Petrographic Study Clyde Forks Deposit

31Fe2SE9597 2.19371 LAVANT 11 010

PETROGRAPHIC S©CiJDY CLYDE PORKS DJSPOSTT LAVANT TOWNSHIP SOUTHEASTERN ONTARIO

RECEIVED SEP ^-i 1987

MINING LANDS SECTION

Jurate Lukoaiu.s B.Se, Geologist Thunder Bay Ontario June 1937 f.O SUMMARY

- T. Sanders currently holds two mining claims located in Lavknt Township,southeatern Ontario. The main economic feature of ^the property is the presence of a small,but potentially ecohoraic Cu-Ag-Sb-Hg-Ba-(Au?) deposit. Diamond drilling to 1970 delineated a mineralized barite horizon within layered calcitic marbles. This zone has been outlined for a strike length of 400 feeft,has an average thickness of 5 feet, and has a dip extent of 600[ feet. Reserves for the deposit are 147*619 tons grading 1.32 oz.Vton Ag, 0.67# Cu, 0.37# Sb, and 0.03# Hg. Barite content of this zone is estimated at 20-75#. Available data indicates the deposit is still open-ended. The mineralogy and concordant nature of the deposit suggests an epitherraal-hot spring mode of genesis. One of the more interesting aspects of this prospect is its similarity to several gold-ant iinony-roercury-barite ocourences in the region (currently held by LAC MINERALS); and indeed its general similarity to large tonnage carbonate-hosted epithermal gold deposits in Nevada (ie. Newmont©s CARLIN Deposit). The property warrants an innovative and serious approach to ;fully evaluate the existing mineralization together with an app©raisal of potential gold mineralization. Sanders is therefore seeking joint venture partners to join in the exploration/development of this property. O K) 20 30 Km.

Figure 1: Property Location Sketch 2.O INTRODUCTION

The Clyde Porks Property consists of two mining claims, located in southeastern Ontario,which are wholly owned by Todd Sanders. Diamond drilling to 1970 has outlined a small,carbonate- hosted,Cu-Sb-Ag-Hg-barite deposit which contains 147.000 tons of low-grade ore. Available data suggests that this mineralized zone is still open along strike and at depth. A petrographic study of evident mineralization was initiated to provide an enhanced appraisal of the genetic and economic features of the deposit. In addition to the main deposit previous geophysical, geochemical,and diamond drilling work has indicated the presence of other sulphide and/or barite zones on the claim group. These areas have not been adequately evaluated, especially with respect to potential gold mineralization . A sample of pyritized- silicified marble,some distance from the tetrahedrite-barite zone,assayed 0.045 oz./ton Au, thus suggesting a moderate possibility of further auriferous sulphide zones on the property. Indeed,the main reason for the acquisition of the property was its mineralogical and geological similarity with several gold-pyrite-tetrahedrite prospects in the area (currently held by Lac Minerals). Also,the style and setting of the mineralization on the property is analogous to many large-tonnage,disseminated gold deposits in North America. Further work is warranted and should attempt to fully delineate the main copper-antiraony-silver deposit,and evaluate the barite content of this zone. Any future work would ideally include a comprehensive assessment of the prospect©s gold potential. Figure 2: Detailed Property Location Sketch 3.0 PROPERTY LOCATION,DESCRIPTION,and ACCESS

The property is situated in the northwestern part of Lavant Township,located approximately 200 km. north of Kingston (Figure l),and consists of two mining claims numbered E.O. 718121 and 718124 which are wholly owned by T. Sanders. Access to the claims is facilitated by paved and all- w^ather roads leading north from the Town of Perth to the Village of Clyde Porks. The property is located 4km west of Clyde Porks and is readily accessible by a series of gravel and drivable bush roads (Pigure:2).

4.0 EXPLORATION and DEVELOPMENT HISTORY

1918-1919: T.Caldwell excavated several pits and trenches to expose a mineralized barite ©vein©jone carload of crude material was reportedly shipped to the U.S.

1957-1960: Lanark Silver Mines carried out soil geochemical, magnetic and self potential surveys; follow-up diamond drilling consisted of 6 holes totalling 1000 feet.

