REPORT ON THE CARIBOU LAKE PROJECT · 2017. 1. 17. · REPORT ON THE CARIBOU LAKE PROJECT Southern Ontario Mining Division Prepared for Diatreme Explorations Inc. March 16th, 2001

REPORT ON THE CARIBOU LAKE PROJECT

Southern Ontario Mining Division

Prepared for Diatreme Explorations Inc.

March 16th , 2001

Prepared by Walter Hanych HBSc.

41H16NE2002 2.21022 MCCONKEY 010

Table of Contents

Summary ...............................................................................................3

Location and Access.................................................................................. 4

Property Description and Tenure.................................................................... 4

Regional Geology ....................................................................................4

Property Geology..................................................................................... 5

Mineralization ........................................................................................5

History and Previous Work.......................................................................... 6

Work History and Summary..........................................................................8

Results of Previous Work............................................................................ 8

Discussion of Past Results ..........................................................................9

1999 Program .......................................................................................10

Results of 1999 Program........................................................................... 11

Recommendations................................................................................... l 2

Conclusion.......................................................................................... 12

Summary Table of Rock Samples.................................................................. 13

References........................................................................................... 20

41H16NE2002 2.21022 MCCONKEY 010C

W. Hanych Diatreme Expl Caribou Lake. Page l Mar 16, 2001

Table of Contents cont

Figures

Figure lProperty Location Map ......................................................................................... follows page 4

Figure 2Claim Map ................................................................................................... follows page 5

Figure 3Compilation Map.............................................................................................. follows page 12

Figure 41999 Results ...................................................................................................... back pocket

Appendices

Appendix lAssay Certificates

W. Hanych Diatreme Expl Caribou Lake. Page 2 Mar 16,2001

SUMMARY

The following report covers the Caribou Lake Property, a 1,580 hectare parcel of 8 contiguous claims staked over the Caribou Lake intrusive. The claims are owned by Diatreme Explorations Inc. of Toronto.

During the last half of November, 1999 the author of this report along with the assistance of consulting geologist Frank Racicot conducted a preliminary geological investigation of the platinum potential of the intrusive. Approximately 35 kilometers of traversing and 93 rock chip samples were collected and submitted for analysis.

Seven target areas were identified for follow up as well the contact of the intrusive remains to be thoroughly investigated.

March 16th, 2001

W. Hanych Diatreme Expl Caribou Lake. Page 3 Mar 16, 2001

CARIBOU LAKE PROPERTY

Location and Access (Fig. 1)

The Caribou Property is located in Central Ontario approximately 62 kilometers north of the town of Parry Sound and 320 kilometers north of Toronto. The property is situated in Mcconkey township and covers the north, and northwest portions of Caribou Lake, NTS 41 H/16 includes the area.

Access to the property is via Highway 69 north to Provincial Highway 522 located 78 kilometers north of the town of Parry Sound. Easterly, along Highway 522 for a distance of 40 kilometers to the general area of the southern portion of Caribou Lake. Concession roads leading north from the highway provide access to the lake itself and the claims.

Property Description and Tenure

The property is 10096 owned by Diatreme Explorations Inc. of Toronto, Ontario and consists of a contiguous group of eight unpatented mining claims comprising 81 units totaling 1,580 hectares of Crown land. The following claims recorded with the Mining Recorder's office of the Ministry of Northern Development and Mines are registered on claim map M192, Sudbury Mining Division.

Claim Number No of Units Hectares

SI 2229459 16 320SI 229460 4 80SI 229461 8 160SI 229462 12 240SI 231040 16 320SI 231041 16 300SI 231042 5 80SI 231043 4 80

Regional Geology

The Caribou Lake intrusive is situated in the Britt Domain of the Central Gneiss Belt in the Grenville Geological Province. The rocks of the Central Gneiss Belt are chiefly 1 800-1600 Ma quartzofeldspathic gneisses of igneous origin with subordinate paragneiss. 1 The Caribou Lake gabbro-norite was intruded into the Britt Domain rocks which are highly deformed gneisses and migmatites of supracrustal and igneous origin forming a complex series of metaplutonic units.

1 Easton, R.M. 1992. The grenville Province and the Proterozoic History of Central and Southern Ontario; in geology of Ontario, Ontario Geological Survey, Special Volume 4, Part 2, p722.


Hudson Bay

^1.

fO T

/r o - **

/* N^,W*^v ^^ f -f- •'ft**

•4-^ ^rt,'

S,

.tg^ ifc^'ij^

^ *r

1^^^ ^*Y

f ^***.

Caribou Lake Property

VWndsorL ./'^-^ \v^,/

Property Location Map

DRAWN BY W. Hanych

SCALE 1:8 500 000

March 2001

FIGURE 1

These domains are a part of a network of continuous zones situated between the Grenville Front Tectonic Zone and the Central Metasedimentary Belt, along which, predominantly northwest directed, deep crustal thrust faulting has occurred resulting in a thickened crust.

Property Geology

The Caribou Lake intrusive is an 1 8km2 , northwest-southeast ebngated, lobate, funnel-shaped body. At its northwest end it measures 2.74 kilometers narrowing down to 305 meters at its southeast end, its long dimension is approximately 8.5 kilometers.

Friedman's work (1957) led him to conclude that the Caribou Lake intrusive is a differentiated body exhibiting changes in modal composition from picrite to olivine norite to norite. This differentiation trend involved chemical changes that were summed up as follows:* Ultrabasic rocks occur only near the eastern tip.* Hypersthene decreases and augite increases as the norite is traced westward across the

intrusive.* The Fe/Mg ratio in hypersthene and the Na-Si/Ca-AI ratio in plagioclase increase

progressively westward.* MgO decreases to the west as FeO, FeA, and the alkalies increase.* Nickel, copper, and chromium decrease progressively to the west. 2

Mineralization

Mineralization in the area is associated with the norite, pyroxenite dikes and in graphitic paragneisses. Pyrrhotite, pyrite, chalcopyrite and titaniferous magnetite occur disseminated and as stringers. The graphitic paragneiss is reported to contain 596 sulphides (pyrite, pyrrhotite and chalcopyrite) which show up geophysically as strong conductive zones. Disseminated sulphides containing anomalous platinum are associated with the norite and pyroxenite. The following table summarizes the significant sample results

Location Cu Ni Pt Comments

N/AN/AL20,C3L15,C4L15,C3L18,C4,5L18,C4,5

Q.32%n.d.

1.3 3 07o1.009/00.2 3 07o0. 070Xo0. 039/0

0.2 2 07o0.3 7 07o0.3 3 07o1.500Xo0.1 59/00.039/00.069/0

n/an.d.

traceSgr/t

n/an/an/a

weathered sulph, norite grab sample, norite reported, norite reported, norite 50 core length, notite pyroxenite dike pyroxenite dike

Reference

Ont Dept M i nes Coleman, 1900 Coleman, 1900 Coleman, 1900 Chubb Syndicate Tylex Corp Tylex Corp

Note: N/^not availabe, n.d^not detected, n/^ not assayed

2 Friedman, G.M. 1957. Structure and Petrology of the Caribou Lake Intrusive Body, Ontario, Canada, in Bulletin of the Geological Society of America, Volume 68, p!531.

W. Hanych Diatreme Expl Caribou Lake. PageS Mar 16, 2001

sm

CLAIM MAP MCCONKEY TOWNSHIP

Ref map M192 Scale linch^/4 mile

FIGURE 2

ê^-1

History and Previous Work

1899Interest was first generated in the Caribou Lake area when mapping and field investigations by Government geologists reported in 1899 (Coleman, p. 259-262) and 1900 (Coleman, p. 170 -171) work which described several pits sunk into rusty zones. The investigations resulted in reported values of up to 1.55 Vo copper, 1.2 94 nickel, and 8 grams platinum from a showing on Lot 1 5, Concession 4. 3

1 900's earlyDuring the early 1 900's, several prospect pits were excavated in the area. On Lot 18, Con 2 and 3 pits were excavated on "diabase" containing iron and copper sulphides. Samples from a pit on Lot 20 Con 3 assayed 1.33*)6 copper and Q.32% nickel. Work on Lot 15 Concession 4 and Lot 18 Concession 4, lead to the discovery of small deposits of muscovite related to granite pegmatite dykes and referenced to, in Statistical Reviews of the Mineral Industry of Ontario (Gibson 1909, and Rogers 1916).

1942Minor work was carried out between the 1930's and 1940's and in 1942 J. Satterly in his report to the Ontario Department of Mines, identified the rocks of the Caribou Lake area as norite.

1950-1 951The first serious exploration program was undertaken by the Chubb Syndicate between 1950-1951. Several magnetic anomalies were drill tested from the ice during the winter of 1951. Four holes totaling 1,795 feet were drilled. The best results were reported as follows:

Hole No. 2; 1 25-175 foot drill depth, 50 feet contained 10 sulphides with low copper and nickelvalues (G.22% andO.151% respectively)4in a silicified norite in contact with a talc alterednorite.Hole No. 3; 177-188 foot drill depth, 11 feet of intensely talcose altered norite with 1 S'%sulphides.Hole No. 5; 187-204 foot drill depth, 17 feet of silicified norite with 10% sulphides.

1954-1 955Newkirk Mining Corporation in 1954 conducted an airborne electro-magnetic and magnetic survey over the Caribou Lake intrusive.

In the same year Aumaque Gold Mines Limited undertook a program of ground electro-magnetic, self potential surveying, and soil sampling at the northwest end of Caribou Lake. Seven anomalies were delineated and diamond drilling was recommended on two of the anomalies, one located east of Round Lake, and the other just north of Deep Bay in Caribou Lake. Approximately 5,300 feet of drilling was completed in 1955 on the strongest conductors, and anomalies. The results of this drilling indicated that the conductors were due to graphite with minor pyrite, pyrrhotite and chalcopyrite, and no significant copper-nickel values were reported.

3 Coleman, A. P., 1900, Ontario Bureau of Mines Report, Volume9, p!70-171.4 Martin, W., C., 1959. Geological Report for Twin Basin Nickel limited, Caribou Lake, McConkey Township,Parry Sound District, Ontario, p 10-15.


1956Records indicate that Twin Basin Nickel Ltd. contracted Aumaque Gold Mines Limited to drill 3,000 feet on their holdings on the Caribou Lake intrusive. The data from this drill program does not appear to have been submitted for assessment work and therefore was not researched.

