42G07SW ECCLESTONE

Transcription

1 42G07SW ECCLESTONE 010 N.T.S. 42G REPORT ON DIAMOND DRILL PROJECT: KAP PROPERTY ECCLESTONE TOWNSHIP, KAPUSKASING, ONTARIO GEMCAL PROSPECTING SYNDICATE DIADEM RESOURCES LIMITED S o a A M MAR 3 O 2Q01 E D BY: R.J. DILLMAN 8901 REILY DRIVE MOUNT BRYDGES, ONTARIO NOL 1WO (519) MARCH 25, 2001

2 REPORT ON DIAMOND DRILL PROJECT: KAP PROPERTY ECCLESTONE TOWNSHIP, KAPUSKASING, ONTARIO GEMCAL PROSPECTING SYNDICATE l. INTRODUCTION SCOPE This report summaries the results of a diamond drill program on the KAP Property located in Ecclestone Twp., Ontario. A total of 877 metres were drilled in seven holes. Core from the program is stored a the end of access road CSR 14, on claim , GRID E. Locations of the drill holes have been plotted on 1:10,000 and 1:2,500 location maps appended to this report. Results of the program are summarized at a scale of 1:500 in vertical cross sections, also appended to this report. LOCATION AND ACCESS The Kap Property is located in Ontario (Figure 1), situated in Ecclestone Township, 40 kilometres southwest of the town of Kapuskasing (Figure 2). The property is seasonally accessible by two-wheel drive vehicle. Following the Cargill Road 35 kilometres southwest of Kapuskasing, the property can be reached via two new logging roads constructed west from the Cargill Road. The logging roads cross the east and southeast corner of the property 10 kilometres west of the Cargill Road. The property is situated on the N.T.S. sheet: 42G; Kapuskasing. MINING CLAIM LOGISTICS AND PROPERTY OWNERSHIP The Kap Property consists of 33 contiguous unpatented mining claims located in Ecclestone Township (Figure 3). Schedule 1 summarizes claim logistics. The claims are owned by Gemcal Prospecting Syndicate and currently held in trust by George Silverman of 75 Acton Road, in North York, Ontario. DATES AND PERSONAL The diamond drill project was completed during times between February 23, 2001 and March 18, Seven drill holes were drilled during the project The project ended at 918 metres of BQ core. The program was supervised by the author of this report: Robert J. Dillman of Mount Brydges, Ontario. Drill core from the program was logged by the author. Logs of each hole are included in this report. Page-1-

3 U.SA PROPERTY LOCATION GEMCAL PROSPECTING SYNDICATE KAPUSKASING REGION, ONTARIO l O km

4 o 10 Km FIGURE 2. LOCATION OF KAP PROPERTY ECCLESTONE TWP., ONTARIO GEMCAL PROSPECTING SYNDICATE N.T.S. 42G

5 J CLAIM MAP KAP PROPERTY ECCLESTONE TWP., ONTARIO OEMCAL PROSPECTING SYNDICATE

6 SCHEDULE 1: CLAIM LOGISTICS GEMCAL PROSPECTING SYNDICATE MARCH 25, 2001 KAP PROPERTY ECCLESTONE TWP., BOURINOT TWP..CARGILL TWP. ONTARIO ECCLESTONE TWP. CLAIM No. No. OF UNITS BOURINOT TWP CARGILL TWP HECTARES ,464 DATE OF RECORDING June 18, 1998 June 18, 1998 June 18, 1998 June 18, 1998 June 18, 1998 June 18, 1998 June 18, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 September 9, 1998 October 22, 1998 October 22, 1998 October 22, 1998 October 22, 1998 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 31, 1999 March 17, 2000 August 2000 August 2000 August 2000 August 2000 August 2000 August 2000 August 2000 August 2000 August 2000 STATUS abandoned abandoned

