41POBNE0118 OPtt-56 TUDHOPE 010

Prospecting 6 SamplingReport

Claims L-1134103-1134106 inclusiveand L-990956 and 990957

TUDHOPE TOWNSHIP, LARDER LAKE MININGDIVISION, Ontario.

l)

Gary Clayton Dunn

1*91

41POBNE0118 OPBBM* TUDHOPE

TABLE OF 01OC

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INTRODUCTION. . . . . . . . . . . . . . . . . . . . . . PageRESULTS. . ....................... . .PagePROPERY DESCRIPTION

LOCATION 6 ACCESS.......... PageACCESS. . . . . . . . . . . . . . . . . . . . . . . . . . . . PagePROPERTY GEOLOGY.................. PagePREVIOUS WORK. . . . . . . . . . . . . . . . . . . . . PageSTRIPPING, SAMPLING

6 BLASTING.............. Page 3PROSPECTING. . . . . . . . . . . . . . . . . . . . . . . Page 4CONCLUSIONS. . . . . . . . . . . . . . . . . . . . . . . Page 5RECOMMENDATIONS. . . . . . . . . . . . . . . . . . . Page 5Dunn l Kor ba property map geology map claim map location map

Appendix . . . . . Sample location mapsample locations .descriptions and

assay results. prospecting traverses

INTRODUCTION This report covers prospecting results fromfollow-up prospecting of last years soil sampling, prospecting and geophysical program.

As well results of detailed work on the auriferous shear zone is included which includes results of heavy metal analysis of selected samples of the pyritiferous shear.

RESULTS Prospecting in the areas of L 2+00 H 0+50S andL 4E 7+75S to follow-up on last seasons anomalous soil results turned up feldspar porphry dykes in both areas.Some quartz veining and shearing was sampled. /.-- On the main shear zone assays to -l* **//*- A", were returned. As well prospecting indicated . 30 *g./-f extensive shearing and a 5ft deep pit not previously seen near 280+00 sw along the shear. ( a topo-fil and flagged line was run the length of the shear for control from 0+00 to 367+00 SW) Greg Curry, geologist, was contracted to map the shear and adjacent area. The results are in a separate report.The shear zone has been traced for over 350m and is a quartz-carbonate system with extensive alteration (limonite,fuschite,ankerite) and mineralization (pyrite and chalcopyrite) with a 2m width in pyroclastic breccia and quartz porphry.

PROPERTY DESCRIPTION,LOCATION fi STATUS The claim groupis part of an original group of ten claims stakedin April 1990 during the staking rush whichresulted when the Temagami Land Caution boundarywas moved.4 northern claims were subsequently optionedto Pelangio Larder Mines and the remaining 6claims were explored in 1991 using OPAPfunding. As well a magnetometer survey wasconducted by the author in December 1991.The area of interest is located in lots l ft 2,concession 111, Tudhope Twp, Larder LakeMining Division, Ontario. The claims are heldin a beneficial agreement by Gregory Dunn,Gary Dunn and Ed Korba and are in goodstanding.The author .Gary Clayton Dunn, is the recordedholder of the six claims covered in this report.

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USD LAKEr^Uon Series[SKAMING DISTRICTS

SECTION—LARDER LAKE Al

lo4Mik*SECTION—REDSTONE RIVER AREA

ACCESS The claim group can be accessed by vehicle up the Cane/Barber Twp road and then by ATV to a creek. The last 1.5 miles can only be negotiated by foot up the Tudhope/Bryce Twp line due to rough terrain. Alternatively one can travel in the road to Heather Lake from the Hill Lake fish hatchery, but one still must travel the last mile or so to the property by foot due to rough terrain.

PROPERTY GEOLOGY The group is underlain by intermediateto felsic volcanics with minor inclusions of diabase and feldspar porphyry dykes. Pyroclastic breccia is found on the group west of heather lake which suggests the proximity to a volcanic vent. Shearing has been traced on claim 990957 parallel to the Palmer- Vaughan-Estival Break.

PREVIOUS WORK During 1991 soil sampling, prospecting and a VLF-EM survey were conducted utilizing OPAP funding This work identified several target areas to be followed up including an auriferous shear zone parallel to the Palmer-Vaughan-Estival Break. As well the author conducted a magnetometer survey on the group in December 1991 which indicated some mag* lows with flanking highs in the vicinity of the VLF conductors.

Although two old pits were discovered on the property no records can be found in the assessment files.

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STRIPPING .SAMPLING, 6 BLASTING During the period Hay 8,9,10 and lith,1992 a crew packed in a pump, hoses and fuel and explosives and stripped, blasted and sampled at pits labelled il to 15 inclusive along exposed portions of the shear zone. The locations and results are indicated on the accompanying map in the appendix.

Date Worker_______Work performed^^

May 8 Jayson Demeester Mob.and handstripping

May 9 Jayson Demeester Sluicing' Ed Korba

May 10 Ea Korba ; Sluicing ft samplingJ Demeester Sluicing

May 11 Ed Korba Sluicing 6 J Demeester de-mob. Greg Dunn "

A Wajax Mark 111 gas operated fire pump was used for the sluicing. The sampling method wa* panel sampling to get a representative sample of exposed areas. The blasting was concentrate^ at Pit 13 and due to the fact that all equipment had to be brought in by Argo then packed more than a mile, Gel-Pak explosives were utilized rather than a plugger and stick powder. The method was explained to us by a Spartan Explosives Rep (Mr Barry Austin) and proved successful in opening up the shear for sampling.

PROSPECTING During the period May 6.7,8 and May 11 theauthor prospected as detailed below to follow-up on last years program.

May 6 VLF conductor L 4E 7+75SMay 7 " "A"May 8 " "H"May 11 vicinity of shear zone

The results are as follows.

L 2+00 w near 0+75S a feldspar porphry intrusion was located. Shearing was noted @ NW strike and an outcrop w&tha series of parallel quartz veins up to 4" wide and dipping to the North @ 45 was sampled. The quartz veins are hematized and pyrite-rich with cubes up to lcm in

L 4+OOE near 7+75 S a feldspar porphry intrusion was located with shearing in the porphry in an E-W direction with some calcite and minor pyrite.

It is difficult to ascertain the size of the above noted intrusions due to overburden cover.

L 2+OOw near 6+25 S a sheared vocanic was observed with a strike of 70* along a linear overburden.filled valley which corresponds to VLF conductor "H" Little mineralization was evident. The area was subsequently soil sampled which is the subject of another report.

In the vicinity of the main shear zone detailed prospecting exposed additional areas of shearing and in particular another Pit was located near 280+00 SW along the shear. The pit appears to be slightly south of the line of the main shear and was blasted to a depth of 5 ft. Judging by the amount of overburden and vegetation in the pit and on the muck pile, the pit was likely dug in the early 1900 s, perhaps around 1907. (no assessment records have been found)

All sample descriptions, locations, and results are on the Map in the appendix.

The shear zone and immediate area was mapped bygeologist Greg Curry, the subject of another :r- report.

CONCLUSIONS The shear and adjacent area was mapped in detail by Mr Greg Curry and is the subject of a separate report.The stripping and sampling shows a well mineralized (Chalcopyrite, pyrite and pyrrhotite) and altered (limonite,ankerite and fuschite) shear zone in pyroclastic breccia with an adjacent quartz porphyry which can be traced for 350 m, with an average width of 2 m.The shear is open at each end and at depth The zone has returned values to *l9f **/?" yt"x - Zt **/?- A.

*75ibf 4f*~ IH and is well covered by our l claim group (The shear sits on the north part of L 990957 and dips to the south with claims L 990956 to the East and L 1134103 to the West)As well as the gold potential there is also the base metal potential. "Additionally,an exposure of very coarse, unsorted pyroclastic rocks in the Heather Lake area suggests the possible presence of a volcanic vent within the Archean Skead Group and can be considered a favourable location for the deposition of massive sulphides "(Johns 1986).

RECOMMENDATIONS The ore potential of the shearzone should be tested at depth by diamond drilling.

