4aB01SE0851 2 .7101 HORWOOD 010

GEOLOGICAL REPORT

ON THE

GRAND SAGANAUY MINES LTD. PROPERTY

HORWOOD LAKE AREA

ONTARIO

RECEIVED

AUG 2 7 1984

MINING LANDS SECTION

by

DON HILLIER, B.Se.

l

P: 1 - t-'.

t*: fci f-'.'

Ingamar Explorations LimitedCedar Hill

Connaught, Ontario PON 1AO

?

June 27, 1984

42B81568851 3.7101 HORWOOD 010C

SUMMARY.................................... ~ f

INTR0PUCTI0W............................... lLOCATION S ACCESS ...,.................. 2

PROPERTY ................................ l

T0P0GRAPW AWP VEGETATION . ............. 3

PREVIOUS EXPLORATION . .................. 4

REGIONAL GEOLOGV . ......................... K?

PROPERTV GEOLOGY ..............'..'........... M

CONCLUSIONS . .............................. J7

REC0MMEWPATIOWS ..........,................ T*

REFEREWCES ................................ J9

CERTIFICATE ............................... 20

F-cgu/ie

F-cga*e 3f 4.3011 4F-cgate 5

Property Location Map C&Um Location Map Re.Q4.onat Gtotogtf General Piopvity Gtotogy PeAu^ed PAOpeAJ^f Geology

m®Jabtt 1 - Table. 0& formation*

Appewctcx A - Claim

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SUMMARY

The Grand Saganauy Mines Limited property consists of nine (9) contiguous, unpatented mining claims. The claims are located in Horwood Township, District of Sudbury, Porcupine Mining Division, Northwestern Ontario. A geological survey was conducted on the property during the month of June, 1984.' The property was found to be underlain by intermediate to mafic metavolcanics, metagabbro and quartz, diorite. Numerous, possibly auriferous (gold bearing) quartz veins were found to occur on the property. Samples were taken from quartz veins con taining sulphide mineralization and these samples are in the process of being assayed for gold content. A follow-up program consisting of detailed prospecting and geophysical surveys has been recommended.

INTRODUCTION

A geological survey was carried out on the Grand Saganauy Mines Limited property between June l, 1984 and June 14, 1984 by Don Hillier, B.Se. A compass and flagged grid established prior to the geological survey was used for location during the survey* The grid, which was also done by D. Hillier, consisted of an east-west baseline and north-south survey lines spaced 400 feet apart. Survey stations were flagged every 100 feet along the baseline and survey lines. The majority of rock outcrops were covered by light moss which had

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INTRODUCTION cont'd

to be stripped off during the geological survey.

It is the purpose of this report to discuss the results of the geological survey and prospecting program. Recommendations for further work to locate

auriferous zones are also included later in this report.

LOCATION AND ACCESS

The Grand Saganauy Mines Limited property is located in Northeastern Ontario at latitude 48 O01' and longitude 82 0 18' or approximately 17 miles.south-

southeast of Foleyet, Ontario (see Fig. #1). The prop erty is situated on the central part of Horwood Peninsula, 1/4 mile east of a small inlet, due east of Pinecone Point.

The property is accessible via boat, which can be rented at a fishing-hunting camp located at the northernmost tip of Horwood Lake.

PROPERTY

The nine contiguous mining claims included

in the Grand Saganauy Mines Limited claim group

Figure #1 — Property Location Map

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PROPERTY cont'd

encompass approximately 360 acres of mining land in the central part of Horwood Township. The claims are registered with the Ministry of Natural Resources, Recording Office, Timmins, Ontario.i The claims are listed below:

CLAIM. NO.

P-725541 P-725542 P-725543 P-725544 P-725545 P-725546 P-725547 P-725548 P-725549

RECORDING DATE

June HlinnHnn

H

27, nnnHnnII

II

1983N

II

II

nnnnn

REGISTERED STAKER

E.J* Korba nH n Nn n n N

At the time of writing the claims were being held by Grand Saganauy Mines Limited.

TOPOGRAPHY A VEGETATION

The area covered by the Grand Saganauy Mines Limited property is generally of low relief, usually less than 50 feet. Scattered outcrop com prises approximately 5 percent of the property. Generally the outcrops are covered by light moss. A large proportion of the property is swamp area,

* '

thick with alders. The remainder of the property is covered by heavier overburden with the main tree types being black spruce, pine and balsam.

HORWOOD

Figure #2 — Claim Location Map

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RREVIOUS EXPLORATION

A review of the assessment work files in the Timmins Resident Geologists' office reveals that previous work done on the subject property includes)

1. A drill program by Hollinger Consolidated Gold Mines carried out in September, 1950. Drill records indicate that six diamond drill holes were completed. Drill logs for two of the holes were found in file #T2119 in the assessment office. No assay results were included with the drill logs.

2. Magnetic and vertical loop electromagnetic surveyswere carried out by Noranda Mines Ltd. in July, 1974. The surveys were conducted on the C. Bruneau claim optioned by Noranda Mines Ltd. This claim included the ground now covered by claim 725545. Weak anomalies were found on.C. Bruneau .claim. File #12125'' in the assessment office contains the results of : these surveys.

The earliest work in the Horwood Lake area was an initial geological investigation by W.A. Parks of the Geological Survey of Canada in 1899 (Parks 1900). T.L. Tanton conducted a general geolog ical survey in 1916 and produced the first geologic map of the Horwood Lake area (Tanton 1917). H.M. Bannerman summarized the geology and mineral occurences in the southern part of Horwood Township (Bannerman 1930;1934). H.C. Laird examined the geology in the southern half of Horwood Township and evaluated

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PREVIOUS EXPLORATION cont'd

several gold properties for the Ontario Department of Mines (Laird 1935). W.D. Harding conducted a geological survey of the Horwood Lake area for the Ontario Department of Mines (Harding 1937). A reconnaissance geologic mapping program conducted by the Ontario Department of Mines included the Horwood Lake area (Thurston et al. 1971). The most recent survey carried out by the Ontario Department of Mines is that of F.W. Breaks (1978).

