41015SW0ei4 a.6236 RANEY 010

Geological Report

of the

Raney Township Property

Swayze Gold Belt

Porcupine Mining Division

Ontario

DEC 2 8 1983

M'. . . *

for

DORE EXPLORATIONS INC.

by

Don Hillier, B.Se. R.S. Middleton, P.Eng.

November, 1983

41015SW0014 2 .6236 RANEY

TABLE OF ov n j. jj it j. o

Page No.

Summary. ........................ i

Introduction. ..................... l

Location and Access .................. l

Property. ....................... l

Topography S Vegetation ................ 2

Previous Work ..................... 2

Survey Method ..................... 4

Regional Geology. ................... 5

Property Geology. ................... 6

Conclusions S Recommendations ............. 14

References. ...................... 15

Certificate

010C

Figure l Figure 2

Table l

Map #1

List of Figures

Location Sketch Claim Sketch

List of Tables

Table of Formations

List of Maps

Geological Survey Map

- i -

SUMMARY

The Raney Lake property of Dore Explorations Inc. consists

of thirty four (34) contiguous, unpatented, 40 acre mining

claims. The claims are located in Raney Township, District of

Sudbury, Porcupine Mining Division, Northeastern Ontario. A

geological survey was carried out during the months of September

and October, 1983 and the property was found to be underlain by

felsic igneous rocks, intermediate and basic metavolcanics,

felsic to intermediate metavolcanics, water lain felsic tuff,

cherty sediments, felsic lapilli tuff, agglomerate and small

gabbroic and "dioritic" intrusives. Zones of pyrite

mineralization and carbonate alteration were also observed. The

property is associated with magnetic high gradient areas that

link to known occurrences of iron thoeliites and ultramafics in

other parts of Raney and Rollo Township (to the east). A

follow-up program of I.P., magnetometer and some trenching is

recommended.

INTRODUCTION

This report has been prepared at the request of Irwin

Pasternak, President of Dore Explorations Inc. A detailed

geological survey was carried out on the group of thirty four

(34) claims located in the Raney Lake Area, District of Sudbury,

Ontario, in October 1983.

A cut grid at 120 meter line spacing was established on the

property during August - September, 1983 and was used for

location during the geological survey. The geological survey was

conducted by and under the supervision of Don Hillier B.Se. with

assistance by Dave Hurst B.Se. The purpose of this report is to

describe the mapping results.

LOCATION AND ACCESS

The property is located in north-eastern Ontario at latitude

47" 47' and longitude 82* 45' or approximately 32 miles southwest

of Foleyet, Ontario (see figure #1). The property is located on

the west side of Raney Lake and extends westward to the Ivanhoe

River.

The property is accessible via float plane leased at Ivanhoe

Lake which is located 4 miles southwest of Foleyet.

PROPERTY

The property described in this report consists of 34

contiguous, unpatented, 40 acre mining claims located in the

Raney Lake Area, Porcupine Mining Division, Ontario; and are

described as follows:

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From RanevTwo. claim sheet no. M 1069

ROBERT S MIDDLETON EXPLORATION SERVICES INC

DORE EXPLORATIONS INC.T,Ile RANEY TOWNSHIP PROPERTY

PORCUPINE MINING DIVISION

CLAIM INDEX MAPNOV. 88

P CJ

l* -1/2 ail*

Approved

FK3.2M.S.F,Ir M-S

- 2 -

Claim Nos. No. of Claims Date Recorded

591339 - 342 inclusive 4 March 24, 1982

636035 l March 24, 1982

636272 - 276 inclusive 5 March 30, 1982

724304 - 310 inclusive 7 June 15, 1982

724322 - 338 inclusive 17 June 15, 1982

These claims are currently being held in trust by Ingamar

Explorations Limited for Dore Explorations Inc., in the names of

the claim stakers and at this time are in the process of being

transferred to Dore Explorations Inc.

TOPOGRAPHY 6 VEGETATION

The Dore Explorations Raney Lake claim group lies within an

elevated ridge valley type setting. Relief is about 100 feet

with local elevations up to about 180 feet above lake level

(Raney Lake). Most of the property is masked by glacial till and

outwash with most outcrops confined to the edges of ridges.

The Dore property is flanked by the Ivanhoe River to the

west and Raney Lake located to the southeast. A series of small

lakes trend through the central northeast axis of the property.

Jackpine, spruce, balsam, birch, cedar and poplar are the

principal tree mixture covering the property.

PREVIOUS WORK

A review of the assessment work files in the Timmins

Resident Geologists' office reveals that no previous work has

- 3 -

been submitted on any portion of the Dore Explorations claim

group. The earliest work in the Swayze Area including Raney

Township was carried out for the Ontario Department of Mines by

Furse G.D. (1932) and Rickaby, H.C. (1935). Further work done in

the area includes a regional geological mapping program carried

out by the Ontario Department of Mines in 1970-1971, an airborne

aeromagnetic survey flown in 1963 and an airborne ̂ NPUT

electromagnetic survey flown in 1982. Sporadic exploration has

been carried out on properties in the immediate vicinity located

east and southeast of the Dore Explorations claim group. This

work has been summarized by F.P. Tagliamonte in his qualifying

report - Report on the Raney Township Property, Porcupine Mining

Division, Swayze Gold Belt, District of Sudbury, Ontario

submitted in October, 1983 and is as follows:

1932 ft 1935 Throme - Greaser Gold ShowingReported on by Furse G.D. (1932) and Rickaby H.C.(1935)Located on South shore of small pond north of RaneyLake.2" wide quartz vein traced for 100* in arkose andimpure quartzite.Vein strikes Az 0802 and dips steeply north.Vein contains pyrite, carbonate and a little nativegold.Smaller 6" quartz vein in feldspar porphyry 500' southof larger vein strikes Az 0602 and traced for 100'. Atone location native gold, pyrite, chalcopyrite, galenaand tourmaline was reported.

