RPT DESCRIBING REC PROSPECTING GEOL & IP SUR SAULT PROJ

REPORT DESCRIBING RECONNAISSANCE PROSPECTING. GEOLOGICAL AND INDUCED POLARIZATION SURVEYING.

SAULT PROJECT. SAULT STE. MARIE. ONTARIO

4IN08SE0020 2.143*8 RUNNALLS

010

Robert I. ValliantTri Origin Exploration Ltd.August 7, 1991

2 .l 4308

CERTIFICATE OF QUALIFICATIONS

As author of this report on the Sault Property of Tri Origin Exploration Ltd., I hereby make the following statements:

1. l an an Officer and Director of Tri Origin Exploration Ltd. My office address is 78 Asquith Ave., Toronto, Ontario.

2. I have received the following degrees in Geological Sciences;

B.A. Se. 1977 University of Waterloo, Waterloo, Ontario

Ph.D. 1981 University of Western Ontario, London,Ontario

3. I am. a fellow of the Geological Association of Canada and a member of the Society of Economic Geologists. I am a member of the Prospectors and Developers Association of Canada, the Canadian Institute of Mining and Metallurgy and theGeological Society of America.

4. I have been practicing as a professional geologist for overten years.

5. I jcnducted geological mapping and prospecting on the property and supervised all work contained within this report. I have reviewed all assessment files held by the Ontario Geological Survey pertaining to this property.

Dated at Toronto, Ontario November 17, 1991

Robert I. Valliant.

41NBBSEeaae 2.14308 RUNNALLS O1OC

Sault Project

Sault Ste. Marie, Ontario

Report Describing Reconnaissance Prospecting, Geological and Induced Polarization Surveying, Sault

Project Sault Ste. Marie, Ontario

Introduction. . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . . , . . . . . . . . . lProperty Location and Description......................!

-7

Part A: Property Reconnaissance and GeologyIntreduction. . . . . .... .. . .. . . . . . . . .. . . . . . . . . . . . . . . . . . . . . 2Results.. ... ....... . . . . . .... . . . . . . . . . . . . . . . . . . . . . . . . . . .2Geological Mapping.. . . . . . . . . . . . .. .. . . . . . . . . . . . . . . . . . . . . 5

Part E: Geophysical SurveyingIntr oduction. . . . . . . . . . . . ...... .. . . . .. . ......... . . . .....5Survey Method. . . . . . . . . .. . . . . . . .... . . . . . . . . . . . . . . . . . . . . . 6Results. . . . . . .. . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . 6Recommendations........................................7

Part C: ExpendituresExpenditures. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

ficate of Quaiifications. . . . . . . . . . . . . . . . . . . . . . . . . . 9Bibliography C e r

Appendix 1; Rock Sample Descriptions............attachedAppendix 2 ; R eport of Geological Mapping and

Geophysical Survey, June, July 1990D.A.Meyer and M.J.Perkins.....,.....attached

Appendix 3; Technical and Logistical Report for the Induced Polarization Survey, Doyle Lake, Batchawana, Ont.........attached

Location Map... . .. . . . . . . . . . . . . . . ........attachedClaim Location Map......................attachedReconnaissance Map, 1:5,000, Nl/2.......attachedReconnaissance Map, 1:5,000, Sl/2.......attachedGeology Map, West Grid, l:2,500.........attached

rig Fig Fig .

rigFig

Gee logy Map, Doyle Lake Grid, l:2,500...attached I.P. Map, West Grid, l:2,500............attachedI.E. Map, Doyle Lake Grid, l:2,500......attached

Sault Project

Sault Ste. Marie, Ontario

Report Describing Reconnaissance Prospecting, Geological and Induced Polarization Surveying, Sault Project, Sault Ste. Marie, Ontario

Introduction

This report describes work completed on the Sault property during the period April 31, 1990 to January 11, 1991 except for diamond drilling which is described in a seperate report dated January 14, 1991. The report is divided into three parts: Part A -Property reconnaissance prospecting and geology; Part B

Geophysical surveying and Part C - Expenditures. Illustrations include two property location maps, 1:5,000 plan maps of property reconnaissance geology, 1:2,500 plan maps of West grid geology and I.P. anomalies and 1:2,500 plan maps of Doyle Lake grid geology and I.P. anomalies.

Property Location and Description

The Sault property is located 90 km north of Sault Ste. Marie, Ontario in the east half of Runnalls Township (fig. 1) and falls under the jurisdiction of M.N.R. administrative district of Wawa in the Sault Ste. Marie mining division. The property is joined to the Trans Canada Highway by 60 km of logging road which provides truck and A.T.V. access otherwise the property is most easily reached by float plane to Doyle lake.

The Sault property consists of 100 unpatented mining claims registered in the name of Tri Origin Exploration Ltd.(fig.2). No option agreements or contractual obligations apply to this property. The following is a list of claims which comprise the property:

SSM 1136231 SSM 1136251 SSM 1136271SSM 1136232 SSM 1136252 SSM 1136272SSM 1136233 SSM 1136253 SSM 1136273SSM 1136234 SSM 1136254 SSM 1136274SSM 1136235 SSM 1136255 SSM 1136275SSM 1136236 SSM 1136256 SSM 1136276SSM 1136237 SSM 1136257 SSM 1136277SSM 1136238 SSM 1136258 SSM 1136278SSM 1136239 SSM 1136259 SSM 1136279SSM 1136240 SSM 1136260 SSM 1136280SSM 1136241 SSM 1136261 SSM 1136281

SSM 1136291 SSM 1136292 SSM 1136293 SSM 1136294 SSM 1136295 SSM 1136296 SSM 1136297 SSM 1136298 SSM 1136299 SSM 1136300 SSM 1136301

SSM 1136311SSM 1136312SSM 1136313SSM 1136314SSM 111714SSM 111715SSM 111716SSM 111717SSM 111718SSM 111719SSM 111720

SSM 1136242 SSM 1136243 SSM 1136244

SSM 1136245 SSM 1136246 SSM 1136247 SSM 1136248 SSM 1136249 SSM 1136250

SSM 1136262 SSM 1136263 SSM 1136264


SSM 1136282 SSM 1136283 SSM 1136284


SSM 1136302 SSM 1136303 SSM 1136304


SSM 111721 SSM 111722 SSM 111723


Line Cutting

Linecutting was conducted on the property during May and June 1990 by Service Exploration of Rouyn-Noranda, Quebec. Baseline for the West grid (fig. 3) was oriented at 335 degrees parallel to strike of underlying rock units with crosslines oriented at 65 degrees at 100 metre separations and were chained and picketed at 25 metre stations. The West grid was cut to replicate as closely as was possible the previous grid 7 cut by Granges during 1986. Line 13N was extended eastward to intersect a logging road at 28+SOm east. A second grid, the Doyle Lake grid (fig. 4) was cut at the same orientation and line spacing as the West grid with its baseline originating at L13N, 20+OOE.

Part A: Property Reconnaissance Prospecting and Geology

Introduction

Reconnaissance traversing and prospecting was conducted on the Sault property by D. Sheehan and R. Valliant from time to time during the spring, summer and fall of 1990 for a total of 25 man- days. Additionally, reconnaissance mapping was conducted by D. Meyers and M. Perkins during June and July, 1990. This work was carried out to determine the nature of the geological environment which is host to gold and base metal mineralization and to assess the nature and style of this mineralization. Diamond drill core from previous exploration programs (Harder, 1986) was relogged and where necessary sampled to further verify results from previous work and further delineate controls on mineralization.

Results

Reconnaissance traversing and prospecting at the Sault property resulted in gaining an understanding of the general geology of the property, providing a preliminary assessment of known sulphide occurrences, obtaining preliminary geochemical data and preparation of a base map outlining general geology, claim locations, grid locations and general geographical features (figs. S&4).

The majority of past exploration work on the property has been

conducted by five companies; Algoma Central Railway, 1962, Rio Tinto Canadian Exploration Ltd., 1964, Canex Aerial Expl. Ltd. 1966, Geophysical Engineering Ltd. 1975, and Granges Exploration Ltd. during the early 1980's. Algoma Central Railway flew an airborne geophysical survey and trenched sulphide-rich rocks east of Doyle Lake. Rio Tinto followed up on Algoma's work conducting limited ground geophysical and geological surveys which resulted in trenching of a number of sulphide occurrences. Three of the most significant of these trenches contained 0.01 ounces per ton gold and 0.02 percent copper across 13.7m, 0.02 ounces of gold per ton across 4.0 m and 0.3 percent copper across 7.6m. Canex Aerial drilled one diamond drill hole in a sulphide occurrence and Geophysical Engineering drilled two diamond drill holes in sulphide occurrences each reporting low metal contents. Granges conducted followup ground geophysics and geological mapping on a number of conductors located during an airborne magnetic and E.M. survey for Dryden Resources Inc. flown during 1980. Nine diamond drill holes were completed by Granges within the present Tri Origin property, five of which attempted to trace a newly discovered zone of auriferous, disseminated and massive sulphide for a strike length of 150m. Gold content of up to 5.5 grams gold per tonne across 0.8m was reported during this program. Field examination and re- interpretation of assessment data and drill core from earlier programs has resulted in recognition of a large number of untested gold and base-metal targets within the property.

Bedrock is well exposed especially along ridge tops and scarps extending northward from the Batchawana River. At the bases of the scarps and in topographic lows rock exposure is limited. In general overburden is sand-rich with a well developed humus layer and varies in thickness from nil to a few metres where drill hole data is available. Average overburden thickness is estimated to be 2 metres on high ground however may be much thicker in topographic lows near scarp faces.

The property is underlain by metavolcanic, metasedimentary and metamorphosed felsic intrusive rocks at the north-eastern part of the Batchawana greenstone belt. Property geology consists of alternating north-striking, steeply east dipping felsic volcanic, volcaniclastic and sedimentary rocks which contain at least three extensive disseminated and massive sulphide-bearing units. These rocks are intruded by an elongate, north-trending felsic stock and northwest-trending diabase dykes and all rocks are complicated by major northeast-trending structures which may have had influence on location of sulphide occurences.

Mafic volcanic rocks occur in the northeast corner of Runnalls Township and form the stratigraphic base to the volcanic sequence exposed on the Tri Origin Property. These rocks consist primarily of hornblende and plagioclase-rich tuffs and flows which have a tholeiitic basalt composition (Grunsky, 1981), Fine grained, schistose mafic tuff comprising units up to 15m thick intercolated with felsic tuff are restricted in occurrence to the northeast part of the property. These mafic tuffs strike 320 degrees, dip steeply

east and in places contain minor amounts of iron carbonate.

Felsic volcanic and volcaniclastic rocks underly the majority of the property. The volcanic rocks vary in fragment size from coarse lapilli to fine ash which is interbedded with quartz and/or feldspar crystal-rich units and in texture from schistose to massive and thickly bedded or to well-bedded on a centimeter scale. Composition of these rocks varies from dacite to rhyolite (Grunsky, 1981). Fine grained rhyolite which appears to be flow banded occurs at the southeastern part of the property near Granges grid 8. Coarse lapilli tuff is exposed east of Doyle lake and forms a unit which can be traced northwestward to the property boundary. This rock contains rhyolite fragments up to 12cm in length in a fine grained intermediate matrix which in places is host to garnet porphyroblasts. Northeast of Doyle Lake the lapilli are within a matrix of semi-massive to massive pyrite which in part comprises an airborne E.M. anomaly drilled at its northern extent by a single hole in 1975. Lapilli up to 1.5 cm in length have also been observed forming units along the west and east margins of the Doyle Lake grid, southeast of the Doyle Lake grid and at the central and east parts of the West Grid. Fine grained felsic tuff is in general, quarz and sericite-rich. In places, hornblende and\or biotite is abundant in compositionally controlled layers and minor amounts of epidote, carbonate and chlorite occur locally. Thickly bedded felsic tuff commonly contains quartz and\or feldspar crystal-rich layers from a few tens of centimeters to 4 meters thick. Thinly bedded felsic tuff is sericitic and weakly foliated parallel to layering. In places, truncated layering indicates a west facing direction for the tuffs however at the central and western parts of the Doyle Lake grid and eastern part of the West grid layering which is contourted and folded over the scale of a few meters indicates that structural repitition of rock units may occur through the central part of the property. Pink to red garnet is a minor constituent of these rocks especially in the vicinity of pyrite occurrences. Sillimanite and either andalusite or cordierite have been tentatively identified in tuff southeast of Doyle Lake and west of Cloudy Lake.

