244P606245P606246P606247P606248P606249P606250P606251P606252P606273P606274P606308P606309P606310P606311P606318P606319

P606326 P606327 P606328 P606329 P606330 P606331 P606332 P606333 P606334 P606335 P606336 P606339 P606340 P606341 P606342 P606343 P606344 P606345 P606349 P606350 P606399 P606400 P606401 P606402 P606403 P606404 P606405 P606406 P606407 P606408 P606409 P616410 P606411 P606412 P606413 P606414 P606415 P606416 P606417 P606435 P606436 P606437 P606438 P606439 P606442 P606443

P606444 P606445 P606446 P606447 P606448 P606451 P606452 P606455 P606458 P606459 P606460 P606461 P606462 P606473 P606474 P606475 P606476 P606486 P606487 P606488 P606489 P606490 P606491 P606492 P606496 P606497 P606498 P606499 P606500 P607001 P607002 P607005 P607006 P607007 P607008 P607009 P607010 P607011 P607012 P607013 P607020 P607021 P607022 P607023 P607024 P607025

P607026 P607062 P607073 P607074 P607081 P607082 P607085 P607086 P607088 P607089 P607090 P607097 P607098 P607099 P607106 P607107 P607108 P607109 P607110 P607111 P607112 P607113 P607114 P607115 P607116 P607117 P607118 P607119 P607120 P607121 P607122 P607123 P607124 P607125 P607126 P607127 P607128 P607129 P607130 P607131 P607132 P607133 P607134 P607135 P607136 P607137

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Claims recorded April 15, 1981 and currently under extension to April 12, 1985:

P615989 P615997P615990 P615998P615991 P615999P615992 P616000P615993 P616005P615994 P616006P615995 P616007P615996 P616010

Claims staked in 1984:

P616011 P616012 P616014 P616015 P616016 P616025 P616026 P616027

P616030 P616031 P616032 P616035 P616036 P616037 P616040 P616041 P616042

P807250 Recorded June 21, 1984, due Oune 21, 1985 P808244 Recorded Aug. l, 1984, due Aug. l, 1985 P808245 P808246

4.0 PREVIOUS WORK

The discovery of the Kenty Mine in 1931 sparked considerable exploration acti vity throughout the Swayze belt. Gold mineralization at the Kenty Mine is related to quartz-carbonate veining within mafic volcanics and intrusives, and metasediments. Two ore shoots were reported to occur on surface: No. l vein - 6.3 feet wide, 50 feet long, averaging 0.39 oz/ton Au, and No. 2 - 3.7 feet wide, 72 feet long, averaging 0.67 oz/ton Au. Between 1931 and 1934, Kenty Gold Mines Ltd. sank 2 shafts, with some 6,750 feet of lateral development. The number l shaft is 510 feet deep and the number 2 shaft 534 feet deep.

The 1948 Financial Post Survey of Mines reported possible reserves of 69,000 tons in the number one shaft area and 290,000 tons in the number 2 shaft area of undetermined grade.

Vancouver based Heron Resources currently hold the property, and to date have carried out geology, soil sampling, magnetometer and IP surveys, as well as extensive stripping and trenching, dewatering of the number l shaft, and diamond drilling.

Following the discovery of the Kenty Mine, gold was subsequently found on an island in Cree Lake, and later 3500 feet east on the mainland. Gold was reported to be in a quartz-carbonate-sulfide vein system within sheared tuffs and andesite-basalts, averaging 2 feet in width. Flint Rock Mines Ltd. carried out a 34 hole drill program in 1961-62.

Gold was also discovered east of Cree Lake in the early 1930's, south of the lake referred to as Hook Lake. Buffalo-Canadian Gold Mines Ltd. trenched and stripped the showing, and carried out some drilling in the 1930's. Mineralized quartz within "silicified and carbonatized shear zones" assayed from 0.02 to 0.08 oz/ton Au.

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Goldstar Explorations Ltd. carried out an electromagnetic survey and sub sequently drilled 5 boreholes in 1964 in Denyes township.

Canadian Nickel Company Ltd. carried out an airborne geophysical survey in the fall of 1981. The magnetometer survey helped to delineate the structure of the area. A series of ultramafic flows, sills and intrusives with a broad, high magnetic signature, was outlined in a horseshoe shape, revealing the synclinal folding present. The electromagnetic survey detected only two medium strength conductors, both attributable to graphitic metasedimerits. Reconnaiss ance geological and humus sampling surveys were carried out prior to gridding.

5.0 REGIONAL GEOLOGY

The claims are underlain by Archean rocks of the Swayze greenstone belt. The belt is about 45 km long and 29 km wide and is truncated at its western extre mity by the Kapuskasing structural zone; the Michipicoten-Wawa belt is probably the westerly equivalent or extension of the Swayze belt west of the Kapuskasing structure. To the east the belt bifurcates, with one arm trending towards the Porcupine area of the Abitibi belt, and the southern arm trending towards Gogama and Shiningtree.