Sporadic gold exploration in theHorwood Lake area dates back to 1909 with prospecting inspired by important gold discoveries being made during the same year in the nearby Porcupine district. Exploration programs carried out on properties in the Horwood Lake area were summarized by F.W. Breaks 1(1978) and are as follows:

*

D AJAX OCCURENCEGreat Pike Lake - Hardiman Bay area, one

and one-half miles south of the southeast corner of the Grand Saganauy claim group., A detailed geological mapping program to examine possible gold mineralization Within quartz vein systems and/or shear zones.

2) J. CHARLEBOIS (GROUNDHOG MINE)Horwood Peninsula area, one and one-half

miles southeast of the Grand Saganauy Mines Limited claim group. The first significant gold discovery in the area recorded by Tom Jessop in 1918. In 1928-29, Nipissing Mining Company Limited optioned the 12-claim

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PREVIOUS EXPLORATION cont'd

Jessop property and indicated the presence of a mineralized quartz vein with economic gold values. The vein was reported to be situated within a narrow northwest-trending shear zone and minera lization was traced for 96 feet along strike. Ttfe average grade calculated by channel sampling at inter vals of 5 feet was 0.54-ounces gold/ton over a width of 1.94 feet. Two test pits were excavated on claim 9807 and the average grades are indicated below:

Pit 1 Pit 2

GRADE WIDTH LENGTH(ounces gold/ton) (feet) (feet)

7.23 1.19 90.63 3.1 16

In 1929, Spruce .Falls Power and Paper Company Limited constructed a dam at the inlet of Groundhog Lake and the original showing was flooded by 15 feet of water. No .further work was reported to have been done by Nipissing Mining Company Limited. In 1934, Groundhog Gold Mines Limited aquired the property and enlarged the claim group. Minimal development was carried out until 1947-48 when geo- 'logical and geophysical surveys were followed by approximately 8000 feet of diamond drilling. Strike of mineralization was extended to 1000.feet, averaging 0.31 ounces gold/ton over 3.4 feet width. Results of a magnetometer survey conducted in 1948 failed tp extend the mineralized zone to the southeast under overburden

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PREVIOUS EXPLORATION cont'd

cover or to the northwest under the lake. The 33

claim group was reduced-to 4 patented claims (59804,59806,

S9807 and S9811).

3) DEBURMAC OCCURENCEExact location unknown, approximately

three miles south of Grand Saganauy Mines Limited claim group. Investigation of a narrow east to southeast trending, steeply dipping, mineralized quartz vein. Surface sampling highest assay was 0*40 ounces of gold over 3.5 feet. At least 2,778 feet of diamond drilling was carried out.

4) DONALDA MINES LIMITED (1965)

Located in south-central Horwood Township! four miles south of Grand .Saganauy Mines Limited property. Combined electromagnetic-magnetometer survey with interest centered upon a southwest-trending mineralized shear zone. The geophysical surveyr.failed to reveal any anomalous area of possible economic potential at that time.

i

5) HARBIMAH BAY . MINES LIMITED (1916)Located five miles southwest of the Grand

Saganauy Mines Limited property. A ground magnetometer survey outlined several anomalous zones. Ten diamond drill holes totalling 2,196 feet investigated the more important anomalies. Five of these drill holes probed a gold occurence which at surface carried minor pyrite, carbonate and gold, with .the best chip sample over a width of four feet running 0.38 ounces gold/ton.

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6) SMITH-THORNE MINELocated along the eastern shore of Horwood

Lake 1,500 feet south of Hardiman Bay entrance, four miles south of Grand Saganauy Mines Limited property* Gold was discovered in a 30-inch wide massive quartz vein for a length of 60 feet. Channel sampling recorded 0.75 ounces gold/ton over the vein width. In 1935 Hollinger Consolidated Gold Mines.optioned the property, sunk B shaft, and carried out extensive underground sampling and diamond drilling and outlined:several small lenses of economically important gold mineralization:

GRADE DIMENSIONS (ounces gold/ton) (feet)

200 . 0.20 20 x 4,90.23 30 x 4.2

325- ——— . ——— '

570 0.85 90 x 3.50*51 55 X J , 3 0.28 79 x 2.7

Hollinger Consolidated Gold Mines drillid three relatively deep (1300-1400 feet) diamond drill holes and continuity of projected gold mineralization below the 570 foot level was not established by these holes. The Hollinger option was curtailed in early 1937 because the volume of gold mineralization was insufficient to support a major mining operation*

Later in 1937 Tionaga Gold Mines Limited ' proceeded with development. Further deepening of the shaft to 731 feet was undertaken in February 1938.

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6) cont'dAdditional levels were established at 450 feet and 570 feet. During 1938 and 1939, 6653 tons of ore were processed at the minesite. Total production amounted to 2,299 ounces of gold and 404 ounces of silver.

7) ' LIBERATOR PROSPECTING SYNDICATE (1946)Located four, end one-half miles south of

Grand Saganauy Mines Limited property. A geologicalt

survey covering a portion of a prominent northeast- trending mineralized shear zone. Extensive develop ment was recorded by several mining companies in prev ious years, commencing in 1933.

8) OROFINO MINES LIMITEDLocated seven miles southwest of Grand

Saganauy Mines Limited property. Visible gold discovered in 1933 and 12 claims were staked by J. Burke and J. Mclllroy. Hollinger Consolidated Gold Mines Limited optioned the property in 1935 aftd drilled 25 holes totalling 4,800 feet in addition to trenching and channel sampling. The option lapsed in 1938 and the claims were restaked by Mining Research Corporation and 13 new claims were added to the group. This claim group was squired by Orofino Mines Limited in 1945. Stripping and trenching along with extensive diamond drilling established continuity of mineralization to a depth of atleast 200 feet over a strike length of 700 feet. In 1948-49 a 200 square foot vertical shaft was excavated

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8) cont'dto a depth of 306 feet with levels at 150 feet and 275 feet. Total amount of diamond drilling recorded by Orofino Mines Limited is 21,112 feet. Ore reserves were tentatively placed at 105,000 tons averaging 0.27 ounces gold/ton. Several diamond drill holes 800 to 1000 feet in length were drilled in 1962-63.