1964-1968: West Branch Explorations conducted a reconnaissance soil/stream geochemical survey over a wide area which outlined several significant mercury /copper anomalies. The company also undertook extensive diamond drilling in the vicinity of the main barite-tetrahedrite showing (30 holes for a total of 4000 feet). In 1967 a 90 foot adit with two short cross-cuts was driven into the main mineralized horizon by West Branch Explorations.

1969-1970: Carndesson Mines Limited carried out soil geochemistry and geological mapping of the property and drilled at least 24 holes for a total of 5300 feet.

1984: In January,1984 T.Sanders staked out the two claims which presently comprise the property. In February of the same year Sanders entered into a grubstake/option agreement with Lacana Mining Corporation who paid for the staking of 11 additional claims. In May and June,1984 Lacana carried out sampling of the main occurrence to evaluate its precious metal potential. Very disappointing gold-silver results and the fact that the old drill core was not available precluded any further involvement in the property by Lacana. In September Hpnestake Mineral Development Company visited the property and carried out limited sampling which did confirm the presence of significant copper-antimony-raercury-silver-barite mineralization.

Table 1 1 Carndesson Mines Limited, Drill Hole Assays Hole No. Core Length Mercury Copper Antimony Silver feet percent percent percent ounces 1 9.0 .035 .38 .75 2.1 3 1.7 .05 1.32 .62 2.28 45 " 4.0 .045 1.50 - .68 1.97 6" 1.6 .046 .95 .53 1.6 2. S .02 .27 .38 1.7 7 2.5 .041 .45 .21 .53 10 14.2 .016 .50 .14 .41 12 2.8 .039 .46 .22 1.30 13 S. S .024 .61 .20 .74 1.9 .025 .30 .26 1.11 14 4.2 .02 .48 .22 1.00 16 15. ©0 .031 .57 .25 1.10 19 6.2 .05 .79 .39 2.01 20 3.0 .30 .67 .43 1.99 5.0 REGIONAL GEOLOGY

The consolidated lithologies of the region are Precambrian in age and form part of the Grenville Structural Province of the Canadian Shield. In particular the Clyde Porks Area is underlain by a northeasterly-trending, linear, metasedimentary -metavolcanic belt which is characterized by a dominant NE- trending,shallowly plunging,antiformal structure (Clyde Porks Antiform) which in turn is marked by a core sequence of carbonate and clastic siliceous inetasediments (Figure:3). Metamorphism is of low amphibolite grade.

6.0 PROPERTY GEOLOGY

The property is generally underlain by a layered marble sequence with relatively thin,conformable units of amphibolite (mafic raetavolcanics) and biotite-quartz-feldspar paragneisa (clastic metasediments). This entire assemblage is marked by multiple cylindrical folds- oriented 055 O ,plunging 25-35 O ifE. Several late (Tertiary ?),small-scale,granite pegmatite dykes are also evident (Figure 4). Identified faults trend NE and approximate the regional Strike. l Amphibolite 3 Paragneiss Marble

Scale l" to l mile

Figure:3 Regional Geology 7.Q: MINERALIZATION

7.1 General Description

Identified sulphide mineralization consists mainly of high Hg-Ag tetrahedrite,pyrite,and chalcopyrite with subordinate pyrrhotite,stibnite,sphalerite,arsenopyrite,getchellite cinnabar,chalcostibnite,and molybdenite. This mineralization is fairly widespread throughout the marble assemblage,and generally consists of 1 to 2# disseminated sulphides which are mainly confined to narrow and discrete horizons. Weaker,more erratic mineralization is also evident within metavolcanics and clastic metasediments.