7 TOPOGRAPHY AND LAND-USE Typically, the Kap Property is defined by broad, flat terrain. Relief is low with local variations of 10 to 20 metres. The most dominate topographic feature on the property is a northeast trending ridge of outcrop crossing the west boundary of the property and forming part of the east slope of the Opasatika River valley. The central area of the property is cut by Ecclestone Creek. The creek drains northward and has poor drainage due to damming by beaver dams. Ridges and lineaments on the property are orientated northeast and northwest. Both directions coincide with large, regional geological fault structures which cut northeast through the area or with the general trend of underlying geological rock units. Outcrop exposure across the property is poor and mostly restricted to areas of higher relief. The greatest extent of outcrops are found in the vicinity of the ridge located along the western boundary of the property. The ridge of outcrop trends northeast into the central area of the property. Eastern areas of the property are swampy and outcrops are rare. Most areas of the property have been extensively logged. The operations have left isolated stands of mature poplar and buffer zones of spruce, jack-pine, birch and poplar along most of the creeks and lakes on the property. Forested areas extend over the southwest side of the property. II. REGIONAL GEOLOGY BEDROCK GEOLOGY The Kap Property is situated within a region underlain by four Archean bedrock domains (Figure 4). The domains include: 1.) a metavolcanic suite consisting of amphibolite, schists and amphibole-pyroxeneplagioclase gneiss; 2.) a metasedimentary suite consisting of greywacke, arkose, and iron formation; 3.) a migmatite-metasedimentary-metavolcanic complex consisting of supra crustal, metavolcanic and minor metasedimentary rocks, and mafic and granite gneiss; 4.) felsic intrusive suite consisting of massive granite, foliated granite and granite pegmatite. The north and west areas of the property are underlain by east-west striking metasedimentary schists and mafic metavolacinic flows belong to the Quetico Subprovince. South and east areas of the property are underlain by hornblende-quartzfeldspar gneiss and granite bodies belonging to the Wawa Subprovince. Page -6-

8 f- KAP j;, PROPERTY ip Proterozoic :1e Diabase Dikes 24 Carbonatite 21a Diabase Dikes 17a Diabase Dikes ^rc/iea/7 15 Granodiorite to granite 13 Granite 11 Tonalite to granodiorite S Migrnatized Supracrustal Rocks 7 Metasedimentary migmatites and paragneisses Felsic to intermediate rocks Mafic to intermadiath metavolcanic rocks Granulite Hacies -H 10 Km FIGURE 4. GEOLOGY j^p PROJECT, KAPUSKASING, ONTARIO GEMCAL PROSPECTING SYNDICATE

9 The sequence has been intruded by northwest trending Archean diabase dykes and northeast trending Proterozoic diabase dykes. The property lies within the LePage Fault System. This system is part of the western margin of the Kapuskasing Structural Zone (KSZ) and consists of a series of parallel northeast trending fault structures which include the Rufus Lake Fault and Opasatika Lake Fault. Both faults cross the property and are easily identifiable on the regional government airborne magnetic survey sheets. The Rufus Lake Fault can be traced through the Cargill Carbonatite complex, located 15 km northeast of the property. Faults associated with the LePage Fault System were active through the late Proterozoic. The structures exhibit both strike-slip and vertical displacement. Aeromagnetic data suggests faulting has occurred along northwest orientated fractures. In the field, these structure are evident by a series of northwest orientated lineaments. The age of these structures is uncertain since some appear to be older and some are younger than northeast orientated faults associated with the KSZ. Throughout the Archean and into the late Proterozoic, the region has been intruded by swarms of diabase dykes. The orientations of the dykes coincide with the major fault zones. Diabase is easily recognizable on the government aeromagnetic sheets. Some of the dykes trending northwest appear to cross both the northeast orientated faults and some diabase dykes suggesting that a young dyke phase has occurred in this direction. QUATERNARY GEOLOGY Surficial deposits of glacial till cover most areas of the property. Till was deposited during several pulses of the Wisconsinan glaciation. Striae found in the region suggest three ice advances have occurred, the youngest advance was orientated 1200 and two older sets orientated 1600 and 2200 (Boissoneau, 1968). On the Kap Property, a striae was recorded at an orientation of PREVIOUS WORK Diamond exploration has not been documented in this region until the release of results obtained in 1997 of a heavy mineral survey preformed by the Ontario Geological Survey over a section of the Kapuskasing Structural Zone, south of Kapuskasing, Ontario. Sporadic diamond exploration occurred through the mid-60's at Coral Rapids, north of Kapuskasing and more recently, in the Wawa region where four kimberlite and several alluvial diamonds have now been discovered. In 1987, some areas of the Kap Property were covered by airborne magnetic and electromagnetic surveys preformed on behalf of Golden Trio Resources Limited. The surveys were followed by geological work. Page -8-