Lithological studies of the ". surrounding rock should be conducted to look for alteration haloes.

The possibility of a dilatent zone west of pit f4 where there is a N/E trending valley could be examined by soil sampling and geophysics.

ADDENDUM

NATIVE GOLD ANALYSISSamples 3137 and 3138 were analyzed

by Acme Lab in Vancouver for metallic gold (native gold). The results wre similar to the fire assay results and support the following gold grain count analysis which indicates that the gold is free gold and not present within the sulphides, (see appendix for results)

VISIBLE GOLD COUNTSSamples 3113 and 3113 were submitted to

TSL Labs and forwarded to Overburden Drilling Management for visible gold count. The results indicate the gold is "free gold" and not tied up within the sulphides. Gold grain size is in the 10 to 75 micron range. (see appendix for results)

CERTIFICATION

I Gary Clayton Dunn of La Ronge Saskatchewan do certify that I am a graduate mining technologist of the Haileybury School of Mines and have practised my profession in the mining industry continuously since 1974

dated at La Ronge Saskatchewan

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Gary Clayton Dunn

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MAY 22 '92 14:99 TSL LftBS SHSK. 1-306-242-4727 PflGE 2

TSL LABORATORIESl - MM - 4Mb STREET, EAST

8A8KATOOH SASKATCHEWAN

0006)981-10*9 FAX(90B)MM717

CERTIFICATE OP ANALYSIS

BAMPUfs) FROM Mr. Gary Dunn Box 995La Hong*, Saak, 80J 1LO

•AMP1EWOF ROOk

REPORT No. 84221

INVOICE P.O. s

19303

O. Dunn Projects Tudhopa

31163117311831193120

31213122312331253127

31283129313031313132

31333134313531393140

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COPIES TO: O. Dunn INVOICE TOt O. Dunn

Nay 22/92SIGNED

For WMiuinn on thh raport. plww eontaet Ourtemw awvte Otpartmwit. SwnplM, Puli* and Rtfwtt dteirdwl two month* from th* d*t* of thU raport.

Page l of l

TSL LABORATORIES2 - 302 - 48th STREET. EAST

SASKATOON. SASKATCHEWANS7K6A4

© (306) 931-1033 FAX (306) 242-4717

CERTIFICATE OF ANALYSIS

SAMPLEIS) FROM Mr. Gary Dunn Box 995La Ronge, Sask. SOJ 1LO

SAMPLEIS) OF Rock

REPORT No. S4028

INVOICE ft: 19126 P.O.:

G. Dunn Project: Tudhope

311331143115

Au ozt

.002

.001

.033

Cu

34025

730

COPIES TO: 6. Dunn INVOICE TO: 6. Dunn

Mar 24/92SIGNED

CTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report.

Page l of l

ICP - .500 QRAN SAMPLE IS DIGESTED WITH 3ML 5*1-2 HCL-HN03-H20 AT 95 DEQ.C FOR ONE HOUR AND IB DILUTED TO 10 NL WITH WATER.

THIS LEACH IS PARTIAL FOR MN FE SR CA P LA CR MO BA TI B W AND LIMITED FOR NA K AND AL. AU DETECTION LIMIT BY ICP 18 3 PPM.

ASSAY RECOMMENDED FOR ROCK AND CORE SAMPLES IF CU PB ZN AS > IX, AQ > 30 PPM ft AU > 1000 PPB - SAMPLE TYPE: ROCK

PT" BY FIRE ASSAY ft ANALYSIS BY ICP/ORAPHITE FURNACE. -100 MESH AU BY FIRE ASSAY FROM 1 A.T. SAMPLE

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41P09NE0118 OP92-56 TUDHOPE 020

SOIL SAMPLING

CLAIMS L^1134103 6 1134104

TUDHOPE TOWNSHIP, LARDER LAKE MINING DIVISION, ONTARIO

by: Gary Clayton Dunn Mining Technologist

date: July 18 1992

OPAP 092-056

l41P09NE0118OP92-56 TUDHOPE 020C

TABLE OF CONTENIb

INTRODUCTION..........................................page l

RESULTS...............................................page l

LOCATION MAP..........................................page 2

DISPOSITION 4 GEOLOGY SKETCH..........................page 3

PROPERTY DESCRIPTION 4 LOCATION.......................page 4

ACCESS................................................page 4

PROPERTY GEOLOGY......................................page 5

PREVIOUS WORK.........................................page 5

AIR PHOTO OF STRUCTURES...............................page B

TOPO MAPJ'ROPOSED DRILL ACCESS....................... page 7

PROSPECTING S SAMPLING................................page 8

CONCLUSIONS..........................................-page 9

RECOMMENDATIONS.......................................page 9

APPENDIX

INTRODUCTION: This report covers a soil sampling survey conducted over mining claims 1134103 and 1134104 with the purpose of tracing the extension of the known auriferous quartz carbonate shear found on mining claim 990957.

Detailed work on the shear resulted in the discovery that it contained Pb and Zn and Ag as well as the Au and Cu previously known.

With this knowledge the soil samples from Bl horizon soils were submitted to ACME Lab in Vancouver for ICP 5-element analysis. In the past the PPb Au assays were not producing definate targets.

RESULTS: The survey successfully identified a couple of target areas. Anomalous Cu, Ni and Ag haloes were centred over VLF conductor "H". As well a strong Zn and Cu anomally is located in a shallow creek valley just downslope from VLF conductor "G".

Two spot highs of Au and Ag up to 3 ppm were also identified.

PROPERTY DESCRIPTION S LOCATION: The two claims coveredin this report are part of a group of ten claims stakedduring the staking rush when the Temagami LandClaim Boundary was relaxed. Four claims to thenorth were subsequently optioned to PelangioLarder Mines and the remaining 6 claims areregistered to the author and are all in goodstanding. The claim group is located inlots l S 2,concession 111, Tudhope Twp, LarderLake Mining Division, Ontario.

Property Locotibn

LOCATION MAP

SCALE: l inch to 4 miles

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ACCESS: The claim group can be reached by driving up the Elk Lake Highway to the Cane/Barber Twp road and driving in to the end. From there an Argo all terrain vehicle was utilized to gain access across the beaver pond etc. From there one must still walk over rugged terrain for 2 miles to the claims surveyed. Alternately, one could gain access via the Heather Lake road to Heather Lake but one must still walk the last 1.5 miles through rugged terrain to reach the claims.

PROPERTY GEOLOGY: Detailed mapping by Greg Curry (see his report) shows that the property is underlain by a felsic volcanic sequence including Tuff, rhyolite and in the vicinity of the known shear, pyroclastic breccia. As well intrusions of quartz porphyry are noted.

Structures parallel to the Palmer-Vaughan- Estival Break running at about 070 are considered important.

It is suggested that the largefragments of pyroclastic breccia seen adjacent to the known shear on claim 990957 indicate the proximity to a volcanic vent.

SOIL SAMPLING: The soil sampling survey was conducted by the author on May 4 and May 12 1992. Bl horizon samples were taken with a grubhoe following accepted sampling procedures being careful not to contaminate the samples etc.(about one large handful placed in paper soil bages and labelled).

A compass and topo-chained grid was established for the survey and all sample locations flagged and labelled.

Line 1+SOw was run instead of 1+00 w due to the amount of swamp seen on l^OOw.

The Bl horizon in this area is considered reliable due to the type of soil cover and intermittent outcrop indicating shallow overburden cover.

RECOMMENDATIONSS, CONCLUSIONS: Trie spot highs of 3 ppm Au should be

investigated by prospecting. The anomalous Cu, Ni and Ag haloe over the VLF conductor "H in the vicinity of L2+OOW, 6+25 S should be prospected in detail. The cu, Zn haloe in the vicinity of VLF conductor "G" should also be prospected in detail.

