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S2FI6NE8226 2.1349) PICKEREL 010
2.13491»H '-*V
SIOUX PROJECT
SIOUX LOOKOUT ONTARIO
Assessment Report describing Geology, Induced Polarization Surveying and Diamond Drilling, Sioux Project
Sioux Lookout, Ontario
LANDS SECTION
Tri Origin Exploration Ltd.
Robert I. Valliant August 10, 1990
Sioux Project
Sioux Lookout, Ontario
Assessment Report describing Geology, Induced Polarization Surveying and Diamond Drilling, Sioux Project
Sioux Lookout, Ontario
Introduction
This report describes work completed on the Sioux property during the period August 31, 1989 to February 15, 1990 which qualifies for assistance under O.M.I.P. grant designation number OM89-006. The report is divided into three parts: Part A - Property prospecting and reconnaissance; Part B - Geophysical surveying; and Part C - diamond drilling. Illustrations include two property location maps, plan map of grid, I.P. anomalies and diamond drill hole locations and diamond drill hole sections.
Property Location and Description
The Sioux property is located 20 miles southwest of Sioux Lookout, Ontario in the southwest corner of Pickerel Township (fig. 1) and falls under the jurisdiction of M.N.R. administrative district of Sioux Lookout in the Patricia Mining Division. The property is bordered by highway 72 near its northwest boundary which provides an all-weather means of access. Pickerel arm of Minnitaki Lake covers the southeast part of the property.
The Sioux property consists of 26 unpatented mining claims registered in the name of Tri Origin Exploration Ltd. No option agreements or contractual obligations apply to this property. The following is a list of claims which comprise the property:
Pa.1102278 Pa.1102279 Pa.1102280 Pa.1119522 Pa.1119523 Pa.1119524
Pa.1119462 Pa.1119463 Pa.1119464 Pa.1119465 Pa.1119466 Pa.1119467
Pa.1119468 Pa.1119469 Pa.1119470 Pa.1119471 Pa.1119472 Pa.1119473
Pa.1119474 Pa.1119475 Pa.1119476 Pa.1119477 Pa.1119478 Pa.1119479
Pa.1119480 Pa.1119481
Line Cutting
Linecutting was conducted on the property during September 1989 and was completed and lines extended across Minnitaki Lake during January 1990. Baseline was oriented at 240 degrees parallel to strike of underlying rock units and was chained and picketed at 100-foot intervals. Lines were oriented at 150 degrees at 400-foot separations and were chained and picketed at 100-foot stations. Lines closely follow those used by Braeswood Exploration Ltd.
during 1981 and 1982. Grid was chained and picketed on Minnitaki Lake during January 1990. Lake lines extending north to the shore of the lake did not always encounter bush lines directly in their path. Discrepancies in location were generally 25 feet or less, however, in the case of ice lines 32+OOE, 36+OOE and 40+OOE, it was found that bush lines were actually at 31+OOE, 35+OOE and 39+OOE respectively and have been labelled according to their bush locations. Geophysical surveying of these lines, for example: L39+OOE, was conducted on L.39+00 in the bush, then slowly "jogged" at the lakeshore to L.40+OOE where it was continued across the lake.
Part A: Property Prospecting and Reconnaissance
Introduction
Reconnaissance traversing and prospecting was conducted on the Sioux property, over a period of 8 man-days, to determine the geological environment which hosts gold mineralization and to assess the nature and style of this mineralization. Additionally, diamond drill core from previous exploration programs (Kidd, 1981, 1982) was relogged and where necessarysampled, over a period of 8 man-days, to further verify results from previous work and further delineate controls on mineralization.
Results
Reconnaissance traversing and prospecting at the Sioux property resulted in gaining an understanding of the general geology of the property, providing preliminary assessment of known gold-bearing sulphide occurrences, obtaining preliminary geochemical data for sulphide occurrences and preparation of a base map outlining claim location, grid location and general geographical features.
Bedrock is best exposed along the shore of Minnitaki Lake. Elsewhere rock exposure is limited to small ridges north of the baseline and at the west part of the property. A swamp extends from the bay in Minnitaki Lake at line 0+00 in a southwesterly direction across the property. In general overburden is sand-rich with a well developed humus layer and varies in thickness from a few feet to almost 200 feet at Braeswood drill hole 81-3 (Kidd, 1981) L.28+OOW, 5+OOS. Average overburden thickness encountered by Braeswood drilling was approximately 25 feet.
Rock units strike 240 degrees and dip 080 degrees north and comprise an interlayered sequence of metamorphosed, mafic and felsic volcanic rocks in contact with a monotonous sequence of sedimentary rocks to the south. Primary textures are well preserved, however, a conspicuous foliation is developed parallel to layering in interflow units and fine-grained tuffs which is defined by parallel alignment of chlorite and sericite. The
northernmost part of the property is underlain by a mafic volcanic unit which is both pillowed and massive flows, intruded by narrow feldspar porphyry dykes and sills, and separated by interflow mafic tuff which in places contains abundant magnetite, iron-carbonate and pyrite. A sample of this iron-rich mafic tuff (Echo 89-2) was determined to contain less than 1 ppb Au by FADCP analysis. Narrow pyrite and quartz veinlets and beds in mafic volcanic rock were determined to contain between 10 and 58 ppb gold (samples Sioux 3,18106,18107,18108).