Volcaniclastic sedimentary rocks are fine grained, white weathering and similar in composition to felsic tuff. These rocks are well layered and lack quartz and\or feldspar crystals relative to felsic tuff. As an aid to stratigraphic interpretation these rocks have been corealated as units intercolated with tuff on the West and Doyle lake grids however in many places they are indistinquishabl e from fine grained felsic tuff.

Sedimentary rock becomes increasingly abundant underlying the west part of the property as units 100 to 200 metres thick intercolated with tuff. The west property boundary marks the transition from predominately felsic volcanic rock to a thick sequence of greywacke which underlies the central portion of the greenstone belt. Greywacke i s well described by Grunsky (1981) and in the vicinity of the property grading and scour marks indicate a west facing direction. Sedimentary rock underlying the property is a

transitional type which can be distinguished from tuff and greywacke. The rock is fine grained, layered on a scale of l to a few lO's of cm and does not exhibit well preserved sedimentary textures or Bouma cycle layering as is common in greywacke. The rock is grey weathering and exibits a purpulish hue on fresh surface due to very fine grained, disseminated biotite. A few percent of pyrite occurs within sedimentary rock as a stratigraphic unit of at least a kilometre in strike length at the southwest edge of the property and narrow layers of chert which may contain pyrrhotite, chlorite or pyrite is common at the east part of the West grid and within sedimentary units near Doyle Lake.

The Grey Owl Lake stock intrudes sedimentary and felsic volcanic rock at the west central part of the property. This stock is a light pink, microcline porphyritic quartz monzonite (Grunsky, 1981). A white to pink weathering quartz monzonite intrusion underlies the central portion of the property south of Doyle Lake.

Rocks at the south part of the property strike 330 degrees and dip between 50 and 85 degrees east and gradually change to a 300 degree strike at the north part of the property. A weak foliation parallels layering and produces a quartz sericite schist near sulphide-rich rocks on the West grid. Major faults at an azimuth of 30 degrees crosscut all rocks underlying the property. The most prominent of these faults is an extension of the Batchawana River and all rocks in its vicinity have been deformed and rotated approaching parallelism with the fault. Granges drill holes 14 and 15 testing a strong airborne anomaly at the southeast part of the property are within a similar fault zone and are drilled along strike of rock units. Hence, this airborne anomaly remains untested.

A total of 130 rock samples were collected from outcrop throughout the property (samples MI-61 and Dl-69, appendix 1). The majority of these samples were analysed for Au, Ag, Cu, Pb and Zn and a part of each was retained to form a representative sample suite for the property. The only significant Au analysis was from a pyritic rock near the south part of the West grid which returned a value of 250 ppb.

Geological Mapping

Geological mapping was completed on both the West and Doyle Lake grids by D. Meyers of Kingston, Ontario and M. Perkins of Toronto, Ontario during June and July, 1990. Results of this work are described in a seperate report (appendix 2) and plotted on 1:2,500 scale geological plan maps (figs. S&6).

Part B: Geophysical Surveying

Introduction

Induced Polarization surveying was conducted during July, 1990 by

Mertens S MacNeil Geophysical Ground Surveys Ltd., of Guelph, Ontario (appendix 3). Field crew consisted of:

R. Mertens - Guelph, OntarioJ. MacNeil - Sydney, Nova ScotiaK. MacKenzie- Sydney, Nova ScotiaB, Campbell - Frenchvale, Nova ScotiaD. Gouthro - Frenchvale, Nova Scotia

Survey Method

A total of 25.66 line kilometres of dipole-dipole array I.P. surveying was completed using a Phoenix phase system. Transmitter was a Phoenix IPT1 operating at a frequency of l hertz with a 2.5 kva power generator, the receiver a Phoenix lPV4-Turbo. Dipole or a-spacing for both transmitter and receiver electrodes was 25 metres with readings taken at n value separation multiples of the a-spacing of l, 2, 3 and 4. Resistivity was expressed in ohm- metres and phase values expressed in milli-radians. A "metal- factor" was calculated for each data point using the formula MFs (Phase divided by resistivity) x 100. Psuedosections were plotted for each line surveyed at a scale of 1:2500 and anomalies were transferred to grid plan maps (figs, 7S8).

Results

I.P. anomalies were determined primarily based on their phase response and are illustrated on attached IP plan maps. Resistivities were used to aid in stratigraphic correlations and aid in interpretation of continuity of phase anomalies.

A number of I. P. anomalies were detected during the survey, the majority of which appear to be stratigraphically controlled and can be correlated for at' least three lines along strike. Seven of these anomalies stand out due to the magnitude of their phase response and their continuity:

West GridAnomaly W-l- L.7+OOS to L.14+OON, approximately 4+OOE

- continuous along strike varying between weak and strong phase with moderate to low resistivity.

Anomaly W-2- L.9+OON to L.17+OON, approximately 7+OOE- continuous along strike with strong phase

at its center grading north and south to weak phase response, low to moderate resistivity.

Anomaly W-3- L.0+00 to L.8+OON, approximately 2+OOE- continuous along strike with weak phase response

and moderate to high resistivity.

Anomaly W-4- L.0+00 to L.3+OON, approximately 7+50E- discontinuous along strike, weak phase and

moderate resistivity.

Doyle Lake GridAnomaly D-l- L.13+OON to L.20+OON, approximately 22+OOE

- continuous along strike, strong phase and low resistivity at its centre grading to weaker phase and moderate resistivity to the north and south.

Anomaly D-2- L.15+QON to L.18+OON, approximately 23+OOE- continuous along strike, weak phase and moderate

to high resistivity.

Anomaly D-3- L.13+OON to L.17+OON, approximately 24+50E- continuous along strike, moderate phase and

resistivity grading to a weaker response to the north, survey ended in anomaly L14 to L17N.

Variation in response and slight offsets in anomaly W-l along strike as well as distribution of other I.P. anomalies on the west grid aids in the interpretation that structural discontinuities most likely faults oriented at 30 degrees may crosscut the property. A major fault at the south part of the west grid has either inhibited transmitter current from reaching bedrock or has significantly rotated the orientation of rock units and therefore data from this area is suspect.

Recommendations

1. Diamond drilling, initially of the four main anomalies along their strike length is recommended to determine nature and metal content of these anomalies. To date, only parts of anomaly l have been drill tested and, where intersected, it is known to contain gold and base metal-bearing massive and disseminated sulphide.

2. Trenching of I.P. anomalies is recommended where overburden thickness permits.

Part D: Expenditures

[email protected]......... . . . . . . . . . . .S 7,027.00

GeologyProspecting,(DGS/RV)................... ... S 7 ,500.00Mapping,(Meyers/Perkins)..................S18,123.00

Geophysics25.66 km.Q SlSSS.OO/km. ...................S37,783.00

Report and Map PreparationGervais . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . S 2 ,861 . 00Valliant. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .S 2,700.00

Food and LodgingBatchawana Air Service. . . . . . . . . . . . . . . . . . . . 010 , 415 .00

Total Expenses. . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . .. .S86,409.00

Bibliography

Grunsky, E.G. 1981, Geology of the Grey Owl Lake Area, District of Algoma, O.G.S. Report 205, 76p.

Smith, P. 1984, Report on Dighem III survey Airborne E.M.,Resistivity, Magnetic and V.L.F. Surveys, Batchawana AreaOntario for Manwa Exploration Services Ltd.

Lien H.O. 1964, A.C.R. Project (1963) Ground Geological Survey,submitted as assessment credit on conductors L-l, E-3 and E-6, Twp-25, Range XV, Ontario for Rio Tinto Canadian Exploration in O.G.S. Assessment Files, Toronto.

Harder, G. and Prew, M. 1986, Geophysical (Ground E.M.) Report on 71 claims (10 groups) situated in Runnalls Township, Sault Ste. Marie Mining District, Ontario for Granges Exploration Ltd. in O.G.S. Assessment files, Toronto.

Granges Exploration Ltd. 1986, Work done by Granges Exploration Ltd. on the Runnalls Claim Group situated in Runnalls Township, Sault Ste. Marie Mining District, Ontario in O.G.S. Assessment Files, Toronto.

Siegel, H.O. and Lien, H.O. 1963, Report on ground Geophysical and Geological surveys on A.C.R. option Twp. 25, Range XV, Ontario for Rio Tinto Canadian Exploration Ltd. in O.G.S. Assessment files, Toronto.

i antloration Ltd.

91.

Doyle Lake PropertyRunnalls Twp.Tri Origin Resources Ltd.

Date ROCK SAMPLE DESCRIPTIONSShipped Date

Saiple To Assays Grid Location Saiple Description Nutbtr Swastika Received Easting Northing

Assay Au Ag Cu Zn Pb

HI

- H3

M7

, vX M2

y ilO

\j M 12J M 13

H14

HIS

M16

(117

H18 L/M5

-Di

v D2 J D4

J D5

REPRESENTATIVE SAMPLES

5U bay Doyle L. repeast shore

Sy bay Doyle L. repwest shore

SH bay Doyle L. repnorth end

Central Doyle L. rep

S of trappers rep cabin

295 1700 rep

740 1520 rep

July 7/90 S bay Doyle East shore

294

295685730

355

140

415

700

700

Lake

1715

170015051120

910

485

500

510

514

Rep

400 1625N

400 1625N 335 1025N

654 9SON

Contorted, f. gr., reworked felsic tuff1 arkose Reworked felsic volcanics

Quartz lonzonit*

Reworked felsic vole. /ark in region of diabase Felsic TufftOSS class.)

Milky QV w ^Z specularite (MS sent for assay) Arkose, f. gr., black weathering buff brown White.grey totled BV No apparent sulfs

generally poor beddingMilky-white fit: Bouldw. SpeculariteMilky White QVSial l white QVMottled grey/white sial lQV.Arkose w IZPy diss,euhedral, On.Ptygiatic QV, MinoroxideArkose w IZdiss Pyf. gr., anhedralMilky white QV, largeParallel to creekAppears barrenAs per M17Minor QV froi Sedge Doyle L.9V lOi wide trend 130 shtrd.red, purple hei. stainsRusty band in QVArkose/Wacke at contactwith GraniteBanded Arkose/Vacke (Gneise)Lt. and Dk. bands. Hard.

Srey fresh surface D6 Rep 705 1003N Rep of Hetaseds.Thin banded,H

Hard, Buff colored J D7 " 697 795N Rep of Diabase

^DS ' 790 395N Very fngr KSpar rich Arkose.Thin Banded,

1/09 ' 785 395N Fngr. Kspar rich. Interbnd w ore lafic bands

u D10 " 772 395N Fngr.Buff F/S Plag, Husc.Lai..Ep, Elong.Bio frags

l'Dll ' 760 400N Buff H/S. Grey F/S FngrHed Hard. Epidote

" D12 " 757 400N Buff H/S. Grey F/S FngrFspar XL's?6rains

i' D13 " 747 400N Highly contortedSrvk bands v blocks of Ark

-D14 ' 740 400N Diabase/Diorite 1 D15 f 726 455N Quartzite ' D16 ' Highly fractured 3bd? 'D17 ' 735 425N Highly fractured Diorite?

in Creek (shear zone?)i- D18 ' 715 400N Dirty Ark w Qtz Str.Tr.Py ./D19 ' 645 400N Dirty Arkose. Tr. Py.-020 Rep 625 400N Srvk Fngr Dk Grey F/S 'D21 ' 611 400N 3ba Grwk,ark. Sugary w loc 'D22-D24 Not Taken bands of iedgr.(Fsp XL's ^-025 July 7/90 20 i E of 1-1136263. Felsic Vclc. rlgr.Fsp.Xl's ^026 ' 20 i E of 1-1136264. Sheared ark. Sugary

Mafic bandsUtretched lapilli) UD27 ' near 1-1136264 Fngr sed.Muse.,Qtz.li fn py

U D28 ' 20i E and 20i S of 1-1136264 Froi Trencheh(Float)Black fn la* lIpy

^ 029 ' near 1-1136264 Black vfngr lai sed ilpy-; D30E2 ' 560 025S QV laterial beside Trench ' D30A ' 5600255 Sericitized wall rock,3ab t/DSl ' 570 028S Sheared 3ab J D31A " 570 028S Sheared, Sericitized Sab

at edge of trench1/D32 ' 625 100N V/D33 Rep 560 100N D34 ' 490 l ION Ser Sch. Sab D35 July 7/90 450 OON Float? Rusty Laiinated. 3bd