The claims cover a large east-west synclinal structure, which appears to close near the west end of the property. The syncline is slightly overturned, as all structures dip steeply to the north, and plunges to the west. The location of the synclinal axis was traced with the aid of stratigraphic tops indicators such as graded bedding and pillow facings. On the north limb such features face south, but since they dip steeply north, the structure must be overturned.

Basal to the section is a series of ultramafic to mafic flows, sills and intru sives. These are overlain by a series of mafic to felsic flows, frequently fragmental, and tuffs. Several metasedimentary horizons are also present. The core of the syncline is occupied by a thick section of felsic volcanics and intrusives, primarily feldspar porphyritic rhyolites. The section is intruded by numerous dykes and sills of quartz-feldspar porphyry, and 2 minor granite plutons. A broad band of northeast trending metasediments crosses the west end of the property. A strongly magnetic northeast trending diabase dyke crosses the northwest portion of the claim block, slightly obscuring the magnetic interpretation of the western closure of the syncline.

6.0 GEOLOGICAL SURVEY

A total of approximately 400 km of line at 100 m line spacing was cut in Dore, Denyes and Swayze townships to facilitate the geological survey. Pickets were marked at 25 m intervals along the lines. The field data was plotted at the scale of 1:2500 and copies of the maps are appended.

Four additional claims were added to the claim block during the field season. Three were staked in the southwest corner of the block, east of Sylvanite Lake to close a gap in the original staking. A fourth claim was picked up in the northwestern part of the block. This claim had been held by foreign interests at the time of the original staking.

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The table below outlines the rock units mapped. Note that no age connotation is implied as volcanism is cyclical. A description of the rock units follows:

TABLE l

LEGEND

6) INTRUSIVE ROCKS 6e lamprophyre6d alkalic aphanitic sill, dykes 6c diabase 6b granite 6a quartz-feldspar porphyry

5) METASEDIMENTARY ROCKS5f felsic polymictic conglomerate5e alkalic conglomerate5d grit, conglomerate, reworked tuff5c quartzite5b shale, argillite, siltstone, interflow sediments5a chert, interflow sediments

4) ACID VOLCANICS4f chlorite-carbonate-sericite schist4e quartz-feldspar-sericite schist4d fragmental4c felsic tuff4b porphyritic rhyolite4a massive rhyolite

3) INTERMEDIATE VOLCANICS3d fragmental, locally reworked intermediate conglomerate3c intermediate tuff3b porphyritic andesite-dacite3a massive andesite-dacite

2) MAFIC VOLCANICS2h granitized basalt2g agglomerate2f fragmental2e basic tuff2d gabbro-thick flow2c porphyritic basalt2b pillowed basalt2a massive basalt

1) ULTRAMAFIC ROCKSle flowtop rubble/brecciaId high MgO basaltle serpentinitel b peridotite {^pyroxenite)la ultramafic flows (komatiite)

Note that tuffs have not been mapped as discrete units; in order to distinguish their composition they are classified as mafic, intermediate, or acid tuffs and coloured accordingly.

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6.1 Ultramafic Rocks

The ultramafic rocks occur as a series of ultramafic flows and subvolcanic sills intercalated with mafic flows. Flow textures were found only in the southeast portion of the block, southeast of Dyment Lake, as far west as claim P616025.

The komatiites are characterized by pyroxene spinifex with skeletal crystals ranging in size from l mm to 8 cm. Stratigraphically above^the spinifexoid horizons are flow top breccia-rubble zones, up to several metres thick, con sisting of numerous highly packed subrounded fragments of ultramafic material, often spinifexoid. The rubble zones often grade into poorly developed ultra mafic to (high MgO) basaltic pillows. The entire sequence grades, both laterally and vertically, into "normal" basalts.

Along the north limbs of the syncline no ultramafic rocks were seen. Magnetic mafic rocks occur as intrusives or subvolcanic sills, which are fine to medium- grained and typically oxide rich (magnetite) quartz gabbros in composition.

6.2 Mafic Volcanics

The most frequently exposed rock type on the property is basaltic in compo sition, occuring as massive flows, pillows, tuffs, fragmentals and agglomerate.

The typical basalt is fine-grained, massive, and variably foliated. Pillows are generally absent or poorly developed and hence are poor tops indicators.

Frequently fine-grained basalts can be found which grade into medium-grained varieties, probably representing thick flow centres. Medium to coarse-grained gabbroic basalts, frequently magnetic, are common northwest of Brett Lake.