1972 Claw Lake Molybdenite Mines Ltd.Located over part of Raney Lake and beyond to the east.Aeromagnetic Survey:Ground magnetic survey - 52 milesMagnetics reported to be flat.

Registered trade-mark of Barringer Research Ltd.

- 4 -

1973 - 1982 J - Dex ExplorationsClaim blocks on northeast and southwest end of Raney Lake.1972345' of winkle drilling in 3 holes.Rhyolite with some disseminated pyrite Intersected.1973I.P., Magnetic and Geochemical Surveys produced:9 zones of anomalous chargeabilltes, MagneticDistortions. Highest geochem. - copper 65 ppm. Zn -205 ppm.110' of winkle drilling done.1975-19795 winkie drill holes totalling 1,568'Southeast end of Raney Lake.1982Magnetic and VLF surveys northeast end of Raney Lake byIngamar Explorations Limited and J-Dex Mining andExplorations Ltd.

1976 UMEXAirborne survey southwest end of Raney Lake - Part of a larger program over parts of the Swayze Gold Belt.

1983 Lacana MiningGeological survey work on west boundary of Raney township west of Dore claim group.Carbonatite-alkalic complex rock types associated with the Kapuskasing Structural Zone mapped.

SURVEY METHOD

The geological survey was conducted by D. Hillier, B.Se.

with assistance from D. Hurst, B.Se., during the months of

September and October, 1983. Rock outcrops were tied into a

geophysical grid system (base line/tie line azimuth 035") by

mapping along the cut lines which were spaced at 120 meter

intervals. Where rock outcrop was found between the lines, the

outcrop was followed and mapped. Many outcrops were covered with

3 to 4 inches of moss which had to be stripped off by hand.

Major topographical features and claim posts were tied into the

grid system as accurately as possible.

- 5 -

REGIONAL GEOLOGY

The following regional geology section is taken from

Geoscience Report 157, Geology of the Chapleau Area, Districts of

Algoma, Sudbury and Cochrane hy P.C. Thurston, G.M. Siragusa, and

R.P. Sage, published in 1977.

All bedrock in the Chapleau area is Precambrian in age

except lamprophyre dykes which may be Mesozoic. Parts of three

structural subprovinces of the Superior Province lie within the

Chapleau map-area: the Wawa subprovince, the Abitibi subprovince

and the Kapuskasing Structural Zone. The Wawa and Abitibi

subprovinces include extensive metavolcanic-metasedimentary

belts, surrounded by granitic rocks. The Kapuskasing Structural

Zone consists of high grade (granulite facies and upper

almandine-amphibolite facies) metasediments and scattered

occurrences of mafic intrusive rocks. In the southern part of

this subprovince there is a relatively large body of Archean

basement-type anorthosite. In the Abitibi subprovince the

western end of the largest assemblage of metavolcanics and

metasediments in the Canadian Sheild extends westward into the

Chapleau map-area from Quebec and is abruptly terminated against

rocks of the Kapuskasing structural zone by a fault zone. The

assemblage has been subdivided into several volcanic complexes,

each characterized by a mafic to felsic volcanic sequence and

associated sedimentary and intrusive rocks. Those complexes

lying in part within the Chapleau map area are: the Swayze

volcanic complex, the Deloro volcanic complex and the Kamiskotia

volcanic complex.

- 6 -

The Swayze volcanic complex consists of an east-trending

belt of tnetavolcanics and metasediments 16 miles (26 km) wide at

the eastern edge of the Chapleau map area. It extends westward

from the eastern boundary of the region 46 miles (7A km) to the

Mountbatten-Crockett Townships area, where it is terminated by a

north-trending fault zone. The complex consists, from the

margins inward, of mafic metavolcanics succeeded by metasediments

termed the Ridout Series up to 4 1/2 miles wide. Scattered along

the length of the complex are several centres of Early

Precambrian felsic volcanism and related shallow water shelf and

continental-rise volcanogenic sedimentation, ie. the

Benton-Marion Townships centre, the Denyes-Swayze Townships

Centre and the Raney Township centre.

PROPERTY GEOLOGY

The Dore Explorations claim group is underlain by felsic

igneous rocks and intermediate and mafic metavolcanics with zones

of felsic to intermediate water lain tuffs, lapilli tuffs and

agglomerates. A gabbroic intrusion was found on the southernmost

part of the property and a small quartz feldspar intrusion was

located on the central eastern edge of the property.

Younger diabase dykes were also located. Zones of

disseminated pyrite mineralization were found in the mafic

volcanics and sampled and are to be sent for gold analysis.

The following is a brief description of the rock types

encountered on the property:

- 7 -

MAFIC TO INTERMEDIATE METAVOLCANICS

Unit la) Basalt to Andesite Flows.