J D36 Hest Rep 665 005S Diabase? Grwk? Fngr.Peg Dyke/Qv plastered against

J D37 July 7/90 360 DOON Fngr. Sugary rock. 3bdRusty. 1-2X py stringers

''D3S Rep 715 400S Sheared, fractured Sab vD39 July 7/90 415 400S Fine lai. Fngr Arkose

sugary texture, rusty stain vD4C ' 326 400S sulf. band.Fngr,sugary.Sbd

1-21 diss Py

' 326 400S Float? Bio Sch? Qv?1-21 Py

' 326 400S Fsp XL tuff? Hedgr30Z Fsp XL's. Sheared, frac

V/D43-D49 Not taken

^D50 July 7/90 6rang*s grid 16 Highly contort 2bJDSI - QV

D52 ' ' Qv and wall rock V D53 wD54 ' ' Sulp zone parallel to

Qv 80-85deg, 5-101 Py in kafic-int. rock

^055 ' Qv VD56 ' Quartzite, A:6.5, f.gr.,

1 crystalline bands bio and qtz " D60 ' 2185 1417N Sheared fsp xl tuff,

rusty westering-,51 Py^ D61 " as per D60, f.gr. ash tuff,

use seh., exhalitive appear 10Z py stringers

1/062 ' 2087 1610N flusc sen., footwall to chertband/Qv.

w' D63 ' 350 600S Trench/road over sulp showingf.gr, ash tuff/grvk, li py diss

^D64 ' as above,2-31 Py dissand stringers

''D65 JUly 7/90 " Cx fsp tuff ' D66 ' ' 2b qtz veined and rusty- D67 ' Float?, Qv in tuff ^D68 * 700 775S Sulp stained rock, 3d,2b

on side of cliff, 70deg v D6S Rep Large Garnets in 3a

^ *I19 July 7/90 Road, east edge White, bullish 6v, tr. pyprop. 146az.

JM20 ' Road, turn off Very oxidized unit, cruibly5 cloudy L at Db contact

' y side Cloudy L. Rep of wacke ' 740 300N White Qv, no sulph.

gen confort w. 3bi/ H23 ' 390 425N 3b, arkose w 1Z py

IM euhedral gr.*N24 ' 475 215N Hi Iky Qv., 25i 1.

0.5i w., 1Z py in coneof an-euh octagonal ex.

1/1 M25 ' as per H24 ^H26 " 750 200N White, bullish Qv, 46/72S

w. inclu 3b ^ H27 * El grid Felsic tuff w diss

py .52 along beddingj H28 ' H27tlOOiW Int tuff w 5u garnets J "29 ' El grid, Doyle L. Int tuff tr diss py

N32

1/H33

JL/N34

I/K35

4)36 j K37

^ M38

^ H39

J R40

H41

J M42

H43

' H44

1 H45 1/H46 I/H47

vW48

y H49

'H50

" K51 vH52 4 H53

O H54

M M55

^ H5&

o H57

' El grid east of rdSer Se h w blebs of pyand creek gen 5n thick by 3ci 1.

' 81 W of above Int tuff y 1-2Z py ' 623 100N Mottled grey white Bv,

K-cutting 4b, .25i v ' BOO 110S Grey Bv in 5b, Ut,

near sed contact ' 350 295S 3b w diss py upto

2! in chert/si Itstone' 325 2905 Exhalative interbeds

in 3b, 180/50E .25-. 5 i thick

' as per R35 ' Road, on bridge Mafic interbeds in int tuff upto

nearest east bound lit thickness ' Road, central Int tuff, well fol

prop locally upto 21 pyv narrow Qtz stringers

" Road E of central 6rey Qv w oxide stain, creek in int tuff, K-cutting

uptp lOci thick ' Road U of Whit* Qv in 3a, li nor

Cloudy L staining, predefori " " Grey Qv, irreg isrgins

upto 2x3i. ' Near CP 1-1112718 Boulder w sulphides

above several in area Rep Road at turnoff Granite

to c aip July 7/90 Road, E of creek Btz-ser-sch

flowing into Cloudy L.' 25i E of above Fel-int flow, aphanitic ' 1930 1475N 2b ash tuff, tr py rep 2058 1515N Qtz-feld iusc ser

int-fel tuff July 7/90 2125 1535N White Qv, lOci, confon

no sulp ' 2200 1540N Int-fel vole

ser sch w linor qtz veining ' 2315 1505N Exhalative?,qtz-bio upto 51 py,

v f gr.rep as per H50 July 7/90 2270 1700N as per H50 unit * Int vol, f. gr,, an-eu

ex Py, 21 on bed planes' 2523 1295N 2a,b, IXPy on bedding planes

occn. concentrations upto 20! eu Py

' 2195 1320N Grey lOci bullish Qv,sub concord, linor feld

' 2190 1300N Mottled Qv, .Si thickgrey sulphide, non lag, as per H55

Rep as per M56 July 7/90 2120 1290N Qtz-ser-schist w garnets

-"f!5S rep 1615 1300N 3a,2a, reworked vole tuff ^(teO July 7/90 345 700S 3d, l Z diss Py

along bedding, boulder?"H&t ' as per H&O, upto 51 Py

very f.gr., exhalative boulder? if so not loved far

TRI-ORIGIN EXPLORATION LTD.SAULT PROJECT

DOYLE LAKE, RUNNALLS TWP., ONTARIO

Report of Geological Mapping and Geophysical Survey

Completed June, July 1990

byDavid A . Meyer, B.SeMichael J. Perkins

INDEX

page

INTRODUCTIONLOCATION and ACCESSTOPOGRAPHY, CLIMATE and VEGETATIONCLAIMSPAST WORKPREVIOUS WORK HISTORYREGIONAL GEOLOGYPROPERTY GEOLOGY

Property GeologyWest GridDoyle Lake Grid

INTRODUCTION

LOCATION and ACCESS:

The Doyle Lake property is located in Runnalls Township approximatly 80 km. north of Sault Ste. Marie, Ontario. Centered around Doyle Lake, the property is comprised of 100 contiguous mining claims through the east- central portion of the township.

Access to the property is by float plane into Doyle Lake from Batchawana Bay, about a 20 min. flight, or by 4 wheel drive vehicle using a all-weather logging road that runs well into the property in the south and along the eastern boundary in the north. Branching off this main gravel road, there are also several logging trails suitable for ATV vehicles that connect other portions of the property.

: V

H

One of these trails comes within several metres of the east end of Doyle Lake and continues on to the Montreal River. Another trail comes to within several hundred metres of the SW end of Doyle Lake but has not yet been pushed through. This could not be done in the summer without considerable dificulty and expense. Access to the property area by truck was at the time of this report prohibitively dificult due to the disrepair of several bridges over the Batchawana River and several unlicensed railway crossings south of the property. However, it is the author's impression that these obstacles could be relatively easily overcome in the event of further work requiring heavy equipment or a larger camp.

TOPOGRAPHY, CLIMATE and VEGETATION:

The topography in the area is very rugged with over 150m of relief over the property. The elevation of Doyle Lake is 403m. ASL. Hills cut the property in a south easterly direction with slopes generally 30-70 degrees and a series of creeks and small lakes occupying the low areas between them. These creeks are generally shallow and fast running to the south east into the Batchawana River just south of the property.

The climate is typical of Northern Ontario with temperatures ranging from 10-30 degrees Celsius in the summer season to -40 degees Celsius during winter. The proximity of the property to Lake Superior (50km.) results in the sudden appearance of storms and rainshowers.

Vegetation generally consists of mature pine, maple and birch on the slopes with moderate to dense secondary deciduous growth, and an assortment of the above with balsam fir and alders in the lower areas. Large swampy areas and some of the steeper slopes are dominated by cedar. There is little evidence of logging on the property with the exeption of the north east edge where a large clear-cut exists and the southern end of the West Grid where logging of pine has provided several logging trails.

CLAIMS:

The Doyle Lake property is comprised of 100 contiguous mining claims located in Runnalls Twp, N.T.S. 41 N/8, Map G-2420 Sault Ste.Marie Mining Division Index to Land Disposition. The claims are licenced under the following numbers:

SSM1136231 to SSM1136314 inclusive (84 claims) SSM1111714 to SSM1111729 inclusive (16 claims)

PREVIOUS WORK HISTORY:

Parts of the Doyle Lake Property have been examined for industrial minerals, gold and massive sulphide (copper, zinc) potential since 1953. The various companies involved and their activities, based on assessment records held in the Regional Geologists Office in Sault Saint Marie, are summarized as follows:

1953:Jalore Mining Company Ltd. flew an airbourne magnetometer survey over the entire township of Runnalls (then called TWP.25 R.15).

1960-1962:Algoma Central Railway (ACR) had several prospecting crews in examining the Granitic/Sediment contact for massive sulfide/Au in favourable geology and examining the building stone potential of the Grey Owl Lake Granite. Two showings were found, L-6 east of Doyle Lake and L-5A,near Mallot Lake, using ground EM targeted using airbourne results from the 1953 survey. Both were in Iron Formation. In 1962 ACR completed a follow-up airborne magnetometer and EM survey of the township and completed a detailed examination of the L-6 grid.

1963-1965:RioTinto Canada Exploration Ltd. completed an examination of all anomalies found by the ACR airbourne above. A total of 19 conductors were examined, 8 of which were located on the Tri- Origin Exploration Ltd. ( Grids El(over L6 above), E2, E3, E6, FI, Kl, K2, K3 were cut over the conductors on the Doyle Lake property which were then geologically mapped, geophysically surveyed with mag, EM, and gravity for massive sulphide targets. Initial trenching and channel sampling over the conductors returned assays of up to D.3% Copper over 45 feet on the E3 and E6 grids located north of Doyle Lake. After resampling ACR and RioTinto felt the results were not conclusive enough and recommended two drill holes.

1966:Canex Aerial Exploration Limited drilled a 165 foot hole on the E6 grid locating minor pyrite and pyrrhotite and a graphitic zone they felt to be the conductor. Due to negative assay results they did not feel the conductor warranted further drilling.

1975:Geophysical Engineering Limited drilled two holes over conductors located using the ACR airborne. Hole Al was 700m north east of Doyle Lake on grid E1(L6). It was 130 feet long and located several sulphide zones composed of stringers and seams of pyrite/pyrrhotite (3:1 ratio) up to three feet thick. Hole A2 was drilled 3km south east of Doyle Lake, targeting an airborne geophysics anomally not previously grided.This hole was 123.4 feet long and intersected up to 4 feet of massive pyrite/pyrrhotite in a felsic ash tuff which assayed 20ppb Au, l.4ppm Ag, 209 ppm Zn, and 47 ppm Cu over 2.0 feet.

1983:Noranda Exploration completed ground magnetics and EM over three claims located near grid E4. Their reccommendations were to drill for massive sulphides along South-east trending anomalies. Currently this property lies to the north-east outside the Tri-Origin Exploration Ltd. holdings.

1984:Manwa Exploration Services contracted a Digem III Airborne Survey over the entire property area. This survey was made up of mag, resistivity, EM, and VLF at 1/8 mile spacings for over 2,907 line Km. In this same year Dryden Resources obtained large mining interests in the area.

1985-1986:Granges Exploration Ltd. optioned 600 claims in Runnalls Twp. from Dryden Resources and based on the 1984 airborne information located 10 grids over geophysical anomalies. Three of these grids were located on current Tri-Origin Exploration Ltd. holdings, grids 6,7,8. Anomalies were located on the ground using horizontal-loop geophysics, grids cut, and 17 drill holes completed, ddh's R86-9,12,13,14,15 where located on current Tri-Origin Exploration Ltd. holdings. Interesting results from ddh 86-13 (Grid 7) of up to 5.5gm. Au/tonne over 0.8m and several zones of up to 2.0m massive Pyrite/pyrrhotite prompted a further four ddh's, R86-18, 19, 20, 21. Although there is no record of the drill logs for these holes the core is located at the Core Library in Sault Saint Marie, Ontario, and was examined and quickly logged. All of the holes contained massive pyrite zones in some cases up to 7.0m in length. While there is no record of assay results for these holes a Granges Exploration Ltd.summary report states:

"Of these holes only R86-19 hit any values of interest (2.56 gm/T Au over 0.4 m). This hole was drilled 50 meters down strike from R86-13."