These coarse-grained basalts are typically oxide rich (magnetite) quartz gabbros, interpreted to be thick flows, and responsible for the broad high magnetic zones delineated by the air magnetometer survey.

Locally the basalts are feldspar porphyritic, with phenocrysts up to several centimetres in size. Fragmental flows are also found locally. Subangular frag ments of basalt and andesite, generally several centimetres in size, occur in a matrix of fine-grained basalt. Finely bedded to massive ash and lapilli tuffs are probably more common than indicated; they are frequently indis tinguishable from mafic flows.

Thin conformable interflow sedimentary horizons are often found between indi vidual basalt flows. These are generally chert and argillite-siltstone. It is assumed many more such horizons are present but not encountered due to their recessive weathering, especially along contacts.

6.3 Intermediate Volcanics

Andesites and dacites were lumped together as intermediate volcanics for mapping purposes. These rocks generally occur as transition phases between the basalts and rhyolites, hence are often located Stratigraphically below

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the felsic volcanics. They are typically pale green to greenish-white on weathered outcrops, and light green on the fresh surface. The flows are fine grained, and typically massive. However, a broad band of fragmental andesites {lapilli tuffs) trends easterly north of Brett Lake. Intermediate to felsic subangular fragments, up to several centimetres in size, are found in a matrix of andesitic composition. The fragments are usually aligned subparallel to parallel to the predominant regional foliation. Locally these fragmental s appear reworked, and are hence actually conglomeratic in nature.

6.4 Acid Volcanics

Acid volcanics are very common in the Swayze area. The core of the syncline is occupied by a thick section of rhyolite flows and intrusives, frequently feldspar porphyritic. The claims cover the favourable stratigraphy basal to the acid volcanics, on both limbs of the syncline. Numerous thin lenses and horizons of acid volcanics are intercalated with the basal basalts and koma- tiites. Metasediments such as shales and sandstones appear to have a spatial relationship with the acid volcanics.

Massive rhyolite flows are typically white weathering and white to whitish brown or green on the fresh surface. Subhedral phenocrysts of feldspar, up to several millimetres in size, are very common. The rhyolites are frequently strongly foliated and sericitized, such that they were mapped as sericite schists. Such alteration makes it impossible to distinguish between acid flows and tuffs. Carbonatization along foliation planes is also very common, giving the rocks a rusty weathering colour.

As mentioned above, (feldspar) crystal tuffs are fairly common but difficult to distinguish from feldspar porphyritic flows. Fragmental rhyolite flows can also be found, with angular to subangular fragments of rhyolite, and occasionally chert, within a rhyolite matrix.

Waterlain lapilli tuffs with interstitial pyrite {up to 650 are very common in the northeast corner of the property, in Dore township.

6.5 Met a sedi me ntary Rocks

Metasediments within the claim area represent approximately ID-15% of the rocks exposed. They can be divided into 2 major types:

a) thin interflow sediments representing short breaks or hiatuses between volcanic cycles, and

b) major sedimentary "breaks" representing a lengthy period of erosion and volcanic quiescence.

Metasediments of section (b) occur as a broad band which trends east-west south of Cree Lake, then swings northwest through Halcrow township then north east through Denyes township, crossing to the north of the northwest corner of the claim block. This horseshoe shape mimics the structural sequence found within the claim block, and hence may represent a synclinally folded section basal to the rocks within the claim block.

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Metasediments outcropping on the property include:

5a) and 5b) interflow cherts, shales, argillites, and siltstones, found inter calated with volcanic flows. One such horizon in the northwest corner of the property can be traced for l kilometre.

5c) and 5d) quartzites, grits, reworked tuffs. These rocks occur as uncon formable lenses within the volcanics, especially the acid volcanics. They are probably derived from paleotopographic high acid centres and domes. An interesting assemblage of drag folded shales, greywackes, and sandstone is interfingered with acid and basic volcanic rocks in the southwest corner of the property south of Dyment Lake.

5e) "syenitic agglomerate" - this unit, the most unique formation on the pro perty, makes an excellent marker horizon. In hand specimen, it resembles a diatreme breccia, however it occurs as a conformable horizon up to 150 metres thick and can be traced for over a kilometre, south of Dyment Lake. Angular fragments of brick red, fine-grained, occasionally feldspar porphyritic syenite(?) are hosted in a chloritic glassy matrix. Lesser amounts of pyroxene- rich basalt fragments are also present, and to the west subrounded quartz pebbles are present. Pseudo-graded bedding is exhibited, with fragments ranging from metre size blocks to lapilli and ash size. The unit is probably a high- energy agglomerate {the syenitic fragments having been ripped up at depth), although locally it resembles a lapilli or ash tuff.

