aslan l l l l l l l number one GOLD VENTURE TECHNICAL REPORT EXPLORATION/ DEVELOPMENT LIMITED 146 SIMCOt: STKKKT NORTH, OSHAWA, ONTARIO, L lg 4 S7,

Transcription

1 4aA12SE B2 JAMIESON GOLD VENTURE TECHNICAL REPORT number one asan EXPLORATION/ DEVELOPMENT LIMITED 146 SIMCOt: STKKKT NORTH, OSHAWA, ONTARIO, L G 4 S7, 010

2 Principas ASLAN EXPLORATION/DEVELOPMENT LIMITED Board of Directors and Founders t Ken Hoington Dae Hugo * Pau Mack * Borjo (Bi) Mein Engineering Management Engineering and Geoogy Lawyer, Lega Counse Human Resources Management ' ( * Founders ony) Pan P, Davioon Pj?e^eot Management 4IS Andre Tanguay Exporation and Property Deveopment Consutants Dunwoody and Company Accountants, Oshawa, Oht McKay, Mack, S Kisbee Barristers fi Soicitors Oshawa, Ont Barry McHae Ashburn, Ontario Geoogists Dr. W. Karvinen Kingston, Ontario Dr. J. Kirwin, P.Eng Timmins, Ontario

3 PREFACE Asian Exporation/Deveopment Ltd. is offering a joint venture and investment opportunity to expore and deveop a promising god prospect in a 19 caim bock near Timmins, Ontario. This property is adjacent to and south of the Gory Mining and Refining Caim Group which has been successfuy expored and deveoped since 1981 and which is nearing the production stage. BACKGROUND OF AREA Timmins area has been a major producer of god for over 75 years. Since 1908, we over 50 miion ounces of god have been produced from over twenty-four different deposits, making it the argest god producing camp in the word. Refer to Site Location Map (Appendix "A") GEOLOGY A doctora thesis by Dr. J. L. Kirwan (Geoogy of the Precambrian rock of the Porcupine mining area, Canada; University of London, Engand, 1968) interprets the geoogy of this area as "virtuay identica with that of the Timmins, area a few mies to the east, with which the major god deposits there are geneticay associated." In this paper,.he predicts that the Kamiscotia area wi be the next major god camp in this country. This prediction appears to be quite accurate in ight of the recent exporation work done in the area, confirming the geoogica structure as "key rock type for the ocation of god deposits in the Precambrian Shied and esewhere, as we as the fact that the visibe high grade god was found in the caim amost immediatey to the north". {See Appendix 'C') Dr. Kirwan, empoyed as a consuting geoogist on the project, has made some interesting recommendations. To quote: a) "The property is a prime exporation of god and base b) "The fesic intrusive body on these is in part porphyritic, and therefore prospecting focus for potentia god deposits." Preface

4 m Preface c) "Considering the association of the mag netic high to the southwest of Vision Lake with god mineraization, the mag netic data which it defines then must be considered to be of exceptiona import ance." d) "The caims are on the fank of such a structura dome as are the orebodies at Timmins, Kidd Creek, and Kam-Kotia." e) " Three massive suphide orebodies discov ered nearby are of 'strategic importance. 1 " In a report dated December 3, 1982, Dr. W. O. Karvinen * states: "Preiminary basa ti geochemistry reveas the presence of a broad, consistent god anomay, ocated on caims P S. P This indicates a bedrock source up-ice, probaby in the next caims to the north." (But sti within the Asian Caim Group, see Appendix 'C'.) In ight of the recommendation of these eminent geoo gists, this 19 caim group is a property of exceptiona merit, promising to be a ucrative opportunity for the discriminating investor. * In addition see Dr Karvinen's recent report pubished herein under Section 6, Report 'B 1

