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 1136265 SSM 1136266 SSM 1136267 SSM 1136268 SSM 1136269 SSM 1136270
SSM 1136282 SSM 1136283 SSM 1136284
SSM 1136285 SSM 1136286 SSM 1136287 SSM 1136288 SSM 1136289 SSM 1136290
SSM 1136302 SSM 1136303 SSM 1136304
SSM 1136305 SSM 1136306 SSM 1136307 SSM 1136308 SSM 1136309 SSM 1136310
SSM 111721 SSM 111722 SSM 111723
SSM 111724 SSM 111725 SSM 111726 SSM 111727 SSM 111728 SSM 111729
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
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GENERAL GEOLOGY. . f
PROPERTY MAP
Tri Origin Exploration Ltd.
PROPERY LOCATION
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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
0212 (04/91) Not* : Dans cette formula, kxsqu'il designs des personnes, le masculin eat utiKse au sens neutre.
1 li i fi 1 s i
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Cre
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you
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rt m
ay b
e cu
t bac
k. In
ord
er to
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imize
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adve
rse
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cts
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uch
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tions
, ple
ase
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cate
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ich c
laim
s yo
u w
ish
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rioriz
e th
e de
letio
n of
cre
dits
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ease
mar
k (*
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ne o
f the
follo
wing
:
1 . D
Cre
dits
are
to b
e cu
t bac
k st
artin
g w
ith th
e cla
im li
sted
last
, wor
king
back
ward
s.
2.
JS C
redi
ts a
re to
be
cut b
ack
equa
lly o
ver a
ll cl
aim
s co
ntai
ned
in th
is re
port
of w
ork.
3.
D
Cre
dits
are
to b
e cu
t bac
k as
prio
rized
on
the
atta
ched
app
endi
x.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied
your
cho
ice
of p
riorit
y, o
ptio
n on
e wi
ll be
impl
emen
ted.
Hot
el:
Exam
olss
of b
enef
icia
l Int
erac
t are
unr
ecor
ded
trans
fers
. oot
Jon
Mre
emen
ts. m
emor
andu
m o
f aor
eem
enta
. etc
.. w
ith re
aoec
tto
the
min
ing
clai
ms.
Not
* 2:
K
wor
k ha
s be
en p
erfo
rmed
on
pate
nted
or
leas
ed la
nd, p
leas
e co
mpl
ete
the
follo
win
g:
l cer
tify
that
the
reco
rded
hoM
er h
ad a
ben
efic
ial i
nter
est
in t
he p
aten
ted
or le
ased
land
at t
he t
ime
the
wor
k w
as p
erfo
rmed
.Si
gnat
ure
Date
S j 3 0 •j ?
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Numtfo
de
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travaux executes pour
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da
la
reserve
Ji 33
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e
S
33
1
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transferee
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LOT
cred
its q
ue v
ous
recla
mez
dan
s le
pre
sent
rapp
ort
peuv
ent e
tre re
duits
. Afin
de
dim
inue
r les
con
sequ
ence
s de
favo
rabl
es d
e te
lles
redu
ctio
ns, v
euille
z in
diqu
er '
ordr
e da
ns le
quel
vou
s de
sirez
au'
elle
s so
ient
app
lique
es 4
vos
cla
ims.
Veu
illez
coch
er (^
) I'u
ne d
es o
p tio
ns s
uiva
ntes
:
1. D
LOT
cre
dits
doi
vent
etre
red
uits
en
com
men
cant
par
le d
erni
er c
laim
sur
la li
ste.
2.
D L
OT c
redi
ts d
oive
nt e
tre r
edui
ts e
gale
men
t ent
re to
us le
s cla
ims
figur
ant d
ans
le pr
esen
t rap
port.
3.
D L
OT c
redi
ts d
oive
nt M
r* r
edui
ts s
eton
I'or
dre
donn
* an
ann
exe.
Si v
ous
n'av
ez p
as c
hoia
i d'o
ptio
n, la
pre
mie
re s
era
appl
lque
e.
Mot
* 1
- E
vam
nlM
d'ln
MrM
ai h
inA
flela
irM
: cM
alan
a, n
an M
iraote
tniM
- anta
ntM
*u
r dm
* ontlo
n*.
nrn
tnrn
laa
d'M
iten
te.
ate.
Mla
ttte
aux
clai
m*.
Not
* 2:
SI
d**
trav
aux
ont
ete
exec
utes
sur
un
terr
ain
falM
nt I'
obje
t de
lett
re*
pate
ntes
ou
d'un
bal
l, ve
uille
z re
mpl
lr ce
qui
sui
t:
Je c
ertif
ie q
u* le
titu
laire
enr
agis
tni
poss
edai
t un
int
eret
ben
eftc
ialre
sur
la
terr
ain
fais
ant
I'obj
at d
a to
ttras
pat
ente
s ou
d'u
n ba
il, a
u m
omen
t ou
las
tra
vm
iv n
nt
MA
Sign
atur
eDa
te
i 3 0 o
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M
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s -
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f\
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s i
s S
t1 It
J 5
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T X
*.