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41P09NE0118 OP92-56 TUDHOPE030

PROSPECTING and SAMPLING

(phase 11 )

Claims L 990957. L 1134103 6 1134104 Tudhope Township. Larder Lake Mining Division

Ontario

by: Gary Clayton Dunn Mining Technologist

date: August 22, 1992

OPAP 092-056

lTABLE

41P09NE0118OP92-56 TUDHOPE 030C

INTRODUCTION..........................................page l

RESULTS...............................................page l

LOCATION MAP..........................................page 2

DISPOSITION b GEOLOGY SKETCH..........................page 3

PROPERTY DESCRIPTION S LOCATION.......................page 4

ACCESS................................................page 4

PROPERTY GEOLOGY......................................page 5

PREVIOUS WORK.........................................page 5

AIR PHOTO OF STRUCTURES...............................page 6

TOPO MAPJ'ROPOSED DRILL ACCESS....................... page 7

PROSPECTING A SAMPLING................................page 8

CONCLUSIONS...........................................page 9

RECOMMENDATIONS.......................................page 9

APPENDIX

INTRODUCTION: This report covers the second phase ofprospecting and sampling designed to follow up on the results of the spring program of prospecting, sampling, mapping and soil sampling.

Due to the kind assistance of Dr Andrew Gracie, Resident Geologist in La Ronge Saskatchewan, a sample of the 1000 ft long auriferous shear zone on claim 990957 was submitted to Vancouver Petrographies for thin section analysis. This resulted in the discovery that as well as the Au and Cu the zone also carried Pb and Zn.

As well, the Resident Geologist in Cobalt Ontario ( Mr Jim Ireland ) submitted a sample for assay and determined that as well as Au and Cu the zone also conatained Ag.

Based on this information additional sampling and assaying on the DK Zone was warranted.

Soil sample results from the spring program identified the following targets which were also investigated.

L 0+00 9+50S anomalous Au and Ag

L 0+00 6+25S

L 2+OOw 6+50S anomalous Cu, Ni, Ag

L 1+SOw 6+25S

L 1+OOw 3+50S anomalous Cu, Zn haloe

RESULTSrThe program successfully verified the thin sectionresults with assays from the "DK" Zone to 0.06 oz/T Au, ISppm Ag, 4430 ppm Cu,1163 ppm Pb and 1415 ppm Zn.

As well prospecting in the vicinity of L2+OOW, 6+50S on the VLF conductor "H" and anomalous soil zone resulted in the discovery of a new shear zone now labelled the "moosehorn Zone" . Here shearing is seen over a 30m width parallel to the "DK Zone" in a sequence of volcanics grading Tuff to Rhyolite with assays in a parallel 20cm wide quartz vein of 0.11 oz/T Au and 1493 ppm Cu.

i Property Locotibn

LOCATION MAP

SCALE; l inch to 4 miles

FIGURE l

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PROPERTY DESCRIPTION 5, LOCATION: The claims prospected are part of an original group of ten claims staked during the staking rush which resulted when the Temagami Land Claim Boundary was relaxed. Subsequently four northern claims were optioned to Pelangio Larder Mines. The remaining claims are in good standing and registered to the author.

The group is located in Lots l S 2, Cone 111 Tudhope Twp, Larder Lake Mining Division, Ontario.

ACCESS: Access to the property can be gained Via the Heather Lake road from the Hill Lake fish hatchery west of Englehart to Heather Lake and then by foot 1.5 miles to the group. Access is also gained by driving up the Elk Lake Highway to the Cane/Barber Twp line and then in to the end of the road. From there one must travel by foot fot 3 miles over rugged terrain to access the group. An ATV was used in the spring program to access the first mile or so but from there one must still go on foot.During the August program access was gained with an eye to skidoo travel in the winter and the best routing for diamond drill access. In the 60's Trihope Mining gained access to the north end of this group up the "leeville" road. This route it appears would be suitable for drill and skidoo access in the winter only as it is quite wet in places. An old road ran north almost to the claim group.It is grown up with alders but could be brushed out and utilized.(there was an old farm and field up this road, now overgrown) This is the suggested route for diamond drill access in the winter months.

y

PROPERTY GEOLOGY The p roperty i s underlain by a volcanic sequence of the Skead Group. In the vicinity of the DK Zone pyroclastic breccia is encountered which suggests the proximity to a volcanic vent. As well at the E-end of the shear quartz porphyry is seen, which may be related to the large porphyry intrusions in Bryce Twp.

In the vicinity of the Moosehorn Zone a volcanic sequence of sheared lapilli tuff and possibly feldspar porphyry and rhyo dacite is seen.

PREVIOUS WORK The property has been systematically explored for the past two year using OPAP funding. VLF surveying, Mag surveying, soil sampling and prospecting have all been utilized in an effort to locate auriferous shear zones.

A 1000 ft long, 2m wide shear zone was successfully located on claim 990957. This zone was subsequently mapped and sampled after sluicing.

The spring soil sampling program turned up anomalous values coincdent with the VLF conductors.

Referring to Greg Curry's geology report from the spring program, he recommends using Cu and Zn as pathfinder metals in the soil sampling program as well as following up on the VLF conductors to locate parallel shears.

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PROSPECTING AND SAMPLING: During the period August 9-13 Inclusive the author with a helper prospected, stripped and sampled (see map in appendix) parts of mining claims 990957. 1134103 and 1134104. The "DK" Zone in the vicinity of Trench 3 and Trench 5 was further mucked out and sampled. The assay results verified the presence of Au, Ag, Cu, Pb and Zn shear and are appended.The spot highs of 3ppm Au were investigated but only minor shearing @ 070 was seen and the thin, barren quartz stringers returned negligible Au. The area of L 2+OOw, 6+50S was concentrated on due to the anomalous soil haloe and coincdent VLF conductor. Here shearing was discovered and detailed work over 3 days resulted in the discovery that the shearing extended over a 30m width in a volcanic sequence parallel to both the "DK Zone" and the Palmer-Vaughan-Estival Break.An enclosed quartz vein at the same orientation returned Au and Cu values. Visible chalcopyrite was noted.The outcrop here is composed of a sheared Rhyodacite with pyrite crystals and is carbonatized (reacts to HCL)The outcrop exposure drops off into a muskeg to the west and is covered by overburden to the East. A definite structure is coincident with the VLF conductor. The area of the anomalous Cu and Zn in soils near VLF conductor "G" was examined. The high values are in an intermittent creek valley but it is of note that this area is downslope from VLF conductor "G" and may well indicate that structure. The outcrop exposure is poor in this area.The conductor or anomalous soils was not explained by prospecting.

Date Employee Work

Aug 9 Jayson Demeester stripping S, mucking Southshore Rd out T-3 T-5 Astorville Ont

Aug 10 " Strip outcroppack samples

Aug 11

Aug 12 S 13 Wayne Batisse Strip O/C Moosehorn Zone Matachewan Ont Pack samples

CONCLUSIONS: Two parallel structures have been discovered to date parallel to the Palmer-Vaughan-Estival Break. The Moosehorn Zone displays shearing in a volcanic sequence over a 30 m width with assays to 0.11 oz/T Au and 1493 ppm Cu.

The DK Zone has been traced over a 1000 ft length and 2m width with assays to 0.194 oz/T Au, 13 ppm Ag, 7568 ppm Cu,1163 ppm Pb and 1415 ppm Zn.

Air photo interpretation suggests a N/E trending structure cutting these two zones (see fig l in appendix). The possibility of a dilatent zone exists.

The exposure of pyroclastic breccia cut by the DK Zone suggests the proximity to a volcanic vent.

"Additionally, an exposure of very coarse unsorted pyroclastic rocks in the Heather Lake area suggests the possible presence of a volcanic vent within the Archean Skead Group and can be considered a favourable location for the deposition of massive sulphides" JOHNS 1986.

RECOMMENDATIONS: The ore potential of the two zones should be tested to depth by diamond drilling.The zones may well widen and become more mineralized at depth.

A detailed grid should be cut @ 50 line

spacing and an IP survey conducted as well as geological mapping of the entire property. One could also consider a lithogeochemical surveyto outline an alteration haloe.

As recommended by Greg Curry in his geology report the other VLF conductors should be examined (A.A+ and G) as they display similar characteristics as conductor H which was on the 30m wide Moosehorn shear Zone.