5 REPORT 'A' 42A12SE JAMIESON 0 10C Summary...,...,...,.. t 1. INTRODUCTION 1.1 Property and Location Accessibiity......' Topography and Faciities REGIONAL AND ECONOMIC GEOLOGY 2.1 Introductory Note Regiona Geoogy Geoogy of the Caims... 5 B 2.4 Airborne Eectromagnetic Surveys Ground Magnetometer Surveys Ground Eectromagnetic Surveys Detaied Magnetometer Survey (Caim 12557) Economic Indicators and Potentia HISTORICAL AND PREVIOUS DEVELOPMENT OF THE PROPERTY 3.1 Historica Highights Exporation and Deveopment of the North Caim Group. 3.3 Exporation of the Asian Caim Group... t. CONCLUSIONS RECOMMENDATIONS. REPORT 'B* 6. SUPPLEMENT...Submission by Dr. W. 0. Karvinen REFERENCES APPENDICES Appendix 'A 1 - Location Map Appendix 'B' - Asian Caim Group Appendix 'C 1 - Basa Ti Driing

6 Pubished: November 21, COMPILATION OP AVAILABLE INFORMATION ASLAN EXPLORATION / DEVELOPMENT LIMITED ON CLAIM GROUP PROPERTY IN ROBB AND JAMIESON TOWNSHIPS DISTRICT OF COCHRANE ONTARIO by Andre Tanguay and T W U /r^ Ray VanDenberg, P.Eng. Report 'A1

7 M Summary SUMMARY It is strategicay important that the subject property (herein caed the Asian Caim Group) is ocated on ground which is structuray very simiar to orebodies at Timmins, Kidd Creek, and Kam-Kotia. The Asian Caim Group, according to geoogist Dr. J. L. Kirwan, contains "a porphyry body/ a key rock type for the ocation of god deposits in the Precambrian Shied. The porphyry orebodies in Timmins are wrapped in godbearing quartz veins that are found in the Hoinger, Me Intyre, and Dome mines. This existence of porphyry amost DEMANDS detaied work be done on the ground." Actua god mineraization, ocated through the expo ration and deveopment of the caim group to the north, and discovery of god anomaies by consuting geoogist Dr. W. O. Karvinen, combined with the above factors makes the property one of exceptiona interest. Indeed/ this ground offers a "first-cass exporation target for god." Herein is outined a program of geophysica profiing, basa ti driing, exposure of mineraized areas, extensive samping/metaurgica testing and tria custom miing of favourabe rock. one

8 1. INTRODUCTION 1.1 PROPERTY AND LOCATION The property which is the subject of this report is a contiguous bock of mining caims owned by Asian Expo ration/deveopment Ltd. ocated in the southeastern part of Robb Township and southwestern part of Jamieson Township, approximatey 25 mies northwest of Timmins, Ontario. The property of interest, here referred to as the Asian Caim Group is a bock of 19 unpatented caims (see Location Nap, Appendix A) each comprising an area of approximatey 40 acres. The Asian caims are regis tered in the Porcupine Mining Division recording office in Timmins under the foowing numbers: P to P incusive Robb Township P to P incusive Robb Township P to P incusive Jamieson Township P to P incusive Jamieson Township Located immediatey to the north o.f the Asian Caim bock are a group of 3 patented caims (see ocation map, Appendix A) under Gory mining and Refining ownership. For future, reference,, this group wi be referred to as the patented Gory Caim Group. Two previousy producing mines,- the Kam-Kotia and Jameand, ie within 1-1/2 mies of the property. They were proific producers of copper, zinc, god, and siver unti depetion of their ore reserves resuted in their cosure. 1.2 ACCESSIBILITY The property is reached via Highway 576, an a-weather paved road, which joins Highway 101 four mies west of Timmins, Ontario. Highway 576 passes just west of the caim group enroute to Kam-Kotia Mine. The property interior is accessibe via a short ogging road which branches eastward from Highway 576 south of the Litte Kamiskotia River. Introduction two