Other properties worked on in the Horwood Lake area failed to indicate any significant gold occurencea.

REGIONAL GEOLOGY

The following regional geology section is taken from O.G.S. Report 169, Geology of the Horwood Lake Area, District of Sudbury, by F.W. Breaks, pub lished in 1978.

The Grand Saganauy Mines Limited property is located within a portion of the Swayze greenstone belt in the Superior Province of the'Canadian Shield. More specifically, the property lies within a generally east- west-trending Archean metavolcanic-metasedimentary- metagabbroic belt. The general area, referred to as the Horwood Lake area, is situated within the Horwood Lake Sheet, Map 2329 (see enclosed portion, Fig. #3), which was mapped by F.W. Breaks and associates for the Ontario Department of Mines in 1971.

p. 1 ".

TABLE 1

TABLE OF FORMATIONS FOR THE HORWOOD LAKE AREA

CENOZOICQUATERNARY

RECENTLake, stream, and swamp deposits

PLEISTOCENEGlacial drift, sand, gravel,'boulders and varved clays.

UNCONFORMITY PRECAMBRIAN

MIDDLE TO LATE PRECAMBRIAN (PROTEROZOIC) f, MAFIC INTRUSIVE ROCKSf Olivine diabase dikes (Abitibi-type), quartz f diabase, and porphyritic diabase dikes.

INTRUSIVE CONTACT 'EARLY PRECAMBRIAN (ARCHEAN)

LATE FELSIC TO INTERMEDIATE INTRUSIVE ROCKSBiotite granodiorite, biotite quartz mon zonite, porphyritic biotite granodiorite, porphyritic biotite quartz monzonite, biotite-lhlornblende quartz diorite, horn blende monzonite, xenolithic granitic rocks, hornblende quartz monzonite, aplite dikes, muscovite granodiorite, hornblendegrano diorite, ;biotite-hornblende diorite.

INTRUSIVE CONTACT EARLY FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

Biotite trondhjemite, biotite-hornblende trondhjemite, biotite-hornblende diorite, quartz porphyry, feldspar porphyry, quartz?* feldspar porphyry,'migmatite.

INTRUSIVE CONTACTMAFIC AND ULTRAMAFIC INTRUSIVE ROCKS

ULTRAMAFIC INTRUSIVE ROCKSDark green-black serpentinite, light blue- green serpentinite, talc-carbonate serpentinite, sheared serpentinite.

MAFIC INTRUSIVE ROCKSMetagabbro, xenolithic metagabbro, porphy ritic to equigranular diorite,, hornblendite, metagabbro dikes.

METAVOLCANICS AND METASEDIMENTS METASEDIMENTS

Greywacke, conglomerate, chert, chert breccia, quartzite, arkose, slate.

jfe-*-,.

TABLE 1 cont'd

FELSIC TO INTERMEDIATE METAVOLCANICSTuff, lapilli-tuff, tuff-breccia, pyroclastic breccia, felsic flows, quartz-feldspar crystal tuff, feldspar and/or quartz porphyry subvolcanic rocks, miarolitic subvolcanic rocks.

MAFIC TO INTERMEDIATE METAVOLCANICSAmygdaloidal metavolcanics, pillowed meta- volcanios; crenulated metavolcanics, laminated metavolcanics, medium-to coarse -grained metavolcanics, mafic breccia, amphibolitized metavolcanics, massive metavolcanics, garnetiferous metavolcanics, variolitic metavolcanics, porphyritic andesite, migmatized metavolcanics.

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REGIONAL GEOLOGY cont'd

The oldest rocks in the Horwood Lake areaare the felsic and mafic metavolcanic sequences whichcontains minor interflow metasediments.

The felsic metavolcanics occur as scattered, generally small units, and comprise approximately three percent of the metavolcanic sequence within the map area. The felsic sequence is composed of fine-grained, weakly to moderately foliated metavolcanics, probably derived from dacitic to rhyolitic pyroclastic deposts, consanguinous subvolcanic intrusive rock and subordinate felsic flows. Coarse phases of the pyroclastic meta volcanics vary from lapilli-tuff to pyroclastic bre.ccia* Spherulitic and pillowed felsic roetavolcanics rarely occur. Porphyritic types and miarolitic cavities lend support to the theory that the felsic metavolcanics are early rhyodacitic subvolcanic-volcanic masses.

Mafic to intermediate metavolcanics predom inate and underlie approximately 70 percent of the Horwood Lake area. The majority of the mafic metavol canics have been affected by greenschist facies meta morphism. The mafic metavolcanics vary from massive varieties which display pillow and amygdaloidal struc tures to varieties which are moderately to intensively sheared and carbonitized.

Massive, very fine grained, pillowed,Jet- black mafic metavolcanics of basaltic composition occur in two areas (west boundary of Horwood Township,

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REGIONAL GEOLOGY .cont'.d

north of Swayze River and east side of Horwood Lake, south of Pinecone Point) of Horwood Township.

Laminated mafic metsvolcanics characterized by fine, subtle color banding occur in the Great Pike Lake area and possibly represent mafic tuffs*

Massive ,ii medium to coarse grained amphibo- litized mafic rocks occur in the area and probably represent the coarser textured part of mafic lava flows.

Mafic breccias occur in areas of good exposure and usually contain lapilli-size fragments. These breccias are volcanogenic in origin. Autoclastic flow- top and flow-bottom breccias are notably scarce, even within excellently exposed areas of massive pillowed mafic metavolcanics.

Isolated pods of detrital metasediments occupy an insubstantial part of the Horwood Lake area. Greywacke, conglomerate, chert, quartzite, arkose and slate were the metasediment typ.es found to occur in the area.