The ground to the west is closed to staking due to the Temagami Indian Band Land Caution. When the boundary is lifted, the claims will be moved to their full size and one should agressively tie-on more ground to the west.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 1 87. POJ 1KO

HAILEYBURY. ONTARIO TEL: 672-31O7FAX: (7O5) 672-5843

Ckrttfirat*NO. 192

SAMPLE(S) OF:

SAMPLE(S) FROM:

Rock ( 6

DATE: August 12, 1992

RECEIVED: August 1992

Sample #

314131423143314431453146

Au ppb

1080121118118111851

Ag ppro

Cu ppm

Pb ppm

Zn ppm

1318454430

1493

146*

1163

265*

1415

: * no charge,

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE COLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS

BELL-WHITE ANALYTICAL LABORATORIES LTD.

BY: XEROX Telecopier 7017! 8-21-92 I 14=12 i 7056423300* 306 425 4110;*

Swastika LaboratoriesA Division of AM*ytr* CoiporaUon Ltd.

Assaying - Consulting - Representation

' Assay Certificate 2W-Q881-RA1

j Comply: GARY DUNN Dal.: AUG-21-92j Prtjoct: Copy l. BOX995,LARONOB,SA5KSOJILOl Attn: 2. FAX 306-425-4110ii We hereby certify the following Assay of 5 ROCK CHIP AND ROCK samplesl submitted AUG-14-92 by.

! Saoqple ( Ntanber; 31427

3147 1 3148 j 3149

i i

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1

1j

i

Au Au check oz/ton o? 1 ton0.060 0.002 0.084 0.108 0.108 0.014

Ag Cu Pb PIM PIM PIM3.0 2030 741

30 616

1290 31

Zn PIM539

Certified by_

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705)642-3244.

CERTIFICATION

I Gary Clayton Dunn of La Ronge Saskatchewan do certify that I am a graduate mining technologist of the Haileybury School of Mines and have practised my profession in the mining industry continuously since 1974

dated at La Ronge Saskatchewan , ^

tGary Clayton Dunn

41PO9NE0118 OP92-S6 TUDHOPE 040

REPORT ON SPRING 1992 EXPLORATION ACTIVITIES TUDHOPE TOWNSHIP, ONTARIO

LARDER LAKE MINING DIVISIONDISTRICT OF TIMISKAMING

CLAIMS L-990956, L-990957

^2*a-C^,d^

September 1992 G.L. Curry BSc.

41PO9NE0118 OP92-S6 TUDHOPE

TABLE040C

i l

SUMMARY RECOMMEKDATIONS

i.O INTRODUCTIONi . l Property and Ownership 1.2 Physiographyl O T r-* —k ^a 4- -S (—i *^ s ••-t c' A '~- ~* *^ *~ -—l---/ lj^-; 1—3. J j.Ori ^AiiG H--^*5cjii

1.4 Provicus Work1.5 Objectives for 1992L.6 Program in 1902

2.0 GRID ESTABLISHMENT

3.O GEOLOGY3.1 Rc-gicnal Geological Setting3.2 Local Geological Setting

4.0 MINERALIZATION4.1 Target Definition 4

5.0 DK SHEAR ZONE - OUTCROP STRIPPING, MAPPING AND PROSPECTING5.1 Results - Description of Shear Zone 45.2 Results - Detailed Description of Pits and

Sarsplo Results 5

23

6.0 PETROGRAPHIC WORK

7.O DISCUSSION

S.O CONCLUSIONS

9.0 RECOMMENDATIONS

REFERENCES

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LIST OF FIGURES-a ;r e

FIGURE i Location Map i FIGURE 2 Disposition Map i i FIGUFH 3 Geolcgy Map of DK Shear Zone- Grid and Back

Detailed Geology of Pits FIGURE 4 1902 Prospecting Results Back

LIST OF TABLES

Table i : DPC Shear Zone "Pits" Significant Analytical Re-cults

APPENDICES

APPENDIX I : Sunmary and Distribution oi Eield Work for 1992APPENDIX II : Field Personnel 1992APPENDIX III : Outcrop Sample Descritions and ResultsAPPENDIX IV : Petrcsraphic ReportAPPENDIX V : Statemont of Qualifications

i Property Location

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SUMMARY

Claims L-990956 and L-990957 are located in Lot l, Concession 111, Tudhope Township, Larder Lake Mining Division, Ontario, NTS 41 P/9. These claims are recorded to Gary Clayton Dunn. P.O. Box 995, La Ronge, Saskatchewan, SOJ 1LO.

Exploration activities were concentrated over the western portion of claim L-990956, and the eastern portion of clain L-990957.

The claim blocks are underlain by the southern extremity of the Early Precambrian metavolcanics of the Abitibi Greenstone Belt. Specifically, the geology consist of: intermediate volcanic pyroclastics, lapilli tuffs, ash tuffs, and a subordinate quartz- feldspar porphyry intrusive.

The Spring 1992 exploration program comprised: grid establishment, outcrop stripping, prospecting, and mapping. The program followed-up positive results from the 1991 exploration program. The area of interest was a gold bearing quartz veined shear zone, now referred to as th DK Shear Zone, which occurs within a intermediate pyroclastic breccia, and ash tuff.

The DK Shear Zone was traced along strike for 335 m by prospecting and by five overburden stripped pits emplaced over the projected strike. Outcrop stripping exposed trace to 2,'f. chalcopyrite, pyrite, and minor galena and sphalerite mineralization within and adjacent to the quartz vein. The quartz veins are: fractured, brecciated, locally boudinaged and rodded, and are commonly sericitized and carbcnatized. Grab samples returned maximum assays of 0.061 oz/t.cn Au, 8.2 ppm Ag, and 0.49 *~', Cu. A quartz-feldspar porphyry occurs at the extreme northeast end of the shear.

RECOMMENDATIONS

Because of the positive results to date, the following programs are recommended.:

1) re-analyze all grab samples for zinc and lead.2) explain the VLF conductors obtained during the May, 1991 survey, through prospecting and soil sampling. These conductors parallel the strike of the DK Shear Zone, and occur in close proximity to it.3) test for additional mineralized shear zones on the properties using detailed prospecting and soil sampling techniques.

INTFGDUC7 ION

un May c- f 1-1*92 3. 12 day gold exploration. prcgrarr. was c endue*: i? d over portions o/ claims L-OOOO^ft, and L -000957 utilizing f undine; provided by the Ontario Prospecting Ass istance ?'roc'ra:n. The details and results ai this program arc- presented in this re per*.

1.1 P r c port y and OwnershipClaim blocks L-99005C/ L-990957 are located in; let l Concession 111, Tudhope Township, Larder Lake Wining Division, Ontario, NTS reference 41 P--9 (Figures l S 2). Those claims are part of an original block of 10 claims stacked April, 1990 and are recorded to Gary Clayton Dunn. P.O. Box 095 La Rongo, T:;; z:katchewan ^Recorded April 4/00).

l . 'I: PhysiographyThe claims are character ized by lev/ undulating relief with local rolief locally (--:-:ceed i ng 15 ra. Valleys and depressions are comma M l y filled with thick glaciofluvial material and/or muskeg. Outcrop ijxrjcsure is gcod at 45 to 55^

1.3 Location and AccessThe c la lias are located within NTS :nap sheet (1:50 000:- 41 P/9. The claims are located approximately 12 kms. east of Elk Lake, Ontario or 45 air-kilometers south of Kirkland Lake Ontario.

Accosr. to t ho southern c-dge of the clairr.s is gained by a 2 km traverse north along the Bryce/Tudhope Township line, which loaves the Cane/Barber Township road located west of the town of Kenabeck. Tho township road runs north-south off of the Elk Lake Highway #560.

l . 3 Previous workPrevious work en the claims is summarized Below:

12512 ^ (~? ) '- t renching alcng a gold bearing northeast- trending shear ::one, OIow referred to as DK Shear Zone), exact time- and results unknown.

il^.'''r '5.:lZ-'5.I-^L2LLLi-if!.2. : Siak ing/ prospect i ng prohibited in Tudhsr-e Township area due to litigation over land ownership (Indian Land Caution, Tenagarci Indian Band).