9 m Introduction 1.3 TOPOGRAPHY AND FACILITIES The terrain of Robb, Jamieson and adjacent townships is generay fat or very genty roing his though a few scattered monadnocks may produce a oca reief exceeding 400 feet in paces. In detai in some oca ities the ground may be rugged with ow rounded ridges and his separated by narrow drift-fied vaeys and ravines. This is the case on the subject property. Forest cover consists of a mixed growth of spruce, pine, cedar, basam, popar, birch, aders, and wiow. Over burden consists of gacia tis, outwash sand and grave, and humus probaby nowhere exceeding 50 feet in thickness. The Litte Kamiskotia River which fows through the caim bock, and Vision Lake ocated on the northeast, with Kamiskotia Lake on west, a provide reiabe sources of water. Hydro eectric power is avaiabe from two transmission ines which run adjacent to the property. Nearby Timmins 1 communities serve as a reiabe source of experienced mine abour, equipment and suppies. There are no permanent camps on the property but materias for such accommodations can be easiy transported to the site. three

10 M Geoogy 2. REGIONAL AND ECONOMIC GEOLOGY 2.1 INTRODUCTORY NOTE The foowing summary of the Regiona and Economic Geoogy of the Robb-Jamieson area is an excerpt from a geoogica report on the subject property by Dr. John L. Kirwan 1, consuting geoogist. Pease note that comments made by Dr. Kirwan regarding geoogica occurrences on caims and are in reference to the caim group referred to in this report as the patented Gory Caims. {See Location Map, Appendix A). 2.2 REGIONAL GEOLOGY Ontario Geoogica Survey geoogica map 2205 at a scae of 4 mies to the inch shows the Robb-Jamieson area to be argey underain by a compex of Precambrian fesic and mafic avas and procastic rocks/ generay steepy dipping and trending northwestward and in cose as sociation with intrusions of granites and gabbro, aso of Precambrian age. A doctoria thesis by the writer (Kirwan, J. L. Geoogy of the Precambrian Rocks of the Porcupine Mining area, Canada; University of London, 1968) interprets the structure of this area as argey doma, with the avas and pyrocastic rocks wrapped around a gabbro-granite compex which probaby served as the source materia for the extrusion of the avas. Porphyries within this compex woud be, by this interpretation, actua vovanic feeders. The importance of this interpretation is that it is virtuay identica with that of the Timmins area a few mies to the east, with which the major god deposits there are geneticay associated. A simiar structura-genetic reationship is interpreted for the Texas Guf (Kidd Creek) massive sufide mining areas in the Canadian Shied, for exampe, the Noranda area of western Quebec. In the Robb-Jamieson area there appears to be good evidence for a genetic reationship between the struc tura doming and at east the sufide occurrences, for the Kam-Kotia, Genex, Jameand-Dominion Guf, and Canadian Jamieson deposits a appear to be essentiay in the same geoogica unit which wraps itsef around the granitic core to the interpreted dome, and at east one god deposit, the od Lay Mine in Turnbu Township appears to have simiar setting. For these reasons the writer beieves that the area surrounding the granitic core of the Kamiskotia Dome, in which the present caims are situated, is a prime target area for exporation for god and base metas. four

11 Geoogy 2.3 GEOLOGY OF THE CLAIMS Ontario Geoogica Survey Maps P. 694 (Robb Township) and P. 695 {Jamieson Township) * both at a scae of 1320 feet to the inch and both issued in 1971, show that the caims area is underain by Precambrian fesic and mafic intrusive rocks around which are wrapped mafic and (interpreted) fesic vocanics, the whoe cut by northstriking diabase dikes.. Work by.the writer indicates that many of these dikes in the Kamiskotia area occupy fauts, each with a eft-handed dispacement of a few tens of feet. Of particuar interest is the fact that the fesic intrusive body-on th-ese caims is in part porphyritic and therefore a prospecting focus for potentia god deposits. Outcrop is fairy sparse so that much of the geoogica information is derived from interpretation on geophysica data and is therefore ess dependabe than that derived from outcrop information. A rocks trend northwestery and dip steepy to the northeast. 2.4 AIRBORNE ELECTROMAGNETIC DATA An airborne survey using the Barringer INPUT system conducted on northeast-trending fight ines at a 660 foot spacing and a terrain cearance of 165 feet was examined in the writer's fies. No eectromagnetic conductors were recorded in this survey from the air. 2.5 GROUND MAGNETOMETER SURVEYS Ontario Geoogica Survey compiation maps P. 521 and P. 598 for Robb and Jamieson Townships respectivey, each at a scae of 1320 feet to the inch pubished in 1971 and 1970 respectivey, show isomagnetic contours from readings made by ground magnetometers in these two townships, incuding the present caim group. Compiation maps P. 676 and P. 677 show the geophysica grids from which the isomagnetic maps were made. These were cut at a 400 foot spacing and oriented northeas tery from a northwest-trending baseine. The southwest portion of the caims in Jamieson Township were not covered in the compied surveys and were covered on a reconnaissance eve by Ontario Geoogica Survey fied geophysicists. five