7*2 Main Zone Description

i This zone contains 3 to 15# disseminated to coarse blebby sulphides (mainly:tetrahedrite,pyrite,chalcopyrite and stibnite) and is about 20 feet in width. This zone is marked by a central corse of higher grade mineralization which varies in thickness from 1.5 to 15 feet (5 foot average). This zone is primarily located within a folded,barite-rich,pinkish (high Mn) marble horizon which trends 320 O725-40 O . Previous diamond drilling (Table: 1) has outlined the zone for 400 feet along strike and for 600 to 700 feet down-dip. Current inferred reserves are 147,000 tons grading 0.67# copper,0.37^ antimony,0.03^ mercury,and 1.32 oz./ton silver. Barite content is estimated at 25 "to Pegmatite

Biotite gneiss

Amphibolite

Marble

Diamond drill hole-1969 pre-1969

Mineralized outcrop

4: Detailed Property Geology l 1*0©

JOG VOO f 00 ft

.. L

(..A ^ 1S?

Seal*

Figure:5 Location Sketch Main Workings y/*.*©

Figure:6 Adit and Main Barite Pit Sample Locations r*r

A©* t ^ t*

V I S .X

l. *

Figure:? Location Sketch Surface Workings This mineralization is exposed on surface by a series of prospect pits,stripped areas,and a short adit (figures:5, 6 and 7). In tne main prospect pit a 3.5 foot wide massive barite horizon is exposed which contains 5# disseminated to patchy tetrahedrite and pyrite. Within the adit sulphides occur as stringers and patchy aggregates usually in association with irregular masses of barite.

8.0 THIN SECTION PETROGRAPHY

A polished thin section of typical mineralized barite was prepared from a sample taken from the main (barite) pit. This sample was selected as it is representitive of the deposit as a whole. ; The selected specimen consists of massive barite with 1-2,^ disseminated and nodular sulphides. d.1 Gangue Phases

BARITE: (955^),medium grained,5x6mra average,anhedral crystals in a mosaic texture. Grain boundaries are usually sutured or lobate,and may be marked by granulation. Pew grains display strained extinction and polysythetic twinning. Fluid inclusions are common while mineral inclusions are very rare.

SERICITE: (2^),occurs mainly as ragged laths and fibrous masses averaging 0.4 x 0.1 mm in size. Small sericite inclusions may be found within quartz. FIGURE P-1 : Digitized computer imago of thy thin section showing massive barite. In the centre of the imago the opaque metallics are evident as an interstitial aggregate. Calcite,quartz and sericite are the typical gangue ©Minerals, (field of veiw approx 11 mm) QUARTZ: (l-2#) anhedral grains averaging 0.4 mm in size and are interstitial to other minerals. Strained extintion and blueish inicrolites are common.

CALAITE: (O#), occurs as 0.1 ram average anhedral grains.- Calcite is often intermixed with sericite and eoiiiaonly displays polysynthetic twinning.

8.2 Opaque Phases

The opaque metallic phases constitute about 1-2^ of the sample and average 0.3 ram in size. The most abundant metallic minerals are tetrahedrite,stibnite and chalcopyrite. Minor amounts of pyrite,arsenopyrite,chalcostibnite,and getchellite are also evident. Secondary metallics include cinnabar,malachite azurite,covellite,and digenite. Opaques are interstitial to barite and occur mainly as nodualr aggregates.

TETRAHEDRITE forms anhedral grains,averaging 0.6©flm in size,which are interstitial to barite. Tetrahedrite may be rimmed by getchellite or chalcopyrite. Small inclusions of gangue are also evident.

CHAlCOPYfllTE occurs are subhedral to euhedral grains averaging O.Jfflm in size. Grain boundaries between chalcopyrite and tetrahedrite as straight. In some case chalcopyrite embays pyrite.

STIBNITE forms anhedral grains averaging lean than 0.1mm in size, It is a light grey colour and displays low bireflectance. Stibnite grains form irregular masses that are typically rimmed by ohalcostibnite. Figures P-2,3,and 4 Typical viev^rf of mineralised barite occurs as anhedral grains up to 0.5 mm,and some skeletal and irregular grains are observable. In reflected light the mineral is blueish grey and marked by high reflectance pleochroism and anisotropy. Getchelite may have inclusions and rims of chalcostibnite or chalcopyrite and inclusions of arsenopyrite.

ARSENOPYRITE forms euhedral bladed crystals of 0.3rara in length, which are usually associated with tetrahedrite and chalcopyrite. In one case arsenopyrite displays a sutured contact with barite.