In addition to the drilling a soil sampling program was completed for gold over the conductor intersected by ddh R86- 13 but failed to locate a continuous anomaly. Granges felt the results were not interesting enough to warrant further expenditures.

No work has been recorded on the property since the above.

SUMMER, 1990 PROGRAM:

Between June 4th and July 5th, 1990 a program was carried out consisting of cutting and slashing on two grids, geological mapping and Induced Polarization (IP) geophysics over the grids, inspection

of the Northern and Western claim boundaries of the property, and reconnaissance mapping to outline the general geology of the property and locations of roads and trails.

Linecutting commenced on May 22nd and was completed on June 5th. To establish the West Grid, located at the south west corner of Doyle Lake, the existing Granges 1986 "number seven" grid was recut and repicketed at 25m intervals by Paul Bedard of Val D'Or, P.Q.. The grid consists of a baseline (00) and a tieline (8E), oriented at approximately 335 degrees azimuth with crosslines every 100m. The crosslines run from 17N to 8S.

Line 13N was extended on a bearing of 65 degrees azimuth across the southern edge of Doyle Lake to the station 20+OOE. At this point, a new grid, called "the Doyle Lake Grid" was laid off and cut at the same orientation and intervals as the West Grid. In most places the Granges grid was easily followable with the exception of the south end where clear cutting has been carried out since 1986. In places, topography and the waste from clear cutting resulted in minor chaining inacuracies but a "best fit" method was used to place the grid on the map using known points of topography such as creeks, swamps and lakes.

At approximately the same time, Geological mapping was carried out over the cut grids at 1:2500 scale. Coverage was obtained by walking each line and investigating all outcrops within 25 metres of the line. Representative samples were taken as well as those for assay. Assay samples were sent to Swastika Laboratories in Kirkland Lake for analysis for Cu, Pb, Zn, Ag, and Au.

Also at approximately the same time, an IP survey was completed over the grid by Mertens and McNeil Geophysical Ground Surveys Ltd. with N S 5 25m. electrode spacings. IP pseudo-sections were produced in the field each night and preliminary observations were made to pin-point conductors. Areas outlined in this manner were reinvestigated for mineralization or other sources of conductivity. A detailed report on this survey is to be produced indepentantly.

A partial claims survey of the property boundary was also undertaken to determine the location and condition of posts and lines. Data on the North claim boundary is included in the appendix. Any posts encountered while mapping were tied in to either the geological grid or to topography as well as possible.

On July 7th the camp was dismantled and all Geophysical and Geological personnel returned to Batchewana Bay airbase.

REGIONAL GEOLOGY:

The entire area has been mapped by the Ontario Geological Survey (OGS) on a regional scale by E.C.Grunsky and G.M. Siragusa, (OGS Reports 205 and 243 respectively). Some dissagreement appears to exist between the two authors as to geological interpretation especialy in the area of the petrology of the sediments/felsic

volcanics which make up the bulk of the rocks underlying the twomain Tri Origin grids.

PROPERTY GEOLOGY:

The geology of the property consists of a seqence of felsic to intermediate tuffs interbedded with clastic metasediments such as greywackes and arkoses. The general strike of the units is 160 degrees and dipping to the east. Tops have been suggested to the west making the sequence overturned. The metasediments are predominantly composed of reworked felsic to intermediate volcanic material making their distiction from the metavolcanics difficult and often arbitrary. The same classification scheme used by the Ontario Geological survey was used for mapping on the Tri Origin claims.

Numerous diabase dykes cut the property at approximately 140 to 160 degrees. These are predominantly massive but a few are porphyritic. Major dykes are often accompanied by offshoots at angles from 60 to 90 degrees. The diabase tends to occupy the topographic highs on the property obviously due to its resistance to weathering.

The edge of the Grey Owl Lake granitic stock is located near the western edge of the property and another granitic/monzonitic body lies in the centre of the property. Both are massive, coarse grained and have pegmatitic off-shoots.

THE WEST GRID:

The main target on the west grid was a long, fairly continuous airborne geophysical anomaly which had been drilled most recently by Granges. The sulfide zone was found in mapping at approximately 3+50 E to 4+00 E in the southern part of the grid but in the main target area it was poorly exposed due to down-weathering. Some effort was made to try to make a distinction between the petrology of the hanging wall and footwall but due to the interbedded nature of the sequence this was poorly established. There may be some basis for calling the rocks to the east more felsic and the rocks to the west more sedimentary but additional detailed mapping is recommended before such a conclusion could be justified. Several locations exist where trenching of the sulfide zone would be very easy due to shallow overburden and good drainage ( a near verticle cliff) for waste water.

Several other targets were investigated on the main "West" grid. Several major quartz veins were discovered and sampled. Both had associated hematite. Strike information leads to the possibility that the two outcrops represent the same vein but there are no other exposures of the vein in between.

A secondary IP target was observed in the northern part of the

grid centred around the creek. No explanation was found during mapping. Shear zone weathering here may have destoyed any exposure of mineralization on surface.

DOYLE LAKE GRID:

The Doyle Lake grid is underlain by rocks that appeared to the author to be nearly identical to those of the West grid. Interbanding of sediments and felsic volcanics made clear distinction difficult. More detailed mapping and petrology is recommended. The sulfide zone was mapped in only one location due to low percentage outcrop and possible trenching or shear zone weathering.

Mapping of the rest of the propery was done at 1:5000 scale and keyed on the five other showings on the property. The Granges grid on the Northwest end of Doyle Lake was the only other grid which was useable. Sequences of felsic to intermediate volcanics and sediments were found on all the grids and some exposure of sulfide mineralization was found. However, differentiation of volcanics and sediments (as on the OGS maps) was not possible at this scale and more detailed or extensive mapping and/or petrology/geochemistry is recommended before this distinction could be made.

y/*

TRI ORIGIN EXPLORATION LTD.

78 ASQUITH AVENUE , TORONTO , ONTARIO.

TECHNICAL AND LOGISTICAL REPORTFOR THE

INDUCED POLARIZATION SURVEYDOYLE LAKE

BATCHAWANA,ONTARIO

Box 1682, Guelph Ontario N1H 6Z9 * Box 1063, Sydrwy Nov*ScotaB1P6J7

MERTENS d MacNEIL GEOPHYSICAL GROUND SURVEYS LTD. was contracted

by Dr. R. Valliant of TRI ORIGIN EXPLORATION LTD. , 78 Asquith Avenue ,

Toronto , Ontario, to carry out an Induced Polarization survey on their

Doyle Lake Property near Batchawana , Ontario. Mertens 6 MacNeil Ltd.

carried out this survey during July, 1990.

PARAMETERS \\\\\\\\\S\\\

The parameters of the survey were as follows :

1. Number of kilometers @ "a": 25 metres 24.850 kras,@ "a"s 10 metres 0.810 kms.

2. Array : Dipole - dipole

3. Spread : " a " = 25 km. " a " = 10 km.

4. Dipole Seperation : " n " * 4

5. Method : Phase ( with reference cable control)

6. Frequency : 1.0 hz.

EQUIPMENT \\\\\\\\\\\

The equipment used for the survey was :

1. Receiver : Phoenix IPV - 4 Turbo

2. Transmitter : Phoenix IPT1

3. Motor Generator : M.G. 2 output 2.5 kva.

4. Electrodes : Aluminium foil

Box 1682, Guelph Ortwio N1H 6Z9 e Box 1063. Sydney Nova Scotia B1P 6J7

ACCESS \\\\\\\\\

The access to the grid was by truck to Batchawana Bay, Ontario.

The grid was reached by air from Batchawana Bay using Batchawana Air

Service's Beaver on floats . The camp was set up on Doyle Lake.

MOBILIZATION \\\\\\\\\\\\\\\

The crew and equipment were mobilized from Guelph , Ontario by truck

to Batchawana Bay, Ontario.

CREW MEMBERS \\\\\\\\\\\\\\\

JACK MacNEIL P.O. Box 634, Bedford, N.S. B4A 3H4

RON MERTENS P.O. Box 1682, Guelph , Ontario. NIB 6Z9

DAVE GOUTHRO Frenchvale , N.S,

Kevin MacKenzie Sydney , N.S.

BLAISE CAMPBELL Frenchvale , N.S,

l lTri Origin Property

--- . l

soj^s.A-' J

* * t^V:'5:^:55iig'Tî1:U'ft^S:'ir'' WW-WIITI *K' * * * *^feW^**ii?îk'' ' y rx -r ic no

GENERAL GEOLOGY. . f

PROPERTY MAP

Tri Origin Exploration Ltd.

PROPERY LOCATION

j r'3*"7 L- "3ti^—,^la^

:^-o- *- ;; T^ x* ~•j V - - - -r-^^1 - -' - - ,* r.,. - - -r l l f . ., - \. ' J-. "r

r,- -XK-^--

KUDEX TO LAND DISPOSITION

RUNNALLS

V.h , AIM/.INISTRATIVE f

WAV/A -I..UilNG DiV'.S.OH

SAULT STE. MARIELAl.'U TITIES/R1GIS1RY DIVISION

ALGOMA

41Na8SE8828 2.14388 RUNNALLS 300

ntanoMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

November 2 2, 1 991

Mining Lands Branch Geoscience Approvals Section 159 Cedar Street, 4th Floor Sudbury, Ontario P3B 6A5

Toll Free: Telephone: Fax:

1-800-465-3880 (705) 670-7264 (705) 670-7262

Our File: 2. 14308 Your File: W. 9150. 5008

Mining RecorderMinistry of Northern Developmentand Mines875 Queen Street EastP. O. Box 669Sault Ste. Marie, Ontario.P6A 2B3

Subject: Approval of Assessment Work submitted on Mining Claims SSM 1136231 et al Runnalls Twp.

The deficiencies in the Geological and Geophysical Surveys, submitted on Report of Work W. 9150. 5008 have been rectified.

The assessment work credits listed on the revised work credit forms for Geological mapping and Geophysics have been approved under Section 12 and 14 as of the above date.

Note a correction to claim numbers on original Work Report W. 9150.05008 for claim numbers SSM 111714 - SSM 111729 inclusive should be SSM 1111714 - SSM 1111729 inclusive.

Please indicate this approval on your records.

Yours sincerely,

Ron GashinskiSenior Manager, Mining Lands BranchMines and Minerals Division

'A/j l Enclosures:

cc: ^/Assessment Files Office Toronto, Ontario

Resident GeologistSault Ste. Marie, Ontario

FILE NUMBER: 2. 14308DATE: November 22, 1991RECORDER'S REPORT NUMBER: W9150-0 5008

RECORDED HOLDER: Tri Origin Exploration LTD. CLIENT NUMBER: 203126 TOWNSHIP OR AREA: Runnalls Twp.