This unit underlies the main proportion of the property and

occurs as massive to well foliated andesitic to possible

tholeitic basaltic flows. These fine to medium-grained rocks

consist of hornblende, plagioclase, biotite, chlorite and

calcite. In places this unit is well foliated with an average

strike between 070 and 080Z. Zones of green carbonate alteration

were found on L2520S - 10E, L1320S - 800E and at 1380S - 600E.

Disseminations, blebs and cubes of pyrite were noted and sampled

for later gold analysis. Small discontinuous quartz veins were

found in the metavolcanics near L360N 700E and appear to be

infillings of epigenetic, hydrothermal origin. No sulphide

mineralization greater than 5% was seen. The metavolcanics

occasionally contain felsic looking l foot long bleached zones.

Within the mafic volcanics, beds of fine-grained intermediate to

mafic tuffs occur. The metavolcanics weather a dark green to

grey colour and sometimes weather to a rusty brown colour when

containing iron sulphides. The weathered surfaces are generally

smooth but vesicles and less resistant flow bands were seen.

There is a possibility of ultramafic volcanics occurring within

the mafic volcanics area but this could not be determined in the

field and requires some of the rock samples taken to be sent for

whole-rock analysis.

- 8 -

Unit Ib) Porphyritic Flows and/or Dioritic Intrusives

This unit appears as discrete intrusions and as narrow zones

within the intermediate to mafic metavolcanics. Units of less

than 2 meters thick were seen and this unit is generally massive.

The rocks near the contact of the "diorite" are often sheared.

White feldspar phenocrysts (up to 8 mm in size) are surrounded by

a dark fine-grained matrix. Minor quartz and hornblende laths

(up to 6 mm) also occur. This unit is generally medium grained

however grain size decreases closer to contacts and which may

represent chilled zones. The rocks occasionally contain calcite

and only minor disseminated pyrite was seen.

Unit le) Pillow Lava

The pillow lavas were only found in two locations at B/L

00-2440S and L2400-360E but are probably more extensive beneath

the overburden cover. On B/L 00 at 2440S the pillows have

chloritic rims and have an average size of 45 cm by 20 cm. Some

of these pillows seem to be broken or shattered. At this outcrop

it was hard to determine the direction of pillow tops due to

stretching of the pillows caused by metamorphism, but tops seem

to be facing south since pointed bottoms were almost recognizable

on the north side of the pillows. On L2400 at 360E the pillows

also had chloritic rims and were an average size of 0.7 m by 30

cm with some as large as 1.3 m by 35 cm These pillows were also

stretched but tops appeared to be facing south. Minor carbonate

(calcite) and quartz veining was also noted in the outcrop at

2400/360E.

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FELSIC TO INTERMEDIATE METAVOLCANICS

Unit 2a) Felsic to Intermediate Meta Volcanicst

The felsic to intermediate metavolcanics were found on L240S

at 600E, 640E, 720E and 740SE; on LOOS at 600E and 620E; and on

L120N at 600E. This unit is light grey-green to tan coloured,

fine grained, occasionally well foliated and dacitic to rhyolitic

in composition. The well foliated zones may be tuffaceous but

were too fine-grained to properly identify. On L120N at 600E

this unit is slighly crenulated and this may be due to the

intrusion of a diabase dyke located 20 m south of this point.

These rocks weather to a white to buff or orange colour and

generally have a relatively smooth weathered surface. Only minor

carbonate and disseminated pyrite was noted.

Unit 2b) Lapilli Tuff

The lapilli tuff unit was found on L1920S at 1640E and

1500E; L2040S at 1500E; L2160S at 1220E and on L2520 at 570E. On

L1920 at 1640E and 1500E stretched lapilli size, white, fine

grained, felsic fragments are found within an aggloraeratic unit.

The matrix is fine grained and rhyolitic to dacitic in

composition. No sulphides were seen at either outcrop. On

L2040S at 1500E and on L2160S at 1220E, white and pink lapilli

size fragments were seen in a fine-grained felsic tuff unit. The

lapilli were stretched and were 1.5 cm to 4 cm by 0.5 cm in size.

No sulphides and only minor carbonate was seen. On L2520 at

570E, lapilli size (l cm x .25 cm) fragments in a fine-grained

intermediate matrix are associated with an agglomeratic unit.

Minor disseminated pyrite and minor carbonate occur in this

- 10 -

outcrop.

Unit 2c) Agglomerate

This unit outcrops on L1920S at 1500E and 1640E, L2160S at

370W and on L2520S at 570E. On L1920 at 1640E stretched, white,

fine-grained, felsic fragments, 15 cm by 3 cm in size are found

within a fine-grained, light green-grey, siliceous matrix of

rhyolitic to dacitic composition. Only minor carbonate and no

sulphides were seen at this outcrop. On L1920S at 1500E the same

unit as described above occurs with some fragments up to 60 cm by

10 cm in size. The white, stretched fragments are slightly more

resistant to weathering and show up clearly on a weathered

surface. No sulphides were seen at this outcrop. On L2160 at

370W an agglomerate containing fine-grained rhyolitic to dacitic,

porphyritic and intermediate bombs in a fine-grained felsic to

intermediate matrix occurs. The bombs which have a round shape

with squeezed ends are up to 60 cm by 10 cm in size, with the

average size being approximately 30 cm by 10 cm. Minor carbonate

and disseminated pyrite up to 1 7, were found in some of the

rhyolitic to dacitic bombs. On L2520 at 570E an agglomerate unit

containing lenticular felsic fragments 2 to 3 cm in size and

subordinate lapilli tuff occurs. The white lenticular felsic

fragments tend to align themselves forming concentric rings.