5f) felsic polymictic conglomerate. This is also a fairly high-energy sedi mentary rock, found interbedded with massive rhyolite flows, north of Freymond Lake and not on the present grid. Subangular to rounded fragments of slate, argillite, chert, quartz, and rhyolite, ranging in size from one millimetre to several centimetres, are hosted in a fine-grained felsic matrix. The rock contains S-5% fine-grained disseminated pyrite and is weakly carbonatized. Pyrite has also replaced fragments of slate and argillite.

6.6 Intrusive Rocks

Intrusive rocks within the claim block can be divided into 4 major types.

a) Quartz-feldspar-porphyry - the claim area is intruded by innumerable sills and dykes of feldspar-quartz porphyry, ranging in width from less than l metre to 50 metres. Individual sills can be traced for up to 1.3 km. These rocks are white to pinkish white both on the fresh and weathered surfaces with numerous phenocrysts of feldspar and locally of quartz. They are dacitic to rhyolitic in composition. There may be a genetic relationship between these rocks and some of the fragmental and or porphy ritic andesite-dacite flows as the two are often on strike with each other. North of Brett Lake a 200 metre wide unit mapped as intrusive porphyry may be a porphyritic acid volcanic flow.

b) Diabase - a major diabase dyke, up to 75 metres wide, crosses the property at 060 to 070 . The diabase is coarse-grained, extremely friable and strongly magnetic. It can be mapped for 9 km across the property and has been traced via geophysics (mag) along strike south of Timmins, through Lake Abitibi and on into Quebec. A thinner northwesterly trending arm branches off the main dyke north of Dyment Lake.

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c) Alkalic, aphanitic sills, dykes - these rocks are very fine-grained to aphanitic, with a chilled, quenched appearance. They are generally wine coloured, often magnetic, and contain minor amounts of pyrite. They may represent quenched oxide-rich gabbros.

d) Lamprophyre - a black, medium-grained magnetic biotite lamprophyre dykeoutcrops west of Swayze Lake. The magnetic survey suggests that the dyketrends at 135 .

7.0 MINERALIZATION

Northeast of Swayze Lake a carbonate alteration zone was discovered on claim 607130. Highly carbonatized mafic and felsic tuffs with disseminated pyrite (up to 530 host a number of large quartz veins trending at about 340 and 070 . The veins carry variable amounts of pyrite and chalcopyrite (up to 5ft). All Au assays were low, the highest being 15 ppb.

The gridded claims in Dore township cover felsic lapilli tuffs with an inter stitial pyrite content of up to 6ft. Such rocks are locally anomalous 1n gold, with typical values of 50-80 ppb and a high of 2.12 ppm. A persistent set of thin north-south trending quartz veinlets is present which also carry weakly anomalous gold values.

8.0 STRUCTURE AND ALTERATION

The rocks in the claim area have been folded into a slightly overturned syn cline; all units dip steeply north, and yet pillow facings and graded bedding give contradictory tops on opposite sides of the syncline. Small draa folds indicate that the syncline has a north-westerly plunge, typically 65 towards 3200 .

The ground magnetometer survey indicates that local shearing and faulting is common. Only 2 major faults are obvious. Both trend 340-350 , and both are sinistral with apparent offsets of approximately 500 metres. One fault crosses the eastern end of the Cree Lake grid, passes through the northwest arm of Brett Lake and off the property. The second fault runs up the southeast arm of Dyment Lake. The ground mag survey readily identifies this fault.

The regional structure is well reflected within the outcrops exposed along the shores of the long lake south of Dyment Lake. Intercalated volcanics and sediments show rapid facies variations and are drag folded, Z style, showing a plunge of roughly 65 to the northwest. This suggests an anticlinal axis to the south, which is shown to exist on ODM map 2221. The area is pervasively carbonatized but no anomalous gold values were recorded.

All the rock names used in this report should be prefixed with a "meta", as a regional metamorphism of lower greenschist facies is present. Locally the rhyolitic tuffs and flows, and mafic and ultramafic rocks, have undergone varying degrees of iron-carbonatization. The ultramafic rocks are frequently serpentinized, and locally have undergone a talc-chlorite-carbonate alteration. The rhyolitic rocks have experienced varying degrees of sericitization.

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11.0 CERTIFICATE OF QUALIFICATIONS

I, Robert C. Bell, of the City of Sudbury, in the Province of Ontario,

HEREBY CERTIFY:

1. That I reside at 1149 Southview Drive, Sudbury, Ontario, P3E 217.

2. That I am a graduate of the University of Western Ontario, London, Ontario with a degree of Bachelor of Science (1980).

3. That I am a Geologist with the Canadian Nickel Company Limited (subsidiary of Inco Limited) of Copper Cliff, Ontario, POM 1NO.