Total Assessment Credit claimed: $86 / 409. 00

Level of Assessment Credit to be Approved on November 22, 1991 will be $ 85, 101. 00

CLAIM NO. VALUE OF ASSESSMENT WORK DONE ON CLAIM

SSM 1136231 $ 330.00SSM 1136232 $ 330.00SSM 1136233 $ 330.00SSM 1136234 $ 0. 00SSM 1136235 ^ 0. 00SSM 1136236 ^ 0. 00SSM 1136237 ^ 0. 00SSM 1136238 $ 330.00SSM 1136239 $ 0. 00SSM 1136240 $ 330.00SSM 1136241 $ 330.00SSM 1136242 $ 0. 00SSM 1136243 $ 0. 00SSM 1136244 $ 0. 00SSM 1136245 ^ 0. 00SSM 1136246 S 0. 00SSM 1136247 $ 330.00SSM 1136248 ^ 330.00SSM 1136249 $ 330.00SSM 1136250 IS 330. 00SSM 1136251 $ 2198.00SSM 1136252 $ 2198. 00SSM 1136253 $ 330. 00SSM 1136254 $ 0.00SSM 1136255 $ 330.00SSM 1136256 JJ 330. 00SSM 1136257 $ 330.00SSM 1136258 $ 330.00SSM 1136259 $ 330.00SSM 1136260 $ 0. 00SSM 1136261 $ 330.00SSM 1136262 S 330. 00

VALUE APPLIED TO THIS CLAIM

$ 851. 00S 851. 00$ 851. 00$ 851. 00S 851.00$ 851. 00$ 851.00^ 851. 00S 851. 00^ 851. 00$ 851.00$ 851. 00S 851. 00$ 851. 00$ 851.00$ 851. 00$ 851.00$ 851. 00S 851. 00$ 851. 00$ 851. 00^ 851. 00$ 851.005 851. 00$ 851. 00$ 851.005 851. 00$ 851.00$ 851.00$ 851.00^ 851. 00^ 851. 00

VALUE ASSIGNED FROM THIS CLAIM

S 1347. 00 $ 1347. 00

SSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSM

113626311362641136265113626611362671136268113626911362701136271113627211362731136274113627511362761136277113627811362791136280113628111362821136283113628411362851136286113628711362881136289113629011362911136292113629311362941136295113629611362971136298113629911363001136301113630211363031136304113630511363061136307113630811363091136310113631111363121136313113631411117141111715

$ 330. 00$ 330. 00^ 330. 00S 3 30. 00

$ 0. 00$ 0. 00

$ 330. 00^ 330. 00$ 330. 00$ 330. 00$ 330. 00S 3 30. 00$ 330. 00

S o. oo$ 0. 00$ 0. 00

$ 330. 00$ 330. 00

$ 0. 00$ 0. 00

$ 330. 00$ 330. 00$ 330. 00

$ 2198. 00S 2 198. 00$ 2198. 00$ 330. 00

$ 0. 00$ 0. 00

$ 330. 00$ 0. 00$ 0. 00

$ 2198. 00^ 2198. 00^ 2198. 00$ 330. 00

$ 2198. 00$ 2198. 00$ 2198. 00S 2 199. 00i 2199. 00$ 2199. 00$ 2199. 00$ 2199. 00$ 331. 00

$ 0. 00$ 2199. 00$ 2199. 00$ 2199. 00$ 2199. 00

$ 0. 00S 0. 00$ 0. 00

$ 2199. 00

O 851. 00 $ 851. 00 $ 651. 00 $ 851. 00 ^ 851. 00 S 851. 00 ^ 851. 00 $ 851.00 $ 851. 00 $ 851.00 S 8 51. 00 $ 651. 00 $ 851.00 $ 851.00 $ 851. 00 $ 851.00 ^ 851. 00 O 851. 00 iS 851. 00 O 851. 00 S 851. 00 $ 851. 00 $ 851.00 $ 851. 00 ^ 851. 00 $ 851.00 O 851.00 ^ 851.00 O 851. 00 $ 851. 00 $ 851. 00 ^ 851. 00 ^ 851. 00 O 851. 00 S 851.00 S 851. 00 5 851. 00 $ 851.00 ^ 851. 00 S 851. 00 $ 851. 00 S 851. 00 S 851. 00 $ 851. 00 g 851. 00 $ 851. 00 O 851. 00 $ 851. 00 $ 851.00 $ 851.00 $ 851.00 0 851. 00 ^ 851. 00 ^ 851. 00

O 1347.00 $ 1347. 00 ^ 1347. 00

$ 1347. 00 0 1347. 00 $ 1347. 00

$ 1347. 00^ 1347. 00S 1347. 00O 1348. 00$ 1348. 00^ 1348. 00S 1348. 00S 1348. 00

$ 1348. 00 ^ 1348. 00 S 1348. 00 $ 1348.00

$ 1348. 00

SSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSM

11111111111111

11111111111111

11111111111111

17161717171817191720172117221723172417251726172717281729

$$$$$$$

$$$$$

2199.2199.2199.2199.2199.2199.2199.$ 0.$ 0.

2199.2199.2199.2199.2199.

0000000000000000000000000000

TOTAL CLAIMS

100 $ 85101. 00

$ 851. 00 $ 851. 00 ^ 851. 00 ^ 851. 00 ^ 851. 00 $ 851. 00 $ 851. 00 $ 851. 00 $ 851. 00 $ 851. 00 g 851. 00 $ 851.00 S 851. 00 $ 852. 00

$ 1348. 00 $ 1348. 00 $ 1348. 00 $ 1348. 00 ^ 1348. 00 0 1348. 00 ^ 1348. 00

$ 1348. 00 O 1348. 00 $ 1348.00 $ 1348. 00 $ 1347. 00

$ 85101. 00 44472. 00

Ministry ofNort' n Developmentand ... .tea

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

Personal ink^pon collected on this form Is obtained under tha authority of tha Mining Act. This Information wM ba used for this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development md Sudbury, Ontario, P3E 6A5. telephone (705) 670-7264. *} ~"

Floor. 150 Cedar Straat,

08Instructions: - Please type or print and submit in duplicate.

- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder.

- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

Racordad HoMar(s) CUsnt No.203

Addrass

Division

phono No.

Mining Township/Araa ' or Q Plan No. / Qn nnal

Datas Work Parformed

From: To:

Work Performed (Check One Work Group Only)Work Group

X Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

/i~r)*-C,i*.tfriryj t •^•e*?/'* *jy ^ /^K*^tfcc^ /S^**'~ta^T's***S s \r *^f r

RECEIVEDAim 3 8 1991J-\UU W " i~-- -

MINING LANDS oLv '

^ BECORDED.

AUG 1 5 1991

Receiot

Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Person* and Survey Company Who Performed the Work (Give Name and Address of Author of Report)

(attach a schedule H necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at tha tima tha work was performed, the claims covered in this work report ware recorded in the current holder's name or held under a benefid by tha currant recorded holder.

Recorded Hofder or Agent (Signature)

Certification of Work Reportl certlty that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or attar its completion and annexed report Is true.

ano AOC.*M ot rerson certifying

Telepone No. Date Cartmad By

For Office Us* Only-^^^ Total Value Cr. Recorded ' Date Recorded

Deemed/Mpproval Date

Wningl

Date Approved

Date Niolice for Amendments Sent

RECEIVED

15AOU 1991

Ontario

Mini! *f'North*. 11 Developmentand Mines

dudu Nord

Statement of Costs for Assessment Credit6tat des coOts aux fins du credit d'evaluation

Mining Act/Loi sur les mines

Transaction NoJN* de transaction

M J 4/56-

2.14308Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should b* directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente tormute sent recueillis en vertu de la Lol sur lee mine* et sen/front a lenir a jour un registre des concessions minieres. Adresser toute question sur la collece de ces renseignements au chef provincial des terrains mirier*, ministere du Devetoppement du Nord et des Mines. 159, rue Cedar. 4* etage, Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Coots directs

Type

fafafeWAel

Salalree

Contractor'* end Consultant's Fee*Droned*

et de ('expert- consell

SupoHeeUsed Fournttures utilleee*

Equipment Rental Location d* materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Typ* h'*4**Jti"f

9~*jf4*4C*lyH*3

•*S / i f*. fer f 'f ***/))

Type f

Type

Amount Montant

l-foo-•*t 021~'

S*t J2*t ^3f 7*^ "

S&i *

Total Direct Costs Total des couts directs

Totals Total global

7****f

te*h*9

WH

2. Indirect Costs/Couts Indirect** * Note: When claiming Rehabilitation work Indirect coats are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirect* ne sont pas admissible* en tant que travaux d'evaluation.

Type

Transportation Transport

Food and Lodging Nourrtture et

Mobilization and Demobilization Mobilisation et demobilisation

DescriptionType

Amount Montant

Sub Totsl of Indirect Costs Total psrtlel des couts Indirect*

Amount Allowable (not greater than 20* of Direct Costs) Montant admissible (n'excedant pea 20 H des touts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and AflewaMe d'evaluation Indirect coots) fToM dn cote dncfc

Totals Total global

A}f4^

/*f #S'

".j'*'K*hf

t

r

l

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Letitulaireenregistre sera tenude verifier lee depenees demandess dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluation preaentes.

Filing Discounts

1. Work filed within two years of completion is claimed at lOOIfc of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans les deux arts suivant lew achevement sont rembc>ursesa1M%<fetovaleurtotatesusfnentkx>ne•ducr^

2. Work filed three, four or five years after completion is claimed at 50*Vfa of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50 -

2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 "tt de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit d'evaluation

x 0,50Evaluation totale demandee

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as (Recorded Holder, Agent, Position in Company)

to make this certification

Attestation de l'etat des couts

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engages* pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-Joint.

l am authorized Et qu'a titre depoctv occup4 d*w li

je suls autorise

a faire cette attestation.

Signature

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NumaVo d* rapportsur 1** travaux executes

pour ('affectationd* la reserve

Numero d* claim

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1134,213

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Lea

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its q

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en a

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MJni.-lry of Noril.Grn Dcvc and fv'iiics

r-B* f^-wv-* a^* jj-^x r ^, T- "rî f-* T-"-fci...,îr.J*. t O LAEvF5 f:^,-

PLAH

G-2420TOWNSHIP

RUNNALLS

-t

tt~ L uF ISSUE

--3 8 1991

XT STE. MARIE "ÔRDER'S OFFICE

V/AV/A r-MiiiJi-JGCv/.SiOH

SAULT STE. MAUr.'DTITlES/RI-GISTRY DIVISION

ALGOMA

i;. E

1000

10DD

Scale 1:?0 000

looo 2 DOO SOD: 4000 S'?QO -! coo 10 C :-o- F,

Conlour Interv.al 10

ARtAS V;iTHDRA\VN PKC ' f ,3POt.'!TION

r.'.RO- Mining Rig'-.ts C -- . S:iO- Surface Pigh'^ T--v

rM-i S- Mining and Si, r.-;- F ..-.'.s

SYMBOLS Description No. Date

BoundaryTownship. Meridian. Baseline.

Road allowance; surveyed ... shoreline...

Lol/Concession; surveyed... unsurveyed

Parcel; surveyedunsurveyed

Righl-of-way; road

railwayutility , . ... . . ...

Reservation

Cliff. Pit. Pile

ContourInterpolated Approximate Depression ...

Control point (horizontal) .

Flooded land........

Mine head frame ..................................... ........ a

Pipeline (above ground)

Railway; single track....................... ..... .. ————————double track .. ... ...... .. ........ .... .. ————————abandonee . . .. ... . .. . . ... ... . —— —— ——

Road; highway, county, township access ...... . . . . . . . . . .trail, bush ...,. .. .... . ,...........,.......... —- — — — --

Shoreline (original}.

Transmission tine

Wooded area.. -.. —. ~

DISPOSITION OF CROWN LANDSPatent

Surface 4 Mining Rights Surface Rights Only Mining Rights Only

LeaseSurface 4 Mmn. ^ Rights Surface Rights Only Mining Rights Only . .

Licence of Occupation

Order-in-Council . . .

Cancelled

Reservation

Sand 4 Gravel.

.B..B

..T

oc ©O

T HI- IMFORMATt' IT. TNA~" APPFC.RS ON T Mi's M Af- HAS BFEN COMPll FT, FROM VARIOUS SOURCF', AND ACCURAC V i:. NT

.f jr.WiRHiNCi T O STAKE iN(i Ci AIMS SHOW. TSUIT WITH THE W RFCORDER MIMNORTHF-HN DF .'E L O^MFNT AND M INES COR f-'.:OITIONAL. INFÎRMATIONf IN THF '^TATUi, "r T H(

S SHOWN MT^f f ir.

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41N085E0ei20 2 .14308 RUNNALLS

DOYLE

LAKE

5.

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Outcrop area, small outcrop

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Sample location and number

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Revised By

, V

Date

Nov., 1990Tri Origin Exploration Ltd.