Apr i^/OOj Staking restriction lifted on part of the Tudhope Township. Claims mentioned in this report were acquired.

vM: prospecting, soil s a rao l ing and VLF surveys done over portions o f - i/iirts L--'? O O O 5^ and L-OOOO57 utilizing OPAP funding. The VL? surv.-sv de- 1 i nc.a* :;d a sorie:; of oast-west, cor.iu.'icrs parallel the Pal-er-Vaughan-Estival Prcak. Se- i I dclir^at^d woaklv anomalous values in the vicir.'y of the "IF

ccniuctcrs. Trenching over the DK shear sc:;e discovered ir: the 10:0's - ?) was rediscovered and resampled returning a maximum -r r..i b sarr.ole v.ulue T: f 0.10-1 o::/-1: on Au and G.07% Cu.

-01: -la; 1 not D me ter survey over t ho mineralized I'K Shear Z^ne and~VLF conductors outlined in May/91. The survey outlined the shc-ar as a relative "lew" expression with flanking mag

i . "r Ob.-; e c t i ve 3 in 1 002Th-2 objectives of the 1992 program wore to:1) evaluate the area of the DK Shear Zone.2"! g round check VLF conductors by prospecting and soil a

sampling survey.3 ^ evaluate the mineralized potential of drift covered areas

using soil sampling surveys.

l . -5 Program ir. 1902w

l ) grid es nabl ishmer.t .? '- Trapping, prospecting and outcrop stripping of the DK Shear

Zone . .' ) or~ c s p-ec t aiid soil sarnoie in areas c ± * LA* concuctors.

2.0 GRID ESTABLISHMENTA flagged grid was established over the mineralized DK Shear Zone located in 1091. The baseline occurs along the known strike of t h fi shear. while crosslinks were established at intervals coinciding with the washed pits. Lines extended 100 K. north and i;outh of the baseline.

• J,. O GEOLOGY

3.1 Peg i o na l Geological Setting_ f' nG claims occur within ^ho Tudhope

Township of the Hill Lake area. This area is underlain by the :.c;:thern extremity of the Early Precambrian me tavolcan ics of the Abitibi Greenstone Bc: Ir. Th 1 c-. oortion of the Belt comprises in^e: mediate to felsic calc-alklic pyroclastic rocks, which vary "La-orally from unsorted pyroclastic breccia, tuff-breccia, i^Tji i j-i~Tuij. an~ i^u-i.i : -- i.n b/rvce ano lud^iope ^ownshios to a i^-e^^er :cr-.ed. bedded secu-^nce of lapi l l i - tuf f , tuff. lapillistone and pyrccla--tic breccia in the Beauchamp and Dack Townships. Because o* Tine vo-rv coarse "c-yr oc las* ic roc^cs which occur in tne Tu^noTue Township a volcanic vent has been suggested to occur in the Heather lake area of the Bryce Township, (1.7 km east of 990056 St 90CO57). The volcanics are locally intruded by dykes of intermediate composition, the source of which could be a feldspar porphyry, 5.6 square kras, which occurs within the Bryce Township.

_990055 and 000957 ^r^ largelyi n t--r ni-2 ;ii i a t o vc3iC:inic pvrcc .ast ic oreccias along

rdir:atc- intermediate volcanic ash and lapilli tuffs. ..ill

of which are precamb: ian in are arid belong to the Skead Group. The rocks arc D: greenschist metamorphic facies.

Outcrops within -.he vicinity of the gold-bearing DK Shear Zone- located in claims L-OOOvsO and L-990957 wore- mapped by G. Curry during M^y 11-12/02 and i 3 presented on Figure 3.

INTERMEDIATE VOLCANICS 'Unit 2) comprise QQ-%. of the outcrops within the vicinity of the shear zone. They comprise pyroclastic breccias and subordinate ash and lapilli tuffs. Outer-ops weather greenish grey, v/h i l o or. fresh surface the rocks arc dark green. They are massive to local lv foliated/shoared. Chlorite and/or carbonate cormanly occur along fracture and foliation surfaces.

Ash tuffs (Unit 2a ' comprise less than 5 J4 of the volcanic assemblage. They are fine-grained ^ less than l itm 1* , and are finely to moderately laminated to thinly bedded and may contain significant amounts of calcite alcns; lamination planes.

Lapilli tufi Unit 2 ':: l comprise 20 to 25'i of the volcanic assemblage. It is comprised, of fine-grained intermediate to rr-zjf ic volcanic rock fragment:, and sub-rounded white/pink feldspars varying in size from 4 to 10 iron. The clasts are well rounded arid are sot in a fine-grained. well sorted intermediate matrix. Chlorite and carbonate and rare sericite alteration occur a l or. 5: local fracture surfaces.

Intermediate Pyr c-.- last i c Breccia '.Unit 2 o) comprise 70 to 752. of the volcanic assemblage. The breccia is composed cf f ragrn^ntc/bl oc x -~. varying in size from 12 to 50 cm, which are set ir. an ash and lapilli matrix. The py r ac l ac tic material is composed of subangular fi agmonts of intermediate volcanic r:sh ^r.-l lapilli tufr. The ma t r i:-: is more mafic in composition -;hir: its in'-or por ated frag::.enr.s 'blocks.

FELSIC TO IKTHRMni.'IATE INTRUSIV^S ^'Jnit 7) compr i-i.c lo-; r- th.^n -f{. :;f the r;utc- r :::us wit:. In the vir.inity of the shear mono.

Quartz Fildsr^r Tcipjivrv M.r nit 7-:) is the mo^t pre lorti :.a t i c-:r -he rLJpr,.; -r. int. r us L ve--:-. Thii uni* is restricted to the . i:: * r e ra..- c^-.-.r-rn r/or t - on Df the IK Shes: Zcr;e. Outcrops weather grev whit"' AT. "i are :aa:;s L vn to v;e.slr. lv -" hc.3 r od . T:;-- porphyry cant.-ins 20 to 30"^- sub rounded quart- ar.d feldspar phenocryst^ Crsax. 8.0 ram; se^ ir. a very f ine-.grained f e Idspat hic-ouartz rich n^tr:::. Feldspar phenocrysts are commonly clay altered. Carbonate, sericite and rare fuchci 4-^ cccur r-1 or. g fracture ar.d/cr shear pl-.ar.os. Seccr.dary quartz stringers and veins commonly occur within the Dcrohv:y when in r: OR t ac t w i r. h the volcanics.

Feldspar Porphvry ;Ur. i* 7b.^ occurs as two outcrops in the cvrr.-mc south esr t ion cf the- r: id '-L 3 2-^OOSV/l-t-i OS ) . Oi.itcrori'- v.-.-; a t he r

- 4 -

rr^y and are massive, and contain 25^ subangular feldspar ohenocrysts 'max. 5.0mm) set in a felsic matrix. Feldspar nhenocyrstc are cornr-.cnly clay altered.

l .0 M I MURAL I ZAT I OK

4. i Target DefinitionGold occurrences which have been found in the Tudhope Town-ship aroa are hosted within intermediate/mafic volcanics. The gold mineralization commonly occurs within carbonat ized-quartz veins found in northeast trending shear/fault zones, which parallels the rsa; or " Pa Imer-Vaughan-Est ival Break", (N 060 degrees E). Those veins have associated pyrite, chalcopyrite mineralization.

5.0 DK SHEAR ZONE - OUTCROP STRIPPING, MAPPING Si PROSPECTING Twelve nandays were spent outcrop stripping, mapping and prospecting along a previously discoverd gold bearing shear zone, (now referred to as the DK Shear Zone). The shear zone was rediscovered in May of 1991.

Five old pits which exposed the shear zone along strike were recpar.ed using a wajax pump to expose fresh sampling surfaces. Mineralized quartz-carbonate vein/stringer material along with strongly altered rock hosted within the shear zone were routinely sampled and exposed.