1957In 1957 G.M. Friedman published in the Bulletin of the Geological Society of America Volume 68 pi 531- 1564 the results of his study of the Caribou Lake intrusive conducted between 1953-1955. This manuscript titled The Structure and Petrology of the Caribou lake Intrusive Body, Ontario, Canada is the most comprehensive geological study to date. His petrographic work described the similarities of the Caribou lake intrusive to the Stillwater Complex in Montana.

1959W.C. Martin produced a compilation report for Twin Basin Nickel Limited in 1959 in which he recommended the property for further work and outlined a S100,000 exploration program. He also compared the Caribou Lake intrusive with the Sudbury nickel erruptive.

1963In 1963 the Loring Syndicate contracted McPhar Geophysics Limited to survey their claims on Caribou Lake. A program of induced polarization, resistivity, mag and gravity surveying was undertaken. Approximately 60*X) of the intrusive was gravity surveyed, the northwest portion west of Deep bay was not covered by this survey

1968During the winter of 1968 an electro-magnetic survey was carried out by Geosearch Consultants Limited for the Hudson Bay Exploration and Development Company Ltd. Several strong conductive zones were delineated in the area between Round Lake and Burnt Lake.

In the summer of the same year, Hudson Bay Exploration through Midwest Drilling drilled 11 holes to test the conductors. A total footage amounting to 4,075 feet was drilled. Assessment records indicate that four of the holes were submitted for credits.

1986Platinova Resources Ltd. staked the Caribou Lake intrusive in the spring of 1986 and did a limited rock sampling program consisting of 16 samples from various lithologies. 5

1987Noramco Explorations Inc. commissioned Dr. P. Whittaker in 1987 to evaluate the platinum potential of the Caribou Lake intrusive. Twenty five samples were collected from known showings and assayed for gold and platinum. Although no significant results were obtained, his report states that the potential exists for significant platinum mineralization. At the same time the property was flown by Aerodat in which a sensitive magnetometer survey was conducted.

1991

5 Whittaker, P.J. 1987. Caribou Lake Platinum Property, Platinova Resources Litd., Report prepared for Noramco Explorations Inc., p7.

W. HanychDiatremeExpl Caribou Lake. Page? Mar 16,2001

Sometime prior to 1991, possibly 1989, J.R. Atkinson staked 18 claim totaling approximately 288 hectares centered around Deep Bay in the northwest end of Caribou Lake. The claims were optioned to Tylox Resources Corporation of Vancouver, British Columbia which undertook a limited program of geological mapping rock and soil sampling in the fall of 1991.

A total of 14.25 kilometers were traversed and 136 soil and 18 rock chip samples were collected. The samples were analysed for gold, silver, cobalt, copper, manganese, molybdenum, nickel, lead, zinc and iron. 6 The platinum group elements were not assayed for in this program.

1992In late 1991 or early 1992 the claims held by Atkinson were transferred to Tracer Petroleum Corp. of Vancouver, British Columbia. In February of 1992 Tracer Petroleum Corp. completed a program of horizontal loop electromagnetic (HLEM) and total field magnetic surveying totaling 11.4 kilometers. An independent geophysical report of the results of this program was prepared by F. L. Jagodits, Geophysical Consultant.

Work History Summary

1951 Chubb Syndicate1954 Newkirk Mining1955 Aumaque Gold Mines

1956 Twin Basin Mines1957 Friedman 1964 Loring Syndicate 1968 Hudson Bay Exploration

and Development1986 Platinova Resources

1987 Noramco, Exploration1991 Tylox Resources1992 Tracer Petroleum

Mag Survey, 1,795 ft. drillingAirborne EM and MagResistivity, EM, SP, Mag,Soils, 9 Drill Holes-5,333 ft.Drilling-3,000 ft.Petrological and Structural evaluationMag, IP, Resistivity, Gravity, Trenching

EM, Mag, 11 Drill holes-4,075 ft. Surface Sampling

Surface Sampling, Mapping, Airborne Mag Mapping and Sampling HLEM, Mag

Collectively the above exploration efforts have resulted in a total of 14,203 feet (4,329 meters) of diamond drilling.

Results of Previous Work

The following significant results of the past work are highly favourable and relevant for targeting the platinum potential of the intrusive:

* An historical sample is reported to have assayed 8 grams platinum.* Diamond drilling intersected a silicified norite with 50 feet returning values of Q.23% Cu,

and 0.15 0Xo Ni.

6 Atkinson, J. R. 1991. Report of Work, Caribou Lake Property, Ontario, prepared for Tylox Resources Corporation, Vancouver, BC, p2.

W. Hanych Diatreme Expl Caribou Lake. PageS Mar 16, 2001

* The intrusive is described as a differentiated mafic body.* Chemical aspects of the intrusive (ie. iron rich pyroxenes) have been compared with the

pyroxenes from the upper part of the Stillwater complex.7* Sulphidic-graphitic sediments (paragneisses), have been intersected in diamond drilling.* A coincident mag high-gravity high (2,200ft x 600ft) is situated in the narrows of Caribou

Lake, south of Deep Bay on lots 17 and 18 concession 4.* A curvilinear north-south trending IP anomaly (1200ft x 30ft) exists on lot 15

concessions 4 and 5.* Two samples from the recently discovered pyroxenite dike within the main norite mass

assayed nickel (256 ppm and 630 ppm) and copper (713 ppm and 271 ppm) on lot 18 concessions 4 and 5.

Discussion of Past Results

Four diamond drill campaigns, and limited surface sampling, mapping, and geophysics, coupled with two airborne surveys have resulted in inconclusively assessing the platinum potential of the Caribou Lake intrusive. This is overwhelmingly due to the fact that most of the programs with the exception of the limited work done by Platinova Resources concentrated on its copper- nickel potential. The significance of the above results in the order itemized above are discussed below :

* The Caribou Lake intrusive is reported to contain platinum and highly anomalous copper- nickel values over significant widths.

* Friedman (1957) concluded that the Caribou Lake intrusive differentiated in the sequence picrite, olivine-norite, to norite, in which case it may have also fractionated and precipitated platinum group element (PGE) rich sulphides.

* The chemistry of the intrusive is favourable and compares with known platiniferous deposits.

* The sulphidic-graphitic sediments that form the country rocks may have acted as the sulphide source, contaminating the magma causing sulphide saturation and the precipitation of PGE rich sulphides.

* The coincident mag-gravity high may represent a metal rich portion of the intrusive.* The curvilinear IP zone correlates with: a) the trenched area from which the 8 gram sample

was obtained, b) the concentric topographic bands that Friedman (1957) attributed to evidence of the differentiation of the intrusive, c) the strike continuation of the intersection that was intersected by the Chubb Lake syndicate (1951) in diamond drill hole 2(50 feet of 0.23%Cuand0.15% Ni).

* The pyroxenite dike with the anomalous Cu-Ni values may represent a phase of a multiple injected magma. The Tylox Resources (1991) program did not assay for platinum therefore, it is not known if this dike is platinum enriched. Atkinson (1992, former consultant with Tylox) made reference to the Robie zone of the Lac des Iles Complex in northwestern Ontario, by quoting Sutcliff (1987, pi 77), "one pod of high grade mineralization is

7 Friedman, G.M. 1957. Strucure and Petrology of the Caribou Lake Intrusive Body, Ontario, Canada, in The Bulletin Of the Geological Society of America, Volume 68, p 1553.


associated with altered pyroxenitic to melagabbro rocks right at the contact between the Eastern and Western Gabbros. 8

The Chubb Syndicate in diamond drill hole No. 5 intersected 87 feet of black pyroxenite within an altered norite . A seventeen foot section of norite near the upper contact of the pyroxenite was estimated to contain 1096 sulphides. However, there may be a down dip component to this intersection.

An intense talc-chlorite alteration was noted in the Chubb Syndicate diamond drill holes No. 3, 4 and 5. This may indicate a hydrothermal component with an associated shear zone. Shear zones cutting mafic-ultramafic host rocks are known to be enriched in platinum and palladium.

1999 Program

The 1999 exploration program was designed to identify potential sites for follow-up work. A program of prospecting and sampling was undertaken over areas that in the past were either under-explored or not explored at all. The program evaluated the land holdings of Diatreme Exploration Inc.(see claim map), for this reason and because of the cottage infrastructure in the southeast portion of Caribou Lake the southeast section was not included in this program

Since most of the past work evolved around lake shore access, an air photo study was undertaken to determine access trails within the interior and northern portion of the intrusive. The air photos greatly facilitated the establishment of traverse lines by revealing trail access and potential outcrop areas. From this study it became quite apparent that water transport would be of limited use and ATV transport would provide the means to access the interior and northern portions of the intrusive. The ATV became an invaluable transport, greatly facilitating field movement by maximizing the ground cover for prospecting, and the transport of heavy rock samples.

A digital map file of the area was obtained to facilitate sample location plots. Field maps with UTM co-ordinates were prepared and all samples were referenced to the UTM grid by GPS locate. Topographic features were picked off air photos and the digital topo-base as a further aid to confirm GPS locates when required.

A total of 35 kilometers of prospecting traverses were completed and 93 rock samples collected. These samples were subsequently described and sent to Chemex Labs in Mississauga. The samples were analyzed for 32 elements by the ICP-AES method and for Au.Pt.Pd and Rh by the FA-ICP method.The results of these analyses are tabulated in Schedule l presented as copies of the original certificates.

8 Atkinson, J.R. 1992. Report of Work Caribou Property, Onario, NTS 41H/16, prepared for Tracer Petroleum Corp., p 6.


The results of all the field work was compiled on a digital topographic base map at a scale of 1:5 0000. Traverse lines, outcrop distribution, major contacts, sample location and significant results were plotted for reference.

Results of 1999 Program

Overview' Mapping and sampling of the Caribou Lake intrusive proved to be more difficult than

originally anticipated despite the efficient methodology employed. Much of the norite outcrop that is not underwater has been so intensely oxidized that the rusty rotten rock material crumbles into pieces. The prevalent rust also obliterates the mineralogical and textural features of a sample necessitating much hammering with 3-5lb sledges to obtain a fresh sample.Portions of the eastern, western and northern contact of the norite was determined and does not significantly differ from past interpretations.

* The platinum values reported in the past could not be substantiated.* Weakly anomalous Ni,Cu,Pt,Pd and Rh values were obtained.* The interior of the intrusive consists of a complex inetermixed zone of paragneiss often

graphitic and pyritic with norite. This may represent proximity of the floor of the intrusive at present erosional levels.