CHALCOSTIBNITE mainly occurs as fine fracture fills within stibnite,tetrahedrite and barite. It also occurs as an exolution rim around getchellite.

PYRITE occurs as fine ( < 0.1 ram) anhedral grains and is marked by ragged contacts with tetrahedrite and chalcopyrite,which suggests chemical disequilibrium. Inclusions and rims of pyrite and chacopyrite are common.

CINNABAR mainly occurs as an alteration product rimming tetrahedrite.

COVELLITE occurs in trace amounts within sericite and in one case as a reaction rim between tetrahedrite and barite. Most grains are less than 0.1 ram in size and are light blue in reflected light with moderate bireflectance,strong pleochroism and anisotropy.

DIGENITE forms medium powder blue colored grains of low bireflectance and which are less than 0.1 mm in diameter. In a single instance this mineral was observed to rim chalcopyrite when in contact with getchellite and arsenopyrite. TABLE:2 CLYDE PORKS PROSPECT : ASSAY RESULTS

SAMPLE: ASSAY RESULTS

Location and Au Ag Descriptions oz./ton ^

ADIT SAMPLES; MINERALIZED ZONE

#4949 tr. 11.14 2.5 4-9 .57 .67 .38 58.18

# 18209 tr. 0.82 0.4 0.3 .02 chip samples

Wb 5 (2 ft.) 1 .24 0.7 0.3 .01

Wb 7 (6.4 ft.) 0.39 0.2 0.1 .02

Wb 8 (5 ft.) 1.44 1.0 0.3 .04

Wb 9 (5 ft.) 0.74 0.8 0.2 .03

^ARITE VEIN MAIN PIT

Cu-8-1 tr. 0.32 1.0 0.1 .04

Cu-8-2 tr. 2.96 0.8 0.5 .08

4947 tr. 1.02 0.3 0.3 .05 .04 .03 88,28 f 1 PIT 0.01 4.27 1.7 0.5 .14 f 2 PIT tr. 0.63 0.3 0.1 .02 .02 a.00

Zoltan Showing 0.045 0.04 9.0 ASSAY and ©OHE TESTING

Significant assay results are summarized in Table: 2; sample locations are presented in Figures:6 and 7.

9.1 Tetrahedrite Analyses A sample of tetrahedrite from the prospect was tested (Department of Mines Laboratory-Ottawa) and assayed "fffo copper, 21# antimony, 3.9^ mercury, and 0.37?a silver. This testing confirms that these metals are primarily related to tetrahedrite.

9.2 ©Ore© Testing

A sample of the mineralized barite vein, from the main prospect pit,waa sent to the Mines Branch Ore Dressing laboratory in 1919. The sample assayed 96.25# barite, 0.52 copper,and 1.90 oz./ton silver. The material was ground to -1000 mesh and floated in a Janney floatation apparatus. Tailings produced were clean,white and assayed 97.75# barium sulfate and also showed trace amounts of tin. TABLE 3: Selected Assay Dataj Polymetallic Gold Prospects,Lavant Township,southeastern Ontario

(after Carter et.al.,1980)

Prospect and Sample Assay Data Ownership Descriptions Ag Au Cu Sb Hg oz./ton oz./ton Darling well min©d marble 0.32 0.73 1 .10* 0.53* Prospect (pyrite+tetrahedrite) (LAC) min©d marble tr 0.02 13 ppm 0.01* min©d marble tr 0.07 34 ppm 0.03* min©d quartz vein 0.11 0.22 0.71* 0.23* 180ppb ( tetrahedrite) Green Lake min©d marble 0.16 0.12* 0.13* 170ppb Prospect (py+cpiH- tetrahedrite) { LAC ) well min©d marble 3.35 0.19 0.47* 0.18* min©d marble tr 0.05 30ppm 60ppin well min©d marble 3.01 0.10 0.36* 0.21* Joes Lake well min©d marble 1 .98 0.44 2.50* 0.58* 3 . 6 ppm Prospect ( tetrahedrite+py+cpy) ( LAC ) uiin©d marble 1 .22 0.14 0.62* min©d marble 0.75 0.13 0.50* 0 i 1 6* min©d marble 0.10 0.01 0.07* 0.04* 1 20ppb 1 .5© msv. py. lens 0.15 0.53* 0.19* 47 5 ppm 10.0 DISCUSSION