A total of 24 rock samples were collected and sent in for Au, Ag and Cu determinations to TSL Laboratories located in Saskatoon, Saskatchewan.

5.1 Results - Description of Shear ZoneDetailed geology of pits is presented on Figure 3. Sample locations and analytical results are plotted on Figure 4. Sample descriptions along with results can be found in Appendix III.

The shear zone has been followed by 5 pits at intervals for a strike length of 335 m. The zone occurs within a variably sheared outcrop of intermediate volcanic pyroclastic breccia and ash tuff. A quartz-feldspar porphyry has been exposed within the extreme northeast end of the shear. The shear varies in intensity of developed fabric from strongly foliated to being reduced to a schist. The shear also undulates in width along strike from 0.3 to .3 maximum of 2.5 ra. Irregular shear controlled quartz- carbonate veins /stringers occur within all trenches. The quarts - carbonate veins/stringers trend at Az 053 to 070 degrees and dip at 85 degrees southeast to near vertical.

The quartz-carbonate veins/stringers are highly strained, locally brecc iatcd/rodded and/or vuggy and gcssaned. They vary in length* r- r ~.~r* n 1 4- ~ O ^ ~i T. r (-l ^r* .LlvJ**. *j . i L -j . _ . ^ .d uili^f. j. l L

and rare fuchsite occur along the selvedge of the veir.s/str ingers ::-:" coating fracture surfaces. Adjacent to the quartz-

- 5 -

carbonate the volcanics are commonly intensively sheared, or reduced to a chloritic schist, and loyally bleached (grey).

Mineralisation occurs within or adjacent tc cunr t z--carbonate vi.: i ns/str i ngers and is con-posed of pyrite, chalcopyrite and less commonly galena, sphalerite and rare cuprite. The sulphides occur as disseminations. irregular clots, or as thin discontinuous veiniets, and locally as "matty" fracture infills within the brecciated segments of the quartz--carbcnate vei ns/str i ngars . They may form up to 2' over restricted intervals. Copper oxide (malachite) collison! y crcurs within the more weathered cuartz- carbonate ve i ns-' st r i ngers.

5.2 Results - Derailed Description of Fits and .Sample Results

Pit #1 c.32*-00 SV/E.L. - exposed for 10 m x 6 m. Best exposure cf the quart z - feldspar porphyry in contact with intermediate volcanic. Within 0.1 m of the contact with the volcanics the porphyry is: moderately sheared at 053 degrees/P-5 degrees SE, sericite and fuchsite altered, and contains 5"X quartz- carbonate veins. The veins are vuggy and redded (055 degrees CV). Within 3 ra of the contact with the porphyry the volcanic is: intensively sheared, locally reduced to a chloritic schist, with an overall bleached look. The quartz-carbonate veins/stringers, located within the volcanic, ' r '. 2 'xi) , are brecciated and bcudi r.aged .

Pyr i te/cha lcopyr i te ~-:.p to 2.7* a long with trace galena occur within and along the selvedge cf the quartz-carbonate veins/stringers. Grab samples returned maximum values of: 120 ppb Au, O. \ ppm Ag ani 23 ppm Cu.

Pit #2 (97*00 .vW/B. L. ) exposed for 3 m x 2 m. A "sliver" of quartz-feldspar porphyry. ( 2 ra x 0.2 ra) occurs within the volcanic. The porphyry is intensively sheared at 070 degrees/32 degrees .C'W, and weakly carbcnatized/sericitized. The volcanic contact is reduced tc a chloritic schist. Quartz-carbonate occurs as str ingers/pods and is restricted to the volcanics '-'-. 17,). Slickensides within t ho volcanics are oriented at 070 degrees/55 degrees SW. A bleached alteration halo extends for 5 m :ntc the volcanics south of t ho pit.

Pyr i te/chalc.opyr ite up to l '/* a long with trace galena ocrurs within the quartz-carbonate stringers/pods. Grab samples returned maximum values of: 260 ppb Au, 3.4 ppm Ag and 91O ppm Cu.

Pit #3 (209+00 CW/3.L.) exposed for 12 m x 2 m. The volcanic is variably sheared along strike (053 degrees/35 degrees ). The volcanic is weakly tc moderately chloritized, with a moderate development of carbonate, j.nd sericite along shear cand fracture surfaces. A '.-.r--c : "i j t- -.-d quarto-carbonate vein 2.5 m x 0.5 ra occurs parallel to the shear, it has a pitted surface and a r. strained texture.

- 6 -

Pyrite, chalcopyrite, galena and sphalerite occur up to 2 7. within the quartz-carbonate vein, as fracture controlled disseminations. Galena also occurs as fracture controlled ve inlets. Grab -samples returned values in thor 250 ppb Au to 0.10 oz.'ton/ Au, 2.0 ppm Ag to 0.30 c-/ton A.g and 530 ppm Cu to 0.76 ua^Tztn C u range. Two grab samples were analyzed for platinum and returned values of 4 ppb.

Pit #5 (262*-00 SV/OfOO S) exposed for 4 ra x 2 m . The shear within this pit is '- l is wide, (032 degrees/90 degrees) and is offset to the south of the ^ain shear zone by 9 ra.

Trace chalcopyrite and cuprite (?) occur as disseminations along quartz-carbonate coated fracture surfaces. A grab sample returned values of 0.053 oz/ton Au, 2.2 ppm Ag and 1800 ppir Cu.

Tit #4 (367+00 SV/B.L.) exposed 5 m x l . 5 m. The shear within this pit is ' l ra. wide, (068 degrees/85 degrees SE). Several quart-carbonate veins/stringers occur subparallel tc the shear, they are bcudinaged, pitted and irregularly gocr-saned. The volcanic is weakly chloritized and carbonaticed with rare sericite developed along shear surfaces.

Trace to i Y, pyrite > chalcopyrite occurs along quartz-carbonate selvr-dges. A grab sample of a pyrite, chalcopyrite bearing quartz-carbonate stringer returned values of: 30 ppb Au, 0.25 oz/tcn Ag and 47 ppra Cu.

Significant analytical results are summarized in Table 1.

TABLE i : DFC SHEAR ZONE "PITS" - SIGNIFICANT ANALYTICAL RESULTS Trench No. Sample No. Au Ag Cu ^

(ppb cz/tjjTi) (ppm 2 .ili2H' f.2.E-i?

I no significant values2 no significant values3

45

0

3333Q

3o ^

116L 1812C123137133130139

0.0.0.0.0.0.

300.

10051040

. 061044

. 059

. 053

5.9 .5.O

9.8.7.2.

0o320

. 88

. 2

590980

n

0.0.0.

470.

2 '5

. 492676

. 13

6.0 PETROGRAPHIC WORKOne rock sample takenVancouver Petrographies, located in Vancouver B.C. to determineits ~inera Ice: ica l composition. The sample was cf a r:ineral izedtr o r-r iated auartz vein. Petrographic description r. s wo 11 acac ic:npanvi n," c-icturcs ran be found in AcoendiM IV.

- 7 -

7.O DISCUSSIONThe spring exploration program focused on upgrading the DK Sh?arZone- discovered in 1991, this was accomplished by: outcropz '. r i iM^int* ^ e c - c -? i c a l riia o o i n , a n *.A o r o s TDO o t i n s^.. * ' i p i i . j * ii—t ~ ~ cj

The DK Shear Zone occurs within an intermediate volcanic pyroclastic breccia, and ash tuff. The shear zone has a strike length of 335 m and a variable width of 0.8 to 2.5 m, quartz- carbonato veins and stringers up to a maximum of 2.5 m long and 0.5 ra wide occur within the shear. The sulphide mineralization os expo-no d by overburden wash i rig is restricted tc the- quarts veins and consists of: pyrite, chalcopyrite, galena, -sphalerite along with rare cuprite. Grab samples returned elevated values in both gold and base raetals, (Section 5.2). The highest geochemical values were obtained from Pit tt 3. I t contained the higher percentage or quartz veining, and carbonate and sericitic alteration, as well as sulphide mineralization. A quartz-feldspar porphyry was exposed at the extreme northeastern end of the shear zone. Grab samples taken from the porphyry as well as the acc-cnip.-any ing quartz veining returned lower values with respect to samples taken of cthor quartz veins further along strike.