* The graphitic-pyritic horizons appear to be the cause of the conductors and IP anomalies that have been delineated by past geophysical surveys.

* Anomalous Ni and Cu values show a direct relationship with a concomitant increase in Co, Cr and Fe values.

* There is no direct relationship between the twofold increase above the background values of PGE's and Cu and Ni values.

* Anomalous PGE values (combined Pt-Pd-Rh) totaling 0.340gXt (340ppb) were obtained from contact zones within the intrusive, (see below).

The 1999 program tentatively established seven areas that warrant follow-up prospecting.Although the values in all cases were low they appear to be spatially associated with contactareas where PGE and Ni-Cu mineralization may be associated with the border phase of theintrusion. The margin of the intrusive also remains to be investigated.' Area 1

The pyroxenite sill-dike on the east shore of Deep Bay hosts weakly anomalous Ni and Cu values ranging from 109-319 ppm Cu and 224-981 ppm Ni. Two of the six samples (752259 and 752260)that show a twofold increase in PGE (Pt 14g7t-Pd .14g7t-Rd .06g7t) appear to be spatially associated with the eastern contact of the pyroxenite with the norite-paragneiss.

* Area 2Two samples 752206 and 752258 returned PGE values (Pt .14g7t-Pd .14gXt-Rd .OGg/t) two times greater than the apparent background values. These samples were obtained from an outcrop 200meters north of the northwest corner of Deep Bay. Given that samples 752259 and 60 returned identical results and appear to be spatially


associated with eastern contact of the pyroxenite, then, the samples of Area 2 may be spatially associated with the western contact.

* Area 3Sample 752193 assayed 231 ppm Cu and 211 ppm Ni. The norite-granite contact was observed in the stream bank in proximity to this sample as a possible roof pendant.

* Area 4Sample 752253 returned value of 803ppm Ni and 309 ppm Cu. This sample was taken near the margins of the western contact.

* Area 5Although the sample (752284) did not return significant results the rock was described as a pyroxenite and therefore the area warrants further prospecting.

* Area 6Four samples from this area (752202-5 and 08) of mela-norite consistently returned weakly anomalous values of Ni(98-130ppm) and Cu( 106-171 ppm). This area is near the western margins of the pegmatoidal phase of the intrusive.

* Area 7An old pit was discovered at this site and although the sampling returned negative results for PGEs the area is on strike of the IP chargeability linear that is associated with the pit from which the original 8 gram sample was obtained.

Recommendations

Follow-up prospecting is recommended for areas l .2,3,4,5,6 b 7 (see figure 3). A program of detailed mapping, prospecting and chip sampling should be undertaken to evaluate the potential of these sites. The margins of the intrusive remain to be investigated for contact style PGE mineralization.

Conclusion

The 1999 program was by no means an exhaustive sampling of the Caribou Lake intrusive, sufficient samples were taken to isolate areas that still offer potential for hosting PGE mineralization. The norite body was regarded to represents a compositionally stratified layered intrusive complex containing zones of mixing of different magma types coupled with a possible hydrothermal component. This was neither verified or dismissed by the results of the above program.


Anomalous Ni(803ppm)-Cu(309ppm)CARIBOU LAKE PROPERTY

COMPILATION MAP

LEGEND

AREA SELECTED FOR FOLLOW-UP PROSPECTING

IP CHARGEABILITY ZONE

EM CONDUCTOR AXIS

AREA OF GRAVITY HIGH

NORITE

PYROXENITE

ecu-Ni PROSPECT-SHOWING

VA9 DRILL HOLE LOCATION C-Chubb Syndicate, 1951 (1,795 ft.)A-Aumaque G.M.L, 1955 (5,333 ft.) M-Hudson Bay Expl., 1968 (4,075 ft.)

Anomalous Ni(211 ppm)-Cu(231ppm)

0.34 g/t combined PGE

396 sulphides - po, py

Norite and paragnass n^ po,py,gf 8.0 g/t Pt, 1899

YL.H. LOST HOLE

\ peg. PEGMATITE

\ so/ STRIKE 4 DIP OF IGNEOUS LAYERING

Caribou River

Caribou LakeAnomalous Ni-Cu

in-™ir ^-*^; '

SCALE 1:35000

FiGURE 3

Drawn by: W. Hanych March 2001

SUMMARY TABLE OF ROCK SAMPLES

SAMPLES

752151E0567436N5088107752152E0567235N5088715752153E0567744N5088729752154E0567744N5088729752155E0567846N5088592752156E0569674N5088086752157E0569674N5088086752158

752159

752160E0569724N5088052752161

DESCRIPTION

Mela-norite, fine grained, gritty, protoclastic texture, M40-P60, no significant mineralization. Mela-norite, med-coarse grained with 5mm pyroxene crystals, pegmatoid, very rusty, M60-P40. Leuco-norite, M40-P60, medium grained, near contact with paragneiss,

Leuco-norite, M40-P60, medium grained, S-5% graphite, may have partially assimilated paragneiss. Leuco-mela-norite, M50-P50, medium grained, very rusty, trace pyrite.

Leuco-norite, M40-P60, at cp showing no mineralization observed.

Leuco-norite, M40-P60, from same outcrop as above sample, 5 meters south.

Pyroxenite, intense blue tinge to plagioclase, weakly magnetic, 596 biotite, no mineralization observed, located 30 meters north of 7521 56. Pyroxenite, blue plagioclase, weakly foliated at 025V68'W, from same location as 752158. Pyroxenite, trace cp and po.

RESULTPtg/t

*:.07

..07

^07

c. 07

<.07

..07

<.07

<.07

Pdg/t

<.07

<.07

*:.07

^07

<.07

<.07

<.07

*:.07

Rhg/t

<.03

..os

*c. 03

<.03

<.03

<.03

^03

<.03

Nippm 13

37

2

3

3

32

22

880

Cuppm 11

45

13

18

7

17

14

170

<.07 <.07 559 126

*c.07 ^07 ^03 779 102

<.07 <.03 790

<.07 <.03 973

144

177

Pyroxenite, 1/4-196 sulphides, < .C cp40-po60, 1-2mm grains, cp associated with po, located 5 meters north of 752160.

752162 Pyroxenite, 1/2-196 sulphides, < .C cp30-po70, interstitial sulphides with cuspate edges, located 20 meters north of 752161.

Note: numbers below the sample number are the GPS co-ordinates for the sample, UTM easting and northing.



SAMPLES

752163

752164E0569701 N5088238752165

752166

752167

752168

752169E0570546N5087818752170

752171

752172

752173E0570841N5088088752174E0570779N5088155

DESCRIPTION

Pyroxenite, 1/4-196 sulphides,cp30-po70, located 10 meters north of752162Pyroxenite, trace sulphides.

Pyroxenite, trace sulphides, located 5 meters east of 7521 64. Pyroxenite, blue plagioclase very distinct, locate at southeast shore entrance to Deep Bay. Pyroxenite, very distinct blue plagioclase, located 5 meters west of752166.Leuco-norite, M50-P50, blue feldsparsnoted, trace po, located 3 meters west of752167.Paragneiss xenolith, 3'fo sulphides,py and graphite.

Leuco-norite, M50-P50, rusty with trace sulphides, located 1 meter east of 752169.Mela-norite, M60-P40, medium to coarse grained, trace sulphides, located beside 752169. Mela-norite, M60-P40, medium grained, trace sulphides, located 3 meters east of 752169. Leuco-mela-norite, M50-P50, very rusty-oxidized, crumbly, no significant mineralization. Paragneiss, S-7% fine grained py sample taken adjacent to the norite contact, 080 V90'.

RESULT Pt Pd Rh Ni Cug/t g/t g/t ppm ppm

.07 *:.07 .e .03 929 78

*c .07 *c.07 *:.03 819 73

^07 ^07 ^03 909 155

*c.07 ^07 ^03 835 319

*:.07 -c.07 ^03 283 109

^07 .c .07 *:.03 224 99

*c .07 ^07 ^03 98 141

*:.07 *:.07 < .03 41 76

^07 *:.07 *:.03 132 99

^07 *;.07 ^03 15 22

^07 ^07 ^03 13 114

*:.07 K:.07 < .03 137 82




SAMPLES

752175

752176E0570858 N5087767752177E0569747N5088465752178E0570198N5088593752179

752180E0570399 N5088852752181E0570399N5088852752182

752183E0570573N5088808752184E0570573N5088808752185E0570328N5089080752186E0570166N5089282

DESCRIPTION

Paragneiss, 3 meters north of above mentioned contact, intensely oxidized.Leuco-mela-norite, medium grained, trace sulphides.

Pyroxenite, trace po.

Leuco-mela-norite, M50-P50, medium grained, 1/2-196 sulphides, po70-cp30.Leuco-meal-norite, medium grained, no mineralization observed, located 4 meters east of 752178. Leuco-mela-norite, M50-P50, coarse grained, 196 sulphides, po90-cp5-py5, trace garnet, 396 biotite, blasted boulder. Leuco-mela-norite, M50-P50, coarse grained, 396 sulphides, po90-cp5-py-5, pit 2x3 meters, source of 752180. Leuco-mela-norite, 396 sulphides, po90-cp5-py5, from same pit as 752181.Mela-norite, fine grained, 396 sulphides, py70-po25-cp5.

Mela-norite, M60-P40, fine grained,gritty, protoclastic texture, tracesulphides.Paragneiss boulder, 196 py asfracture filling, fine-mediumanhedral grains.Mela-norite subcrop, prominentgarnets, 196 py.

RESULT Pt Pd Rh Nig/t g/t g/t ppm

<.07

.07 22

Cuppm

15

93

< .07 < .07 < .03 558 50

< .07 < .07 < .03 26 32

^07 <.07 <.03 16 25

c .07 <.07 <.03 32 31

< .07 < .07 < .03 45 39

<.07 .c .07 <.03 35 28

<.07 ^07 <.03 28 24

<.07 -c .07 <.03 5 9

<.07 <.07 *t.03 13 18

<.07 <.07 ^03 8 7



SAMPLES

752187E0569992N5089207752188E0570207N5088671752189E0568568N5089690752190E0569076N5089608

752191

752192

752193E0568433N5089825752194E0570430N5087830752195

752196E0569615 N5087950

752197

752198


DESCRIPTION

Pyroxenite, narrow 1 5-20 cm dike, trace po.