An important feature of the property is the potential for gold mineralization in addition to the known Cu-Ag-Sb- Ba-Hg deposit. The prospect is similar to several marble-hosted, disseminated,gold-pyrite-tetrahedrite showings in the area (Table: 3). Gold mineralization,at these occurrences,appears to be related to the degree of pyritization and/or silicification in marble host rocks. In terms of the overall geochemistry and style of mineralization ,the Clyde Porks Property is generally analogous to many large disseminated gold deposits in North America. The prospect is characterized by an anomalous Ag,(Au),As,Sb,Cu,Hg,Ba,and (Mo?) content which is also an overall feature of large-tonnage,replacement-type, carbonate -hosted,disseminated gold deposits such as: Carlin,Cortez and Getchell in Nevada. Gold-pyrite-tetrahedrite (+X- barite -molybdenite-stibnite) mineralization is also evident at Hemlo,Ontario and Bousquet Quebec (Figures: Q and 9)*

11.0 CONCLUSIONS

Previous work on the property has outlined a small,(but apparently open-ended),carbonate-hosted,polymetallic deposit with reserves of 147,000 tons grading 0.67/* Cu, 0.37# Sb, 0.03^ Hg,and 1.32 oz./ton silver. This zone also contains significant amounts of barite. The entire setting and style of the prospect together with the presence of low gold values indicates a moderate potential for gold mineralization. HOT SPRINGS DEPOSITS

A /^^ © *©-*s mm k-sx*,.-*Y^x A T HEAT T CHEMICAL TRAPS j ^ SOURCE ^^^ POROSITY TRAPS

(METALS: Au Sb,Mo,As,Hg,TI,Ba,W)

EPIGENETIC

(l) Carlln, Nevada (4) Golden Acres, Nevada (D Homestak*, North Dakota (D QoldfWde. Nevada (D Timmins Camp (D Cu-Au Porphyry Deposits

SYNGENETIC

m New Zealand Model

FigureB © - Epithermal Model of Gold Deposits (D C T ID GOLDEN LAC MINERALS (O SCEPTRE" CORONA-TECK CORP

CO CI 18 10 ft 3 NORTH ZONE WEST WILLIAMS WEST ZONE EAST ZONE Z IB DEPOSIT DEPOSIT Au Mo. Au nID tti Au,Ag.Mo,T* Au,Mo,Ba,Sb,Hg 3 i- At.Ag H- calc-silicates A pelites O N n n Barren Sulphide Zone n a Py, Po ^pyrite cep 1 w ID rt 3 T upper siliceous ore n DI IDin rtH- o D* i rt (b I TD3- rg H. 3 n MILE 38 OCCURRENCE LAKE SUPERIOR O 73 SOUTH ZONE n IGHWAY ZONE or or GOLIATH LOWER ZONE MUIR ZONE t 1 km O horizontal scale DI

tJin 12.0 RECOMMENDATIONS

Additional work on the prospect would first entail a detailed examination of all surface showings with attendant sampling for Au,As,Cu,Sb, Ag,Mo and Ba where warranted. , Dependant upon the results of this work a follow-up soil or lithogeochemical survey would assist in detailing zones of gold-sulphide and silver-copper-antiraony mineralization and thus provide a preliminary assessment of the property©s economic potential.

tJurate Lukosius- Sanders Thunder Bay,0nt. June 198/7^ RESUME

Jurate Lukosius-Sanders S.I.N.:458 158 490 149 Duke Street Prosp.Iic. : A45626 Thunder Bay, Ontario , status .-married P7A 5S9 © age: 27 (807)-345-7571

Objective - Desire work as an exploration geologist.

Education - Received BSc. specialist geology degree from the University of Toronto in 1982. Currently completing a Masters degree in geology at Lakehead University in Thunder Bay. Thesis : Geology, Mineralogy and Petrology of the Centre III Syenites of the Coldwell Alkaline Complex, Ontario, Canada.