4. That I have practised my profession as a geologist since 1980, having worked in British Columbia, Ontario, Quebec and the Northwest Territories.

5. That I visited the areas discussed in this report and that the work described in this report was carried out under my supervision.

6. That I am an associate of the Geological Association of Canada.

Dated at Copper Cliff, this 21st. day of January, 1985.

Robert CrBeTT

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9,0 CONCLUSIONS AND RECOMMENDATIONS

The claims are underlain by a folded sequence of volcanics and metasediments intruded by late porphyry dykes. The volcanic rocks range in composition from ultramafic to felsic. Favourable alteration such as carbonatization was observed in several areas. Gold values are only rarely anomalous.

Outcrop exposure is generally poor, especially at the western end of the pro perty. Hence vast areas of the property remain essentially unexplored and would require further evaluation via (basal till) reverse circulation drilling, IP, etc.

10.0 REFERENCES

Cunningham, L.J. (1982): Report on the Swayze Township property of Troudor Resources Inc., O.G.S. Assessment Records, Timmins, Ontario.

Donovan, J.F. (1965): Swayze and Dore Townships, O.G.S. G.R. No. 33.

Evelegh, F.J. (1982): Report on Geophysical Surveys, Sylvanite Group ofClaims, Denyes Township, Porcupine Mining Division, Province of Ontario, O.G.S. Assessment Records, Timmins, Ontario.

Lewin, E.M. (1962-63): Drill Logs, Flint Rock Mines Ltd., Swayze Township, O.G.S. Assessment Records, Timmins, Ontario.

MacQuarrie, D.R., and Sheldrake, R.F. (1982): VLF-EM and Magnetometer Survey on the Cree Lake Gold Prospect of Troudor Resources Inc., O.G.S. Assessment Files, Timmins, Ontario.

McKechnie, D.L. (1962): Report on Flint Rock Mines Ltd., Swayze Township, O.G.S. Assessment Records, Timmins, Ontario.

Northern Miner Press Ltd., April 12, 1984; "The Northern Miner".

Phelan, L.G. (1964): Drill Logs, Goldstar Ltd., O.G.S. Assessment Records, Timmins, Ontario.

Rickaby, H.C. (1934): Swayze Gold Area, O.D.M. AR 43, Part 3.

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FIGURE 2 Canadian Nickel Company Limited

SWAYZE PROJECT, ONTARIO Claim Location Map

SCALE P5OOOO

Canadian Nickel Company LimitedCopper Cliff * Ontario POM 1NO

REGISTERED MAIL

January 23, 1985

Mr. F. W. MatthewsSupervisor, Projects SectionMinistry of Natural ResourcesRoom 6450Whitney Block, Queen's ParkToronto, OntarioM7A 1X1

Dear Mr. Matthews:

Enclosed is a geological report in duplicate being submitted under the Special Provisions Section as assessment work on the following 237 claims located in Swayze, Denyes, and Dore Townships, Porcupine Mining Division,

P574149 P574154 P576194 P588859 P588997 P605017 P605077 P605125 P605135 P606243 P606273 P606308 P606317 P606324 P606339

•51 incl.

•95•64 incl.•9000 incl

•78•32 incl.

•52 incl.•74•13 incl.•21 incl.•36 incl.•45 incl.

P606349 P606399 P606435 P606442 P606451 P606455 P606458 P606473 P606486 P606496 P607001 P607005 P607020 P607062 P607073

•50•417 incl,•39 incl.•48 incl.•52

•62 incl.•76 incl.•92 incl.•500 incl•02•13 incl.•26 incl.

•82 incl.

P607085 P607088 P607097 P607106 P615989 P616005 P616010 P616014 P616025 P616030 P616035 P616040 P807250 P808244

•86•90•102 incl.•37 incl.•6000 incl•07 incl.•12 incl.•16 incl.•27 incl.•32 incl.•37 incl.•42 incl.

•46 incl.

The report of work covering this submission was forwarded to the Mining Recorder in Timmins and subsequently recorded on December 11, 1984.

I trust that this report will be considered satisfactory by your department.