White lapilli l cm in size were seen in the fine-grained

intermediate matrix. The felsic to intermediate bombs were

rounded with squeezed ends. Minor quartz veining, carbonate and

disseminated pyrite were also seen at this outcrop.

- 11 -

Unit 2d) Quartz Feldspar Porphyry

Quartz feldspar porphyry was found on L600N near 880E and at

900E. The unit is medium to coarse-grained, grey green in colour

and consists of quartz and feldspar phenocrysts in a fine-grained

matrix. The origin of these intrusions has not been determined

since this rock type occurs as small discrete entities within the

metavolcanics. Minor carbonate alteration was noted and sulphide

mineralization was less than 1/E. This rock type weathers to a

white to buff colour and has a relatively smooth weathered

surface. It is noted that quartz porphyry occurs east of Raney

Lake on the J. Dex property and that porphyry contains quartz

veins with gold values, see Rickaby, B.C. (1935).

Unit 2e) Water Lain Felsic Tuffs and Cherty Sediments

This unit occurs on L1680S at 1500E and 1550E, L1800S at

1500E and on L2040S at 1500E. The tuffs and cherty sediments are

very fine-grained, siliceous and on weathered surfaces show

alternating light grey-green and dark grey bedding. No distinct

features were seen to determine the tops for this unit. On LI680

at 550E, fine-grained black cherty sediments are interbedded with

the felsic tuffs. On L2040 at 1500E, lapilli tuff with white to

pink lapilli occurs. Only minor disseminated pyrite was seen.

Unit 2f) Intermediate Dyke

This rock occurs as a narrow 2' wide dyke at L2160S 360W.

It cuts the agglomeratic unit described earlier. The dyke has a

very fine grained siliceous matrix that is light grey-green in

colour. Hornblende laths up to l cm in size are distributed

randomly throughout. This unit may be dacitic in composition and

- 12 -

could not be traced for any distance due to lack of outcrop. No

significant sulphide mineralization was found in this unit.

Unit 5a) Gabbroic Intrusives

Gabbro was only seen in one area, on lines 2400S and 2520S

at 850E and 700E respectively. The gabbro is medium to coarse

grained, dark grey green in colour and has an ophitic texture.

The mineralogy consists essentially of plagioclase and pyroxene

and/or amphibole. No structural relationships were seen and only

minor disseminated pyrite was found in this unit.

Unit 6a) Quartz Monzonite

Massive, leucocratic quartz monzonite occurs on the

northwestern edge of the property. The quartz monzonite is

reddish-pink to buff coloured and medium to coarse grained. The

main constituents are quartz, orthoclase and/or microcline,

plagioclase, biotite and minor hornblende. The quartz which

constitutes 10 to 15 percent of the rock occurs as anhedral

grains interstitial to the feldspar crystals. The plagioclase

occurs as equigranular aggregates showing interlocking texture

and also as individual grains in a finer

plagioclase-microcline-quartz groundmass. The potassic feldspars

generally occur as phenocrysts of microcline, usually perthitic

containing inclusions of plagioclase, quartz and biotite.

Biotite is the major mafic mineral and constitutes between 2 and

5 percent of the quartz monzonite. It occurs as fresh, well

defined plates or platy aggregates. Only minor hornblende which

generally alters to chlorite was seen.

- 13 -

Unit 9a) Quartz Diabase Dykes

The diabase dykes found on this property are dark grey to

black, fine to medium grained and equigranular. The finer

grained diabase may represent chilled zones near contacts. The

diabase is massive and consists of pyroxene, feldspar and quartz.

The diabase is slightly magnetic and contains minor disseminated

pyrite. The diabase dykes occasionally have a mottled appearance

and have a distinct rusty-brown to buff coloured weathered

surface. Due to lack of outcrop the diabase dykes could not be

traced over any significant distances.

- 14 -

CONCLUSIONS AND RECOMMENDATIONS

Further geophysical surveys should be done on the property

to delineate possible sulphide zones buried beneath overburden

cover in either the raafic-ultramafic rocks or the felsic tuffs.

If anomalous gold values are received from the samples taken on

the property a trenching/stripping program should be undertaken.

A magnetometer survey with readings taken every 20 m on the cut

lines will help delineate contacts that could not be found due to

overburden cover. An induced polarization survey is recommended

for the volcanic areas. Diamond drilling will depend on the

results obtained from the geophysical surveys.

Respectfully Submitted,

Don Hillier, B.Se.

Robejrt S. Middlet

- 15 -

REFERENCES

Furse, G.D. (1932)Geology of the Swayze Area; OntarioDepartment of Mines, Vol.XLI, Part III, 1932, pp 35-53

G.S.C. - O.D.M. Aeromagnetic Map No. 22A6 G 1""4 miles

Rickaby, H.C.Geology of the Swayze Gold Area; OntarioDepartment of Mines Vol. XLIII, Part III, 1934, pp 1-36

Tagliamonte, F.P. (1983)Report on the Raney Township Property,Porcupine Mining Division, Swayze Gold Belt,District of Sudbury, Ontario for Dore Explorations Inc.

Thurston, P.C., Siragusa, G.M. and Sage, R.P. (1977) Geology of Chapleau Area, Districts of Algoma, Sudbury and Cochrane, ODM Geoscience Report 157 with maps 2221, 2351, and 2352.