Many discrete equigranular to porphyritic raetagabbroic plutons and rare, narrow metagabbroic dikes occur in the area. The metagabbro plutons appear to be intrusive into the mafic metavolcanic pile. The metagabbroic dikes crosscut the mafic metavolcanics.

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REGIONAL GEOLOGY cont'd

Intrusive serpentinized ultramafics occur as numerous small pod-shaped bodies in southeastern Horwood Township.

The earliest felsic intrusive rocks in the area are syntectonic, foliated, equigranular trondh jemite, diorite, quartz,:feldspar and quartz.feldspar porphyries. Biotite trondhjemite and hornblende- biotite trondhjemite occur as phases of the large Hardiman Lake Pluton, whereas the porphyry rock types occur as narrow discordant to concordant sheets.

The later felsic to intermediated intrusive rocks occur as three plutonic masses named the Hoodoo Lake Pluton, Kukatush Pluton and the Horwood Peninsula Pluton. The Hoodoo Lake Pluton consists of leucocratic medium grained biotite porphyritic granodiorite. The predominant granitic phases of the Kukatush Pluton are hornblende and biotite-hornblende monzonite, although local zones of biotite-hornblende diorite and hornblende quartz monzonite also occur. The Horwood Peninsula Pluton consists largely of fine.'to medium grained massive, equigranular, biotite-hornblende quartz diorite with lesser portions of biotite-hornblende granodiorite* Numerous smaller, less important late felsic intrusive bodies also occur in the area.

Swarms of Late Precambrian (Proterozoic) diabase dikes intrude all the aforementioned rock groups.

LEGEND

CENOZOIC*

QUATERNARY

stream, and swamp deposits.

PLEISTOCENEGlacial drift, sand, gravel, boulders, and varved clays.

UNCONFORMITY

PRECAMBRIAN*MIDDLE TO LATE PRECAMBRIAN

IPROTEROZOIC)

MAFIC INTRUSIVE ROCKS

i Diabase, unsubdivided.9a Olivine diabase dikes (Abitibi-type).

8a Quarit diabase dikes,Sb Porphyritic quartz diabase dikes.

INTRUSIVE CONTACT

EARLY PRECAMBRIAN (ARCHEAN)

LATE FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

Unsubdivided.equigranular biotite granodiorite.Porphyritic biotite granodiorite.Porphyritic to equigranular biotitequartz monzonite.Muscovite granodiorite.Aplite dikes,Xenolithic granitic rocks,Biotite-hornblende quartz diorite.Hornblende mon ionite.Hornblende quartz monzonite.Hornblende granodiorite.

l ' 7 71 Jb 7c

7m Biotite-hornblende diorite,INTRUSIVE CONTACT

EARLY FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

~"j 6 Unsvbdivided.** ' 6* Biotite trondhjemite.

Sb Biotite-hornblende trondhjemite.Se Biotite-hornblende diorite.6d Migmatite.6e Quartz porphyry, feldspar porphyry,

and quartz-feldspar porphyry.

INTRUSIVE CONTACT

MAFIC AND ULTRAMAFIC INTRUSIVE ROCKS

ULTRAMAFIC INTRUSIVE ROCKSSt Dark green-black serpentinite.Sb Light blue-green serpentinite.Se rale-carbonate serpentinite.Sd Sheared serpentinite.

MAFIC INTRUSIVE ROCKS

*a Metagabbro.ib Xenolithic metagabbro.4c Porphyritic to equigranular diorite.4d Hornblendite.4e Melagabbro dikes.

INTRUSIVE CONTACT

METAVOLCANICS AND METASEDIMENTS

METASEDIMENTS3a Greywacke.3b Conglomerate.3c Chert, chert breccia.3d Quartzite.3e Arkose.3! Slate,

FELSIC TO INTERMEDIATE METAVOLCANICSt Unsubdivided.la Tuff, lapilli-tuff.Ib Tuff-treccia, pyroclastic breccia,le felsic flows.fd Quartz-feldspar crystal tuffs.fe Feldspar and/or quartz porphyry

subvolcanic rocks, f f Miarolitic subvolcanic rocks.

MAFIC TO INTERMEDIATE METAVOLCANICSi Untubdivided.fa Amygdaloidal metavolcanics.i b Pillowed metavolcanics.le Crenulated metavolcanics.id Laminated (possibly mafic tuffs in

part) metavolcanics. le Medium-to coarse-grained metavol-

lg Fine-grained melavolcanics.1h Malic breccia,t] Amphibolitized metavolcanics.Ik Massive metavolcanics,1m Garnetiferous metavolcanics.In Variolitic metavolcanics.1p Porphyritic andesite.iq Migmatized melavolcanics.

A| •W

cl"

w4 W

SilverArtenopyriteGoldChalcopyriteGalenaMolybdenitePyrrhotitePyriteQuartzSphalerite

Figure #3 — Regional Geology

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REGIONAL GEOLOGY cont'd

Three prominent faults occur in the area and include the north trending Horwood Lake Fault, north trending Hoodoo Lake Fault and the eaat to northeast trending Hardiman Bay Fault. Smaller north to northwest trending faults and lineations also occur in the are.

A macroscopic anticlinal fold is thought to occur in Horwood Township with it axial plane trace trending northeast between East Harsh Island and the northwestern shoreline of Horwood Peninsula. The fold axis is thought to deflect southwest to a more southerly direction in the southern half of Horwood Township. The only other macroscopic fold system is comprised of an east-west trending antiform and synform located just west of Great Pike Lake. It is thought that this folding has been caused by the diapiric emplacement of the Hardiman Bay Pluton (Breaks 1978).

PROPERTY GEOLOGY '

The Grand Saganauy Mines Limited property is underlain by mafic to intermediate metavolcanica, metagabbro and biotite-hornblende quartz diorite. The grade of regional metamorphism is gnerally within green schist facies, although closer to the Horwood Peninsula Pluton it probably reaches lower amphibolite grade. This could not be determined due to the lack of rock exposure near the contact.