Felsic volcanic rock forms a unit of interlayered quartz-crystal rich ash flows, sericite-schists, massive quartz and feldspar porphyritic flows or intrusive rocks, intercolated chloritic, mafic tuff and coarse-grained fragmental rock consisting of feldspar porphyry fragments in a chloritic and pyritic matrix. The felsic unit is approximately 1200 feet thick, at the central part of the property and is believed to thicken to the southwest. A sample of quartz feldspar porphyry from Minnitaki lake was found to contain 7 ppb gold (sample 89-3) and pyritic interflow material within sericitic felsic tuff was found to contain 41 ppb gold (sample 18102)
Chert containing abundant tourmaline, magnetite, pyrrhotite, and pyrite forms a unit up to 100 feet thick, extending along the southern contact of the felsic volcanic unit. Chert is fine grained, recrystallized white quartz containing narrow seams of black tourmaline and magnetite, disseminated pyrite and pyrrhotite and layers of massive pyrite and fine-grained magnetite ranging from 1/2 inch to 20 feet in thickness. This unit was intersected in diamond drilling with 2 holes in 1950. (El pen Ray Mines Ltd., 1950) and 4 holes during 1981/82 (Kidd, 1981, 1982). Magnetite content of the chert increases in a westerly direction, whereas pyrite content increases to the east and south where, in places, it forms a "cap" of massive sulphide along the southern boundary of the chert. Sampling of the chert indicates that this rock is anomalous in gold with values averaging approximately 25ppb (samples 18109,18110,18111,18112,18114,18115) but ranging to 552 ppb (samples Sioux 1,18103,18105). Gold content of chert increases with pyrite abundance and is reported at up to 0.05 o.p.t. (El Pen Ray Mines Ltd., 1950) and 0.04 o.p.t. (Kidd, 1982). Gold content of a selected massive sulphide sample was 1100 ppb (sample Sioux 2) as confirmation of previous work. This unit remains largely untested along the length of the property.
A monotonous sequence of well-bedded and graded greywacke forms a unit in contact with the chert and underlying the southeastern part of the property. Grading, scour marks and rip-up clasts within these sedimentary rocks indicate south-facing directions. Beds average 5 to 10 feet thick and some of the finer grained layers are graphite-rich. Where observed greywacke was devoid of sulphide mineralization.
Recommendations
The following are recommendations of work to be conducted based on preliminary reconnaissance surveying at the Sioux property:
1. Geological mapping2. Trenching of chert unit where overburden thickness
permits3. Induced Polarization surveying to delineate massive and
disseminated sulphide within the chert unit and adjacent rocks
4. Diamond drilling
Part B: Geophysical Surveying
Introduction
Induced Polarization surveying was.conducted during January, 1990 by Mertens & MacNeil Geophysical Ground Surveys Ltd., of Guelph, Ontario. Field crew consisted of:
R. Mertens - Guelph, OntarioJ. MacNeil - Sydney, Nova ScotiaK. MacNeil - Sydney, Nova ScotiaD. Brown - Dominion, Nova ScotiaB. Campbell - Frenchvale, Nova ScotiaD. Gouthro - Frenchvale, Nova Scotia
Survey Method
A total of 20.4 line miles of dipole-dipole array I.P. surveying was completed using a Phoenix phase system. Transmitter was a Phoenix IPT1 operating at a frequency of 1 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 100 feet with readings taken at n value separation multiples of the a- spacing of 1, 2, 3 and 4. Resistivity was expressed in ohm-meters and phase values expressed in milli-radians. A "metal-factor" was calculated for each data point using the formula MF=(Phase divided by resistivity) x 100. Psuedosections were plotted for each line surveyed at a scale of 1:2400 and anomalies were transferred to a property plan map (fig.3).
Results
I.P. anomalies were determined primarily based on their phase response and are illustrated on attached IP plan map. 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. Four of these anomalies stand out due to the magnitude of their phase response:
Anomaly 1 - L.31+OOE to L.39+OOE, approximately 18+OON- continuous along strike with moderate phase and high resistivity
Anomaly 2 - L.0+00 to L.20+OOE, approximately 8+OON- continuous along strike with moderate phase
at its center grading northeast and southwest to weak phase response, low to moderate resistivity
Anomaly 3 - L.52+OOW to L.64+OOE, from approximately 12+OOS at the southwest, crossing the baseline at L.8+OOE and extending to 4+OON at the northeast part of the property
- discontinuous along strike from weak to very strong phase response, complex resistivity with very low resistivities in places flanked to the north by very high resistivities.
Anomaly 4 - L.44+OOE to L.56+OOE, approximately 22+OOS- continuous along strike, moderate phase, low
resistivity
Discontinuity of anomaly 3 along the length of the property and distribution of other I.P. anomalies leads to the interpretation that structural discontinuities most likely faults oriented at 120 degrees may crosscut the property. The swamp south of the baseline and west of line 20+OOW has apparently inhibited transmitter current from reaching bedrock 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 3 have been drill tested and, where intersected, it is known to contain gold-bearing massive sulphide.
2. Trenching of I.P. anomalies is recommended where overburden thickness permits.
Part C: Diamond Drilling
Introduction
A 2000-foot diamond drill program was contracted to Tonto Drilling of Burnaby, B.C. Drilling was commenced January 31, 1990, using a Longyear 38 drill and BQ diameter rods. Drilling was conducted in two, twelve-hour shifts per day with crew as follows:
D. Hosking, North Bay - Operations ManagerV. McLeod, Winnipeg - ForemanJ. Leask, Winnipeg - RunnerJ. Law, Winnipeg - HelperJ. Christensen, Winnipeg - Helper
Drillhole Locations and Results
Three diamond drill holes were completed for a total of 1854 feet. These holes were located to drill I.P. anomaly 3, especially where the anomaly extended under the cover of ice into Minnitaki Lake.
D.D.H. Location Azm. Incl. Depth
S 90-1 L.8+OOE, 2 + 50N 146 -55 525S 90-2 L.11+60E, 2 + 50N 148 -55 523S 90-3 L.4+OOW, 2 + OON 146 -60 806
Drill hole S 90-1 was collared on Minnitaki Lake. Water depth was 8 feet and a total of 76 feet of casing was used to penetrate bedrock. Upon completion the hole was cemented from a plug set at 345 feet down hole for approximately 70 feet and casing was pulled. The hole intersected felsic lapilli and crystal tuff for the first 334 feet, sulphide-rich tuff and chemical sedimentary rock for 120 feet and greywacke for the remaining 71 feet of the hole. Graded beds, scour marks and rip-up clasts indicate a south facing direction for the rocks intersected. Inspection of I.P. psuedosections and diamond drill section (fig. 4) indicates that the sulphide-rich rock dips 80 degrees north.