TABLE l l__________TABLE OF FORMATIONS—————^————^———

CENOZOICPLEISTONCENE AND RECENT

Till, sand, boulders, clay

UNCONFORMITY MESOZOIC

7LATE JURASSIC TO EARLY CRETACEOUS Lamprophyre dikes

INTRUSIVE CONTACT

PRECAMBRIANLATE PRECAMBRIAN

MAFIC TO INTERMEDIATE INTRUSIVE ROCKS1Hornblende syenite, syenodiorite

and diorite, hornblende monzonite, porphyritic hornblende diorite, quartz diorite, and gabbro, mafic hornfels

CARBONATITE-ALKALIC COMPLEXES 1Alkalic syenite, pulaskite,

brecciated alkalic syenite, fenitized rocks, massive mafic nepheline syenite (malignite), massive to foliated nepheline syenite, sovite (calcite-rich igneous rocks), magnetite- apatite rock, urtites, ijolites, melteigites (nepheline-pyroxene rocks)

INTRUSIVE CONTACT

EARLY TO MIDDLE PRECAMBRIANMAFIC INTRUSIVE ROCKS

Diabase, quartz diabase, granophyre

INTRUSIVE CONTACT

EARLY PRECAMBRIANSHAWMERE ANORTHOSITE COMPLEX

Anorthosite to gabbroic anorth osite, anorthositic gabbro and gabbro, brecciated anorthositic to gabbroic rocks, gneissic to flaser-textured tonalite and monzonite

INTRUSIVE CONTACT

KAPUSKASING STRUCTURAL ZONE ROCKSMetamorphosed mafic to inter mediate intrusive rocks, melanocratic granulite, pelitic and psammitic granulites, meta- sedimentary and raetavolcanic gneiss (upper amphibolite facies), arkosic metasediments

FAULT CONTACT

FELSIC IGNEOUS AND METAMORPHIC ROCKSFelsic Intrusive and Hybrid Rocks

Massive to gneissic, biotite and hornblende trondhjemite, grano diorite, quartz monzonite, and minor quartz diorite, syenitic rocks, pegmatite, aplite, augen gneiss, granodiorite to diorite (in part hybrid rocks), porphy ritic 'granitic' rocks

INTRUSIVE OR GRADATIONAL CONTACT

Migmatitic RocksMigmatite with metavolcanic

paleosome of quartz-feldspar- hornblende gneiss, migmatite with metasedimentary paleosome of biotite-quartz-feldspar gneiss

INTRUSIVE CONTACT

MAFIC TO ULTRAMAFIC INTRUSIVE ROCKSDiorite, gabbro, ultramafic rocks

and their serpentinized equivalents

INTRUSIVE CONTACT

METASEDIMENTS 2Greywacke, arkose, quartzite,

conglomerate, argillaceous fine grained raetasediments, biotite-quartz-feldspar schist and gneiss, migmatized raeta sediments, iron formation

METAVOLCANICS 2Felsic to Intermediate Metavolcanis

Rhyolite to dacite flows and fragmental rocks, tuff, lapilli-tuff, agglomerate, breccia, porphyritic flows, quartz-feldspar porphyry, iron formation

Mafic to Intermediate MetavolcanicsBasalt to andesite flows and

porphyritic flows, pillow lava, mafic pyroclastic rocks, layered amphibolite, diorite, gabbro, migmatized mafic meta- volcanics, iron formation

Notes1 Relative ages unknown, radiometric ages equivalent; these

units appear to be spatially associated with the Kapuskasing Structural Zone.

2 Age relationships among mafic metavolcanics, felsic metavol- canics and metasediments are variable.

Certification

I, Don Hillier, B.Se., of Timmins, Ontario, certify that:

1. I am a graduate of the University of British Columbia, Vancouver, B.C., with a B.Se. degree in Geology obtained in 1981.

2. I have been practising my profession in Canada since 1981.

3. I have no direct or indirect interest in the properties, leases or securities of Dore Explorations Inc. nor do I expect to receive any.

Dated this 16th day of November, 1983, Timmins, Ontario.

Don Hillier, B.Se.

CERTIFICATION

I, Robert S. Middleton, P.Eng., of 136 Cedar Avenue South, in the City of Timmins, Province of Ontario, certify a s follows concerning the Dore Explorations Inc. property and dated 16th day of November, 1983.

1) I am a member in good standing of:

a) Geological Association of Canada (FGAC)b) The Association of Professional Engineers of

Ontarioc) European Association of Exploration

Geophysicistsd) Society of Exploration Geophysicistse) Canadian Institute of Mining and Metallurgy

2) I am a graduate of the Michigan TechnologicalUniversity, Houghton, Michigan, U.S.A. with a B.S. degree in Applied Geophysics obtained in 1968, and an M.S. degree in Geophysics in 1969.

3) I have been practising ray profession in Canada,occasionally in the United States, Central America, Europe and South Africa for the past 14 years.

Dated this 16th day of November, 1983 TIMMINS, Ontario

Robert S. Middleton, P.Eng.