Mela-norite, M70-P30, medium grained, trace sulphides.

Paragneiss, 1-396 py and graphite.

Paragneiss, quartz60-feldspar30- biotitelO, trace garnet, 396 py, gritty and granular, at norite- paragneiss contact. Leuco-mela-norite, M50-P50, at same contact as above, no mineralization observed. Leuco-mela-norite, M30-P60-G10, medium to coarse grained, no significant mineralization. Leuco-mela-norite, M50-P50, 196 coarse po, trace py, 1096 garnet, very fresh looking. Mela-norite, M70-P30, medium grained, 196 sulphides, po90-cp10, location of Tylox copper showing. Mela-norite, coarse grained, 196 sulphides, po90-cp10, 2 meters south of 752194.Leuco-norite, 10-1 596 po, trace cp, blasted trench 2.5x4.5 meters at edge of east shore of Deep Bay, heavily oxidized, cp associated with po, fine to coarse grained with 1 cm po grains. Leuco-norite, east face of trench, 596 sulphides, po90-py10-cp10, fine to coarse grained.Leuco-norite, north wall of trench, 596 sulphides, po90-cp10, medium grained.

RESULT Pt Pd Rh Nig/t g/t g/t ppm

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

4

22

11

16

8

9

211

52

97

334

Cuppm

13

42

49

42

17

5

231

61

99

288

•c .07 -e .07 *:.03 389 316

.03 172 163




SAMPLES

752199

752200

752201E0568858N5086868752202

752204E0568840 N5086905752251E0567333N5088344752252

752253E0567200 N5088841752254E0567103N5088797752255E0567574N5088932752256 EOS68046 N5088548752257E0569525N5088816

DESCRIPTION

Leuco-norite, east face of trench, 396 S 1**) fine to medium grained sulphides, po60-py40-tr cpMela-norite, medium grained, S-5% sulphides, po95-cp5, located 20 meters north of trench.Paragneiss-leuco-norite, contact zone, 5*J6 py, graphitic.

Mela-norite, 40 meters north of 752201, in narrow gorge at base of beaver dam, rubble pile, coarse grained, 1-307o, sulphides, po90-py5-cp5. 752202, mineralization same as above. Mela-norite, coarse grained, S-5% sulphides, po99-tr cp, very rusty.

Paragneiss, quartz60-feldspar30- biotitelO, sugary quartz, 396 garnet, trace graphite and py. Leuco-norite, M30-P70, rusty, fine grained, protoclastic texture, Located 100 meters northeast of 752251. Leuco norite, M20-P80, up to 3ô fine grained anhedral sulphides, very rusty area 1 meter wide. Paragneiss, T-2% fine grained py and graphite.

Mela-norite, M60-P40, medium grained rusty, ^cl/4% sulphides.

Leuco-norite, M40-P60, rusty, coarse grained, trace po and py.

Leuco-norite, M40-P60, fine grained, massive, trace py and po.

RESULTPtg/t

.07

.07

Pdg/t

^07

^07

Rhg/t

e. 03

*:.03

Nippm

279

265

Cuppm

289

166

^07 ^07 *:.03 25

^07 *c.03 98

.07

.07

.07

.07

*c.07

*:.07

*:.07

<.07

<.03

^03

<.03

<.03

122

18

72

309

^07 ^03 41

.07 <.07

.07 < .07

.03 26

25

53

137

106

44

96

803

181

26

128 99

14



SAMPLES

752258E0569580 N5088533752259

752260752261

752262752263E0570939 N5087660752264E0570511N5087842752265

752266E0570812 N5087650752267

752268E0570198 N5088623752269E0570492N5088838752270

752271E0570399 N5088852


DESCRIPTION

Paragneiss, very rusty, 1 S-20% graphite, sugary quartz, possible norite mixing, see sample 752206Paragneiss, sugary quartz, very rusty, quartz60-feldspar30-biotite1 0. Paragneiss, very rusty, 3-596 graphite, Pyroxenite, trace po and cp, located 66 meters northeast of 7521 60. Pyroxenite, trace po and cp. Leuco-mela-norite, very rusty, intensely oxidized, strongly magnetic, 2096 magnetite.Leuco-norite, medium to coarse grained, trace cp.

Leuco-mela-norite, M50-P50, medium to coarse grained, trace cp, located 50 meters east from 752264. Leuco-norite, very rusty, intensely hematized.

Leuco-mela-norite, trace po and cp,located 5 meters east of 752266.Leuco-mela-norite, M50-P50, finegrained, trace po, cp, py, S-7%magnetite.Mela-norite, M50-p50, fine grained,596 fine grained disseminated py.

Leuco-norite, M40-P60, very rusty and crumbly, T-3% coarse grained py, located 5 meters southwest of 752269. Leuco-mela-norite, M50-P50, very coarse grained-pegmatoidal, moderately magnetic.

Pt Pdg/t g/t

c. 14 -c .14

*:.14 ^14

< .07 < .07

< .07 < .07

< .07 < .07

^14 <.14

< .07 < .07

RESULT Rh Nig/t ppm

< .06 55

^06 7

^06 14 < .03 826

< .03 981 < .03 41

< .03 53

< .06 36

< .03 22

.07 < .07

.c .07

< .03

^03

34

7

^07 *c.07 ^03 54

. 07 ^03 52

<.07 <.03 3

Cuppm

207

20

108.123

119193

63

36

86

54

24

79

72



SAMPLES

752272E0570409N5089161752273

752274E0569914N5089480752275E0568868N5089690752276

752277

752278

752279

752280

752281

752282

752283

752284752285


DESCRIPTIONPtg/t

Paragneiss, rusty, 196 py, 10 meters < .07 west of pink granite contact.

Mela-norite, M60-P40, very rusty, intensely oxidized, crumbly, moderately strongly magnetic. Paragneiss, minor py and magnetite.

Mela-norite, medium grained, 196 fine grained disseminated py.

Mela-norite, M60-P40, 396 garnet, 196 very fine grained py, trace po, located 100 meters southeast of 752275. Leuco-mela-norite, medium grained, 196 sulphides, po50-py50, located 115 meters southeast of 752275. Leuco-mela-norite, medium grained, very rusty, intensely oxidized, possible assimilation of paragneiss, minor coarse grained py, located 200 meters southeast of 752275. Paragneiss-norite, assimilation zone, 3-596 garnet, 15 fine grained disseminated py.Leuco-mela-norite, medium grained, rusty, trace po.Mela-norite, rusty, medium to coarse grained, minor py, trace cp. Mela-norite, medium grained, minorPY-Paragneiss, very graphitic on planar surface, possible contact with norite. Pyroxenite, medium grained, trace cp. Leuco-norite, M40-P60, medium grained, trace po, weakly magnetic.

RESULT Pd Rh Ni

g/t g/t ppm

.07 < .03 15

< .07 < .07 < .03 11

c .07 .c .07 *:.03 6

<.07 <.07 <.03

.07 <.07

: .07

15

28

23

c .07 .c .07 <.03 36

< .03 47

< .07 < .07 < .03

< .07 < .07 < .03

< .07 < .07 < .03

<.07 <.07 <.03< .07 < .07 < .03

34

47

120

3

1317

Cuppm

57

22

24

44

24

161

99

55

82

38

13

2226



References

Atkinson, J.R. 1992. Report of Work Caribou Property, Onario, NTS 41H/16, prepared forTracer Petroleum Corp., p 6.

Atkinson, J. R. 1991. Report of Work, Caribou Lake Property, Ontario, prepared forTyloxResources Corporation, Vancouver, BC, p2.

Coleman, A.P. 1899. Copper in Parry Sound District; Ontario Bur. of Mines; Rept 8, Pt2, p 259-262.

Coleman, A.P. 1900. Copper and Iron Regions of Ontario; Ontario Bur. of Mines; Rept 9, Pt l,P143-191.

Davidson, A., Culshaw, N.G. and Nadeau L. 1982. ATectono-Metamorphic Framework for Part ofthe Grenville Province, Parry Sound Region,Ontario; in Current Research, PartA, Geological Survey of Canada Paper 82-1 A, p 1 75-1 90.

Easton, R.M. 1992. The grenville Province and the Proterozoic History of Central and SouthernOntario; in geology of Ontario, Ontario Geological Survey, Special Volume 4, Part 2,p722.

Friedman, G.M. 1957. Structure and Petrology of the Caribou Lake Intrusive Body, Ontario,Canada; Bulletin of the Geological Society of America, Vol. 68, p 1531 1 564.

Gibson, T.W.I 909. Statistical Review; Ontario Bureau of Mines; vol. 18, Pt 1, p.5-70. Hulbert, L.J., Duke,J.M., Eckstrand, O.R., Lydon, J.W., Scoates.R.F.J. 1988, Geological

Envirnoments of the Platinum Group Elements, Geological Survey of Canada, OpenFile 1440, p 148.

Kretschmar, U. 1986, Geological Report on the Caribou Lake Platinum Property, prepared forPlatinova Resources, Calgary.AB. P 12.

Macdonald, A.J, Cherry, M.E. 1988, The Platinum Group Elements in Ontario, OntarioGeological survey, Ministry of Northern Development and Mines, Open File Report5681, p279.

O.Martin, W., C. 1959. Geological Report for Twin Basin Nickel limited, Caribou Lake, Mcconkey

Township, Parry Sound District, Ontario, p 1 0-1 5.Rogers, W.R.1916. Statistical Review; Ontario Bureau of Mines; Vol. 25, Pt l, p 1- 51. Whittaker, P.J. 1987. Caribou Lake Platinum Property, Platinova Resources Litd., Report

prepared for Noramco Explorations Inc., p7. Wilson, G.C. 1994, Mafic-Ultramafic Intrusions, Base-Metal Sulphides, and Platinum

Group Element Potential of the Grenville Province in Southeastern Ontario, OntarioGeological Survey, Ministry of Northern Development and Mines, Open File Report5880, p 196.


CERTIFICATE OF QUALIFICATION

l Walter Hanych of the town of Collingwood, Province of Ontario, do hereby certify that:

1. l am a geologist and reside at # 235 11 th line Collingwood,0ntario, L9Y*3Z3. Telfax 705 445 6440

2. l graduated from Laurentian University in 1979, with an Honours Degree of Bachelor of Science in Geology.

3. l have been practicing my profession since graduation and that l am a member of the Association of Geoscientists of Ontario and a Fellow of the Geological Association of Canada.