VV — Mafic to Intermediate Metavolcanics

— Hornblende- Biotite and Quartz Diorite

— Metagabbro

Figure /M — General Property Geology

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PROPERTY GEOLOGY cont'd

Fine-grained, massive to pillowed metavol canics underlay the main proportion of the property. An intruding metagabbroic pluton is found on the eastern portion of the property while biotite- hornblende quartz diorite of the Horwood Peninsula Pluton is found on the northern part of the claim group-. Sulphide bearing (up to five-percent disseminated and cube pyrite)and possibly auriferous (gold bearing) quartz veins occur in both the metavolcanics and the metagabbroic intrusive.- These quartz veins are epigen etic and hydrothermal in origin. The following is a detailed description of the rock types found on the property:

a) MAFIC TO INTERMEDIATE METAVOLCANICS

The mafic metavQlcanics on the Grand . Saganauy Mines Limited property are generally fine grained and massive in character, however pillowed structures were seen at two locations. Mineral composition consists of chlorite, actinolite, albltlc plagioclase, epidote and calcite. Foliation was generally poorly developed. Well formed pillows two to three feet in size were seen at two locations; at 4E-6S and L40E-10S. Tops were facing south at both locations. Interstitial breccia between adjacent pillows was seen at L4E-6S.

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PROPERTY GEOLOGY cont'd

b) METAGABBRO INTRUSIVE

On the eastern part of the claim group a metafjabbroic pluton intrudes the metavolcanic unit. The metagabbroic pluton is massive in character, medium to coarse grained and has a distinct rough weathered surface. The white inclusion riddled, plagioclase and quartz grains tend to be- more resistant to weathering, giving the metagabbro a speckled "dioritic" weathered surface. On fresh surfaces the metagabbro is dark green-black with fibrous actinblite and prismatic hornblende grains being. easily recognizable. Numerous quartz veins, one of which is greater that 15 feet wide, occur with in the metagabbroic unit. Sulphide mineralization varies from 1-53 in quartz veins to 10-158 in the adjacent wallrock. Quartz veins with sulphide minera lization tend to occur in close proximity to the metavolcanic-metagabbro contact.

c) LATE FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

On the northern part of the claim group biotite-hornblende quartz diorite of the Horwood Peninsula Pluton intrudes the metavolcanic unit* The granitic mass is leucocratic, massive, equi granular and fine to medium grained. Amphibolitized metavolcanic xenoliths up to two feet in size were seen near the metavolcanic-quartz diorite contact.

PROPERTY GEOLOGY cont'd (c)

The quartz diorite consists of plagioclase and horn blende. The weathered surfaces display a distinct speckled "dioritic" aspect. In the field the quartz diorite is easily recognized due to the fact that all samples from this pluton attracted a hand-held magnet to varying degrees of intensity.

CONCLUSIONS

The Grand Saganauy Mines Limited property represents part of a submarine volcanic pile which has been later intruded by a metagabbroic stock and a quartz diorite pluton. Several mineralized quartz veins were found on the property and samples are in the process of being assayed for gold'content. Many of the mineralized quartz veins occur in proximity to the metavolcanic-metagabbro contact and this contact should be considered as a priority target area. Several gold occurences including Orofino Mines Limited property occur within intrusive metagabbroic stocks, or in close proximity to metagabbroic stocks. Future work on this property should be concentrated at or near the metavolcanic—raefeaga/bbra contact with possible shear zones being the most favourable locations for auriferous quartz vein systems.

.-48--.

RECOMMENDATIONS

Several mineralized quartz veins were found on the property, however a large proportion of the property is covered by overburden. Therefore, it is my general recommendation to continue exploration for auriferous quartz veins and/or possible sulphide horizons which may be concealed by overburden cover. Specific recomm'endations are as follows!

J. A further detailed prospecting, stripping and sampling prdgram is recommended to explore for possible auriferous quartz veins which may be covered by light overburden.

2. If anomalous gold values are received, then ..:. trenching to obtain representative samples will be required.

3. A linecut geophysical grid, with lines spacfedoat 400 feet intervals, should be established over the entire property.

4. An electromagnetic survey should be done on the property to delineate possible sulphide zones buried beneath overburden cover.

5. A magnetometer survey would help delineate contacts that could not be found due 1 to.overburden cover. th,e contact between the metagabbroic intrusive and the metavolcanics is a good target area. Possible

\

concentations of pyrrhotite mineralization would also be found using this survey.

6. If anomalous zones are obtained from the above surveys an induced polarization survey should be conducted over selected areas.

7. Diamond drilling will depend on the results of the geophysical surveys.

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REFERENCES

Bannerman i H.M.1930: Mineral Occurences in Woman River District) Ontario}

Geol. Surv. Canada, Summary Report for 1929, Part C, P. 1-19.

1924: Rush Lake Area, Sudbury District, Ontario; Geol Surv. Canada, Summary Report for 1933, Part D, P. 38-82.

Breaks, F.W.1978: Geology of the Horwood Lake Area, District of Sudbury;

Ontario. Geological Survey Report.169, 67p. Accompanied by.Map 2329, scale 1:31,680 (1 inch to H mile).

Harding W.D.1937: Geology of Horwood Lake Area, Ontario. Dept. Mines, Pol. 46,

Pt. 2, 34p. (published 1938). Accompanied by Map 46a, scale 1 inch to 1 mile.

.Laird, H.C.1935: Horwood Lake Area; Ontario Dept. Mines, Vol. 44, Pt. 7,

p. 31-37, (pMPHshed 1936)., * . ^ i "",- * f \ . t.. - .. — -' - o -- j f * f ,' ** '

Parks, W.A..4900:. Niven's Base Line, 1899; Ontario Bur. Mines,

Vol. 9, p. 125-142.