12 Geoogy The ground magnetometer surveys show severa features of interest. North-south oriented magnetic ridges are most certainy due to diabase dikes occupying faut panes of the Mattagami River Faut system which, for the most part, have eft-handed dispacement. In the area near and northward from the 7 mie post of the township ine, magnetic disturbances invoving irreguar "ows" pro baby refect the presence of a granitic porphyry that is mapped in that area. Esewhere on the property there are generay northwest-trending magnetic responses which refect the differing compositions of the north west-trending vocanic rocks referred to. Of particuar interest are severa northwest-trending magnetic zones, ova in shape and severa hundred to a thousand feet in ength. One of these, on caim 12557, is associated with the known god-bearing zone of the caim bock. The presence of other, simiar, magnetic zones on the property may indicate the presence of simiar mineraization. Magnetic responses off the caim bock to the east indicate that a northwest-trending faut probaby passes through the magnetic body on caim Other mag netic bodies in the southwest part of the ground appear to be simiar in faut zones, though the evidence is ess cear-cut than for that on caim GROUND ELECTROMAGNETIC SURVEYS Compiation Maps P. 676 and P. 677, aready referred to, show axes of eectromagnetic conductors ocated on the grid ines shown. No conductors are shown on the caims in Jamieson Township (athough it shoud be remembered that the southern part of this ground was not surveyed). On the ground in Robb Township there are 4 weak conduc tors in the southern part of the ground, and one weak conductor on caim in cose association with the magnetic body aready referred to, and two weak conduc tors on the adjoining caim to the west, near the tip of the magnetic body. A MAXIN eectromagnetic survey was conducted for the present owners of the ground and profies avaiabe for that part of the survey conducted on ines 2+00, 3+00, 4+00, 5+00, and 6+00 me. The exact ocation of these ines is not given, though they probaby correspond with simiary numbered ines on a ground magnetic contour map on which a northeast-trending grid from a northwest (Az 125 degrees) baseine is shown. These ines are 100 metres apart, with ine 6+00 me entering the west side of Vision Lake on Caim t SIX

13 Mf History 3. HISTORICAL AND PREVIOUS DEVELOPMENT OF THE PROPERTY 3.1 HISTORICAL HIGHLIGHTS The Robb 6 Jamieson Townships properties have had pros pecting and exporation activities carried out in their vicinity for more than 60 years. As mentioned pre viousy, severa producing mines in the area, namey the Kam-Kotia, Jameand, and Canadian Jamieson Mines Ltd., ceary indicated that occurrences of god, siver, copper, zinc, and ead coud be economicay viabe. Portions of the subject property have been partiay expored by various interests over the past 38 years incuding Mining Corporation of Canada (1946), New Wacoro Mines (1946), Kirkand Mineras (1959), Mespi Mines (1964), Canadian Lencourt Mines (1966) and Facon bridge Nicke Mines (1971). With reference to the Ontario Geoogica Survey assessment fies in Timmins, consuting geoogist John Kirwan summarizes previous work done on the ground as foows: A * Fie T311; Mining Corporation of Canada (1946) Essentiay, a program of geoogica mapping was preformed, with the principa resut being the definition of the body of quartz fedspar porphyry on the property. B. Fie T1373; Canadian Lencourt Mines Limited (1966) This program invoved geoogica mapping and a magnetometer survey, the resuts of which are on the Ontario Geoogica Survey Preiminary Maps aready referred to. C. Fie T497; Faconbridge Nicke Mines Limited (1971) This work invoved considerabe geoogica mapping, a magnetometer survey using a Me.Phar M200 magneto meter, and eectromagnetic survey with the Mc- Phar S515 vertica oop unit. Weak eectromagnetic conductors are reported on caims P854461, P854457, P854468, and P eight