4. l consent to the use of this report in submissions for assessment credits or similar regulatory requirements, and to regulatory authorities.

5. That l am the author of this report and supervised the field operations, and the collection of data from which this report is generated.

Walter Hanych

Collingwood, Ontario

March 16th , 2001

rj

r r rrr n n

ini j' r

nb i

P pi ,

nn

D l

Acgcgîv//-AS)S)(alj7 * ifU i ir1 î IL^

n

r

Chemex Labs Ltd,Analytical Chemists" Geochemists * Registered Assayers

5175 Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: HANYCH, WALTER

P.O. BOX 688 COLLINGWOOD, ON L9Y 4E8

Comments: ATTN: WALTER HANYCH

A9935323

CERTIFICATE A9935323

(RRG ) - HANYCH, WALTER

Project: CARIBOU LAKE P.O. # :

Samples submitted to our lab in Mississauga, ON. This report was printed on 20-DEC-1999.

SAMPLE PREPARATION

CHEMEXCODE

205226

3202

NUMBERSAMPLES

939393

DESCRIPTION

Geochem ring to approx 150 mesh0-3 Kg crush and splitRock - save entire reject

ANALYTICAL PROCEDURES

CHEMEX CODE

2538252925302539

NUMBER SAMPLES

93939393

DESCRIPTION METHODDETECTION

LIMITUPPER

LIMIT

Au g/t - part, cupel. FA-ICP FA-ICP-ARRAYPt g/t - part, cupel. FA-ICP FA-ICP-ARRAYPd g/t - part, cupel. FA-ICP FA-ICP-ARRAYRh g/t - part, cupel. FA-ICP FA-ICP-ARRAY

0.030.070.070.03

500500500500

Chemex Labs Ltd,Analytical Chemists * Geochemists * Registered Assayers


To: HANYCH, WALTER


Project: CARIBOU LAKE Comments: ATTN: WALTER HANYCH

Page Number :1-ATotal Pages :3Certificate Date: 17-DEC-1999Invoice No. : 19935324P.O. Number :Account : RRG

SAMPLE

752151752152752153752154752155

752156752157752158752159752160

752161752162752163752164752165

752166752167752168752169752170

752171752172752173752174752175

752176752177752178752179752180

752181752182752183752184752185

752186752187752188752189752190

PREPCODE

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

Ag Al As B Ba Be Bippm \ ppm ppm ppm ppm ppm

CERTIFICATE OF ANALYSIS A9935324

Ca Cd Co Ci Cu Fe Ga Hg K La Mg Mn\ ppm ppm ppm ppm \ ppm ppm \ ppm \ ppm

< 0.2 0.90 < 2 < 10 30 *: 0.5 < 2 0.64 < 0.5 20 141 11 2.89 -: 10 < 1 0.06 < 10 0.38 385< 0.2 1.64 < 2 < 10 110 < 0.5 < 2 0.90 < 0.5 28 118 45 2.35 < 10 < 1 0.18 < 10 0.85 280< 0.2 0.77 < 2 < 10 80 < 0.5 < 2 0.45 < 0.5 5 80 13 2.83 < 10 < 1 0.08 < 10 0.29 395< 0.2 0.75 < 2 < 10 120 < 0.5 < 2 0.45 < 0.5 8 81 18 2.30 < 10 < 1 0.07 < 10 0.22 445< 0.2 0.89 < 2 < 10 150 < 0.5 < 2 0.46 < 0.5 12 75 7 3.11 < 10 < 1 0.21 < 10 0.44 250

< 0.2 1.00 2 < 10 150 < 0.5 < 2 0.72 < 0.5 12 119 17 1.35 < 10 < 1 0.20 < 10 0.61 200< 0.2 0.84 < 2 *: 10 70 < 0.5 < 2 0.58 < 0.5 9 84 14 1.08 -c 10 < 1 0.09 < 10 0.32 165< 0.2 0.84 < 2 130 80 < 0.5 2 0.28 < 0.5 73 287 170 5.85 < 10 2 0.10 < 10 9.05 745< 0.2 0.87 < 2 110 130 < 0.5 < 2 0.47 < 0.5 55 429 126 4.28 < 10 < 1 0.26 < 10 6.60 625< 0.2 0.84 < 2 90 50 t 0.5 < 2 0 .40 < 0.5 69 239 102 5.29 -: 10 3 0.10 < 10 8.70 635

< 0.2 0.79 < 2 150 60 * 0.5 < 2 0.40 < 0.5 66 238 144 4.93 < 10 1 0.10 < 10 7.48 595< 0.2 0.76 < 2 110 50 -: 0.5 < 2 0.30 < 0.5 80 242 177 5.89 < 10 3 0.08 < 10 9.77 745< 0.2 1.20 < 2 170 70 *: 0.5 20 .36 < 0.5 85 333 78 6.39 *: 10 4 0.11 < 10 10.95 945< 0.2 0.81 < 2 120 60 < 0.5 < 3 0.28 < 0.5 75 242 73 5.88 < 10 3 0.11 < 10 10.30 780< 0.2 0.84 < 2 190 50 -c 0.5 < 2 0 .22 < 0.5 76 241 155 5.79 < 10 4 0.06 < 10 9.65 745

< 0.2 0.56 < 2 40 60 < 0.5 2 0.34 < 0.5 49 163 319 2.97 < 10 1 0.11 < 10 3.54 275< 0.2 0.70 < 2 < 10 70 < 0.5 < 2 0< 0.2 1.49 < 2 < 10 70 < 0.5 < 2 0< 0.2 3.47 < 2 < 10 70 0.5 < 2 2< 0.2 1.27 < 2 < 10 60 < 0.5 < 2 0

< 0.2 1.45 < 2 < 10 80 < 0.5 < 2 0< 0.2 1.14 < 2 * 10 90 < 0.5 < 2 0< 0.2 1.31 < 2 < 10 50 < 0.5 < 2 0< 0.2 1.43 < 2 < 10 10 < 0.5 < 2 0< 0.2 1.50 < 2 < 10 50 < 0.5 < 2 0

< 0.2 1.86 < 2 < 10 50 < 0.5 < 2 0< 0.2 0.86 < 2 130 90 < 0.5 < 2 0< 0.2 1.15 < 2 < 10 160 < 0.5 < 2 0< 0.2 1.24 < 2 < 10 190 < 0.5 < 2 0< 0.2 1.20 < 2 < 10 180 < 0.5 < 2 0

< 0.2 1.05 2 < 10 150 < 0.5 < 2 0< 0.2 0.98 < 2 -c 10 150 < 0.5 < 2 0< 0.2 0.86 < 2 *: 10 80 -c 0.5 < 2 0< 0.2 0.87 < 2 ^: 10 140 < 0.5 < 2 0< 0.2 1.71 < 2 < 10 80 < 0.5 < 2 0

< 0.2 1.29 < 2 < 10 210 i 0.5 ^ 2 1< 0.2 1.44 ' < 2 < 10 330 < 0.5 < 2 2< 0.2 0.69 < 2 < 10 100 < 0.5 < 2 0< 0.2 1.49 6 < 10 320 *: 0.5 < 2 0< 0.2 1.09 8 < 10 140 < 0.5 < 2 0

.51 < 0.5 21 200 109 1.77 < 10 < 1 0.12 < 10 1.75 190

.89 < 0.5 21 158 99 1.73 < 10 < 1 0.17 < 10 1.30 245

.80 < 0.5 64 161 141 3.72 10 .ci 0.04 20 0.60 140

.66 < 0.5 29 77 76 1.96 < 10 < 1 0.10 < 10 0.33 140

.93 < 0.5 61 75 99 2.54 < 10 < 1 0.12 < 10 0.38 105

.63 < 0.5 11 65 22 1.23 < 10 < 1 0.15 < 10 0.41 90

.61 < 0.5 12 84 114 5.33 -: 10 < 1 0.09 < 10 0.24 140

.73 < 0.5 82 52 82 4.08 < 10 < 1 0.03 < 10 0.29 195

.71 < 0.5 17 88 15 2.25 < 10 < 1 0.05 < 10 0.61 390

.96 < 0.5 11 66 93 1.74 < 10 < 1 0.10 < 10 0.35 105

.53 < 0.5 55 233 50 4.69 < 10 < 1 0.13 < 10 6.60 525

.48 < 0.5 43 87 32 3.75 < 10 < 1 0.32 < 10 0.71 370

.50 < 0.5 33 109 25 3.60 < 10 < 1 0.36 < 10 0.74 360

.69 < 0.5 80 98 31 6.19 < 10 < 1 0.37 < 10 0.69 395

.66 < 0.5 91 79 39 4.75 * 10 -ci 0.34 < 10 0.61 30S

.57 < 0.5 70 79 28 4.11 *: 10 < 1 0.32 < 10 0.56 290

.53 < 0.5 51 65 24 3.04 -: 10 < 1 0.12 < 10 0.54 370

.44 < 0.5 26 81 9 3.85 -: 10 < 1 0.25 < 10 0.42 405

.62 < 0.5 9 76 18 3.57 < 10 < 1 0.17 20 1.58 385

.12 < 0.5 24 70 7 2.71 < 10 < 1 0.32 < 10 0.97 395

.16 < 0.5 21 60 13 4.82 < 10 *c 1 0.52 40 0.35 685

.34 < 0.5 62 71 42 3.19 < 10 < 1 0.15 < 10 0.39 350

.53 < 0.5 13 120 49 3.40 < 10 < 1 .0.29 < 10 0.41 375

.50 < 0.5 28 109 42 3.04 < 10 < 1 ' 6..20 < 10 0.44 450

t 1 ~/

- \ i n i nCERTIFICATION:



To: HANYCH, WALTER



Page Number :1-B Total Pages : 3 Certificate Date: 17-DEC-1999 Invoice No. : 19935324 P.O. Number : Account : RRG

SAMPLE

752151752152752153752154752155

752156752157752158752159752160

752161752162752163752164752165

752166752167752168752169752170

752171752172752173752174752175

752176752177752178752179752180

752181752182752183752184752185

752186752187752188752189752190

PREPCODE

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

229329229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

Ho Na Ni P Pb S Sbppm \ ppm ppm ppm \ ppm

< i 0.06 13 1030 < 3 < 0.01 < 2< 1 0.19 37 150 < 2 0.09 < 2< 1 0.07 2 700 < 2 0.05 < 2< 1 0.06 3 750 < 2 0.05 < 2< 1 0.07 3 570 < 2 0.03 < 2