10 The Kap Property was bordered to the south by Canabrava Diamond Corporation but these claims have elapsed. Berland Resources also held claims in Ecclestone Township but these have elapsed. Within the region, Agrium Resources is mining apatite from the Cargill Carbonatite located in Cargill Township. The operation produces phosphate to be used as a fertilizer. In the fall of 1999 a claim was staked adjoining to the northeast corner of the Kap Property. The claim is owned by unknown parties and ties onto patented claims covering the Cargill carbonatite. III. SURVEY RESULTS AND DISCUSSION RESULTS OF DRILL PROJECT KAP-1: J GRID KAP-1 drill hole tested ground under several boulders of which host a series of diatreme dikes. The boulders are situated close to a Cr-Ni humus anomaly coincide with a strong linear magnetic feature. Kap-1 drill intersected a 1 metre wide mafic dike, possibly of pyroxenite composition but did not intersect diatreme material. KAP-2: J GRID The KAP-2 drill hole also tested the boulder anomaly. Results were similar to the initial hole. Diatreme material was not encountered. KAP-2 tested the area at right-angle to the KAP-1 drill hole. The orientation of the diatreme dikes in the boulders are at right-angle to the direction of gneissosity of the wallrock. KAP-3a and KAP-3b: J GRID KAP-3a and KAP-3b drill holes tested a series of linear magnetic anomalies situated up-ice (with respect to glaciation) from a sequence of stream sediment heavy mineral samples found to contain hundreds of fresh bright green chrome diopside and lesser amounts of chromite, picroilmenite and orange and pink garnet. As a result of unstable bedrock, KAP-3a was abandoned at 22.6 metres. Page -9-

11 KAP-3b intersected three lamprophyre dikes ranging 0.18 m, 0.7 m and 0.3 m in width. The dikes are strongly porphyritic with pellet to euhedral shaped crystals of bright green clinopyroxene up to 2 cm wide and much lesser light blue amphibole and traces of small pellets of black mica in a very fine grained dark grey matrix of black mica and serpentine. Initial microprobe analyses of a thin-section made from one of the dikes (appendix; sample KAP-3B) indicates the matrix to be biotite-phlogopite mica H- serpentine calcite opaques (titano-magnetite). Phenocrysts are composed of zoned diopside, having iron-rich rims and chrome-rich cores with up to 1.20Xo Cr2O3, and chrome-bearing alkali amphibole with composition tending towards riebeckite. KAP-4: A GRID KAP-4 drill hole tested a potential kimberlite target defined by a Cr-Ni-Mg-Pd-Rb mobile metal ionization (M.M.I.) anomaly coincident with a strong lense-shaped magnetic feature situated up-ice from a series of stream sediment heavy mineral samples and esker samples found to contain chromite, picroilmenite, clinopyroxene and Mg-Ca almandine garnet. KAP-4 drill hole intersected sheared metasedimentary schists, mafic metavolcanic basaltic units and a strongly magnetic peridotite body. The peridotite is very-fine grained and weakly mineralized by disseminated magnetite. Pyrite occurs in trace amounts in thin serpentined fractures. The peridotite unit is approximately 54 metres wide and is believed to be the cause of the strong magnetic response detected over the area. The peridotite is potentially a platinum-palladium target and has been sampled accordingly. KAP-4 intersected a sheared metasedimentary unit situated above the peridotite unit. A 3.5 metre section hosts several fine pyrite- sugary quartz stringers. The interval has been sampled as potential gold-base metal mineralization. KAP-5: A GRID KAP-5 drill hole tested a potential kimberlite target defined by a Cr-Ni-Mg-Rb mobile metal ionization (M.M.I.) anomaly coincident with a circular magnetic feature situated in the vicinity to an esker found to contain chromite, clinopyroxene and Mg-Ca almandine garnet. Page-10-