Thurston, P.C., Sirogusa, G.M., and Sage, R.P.1971: Operation Chapledy, Hor^opd take Shis^J^s^sictftlof

Algpma, Cochrane^and; ?uoT)uryi.O:nta Northern Affairs^ f*relim^ Map; P. 673)66(61. 'spri; Scale 1 inch to 2 miles, Ueblogy 1970."- *

Tanton, T.L.1917: Reconnaissance along Canadian Northern Railway between

Gogama and Oba, Sudbury and Algoma District; Geol. Sur. Canada, Summary Report for 1916, p. 179-182.

I, Pon Hillier o{ l/oncouve*, E^-ctci/i Columbia, hereby certify that:

1. I fco-W a Bachelor oi Science. Peg*ee in Ge.ol.ogy irom the. University oi faitUh Columbia, having graduated in May, 1981.

2. I have. .pJiactUed my ptoitMion in exploration continuously Aince. my graduation.

3. I have, bated my conclusion* andcontained in thi* *e.po*t on my knowledge, oi the, oxea, P*e.viou4 expcA^ence, and on results oft iieJtd work conducted on the. property during 'the. month o^ June., 1984.

4. l hold no interest, dire.ctly or indirectly in thisproperty other than professional ie.es, nor do 7 expect to reczive. any interest in the, property,

Timmins, Ontario, Canada Don Wittier, 8 .Se.Otologist.

AUDIT Wtlt*

39TO50 © IB"1 Mining Claim RwouroM ontirto Th* Mining Act

HtCOIIOrO IN THE N*NC Or

' Joseph Edward KorbaLICCNCC NO.

M20807• tCNPT HO.

263247tOOKO

R. R. # 1, Connaught, Ontario'. PON 1AO

OFriCE UH ONLY

!!SoII

Soil

KKOIMt

June 11/84 - Order of Mining

June 13/84V

-

20

•AUNCC

Se barthe time for work, ur February 27, 1985.

Geological l

__ ,.

DESCftlPT ON or cum

Mtl MCOROIt

June 27 t

CUUMNO.

P— .755541 x

1983.•MI AX* UK! or mxinf r.T.

June 17, 1983 at 7:00 A. li. x

HORWOOD TOWNSHIP

RESERVATIONS — *0 FOOT MVACI WOHTI MKNVATIp! (AND ANOMW liM Wit), HAT MM 1 AMUM) AU UKCt AND NVIM.

r HI NO725541

\d s Commi ss.ioner, ..ex t end i ng \til and including

(#202/84)

— - — r~;-^-;;nS';"^'(W. R. #238/84)

HSlEsi^*^^''1 " 1'"^" 1i - ^wk 1 kw 1

L... i^—-"