< 1 0.12 32 820 < 2 0.04 < 2< 1 0.13 22 710 < 2 0.04 < 2< 1 0.08 880 120 < 2 0.11 < 2< 1 0.10 559 610 < 2 0.12 < 2< 1 0.13 779 160 2 0.12 < 2

< 1 0.13 790 180 < 2 0.15 < 2< 1 0.09 973 90 < 2 0.18 < 2< 1 0.10 929 90 2 0.08 < 2< 1 0.07 819 200 < 2 0.08 < 2< 1 0.06 909 120 2 0.15 < 2

< 1 0.09 835 90 < t 0.36 < 2< 1 0.11 283 140 < 2 0.12 < 2< 1 0.13 224 110 < 2 0.13 < 210 0.35 98 1380 6 1.62 4

< 1 0.19 41 150 < 2 0.32 < 2

< 1 0.25 132 170 < 2 1.09 < 2< 1 0.19 15 250 < 2 0.04 < 2< 1 0.21 13 340 2 0.29 < 2< 1 0.22 137 160 < 2 1.95 4< 1 0.15 6 180 < 2 0.11 < 2

< 1 0.34 22 70 < 2 0.11 < 2< 1 0.16 558 180 < 2 0.06 < 2< 1 0.07 26 300 < 2 0.27 2< 1 0.08 16 340 < 2 0.19 2< 1 0.07 32 380 2 1.31 < 2

< 1 0.06 45 340 < 2 1.37 < 2< 1 0.07 35 380 < 2 1.04 < 2< 1 0.06 28 700 < 2 0.73 2< 1 0.05 5 720 2 0.15 < 2

3 0.06 13 1830 < 2 0.17 < 2

< 1 0.10 8 320 2 0.19 * 2< 1 0.05 4 6400 < 2 0.10 2< 1 0.05 22 400 < 2 0.54 < 2

5 0.11 11 270 < 2 0.33 < 21 0.05 16 630 < 2 0.35 < 2


Se Sr Ti Tl U V W Znppm ppm * ppm ppm ppm ppm ppm

6 10 0.09 < 10 10 104 < 10 286 33 0.05 < 10 -c 10 36 < 10 205 20 0.15 < 10 < 10 140 < 10 225 20 0.14 -c 10 < 10 129 < 10 225 15 0.16 < 10 < 10 391 < 10 18

5 23 0.07 < 10 -: 10 43 < 10 223 23 0.05 -c 10 *: 10 32 < 10 16

.ci 28 0.05 < 10 10 23 < 10 143 17 0.11 < 10 < 10 40 < 10 14

< 1 18 0.04 < 10 < 10 17 < 10 10

-: 1 25 0.05 t 10 < 10 17 < 10 12*c 1 28 0.04 < 10 10 16 < 10 12

1 27 0.04 < 10 10 21 < 10 14< 1 21 0.04 < 10 10 15 < 10 26< 1 21 0.04 < 10 10 15 < 10 16

1 12 0.06 < 10 < 10 17 < 10 21 15 0.07 < 10 < 10 22 < 10 41 15 0.06 < 10 < 10 19 < 10 25 199 0.03 < 10 30 97 < 10 204 42 0.05 < 10 < 10 39 *: 10 6

4 46 0.05 *: 10 < 10 40 < 10 104 33 0.07 < 10 < 10 46 < 10 64 49 0.12 < 10 10 159 *: 10 23 37 0.01 < 10 < 10 33 < 10 65 28 < 0.01 < 10 < 10 42 < 10 34

4 59 0.04 < 10 < 10 33 -c 10 61 21 0.05 < 10 < 10 20 < 10 206 13 0.20 *: 10 < 10 432 < 10 267 15 0.22 < 10 < 10 387 < 10 227 10 0.22 < 10 < 10 513 < 10 38

5 11 0.16 < 10 10 213 < 10 345 10 0.15 < 10 < 10 194 < 10 306 11 0.09 < 10 10 84 < 10 326 14 0.14 *: 10 .: 10 274 < 10 26

11 14 0.05 < 10 10 72 < 10 22

8 13 0.13 < 10 < 10 89 < 10 384 47 0.04 < 10 10 81 < 10 567 9 0.26 < 10 < 10 325 < 10 147 25 0.16 < 10 10 145 < 10 309 11 0.09 < 10 < 10 115 < 10 14 ( \

\ -fCERTIFICATION:.

Chemex Labs Ltd,Analytical Chemists". Geochemists * Registered Assayers


To: HANYCH, WALTER




SAMPLE

752191752192752193752194752195

752196752197752198752199752200

752201752202752203752204752205

752206752207752208752251752252

752253752254752255752256752257

752258752259752260752261752262

752263752264752265752266752267

752268752269752270752271752272

PREPCODE

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

Ag Al As B Ba Be Bippm \ ppm ppm ppm ppm ppm


ea Cd Co Cr Cu Fe Ga Eg K La Mg Mn\ ppm ppm ppm ppm * ppm ppm \ ppm \ ppm

< 0.2 0.89 < 2 -c 10 190 < 0.5 < 2 0.47 < 0.5 19 85 17 2.19 -c 10 < 1 0.29 < 10 0.48 215< 0.2 0.94 2 -: 10 260 -c 0.5 < 2 0.41 .c 0.5 23 78 5 1.80 < 10 *: 1 0.46 < 10 0.68 200< 0.2 0.91 < 2 < 10 140 < 0.5 < 2 1< 0.2 0.30 4 < 10 70 < 0.5 < 2 0

.18 < 0.5 90 93 231 3.30 < 10 < 1 0.26 < 10 1.03 235

.21 < 0.5 64 41 61 2.49 < 10 < 1 0.13 < 10 0.35 60< 0.2 0.32 < 2 .: 10 80 < 0.5 < 2 0.25 < 0.5 121 71 99 2.74 < 10 *c 1 0.10 < 10 0.43 95

< 0.2 1.11 < 2 < 10 70 < 0.5 < 2 0 .68 < 0.5 98 102 288 4.71 < 10 < 1 0.12 < 10 0.49 200< 0.2 1.20 4 < 10 50 ^ 0.5 < 2 0.65 < 0.5 123 108 316 5.52 < 10 * 1 0.09 .: 10 0.43 260< 0.2 1.32 < 2 < 10 60 < 0.5 < 2 0< 0.2 1.48 < 2 .: 10 50 -: 0.5 < 2 0< 0.2 1.04 < 2 .c 10 130 .c 0.5 < 2 0

< 0.2 0.71 < 2 < 10 60 * 0.5 .c 2 0

.79 < 0.5 60 107 163 3.30 < 10 < 1 0.10 < 10 0.46 195

.82 < 0.5 90 126 289 4.94 *: 10 < 1 0.08 < 10 0.39 270

.59 < 0.5 67 130 166 3.97 < 10 < 1 0.31 * 10 0.70 225

.33 * 0.5 26 98 53 2.70 < 10 < 1 0.12 10 0.16 120< 0.2 0.86 < 2 < 10 120 < 0.5 < 2 0.49 < 0.5 69 99 137 3.48 < 10 < 1 0.24 < 10 0.52 190< 0.2 0.87 * 2 c 10 110 -c 0.5 < 2 0< 0.2 1.14 18 < 10 200 < 0.5 < 2 0< 0.2 0.46 4 .c 10 90 < 0.5 < 2 0

< 0.2 0.83 < 2 < 10 90 .: 0.5 < 2 1< 0.2 0.82 < 2 .c 10 30 < 0.5 < 2 0< 0.2 0.51 < 2 < 10 120 < 0.5 < 2 0* 0.2 2.33 < 2 < 10 100 < 0.5 < 2 1< 0.2 1.44 < 2 < 10 160 < 0.5 < 2 0

< 0.2 1.07 < 2 < 10 40 < 0.5 < 2 1< 0.2 1.73 8 < 10 100 < 0.5 < 2 0< 0.2 1.04 < 2 < 10 170 < 0.5 < 2 0< 0.2 1.10 2 < 10 200 < 0.5 < 2 0< 0.2 1.44 2 < 10 120 < 0.5 < 2 0

< 0.2 0.77 < 2 < 10 70 < 0.5 < 2 1< 0.2 0.77 4 10 90 < 0.5 < 2 0< 0.2 0.13 < 2 < 10 60 < 0.5 < 2 0< 0.2 0.73 < 2 170 240 < 0.5 < 2 0

0.2 1.06 < 2 140 60 K 0.5 < 2 0

.c 0.2 0.33 .c 2 -c 10 20 .c 0.5 < 2 0< 0.2 1.65 2 < 10 70 .c 0.5 < 2 0< 0.2 2.16 6 -: 10 80 < 0.5 < 2 1< 0.2 1.84 < 2 < 10 40 t 0.5 < 2 0< 0.2 2.15 2 < 10 60 < 0.5 < 2 1

< 0.2 1.17 12 < 10 230 < 0.5 * 2 0< 0.2 -0.98 6 < 10 110 < 0.5 < 2 0< 0.2 0.97 12 < 10 60 < 0.5 < 2 0< 0.2 1.14 < 2 < 10 180 < 0.5 < 2 0< 0.2 0.91 4 < 10 110 < 0.5 < 2 0