12 KAP-5 intersected sheared and gneissic metasediments, diabase and two thin mafic dikes which are believed to be sheared equivalents of peridotite and diabase. The diabase is the probable cause of the magnetic response. KAP-6: E GRID KAP-6 tested several subtle northwest trending linear magnetic features situated in the vicinity to a group of stream sediment heavy mineral samples containing traces of the kimberlite indicator minerals: chromite, picroilmenite, chrome diopside and G9 pyrope. KAP-6 intersected a variety dikes consisting of diabase, two lamprophyre dikes, a mafic dike and a small diatreme dike. The lamprophyre dikes are between 0.45 to 0.65 metres wide, black in colour, and have a very fine grained-aphanitic matrix. Phenocrysts 0.5 cm wide are subtle, mostly dark in colour and some what indistinguishable from the groundmass. The phenocrysts are composed of the blue amphibole, pyroxene, black mica and possible olivine. Chrome diopside is present in rare amounts. The small diatreme dike encountered in the hole is ^ cm wide. The dike has a very fine grained-aphanitic matrix which is grey in colour. The matrix contains several angular clastes of wallrock and syenite up to 5 cm wide. The dike is similar to the diatreme dike found in outcrop on line 0+50W, 12+75N and to the diatreme dikes found on the J GRID. KAP-7: GRID J KAP-7 drill hole tested linear magnetic features 200 metres to the north and on strike from the magnetic features believed to represent the lamprophyre dikes intersected in KAP-3b. KAP-7 intersected six lamprophyre dikes similar in composition to the chrome diopside lamprophyre dikes in KAP-3b. The dikes range between 0.01 metres to 1.6 metres wide, the largest of which contains pellets and euhedral grains of bright green clinopyroxene 2 cm in size. Page-11-

13 DISCUSSION OF RESULTS DIAMONDS The chrome diopside bearing lamprophyre dikes are believed to be the source of abundant chrome diopside found in Gosselin Creek and the tributary cutting across the south part of GRID J. Additional analyses of the dikes are needed to determine if the dikes are the source of chromite, picroilmenite and garnets also found with the chrome diopside in the heavy mineral samples. Microprobe analyses of clinopyroxene megacrysts from the dikes indicate diopside core compositions with sufficient chrome (H 0Xo Cr2O3 ) to be classified as 'chrome diopside'. The composition differs from kimberlitic chrome diopside (type 1) due to low sodium (NaO) content (Type 2). Chrome diopside from the lamprophyre dike tested has a chrome: sodium ratio of approximately 2:1. Microprobe analyses suggests the lamprophyre dikes represent primitive deepseated magma the composition of which has an overlap with some favorable characteristics of magma associated with diamond. On the basis of this, lamprophyre dikes in holes: KAP-3b, KAP-7 and KAP-6 have been sampled for digestive analyses for diamond. The low sodium composition of the chrome diopside correspond to Type-2 chrome diopside found elsewhere on the property. The minerals were first detected in the region during the 1998 heavy mineral survey conducted by the Ontario Geological Survey (Morris, Crabtree and Averil, 1998). Heavy mineral sampling on the property has defined four additional areas where significant quantities (+50 grains per sample) of Type-2 chrome diopside occur. The areas include: GRID E, GRID l, GRID C and GRID D. The areas are situated mostly on the east side of the property in the vicinity to the Opasatika Lake Fault. Diatreme dikes (as found on GRID J) also follow this trend and occur in outcrop on GRID E and GRID l. Kimberlite indicator minerals have been found in the vicinity to all the Type-2 chrome diopside anomalies. The minerals include: chromite, picroilmenite and G9 pyrope garnet. Some Type-2 chrome diopside found on GRID D has a slight increase in sodium and is more akin to kimberlitic diopside. Page-12-