Drill hole S 90-2 {fig. 5) was collared at the edge of Minnitaki lake with water depth of less than 2 feet and a total of 10 feet of casing necessary to penetrate bedrock. Felsic lapilli and crystal tuff were most abundant in the first 284 feet of the hole overlain to the south by sulphide-rich tuff and chemical sedimentary rock for 152 feet which in turn was overlain by greywacke to the end of the hole. Sulphide-rich rock has been categorized into four types as described in drill logs (appendix 1);
1. Upper semi-massive sulphide unit2. Chert3. Lower semi-massive sulphide unit4. Chloritic schist
The lower semi-massive sulphide and chloritic schist were not apparent as corealatable units in earlier diamond drilling conducted at the west part of the property by Braeswood Exploration Ltd. (Kidd, 1981,1982). Also, magnetite is much less abundant in rocks intersected during the present program as compared to that in drill core examined from earlier Braeswood programs.
Drill hole S 90-3 (fig 6) was collared in swampy ground at the west edge of Minnitaki Lake with a total of 144 feet of casing necessary to penetrate bedrock. Felsic lapilli and quartz crystal tuff were most abundant in the first 626 feet of drill core and were overlain
to the south by chloritic tuff, schist and a fault zone to 663.6 feet downhole. Chert with narrow seams or layers of magnetite and veinlets of pyrrhotite was intersected to 724 feet downhole followed by interbedded massive sulphide and chert to 730 feet. The remainder of the hole was well bedded greywacke.
Recommendations
Gold-bearing massive sulphide mineralization was indicated from previous work on this property and new discoveries were made during the present program. Additional exploration is necessary to further understand the nature of these gold occurances and to test other undrilled geophysical anomalies. Recommendations are;
1. Geological mapping of the property and trenching of I.P. anomalies where possible.
2. Detailed I.P. surveying at 200 foot line spacing.3. Shallow diamond drilling along strike of known sulphide
occurances and to test undrilled anomalies.4. Reconaisance deep diamond drilling and down-hole geophysics
down dip from known sulphide occurances.
3. Lower semi-massive sulphide unit4. Chloritic schist
The lower semi-massive sulphide and chloritic schist were not apparent as corealatable units in earlier diamond drilling conducted at the west part of the property by Braeswood Exploration Ltd. (Kidd, 1981,1982). Also, magnetite is much less abundant in rocks intersected during the present program as compared to that in drill core examined from earlier Braeswood programs.
R.§.commendat.io.ns.
Gold-bearing volcanogenic sulphide mineralization was indicated from previous work on the property and new discoveries were made during the present program. Additional exploration is necessary to further understand the nature of these gold occurances and to test other undrilled geophysical anomalies. Recommendations are;
1. Geological mapping of the property and trenching of I.P. anomalies where possible.
2. Detailed I.P. surveying at 200 foot line spacing.3. Shallow diamond drilling along strike of known sulphide
occurances and to test undrilled anomalies.4. Reconaisance deep diamond drilling down dip from known
sulphide occurances.
sub-
\
Linecutting: Contract to L.Carpenter Sioux Lookout, Ont.
13.56 miles @ $240/mile 9.7 miles 120/mile tags,etc............... .sub-total...$4469.55
Prospecting: R.Valliant, D.Sheehan Outcrop and drill core examination, map and report preparation.
22 days @ $300/day..............sub-total...$6600.00
Geophysical Surveying:Contract to Mertens MacNeil Geophysical Surveys Ltd. Guelph, Ont.
20.4 miles @ $2352.70/mile......sub-total...47995.00
Diamond Drilling:Contract to Tonto drilling Burnaby, B.C.
2000 feet @ $17/ft. mobilization $5000 moves, non-operating time as per contract. Assaying, reports , etc . . .
1048 feet $27/ft..............sub-total...28296.00
r:
N.Y.
KILOMETRES
Tri Origin Exploration Ltd.
Sioux Project1 - Locod\ov^ Map
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S2F16NE8226 2.13491 PICKEREL 020
i " ™ ~~£. I • •acNeilrteriGtophyWal Ground Survty^Od.
TRI ORIGIN EXPLORATION LTD.
78 ASQUITH AVENUE , TORONTO , ONTARIO.
TECHNICAL AND LOGISTICAL REPORTFOR THE!
INDUCED POLARIZATION SURVEYMINNITAKI LAKE
SIOUX LOOKOUT,ONTARIO
60x1682, Quelph Ontario N1H 629 • Box 1083, Sydney Nova Scotia B1P6J7
rt ens aclSleilQcophytaal Ground SurvtyuDd.
MERTENS & MacNEIL GEOPHYSICAL GROUND SURVEYS LTD. was contracted
by Dr. R. Vaiiiant of TRI ORIGIN EXPLORATION LTD. , 78 Asquith Avenue ,
Toronto , Ontario, to carry out an Induced Polarization survey on their
Minnitaki Lake Property near Sioux Lookout , Ontario. Mertens & MacNeil
carried out this survey between January 6, 1990 and February 1, 1990.
PARAMETERS \\\\\\\\\\\\\
The parameters of the survey were as follows :
1. Number of miles : 20.4 miles ( 33.0 km. )
2. Array : Dipole - dipole
3. Spread : " a " = 100 feet
4. Dipole Seperation : " n " = 4
5. Method : Phase ( with reference cable control)
6. Frequency : 1.0hz.
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 : Land : Stainless steel rods
Lake : Aluminium foil and wire
Box 1682, Guelph Ontario N1H 6Z9 • Box 1083, Sydney Nova Scotia B1P6J7
lacGtoph^cal Ground SurvtywOd.
ACCESS \\\\\\\\\
The access to the grid was by truck along Highway 72 approximatly
25 miles south of the town of Sioux Lookout. Snowmobiles were used for
access to Minnitaki Lake and the south end of the grid.