- f 984 "fco present - Self-employed. Contract and geological consulting for industry, as well as research, exploration, staking and development of own properties. Job descriptions, localities and the commodities sought have been highly variable.

1986 - Worked for Homestake Mineral Development Company for a three month period. Two projects in Manitoba, both gold targets. One, along the Berens River, was a reconnaissance mapping and sampling program, A second project east of Flin Flon (Elbow lake), involved detailed mapping and sampling.

1983 - Employed by Noranda Exploration as a senior exploration geologist. Organized and ran gold exploration programs for two properties in northwestern Ontario. Work included detailed and reconnaissance mapping, humus geochemistry, blasting trenches, stripping, air photo interpretation, geophysical data interpretation, rock geochemistry, preparation of maps and reports, and the delineation of drill targets. Supervised drilling operations on a couple of base metal properties, including logging core and the preparation of reports.

1983 - Self-employed. Researched, staked, and worked on gold properties in northwestern Ontario.

1982-83 - Worked for "Mining Sector Work Program", a job creation program, based at the Thunder Bay Museum. Prepared a major report on geology and glaciation, the history of mining, mining technology, exploration and related themes, for an area of about 130 km radius around Thunder Bay. Various maps were prepared. Many data resources were collected and compiled. The work was performed in conjunction with the Ministry of Natural Resources, Geology Division, utilizing the Historical Pile, Assessment Piles and various other sources. 1982 - Employed by Homestake Mineral Development Co. as senior exploration geologist. Helicopter-supported reconnaissance geological mapping and sampling around most of the Yukon Territory and northern British Columbia, in search of economic gold mineralization. Mapping, soil, stream sediment and whole rock sampling, reports, maps, summaries, interpretations. 1982 - Employed by University of Toronto Geology Department as tutor for the third year Precambrian geology class. Supervised 45 students in laboratory sessions, consisting of thin section and hand specimen petrography, map interpretation, structural exercises and literature research.

1981 - Employed by Geological Survey of Canada, as senior mapping geologist. Helicopter-supported reconnaissance geological mapping and sampling in north-central Northwest Territories, to produce first maps over large regions of geologically complex terrain. More specifically, analysis of the Thelon Front, the eastern border region of the Slave Structural Province. Mapped and collected rock samples for a geochemical study (BSc. thesis) of an Archean volcanic complex. Study included major, minor and rare earth elements, structural interpretation, petrography, petrology and effects of metamorphism.

1980 - Employed by Newmont Exploration of Canada Ltd., as junior geological assistant. Detailed geological mapping and sampling of property northwest of Noranda, Quebec, in search of massive sulphide and gold deposits. Primarily assisted in detailed mapping and whole rock sampling. Also : individual detailed mapping project, overburden stripping, surveying, mapping and sampling of blasted trenches, individual reconnaissance mapping project, quick-logging core, electronic elevation survey, data compilation and drafting.One and a half months in the Matachewan, Ontario area.

1979 - Employed by Newmont Exploration of Canada Ltd., as junior geological assistant. Same property as above, nature of the work much the same. Altogether two months spent on overburden stripping program and detailed mapping around mine site and prospects. Detailed mapping for the rest of the summer. Assistant around drill sites. Data compilation and drafting, as well as carpentry work. Memberships - Currently a. member of the PDA and GAC. Formerly CIMM and Past-President of the University of Toronto Coleman Geology Club.

References - Please refer to the following page. Previous Employers

1986 - Horaestake Mineral Development Company Terry Chandler, Mike Flanagan Ste. 640-1380 Burrard Street Vancouver,B.C. V6Z 2H3 (604)-684-2345

1983 - Noranda Exploration Stewart Wallis, Paul Nielsen P.O.Box 2656 Thunder Bay, Ontario P7B 5G2 (807)-623-4339

1982-83 - Thunder Bay Historical Museum Gerrie Noble, Joseph Winterburn 219 South May Street Thunder Bay, Ontario (807)-623-0801

1982 - Hoinestake Mineral Development Company Jeffrey Abbott, Robert Boyd as above.