In the same area, a number of VLF conductor trends at a similar orientation to the DK Shear Zone, (VLF Survey, G.C. Dunn, May 1991). Those conductors have yet tc be adequately explained.

The potential for this area lies in delineating other mineralized shear zones, and/or locating a larger body of quartz-feldspar porphyry that may have been the reason for the shearing and -.he source of the mineralization. This would be best accomplished by detailed prospecting, and a tight soil sampling survey, ''25 m line spacings; 5 m sample sites), in the immediate area, and in particular over the VLF conductive trends. ?b and Zn might be useful pathfinder elements because of the presence of galena and sphalerite in the quartz vein contained within the shear zone.

3.O CONCLUSIONSSignificant results from the 1992 spring exploration program are

l t through outcrop stripping and mapping of the DK Shear Zone it has a known strike length of 353 ra, and a variably width of O.S to 2. 5 is.2) five pits emplaned over the shear zone e::posed shear controlled quartz-carbonate veins with pyrite, chalcopyrite, galena and sphalerite mineralization. One grab sample returned ,0.01 oz/ton Au. 3.2 ppn Ag, and 4900 ppni Cu.3) a quartz-feldspar porphyry was exposed in two of the pits loiat^d in the northoartern er.d ~jf ~he shear.

- 8 -

9.0 RECOMMENDATIONSThe following program is recommended:

1) re-analyze all grab samples for zinc, and lead.2) test for additional mineralized shear zones on the properties using detailed prospecting and soil sampling surveys.3) explain the VLF conductors obtained during the May 1991 survey through prospecting and soil sampling surveys.

- 9 -

REFERENCES

Johns G.V. , 1986 : Geology of the Hill Lake area, District of Timiskaming; Ontario Geological Survey., Report 250, pg. 1-44.

Dunn G.C., (1991) : Soil Sampling, Claims 990956, 990957 and 1134105, Tudhope Township, Larder Lake Mining Division, Ontario, OPAP 091-019.

Dunn G.C., (1991) : VLF Survey, Claims 990956, 990957 and1134104 and 1134105, Tudhope Township, Larder Lake MiningDivision, Ontario, OPAP 091-019.

Dunn G.C., (1991) : Magnetometer Survey, Claims 990956, 990957 1134104 and 1134105, Tudhope Township. Larder Lake Mining Division, Ontario, OPAP 091-019.

APPENDIX I SUMMARY AND DISTRIBUTION OF FIELD WORK FOR 1992

APPENDIX I SUMMARY AND DISTRIBUTION OF FIELD WORK FOR 1992 For Claims L-990956 and L-990957

PERIOD FROM : May 8 To : May 11

ACTIVITY UNIT TOTAL

grid preparation mandays outcrop stripping

10

mappingreport writing

mandays mandays

23

rock(Au, Ag, Cu)

rock(Pt)

petrographic

sample

sample

sample

24

thinsect ion

APFIlfDIX II FIELD PERSOHHEL 1992

APPENDIX II : 1992 FIELD PERSONNEL

ACTIVITY PERSONNEL OCCUPATION PERIOD

Grid Preparation Gary Dunn Technologist May 9-10Outcrop Stripping Greg Dunn Laborer May 11Outcrop Stripping Jason Demester Laborer May 3-11Outcrop Stripping Ed Korba Prospector May 9-11

Mapping Greg Curry Geologist May 11-12

APPEHDIX III OUTCROP SAMPLE DESCRIPTIOHS AHD RESULTS

APPENDIX IV PETROGRAPHIC REPORT

Sample 3138

Microscopic description Because of the brecciated nature of the rock relative percentages of gangue minerals and opaques are widely varied over short intervals.

Quartz; 45 !fc, anhedral, (^05 to ^.0 nun). Coarse interlocking grains shattered by shear to form fine-grained weakly foliated layers/partings. Results in lensoids of coarser intelocking grains in a finer sheared groundmass. Strained extinction. [Shear stage l, and affected by subsequent stages] .

Sericite; 25%, anhedral (microgranular to 0.2 mm). Irregulardiffuse to compact, foliated/felted, irregular masses, and contorted, irregular lensoidal stringers/partings aligned with and cutting across major shear direction. Encloses lensoidal clusters of fine quartz grains. Intermixed fine quartz in more diffuse clusters. [Shear stage l and 2, affected by subsequent stages].

Carbonate; 2(^, anhedral (t:. 05 to 0.5 mm). Irregular clusters, diffuse discontinuous networks among quartz and sericite. Generally segregated into crackle breccia fracture and breccia cavity infillings. Associated with opaques. [Shear stage 3 ] .

Chlorite(?); 3%(?), anhedral (microgranular to 0.2 mm). Very minor weakly foliated clusters in discontinuous partings/diffuse networks. Associated with carbonate. Inconspicuous, may be sericite at thin edge of section.

Plagioclase(?) ; Suspected, but not confirmed in thin section or by etching in stained slab. Minute featureless grains intermixed with quartz in diffuse sericite clusters.

Sphene/leucoxene; < l%, anhedral (microgranular to -*:.05 nun). Irregular clusters with sericite along shear planes.

Reflected lightOpaques S'i. Show strong fracture control.

Chalcopyrite; ^ *, anhedral (-c. 01 to 0.6 mm). Irregular grains, clusters of grains. Margins have thin rims of hematite (red internal reflection), chalcocite and covellite. Associated pyrite, galena, sphalerite. Blebs in sphalerite. Strong fracture control.

Pyrite; 3%, anhedral/euhedral, (*c.01 to 0.5 mm). Disseminated grains, clusters of grains (to ^.0 mm). Generally segregated but some association with sphalerite, chalcopyrite. In fracture controlled clusters.

Sample 3138

Sphalerite; 2% / anhedral, (-c. 05 to ^.0 mm). Irregular clusters Fracture controlled. Contains chalcopyrite blebs with fairly even distribution. Associated with chalcopyrite, galena, pyrite.

Galena; ^1^, anhedral, ("C.Ol to 0.2 mm). Very irregular grains clusters of grains. Associated chalcopyrite, sphalerite. Occurs in minute hairline fractures with carbonate and possible sphene.

Covelite; traces, anhedral (-c. 01 to -c. 05 mm). Rims somechalcopyrite in concentric layers with chalcocite and hematite(?)

Hematite; -c-^^, anhedral, (-c. 01 to .05 mm), forms rims on some pyrite and chalcopyrite grains. Strong red internal reflection when powdered by needle.

Chalcocite; traces, (":.01 to .05 mm) as for covellite, concentric rims on chalcopyrite. Lacks red internal reflection of hematite when powdered by needle.

Tellurides; anticipated but not detected. Assays? Trace element analyses?

Suggested paragenesis of opaques.

Pyrite ^——————

Sphalerite —^^—^-———

Chalcopyrite -—^—^——--^--

Galena ——^———^-——

Chalcocite ——^———^—

Covellite ________

Hematite ________

Multistage quartz (sericite, carbonate) mineralized breccia

Summary descriptionProtolith is obliterated. Breccia composed largely of quartz, lesser sericite and still less carbonate. These major constituents are segregated suggesting introduction during separate stages of shearing/brecciation. Quartz groundmass is cut by granulated shear planes and contains irregular masses, screens, contorted partings of sericite and intermixed sericite/lesser quartz. These follow the granulated quartz shear foliation but also cross it at varied angles. Superimposed on this are crackles, crossing previous shears and breccia voids of subsequent brecciation infilled by carbonate and associated sulphides.

Sulphides are fracture breccia void controlled and have erratic distribution and abundance. Sphalerite predominates, followed by pyrite, lesser chalcopyrite with very minor associated secondary rims of covellite, chalcocite and hematite.