14 M History 3.2 EXPLORATION S, DEVELOPMENT OF THE NORTH CLAIM GROUP Eary in 1981, Gory Mining and Refining- Ltd. Initiated a program of reconnaissance basa ti geochemica surveying under the direction of consuting geoogist Dr. W. O. Karvinen. This exporation effort was concen trated on the 3 patented Gory caims (P14405, P12556, and P12557) in order to evauate the base meta as we as precious meta potentia of the bedrock buried beneath these particuar caims. Resuts of the basa ti samping which consisted of a program of 72 dri hoes, yieded severa vaues anomaous in god, but none anomaous in base metas. 2 In the winter of 1981, under the direction of Gory Mining representatives, stripping in the vicinity of magnetic anomay "A" on Caim ocated carbonated rock, an "indicator of possibe god mineraization." Athough packsack dri hoes faied to intersect the carbonated zone", continued stripping did yied rock sampes with assay vaues up to 0.18 ounces of god to the ton. A further set of 50 basa ti sampes were taken showing ony imited anomaous god vaues but Dr. Karvinen did recommend aternative geophysica surveying owing to the "unacceptabe" nature of the ti encoun tered in samping. 3 Two hoes dried obiquey through magnetic high anomy "A" in cose proximity to earier trenching activity intersected severa "zones of carbonate ateration, minor mineraization in copper, zinc, ead and sub-ore vaues in god." The possibiity of the association of magnetic highs with zones of ateration is suggested by Dr. Karvinen, who recommends further trenching and.. driing of oca eectromagnetic conductors.4 Foowing a program of trenching and samping in the summer of 1982, an area of anomaous god vaues was defined with two sampes assaying at 0.18 and ounces of god per ton.6 In response to further recommen dations by Dr Karvinen, additiona driing of 5 hoes at various anges was undertaken in ate 1982, ocating severa more zones of ateration at various depths, in cose proximity to anomoy "A". Dr. Karvinen did not recommend further work for the Gory Caim Group. Samping preformed by geoogist Gary M. Poetsche in the spring of 1983 at the trench site, produced assay vaues of 0.005, 0.68 (with 0.26 siver), and ounces of god per ton. Documented observances of fecks of visibe god and parae quartz stringers in carbonated rock are contained in his report, aong with recom mendations for further samping 6. nine

15 M History Additiona stripping of ground at the site of anomay "A" continued through the autumn of 1983 under Gory Mining and Refining direction. These efforts were significanty successfu in exposing a arge area of carbonate rock containing some quartz veins with visibe god. Dr. J. L. Kirwan, in a visit to the pit site in ate 1983, made the foowing comments about his obser vations: The writer visited the property in the fa of 1983 just before it became snowed in. At the time the arge area of stripping was exposed, the bottom of the pit was water-fied, and stripping was procee ding northeastward, but the target area namey the magnetic high had not yet been reached. Most, if not a, of the rock exposed in the pit was of highy carbonated, neary massive, green basat or andesite. In one arge bock of 6 or 7 ton size, which was oose presumaby due to basting, two very reguar quartz veinets were seen, of about haf an inch thickness, separated from each other by about 10 inches of green massive carbonate, and absoutey parae with each other, with visibe god on the exposed surface of the more exposed vein. This god occurred as more or ess reguary spaced fecks visibe as god from severa feet distance, each severa inches from its neighbour. Other veins in the pit were said to more or ess radiate outward from the area -of the magentic high EXPLORATION OF THE ASLAN CLAIM GROUP Exporation of the subject property by the present owners was initiated in the autumn of 1982 with a program of overburden driing and basa ti samping. A tota of 78 hoes were dried aong an east-west samping ine (see Appendix "B" for ocation) which passed through the caims. Sampes from these hoes were tested to determine the distribution of basa ti across gacia ice direction, depth to bedrock, and aso anayzed for god content. In summarizing the resuts of this exporation program Dr. W. O. Karvinen verified the suitabiity of the ti encountered for this method of geochemica surveying. The most significant resuts of Dr. Karvinen's basa ti geochemica exporation was the ocation of sampes "anomaous" in god on caims P and P (see Appendix "C" for basa ti driing particuars). Dr. Karvinen indicated that these vaues are representative of a "broad, consistent god anomay", whose bedrock source is up-ice, probaby in the next caims to the north. 7 ten