1982 - University of Toronto Geology Department Dr.A.M.Goodwin 170 College Street Toronto,Ontario M5S 1A1 (416)-978-3022

1981 - Geological Survey of Canada John Henderson, Peter Thompson and Tony Frith 588 Booth Street rras.346, 348 and 306 resp. Ottawa,Ontario K1A OE4 (613)-995-4864

1980,1979 - Newmont Exploration of Canada Limited Alan Coope, Roly Ridler, Larry Baldwin and Bob Stewart Suite 2840 Commerce Court West Toronto, Ontario M5L 1E3 (4l6)-362-1687 oq. pa^oapoad^Tpv

.091

(8*uoo*02 0*3

m Ministry of Ontario 77 Grenville Street Geoscience Northern Development Geological 11th Floor Laboratories Toronto, Ontario and Mines Survey M7A 1W4 Report •Ontarid, Telephone 965-1337

Issued MR. T SANDERS GEOLOGIST 149 DUKE STREET, THUNDER BAY,ONTARIO 04=42-87- P7A 5S9

SAMPLE SILVER k^i* NUMBER Ag oz/ton CF-1 0.60 -2 0.92

This is an interim report for samples entered in your name on JULY 30, 198; additional work will follow as soon as possible

Fees Received: PAID 38 COUPS. CARD #3670

Chris Riddle, Chief Analyst JULY 31, 1987

Except by specie! permission reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.

1270 (66/10) Ministry of Ontario 77 Grenville Street Geoscience Northern Development Geological 11th Floor Laboratories Toronto, Ontario and Mines Survey M7A 1W4 Report Telephone 965-1337

litued to.© MR. T SANDERS GEOLOGIST 149 DUKE STREET, THUNDER BAY,ONTARIO P7A 5S9

FURTHER TO CERTIFICATE 0442-87

SAMPLE CHLORINE FLUORINE ANTIMONY MERCURY NUMBER CI Sb \\. F \ Hg ppm \s ppm ppm ppm CF-1 75 100 897 170 CF-2 58 100 1473 280

This is an interim report for samples entered in your name on JULY 22,1987; additional work will follow as soon as possible

Fees Received: 16 COUPS.CARD #3670

P^*v

Chris Riddle, Chief Analyst AUG.31,1987

Except by special ptrmission reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.

1270 ( 86/10) Ministry of Ontario 77 Grenville Street Geoscience Northern Development Geological 11th Floor Laboratories Toronto, Ontario andMines Survey M7A 1W4 Report 'Ontari' Telephone 965-1337

Issued, td MR. T SANDERS GEOLOGIST 149 DUKE STREET, THUNDER BAY,ONTARIO P7A 5S9

FURTHER TO CERTIFICATE 0442-87

SAMPLE COPPER ZINC BARIUM MOLYBDENUM NUMBER Cu f*j*) o- 1 ppm " ppm 0 ppnf^©^ ppif ©O © S" © CF-1 1400 59 49.81 0 -2 3270 165 52. 2% O

This is an interim report for samples entered in your name on JULY 22, 198; additional work will follow as soon as possible Fees Received: DE PT.

Chris Riddle, Chief Analyst AUGUST 6, 1987

©t y i

Except by specie! permission reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.

1270 (86/10) , Ministry of Report of Work 41. 7 \ lyOffhern Deveiooment ^ *. M ines (Geophysical,,r , i Geological,r , i .•r.tano Geochemical and Expenditures) 3IF82SE9597 2.10371 LAVANT 900

Mining — uio not use shaded areas below. w' To'.vtisnio O' A re-3 r-t ___. k-j I.SL_., Ciaim Hoioer(s) Prosoector s Licence Kio. V S

Azores! . Jts*Ajce,.st.-.. j.j-vcv Company ^r Date of Survey {from fij ;o To:at M-:es of hne C-t ''.'U, Yr. Name ana Address o' A'jiror tot 3cc Tecnmcni report) s *T. VuLK- s^.. Credits Requasted per Each Claim in Columns at right Vlining Claims Traverseci^Lista in numerical sequence) Special Provisions Geoonysicai n"a vvs uDer For first survey: - E'ectrornacjnet'C Enter 40 days. (This includes lino cutting) - Vagnetorneter