Yours

W. V. Rodney Exploration Departr

IM/nk

RECEIVED

JA * 2 l J 1985

WINING LANDS SECTION

Exploration subsidiary of

INCO LIMITED

41015SE8111 2 .7716 DORE 900

Mining Lands Section

Control Sheet

File No s3. 77/6-

TYPE OF SURVEY GEOPHYSICAL ^ GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

MINING LANDS COMMENTS:

Signature of Assessor

Date

1985 03 OG Your File: 530/84 Our File: 2.7716

Mining RecorderMinistry of Natural Resources60 Wilson AvenueTliiiwins, OntarioP4N 2S7Dear Sir;RE; lw tice of Intent dated February 8, 1985

Geological Survey on Mining Claims P 574149, et.aal., 1n Swayze, Denyes 4 Dore Townships

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours sincerely,

S.E. YundtDirectorLand Management Branch

Whitney Block. Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-4888

S. Hurst:me

cc: Canadian Nickel Company Limited Copper Cliff, Ontario POM 1NO Attention: I.D. McCasklll

cc: Mr. G.H. FergusonMining ft Lands Commissioner Toronto, Ontario

Encl.

cc: Resident Geologist Timmins, Ontario

Ministry of Natural

jurcesOntario

Technical Assessment Work Credits Date

1985 02 08

File2.7716

Mining RecorderU Reop/t of Work No. 530/84

Recorded Holder

CANADIAN NICKEL COMPANY LIMITEDTownship or Area

SWAYZE. DENYES. DORE TOWNSHIPS

Type of survey and number ofAssessment days credit per claim

i . —— . ————————————————————————i Geophysical1* Elartrnmagnatic

1 Mflf)nttnmat"l: -

lppHinmatrlr

f-;

'Sil:

1 nth.rt", P::':

days

days

days

days

days

.g Section 77 (19) S** "Mining Clalmt AitetMd" column

l' 40| Geologicali: :-" ftanohemiral1

l Man days Q Airborne

Special provision ED Ground

*

days

days

D

0

JH Credits have been reduced because of partialcoverage of claims.

CD Credits have been reduced because of correctionsto work dates and figures of applicant.

#' ;V,::

Mining Claims Assessed

P 574151-54576194-95588859 to 864 incl.588997 to 9000 incl.605017605077-78605125 to 131 incl.605135606244 to 252 incl.606273-74606308 to 313 incl.606317-18606325 to 336 incl.606339-40-41-42606344-45-49-50-99606400-01-02-03-06-07606409 to 417 incl.

P 607098-99-100607106 to 125 incl.607127 to 137 incl.615992 to 6000 Incl.616005-06-07616010-11-12-14-15616025-26-27-30-31-32616035-36-37-40-41-42807250808244-45

606435 to 439 incl. 606442-43-44-46-47-48-51-52-55606458 to 462 incl. 606473 to 476 incl.606486 to 492 incl.606496 to 500 incl.607001-02607005 to 013 incl.607020 to 025 incl.607062607073 to 082 incl.607085-86-88-89-90

Special credits under section 77 (16) for the following mining claims

30 DAYS CREDIT

P 605132 606243606319-24-43 606404-08 607026-97

P 607101-02-26 615^89-90-91

20 DAYS CREDITP 574149-50

606320-21 606405-45 616016 808246

credits have been allowed for the following mining claims

LJ not sufficiently covered by the survey Q Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:

Ministry ofNaturalResources

1.985 02 089, -111 (o

Your File: 5 30/84

Mining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at 416/965-4888.

Yours sincerely,

;.E. YundtDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3S. Hurst:mc

Encls.

cc: Canadian Nickel Company Limited Copper Cliff, Ontario POM l NO Attention: I.D. McCaskill

cc: Mr. G.H. FergusonMining 4 Lands Commissioner Toronto, Ontario

845

Ministry ofNaturalResources

Ontario

Notice of Intent

for Technical Reports

1985 02 08

2.7716/530-84

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

846 (82/5)

\

•if

SCHEDULE A

P574149P574150P574151P574154P576194P576195P588859P588860P588861P588862P588863P588864P588997P588998P588999P589000P605017P605077P605078P605125P605126P605127P605128P605129P605130P605131P605132P605135P606243P606244P606245P606246P606247P606248P606249P606250P606251P606252P606273P606274P606308P606309P606310P606311P606312P606313P606317P606318

P606319P606320P606321P606324P606325P606326P606327P606328P606329P606330P606331P606332P606333P606334P606335P606336P606339P606340P606341P606342P606343P606344P606345P606349P606350P606399P606400P606401P606402P606403P606404P606405P606406P606407P606408P606409P606410P606411P606412P606413P606414P606415P606416P606417P606435P606436P606437P606438

P606439'P606442P606443P606444P606445P606446P606447P606448P606451P606452P606455P606458P606459P606460P606461P606462P606473P606474P606475P606476P606486P606487P606488P606489P606490P606491P606492P606496P606497P606498P606499P606500P607001P607002P607005P607006P607007P607008P607009P607010P607011P607012P607013P607020P607021P607022P607023P607024

P607025P607026P607062P607073P607074P607075P607076P607077P607078P607079P607080P607081P607082P607085P607086P607088P607089P607090P607097P607098P607099P607100P607101P607102P607106P607107P607108P607109P607110P607111P607112P607113P607114P607115P607116P607117P607118P607119P607120P607121P607122P607123P607124P607125P607126P607127P607128P607129