41015SW0814 2.6236 RANEY 900

1984 05 03 Your Files 375Our File: 2.6236

Mr. Bruce HanleyMining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

RE: Notice of Intent dated April 9, 1964. Geological Survey on Mining Claims P 591339 et al in the Township of Raney

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 6643Queen's ParkToronto, OntarioM7A 1W3Phone: (416) 965-6918

M.E. Andersontsc

cc: Dore Exploration Ltdc/o R.S. Middleton Exploration Services P.O. Box 1637 Timmins, Ont

cc: Mr. G.H. Ferguson cc: Resident Gevfrftgist Mining s Lands Commissioner Timmins, Ontario Toronto, Ontario

© Ministry of Technical Assess Natural Resources Work Credits

Ontario

ment P"*2.6236

Bm Mining Rtcorder'i Report of

1984 04 09 WorkW 375

Recorded Holder DORE EXPLORATION LTD

Township or Area RANEY TOWNSHIP

Typ* of survey and number of Assessment days credit per claim

Geophysical

Incisor! fi^xriltaion rlays

Section 77 (19) S** "Mining Claim* AtimMd" column

40ftpnlnrjiral riayi

Rpnrhpmiral rlays

Man days O Airborne D

Special provision S Ground H

[~3c Credits have been reduced because of partial coverage of claims.

l l Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

P 591340 to 42 inclusive 636035 636272 724304 to 08 inclusive 724310 724322 to 28 inclusive 724330 to 34 inclusive 724336 to 38 inclusive

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

30 DAYS CREDITED 10 DAYS CREDITED

P 591339 P 636276 636273-74 724329 724309 724335

No credits have been allowed for the following mining claims

Lj^ not sufficiently covered by the survey 1 — 1 Insufficient technical data filed

P 636275

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)—60:828 (83/6)

Ministry of NaturalResources

Ontario

•

1984 04 09 Your File: 375Our File: 2.6236

Mr. Bruce HanleyMining 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. F. W. Matthews at 416/965-6918.

Yours very truly,

S. E. YundtDirectorLand Management Branch

Whitney Block, Room 6643Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1316

M. E. Anderson:mc Encis.

cc: Dore Exploration Ltdc/o R. S. Middleton Exploration Services P.O. Box 1637 Timmins, Ontario

cc: Mr. G. H. FergusonMining S Lands CommissionerToronto, Ontario

Ministryof Notice of Intent NaturalResources for Technical Reports

Ontario

1984 04 09

2.6236/375

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)

Ministryof GeotechnicalSees Report

Ontario Approval

File

Mining Lands Comments

-oka*!.

To: Geophysics

Comments

l l Approved [ | Wish to see again with correctionsDate Signature

To: Geology - Expenditures 1 *\( . C fc. i/l i T//-

Comments

Approved l l Wish to see again with correctionsSignauir

-f—

To: Geochemistry

Comments

Approved Wish to see again with correctionsDate Signature

To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1593 (81/10)

] M Vie l C.liL'tl JaAnfl/l/l 11,

Assessed

Approved Reports of Work sent out

Notice of Intent filed

Approval after Notice of Intent sent out

Duplicate sent to Resident Geologist

Duplicate sent to A.F.R.O.

n , gf

r

. w'7

7 ^ \ j AcA n csj JO ^Tf

v/c^cM\ C rj ^ . ) d

0

1984 01 10 Your File: 375Our File: 2.6236

Mr. Bruce HanleyMining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

We have received reports and maps for a Geological survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims P 591339 et al 1n the Township of Raney.

This material will be examined and assessed and a statement of assessment work credits will be Issued.

Yours very truly,

J.R. MortonActing DirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-1380

A. K1nv1g:mc

cc: Dore Explorations Ltdc/o R.S. Middleton Exploration Services P.O. Box 1637 Timmins, Ontario

Ministry ofNaturalResources

Ontario

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

V.The Mining Act

Type of Survey!*)

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 enteredin the "Expend. Days Cr." columns.

— Do not.use^tiadEd areas below. ip or Area

Adoress

. S . M \Q

Survey Company |Date of Survey (from Si to) Total Miles of line Cut

Name and Address of Author (of Geo-Technical report)

V\\y^5J2 "~" ' T^.O. ' r C^WrfryreAQCredits Requested per E^ch Claim in Columns at right___ Mining Claims Traversed (List in numerical sequence)Specia Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: us ng the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side

and enter totallsl here

PORCUPINE MINING D

jSiBEn DEC -119

A.M.

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

Geophysical ^sper

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological jrf*b

Geochemica

*~ L , i Days per Geophysical ! C (va , m

- Electromagnetic

- Magnetometer ;

'v'siowRaaion etric i

ID) - i:-'/^rvgeoioic^ sJ-^'

Geocpeflyc 1 i

I.I.I vly ; Davs p er"" Claim

Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power stripping't vpe of Work Performed

Performed on Claim(sj

i

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

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

Mining ClaimPrefix | Number

7J2^/ 308-72^ 305

Expend. Days Cr.

Mining ClaimPrefix

P*Number

7^^322.

7^331

Expend. Days Cr.

Total number of mining claims covered by this report of work.

Certification Verifying Report of Work

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

and Postal Address of Person Certifying

Date Certified Certifi.edny (

—l y -

RANEY TOWNSHIP

Claiims Recorded

724306 - 724310 June 14, 1983

724322 - 724338 June 14, 1983

591339 - 591342 On Extension to Dec. 15, 1983

636035 - On Extension to Dec. 15, 1983

636272 - 636276 On Extension to Dec. 15, 1983

Ontario

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)

Township or Area

Claim

( Q &Oi c? r-1 c./

Survey Company.

Author of ReportAddress of Author

\p-FL

t V-VS.