SAULT PROJECT — ONTARIORUNNALLS TOWNSHIP

DOYLE LAKE GRID

GEOLOGY^ /^f^^ , ^^^— ' f-

Date-- Aug., 1990 N.T.S.: 4IN/8 By^ D. M. , M. R Dwg.No.:

L-8

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Limits of surveyed line

100 200

41N08SE0Ba0 2.14308 RUNNALLS 260 METRES

Revised By Date Tri Origin Exploration LtdSAULT PROJECT — ONTARIO

RUNNALLS TOWNSHIP

DOYLE LAKE

l. P PLAN MAPf \t\i4jr*~ ^ -

DIPOLE DIPOLE 3 a = 25mDate: Nov., 1990 N.T.S.: 4IN/8 By: R.V. Dwg.No.:

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f ' \MF IP RES \ i \ RES IP MF20 80 8000 \ y' x J-80DO OJ ^0

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^r GC

^^"^ -JLL

o. o. 0 i ,., ,, -, — ,— ,--.- — r~ —— i . -t' — :~ t , — . .0 s -C

TOPOGRAPHY

filter "m. 21K 2W 31K 22K 7S97 B86S UK 6329 filter RESISTIVITY

(-1=1 25X t v!2K j XK ** 2BKxxv5739 516S* \^21K n=l tohm-m)

0=3 KK\ m \ wf//^ r 1*^^ east //^ ( f ^ n ~ 3^x^ * — ' ^Jj^^ B S ^*\ f t s ^*^ \ 1 \

0 = 4 38B^- 25H - ^mi -Î3K 13^' ' 3341 "-61.631 \ 12K n s 4

2+50 E 3*00 E 3*50 E 4+00 E

filter 1212132031*593631 filter PHASE

0=2 9.5- ——— fî^J/J,3 / ** M^ 68 V\ 8 n E 2

n s 3 3-* ''l^/^J8 x M c * ^v H V *? n s 30 = 4 4.2 ''17/42 47 36 32^^- 57 \ 23 0=4

INTERPRETATION

2+50 E 3KO E 3^50 E 4+00 E

filto- 0 .1 .1 .1 -3 .7 l.l .6 .9 niter METP|L FACTOR

0=1 .1 .2 .1 o .1 , , .9, -l.e/^.l 0=1 Up/res* 100)

0=2 0 .1 0 D .6 ~"".6-^ .-P J"5* ^ n = 2

0 = 3 0 0 .1 .5 -* "~^ '){,(C^\U\' 2 R Z ^

0 = 4 o .1 . 6 \ .4 , 3 X xi.i — .(' \ .2 n-4

LCne 600 S

Q[poLe-D ipole Array

1 — ® — 1 1 — — 1

\ /XX ~r-

^v'" n * 1, 2. 3, 4 plot pofnt

Flit ered Prof i 1 es

filter Res is t lv i t y — — — —— *

Metal Factor ———————— - * * ** * * *

Logar i thm Tc Contours J' K 5 * 2- 3' 5- 7- 5 ' 10,...

Insiruments! IPT1, IPV4 Frequency: 1 . 0 Hz

Operator: J.H.N.


INDUCED POLARIZATION SURVEYDoyle Lake Grid, Sault Project,

Batachawana. Qntarto.

Oaie: June \ 1990 N.T.S. 41 N/8

Scale! 1 : 2500

MERTENS S MacNEIL LTD.EEOSOFT ItmJ Software for the Earth Sciences, Toronto, Canada

41Na8SE0020 2,14306 RUNNALLS 290

1MF IP RES\ RES IF MF 20 80 ecoo-I . r6000 r60 r20

\ /\ a]0. 40. 4COO. 7 v 7 N. \ . -4000 .40 .10 0~

x^/ Nv X aUJi—

D- o. o , , , , i , i , n -D .a

f

TOPOGRAPHY

•JT^XJ L HTTJJ l.

f 1 1 ter yW3 dist) /j* AAJ J3A f il ter RFS T ST T V T T Y

n*l 17K -xxlEBS,vv tfK-~xJEe 0=1 lohm-m) ^//\^î^

n s 2 ZW5 *C SZAT^y^l^— — -1SB 0 = 2

3+50 E 1+00 E

filter 3* K M 28 32 filter PHASE

1-1=1 17 . , EC s w v-^.B.9 0=1 CmvllE-rad!

0 = 2 5fl 70 J^fl6 A n ::: ^

0 = 3 54 ^^1 46 \25 0 = 3

0=^1 29 —— 31 36^-2? 0 = 4

INTERPRETATION

3+50 E 1+00 Efilter Li 2.4 L.2 1.4 t filter MEJAL FACTOR

0=1 -i y/ x 4 ' //y .T^fcsMa .9 0=1 ip/res * IDD)

O j /^^ - 1 1. 1 M ,-^T^ - Q

0=4 1.6 t ' .4— .6 .6 0 = 4

LJne 500 S

Dlpole-Dlpole Array

a ra a

N f•^ s \ xN X\ / oc\ x a s /b m

^\'' n = 1. 2. 3, 4p to t point

Filtered Profiles

f liter Resistivity —— —— —— —— * Polar i2at ion —————————— * *

Metal Factor ———————— - * * *

Logar i i h m i c Con-tours l ' K 5 ' 2' 3- 5' 7- 5 ' 10*.-.

lostruments: 1PT1. IPV4 Frequency I 1.0 Hz

Operator: J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Grtd t Sault Project,

Batachawana, On tar Co.

Date: June \ 1990 N.T.S. 41 N/8

Scale: 1 : 2500

MERTENS S MacNEIL LTD.EEOSOFT ttml Software for the Earth Sciences, Toronto, C anada

41N08SE0028 2 .14308 RUNNALLS 300

0-33 E 1-HDO E 1*50 E 2*00 E 2+5Q E 3-00 E 3*50 E 4-00 E fl-50 E 5*CO E 5-5C E &CO E

0*50 E 1*00 E 1+50 E 2*00 E Z*-SO E J*OD E J*SO E 4-00 E -1+50 E 5*00 E S*SO E 6*CO E

u 1.3 z.s e.? 10 15 a K e

i 4 s.e- s

p 23 y is is IE w is n e .? e.? f;ltw FHASF

K c B 33-2 n 23 -is]S

i; 17Ts n " 3

n s 4

DjOÊ 1--00 E JÔj^ 2-CO E 2*50 E 3*DO E 4fCO E 4*50 E 5HX E 5*50 E 6*00 E

flit: O D O O O .1 .1 .4 1.4 1.4 ,7 .5 l. S .3 .2 .1 .1 .1 .1 . 1 .1 . ; f;lt e

INTERPRETATION

METAL FACTOR l Jp/res * 100)

0=2

nM -i

o .1 D o c o o o < I i '——HI ^-^"O o o o .6 .B

.1 t O O .3 .* S 1.1 * .8 —".7 — — .S .! ^ .B ^ .1 0=4

Resist tvity —— — —— ——Polar Izat Ion —————————Me-tal Factor ————————- * * t

Logsr T Ihfn [cContours ]- '-S. 2- 3, 5, 7.5, I D,

Instruments: IPT1, IPV4 Frequency! 1 . 0 Hz

Operator: J.M.N,


INDUCED POLARIZATION SURVEYDoyle Lake Gr I d, Sault Project

Balachawana, Ontar Eo.

Date! June \ 1990

Scale: l : 2500

N.T.S. 1 1 N/6

MERTENS fi MacNEIL LTD.ifutOFf tin! SoftKaco for tha Earth ScJancas, Toronto, Canada

41N08SEB020 2.14308 RUNNALLS 310

MF ZO-

H————i————l————————h-

1+CD E 1+50 E 2+00 E 2+50 E 3*COE 3+50 E 1+00 E 4+50 E 5+COE 5tSO E2w; 3* 3* 31K GIST 3630 7289 IK 3* W •W 39C 30K S* 3CK 31K f[lter

[400 E 1*50 E 2*00 E 2+5G E 3400 E 3*50 E 4+OOE 4+50 E S*00 E 5+50 E &KDQ E

filter 17 13 12 8.6 7.5 6 5.5 B.3 H K S 3* 35 O 30 ffi 22 20 IB la 21 H 11

0=2

0 = 3

0 = 5

MF 0

.10

1-KB E 1*50 E-4——l——l——l——t. Z+O) E 2+5D E 3*00 E 4+50 E 5+00 E 5**0 E 6+CO E

fllto- .1 .1

0=1 .1 .1

n:2 -i

0 = 3 .1 n^ 4 n*5

.1 .1 .1 .1 .1 .1

.t 1.3 2.3 .7 .S .1 .1 .1 .1

.1 .1 .1

.1 .1 .1 Hit

r-'^^Y^-L — ^.SA( l S-L

*Vj

^ ^SK 1.1—^ -E

.1 .1 .2 .t

O . 1 .2

O O .2 .1

C .3 .1

TOPOGRAPHY

RESISTIVITY

lohm-m)

PHASE

(rnilli-radJ

INTERPRETATION

METAL FftCTC)Rn-1 ITp/res* 100)

GEOSOFT (Im! Software for t ha Earth Se lane**, foronto; Canada

Line 3 00 S

D^pole-D Ipole (Vray

\s s\ s

p l o l po i r 1

a = {3 n

n - 1. 2. 3, 4

Fll tered Prof I l

Resistivity ——————Polar izat ion —————————Metal Factor —————————-

filter*

* ** * *

Loqar i thm [c Contours - J- 5 ' 2- 3- ^, 7.5, 10,

instruments: IPT1. IPV4 Frequency^ J. Q Hr

Operslor: J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Grid, Saull Projecl,

Batachawana. On tar ED.

Data: June \ 1990

Scale: 1 ! 2500

N.T.S. 11 N/8

MERTENS S MacNEIL LTD.

4IN085E8020 2.l1308 RUNNALLS 320

MF

10.

OJ

IP RES80., 8COO-,

40. 4000.

OJ O

IP -BO

-40

OSO E 1+03 E USD E 2+00 E 2+50 E 3+00 E 3+50 E 4+QQ E 4+50 E 5tOQ E

0+50 E 3+00 E L+50E 2+00 E 2+50 E 3+00 E 3+50 E 4+00 E 4+50 E S4QOE

filter 9.* 8.9 ELS 6.1 7.2 B. B 10 12 15 22 3Z 3D 26 24 23 21 21

14 14 —— IS

2! -\ 16 15 18 IB r 1 2

31 22 22 !S

25 21 26-43 3D 23 25 27.5———-7.1 1 .9 7.1 6.6 ' a.B

MF-20

-t——i——i——.——i——i——v-

0+50E t-^DE 2*00 E 2+50 E 3+OJ E 3+50 E 4*00 E 4+50 E-t——i——l——i——l——i——i- 5+ODE

fllte-

n=2

0 O O .1 .1 O

.t .1 .1 .1 .1 .1

O .1 .1 .2 .6 .6 ,5 . 4 .9

.1 .1 . , I.2-. ^..5.... .2

.1 .1 filter

.1 .1 .1

D D O O D O O D O .IJ.S^.B

O O ODOOOQO.1.4.2

O O D O D O O D Q .1 .3 .2 .3

.1 .i .1 .2 .1 .1 .i n s l.i .1 .1 .1 o o n ~ 2

.^ a .1 .1 .i o r^3^N .3 .1 .1 O .1 (-1 = 4

enUJ

o.Do: CLd LU o:LU

TOPOGRAPHY

RESISTIVITY(ohm-fn)

PHASE( m C11 E-rad)

INTERPRETATION

METAL FACTOR

t [ p/res * 1003

Line 200 S

D[pole-DipoLe Array

l—————l-

\ / - r-s s a = 2b m \/ n = 1. 2, 3, 4

plot point

F I I ter ed Profiles

Resistivity ——Polar tzat ion —————

Metal Factor ————

filter*

* *

Logar Mhm icConcurs L 1-5, 2 , 3 , 5, 7.5, ID,

Instruments: IPT1. IPV4 Frequency! 1.0 Hz

Operator: J.M.N.


INDUCED POLARIZATION SURVEYDoy l e L ake G rid, S auli P roject,

Batachawana, O nlar io.