^x
fy
'-
^ \
(N
\
Ify 3*2
Nil
Bf!
3 * ifi? o|si
Cre
dits
you
are
cla
imin
g in
this
repo
rt m
ay b
e cu
t bac
k. In
ord
er to
min
imize
the
adve
rse
effe
cts
of s
uch
dele
tions
, ple
ase
indi
cate
from
w
hich
cla
ims
you
wish
to p
rioriz
e th
e de
letio
n of
cre
dits
. Pl
ease
mar
k (^
) on
e of
the
follo
wing
:
1. D
Cre
dits
are
to b
e cu
t bac
k st
artin
g w
ith th
e cla
im li
sted
last
, wor
king
back
ward
s.2.
D
Cre
dits
are
to b
e cu
t bac
k eq
ually
ove
r all
clai
ms
cont
aine
d in
this
repo
rt of
wor
k. v
3.
D C
redi
ts a
re to
be
cut b
ack
as p
rioriz
ed o
n th
e at
tach
ed a
ppen
dix.
In th
e ev
ent t
hat y
ou h
ave
not s
peci
fied
your
cho
ice
of p
riorit
y, o
ptio
n on
e wi
ll be
impl
emen
ted.
Mnt
ai*
FM
Hin
lea
of h
anaH
rial I
nter
est e
r* u
nrec
orde
d tra
nale
ra n
ntta
n M
ireem
*nt*
mem
oran
dum
at
enre
emen
t* *
ti*
wrt
hr^
M^r
tto
the
min
ing
clai
ms.
Not
e 2:
If
wor
k ha
* be
en p
erfo
rmed
on
pate
nted
or
ton
ed t
end,
ple
ase
com
plet
e th
e fo
llow
ing:
l cer
tify
that
the
rec
orde
d ho
lder
nad
a b
enef
icia
l Int
eres
t in
the
pate
nted
or
leas
ed la
nd a
t the
tim
e th
e w
ork
was
per
form
ed.
Sign
atur
eDa
te
NumaVo d* rapportsur 1** travaux executes
pour ('affectationd* la reserve
Numero d* claim
M 36 282-
S/ 362*3
/t 36
/S 3 6 23 J
1134,213
i J 36
Nombre d'unites
daeWma0241 (06*1)
Valeur des travaux devaluation
executes sur ce claim
/oo'
/oo
too'
too
*2ooo
* 2 oo ^~ i
*3ft*.'
/QO
/O*'
^
f 1&&
*
JO*'
J 06 '
too'
y'
2 f 000
/oo
Valeur affectee
ace claim
Oo^r
^
*.
n
l*
*
*
M
"
M
u-
*""li
** u4 "
Vstour total* tf*a Vatow total* o** travaux travaux *x*cut*s qul i *t* affect**
Valeur transferee
dece claim
tt 3 6
UK'
Sod '
/l 36 '
TotalAMMM^AA^Auaiiaiaiv
Reserve : travaux a, reclamer
a une date ulterieure
Raatrva total*
P ~8*?si.0 —(0—.
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si! Claim Number
(see
Note
2)
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f
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1 8. 1
Cred
its y
ou a
re c
laim
ing
in th
is re
port
may
be
cut b
ack.
In or
der t
o m
inim
ize th
e ad
vers
e ef
fects
of s
uch
delet
ions,
pleas
e in
dica
te fr
om
which
cla
ims
you
wish
to p
rtoriz
e th
e de
letio
n of
cre
dits.
Plea
se m
ark
(^)
one
of th
e fo
llowi
ng:
1. D
Cre
dits
are
to b
e cu
t bac
k st
artin
g wi
th th
e cla
im li
sted
last,
work
ing
back
ward
s. 2.
D C
redi
ts a
re to
be
cut b
ack
equa
lly o
ver a
ll cla
ims
cont
aine
d in
this
repo
rt of
wor
k. 3.
D C
redi
ts a
re to
be
cut b
ack
as p
rioriz
ed o
n th
e at
tach
ed a
ppen
dix.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied
your
cho
ice o
f prio
rity,
opt
ion
one
will
be im
plem
ente
d.