Because the sample is from the Kirkland Lake area tellurides and gold were anticipated but none were identified in either of the polished thin sections.

3138 92 R XXI-OA Polarized light O . l mm

Early stage sheared quartz-rich groundmass, diffuse very fine quartz-sericite screen lower right. Late carbonate-filled crackle breccia. Large dark grains are quartz in extinction.

3138 92 R XXI-3A Polarized light O. l mm

Compact felted sericite mass following and crossing foliation in quartz. Carbonate in subsequent fractures lower right.

3138 92 R XXI-8A Polarized light O. l nun

Strong shear foliation in quartz [upper left to lower right]. Sericite filled cross fracture [shear]. Clusters of sphene(?) granules centre left. Black areas are epoxy-filled holes.

3138 92 R XXI-9A Polarized light O . l mm

Foliation in coarse quartz cut at a high angle by sericite and "granulated" quartz-filled shear planes.

3138 92 R XXI-4A Reflected light O . l nun

Pyrite [Pyr] centre and upper left. Chalcopyrite [Cpy] bright yellow. Galena [G] smaller grains light grey slight bluish tint associated with pyrite, chalcopyrite and in hair line fractures.

3138 92 R XXI-5A Reflected light 0. l nun

Sphalerite with chalcopyrite clusters of minute pinpoint grains and larger blebs and one grain of galena. Additional galena with pyrite top left and in hairline fracture lower right.

3138 92 R XXI-6A Reflected light O . l nun

Pyrite, cream; chalcopyrite, yellow; sphalerite, purplish grey; galena, white; covellite, blue.

APPEMDIX V STATEMEHT OF QUALIFICATIOHS

APPENDIX V: Statement Of Qualifications

With reference to ray Geological Report on the Tudhope Township Property, claims L-990956 and L-990957, dated September 15, 1992...

I, Gregory L. Curry, do hereby certify that:

1) This report is written for Gary Clayton Dunn, P.O. Box 995, La Ronge, Saskatchewan, SOJ 1LO, in whose names the claims mentioned in this report are recorded under.

2) I graduated from the University of Waterloo in 1981 with a BSc., and have worked in the field of exploration for the past 11 years.

3) I have no interest direct or indirect in the claiios mentioned in this report, nor do I expect to in the future.

4) This report is based upon; study of pertinent geological information on the Tudhope Township, my two days on the claims May 11 and 12, conversations with the claim owner Gary Dunn.

5) My permanent address is P.O. Box 467, La Range, Saskatchewan, SOJ 1LO. (306) 425-3915.

Dated this 15th day of September, 1992 La Ronge, Saskatchewan.

cvlCM

*

Q.

H

UJ

TRUAX TWP M.251

geology reference-COBALTRISIDHNT GFO.

MR (IV "''MR

M M O jl) M R O

' i \ riVb70H

Iiai788

CVJ 00 CVJ

Q.?h-

O

o: OD

47"40

432 "THIS MAP SHOWS THE APPROXIMATE LOCATION

RARRFR TWP M 9HP OF THE BOUNDARIES OF bAKbtK l WH M. ^Ub THE AREA WHICH IS THE

SUBJECT OF CURRENT WON. THE EXACT

NOTES

400 surface rights rebeivntion along the shores of alllakes and rivers

VV ofTownship closed to stoking efftcfivt May 8,1978, Sec 38(f) of The Mining Act.

SurUct *nd Nuini Riohtf on all Crow Linden thtt towthip Ulthdrtwn trot prospecting, (tiding out, ul* or l tut Section 36 R.6.0. I960, Tht Hinin| Act. Order MN 44 l M ttftctivt Octobtr 21, 1982 it 1:42 pi.

1*1 Part of ordir NM 14/82 RE-OPEffl by ortftrO-HLOt-90 NEK tfftctivi April 3, IMO it 7iOO AN E.I.T.

(R?) Surfici md Mnim Rl|kt* Mithirwn f rot lUkiiO Ncti^ ft ^ of thi Mining Act i.8.0. IMO, Or4w y-L2*W NO tfficiivi

on April 1,1910 it 7i01 E.B.T.-f

LEGEND

HATENTfDLAND

PAI EN l ED FOH SURFACE RIGHTS ONLY

11ASE

l ICLNSE OF OCCUPATION

CROWN LAND SALES

CANCLLLCD

MINING RIGHTS ONLY

J.URFACE mOHTS ONLY

HIGHWAY i ROUTE NO.

ROADSTRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES -" used only wild bummor resort locations or when spaca l* fimlUd

TOWNSHIP OF

TUDHOPEDISTRICT OF

TIMISKAMING

LARDER LAKE,MINING DIVISION

SCALE : 1 INCH 40 CHAINS (1/2 MILE)on JBKDATE PLAN NO. M

i')N l \KK)

MINI5TRV OF NATURAL RESOURCESBRANCH/

THE INFORMATION APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON- SUIT WITH THE MtNING RECORDER, MINISTRY OP NORTHERN DIUELOP- MENT AND MINES. FOR AD, DITIONAL INFORMATION ON THE STATUS OF THi LANDS SHOWN HEREON

\"- ^ ' C *

t* f i *a

ILL bt SHOWN FOLLOWING CONFIRMATION BY THE PARTfcS TO THE ACTION.0

200TRIM LINE

l

2**' *)

41POBNE0118 OP02-66 TUDHOPE

rf IT*

5"

.- M

104 00 S

220

PIT 3

trace-2%

O/B

(N

PIT 4

Scale l IOO

PIT 2

55

6/B 85

trace ^w;-^^B5 -•^^

^•7a,d.e Se2d,e

2b,c Bl

Scale l IOO

PIT l

Contact Zone ,d,e rodded

O/B

\ 2d,e /\

^ j^'85 7 2o \ l

O/B

Scale l 100

PIT \Cpy, Py.Go,

, Se , Fu

POND

PLJ3 Cpy, Py, Se, Ga,Sph

0

p

TRUE NORTH

O/B

,* 2oY'^

*2d,e

80*^.-'2d,e-f Se

trace Cpy, Py

Scale l IOO

PIT 5

O/B

trace Cpy.Py

2d,e Se

\2a

Scale l IOO

LOCATION MAPSCALE 1 50,000

1'

1

,

\

^ ,\

IU4I06 li 34105

\ \ ——————

9 M 34I04

o 1

t 1134103

1 \

\\ o

— — - i— * S,\

LOT S

l

LOT i

i

LU0. 0Xooh-/^-~

fa

_ 0

L-990sbT U-99095JI

o*

LJO,y.

CD (4

^ ,^0~'n^ f^^

cone m

\

LOT 1X CONC n

1

LEGEND

8 INTERMEDIATE VOLCANICS (Belonging to Skead Group) 2 a Ash Tuff 2b Lapilli Tuff 2c Pyroclastic Breccia 2d Sheared 20 Carbonated

7 METAMORPHOSED FELSIC TO INTERMEDIATE INTRUSIVE

7a Quartz - Feldspar Porphyry

7b Feldspar Porphyry 7d Sheared 7e Carbonated

ALTERATION

B l Bleached

Fu Fuchsite

Se Sericite

MINERALIZATION

Cpy Chalcopyrite Py Pyrite

Sphalerite Galena

Sph GaCu Cuprite

SYMBOLS

O/ B Overburden••^ "* Quartz -Carbonate Vein/ Stringer

— - — - Geological Contact85

Shear with dip

bbFoliotion with dip Lineation with plunge Outcrop OutlineDK Shear

Uni ''Dm 100 m 150m 200m

GEOLOGICAL MAP of

DK SHEAR ZONE GRIDand

DETAILED GEOLOGY of PITS

CLAIMS L-990956 and L-990957

TUDHOPE TOWNSHIP LARDER LAKE MINING DISTRICT

Scale h 2500

Work by G. CurryDrown by K. Frew

Dote . Sept 1992

Figure 3

I

-t l

T

\

41P09NB0118 OP92-56 TUDHOPE 240

44

A/I

10+00

frs**rf11*1