P607130P607131P607132P607133P607134P607135P607136P607137PSI 5989P615990P615991P615992PSI 5993PSI 5994PSI 5995PSI 5996PSI 5997PSI 5998PSI 5999PSI 6000PSI 6005P616006P616007P616010P616011P616012P616014P616015P616016P616025P616026P616027P616030P616031P616032P616035PSI 6036P616037P616040P616041P616042P807250P808244P808245P808246

Total = 237

Ministry o!NaturalResources

Ontario

t.-

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

f"3 3 l O/

' ^.^ \i

The Mining Act

Instructions: — Please type or print.— If number of mining claims traversed

exceeds space on this form, attach a list. Note: — Only. days credits calculated in the

"Expenditures" section may be entered in the "Expend. Days Cr." columns.

- Do not use shaded areas below.Type of Survey(s)

GEOLOGICALClaim HolderU)

CANADIAN NICKEL COMPANY LIMITEDAddress

COPPER CLIFF. ONTARIO POM 1NOSurvey Company . Date of Sur

CANADIAN NICKEL COMPANY LIMITED ' fflv l W*Nome and Address of Author (of Geo-Technical report)

J. PERRY c/o CANADIAN NICKEL COMPANY LIMITED

Township or Area

SWAYZE .DENYES, DORE TWPS.Prospector's Licence No.

A 17527

vey (from St to), 84 30 , 08 841 Yr. Bay \ Mo. \ Y r.

Total Miles of line Cut

412 km

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Expenditures (excludes power 5 t fiftf?i n6*

Days perClaim

40

Days per Claim

Days per Claim

K K n M f?Type of Work Performed \ [j) {3 ^ lia U V te

Performed on Claim(s) OtU * * tiB4i

A.M.7iftiOilOtll l2il|2|~o|4

Calc ulation of Expenditure Days Credits

Total Expenditures

s . * 15

cTotal

)ays Credits

Instructions Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

ip.

Date RecqrdecLHolder or Agent (Signature)

Dec. 4, 1984 J 'j? W40&S4&/

Mining ClaimPrefix j Number

SE!E SCHEDULE '

1f.

-ft-E^-O-

DEC lRfcciot No

Expend. Days Cr,

A"

R—— H

-i&im

* p E\ — s? — t

1 figtfrf

1

EOf

^

i

Mining ClaimPrefix

CE1c u

19

INDS

Total nu claims cc report of

For Office Use OnlyTotal Days Cr. Dais-"Becorded Recorded 1 j .f l&tf/t

yfl *)(J Date Approved at'Reco/ded

Number

Vft) —————

4984 — —

SECTION

Expend. Days Cr.

Tiber of mining vered by this l)"i~l work. '

-"T S

^•^:. /?,^S2S2Sr/

Certification Verifying Report of Work1 hereby certify that 1 have a personal or witnessed same during and/or after

and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work its completion and the annexed report is true.

Name and Postal Address of Person Certifying

I. D. McCASKILL c/o CANADIAN NICKEL COMPANY LIMITED

COPPER CLIFF, ONTARIODate Certified

POM 1NO Dec. 4, 1984Certified by (Signature) s -s S

G2 (81/9!

SCHEDULE A

P574149 P574150 P574151 P574154 P576194 P576195 P588859 P588860 P588861 P588862 P588863 P588864 P588997 P588998 P588999 P589000 P605017 P605077 P605078 P605125 P605126 P605127 P605128 P605129 P605130 P605131 P605132 P605135 P606243 P606244 P606245 P606246 P606247 P606248 P606249 P606250 P606251 P606252 P606273 P606274 P606308 P606309 P606310 P606311 P606312 P606313 P606317 P606318

P606319 P606320 P606321 P606324 P606325 P606326 P606327 P606328 P606329 P606330 P606331 P606332 P606333 P606334 P606335 P606336 P606339 P606340 P606341 P606342 P606343 P606344 P606345 P606349 P606350 P606399 P606400 P606401 P606402 P606403 P606404 P606405 P606406 P606407 P606408 P606409 P606410 P606411 P606412 P606413 P606414 P606415 P606416 P606417 P606435 P606436 P606437 P606438

P606439 P606442 P606443 P606444 P606445 P606446 P606447 P606448 P606451 P606452 P606455 P606458 P606459 P606460 P606461 P606462 P606473 P606474 P606475 P606476 P606486 P606487 P606488 P606489 P606490 P606491 P606492 P60649S P606497 P606498 P606499 P606500 P607001 P607002 P607005 P607006 P607007 P607008 P607009 P607010 P607011 P607012 P607013 P607020 P607021 P607022 P607023 P607024