Date! June \ 199D

Scale: l : 2500

N.T.5. 41 N/8


41Ne8SE0828 2 .14308 RUNNALLS 330

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f ;l ia- w; i^ i* JST: scs ?ico 21* ISK 431 gn wi 39( iw siz; 22? 2*6 IK 4V. t* 4* *m 33; ;IK SIK ISM rat 3E" ins IIEB IBIS T&t ra filter RFSTSTTVITY

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^=3 iy. j w IjtaB \ ^ f^^^^^- {^*- ^V/V1* "'i 7 ^X/^l^^V'^^-^'^^^^vS^ l ^ ^ J/^JS"'/ ™ /^ Ut^ r-—^ //^n^//^^^- 3 n ::3(1=4 |6K ilK-^lgU- —— BS8^^42ro^^2H^~^ Iftt'^WlJ ' 3W ^J^^Ji !^ ' 2W ' ' m ' ^ {y^^km r isT^ tcS^ToW^ 3W\ ^K~^~^73( ' W W/ 3CK 3*^ 19(^^-1328 ——— '15*1 IB9' ' ' fiffîs* n E 4

0 = 5 •C^-'* "^ n s5 0 = 6 ^ n = 6

OSO E 1+CO E 1-50 E 2+00 E 2-50 E S+CO E J+EC E 1+00 E 4-SO E &CC E 5-50 E &KB E &+S3 E 7+00 E 7+50 E &KO Efiltsf li H 13 S.5 6.5 7.S 3.7 li IZ 14 13 16 12 31 3" S T3 13 17 12 li 9.9 B,! 32 9.7 a4 a5 B.S B,5 10 20 7.9 fClto" PHA'iF

0=1 17 p —— 13 ^.11 - ^ S^^-^.ID IS ——— |9 33 ^ 14 14 ]SX ,!C fi 47 ^7^ -^, 1^ ie^- li IS ——— 15 _____ 14 - — - 17 ^- P^ —— . M I'^-Â^ — y —— a.^ y y y ti l= l ( mill J-rndl

n^2 9.5 13 C^r~""~^'Cir B ^-îA' (T^ 7.s\.i; n C^V^M/7 V x * * l\Ji ^ n C^j^ '•K^TH^^?^'I1CC^ NV^y'''^-ir-j /''^/JWi^ ^S^*" n * 2 0=3 n /^î7 i?", j s.5 \y X" io "•""13 \a.B B.S( iB"Z^^p~~^— is y^^ 23. J 33 31 B 3M. O6 — "~^~ "~^ " ^ B' 6 I0v^ " iTO\6.i s.9 * B.;/ /JJ^(fi a ffft^s n=^ n s4 i 15-^ iz~"^ a.^ ^6.1 —a.*' IT li n^-~^J^~ —— B. e is ' 39' s M se 31 33 ^ IT —— -is IE ' Ij 7.3 —— 7.1- —— 6.1 ^ n*^^ E.I ?.i ' z.s y 'Vi3 — P'rs.s n z 4

0=5 l/ a-' n=50 = 6 e- e rn a S

INTERPRETATION

0+50 E 1+00 E 1-50 E 2+00 E 2+^0 E 3-00 E 3+^0 E 4+CO E 4+SO E 5^0 E t 5+50 E , 6*00 E ( frÔ E | 7+00 E 7+50 E 8+00 E

ftlte- .1 .1 .1 .J .1 .3 -1 -t . 1 0 .1 .3 . 7 I .B 9.5 3.4 .B .3 .1 0 0 0 .1 D .1 .1 .3 1 ? 2.3 S.5 l.B filter METfiL FACTOR

n" 1 - l - l .3 -2 \- ? '- - ! -' - 1 - 1 - 1 0 • 1 \'-\ \^y^^l-^-^- 9 f 1 ,*l 0 - 1 -' .1 0 .1 o . 2 . 1 .4 . 2 \S~ Jb(fc^-i* f 3 n^l lip/res* 100) JlJ/// Vi^^^S--^ /-VV 47/1^^

n :2 .1 .1 .1 -1 -Z .1 .1 .1 0 Q D .1 ( ;sjj 5.3—— 13.1 ———— I^Jlj'O 0 D D D D D 0 .1 .1 .2 .4 jUs^ ^-^J^ J'* ^1=2

n^3 .1 .1 -a .1 .i -i -2 .1 .1 o o -i A/Y liS^^-S^îir — l-'\l"l -lo o o .i o .1 o .z .i /'.7 I jiffifc'&jll/f*-* n z 3[1=4 .1 .1 .1 .1 .2 0 .1 .1 .1 .1 0 .1 .4'*^î.6 -^ .f~~^ , S ~"^.( —— —l.l N .1 D 0 0 D 0 D .1 .3 .s""" . 1^/1 12-^^1 n s 4

n = 5 -* 0=5 n^ 6 0 n c 6

COSO^T Uir.1 Software for tha Esrlh ScJancai, Toronlo, C*raSa

LCne 00 N

Dlpole-Dlpole Array

* no t

KD-n i-®-is y

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^\'' n ^ 1. 2. 3. 4plot point

f i 1 1 er

Polarization ————————— * *Meial Factor -- — ----. * * *

Lcgar r thm le Contours L 1-5. 2. 3, 5, 7.5. 10,...

Instruments: IPT1. IPV4 Frequency! 1 .0 Hz

Operator: J.M.N.



Batachavrana. On tar lo.

Date: June \ 1990 N.T.S. 11 N/8

Scale: 1 : 2500

MERTENS 8 MacNEIL LTD.

41N0BSE0020 2.14308 RUNNALLS 350

^~--.~/ ! ' iMF IP RES J l \ RES IP MF ZQ-, 80., 0X0., -i . - \ - r90CD JC -20

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TOPOGRAPHY

0-SO E 1.00 E lt5D E 2-rCTJ E 2*50 E 3*00 E 3*50 E 4-CC E 4*50 E 5+00 E 5*50 E frtOO E 6*50 E . 7*00 E 7 '50 E

ri K 1 is f a \ \ aw y I st? ese y s-es x i?5i \ ••SS' y PI itx-^^cos-^ l^'~^— l? "\ 1?J-ic'xiS*1 X 29S6x iTa- vSS^-Ci"^^ l*/-' J6"--^ I5? 1 B1 -vi* *Jiii/ y *JJ'/ /if72 vB511 y P37 \ '9* n E ^ tohm-m)

n E 2 1W 1*. __ IW ) 7?fr^ BH3^~~T51t/ [W ___ IW 1W\ IW IW//2W (SK/ Jj,B5a /^3807 ( ZSO/ 4LCff ^^-iSC^-wTOK ( 1 2* 3W \ ]9( [9( ^'UN'V^-IW 7 ll"V ?JCS /JOB \ CM J i.iSl H E 2 —— -^ f \ ^^^ ^ -^s ——— ~^\ .— _ ^* l \ I /t*/.'* -^ ^-~*^ /^^^^ ^v 7 7 i \\ \ V \. -^~~^^ f s ^v l ^^ ^\ 7 f J/ sZ*

0=3 *iaT\ sp-~îiy J6564? /^\-^ ls} /®V\ C^^\ ^^X i^îw\ ^y/^1 3e*0 asas^^Sj y I&^ÎBIS^ t ^4JV\ ?* ^V "? (^"^V,-^ 2?" l/* '"///f^\. ^J //®'x5-)^4 n = ^ nsfl w * i^r- sis E4/ A* ' iw — "~ iac^- aa IEK -Û^^îw --'^xoa^-ses si? '^raes ' 2S* ^-is/-' •KS^~^Sr::^--'sz*~~- sis i* •x *w ' i*^- ISK f -^wt^-voA -âaf'-'îi ' MTB 0=1

&-50 E 1*00 E 1*50 E 2*00 E 2-50 E 3*00 E 3*50 E -KE E 1*50 E 5-CO E 5*53 E &+00 E 6*50 E 7*00 E 7+50 E

f Dta- ID 9.S S.6 fl 6B 8.7 S.4 W 8.9 8. J 6.6 B.3 11 IE 24 3D S 36 3! 22 17 li li li ID S C. G 8.6 5.1 4.2 2 f i Kar PhW5E

n- 1 i: 12 13 13 12- —— aa —— li ^ -IB —— H 13 9.9 ——— li 11 13 i Z4 i 33 40 32 -29 s J S ——— IS 14 14 13 12 ___ )2 ^2 1J i V3.1 5.1 . n 2 1 m ! l1 '"radl

n = 2 5.1 6,7 S. 7 5-^=^4-8 5.5 5.7 6.2 5.8 ^ J3\^~1.7 j.1/ J JO 73 ^^~ 3D^ E S l. 15^ ^J! "'Cgj. ds.E —i" 9-1 ^7 /ÎS) 1 B. 9 ^7.S *.B /^.8 n E 2

n E 3 T? 11^ Te^ s. a /^~" ia^S 8.4 10 ^) B.? sis' — -4.7 xîo X\,E 25 a IB 47 sa^re^"^- 1^^^ w n n iiO^^s ^ 7-7 ^ e.* f B-9 \ i i W~ — ' -s n E 30 = 4 11 ^^^7.8-^^6.S ' S.3- 12 -"/S -7.1 ——— E.9 M -— ~~i7s 10-^22 17 H E'* 56 39^2' ]S ' 11 li 13 12^^~— 3.5 ' 5.1 ^9.e '6.2'^-jti^^^ 1.6 n E 4

INTERPRETATION

O50 E 1*00 E 1*50 E 2*fC E , 2*50 E 5*^0 E 3*50 E 4*00 E 4*50 E 5-CO E 5*50 E 6+00 E 6^0 E 7*p) E 7*50 E

11=1 .1 .1 0 .1 .1 .2 .1 0 .1 .1 .1 .1 .1 .l.,|J-S ./'J i iS^y. -S^—^.J .1 .1 .1 .1 .1 .1 .1 .3 .1 .1 .3 11 = 1 t Ep/res * 100)

0 = 2 .1 0 0 .1 .1 .1 0 0 D D 0 C 0 1 ..9 ,,.T v\^3^XV"^ !j^N^.\-s 0 CO 0 .1 D D .1 .3 .2 .2 1^ = 2

n = 3 .1 .1 .1 .1 .1 .1 .1 o o o o n .s .7 !7~"^76 rj^XVTs~\\.3^ j .2 -i D .1 .1 o .1 .1 .3 . 2 .2 . 1 n s 311 = 4 .1 .1 .1 .1 .1 -1 .1 0 .1 B .1 .4 "-.S .7 f . 3 S' \.1~~ —— 2. t ' '.7 -- .4 .1 D .1 D .1 .1 .1 .4 . t . 1 .1 (1 = 4

Line 100 N

CKpole-D Ipole Array

o ra a

fî r^V. X\ s \ /

N s a - 25 m

^^*'' n " 1, 2. 3. 4 plot point

filterResistivity —— —— —— —— it

Metal Factor ———————— * * t* * * *

Logar i thinic Contours '- 1-5, 2. 3. 5, 7.5. 10,...

Ins-trumenls! IPTI. ]PV4 Trequencyl 1. D Hz

Operator : J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Grid, Sault Pro j eel,

Batachawana, Ontario.

Dal?: June \ 1990 N.T.S. 41 N/8

Scale: ] : 2500


41N08SE0B2B 2 .14308 RUNNALLS 360

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TOPCGRAPWT

RESISTIVITY

PHASE

m '' L ' -r ad)

0-3) E JjCJ^ 2-50 E 5^0 E 3^0 E 4*^0 E 4^50 E 5*00 E t 5^9) E r 6^00 E | 6-50 E f 7-CO E , 7*fQ C

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INTERPRETATION

METAL FACTOR t I p/res * 1DO)

Line 500 N

D;pole-D ipole Array

plot point

a s 25 m

r = 1. 2. 3. 4

F L 1 •ter ed Pr of i 1

Res i st l v ; tL, Polarization Metal Factor

Logar i thr ic Contours

filter

* *

* * *

-5. 2, 3, 5, 7.5. 10,

Instruments: IPT1, IPV4 Frequsncy! 1 . 0 Hz Opera! or: J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Gr Id, Sault Proj'eci

Batachavana, Ontario.

Dale! June \ 1990

Scale: ] : 2500

N.T.S. 41 N/8

MERTENS S MacNEIL LTDJftware lor t he Earth ScisriCBS. Toronto, CnaJj

41N08SE0020 2.14303 RUNNALLS

10.

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Q-SDE i+coE I+SOE 2+co E !^so E s+m E a+so E o+oo E a*so E s+co E S*SOE e*co E &-SQE 7*00 E 7+50 El————————l————i————l————————l————————l————————l————————l————————l————————l————————l————————I————————l————————l————————l————————l————.————l————————l————————l————————l————————l————————l————————l————————l————'————l————————l————————l————————l————.———H————————l————————l—————

f l i to- 13 13( [SI 2JK

0=1

0=4 lw

OSO E 1+00 E U5QE 2*O3 E 2'EO E 3^00 E 3+50 E 4*00 E 4+50 E 5*00 E 5+50 E 6*CO E 6+50 E 7-tflO E 7*50 E

fJHa- 8.7 9.1 13 i; 10 9.6 B.3 7.9 7.Z 9.6 1* 33 33 tt C S 17 ID IS 13 17 l] 10 10 ID 9.9 9.6 6.9 7,8

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TOPOGRAPHY

RFST^TI VTTY

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^p Ej t ^ I JOE | , 2^0 E ^'50 E ^ Wp E | , ^50 E , , 4+00 E- ^ ^J+SQE | , 5KOj 6KD E 6+50 E 7+CO E 7*50 E

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INTERPRETATION

METAL FACTOR

I Ip/res * 100)

9 .s .6 .1 o o -i .9 .1 o .z D n-4

L I ne 600 N

Olpole-D IpolQ Array

plot pa lil

a = 25 m

n - J. 2. 3. 4

F;liered Prof E L

Res i s I i v i t y — —— — ——PolarIzatIon —————————Heial Factor - —— - ——-

filler*

t ** 4 t

Logar i Ihm le Contour l- 5 ' 2. 3, 5, 7.5, 10,

Instruments! I PT1. I PV4 Frequency^ 1 , 0 Hz Operator: J.M.N,


INDUCED POLARIZATION SURVEYDoyle Lake Gr id, Sault Projecl P


Dale: June N J990

Scale! 1 : 2500

N.T.S. 41 N/8

MERTENS S MacNEIL LTD.GE050FT (In) Soflwjra for tha Earlh Setencas", "Toronlc, Canada

2.1430B RUNNALLS 410

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TOPOGRAPhTT

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INTERPRETATION

METfLt ip/res * 1DO)

Line 800 N

Dipole-D Ipole Array

V f - -\ x a s ib m

NV^ n - 1. 2. 3. 4p. l B t pa ; n l

F;ltered Prof I L.