' R.idiOrret'ic For each additional survey: usmg the same grid: Enter 20 days (for each) Geo'ogicii

Geochemical

\'an Days Days Goophystcal * Comolete reverse S'C:c - Etectromagneiic anc enter to:a:lii n&e —-JUHB Magnetometer ANQS-SEITIDN - Other

Geological

Gaochem.cai -SOUTH! :RN ONTARIO MINING DIV. •i ri3o r ne croo'ts Days per Cairn DECEIVED Note: S p-iCiai DfOVIS:0.'- : EiO.--.remarir.et credits no not onri;y —— to Airborr... Su'x-iyS. Vasne:omctcr •"~~An JUL 28 i98/ P.*::; i O'Tie T r 1C -7|8 Expenditures (excludes r- ^~VC6 Of \VorK PPM O' •**.flc; J Periormc-j on C am-i-ii U d2*Ujp AyeJU^Cc ..- ...... —— - — ——

CatcuUtion ot Exoo'Mfu'e Oiys C^eoi'i Total Totai E xDcntn'.ijras Days Credits

s 1 4-2.5". oo -5- is = 1 5 v Total numcer of Timtfi claims covered bv this report Of VvOrk. ( Total Ddvs C'e\*.*s may ô opscr;:on C',1 d i t he claim holder's ———1/îr ^ chorea. Gritcr nunvbor OT cays c'oc.trs r-or claim selected -For OfijceUe Only- ——-t Ij/êjZtuh J ' •n columns at ngnf.

JDare Rr"ccr*:on Hoic^cf or Agon: iSignaturei

Certification Verifyinn Report ut '.'/oik A./// ! hereby certifs- that ! have a personal and int. mate knowledge of the facts set forth m the Report of Work annexed hereto, having performed the v.c-t or witnessed same during and or aft-;- 1 its completion and the annexeo report is true. Nar-in j nu Postal Audruss of Person Certify. ng - ua

(o l EOJI046 l——-... —— -^-V-24-l ~^no\pji- —| J EO 31047 N EO 3,048 J

flUAc. 200Ac. y 200 Ac. 19 ^JtoMpsh l 'OOAc 20

200AC.

—r~—r- \ /rv f . 100 Ac. l 100 Ac .

200 Ac.. 15 16 ./v 100 Ac

ZOO Ac. 15 Re: Report of work (Eastern Ontario) #87-36

Mining Claims EO 718121 and 718124

Assaying:S 229.00

Petrographic Report:S 900.00

Total:SH29.00

Total for assessment S1125.00 Man-day equivalent 75 days

to be applied as follows: 718121 39 days 718124 36 days

RECEIVED SEP 2-! W

MINING UNDS SECTION INVOICE

To: T.Sanders From: J.Lukosius B.Se. 149 Duke St. Geologist Thunder Bay Ontario

June 30 198?

RE:CLYDE PORKS PETROGRAPHIC REPORT

Chargeable fees: sample preparation 3100.00 petrography SJOO.OO report S500.00

Total Amount Due S900.00

J.Lukosius B.So. Geologist ^ .^

SANDERS v A: ! . P7A 5S9 j \ 1 /Uv;

Received from T. Sanders the sum of S900.00 as payment RE: Clyde Forks Petrographic Report

J, Lukosius *o7~~

Clyde Porks Property-

Assay Expenditure Breakdown ( by assay coupon)

Sample numbers CP 1 and 2: mineralized barite

Analysis unit cost total Ag S11.50 S23.00

CI S15.00 630.00

PI &15.00 S30.00

Sb S1 1 .50 S23.00

Hg $15.00 S30.00

Cu S10.50 S21 .00

Zn C$1 0.50 S21 .00

Ba $15.00 S30.00

Mo S10.50 S21 .00

Total assay expenditures:S229.00 LANDS SECTION (claim EO 718124) -T*™ 27 J j B,N l- ""if-i \v -'

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