16 Concusions i 4. CONCLUSIONS A quaified geoogica interpretation of the structuragenetic features of the subject property, focusing primariy on the porphyrytic compex ocated in the Asian Caim Group indicates that the ground is a "prime target for exporation for god and base metas." In ight of the god ocated through the exporation and deveopment of the Gory Caim Group at the periphery Of the magentic high, simiar magnetic zones on the pro perty, and in particuar anomay "C" (see Appendix "D"), are important as "potentia god mineraizartion tar gets". Limited overburden driing and basa ti samping has been successfu in ocating a "broad, constant god anomay" in the Asian Caim Group, the source of which may be associated with the arge magnetic anomay to the north. This concusion, of course, is based on the actua demonstration of the reationship between god mineraization and the magnetic high which is presenty emerging through the exporation and deveopment of the patented Gory Caim Group. eeven

17 m 5. RECOMMENDATIONS Concerning the initia phase of exporation for the Asian Caim Group Dr. J. L. Kirwan has recommended the foowing program: 1. Cut a detaied grid over the subject property, oriented aong the northeast striking ines (@ 100 or 50 foot spacing) and perform: a) detaied, high sensitivity magnetometer work; readings at 10 or 25 foot centres, contouring at 5 to 10 gammas. b) geoogica mapping: This woud define the ateration and serve to check out the structure. c) rock samping for geoogica studies: god, arsenic, boron, and other pathfinder eements. Recommendations B 2. Continue Dr. Karvinen's basa ti driing aong severa traverse ines oriented east-west across I the property, and in addition to the overburden assays, aso perform geochemica work on the bedrock sampes ocated. 3. Perform eectromagnetic work (combined Induced Poarization-Resistivity survey) to define the structure aready ocated or suspected. Of specia interest here are the areas near the periphery of the porphyry pug and over the magnetic highs. 4. Perform stripping of overburden and perform diamond driing on targets ocated or interpreted from the previous work. tweve

18 SUBMISSION by Dr. W.O. Karvinen Report 'B'

19 Suppement i i i i i i i i i i i i i i i i i 6. SUPPLEMENT..,Submission by Dr W.O. Karvinen "' " Background Report and Proposed Exporation Program INTRODUCTION In Sept. 1985, Asian Exporation/Deveopment Ltd acquired 19 unpatented mining caims in Robb and Jamieson townships ocated about 25 mies northwest of Timmins, Ontario. Based on previous work and a genera knowedge of the area, this property Is considered to hod good potentia for the discovery of precious metas. The purpose of this report is to provide background information on the geoogic setting, why the potentia is considered to be high and an outine of how the ground can be best tested for its economic minera potentia. 6.2 PROPERTY DESCRIPTION The most recent work on the property was a tota fied magnetometer survey in Dec and a imited basa ti samping program in Nov The work was done by Dr. W. 0. Karvinen and Associates Ltd. for the Gory Mining and Refining Ltd. who owned the ground at the time. Resuts of the magnetometer survey were used to gain some information on the bedrock geoogy, whie the ti survey indicated a patchy distribution of odgement ti, mainy in bedrock depressions. God anaysis of the tis indicate some anomaous areas In one section of the cross-ice samping ine. Overburden depths aong the ine Indicated depths ranging from O to 50 feet with the average being 21 feet. The property has been hed by various companies and individuas in the past, but most of the exporation work has been directed towards ocating base meta minerai zation. Assessment work has been submitted by six different owners on various parts of the property. These are Canadian Lenoourt (Aerston Option), r. Warne, W. Wison. H. Lookett, and Faconbridge Nicke Mines Ltd. Of these, the work by Canadian Lencourt and Fa conbridge has been most extensive. Their grids covered most of the Asian Group. Ground eectromagnetic surveys were carried out on these grids and two diamond dri hoes to test for conductors were competed. No significant mineraization was encountered. thirteen