P60702B P607026 P607062 P607073 P607074 P607075 P607076 P607077 P607078 P607079 P607080 P607081 P607082 P607085 P607086 P607088 P607089 P607090 P607097 P607098 P607099 P607100 P607101 P607102 P607106 P607107 P607108 P607109 P607110 P607111 P607112 P607113 P607114 P607115 P607116 P607117 P607118 P607119 P607120 P607121 P607122 P607123 P607124 P607125 P607126 P607127 P607128 P607129

PS'07130 P607131 P607132 P607133 P607134 P607135 P607136 P607137 P615989 P615990 P615991 P615992 P615993 P615994 P615995 P615996 P615997 P615998 P615999 P616000 P616005 P616006 P616007 P616010 P616011 P616012 P616014 P616015 P616016 P616025 P616026 P616027 P616030 P616031 P616032 P616035 P616036 P616037 P616040 P616041 P616042 P807250 P808244 P808245 P808246

Total * 237

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s). GeologicalTownship or Ar.a Swayze. Denyes. Dore Twps. ClaimHolder(s). Canadian Nickel Company Limited

Copper Cliff, Ontario POM 1 NO______ Surveycompany Canadian Nickel Company Limited——-^—- Author of Report R- Be11 ' c/0 Canadian Nickel Company Address of A,.thnr Limited. Copper Cliff. Ontario POM 1NO

June 1 - August 30, 1984————Covering Dates of Survey.

Total Miles of Line rut 412 km(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

Electromagnetic.

Magnetometer.

Radiometric

Other-^————.

DAYSper claim

Geological.

Geochemical.

40

AIRBORNE CREDITS (Special provision credit* do not apply to airborne surveys)

Magnetometer. .Electromagnetic. . Radiometric(enter day* per claim)

PATF.! J an- 25, 1985 SIHMATTTRF.; ' *fc- ^JjAtrtKbr of Report or Agent

Res. Geol.. .Qualifications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

'(prefix)' (number)

See Schedule "A"

m

l

TOTAL CLAIMS. 237

837 (6/79)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations _________________________Number of Readings — Station interval ____________________________Line spacing.————Profile scale ———-———^—-——-—-——-—-—--—^-————^———————^——..Contour interval.

Instrument ——yf. Accuracy — Scale constant.

Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ___

ELECTROMAGNETIC

Instrument

Coil configurationToil spparatinn

AccuracyMethod: CD Fixed transmitter D Shoot back Q In lineFrequency , . ~...... ,,,, — ,,,.. ,,,... ,,, , ,— ...- .,.,.,,,—.

(specify V.L. F. station)

D Parallel line

—————— 4Parameters measured.

Instrument.Scale constantCorrections made.

^ Base station value and location .

Elevation accuracy.

Instrument -—^—Method D Time Domain D Frequency Domain Parameters - On time __________________________ Frequency —————

— Off time __________________________ Range ———————— Delay time.——————————————————————————

— Integration time —————..^———-—————^— Power.____-_____________________________.—————————————a*

D Electrode array —Q"Z E lectrode spacing .

Type of electrode

SELF POTENTIAL

Instrument_______________________________________ Range.Survey Method ———————————————————————————————————————————

Corrections made.

RADIOMETRIC

Instrument-——.Values measured.

Energy windows (levels) ———^^—^^-^^^—-—————————^^-^—^^^———— Height of instrument___________________________Background Count. Size of detector———-———————^^—^—^^——————————^^^^^—.—..———-Overburden ———.--———.-—.——-—.^^^^——————-—-——-™—.——.—...——

(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

1 Type of survey——————————————————————

Instrument ^——————-—-^—^^^——————-^

Accuracy.^-—™--^^^^^——-——————-————-Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

Type of survey(s)____

Instrument(s) —————(specify for each type of survey)

Accuracy-——————————^-—.^——(specify for each type of survey)

Aircraft used^-———————-.———————....————.——-—..

Sensor altitude-Navigation and flight path recovery method.

Aircraft altitude_________________________________Line Sparing Miles flown over total area________________________Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material)

Average Sample Weight——————— Method of Collection————————

Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain————————

Drainage Development———————————— Estimated Range of Overburden Thickness.

ANALYTICAL METHODSValues expressed in: per cent

p. p.m. p. p. b.

D D D

Cu, Pb,

Others—

Zn, Ni, Co, Ag, Mo, As.-(circle)

Field Analysis (.Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. ^^———^——.

SAMPLE PREPARATION(Includes drying, screening, crushing, aihing)

Mesh size of fraction used for analysis ————

Extraction Method. Analytical Method . Reagents Used——

Commercial Laboratory (- Name of Laboratory— Extraction Method- Analytical Method —— Reagents Used -^—^—-

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File

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1984

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