m^U^^r"~

•••""''•'' • •^^Ci— *-

~~~~\:

*-. --'

•tetifi NO.

382394

1

^iiBBil^MHmi

DIT

39H'"49 Mining Claim

Th* Mining ActCUUMNO.

q .Tnsph Edward Koi-ba M2QR07 2fi"5?i7 Tiino 97IP ?7, lMl TIMt OF'It AX

Qft^

R. R. # 1, Connaught, Ontario. PON 1AOtu AMI Tint ertuim*

June 17, 1983Bf Q'On A M.

r.?.

s?

ornct

HORWOD TOWNSHIP

Including Land tinder Waterf HI NO

79SSA1

Jure 11/84

June 13/84

c

WORK

20

Order^ of Mining A Lands Commissioner extending.

iieciM ne.

the" time for work, until and including February 27, 1985.______________ (#202/84)Geological. (W. R. #238/84)

InlS^kuSTTOcnS'BtOpyvitnVTntiWoi^tHw"Record Book nnd is not to bo considered ai assuranco ot the validity ol the claim.

382394

PORCUfi;JE MiUTjq DIVISION

02

SuTpuaqxapug•S86T 'Z. 2

aogspueqJ0

•ON 14113)1XHOM SAVd

IKSZtQNIH4

MAN ON* WHO Tt*- SNOUVAUaSBU

dlHSNMOI dOOMHOHMtia J& NOU""*"' Mj*?a"AIMOMM

•1'*

'JTV OOat 3* C86I ?H aurif

NMVII JO INIt aM* IK*OVI NOd '.'^qSneuuoo c -[

•C86T *•ON 13NJ3I1JO 1* t K INI Nl 01410311

•ONHHOallibcvinPm iKinv

7'

l: l-

l

3S ^••L^ ^T ^^ V \f M Eaafuiimaa^•^n^ ^N K ^^^^^^ nwwwffvWuQ DO o5u5o Th* Mining ActCUUMNOP-725544 ^

• ICOIOCO IN THC NAME O r I ICCNCC MO. IICtlM HO. 0*tl MCOItCO

Joseph Edward Korba M20807 263247 June 27, 1983.tto'im IMI MO tint or IIAIIN* M.R. R. # 1, Connaught, Ontario: PON 1AO June 17, 1983 |

at 1:00 P.M. |X

\

S

OFFICE U*t ONLY MCOIOCO Ml*"tt D"C"""OK " Cl*'*

OATC OAVS WORK

- HORWOOD TOWNSHIP

HttenVADONS - J5JWOL SjMf JSJ SUfWffl

t

June 11/84 i Order of Mining A Lands Commissioner extendi

June 13/84V-

•-

1

IBKB

20'

i

the time for work, until and including February 27, 1985. (#2

,NMOUND Ml UMI WO MMM.

725541

ng.

02/84)Geological. (W. R. #238/84)

T li li AV itmnt in n fifYtiv ftl 1^*** J^^I^IA** jn IH&Record Book and is r,st lo bo ec.-isldered *3 assurance of the validity of tho claim.

•' -^viej^4-.ftS^-^^L---.

PORCUfi'jc MINiIMn DIVISIONU~—— f

*

t

iieilM NO.

382394

AUDIT UMUEft JS5J"1 Mining Claiml CUM NO

O CV TOb:^ Ut ""^ Th. Mining Ac,^^M DlCOtOIO IN TMC NAMC or IICIHCI NO. MCflM NO. Mtl MCOMC6

^^ Joseoh Edward Korba M20807 265247 .Tnno 97.

i

1

j tODICIt

R. R. # 1,

|i

P-725545 "

IQftV J•Mf MB ttMt Of ITAKINt rlU

Connaught, Ontario. PON 1AO June 17, 19S3 | at- ^;rn P.M. 1 v

DITt

June 11784*-

Jur.e 13/84V"

~

WO.K

20'

V HORWOOD TOWNSHIP

RueftVATONS — J5*wor Mg{yjjayjuy*jyytp

Including Land Under

Order of Mining ft Lands, Commissioner extend!the time for work, until and including February 27. 1985. f#?Geological. fU.*-#?

Record Book and is not (o bo ccr.s-dcred *3 assurance of the validity o( the c'.aim.

IMOUNO Ml UWf M0 HMM.

Waterf UNO .

| iiecm ne.

ng

07/R6)38/RA)

'JM/I 6 ^^*wMk*j?t#"^^^•"'"^(P' ™ M^R 1 vfllVJ^JHr

PORCUPINE Miy&OIVlSlON

1i

m

*

-*-1.

rr

*UDIT J^MER © Ministry ol Nitural NOIOUfMI

Onurie

IHICOIftCD IN IHt NAMC Or Joseph Edward Korba

LICCNCI NO.

M20807

Mining GTh* Mining

•tcfirt NO.263247

AftDitSS

R. R, # 1, Connaught, Ontario. PON 1AO

. m

g

5

OFFICE UlArONLY

OAH

June 11/84

June 13/84V'

mas

OAYtWORK

20*

,.

—— ' —— a

BAT! ftICO**IP iAUNCC

InimCUUMNO 1

Act P-725546 "Mtl IICOKCe

June 27, 1983. MMtl IN* tint Of SMKINt Ml

June 17, 1983 I at 5:00 P.M. |x

HORWOOD TOWNSHIP

RCSERV/ h T tOWS •*" 400 FOOT HI MMOMOWK^^SS^mi*^ll5^m^'^"W(l'

riL725541 |

Order of Mining 6t Lands Commissionthe time for work, until February 27, 1985.

Geological.

and incluer extending ding

(#202/84)(W R.#238X84)

.-.IB,

t

k̂^f^^r

' l-.-'iinlng Hocordipr PORC!JPi:ii: MIN.JJBUIVISION

-

, "

iienn NO. |

382394

*

*̂

if-*'

?- ^^^A

^

J...*! V.

]J

l'

.V

l"

1

f"

f-.

'f,

1,

H,

s?

s

t ± — .

s.' " K56 """""^ n™' * OUUMNO.onurie Th* Mining Act P~725547 **

Joseph Edward Korba M20807 263247 June 27. 1983^AOOflt

R

;

i

i

5

M Mil Ml tINI Of ITAEINI

.R. # 1, Connaught, Ontario. PON 1AO June 17, 1983 at 7:00 P.M.

f^fftftf i iamAftjiv 9AYS ftAL.HCf POCWIPTION OF CIAIH OFFICE wV^wnLT RCCORDtd v***!1*'

DAT!

June 11/84, .

June 13/84V

-

WORK

. -....

20

v HORWOOD TOWNSHIP

x

*a8M8Br^ w(M-w "iw*

725541

Order of Mining A Lands CpmmJ.ssionP'' extending 'the time fer work, until and including February 27, 1985. (#202/84)

Geological. (W. R. #238/84)

ThlS Abstract is a COOtl Of the rnlripc in (haRecord Book and is not to bo considered aa assuranco of the validity of tho claim.

^WUlfil984-^fS^^Uf^-^--^-

PORCUFiNE MIHJi^ DIVISIONr

v

•(CIIPT HO.

382394

•IT — uyirL -— - •—3UJCTP oSwric Th* Mining Act P-79SS4P '

j^MDEO IN Till NAME OF LICCNCC NO. fttCKlM NO* DATE ftCCOROCD

Weph Edward Korba M20807 263247 June 27. 1Q83."l" Mil *ND fINI OP ItAKIN* M,

..R. # 1, Connaught, Ontario.' PON 1AO June 18, 1983 at 7:00 A.M. v

* I 10

8e

nvmtf* . .-r AUI v 0*** KALAHCt *H*C*IP1ION OF CLAIMOrrlCI UflC ONLY ^ ACCORDED •*t*"ts

Dllt

une 11/84

ur-** 13/84V'

9 f

a

*0"K

20

v HORWOOD TOWNSHIP

"MMwnow-^g^,^

Including Land Under Waterf HI NO

J2554J

Order of Mj.nint ft Lends Commissioner extendingthe time for work, ur.tll and including February 27, 1985. (#202/84)

Geological. (W. R. #238/84)

1MIS Au.'.tc^vt 4 a wyy vf i!ic pnifl^S In tftftRecora Book and is net lo be ccrisidcred aa assurancu of the valic'iiy of the claim.

''IWrlLfW———— ̂ ifalM/