Covering Dates of Survey*

Total Miles of Line Cut.(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- ^

DAYS per claim

Geological.

Geochemical-

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

Magnetometer. .Electromagnetic. . Radiometric

DATE:

(enter days per claim)

SIGNATURE:.Author of Report or Agent

Res. Geol.. .Qualifications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

l

TOTAL CLAIMS.

837 (5/79)

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.)

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 EH

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, ashing)

Mesh size of fraction used for analysis ————

Extraction Method. Analytical Method . Reagents Used ——-

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

.tests)

.tests)

-tests)

GeneraL General.

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.

tbZc

O

2;oH <N

to

Instrument -—-—-—^-—-

Accuracy — Scale constant

Diurnal correction method.

Base Station check-in interval (hours).

Base Station location and value ———

InstrumentOH-(

^ Coil configurationO

lCoil separation .————-————————.——————————————————————^—^-^——--—-——^—^-^—

Accuracy ————————^——-^——^————^--———^——————^——^—-^-^—^—^—^—^—^—^——^—

Method: d Fixed transmitter CH Shoot back O In line CD Parallel line

Frequency_______________________—.______________________________._____(specify V.L.F. station)

Parameters measured——.———————-——-^————-^—^--^——————^—^—^—————————^——^—

Instrument

Scale constant.

Corrections 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.

Electrode array —

Electrode spacing .

Type of electrode

o;

•-Q^HK LU

CO O)o

Hellyer Twp.(M.926)

s M

x

7i4302 1724501,724300,

7 | p r \ V' v i v .rift,**8" 7 *

, S9lV*l 6*^401938*7*1^84™ I 7573J6 | 767SJI j 700,03 Ip - -l - — -J. - ^--) -1 — ^J. . ..l_ — _ i— — -J — — —

P ' P I P-, P |p P P 757332 l'l' ) t l l l ' ' l" p "-j--—— 'l

1709708 .757335

2 M l M

r

-fi M

• y /

H, <*-^**v

^ ^/'-HT^ A

/, J-

\

,/

4M 4- l

5 M -f-

V, _ l 72433A|7*4*08 T" j^76497561 's ;7p~i~~'p"~ \Jp\ /'"pr~~t^*^rJ j i y W i y u-636M9 /' 1^72^333 l 7?4VS lJ7ji4309 I7243JO J724 __ ___/f rt, ~ip" ~~~[py T TP ~ ~ip~XTp~~ TP ~ ip~""*v/-

,A, M . . V l f J/ l l '724318 I/7Z43I6 | 724317 24334 724/530X724327 1724322/1^24 321 1724320 724319 l ,- - -\ r - l- r——-.——— I—^— 4-— — i— -tnr— r .'. r i 4^ — ~ m J P l p l p * p

lj[ | ) (l?-1"l 467483 |^OIO(Z2 J ;PJ 5J^" p

537282— -

111l p7571W

P

1

/b/32?

P

rF™^f\

7280

P37281

P"""1

7J7B

---.

'

.6

S.^-"'

' "^— — -^ — — — J\ ^^-^J — — — — -1',^'-^"7iTJ2^|7-i73l4 [757313

P ' Ip

1

76/32O | 7&73IS

P |P

p

757312

P

l 757319 .767316 .7673 II - — — -r-l-- — — 1 — — .j)P p P

51786 75731 X , 757310

r H P537783

-

P

P Ip

1 P

1 |b9879f)7--

| P /'

i ;696704r-t

700085 1| 700084 1 698796 .6987*93

P , P

70O086

p ^-—^

700087

P

' 00088

V

1767,318 7 57J09 700089 1

-— ~—— — *-4f- —— —— —— - J. ——— —— ^| ^- . . — -,p 7!' p V i

1P ^P T

TO 0083 ' 7OOOM

LP" " j P -. .

700082, 700075T -" ~ -

700081

P

P

|

\69879y2j

' X

K t c\

69 8 fff^

P

698782~P^"

698783

P'

698791 j 698784

7

7OOO7G (98790/

P 1- '\1

7700080 1 700077 {69878 B

-- - - 4 — ^7- 1P 1.r l li.

8*7a'79l S5I79I S5I790 1 , 1 /' li

L.-4-^-— . . . j 700090 | 700079

P |H '

' '.1700078 | 698788 j

P/

xC98?86~r

698786

P T/f"

1698787

OJCD O

3 M

698779 l 75706711

698778|7570687"-|p~ -l

69877717570697 ~ i P*~

l757070

-2"o a:

757074 l,/" -'' O -- ' ' l "-.XI

/f fp ~,I^^Tx7^^""1 ^^^—^—'r^7T\ L j p i /: i r i r i r | r , i r -'/J yf/l/ J/ l j '7243,81/7243,6! ^43,7 ""Tl Ji.fiV.| S.,79, ,.,7.0 j , | | 'j-'- | 724334 |724yt3CN724327 |72 43Ky1?2432 ̂ | 724320 J7243^I9^ J^ -f ~ Ar ~ l"——P —-f----J--4——|-- - - - | 700090 , 700079 | 700076 | 698768 |k98787

|p~TT^7"~ |T7^ -Tr~~^ ^/V/KM"^ i p s, i p py. p ^' p r ' i" " r --f ip- r- p-rrp~"l \/ l y l //| 7 l 7 172^342 l /f l S M6Jk-^!/ l"''"! 581/ 787 S 8 "88 " ir" i !s,00 94 !^0^4.Tji^^^jf^r^^^ i ^, ̂ ^tV