.48 < 0.5 87 92 159 3.92 *: 10 < 1 0.23 < 10 0.53 210

.58 < 0.5 110 134 106 4.62 < 10 < 1 0.41 * 10 0.71 350

.57 < 0.5 106 70 55 4.07 < 10 < 1 0.15 < 10 0.43 265

.79 .c 0.5 42 113 307 4.10 < 10 * 1 0.13 20 0.31 315

.42 .c 0.5 21 68 38 2.61 < 10 1 0.06 < 10 0.33 185

.38 < 0.5 78 68 171 5.26 .c 10 -ci 0.20 < 10 0.36 180

.31 < 0.5 31 74 44 2.00 < 10 1 0.08 20 0.24 135

.75 < 0.5 41 79 96 1.80 < 10 < 1 0.26 < 10 0.53 100

.29 < 0.5 171 153 803 9.81 .c 10 1 0.46 40 0.93 465

.60 < 0.5 29 151 181 3.86 .c 10 < 1 0.37 30 0.74 320

.52 .c 0.5 27 147 26 3.35 *: 10 .ci 0.20 < 10 0.52 335

.60 < 0.5 35 183 99 3.21 < 10 < 1 0.32 < 10 0.57 405

.95 < 0.5 15 107 14 1.28 .: 10 < 1 0.18 < 10 0.49 170

.11 < 0.5 41 148 207 5.35 < 10 < 1 0.08 10 0.19 220

.10 < 0.5 * 1 259 20 4.45 -: 10 .ci 0.42 10 0.43 55

.21 < 0.5 7 399 108 1.70 < 10 < 1 0.08 < 10 0.10 65

.22 < 0.5 77 205 123 6.11 < 10 1 0.06 < 10 9.39 750

.25 < 0.5 88 404 119 6.00 : 10 .ci 0.08 < 10 10.50 940

.15 < 0.5 19 156 193 13.35 10 1 0.02 < 10 0.20 220

.90 < 0.5 12 93 63 0.82 * 10 < 1 0.07 .c 10 0.31 85

.18 < 0.5 8 95 36 0.80 < 10 < 1 0.06 < 10 0.30 85

.89 < 0.5 18 86 156 2.17 < 10 < 1 0.08 < 10 0.25 90

.12 < 0.5 7 94 54 0.99 < 10 < 1 0.07 < 10 0.30 80

.46 < 0.5 25 139 24 4.28 < 10 < 1 0.31 < 10 0.57 315

.53 < 0.5 63 114 79 4.18 < 10 .ci 0.17 < 10 0.50 280

.39 < 0.5 44 102 72 3.77 < 10 < 1 0.13 < 10 0.35 250

.82 < 0.5 22 90 3 5.86 *: 10 < 1 0.43 < 10 0.75 380

.13 0.5 11 113 57 3.45 < 10 3 0|46\ 10 ft-81 190

\ j "7 .,\ fi fi

CERTIFICATION:

Chemex Labs Ltd,Analytical Chemists * Geochemists" Registered Assayers

5175 Timbertea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: HANYCH, WALTER



Page Number :2-BTotal Pages : 3Certificate Date: 17-DEC-1999Invoice No. : 19935324P.O. Number :Account : R RG

SAMPLE

752191752192752193752194752195

752196752197752198752199752200

752201752202752203752204752205

752206752207752208752251752252

752253752254752255752256752257

752258752259752260752261752262

752263752264752265752266752267

752268752269752270752271752272

PREPCODE

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

299299299299299

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

229229229229229

Mo Na Ni P Pb S Sbppm \ ppm ppm ppm \ ppm

< 1 0.06 8 640 < 2 0.13 < 2< 1 0.04 9 820 < 2 < 0.01 < 2< 1 0.05 211 250 < 2 1.12 < 2< 1 0.03 52 330 < 2 0.71 < 2< 1 0.03 97 340 2 1.21 < 2

5 0.16 334 580 < 2 2.44 6S 0.14 389 680 < 2 3.08 < 21 0.21 172 580 < 2 1.40 26 0.20 279 730 < 2 2.29 21 0.09 265 960 < 2 1.37 < 2

6 0.10 25 690 < 2 0.65 < 2< 1 0.09 98 310 < 2 1.24 2< 1 0.09 130 300 < 2 1.68 < 2< 1 0.07 122 690 < 2 1.47 < 2< 1 0.02 34 200 < 2 1.71 < 2

18 0.03 57 7990 2 0.36 < 2< 1 0.11 21 220 < 2 0.24 < 2< 1 0.04 72 370 < 2 1.25 4< 1 0.27 18 530 < 2 0.39 < 2< 1 0.22 72 220 < 2 0.53 2

48 0.06 309 5040 2 ^.00 212 0.13 41 700 < 2 1.16 < 2

< 1 0.08 26 420 < 2 0.15 < 21 0.05 128 1210 < 2 0.63 < 2

< 1 0.19 25 1010 < 2 0.12 < 2

27 0.04 55 4730 < 2 0.34 < 233 0.02 7 1290 8 0.27 < 244 0.01 14 2780 < 2 0.08 < 2

< 1 0.06 826 170 < 2 0.14 4< 1 0.06 981 160 8 0.07 < 2

< 1 0.02 41 110 2 0.06 6< 1 0.31 53 80 < 2 0.06 2< 1 0.42 36 100 < 2 0.06 < 2< 1 0.32 22 30 2 0.28 < 2< 1 0.42 34 30 < 2 0.05 < 2

< 1 0.06 7 300 < 2 0.21 4< 1 0.07 ^54 220 < 2 1.06 2< 1 0.08 52 360 2 0.99 6< 1 0.11 3 660 4 0.01 6

5 0.06 15 420 18 1.72 < 2


Se Sr Ti Tl U V W Znppm ppm 04 ppm ppm ppm ppm ppm

4 13 0.13 < 10 < 10 101 < 10 244 9 0.17 < 10 < 10 123 < 10 385 14 0.09 < 10 10 77 < 10 244 11 0.08 .c 10 -c 10 59 -c 10 86 6 0.08 < 10 < 10 73 -e 10 6

5 26 0.06 < 10 < 10 59 < 10 64 27 0.04 < 10 < 10 47 -t 10 25 34 0.06 < 10 < 10 60 < 10 84 36 0.04 < 10 10 47 -c 10 66 14 0.11 < 10 < 10 77 < 10 18

3 24 0.04 .c 10 t 10 52 < 10 105 16 0.10 < 10 10 76 < 10 104 15 0.11 < 10 10 72 < 10 107 11 0.20 < 10 .: 10 163 < 10 268 7 0.11 x 10 < 10 99 < 10 8

11 35 0.04 < 10 10 158 < 10 346 19 0.03 < 10 < 10 60 < 10 126 14 0.11 < 10 10 213 < 10 143 81 0.04 < 10 < 10 42 < 10 324 41 0.09 < 10 < 10 40 < 10 10

12 23 0.06 < 10 20 207 < 10 326 37 0.10 < 10 < 10 112 < 10 645 14 0.19 -c 10 < 10 246 < 10 265 10 0.12 < 10 < 10 63 < 10 244 40 0.06 < 10 < 10 31 * 10 16

10 38 0.06 < 10 < 10 143 < 10 268 12 0.08 *: 10 < 10 300 < 10 424 14 0.05 < 10 < 10 204 < 10 16

< 1 31 0.03 < 10 < 10 14 < 10 162 20 0.03 < 10 10 23 < 10 46

6 4 0.25 < 10 30 931 < 10 181 59 0.02 < 10 < 10 33 < 10 102 81 0.03 < 10 < 10 36 < 10 IB2 60 0.03 < 10 < 10 26 < 10 23 75 0.05 < 10 < 10 44 t 10 6

5 19 0.24 < 10 < 10 570 < 10 245 14 * 0.12 < 10 10 164 * 10 125 16 0.07 < 10 10 72 < 10 10

10 9 0.17 < 10 20 475 < 10 66 ,-\10 8 0.15 < 10 < 10 107 < 10 214 ( l y

\ f /} i J""l

. ; \!,*,.^l' 1 *L/CERTIFICATION:



To: HANYCH, WALTER





SAMPLE

752273 752274 752275 752276 752277

752278 752279 752280 752281 752282

752283 752284 752285

PREP CODE

299 299 299 299 299

299 299 299 299 299

299 299 299

229 229 229 229 229

229 229 229 229 229

229 229 229

Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn ppm \ ppm ppm ppm ppm ppm \ ppm ppm ppm ppm 3s ppm ppm * ppm \ ppm

< 0.2 1.19 2 < 10 130 < 0.5 * 2 0.81 < 0.5 39 113 22 9.73 10 < 1 0.18 < 10 0.72 410 < 0.2 1.81 8 < 10 570 *: 0.5 < 2 1.70 < 0.5 25 79 9 4.61 -: 10 < 1 1.07 30 1.08 490 < 0.2 0.87 2 -: 10 100 *c 0.5 < 2 0.68 < 0.5 18 80 24 2.06 < 10 -ci 0.14 < 10 0.48 235 < 0,3 1.11 2 < 10 110 .: 0.5 < 2 1.14 < 0.5 33 92 44 3.03 *: 10 *: 1 0.20 < 10 0.64 400 < 0.2 1.30 4 < 10 100 < 0.5 < 2 1.01 < 0.5 19 80 24 1.90 < 10 < 1 0.14 < 10 0.58 220

0.2 1.01 10 < 10 40 < 0.5 < 2 1.16 < 0.5 19 68 161 5.33 < 10 < 1 0.13 < 10 0.32 260 < 0.2 1.17 8 < 10 100 < 0.5 < 2 1.59 < 0.5 39 98 99 4.51 < 10 < 1 0.18 < 10 0.73 450 < 0.2 1.14 10 < 10 160 < 0.5 < 2 0.52 < 0.5 57 119 55 4.45 < 10 < 1 0.30 < 10 0.61 325 < 0.2 0.34 2 K 10 70 -t 0.5 < 2 0.30 < 0.5 38 203 82 2.21 * 10 *: 1 0.13 < 10 0.54 105 < 0.2 0.38 < 2 -c 10 50 < 0.5 < 2 0.46 < 0.5 35 301 38 1.95 -: 10 *: 1 0.10 < 10 0.57 140

< 0.2 0.87 8 < 10 100 < 0.5 < 2 0.50 < 0.5 6 79 13 2.62 < 10 < 1 0.16 < 10 0.32 420 < 0.2 1.33 < 2 < 10 210 * 0.5 < 2 2.12 < 0.5 40 72 22 7.51 < 10 < 1 0.27 10 0.88 780 < 0.2 1.15 10 < 10 190 < 0.5 < 2 1.18 < 0.5 36 69 26 5.02 < 10 < i 0.30 10 0.74 490

0 f ,M v l fiCERTIFICATION: * l. J(42fcC Uf'ci

Chemex Labs Ltd.Analytical Chemists * Geochemists" Registered Assayers

5175Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: HANYCH, WALTER



Page Number :3-BTotal Pages :3Certificate Date: 17-DEC-1999Invoice No. : 19935324P.O. Number :Account : RRG


SAMPLE

752273 752274 752275 752276 752277

752278 752279 752280 752281 752282

752283 752284 752285

PREPCODE

299 299 299 299 299

299 299 299 299 299

299 299 299

229 229 229 229 229

229 229 229 229 229

229 229 229

Mo Na Ni P Pb S Sb Se Sr Ti TI U V W Znppm 't, ppm ppm ppm * ppm ppm ppm \ ppm ppm ppm ppm ppm