MOBILIZATION \\\N\\\\\\\\\\\
The crew and equipment were mobilized from Guelph , Ontario by truck
to Sioux Lookout , Ontario.
CREW MEMBERS \\\\\\\\\\\\\\\
JACK MacNEIL P.O. Box 1083, Sydney , N.S. B1P 6J7
DALE BROWN Dominion , N.S.
DAVE GOUTHRO Frenchvale , N.S.
RON MERTENS P.O. Box 1682, Guelph , Ontario. N1H 6Z9
KEN MacNEIL Sydney , N.S.
BLAISE CAMPBELL Frenchvale , N.S.
Further information may be obtained from:
MERTENS & MacNEIL Geophysical Ground Surveys Ltd.
P.O. Box 1682 Guelph , Ontario.
N1H 6Z9 519X836-3475
Box 1682, Guelph Ontario N1H 6Z9 Box 1083, Sydney Nova
for acNEIL
ens
FFII ORIGIN EXPLORRTION LTD.
Drill Hoia Survey Data
Projact SIOUX
Drill hole nuMber: S98-1 Data: Fab. 15, 1998Drill ad by: fonto drilling Data startad: Fab. 12, 1990Logged by: R. Valliant Data cortplatad: Fab. IS, 1998Cora siza: BO
Purpose: To intersect I.P. anonaly L.8E,8*58S
Connants: Second hole in progran used field labal S90-1Collarad on ice, 6 ft. water, approx. 68 ft. lake sadi riant Casing pullad, hoi a cenontad with 2 bags cowent fron a plug sat at 315 faet.
Collar location: Lina ; 8+66 E Station ; 2+50 N Elevation; lake
Drill hole surveys:
Survey typa conpass acid
Dapth collar
525
ft/« flziMuth ft H6 ft
Dip-55-53
FroH
e.e76.8 10?. 8
112.8
283.8221.8
To
18?. 8 112.8
283.8
221.8335.6
333.6 356.8
356.8 365.8
365.8 368.8
368.8 116.5
116.5 151.5
151.5 525.8
SIOUX
-Description-
Holt No: S90-1
Sanple Fron
CasingFelsic lapilli tuff, sericitic, 186 to 18? frag. 2 CH.Mafic lapilli tuff, chloritic, wall banded, badsfroii 6 in. to 3 ft. thickFelsic quartz x-tal tuff, abundant lapilli, qtz. x-talsfine grained, sub-angular, foliated, qtz. vain 192 to 193.Mafic tuff, chloritic, foliated and crudely banded.Fftlsic quartz x-tal lapilli tuff, variable, in placeshatarolithic frag, rock with subround to lanticulargray frags, to >1 en long, foliated and crudely bandadfin* grained bads with 22 fine diss. py. at 291to 296, 288 to 288.2, 313.2 to 311. Faldspar porphyryarid tuff frags, nor a sari ci tic with appla graari colourfroH 328 to 333.6, abundant po. and py. as lanticularpatches 322 to 326.Chloritic lapilli tuff. Minor qtz.-carb. veinlats andfractures, fina grained diss. py. 12.Schist, chloritic, vary foliated, abundant qtz.-carb.frags, or boudinaged layers, fina grained diss. py Z ','.Louer sulphide unit, sam-Massive py. nad. to finagrained, vuggy, Mixed Hith irregular patches of chertarid Massive chlorite.Chert, py.-rich as irregular bands and veinlats inbrecciated chert to 375 ft., uell bedded, siliceousto 118 ft., chart breccia with fine chlorite and py.froM 37? to 378.5, po-rich chert to 68 as coarseveinlats and clots 117.5 to 121 and 110 to 116.5, topof unit contains More abundant irregular qtz. veins.Upper sulphide unit, py. as fina to vary fina grainedbeds, irregular contacts interbeddad uith grayuackalayers to 5 in. thick and lesser chert to 2 in. thickGrayuacke, Moll bedded, rip-up clasts and scoursindicate tops south, very fine grained with seaMS ofpy. parallel to layering 151 to 161 ft.
To Length ft.
Ru ppb
Ru oz./ton
18127181281812918138181311813218133181311813518136
18137181381813918118
331.8336.8311.8316.8351.8356.8361.8366.8368.8372.8
139.8113.8117.8151.8
336.8311.8316.8351.8356.8361.8366.8363.8372.8375.8
113.8117.8151.8151.5
2.85.85.85.85.85.85.82.81.83.8
1.81.81.83.5
152118
nilnil
?17
16681
368
168333583711
21
188
535638
TRI ORIGIN EXPLORATION LTD.
Drill Hoi a Survey Data
Projact SIOUX
Drill hoi a nunbor: S99-2 Data: Fab. 13, 1998Drillad by: fonto drilling Data startad: Fab. 6, 1998Logged by: R. Valliant Data eonplated: Fab. 12, 199BCora size: BCI
Purpose: To intersect I.P. anonaly L.12E,9+99
Consents: First hoi a in progran, usad fiald labal S98-2. Tan faat of casing left in hoi a.Collared on ica as closa to shoralina as possibla. Lata start dua to nunarous Mechanical problens.