^rammg Hecordery pORCu?;:-4E MIN:NQ ofvisiON

'

Rtccm ne.

382394

,

AUDIT

390Mining ClaimTh* Mining Act

CiMMNO

Wl AC

Joseph Edward KorbaUCCNCC MO.

M20807IICIIM NO.

263247Mtl HCCOMit

June 2 7 1983.

R.R. # l, Connaught, Ontario. PON 1AO•AU *Hi MM l W IUIIN*

June 18, 1983 at 9:00 A.M.

P *

Hi- OZ f

*M 9

H

orrici uti ONLY tiUNCC

HORWOOD TOWNSHIP

RESERVATIONS — AULMOtANOMVim

"725541no.

l June 11/84 Order ,of ..Mining .fit. psloner extending

June 13/84 2D

the time for work, until and including February 27, 198 'L (#202/84)

(W.R.#238/84)

Record Book and is not to bc cc.iC-idered as assurariso ol the va*idi!y ol the claim.

Ontario

Ministryof Report of Work^sources (Geophysical, Geological,

Geochemical and Expenditures)

Type o f S urveyU)

GEOLOGICALClaim Holder(t)

ED. KORBA

42BeisEeesi 2 .7 101 HORWOOD

otpector'i Licence No.M 20807

AddressRR#1 CONNAUGHT, ONTARIO

Survey Company

MAUREX RESOURCES LTD.Date of Survey (from 81 to)

Jy l&

Total Mil** of line Cut

Name and Address of Author (of Geo-Technical report)DON HILLIER GEN. DEL. CONNAUGHT, ONTARIO RON 1AO

k

t

Credits Requested per Each Claim in Columns at rightSpecial 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 Da y t

Complete reverse side and enter total (s) here

Airborne Credits

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

Geophytical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days perClaim

20

Days per Claim

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

if"-

Performed on Claim(s)

Calculation of Expenditure

Total Expenditures

SLL

PORCUPINE MINING DIVISIONJLO E i yInstructions

Total Days Credits mayoe apportioneo at tneciaim noioer s- choice. Enter number of days credits per claim selected in columns at right. ,

DateJune 12, 1984

.f J/er or Agent ^Signature!

[

Certification VerifyingR^ort of Workr——— —————

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix

P

.^^ii.

••W**''*

~^*.-v4i3fMM

tK-n.fc T^

---•-r"*-***

..*.MW :nV

.W^V^.

- -, - **•J 3 - ,f -

S- .

1-.

Number

725541

725542

725543

725544

725545

725546

725547

725548

725549

R E C 0 R

l .HIN13

Kewipi MA. sat

Expend. Days Cr.

Ml

DE

1984

^a

v//

f

Mining ClaimPrefix

;..l- '.5- ~-

'."'. ' 4, ' '^ — J \ :-

,:f-\i., fn&r*

'T-T'"

'••/V^v-,.K.~:?-.i

WW*T"^"*- '•tof&ltf•Vi-JX*•••'iv^jjr'

JKiSj^i^i. .

IP •*//^'m tfe:5^/m.fcWK".: ••"'i -

Number

, ?.*

*IVt:^' C Q

' s tos*0"^

Expend. Day* Cr.

l hereby certify that l have a personal and intimate knowledge of the facts setor witnessed same during and/or after its completion and the annexed report is true.

F l Name and Postal Address of Person Certifying

MAURICE HIBBARD

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

!irCEDAR HILL CONNAUGHT, ONTARIO

Date CertifiedJune 12, 1984

Mining Lands Section

Control Sheet

File No J? 7/0 l

TYPE OF SURVEY GEOPHYSICAL

GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

MINING LANDS COMMENTS:

Signature of Assessor

Date

1984 09 04 Your File: 238 Our File: 2.7101

Mr. Bruce HanleyWining RecorderMinistry of Natural Resources60 Wilson AvenueT1mn1ns, 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 725541 et al 1n the Township of Horwood.

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

Yours sincerely*

S.E. YundtD1rectorLand Management Branch

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

A. Barrisc

cc: Ed Korba R.R. 11Connaughjt,Ontario PON 1AO

cc: Ingamar Exploration s Limited Cedar Hill Connaught, Ontario PON 1AO

INGAMAR EXPLORATIONS LIMITEDCEDAR HILL CONNAUGHT, ONTARIO PON 1AO

TEL. (706) 433-3661 or (706) 264-3100TELEX 067-81602

t W to

August 12, 1984j -i 198A

Mr, Fred Matthewsc/o Ministry of Natural ResourcesLand Management BranchWhitney Block, Room 6450Queen's ParkTORONTO, OntarioM7A 1W3

Dear Sir:

Enclosed are two copies of the geological reports and two copies of the work reports on the following properties:

Grand Saganauy Mines Ltd. Property, Horwood Lake Area, District of Sudbury, 9 mining claims numbered 725541 et al.

Ultrex Petroleum Ltd. Property, Horwood Lake Area, District of Sudbury, 12 mining claims numbered 749472 et al.

Thank you.

Sincerely,INGAMAR EXPLORATIONS LIMITED

Irma Hibbard, Vice-PresidentIH/abEnc.

:, S

•\ \\

X,\

S\

22N

20N

BASELINE Q

10S

12S

14S

16S

18S

no outcropno outcrop16N72554914 N

554712Nsalder, spruceno outcropION

. sprucef: i T \

no outcrop

72554725545

no outcrop

alder , spruceCI t?)poor exposure

1-2XPY

no outcrop

Om m oo

m mO)m O

m mto00m

CO Wm

w o*m o

m

CLAIM INDEX MAP

LEGENDEARLY PRECAMBRIAN (ARCHEAN)

LATE FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

7a Biotite-hornbknde quartz diorite

MAFIC INTRUSIVE ROCKS

4a Metagabbro

MAFIC TO INTERMEDIATE METAVOLCANICS

la Pillowed metavolcanicsl b Fine-grained metavolcanicsle Massive metavolcanics

c;:'

PY

*3

S

OUTCROP

GEOLOGICAL CONTACTSMALL OUTCROPLAVA FLOW; TOP (ARROW)FROM PILLOWSQUARTZ VEIN (WIDTH)PYRITE

SAMPLE LOCATION , ASSAY NUMBER

DRILL HOLE LOCATION

SWAMP

STREAM

LOCATED CLAIM POST

PROPERTY BOUNDARY

CLAIM LINES

INGAMAR EXPLORATIONS LTD.for

GRAND SAGANAUY MINES LIMITEDTitle

HORWOOD LAKE PROPERTYHORWOOD LAKE AREA

PORCUPINE MINING DIVISION

GEOLOGYDate: JUNE 1984 Scale: l" =200/ Drawn: D. Hillier File:84-32 fjn.5

j