^ * l 7 i 7 N/ l V i jlA-^i l l!6.-7oejb'- |y ' j ! \ - ', 'i --f i ] r---, 7.4337 l 724*336 i 724328 j 72^5 1724124 j S 1^690^^^"'!] J ^ ^6279R 1 \ * | 7Z434S j 724349 724330^ 3^1 j 7^4 3sJ j ; 0,909,^'^** ^^

7 x4337 724V336 724328 72X? 6 1724124 l J |k4690^64 8̂V^"7ij -^62798 1 ^ 724348 ' 724346 '724330* 72438 7243S:--." -J —— k" - -^ " P - - .'-1 --.----- p —

l

Halcrow Twp. (M.906)

-f- v*' M

-f ^ i 83628,*J

724362 I7J436I i 724360 1 724369 ptT""H'II"P-- -v- - - *, ', x••58876 '

724^5*3' l^menf( \ ,, , l ?9e376|758J77 1766

ft"

" J(63B03e|636037l836038|636039

3t03-i6

LakeI63^4S I 636042 65804 Li l II

2 M 5 M \1 M 4 M M

Denyes Twp.( M.758)

THF TOWNSHIP OF

RANEYDISTRICT OF

SUDBURY

PORCUPINE'MINING DIVISION

SCALE: 1-INCH 40 CHAINS

DISPOSITION OF CROWN LANDS

PATENT, SURFACE AND MINING RIGHTS ....." , SURFACE RIGHTS ONLY . .. 6" , MINING RIGHTS ONLY... .. ,. O

LEASE, SURFACE AND MINING RIGHTS-—— B" , SURFACE RIGHTS ONLY .^.. __ .. H" , MINING RIGHTS ONLY ............. B

LICENCE OF OCCUPATION ........ ... . .T

KOAPS

'M PR OVEO ROADS

KING S H.CHWAY 1 .

iJftil WAVf,

('f)WE K UNtS

MARSH (IH

ANCtLLED

NOTES400' surface rights reservation along the shores ot all lakes and rivers

DATK ui ISSUt

MAR l ^ 138 \

Mmis'.iyol 1^ uial Ita^

PLAN NO M. 1069ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

410156W8814 2.8236 RANEY 200

Ea

Zf

Ze

2*.

le

Ib

•^-^ GEOLOGIC CONTACT c t;-"OUTCROP ~-*-*- FOLIA! ION

CLAIM POST

LEGEND

tjj X OoIX o

QUARTZ DIABASE

QUARTZ MONZONITE

GABBRO

INTERMEDIATE DIKE

WATER LAIN FFLSIC TUFf-S aC!,-irtYY

CUAHTZ Fi"' ';::r/-^ rc.vr.u^Y

f

LAPILLI TUFF

FELSIC t o I NTERMEDIATE l.' -.'t/.V -)'.C/-; '^S

PILLOW LAVA

DIORITIC INTRUSIVES/PORPHYRhIC FLOV/3

MAFIC to INTERMEDIATE r.KTAVOLCAflCS

-fj-

B Claim post, located

[J Claim post, not located (position approximate)

—QUAKIZ VI:IN-"^1 AKE

- LKI-I'.K

- bVVAMP

41Q)6SwaaM S. 6336 RANEY 210

<

ly*

x'' .1* ' o* l ^"

MJbW,

DENYES TWP

SHEET ZCJ.

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

forDORE EXPLORATIONS INC

Title RANEY TOWNSHIP PROPERTY PORCUPINE MINING DIVISION

GEOLOGICAL SURVEY

Date: D EC.83 Scale: l 2500Drawn: A w ,js Approved:

Minor carb Minor di** py

minor diee py

Minor d lie py Minor carb

Minor dist py Minor carb

I2cm qts vein

lo dlM5959COrb

Sppb Aulafelsic layer

8958 "c Sppb Au

10py carbminor green carb

diu py

pyminor carb

la py.carb

^

LEGEND

9*

fea fa

Zf

2*

?a

QUARTZ DIABASE

QUARTZ MONZONITE

GABBRO

INTERMEDIATE DIKE

WATER LAIN FELSIC TUFFS 8C!::iRTY S^DII'uNiS

QUARTZ FELDSPf3 PORPHYRY

2c

Zfc

le

/" 'l O! liuAl'E

LAI'ILLI TU1-F

hil-SIC t o I UTLh,.U-;DIATE !

PILLOW LAVA

r; - - .s

DIOHITfC INTRUSIVLS/PORPHYKrilC l l O,.3

MAI-IC to INTKRMKDIA'lE f'-.T/.V ^.C " \ ". " ;3 Claim post, located

Claim post, not located (position approximate)

t .•H

y'"GEOLOGIC CONTACT

-^OinCNOp

" I-OLIAHON

CLAIM POST

-OIJ^KIZ VrlfJ ^'1 AKE

i,KI l K

4101SSWBBH S B?3B RANEY aao

RANEY LAKE

\

<

5963

SHEET JE

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

forDORE EXPLORATIONS INC.

Title RANEY TOWNSHIP PROPERTY PORCUPINE MINING DIVISION

GEOLOGICAL SURVEYDate: DEC 83 Scale: 1 ^2500 N.T.S.Drawn: Js AW Approved: File: M -6