U^t. 4
. f
~^m
*m
lmm
m
t km
*.m
llm
tml Im
l m
m l tt m
m*
l..... . o
jj. d
tm
m^*lm
*m
m
mtU
^ft *m
m*****rti*
m
**m
***rm
inttu^ o
* m
m*m
mm
m^m
*tm
~*o
^.1
*1. -.--. m
*
Not
e 2:
H
wor
k ha
* be
en p
erfo
rmed
on
pate
nted
or
leas
ed l
and,
ple
ase
com
plet
e th
e fo
llow
ing:
l cer
tify
that
the
reco
rded
hol
der
had
a be
nefic
ial i
nter
est i
n th
e pa
tent
ed
or te
ased
lend
at t
he ti
me
the
wor
k w
es p
erfo
rmed
.Si
gnat
ure
Date
i j
vt S VI | ^,
*
m
ff n fi li Valeur
tofct
des
qui a tt*
affec 1 1^ ? S
\ \ \
-M N
•v.
SJN
.^ si
N-w ^
.
^^ M —
^^ M (At
.^
^ SJ Ki r*
^ S ^^
^ HJ O
^ ^
•s.. oo
V.
V.
-s.
GN
X
t,{. l Numero
de
claim a.
z
c" o
li
'
v
J0 \ * ^
N x ,
V r
.to \ r*
K) \ 0 \ .
x ^
x X
| X T
^^D ^Wl \ x
u*
rf\ X
M x •*
r s
Vvo
\ k
N \
KJ ^E x 8 \
Valeur
des
travaux d'evaluatio
executes sur
ce claim
3
tiff
9
i V
j? lix
Vrt \
vn\
OL&
^^v \
x.
Mi
(N
V\
(N
\X
(Nv\
\Valeur
transferee
de
ce
claim .J, ss * s-
?2
a.* irve :
reclamer
i date
eure
Lea
cred
its q
ue v
ous
recla
mez
dan
s le
pres
ent r
appo
rt pe
uven
t etre
redu
its. A
fin d
e di
min
uer l
es c
onse
quen
ces
defa
vora
bles
de te
lles
redu
ctio
ns, v
euille
z in
diqu
er I'o
rdre
dan
s le
quel
vou
s de
sirez
au'e
lles
soie
nt a
ppliq
uees
a v
os c
laim
s. V
euille
z co
cher
(^)
l' une
des
op
tions
sui
vant
es :
1. G
Les
cre
dits
doi
vant
etre
redu
its e
n co
mm
enca
nt p
ar le
der
nier
cla
im s
ur la
list
e.2.
D
Les
cre
dits
doi
vant
etre
redu
ita e
gale
men
t ent
re to
us le
s cla
ims
figur
ant d
ans
le pr
esen
t rap
port.
3.
D L
aa c
redi
ts d
oiva
nt e
tre re
dutts
set
on I'
ordr
a do
nna
en a
nnex
e.Si
vou
s n'
avez
paa
cho
iai d
'opt
ion,
la p
rem
iere
ser
a ap
pliqu
ae.
Mnt*
1 -
rr
anin
laa r
i'ln
fArA
ta h
^n
^flr la
lraa -
raaaln
na n
rm a
nra
nla
tria
a
cn
ten
tAB
Bur
HA
* nntlnn*
nm
tnfn
tmm
li'm
ntm
ntm
•
tt*
r+lm
tttm
ux
clal
ma.
Not
e 2:
S
I d
a* t
rava
ux o
nt a
t* e
xecu
tea
aur
un t
erra
in f
alsa
nt I
'obj
et d
e le
ttre
s pa
tent
es o
u d'
un b
all,
veui
llez
rem
pllr
ce q
ui a
uK:
Je c
ertif
ie q
ue l
* tit
ulai
re e
nreo
jstr
e po
ssed
ait
un in
tere
t be
nefic
iaire
sur
le j
Sig
natu
re
terr
ain
fais
anl
I'obj
et d
e le
ttres
pat
ente
s ou
d'u
n ba
il, a
u m
omen
t ou
les
lD
ate
10
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PLAH
G-2420TOWNSHIP
RUNNALLS
-t
tt~ L uF ISSUE
--3 8 1991
XT STE. MARIE "^ORDER'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. INF^IRMATIONf IN THF '^TATUi, "r T H(
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SAULT PROJECT — ONTARIORUNNALLS TOWNSHIP
DOYLE LAKE GRID
GEOLOGY^ /^f^^ , ^^^— ' f-
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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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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 \
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2+50 E 3*00 E 3*50 E 4+00 E
filter 1212132031*593631 filter PHASE
0=2 9.5- ——— f^i^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
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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.
TRI ORIGIN EXPLORATION LTD.
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~
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•JT^XJ L HTTJJ l.
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n*l 17K -xxlEBS,vv tfK-~xJEe 0=1 lohm-m) ^//\^^i^
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)
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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
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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.
TRI ORIGIN EXPLORATION LTD.