Collar location: Lina ; 11+69 E Station ; 2+50 N Elevation; lake
Drill hole surveys:
Survey typa coHpass acid
Depth collar
•136
ft/M flzimith ft H8 ft
Dip-55-52
Ifc-'''«
Fron
6.816. 8
16.8
18.8
?6.5
159.8
165.8
265.8
281.8
383.8
311.8
128.8
,
136.8
To
10.816.8
18.8
?6.5
159.8
165.8
265.8
281.8
383.8
311.8
128.8
136.8
523.8
SIOUX PROJECTHole No:
—————————————— Qescri pti on ————————————
CasingMafic tuff, chloritic, py. as diss. grains andaggregates to 2 CM totaling 2KFelsic quarts x-tal tuff, sericitic, alternatinguith fragnental layers, f el sic frags, to 1 en.Mafic tuff, abundant lapilli, layered, very finegrained carb., f el sic frags, to 5 en at ?6 feet.Felsic quartz x-tal tuff, crude layering, beds uithfine grained tops up to 18 feet thick, sone lapilli.Chloritic lapilli tuff, felsic frags. 1 en by 1 en,coarse to fine grading, tops south.Felsic quarts x-tal tuff, subround f el sic frags.to 8 nn, nornal graded 5 to 18 ft. thick bods, qtz.veins or chert flou tops approx every 5 ft. fron 225ft. uith \K diss. py.Schist, fine grained sari ci tic and chloritic uaxygreen uith fine grained qtz. x-tal s, <1S diss. py.Chloritic tuff, fine grained uell foliated, layersto 3 en thick uith OX py., very fine grainedchlorite schist 299 to 383.Louor sulphide unit, 381 to 385 nassive sulphideand chert frag, breccia, 389 to 311 nassive sulphidepy. Mad grained, vuggy, sons qtz. in MatrixChert, very uell banded, sone sedinentary gradingand cross I ani nations, tops south, po>py in placesto 5X as veinlets and stringers, black chert 329to 338 and 315 to 31?, non-nagnftticUpper sulphide unit, gradational base uith nunerouspo>py veinlets and stringers forning chert brecciapo:py 18:1 at base changing to 1:6 at strati graphictop, nassive py. 131.5 to 132, 133 to 135, altern ating recrystallized sulphide frags, in py. natrixuith very fine grained banded sedinentary py.black chert uith diss. py. 135 to 136Greyuacke, fine to very fine grained, first fivafeet lenticular bedding then alternating bedsfron 2 in. to 5 ft. thick, grading and scoursindicate tops south.
S98-2
Sanple
181161811?181181811918128181211812218123
181211812518126.
Fron To
281.8 286.8286.8 291.8291.8 296.8296.8 381.8381.8 386.8*5oo • D 3 1 1 • 3311.8 316.8316.8 321.8
121.8 126.8126.8 131.8131.8 136.8
Length flu Ru ^^ft. ppb ppb ^^
^^
5.8 185.8 315.8 385.8 nil5.8 195 1955.8 625.8 815.8 15
5.8 ?25.8 115.8 288
TRI ORIGIN EXPLORATION LTD.
Drill Hoi a Survey Data
Project SIOUX
Drill hoi a nunbar: S98-3 Data: Fab. 21, 1998Drill ad by: Tonic Date star-tad: Fab. 13, 1990Logged by: R. Valliant Data conplatad: Fab. 21, 1998Cora siza: BO
Purpose: T«st I.P. anonaly L.*U88H "1+695
Consents: E.O.H.8 886 faat, 31 boxas cora.Hoi a drill ad in aldar suatip at adqa of laka. Plugged at 689 ft. and canantad uith 3 bags cenant.
Collar location: Lina : 1+88W Station : 2+66N Elevation: laka *3 ft
Drill hole surveys:
Survey tgp« Dapth ft/« Rziriuth Dip
Conpass collar ft 1^6 -68 acid 696 ft -59
SIOUX PROJECTHoia No: S98-3
FroM
8.8111.8
165.8
1?8.6
291.0
. 5
To
11-1.6 165. Q
1?8.8
291.6
3??. 5
626.6
626.6 656.6
656.6 663.8
663.6 663.6
663.6 ?21.81
?21.8 ?38.8
?38.8 686.6
-Description-
CasingFalsic tuff, Minor quartz x-tals, nora Abundantfeldspar phenocrysts, C.B.ft. 55 dag.Chlcritic lapilli tuff, foliated, banded, ned. greencolour, probably falsic conposition.Falsic volcanic rock, poorly baddad variable prinarytextures, ueakly foliated, feldspar phanocrysts uithindistinct boundarias to 3 HH., occaisional lapillito 2 en., C.B.R. 69 dag.Falsic lapilli ash flows, wall baddad, darker finagrainad units approx. 19 en. thick alternating withlight colourad feldspar phyric, foliatad lapilliunits approx. 35 en. thick, sona falsic frags, qtzx-tal bearing to 4 en. long.Falsic quartz x-tal tuff, relatively Massive at basaueakly foliatad, occaisional lapilli units 18 CM.thick, tr. py in fins grained straaks, C .B.fi. 56 dag.top half of unit distinct ash flows approx. 6 H.thick, qtz x-tals to 3 HM in cantar of flows uithreverse graded basa and nornal graded tops u.r.t.qtz x-tal size, fina grainad chloritic chenical sad.tops approx. 15 en thick, foliatad uith diss. whitecarb. and up to 8 fi diss. py.Chloritic lapilli tuff, fina qtz x-tals, foliataduith lenticular patches of quartz, average 1 to 2 Xpy and po., probably alteration of x-tal tuff ratherthan distinct lithologic unit.Chlorita scist, foliated, broken core, approx. IXpy., in places 5 cw bands up to "Hi py, chenical sad.Fault ?, sub-angular chart frag, breccia in veryfina grained Massive chlorita natrix.Chart, fina saanlets of nag. throughout, vary finagrained Minor anounts of arsanopy 1% 666 to 66?narrow Massive py layers overlain by Massive nag.and chart frags., ?22 to 724 po-rich chart, po asirregular vainlats, po:py 18:1Sulphide unit, interbadded Massive sulphide layersand chart, fina grainad, Magnetic, top 26 en nassivesulphide fina to Mad. grained sedinantary but appearsbrecciatad, vuggy and racrystalized.Greyuacke, ned. grainad beds 38 CM to 1.5 M thick,fina grainad, dk. grey bads 5 en to 38 en thick.
Sanple FroM To
1815118152
18111 18 H2 18113
18115 16116 1811?
181181811918158
55?. 8 5?8.8
626.6631.8651.8656.8659.5663.5666.8
?22.8 ?21.8 ?2?.8
55?. 5 5?8.5
631.8 636.8 656.8 659.5 663.5 666.8 66?. 6
?21.8 ?2?.8
Length ft.