Res Is t!v11u — — — ——Polsrlzat lor, ————————Mclfll Fictar - ——————-

filter*

* J*

Logar i-thrn icConiours L 1.5, 2, 3, 5, 7.5, 10.

Insiruments: IPT1, IPV4 Frequency: 1. D Hz Operator : J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Gr Id, Sault Project,

Batachawana, Qnlarto.

Dale! June \ 1990

Scale: J : 2500

N.T.S. 41 N/8

MERTEN5 S MacNEIL LTD.(In) Soft war w for the Ear I h 5c lances, Toronto. Canada

41Ne8SEe020 2 .143*8 RUNNALLS 430

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0+50 E WO E ?*COE 7+50 E

f:l ter LI filteraa s.? a.1 B.s a; as ic 13

MF

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f;]ia- .1 .1 O

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TOPCGRAPHY

RESISTrVITY

PHASE(m:l l i-r ad)

INTERPRETATION

METAL FflCTOR

{[p/res * LOO)

OSOFT ttml Soft-are for ]ha Earth Sc-eneos. Toronto, Canada

LCne 1 100 N

Dlpole-Dipole Array

plot peJ

a = 25 m

n * I. 2. 3. 4"

F.'l tered Prof l l '

Res is t lv ; ty POlar I za t Ion Metal Factor

filterf

W * 4 t *

^ v tbm l e Concurs L 1-5. . 3 , 5 , 7.5, 10,

Instruments! IPT1,Frequency: l.O Hz

Operator: J.M.N.


INDUCED POLARIZATION SURVEYSaul i Project

Batachawana, O n t ar fa.

Da-ie: June \ 1990

Scale! l : 2500

N.T.S. 41 N/8

MERTENS S MacNEIL LTD

41N08SE0020 2 .14388 RUNNALLS -4B0

10.

IP eo

40.

RES

40X-

^rTri.-^*.^

0-50 E 1*00 E 1+50 E 2*CO E 2*50 E 3*CO E J*50 E 4+CO E 4*50 E 5*CC E S-50 E 6*00 E 6*50 E 7*00 E 7*50 E

l* f li to-

OSO E I*DO E 1*50 E 2+CO E 2-50 E 3*CD E 3*50 E 4+OD E 1*50 E 5+CO E 5-SO E 6*00 E 6*50 E 7*00 E 7*50 E

f;lter li 8.7 6.7 3.6 5.1 7.1 6,5 6, S 10 11 E O O 41 t] C 19 I Z 7 .7 5 .3 6.4 7.8 B.I 1C 2D "C a 13 19 Filtsr

p i 1

1-1=2 ^rî-.

is i3\ ) s.;rIS 13 -^B." ' I.B- 1.2

45 33 33

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TOPOGRAPHY

PHASF

Itnll 1 !Tra

-j————i-

OSO E 6*00 E 5*50 E 7*00 E 7*50 Efilte

0=3

INTERPRETATION

METAL FACTOR

t ip/reS * 100)

Line 1200 N

D;pole-0;pole Array

a = tî m

n - 1. 2. 3.p 1 s 1 po I r. 1

Ftliered Prof I l

Resistivity —— — ——Polarization ——————————Metal Fa c tor -- — --—-

f i 11 e.-

* * * t *

Logar Ilhm ic Contours ' l' 5 ' 2- 3' 5- ;- 5 ' 1 0 -

Inslrumenis: IPT1, ]PV4 Frequency^ 1 .0 Hz Operator : J.M.N.


INDUCED POLARIZATION SURVEYSaul i Project

Batachawana, Gntarlo.

Dale: June \ ]990 N.T.5. 41 N/8

Scale: l : 2500

MERTENS fi MacNEIL LTD.GE05DFT (In) SoflKare for the^Tarih Scioncs*. Toronla. Canada

4IN08SEa02C 2.14308 RUNNALLS

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0-50 c 1*CO E 1'SO E 2*CO E Z-50 E J^CO E 3*50 E 4*CQ E 5-O) E 1-50 E 6-00 E e*SO E ?-QO E 7*33 E

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pj-|^c;p

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0-50 E J-Qji 1*50 E 2*tQ E 2'50 E 3-pOE 4tCO E 5*4tC E S-SO E 6*00 E 6-50 E 7^00 E 7*60 E

filter 0 0 0 J 1 .7 4.7 2.3

7.9

0=2 0=3 D c o n D o o o o D c o o

o o o .1 .1 o o o o o o o t D

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INTERPRETATION

METAL FACTOR

lip/res * 100)

'e ' ] * 2 ' *n ^ 4

LCne 1400 N

Dlpole-D Ipole Array

•^ i1 a E tb m

XV' n - 1. 2. 3.plo! polnl

F i l t er ed Pr of I l e s

Resistivity —— — ——Polar Tzat ioo —————————Helal Factor - — —— — — —— -

filter *

* * * * t

Logar ilhm ;c Contours -5- 2, 3, 5, 7.5. 10,

Inslruments: IPT1. IPV4 Frequency! 1 . 0 Hz

Oper atgr : J.M.N.

TRI ORIGIN EXPLORATION Ltd.

INDUCED POLARIZATION SURVEYSaul i Prpjec t

Baiachawana, Ontar Eo.

Dale: Jur,e \ 1990

Scale: 1 : 2500

N.T.S. 41 N/8

MERTENS S. MacNEIL LTD.GEIKOFT Tt^l Soft war a for t h* Ejrth Science, Toronto, Canada

2.14308 RUNNALLS 430

Mf jo.

ID-

IP RES ea ecco

40. 4000.

RES IP ,-BOOO so

-*000

1-03 E 1*50 E 2*CC E 2-50 E 3-X E 3-50 E 4--CO E 4. SO E S-OJ E 5*53 E fr*OD E 6+50 E 7*00 E 7*50 E

3!M Sif 28( 131 427 3275 JS33 7^37 131 2*1 33t filter

0-50 E 1-CO E 1*SO E 2-CO E 2*9D E 5^0 E 5*50 E 4--CO E 4*50 e S*OD E 5*50 E 6-K3D E 7*00 E 7+50 E

f;jt*- 7 6 '.S ".B 4.4 S.a 3.* 3-* 1.2 19 I3 IB IS l' 14 IS li 12 U ID a.S E. 9 S.9 li 39 W SO a i; I4 IS filter

17 n sJ1

MF -20

.10

o .a Lo

TOPOGRAPHY

RrÎSTTVrTY

pu/icp

m:ll!-ra

OSO E l*CCe 1'EOE 2*00 E J^ 3*CO E 3*50 E 4+CC E 4*50 E 5-CO E 5-SO E 6*00 E 6*50 E 7*03 E 7*50 E

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3.! 3.3-^ 1.8^-^ .1 .1 .J 00 = 4

INTERPRETATION

METAL FACTOR

lip/res * iOO)

Line 1 500 N

Dlpole-Q Ipole Array

n - 1. 2. 3. 4p 1 0 1 po i rt1

Filler ed Profiles

filterResistivity ———-Polar J zsl l or, ————————

Metal Fsc t or — — — -

Logar ! t hm^c Contours -5, 2, 3. 5, 7.5, ID.

Instruments: IPT1, IPV4 Frequency: 1 . 0 Hz Operator : J.M.N.


INDUCED POLARIZATION SURVEYSaul t Project

Batachavana, Ontario.

Dale: Jjne \ 1990

Scale! ] : 2500

N.T.S. 4 1 N/8

MERTENS S MacNEIL LTD.E05DFT (tint S0fU*ra'for~tha Esr lh Sclentas, Toronto. Cjnsdj

2.143CS RUNNALLS 500

MF IP RES20, eo ecoo \ RES IPt 8000 60

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filler tn 45*

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PHASE

'H I -r ad)

INTERPRETATION

FACTOR

tfp/res* 100)

GEOSOn (I'm) Sb?lwjra fer tha E*rih Selftncos; Toronto, Clanadi"

LCne 1 600 N

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plol psinln - 1. 2. 3. 4

Fill ered Profiles

Res 1st iv i ty

Metal Paclor

Looa- l t bm ic Contours

f:)ter*

* ** * *

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- l' 5 - 2' 3- 5- 7- 5 ' 1 0

Instruments: IPTl , IPV4 Frequency: 1 . 0 Hz

Operator: J.N.N.

TRI ORIGIN EXPLORATION Ltd.

INDUCED POLARIZATION SURVEYSaul 1 Rrojec t

Batachawana. O n tar {o.

Date: June \ ]99D

Scale: I : 2500

N.T.S. 41 N/8


41NB8SE0020 2.14308 RUNNALLS 510

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METAL FACTOR

(Ip/res * 1001

Line 1300 N

D!pole-D I pole Array

I±La ^ 25 m

F ; ] t e r- ~ d

. 1.5, 2, 3, 5, 7.5, 10,


INDUCED POLARIZATION SURVEYDoyle L ake GrCd, S ault P roject

Baiachawana, O n tar to.

Date: June \ 1990

Scale! l : 2500

N.T.S. 41 N/S

MERTENS S MacNEIL LTD.for the Earth Sclqnces, for onto, ~Cinad

41N08SE0B23 2.14308 RUNNALLS 530

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PHASE

INTERPRETATION

METAL FACTOR

tEp/res * IDD]

Line 1500 N

DCpoLe-DIpole Array

i l

\ 7N x -7C\ x a = Zb m

plol po t n'tn = l, 2. 3

Filtered Profiles

Resistivity —————PolarIzatIon ——————————Metal Factor ————————-

Logan i thru i c Contours

Instruments: IPT1, 3PV4 Frequency! 1.0 Hz

Operator: J.M.N.

f Ei ter


INDUCED POLARIZATION SURVEYDoyle Lake Grid, Saull Projecl,


Date! June V 1990

Scale: l : 2500

.T.S. 41 N/8

MERTENS 5 MacNEIL LTD

41N08SE0®2!9 2.1430B RUNNALLS B50

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19+50 E 20+50 E 21+00 E 21+50 E 22+00 E 22+50 E 23+00 E 23+50 E 24+00 E 24+50 E

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RESISTIVITY

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INTERPRETATION

FflCTOR

ip/res * 100J

Line 1700 N

DCpole-Dipole Array

l__l

i /\ s a = 25 rn

\/" n ^ I, 2, 3, 4plol po *n1

F l i i e r ed Profile:

Resistivity —————Polar izat ion —————————Metal Factor ——- —— —

f El ter

i t h m L cContours - 3' 5' 7' 5 ' 1 0

Instruments: IPT1. IPV4 Frequency- 1.0 Hz

Oper ator: J.M.N.


INDUCED POLARIZATION SURVEYDoyle Lake Grid, SauH Pro J eel,

Batachawana, On tar to.

Date: June \ ]990

Scale: ] : 2500

LT.S. 41 N/i

MERTENS 8 M acNEIL LTD.

4tNaeSE0020 2 .14308 RUNNALLS 570

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INTERPRETATION

METAL FACTOR

t Ip/res * 1003

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D t Array

l l

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f:lter*

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Instruments: I PT l, IPV4 frequency: l.Q Hz

Operator: J.M.N.



Batachawana, Ontar Co.

Date: June \ 1990

Scale: l : 2500

N.T.S. 41 N/8

MERTEN5 S MacNEIL LTD..es, Toronto, Canada

580

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RPT DESCRIBING REC PROSPECTING GEOL & IP SUR SAULT PROJ