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
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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
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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,
TRI ORIGIN EXPLORATION LTD.
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
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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
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TOPOGRAPHY
RESISTIVITY
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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.
TRI ORIGIN EXPLORATION LTD.
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
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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
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fllte-
n=2
0 O O .1 .1 O
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.^ 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.
TRI ORIGIN EXPLORATION LTD.
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
MERTENS S MacNEIL LTD.
41Ne8SE0828 2 .14308 RUNNALLS 330
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TOPCGR^PH'f
Q+5C E l+m E 1-50 E 2+CC E 2+50 E JtED E 3+50 E 4^0 E 4+50 E 5.00 E MO E 6+00 E &+50 E 7+00 E 7+SD E 6+03 E
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
1^=1 eSi , l*. J-/49B ——— 1=6.^ /PJ y \TCIJ "^'^txx'f ^^ ^ _ " ^ f (^//fifflS^r '5^— 3^^f\ t ^ L ^ Ml^-- S( /"/ffi i ** X 1 fv ~*-^Si// P3 ^^^'S' ^'^^O^JS-^-S1'^'/ 3Sa n^l tohrn-m]
RS 2 iw w j/j&'y s '5- J ) S?:^^^* <7^l(7 — •efeo^V?9; v^ *'K y ,'^ //ffif^Ss2^^~lI7*~^. ^wsN? ^s^!^ S*J— ~~^. 37V Ss^J /^s ZHI^VBCTI/'MSS} roi/^ifo 7^^-^M^--5S7 n E 2
^=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' ' ' fiff^is* 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'^-^A^ — y —— a.^ y y y ti l= l ( mill J-rndl
n^2 9.5 13 C^r~""~^'Cir B ^-^iA' (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 /^^i7 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 ( fr^O 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^^iir — 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'*^^i.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
\ f^ -" oc-
^\'' 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.
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYDoyle Lake Grid, Sault Project,
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-~^iiy J6564? /^\-^ ls} /®V\ C^^\ ^^X i^^iw\ ^y/^1 3e*0 asas^^Sj y I&^^IBIS^ t ^4JV\ ?* ^V "? (^"^V,-^ 2?" l/* '"///f^\. ^J //®'x5-)^4 n = ^ nsfl w * i^r- sis E4/ A* ' iw — "~ iac^- aa IEK -^U^^^iw --'^xoa^-ses si? '^raes ' 2S* ^-is/-' •KS^~^Sr::^--'sz*~~- sis i* •x *w ' i*^- ISK f -^wt^-voA -^aaf'-'^ii ' 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 /^IS) 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 x^io 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
f^i 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.
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYDoyle Lake Grid, Sault Pro j eel,
Batachawana, Ontario.
Dal?: June \ 1990 N.T.S. 41 N/8
Scale: ] : 2500
MERTENS S MacNEIL LTD.
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.
TRI ORIGIN EXPLORATION LTD.
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
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0=1
0=4 lw
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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,
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYDoyle Lake Gr id, Sault Projecl P
Batachawana, Ontario.
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.
TRI ORIGIN EXPLORATION LTD.
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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TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYSaul i Project
Batachawana, O n t ar fa.
Da-ie: June \ 1990
Scale! l : 2500
N.T.S. 41 N/8
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TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYSaul i Project
Batachawana, Gntarlo.
Dale: June \ ]990 N.T.5. 41 N/8
Scale: l : 2500
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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
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METAL FACTOR
lip/res * iOO)
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n - 1. 2. 3. 4p 1 0 1 po i rt1
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filterResistivity ———-Polar J zsl l or, ————————
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Instruments: IPT1, IPV4 Frequency: 1 . 0 Hz Operator : J.M.N.
TRI ORIGIN EXPLORATION LTD.
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
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GEOSOn (I'm) Sb?lwjra fer tha E*rih Selftncos; Toronto, Clanadi"
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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
MERTENS S MacNEIL LTD.
41NB8SE0020 2.14308 RUNNALLS 510
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TRI ORIGIN EXPLORATION LTD.
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
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f Ei ter
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYDoyle Lake Grid, Saull Projecl,
Batachawana, Ontario.
Date! June V 1990
Scale: l : 2500
.T.S. 41 N/8
MERTENS 5 MacNEIL LTD
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i t h m L cContours - 3' 5' 7' 5 ' 1 0
Instruments: IPT1. IPV4 Frequency- 1.0 Hz
Oper ator: J.M.N.
TRI ORIGIN EXPLORATION LTD.
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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TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYDoyle Lake Grid, Sault Project,
Batachawana, Ontar Co.
Date: June \ 1990
Scale: l : 2500
N.T.S. 41 N/8
MERTEN5 S MacNEIL LTD..es, Toronto, Canada
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