2.8 3.8 3.8
Ru ppb
Ru ppb
8.58.5
5.85.85.83.51.83.81.8
19918
?nilnilnil
?9399
1258
238
1211
213699116
Pickerel /Arm -
O SooI______I_____I
•feet
Tri Origin Explorotlon Ltd. Project
Drill Section hole
Axm 24O*By RV. |Pv*9.No.-
Pt'ckcrcl Arm - MinnitoVt
Tri Origin Exploration Ltd.
Piamoh<i Dnllholt ?0 -£
looking AzmRV. jD*q.No.i
/Tri Origin'Exploration Ltd
Dote-- fefc> TO I By: R-V- [ pwg.No
Mirvslry ofNorthern Developmentjnd FV.ines
/Report of Work *"
. MlTrTRg Act (Geophysical, Geological and Geochemical S52F16NE8226 2.13491 PICKEREL 900
Type of Surveys) Lint,
Mining Division Township or Area
4Recorded Hdder(s) PrBspector's LIcence'No.
Address Telephone No.
Survey ny
Name and Address of Auth'or (of Geo-Technical Report) ' f f Date of Survey (from & to)
0 8? J MO. 1 tft? \ f»y 1 TJo. | *Yr.
Credits "Requested ffer Each Claim in Columns at right ' Mining Claims Traversed (List In numerical sequence)Special Provisions
For first survey:
Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter total(s) here
Airborne Credits
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
• Electromagnetic
- Magnetometer
-Other /. /^
Geological
Geochemical
Geophysical
- Electromagnetic
• Magnetometer
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Other
Days per Claim
<$O
Days per Claim
Days per Claim
Total miles flown over claim(s).Date , Recorderfijolde/ or Agjtntifiignalure)
Mining ClaimPrefix .
fit
ft
P*.
*
Number
116221-$
Mining ClaimPrefix
,
fa
fa
NumberMining Claim
Prefix Number
Certification Verifying Report of Work
Total number of mining claims covered by this report of work.
I hereby certify that I have a personal and intimate knowledge of the facts set forth in this Heport of Work, having performed the work or witnessed same during and/or after rts completion and annexed report is true.Name and Address ol Person Certifying
Certified By (Signature)
For Office Use Only
toiai L>ays Cr. Recorded
Date Approved as Recorded Provincial Manager, MlnmgTands
1362(89/06)
Mining Lands SectionCedar Street, 4th FloorMinistry of
Northern Development ^DBURYT'ontarioand Mines \/P3E 6A5
Ministere du Telephone: (705) 670-7264Developpement du Nord Faxs < 705 > 670-7262et des Mines Your pile . W9003t 223
Our File : 2.13491
November 19, 1990
Mining RecorderMinistry of Northern Development and MinesCourt House BuildingP. O. Box 3000SIOUX LOOKOUT, OntarioPOV 2TO
Dear Madam/Sir:
RE: Notice of Intent dated October 16, 1990 for Geophysical (Induced Polarization) Survey submitted on Mining Claims PA 1102279 et al in Kabik and Pickerel Twp.
The assessment work credits, as listed with the above mentioned Notice of Intent have been approved as of the above date.
Please inform the recorded holder of these mining claims and so indicate on your records.
Yours sincerel
R. C. Gashinski A/Provincial Manager, Mining Lands lines and Minerals Division
rs/dvl Enclosure
cc: Mr. W. D. Tieman Resident GeologistMining and Lands Commissioner Sioux Lookout, Ontario Toronto, Ontario
Tri Origin Exploration Ltd. Toronto, Ontario Attn: Robert Valliant
Ministry olNorthern Developmentand Mines
Technical Assessment Work Credits
Ontario^DimOctober
2.13491TMinlng R ecorder'! Report ofr 19, 1990 Wo 'kTj°-W9003.223
Recorded Holder
TRI ORIGIN EXPLORATION LTD.Township or Ares
KABIK AND PICKEREL TOWNSHIP
Type of survey and number of Assessment days credit per claim Mining Claims Assessed
Geophysical
Electromagnetic.
Magnetometer.
Radiometric _
Induced polarization.
Other —————————
-days
.days
-days
-days
- days
PA 1102279
1119522
1119524
1119462 to 481 incl.
Section 77 (19) See "Mining Claims Assessed" column
Geological ___________:_______days
Geochemical ___________________ days
Man days (~j
Special provision Q
Airborne l~l
Ground (3
Credits have been reduced because of partial coverage of claims.
Credits have been reduced because of corrections to work dates and figures of applicant.
Special credits under section 77 (16) for the following mining claims
30 days credit for Induced Polarization: PA 1102280
10 days credit for Induced Polarization: PA 11022781119523
No credits have been allowed for the following mining claims
f~| not sufficiently covered by the survey insufficient technical data filed
The Mining Recorder may reduce (he above credits it necessary in order thai the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical • 80; Gcologocal • 40; Geochemical • 4 0'; Section 77(19) • GO.