20 M Suppement 6.3 REGIONAL SETTING The property is situated in the Kamiskotia vocanic compex which is noted for its base meta potentia. It ies between the two main Cu-Zn producers in the area, the Kamiskotia Mine to the north and the Jamieson Mine to the south. Athough numerous god ooourenoes are known in the area, no oommerioa deposit has been found. The nearest god deposits are at the arge Porcupine Camp in Timmins where over 55 miion ounces has been produced from oontinous mining dating back to LOCAL GEOLOGY The immediate area of the caims is underain by Archean thoeitic vocanics with minor komatites and andesites which may correate with the god-bearing komatites of the Lower Tisdae Group in Timmins. These are intruded by gabbroic rooks as we as by high-eve, quartz-fedspar porphyries. Immediatey to the south and west of the property are thick sequences of oaoakaine fesic vocanics. The rook has been metamor phosed under greenschist conditions and show evidence of penetrative deformation. The property covers a bedrock topographic high which is exposed in some arge outcrop areas, but on the whoe is covered by a banket of gaciofuvia sediments and ti. Because of its ocation in the Kamiskotia deta compex, it is quite probabe that significant amounts of pre-existing tis were eroded by met waters. This is evident from the preiminary ti survey which indi-* oated about 22Jt of the 78 hoes dried to have good ti. Ti is expected to be protected in the ees of bedrock highs and in some bedrock depressions. 6.5 MINERALIZATION Aterations (sericite, carbonate, siica) generay ac companying hydro-therma god mineraization are most evident in and aong the contact zones of the epizona feisic porphyries. The cosest known mineraization of this type is ocated about 1/2 mie to the south of the property near the same prophyry body which underies a arge portion of the Asian Caim. On the property, two sufide showing are iustrated on government maps. The quartz-fedspar porphyry, which measures at east one mie ong on the property is considered to have the best potentia for god mineraization. It is interesting to note that the amonaous god vaues obtained in the ti survey ooour Just south of the north contact of the prophyry. But because the property 13a

21 * ^ Suppement is extensivey covered with gacia sediments, it is important that surveys in the first phase cover the entire caim bock. 6.6 CONCLUSIONS The regiona and oca geoogica settings indicate a favourabe environment for economic god minerai zation to occur on the property. 6.7 RECOMMENDATIONS It is recommended that a first phase exporation program as outined in the next section be carried out to better define targets for detaied foow-up. 6.7/1 Proposed Exporation Program The first phase of work shoud incorporate the foowing activities: up-grading of the existing grid; seismic and ti surveys; geoogic mapping and interpretation; computer integration of mag netic, seismic, geochemica and geoogica data; concusions and recommendations. a) Grid; The existing grid with stations 400'x 100' requires upgrading as we as surveying of base and tie ines to estabish its exact shape and ocation with respect to survey benchmarks. b) Seismic: Shaow hammer seismic profies are required on the grid to map out bedrock topography. This is necessary for ocating ti sampe sites as we as interpreting future geophysica surveys (ie. I.P.) and geochemica resuts. c) Ti Survey; God anaysis of the -250 mesh fractions of ocay-derived basa ti wi esta bish the anomaous areas worthy of further expo ration. Sampe density need not be more than one site per 2500 sq. feet. d) Bedrock Mapping: Mapping of the major rock types, and particuary aterations reated to mineraization wi greaty assist in defining potentia targets. At the same time, bouders in ti wi be examined. 13b

22 i I e) Integration by Computer of the above Surveys i The computer integration of data using SCAB'S * Geosim program wi bring together and evauate a the resuts of the previous magnetic data as we as the resuts of Phase I work. f) Resuts: At the concusion of Phase I, the areas having the best potentia for the discovery of economic mineraization wi be identified in order of priority. These targets wi be substantiay smaer than the existing property area and wi be centres of concentrated foow-up testing methods. The activities and participants are summarized in Tabe 6.7/2. T W. 0. Karvinen and Associates Ltd. wi have the overa responsibiity of co-ordinating and managing the various technica components of the project. Suppement Sveriges Geoogiska AB (Swedish Geoogica) Sweden - 13c