< 1 0.11 11 230 2 0.24 8 11 12 0.24 10 30 1455 < 10 26 1 0.05 6 3810 2 0.13 4 9 35 0.09 < 10 < 10 198 < 10 98

< 1 0.09 15 1020 < 2 0.20 2 5 20 0.09 < 10 < 10 56 < 10 26 < 1 0.07 28 2410 4 0.56 4 6 19 0.10 < 10 < 10 65 < 10 40 < 1 0.20 23 1320 < 2 0.25 < 2 5 37 0.08 < 10 < 10 50 < 10 26

15 0.10 36 4000 4 0.82 4 9 29 0.06 < 10 10 88 < 10 42 5 0.05 47 3070 < 2 1.23 6 7 22 0.08 < 10 10 93 < 10 86

< 1 0.05 34 420 2 0.71 < 2 6 11 0.16 < 10 10 317 < 10 20 < 1 0.04 47 270 < 2 0.48 < 2 7 6 0.10 < 10 < 10 85 -c 10 8 < 1 0.05 120 250 < 2 0.28 278 0.10 -: 10 .: 10 91 -c 10 8

< 1 0.06 3 910 2 0.02 < 2 6 14 0.12 *: 10 -: 10 128 < 10 20 < 1 0.16 13 5510 < 2 0.21 8 3 47 0.03 < 10 30 76 < 10 48 < 1 0.10 17 2870 < 2 0.27 6 5 26 0.09 < 10 10 90 < 10 32

(\ S

CERTIFICATION:,



To: HANYCH, WALTER



Page Number : 1Total Pages : 3Certificate Date:20-DEC-1999Invoice No. : 19935323P.O. Number :Account : R RG


SAMPLE

752151752152752153752154752155

752156752157752158752159752160

752161752162752163752164752165

752166752167752168752169752170

752171752172752173752174752175

752176752177752178752179752180

752181752182752183752184752185

752186752187752188752189752190

PREPCODE

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

2052052052O5205

2052052052O5205

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

AUg/t

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03 c 0 i 03 e 0.03< 0.03< 0.03

Ptg/t

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07 K 0.07< 0.07< 0.07< 0.07

Pdg/t

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07^ 0.07< 0.07< 0.07

Rhg/t

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< O. 03< 0.03

< 0.03< 0.03< O. 03< 0.03< 0.03

-c 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03

. < 0.03< 0.03< 0.03

\i -7

*

CERTIFICATION:.\! fj If,

Chemex Labs LtdAnalytical Chemists' Geochemists " Registered Assayers


To: HANYCH, WALTER



Page Number :2 Total Pages :3 Certificate Date: 20-DEC-1999 In voice No. : 19935323 P.O. Number : Account : RRG


SAMPLE

752191752192752193752194752195

752196752197752198752199752200

752201752202752203752204752205

752206752207752208752251752252

752253752254752255752256752257

752258752259752260752261752262

752263752264752265752266752267

752268752269752270752271752272

PREPCODE

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

AUg/t

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.06< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.06< 0.06< 0.06< 0.03< 0.03

< 0.03< 0.03< 0.06< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

Ptg/t

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07* 0.07< 0.07< 0.07< 0.07

< 0.14< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.14< 0.14< 0.14< 0.07< 0.07

< 0.07< 0.07< 0.14< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

Pdg/t

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.14< 0.07< 0.07< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

< 0.14< 0.14< 0.14< 0.07< 0.07

< 0.07< 0.07< 0.14< 0.07< 0.07

< 0.07< 0.07< 0.07< 0.07< 0.07

Rhg/t< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.06< 0.03< 0.03< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03

< 0.06< 0.06< 0.06< 0.03< 0.03

< 0.03< 0.03< 0.06< 0.03< 0.03

< 0.03< 0.03< 0.03< 0.03< 0.03 i \

\\

t-

f

r, 1 s}— ———CERTIFICATION: -.- -

Chemex Labs LtdAnalytical Chemists * Geochemists" Registered Assayers


To: HANYCH, WALTER



Page Number :3Total Pages :3Certificate Date:20-DEC-1999Invoice No. : 19935323P.O. Number :Account : RRG

CERTIFICATE OF ANALYSIS

SAMPLE

752273 752274 752275 752276 752277

752278 752279 752280 752281 752282

752283 752284 752285

PREP CODE

205 205 205 205 205

205 205 205 205 2O5

205 205 205

226 226 226 226 226

226 226 226 226 226

226 226 226

AUg/t

< 0.03 < 0.03 < 0.03 < 0.03 < 0.03

< 0.03 < 0.03 < 0.03 < 0.03 < 0.03

< 0.03 < 0.03 < 0.03

Ptg/t

< 0.07 < 0.07 < 0.07 < 0.07 < 0.07

< 0.07 < 0.07 < 0.07 < 0.07 < 0.07

< 0.07 < 0.07 < 0.07

Pdg/t

< 0.07 < 0.07 < 0.07 < 0.07 < 0.07

< 0.07 < 0.07 < 0.07 < 0.07 < 0.07

< 0.07 < 0.07 < 0.07

Rh g/t

< 0.03 < 0.03 < 0.03 < 0.03 < 0.03

< 0.03 < 0.03 < 0.03 < 0.03 < 0.03

< 0.03 < 0.03 < 0.03

A9S

i it

CERTIFICATION:

135323— '-- — :; , -^- " ••;- . , ,.......

-' ol0*jifc/. /,?K 4.

ONIMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):

304303

Survey Type(s):

W0190.00011

2001-MAR-23

2001-JUN-19

Work Report Summary

Status: APPROVED

Work Done from: 1999-NOV-15

to: 2000-JAN-18

DIATREME EXPLORATIONS INC.

ASSAY GEOL

Work Report Details:

Claim*

SO 1229459

SO 1229460

SO 1229461

SO 1231040

SO 1231041

SO 1231042

SO 1231043

External Credits:

Reserve:

Perform

310,707

S2.309

31,470

33,149

32,309

3840

3210

320,994

Perform Approve

310,707

32,309

31,470

33,149

32,309

3840

3210

320,994

SO

Applied

36,400

31,600

SO

36,400

56,000

30

30

320,400

Applied Approve

36,400

31,600

30

36,400

36,000

SO

30

320,400

Assign

33,713

3709

31,470

SO

30

S840

3210

S6,942

Assign Approve

3,713

709

1,470

0

0

840

210

56,942

Reserve

3594

SO

SO

30

SO

SO

SO

3594

Reserve Approve oue pate

3594 2002-MAR-23

30 2002-MAR-23

SO 2001 -MAR-23

SO 2002-MAR-23

SO 2002-MAR-23

SO 2001 -MAR-23

50 2001 -MAR-23

S594

5594 Reserve of Work Report* W0190.00011

5594 Total Remaining

Status of claim is based on information currently on record.

41H16NE2002 2.21022 MCCONKEY 900

2001-Jun-20 14:58 Armstrongjd Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2001-JUN-19

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

DIATREME EXPLORATIONS INC. SUITE 762 P.O. BOX 160, 100 KING ST. W. 1 FIRST CANADIAN PLACE TORONTO, ONTARIO M5X1C7 CANADA

Tel: (888)415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.21022 Transaction Number(s): W0190.00011

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

Although this work has been approved, we did notice a few expenses that were not eligible and should be reduced if submitted again. The maximum eligible vehicle gasoline expenses is SO.SS/km or you can provide all gasoline receipts. The cost of equipment rentals seems high at 3249/day. The purchase of maps and airphotos is not an eligible cost for assessment work credit.

If you have any question regarding this correspondence, please contact [email protected] or by phone at (705) 670-5858.

Yours Sincerely,

LUCILLE JEROME by email at

Ron Gashinski

Supervisor, Geoscience Assessment Office

Gc: Resident Geologist

Robert Gerald Komarechka (Agent)

Diatreme Explorations Inc. (Assessment Office)

Assessment File Library

Diatreme Explorations Inc. (Claim Holder)

Visit our website at http://wvNW.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16054

MINING LAND TENURE

MAP

o oCM

Date /Tim e of Issue Jun182001

TOWNSHIP / AREA

MCCONKEY

13:41 h Eastern

PLAN

M-0192

ADMINISTRATIVE DISTRICTS t DIVISIONSMining Division Southern Ontario

Land TltlesfReglstry Division PARRY SOUND

Mini tt ry of Natural R*sourc** District NORTH BAY

j TOPOGRAPHIC

LAND TENURE WITHDRAWALS

fHPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

M FftEMCH

a RHHTS OK PART OF FREHC h FUVtm RESf BVtO TO

C OHKHPR ELEVfll WK M5F 7 Ffl H.E J* C. FIE;

aawiiini-** on3S W-LL-C 1H4* OH

L-HU^P PWI 1

GeneraHnformatlonand Limitationsvri IrtartH Itni* Vi i Crow. 4l*v citi H tnd trnittse m4

565000ME 566000ME 567000ME 568000ME 569000ME 570000ME 571000ME 57200CME 573000ME

zo o o o o o10

o o oo00o in

o o oCOCOoin

oUTJ

Oo o oCOo

oo oIf* ttf oIO

AST-

LEGEND

Nl Cu PPM-752161

752260 * INDICATES SAMPLE WITHTWOFOLD INCREASE ABOVE BACKGROUND IN PGE

OUTCROP

EXCAVATEQ-BLASTED WORKING

GEOLOGICAL CONTACT

CARIBOU LAKE INTRUSIVE-NORITE

PYROXENITE

100 SOOt t f *

CARIBOU LAKE

CARIBOU LAKE PROPERTY

GEOLOGY-SAHPteE MAP

CRAWN BY: W. HAIWX MARCH 1001

FIGURE 5

41H16HE2002 2.21022 MCCONKEY 210

Problem Page The original page in this document had a problem when scanned and as a result was unable to convert to Portable Document Format (PDF). We apologize for the inconvenience. Problème de conversion de page Un problème est survenu au moment de balayer la page originale dans ce document. La page n'a donc pu être convertie en format PDF. Nous regrettons tout inconvénient occasionné par ce problème.

TIF_JPG_Conversion_Failure_Bad_Header_MNDM111x1

REPORT ON THE CARIBOU LAKE PROJECT · 2017. 1. 17. · REPORT ON THE CARIBOU LAKE PROJECT Southern Ontario Mining Division Prepared for Diatreme Explorations Inc. March 16th, 2001

Documents