626(1)5/12)
FILE NUMBER:
TOWNSHIP/AREA <S)NUMBER OF POLYGONS
K
LEGEND
HIGHWAV A\D ROUTEOTHER
V N !\G C..A A
•JNSURN. E^ Ef.LOT v. SES
_ -OUNOARY
v s s,, . A vs5 A . ^ A A V i '. 7, 3 t j - " : A A V
L'NES
iON PE^EMNtA.. S"EAM
C LCOOING RIGHTS SL;BOU S.ON "•- COMPOSITE PLAN
VERMILION-""WOR STATUS
JORDAN TWRFOR-STATUS REFER TO TWP. PLANTO TWP. PLAN
VARSn O
WINES
TRAVERSE MONUMENT
DISPOSITION OF CPOVVN LANDS
T YP OF DOCL'VE.NT
ACE i ViVNG *C£ = .GHTS ONLY
RIGHTS ONLYLEASE. SURFACE & MINING RIGHTS
SURFACE RIGHTSONLV MINING RIGHTS ONLY
OCCUPATION
••iris DDIHOT y- i j " >-—- r Lzr \ _-Z*L 1^-=^^- _ - _ _ _
oocsi^—^gy^^JTT—- — "—i"V"" ^'"0 '•
§53€73 ^ 153674,''
R.J. 14 153667 ! MMTI
NOTE M 'S-SG P "," TS •-5- J - £S^? ? iS
kCT a S JPO PO I Po I PO
1124873 1124872 I 1124642 Yi™f«437101 | 533(30 533ISI
Pa i Pa Po 1 Po R E F E F1121874 11240661 »24875 s
V.R.O - VtMNG RIGHTS ONLY
3 ? 0. - SL'R C AC5 PlGr,' _ ONE1124643 1124876,
M in n i'' a k /
' i -- .• I UfiJiflfli- r^~^ '— ' '"" -----
———-.___ -I- _
' ...- -i- I .--
89/04/28 L.UP. I - WOOD LOADING SITE
L.U.P. 2 - OUTPOST CAMP
L.U.P. 3 - DOCK__ H. M_ _ _
^FORMATION THAT LU.P. 4,5 - BELL CANADA CABLERS ON THIS . MAPBEEN COMPILEDVARIOUS SOURCES.
T.L.C. - TRAPLINE CABINACCURACY IS NOT
JG TO STAKE MIN- AtMS SHOULD CON- WITH THE MINING DER. MINISTRY OF HERN DEVELOP ftND MINES. FOR AD
KABIK LAKEAND
PICKEREL TWR>* »j r --'nil i C T 3 *\ T P ; C il ( -. j « • i t i J 1 n A t 1 • L l
SIOUX L OOKOUT
E STATUS OF THE SHOWN HEREON
PATRICIALAND TITLES / R EGISTRY 01'. ! v iO\
KEUORA (PATRICIA FOR T ION) •
.inn
fV.l n iiqt?m *?
Br.mch
KE1KEWABIK LAKE rrpfiUARY , 1984.
G-2 0752F16NEB226 2.13491 PICKEREL-538921 B port of '
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GEOPHYSICS
Strong 1. P Phase Anomaly
Medium » "
Weak » n "
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•O PR-1
-O 81- I
O 90-1
DIAMOND D RILLING
El Pen Ray Mines Ltd. 1950
Braeswood Exploration Ltd. 1981 a 1982
Tri Origin Exploration Ltd. 1990
— +• ——
tfJ
Claim Post and Property Boundary
Internal Post and Lines
Swamp
52F16NE8226 2 .13491 P ICKEREL
2. 13491
Tri Origin Exploration LtdSIOUX PROJECT
SIOUX LOOKOUT,ONTARIO
GENERAL COMPILATION
AND IP PLANFeb., 1990 N.T.S.: ; R V. / gmes Dwg.No.
r
^ 82-5
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Medium " » »
Weak » » "
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•O PR-1
-O 8 1- I
O 90-1
DIAMOND DRILLING
El pen Ray Mines Ltd. 1950
Braeswood Exploration Ltd. 1981 8 1982
Tri Origin Exploration Ltd. 1990
—Q Claim Post and Property Boundary
•—— Internal Post and Lines
Swamp
52F16NE8226 2.1349! P ICKEREL eeo
Revised By Date Tri Origin Exploration LtdSIOUX PROJECT
SIOUX LOOKOUT, ONTARIO
GENERAL COMPILATION
AND IP PLANDate-- Feb., 1990 N.T.S.: Byt R.V. / gmes Dwg.No.
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2. 13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM Inn £ takE Lake Sicux Lookout .
Date: Jan\ 90
Interpretation by:
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2. 13491TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYMInn I i ak I L ake Sioux Lookout .
Date: Jan\ 90 Interpratai i on by- Scale; 1 : 2400
MERTENS fi MacNEIL LTD.52F16NES226 2 .13491 PICKEREL £50
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2. 13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM Inn Iiak [ Lake Sioux Lookout .
Oats: Jan\ 90In tarpretat i on by:Scale: 1 : 2400
MERTENS S MacNEIL LTD
5aF16NEB226 2,13491 PICKEREL
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F E I t er ed -V o f I les
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Instrument: IRT1, IPV4-TURB3 Fr equencyl 1 Hz. Operator: J.M.N.
. 13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYMInn Iiak i Lake
S Coux Lookout .
Date: JanN 90 Interpret at ion by: Scale: 1 : 24CO
MERTENS S MacNEIL LTD
52F16NE82a6 E.13491 P ICKEREL £80
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Logar t thro Ic Contours
filter*
* * * * *
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Instrument: IPT1. IFV4-TURBO Fr equency! 1 Hz- Op=rator: J.M.N.
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM Inn I l akI Lake
S Eoux Lookout .
Date: Jan\ 90
Interpratalion b
Scale: i : 2400
MERTENS S MacNEIL LTD52F16NE8226 2.13491 P ICKEREL 300
OJ
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filter 4688 6568 3764 5380 6060 2886 3563
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158 177 ^207^ \115 n = 2
247 n - 3
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2,13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYMEnnMak \ L ake Stoux Lookout .
Date: Jan\ 90 Interpratalion by: Scale: 1 : 2400
MERTENS 8 MacNEIL LTD52F16NE8226 2,13491 P ICKEREL 310
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filter 571 567 546 526 511 625 802 672 2:52 29*7 2734 1024 324 367 268 237 246 2742 2660 4075 2002 1595 617 302 215 LS7 1 39 L30 L25 130 L 23 L SI 154 1 57 161 1 72 246 f ilter
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filter
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-1 -1 -l.l -1 . 7 3.5 7.2 ID 12 6.1 3.9 6.1 12 20 14 7.6
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TOPOGRAPHY
RESISTIVITY
(ohm-nu
[mill t-rad)
INTERPRETf=iTIOM
20+00 S 18+00 S 16+00 5 14+00 S 12+00 S 10+00 S
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n =l -.2 -.8 -.4 -.5 -2 -.2 y^.6.
n=2 -.1 -0 -.7 -.9 -1.8 -.1 -3
n =3 -2.9 -.1 0 -1.1 -2.2 -0 .1 -.3
~-A -37 _ i.a n -.1 -,6 .1 .] 0 "
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Line 1200
Dtpole-Dlpole Array
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Filtered Profiles
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Instrument: IPT1, IPV4-TURBO Frequencyl 1 Hz. Gpsrator: J.M.N.