23 1 rii a Suppement 6.7/2 SUMMARY OF EXPLORATION PROGRAM - ASIAN PROPERTY i i iii i i i i i iii PHASE I ACTIVITY a) Grid survey St f ied mapping b) Compiation of assessment data and on site super vision of above. o) Prep, of base maps d) Consutation on Ti 4 Seismic e) Seismic survey f) Ti survey g) Ti anayses (200 sampes) h) Data integration i) Map production j) - Geoogica mapping 4 report k) Report on G. P. 4 geochemistry 1) Report - BY WHOM T. Kirwan Bruoe Raine W. 0. Karvinen SCAB * W. 0. Karvinen Bruce Raine W. 0. Karvinen Bruoe Raine Dan Vaiancourt SCAB * SCAB * W. 0. Karvinen SCAB * W. 0. Karvinen. i i * Sveriges Geoogiska AB {Swedish Geoogica) Sweden 13d

24 References J ' REFERENCES I I. Dr. John L. Kirwan, "Summary Report, Tesuk Property, Robb fi Jamieson Townships, Ontario", Earth Resources Associates, November 20, g 2. Dr. WoO. Karvinen, "Summary of Work and.resuts, Tesuk Property, Robb Township," February 18, Dr. W.O. Karvinen, "Report of Overburden Driing, Tesuk Property, Robb Township (Survey 2)", February Dr. W.O. Karvinen, "Report on Diamond Driing, Tesuk Property", im August 11, 1982 c. 5. Dr. W.O. Karvinen, "Report on Diamond Driing and Trenching, Tesuk Property, Robb Township", October 23, Gary M. Poetsche, "Property Visit Report, Tesuk Property, Robb Township, Ontario", May 5, Dr. W.O. Karvinen, "Overburden Driing, East Group, Robb and Jamieson 1 Townships", December 3, Dr. W.O. Karvinen, "Background Report and Proposed Exporation Program, Asian Exporation/Deveopment Ltd Property, M Robb and Jamieson Townships, Ontario", November 22, 1985*

25 Appendices

26 APPENDIX 'A Site Location DRY CLAIMS KAMISKOTIA LAKE GROUP 'A' ' GROUP 'B Con II Con ASLAN CLAIMS Jamieson City of Timmins KEY PLAN [Sudbury V South to North Bay ft Toronto Turnbu TIMMINS ONTARIO CANADA

27 APPENDIX 'B' ASIAN Caim Group ANOMALIES'B ANOMALY 'C' (GROUP ' -not shown ASIAN CLAIM GROUP is ocated in the townships of Robb and Jamieson, District of Cochrane, withi-n the City of Timmins. The capita requirement to bring this property into fu production wi be significanty reduced due to the proximity of two major eectrica power 00 ines and Hwy 576 which is paved and maintained year round e O CO UJ

28 APPENDIX 'C' Basa Ti Driing BEDROCK^ \ SOURC God Content: (ppb) in basi ti. Interpretation Drawing, BASAL TILL DRILLING T Basa Ti Driing is a reativey inexpensive method of ocating orebodies by testing the soi for meta partices (precious and/or base) which have been disseminated by the gacier's scraping the tops of ancient vocanic vents and depositing this 'dust 1 in gacia ti down-ice from the source. In areas down-ice from the existing god mines in the Timmins area, the god dust read ings run between 10 and 20 parts per biion (PPB). Resuts on the ASLAN CLAIM GROUP show various readings up to 60 PPB. This is a good indicator of a very strong source of god on the ASLAN property.

29 42A12SE8IB JAMIESON 900 THIS SUDMITTAL CONSISTED OF VARIOUS REPORTS, SOME OF WHICH HAVE BEEN CULLED FROM THIS FILE. THE CULLED MA1ERIAL HAD BEEN PREVIOUSLY SUBMITTED UNDER THE FOLLOWING RECORD SERIES (THE DOCUMENTS CAN BE VIEWED IN THESE SERIES): /, As fan Dw. Pohh