2,13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM I nn I i ak I L ake
S Eoux Lookout .
Date: Jan\ 90 Interpratalton byi Scale: 1 : 2400
MERTENS & M acNEIL LTD
52F16NEB226 2.13491 P ICKEREL 330
MF IP RES200,, 50_ 5000.,
LOO-
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filter 218 406 557 1033 1273 1 C66 1 526 2334 2089 4C89 1736 :549 249 SO 127 240 377 464 333 296 ^35 335 295 231 172 154 1 19 1 18 1 33 1 49 163 231 172 317 423 f ilter
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920 n=4
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filter -1.2 -l.t -1 -.2 3.3 7.2 12 15 12 19 16 26 43 £7 68 37 17 1.1 -1.2 -.7 .1 -.6 -.3 -.2 .2 1.3 .5 L.3 1 .7 1 .7 1.2 1.8 1.9 !.,£
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TOPOGRAPHY
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INTERPRETATION
16+00 S 14+00 S 12+00 S 10+00 S( —— , —— h- 8+00 S 6+00 S 4+00 S ——i——,——h 2+00 5 ——i——_ 0+00 2+00 NH————.————h
4+00 N G+00 N 8+00 N 10+00 N 12+00 N 14+00 N ,——i——. 16+00 N ——i——ifilter -.6 -.6 -1 -1 .2 .9 .6 .6 19 49 1 13 565 397 215 0 -.3 -.1 -.3 -.3 .1 .2 1 .4 1.1 1 .4 1 .3 .4 1.2 . 9
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METAL Fi^CTOR(Ip/res * 1DC1
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Dtpole-Dlpole rVray
I __i
plot polnl
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F [ 1tered DrofE
Resist ivity —— — ——Polarization ————————Metal Factor ————————•
es
filterX
* ** X *
* * * *
Logar i thm ic Contours 2 - 3- 5' 7- 5 ' 1 0 '
Instrurrent: IPT1, IPV4-TURB3 Frequency! 1 Hz. Operator: J.M.N.
2. 13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM inn Iiak I Lak e Stoux Lookout .
Date: Jan\ 90
In terpret at ion by:Scale: 1 : 24CO
MERTENS S MacNEIL LTD52F16NEB226 2.1349] PICKEREL 340
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Instrument: PT1, IPV^-TURBO Frequency* 1 Hz. Operator: J.M.N.
3491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM Inn C1ak t L ake Stoux Lookout .
Dale: JarA 90 InlerpretatIon by: Scale: 1 : 2400
MERTENS & M acNEIL LTD
52F16NE8226 2 .13491 PICKEREL 3S0
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f;3ter 106 154 279 5BO 614 273L +717 321 2354 1594 203 1457 485 4*2 314 165 106 52 42 46 52 51 44 13 21 655 232 826 751 804 69+ 582 350 6*4 671 510 418 393 401 478 554 5*2 531 433 220 filter
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24+00 S 22+00 £ 20+00 S 18+00 S 16+00 S 14+00 S 12*0i3 5 10+00 S 8-t-QC S 6+00 S 4+OC S 2+00 S o+co—I—— 2+00 N 4+OC N 6+00 N 8+OC N 10+00 N 12+00 N 14+00 K i——i——— 16+00 N 18+00 K 20+00 N
filler -13.4 -10.1 -2.8 1 -.3 -.5 .1 .9 1 L.I 1 1.4 -.9 -3.1 -.3 . 2 1 1.6 130 313 587 1273 1293 991 839 270 1.1 -2 -.3 2.4 3.8 2.5 .9 1.7 1.3 .7 .3 -.1 .2 .2 .3 filter
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2. 1 3491TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM inn i iak I L ake Svoux Lookout .
Date: JanX 90 Interpr stalEon b Scale: 1 : 2400
MERTENS 8 MacNEIL LTD
52F16NE8226 2.13491 P ICKEREL 330
*1F IP RES2DO-, 50_, 5COO-,
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22+00 S 20+00 S 18+00 5 16+00 S 14+00 S 12+00 S 10+00 S 8+00 S 6+00 S 4+00 S 2+00 S 0+00 2+00 N 4+00 N 6+00 N 8+00 N 10+DO M 12+00 N 14+00 N 16+00 N 18+00 N 20+00 Nf i Her 63 126 213 364 1401 680 1954 1262 687 731 663 534 396 1 54 L23 94 67 48 38 43 51 55 58 42 36 103 1055 3556 39M 3261 1299 7B6 "6 421 35 7 286 262 299 303 303 284L 2584 2338 2018 "S f I It er
n = 1 35 I 6p / 167 26 41 3631 ^ 25 26 27 29
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filter 3.6 4.7 7.7 8.2 6.8 3.5 8.1 7.9 6.7 4.8 2.1 l.S 1.8 2.5 .4 .3 .6 L.6 1.7 1.3 .6 3.5 7.9 18 10 2 .3 1 .5 1.7 4.9 73 14 10 4,8 L. 7 2.5 .9 3.4 1.9 -.1 -1.2 -1.2 -.3 t.l .7 filter
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2. 13491
TRI ORIGIN EXPLORATION LTD.
INDUCED POLARIZATION SURVEYM [nn I-tak I L ake Sioux Lookout .
Date: J a n\ 90 IntcrpratalEon b
Scaled 1 : 2400
MERTENS 8 MacNEIL LTD
52F16NE8226 2.13491 P ICKEREL •400
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