14 PLATINUM-PALLADIUM The peridotite body intersected in KAP-4 could be a potential platinum group source as suggested by the M.M.I, survey. The intrusion is situated in the vicinity to the Wawa Subprovince and Quetico Subprovince boundary. The development of the boundary and younger Quetico metasedimentary formations is thought to have influenced PGM-bearing intrusions such as Lac Des Isle to occur along the trend of the boundary. On this basis, the peridotite body in KAP-4 has been sampled accordingly. Results are expected soon. IV. CONCLUSIONS AND RECOMMENDATIONS The discovery of lamprophyre and diatreme dikes are very encouraging and demonstrate potential diamond-bearing rocks exist on the property. The dikes reveal the presence of deep penetrating tensional fractures which have been subjected to multiple phases of primitive magma. It is hoped as suggested by the presences of kimberlite minerals in creeks and tills on the property, that a phase of kimberlite magma has also occurred. Favorable results gathered by this program generate the need for additional exploration. A persistent surface exploration program is recommended to locate additional potential diamond-bearing dikes. The exploration program should focus on the east and south regions of the property, covering areas proximal to the major faults trending northeast through the area. A combination program consisting of surface geological prospecting and ground geophysics is required to guide additional diamond drilling on the property. Prospecting in areas of outcrop has demonstrated the potential for dikes to be found. Continuing ground magnetometer and VLF surveys is also strongly recommended and should be supported by additional heavy mineral sampling of creeks and tills. Page-13-

15 An estimate of costs for an additional phase of exploration includes: Prospecting Heavy Mineral Sampling Ground magnetometer and VLF surveys Analyses S8,200 15,000 9, ,200 Respectfully submitted, Robert J. Dillman Geologist Project Manager B.Sc. March 25, 2001 Page -14-

16 CERTIFICATE l, ROBERT JAMES DILLMAN, do hereby certify as follows: [1.] l am a Mining Exploration Geologist and that l reside and carry on business at 8901 Reily Drive, in the town of Mount Brydges, Ontario. [2.] l am a Graduate of the University of Western Ontario, and hold a Bachelor of Science Degree and majored in Geology. [3.] l have been practicing my profession as a Geologist since [4.] l am a Licenced Prospector in Ontario and have been actively engaged as a Professional Prospector since [5.] My report, dated March 25, 2001, titled: "REPORT ON DIAMOND DRILL PROJECT, KAR PROPERTY ECCLESTONE TOWNSHIP, GEMCAL PROSPECTING SYNDICATE DIADEM RESOURCES LIMITED" is based on information collected by myself between February 23, 2001 and March 25, Any other information gathered from other sources has been cited in this report. [6.] The information given in this report is as accurate as to the best of my knowledge and l have not stated false information for personal gain. [7.] l authorize Gemcal Prospecting Syndicate to use this report or any part of, at their discretion but only if proper credit is given. Permission must be given to any other parties wishing to use this report in whole or part. [8.] l have no ownership or financial interest in the property. [9.] l am a member of the Geological Association of Canada. ROBERT JAMES DILLMAN, B.Sc. GEOLOGIST, Datecrat~Mount Brydges, Ontario This 25th day of March, 2001 Page -28-

17 REFERENCES CON'T Ontario Department of Mines Kapuskasing Sheet; Ontario Department of Mines, preliminary geological map P.398, scale 1 inch to 2 miles. Ontario Department of Mines Hearst Sheet; Ontario Department of Mines, preliminary geological map P.397, scale 1 inch to 2 miles. Ontario Geological Survey Bedrock geology of Ontario, east-central sheet; Ontario Geological Survey, Map 2543, scale 1:1,000,000. Ontario Geological Survey Quaternary geology of Ontario, east-central sheet; Ontario Geological Survey, Map 2555, scale 1:1,000,000. Ontario Geological Survey, Kimberlite Pipe Modeling From Magnetic Grids, ERLIS Data Set Scott, G Report of Ground Magnetometer and VLF-electromagnetic surveys on the KAP Property, Ecclestone Township, Ontario. Assessment report. Scott, G Report of Geology and Rock Sampling, KAP Property, Ecclestone Township, Ontario. Assessment report. Stephenson, D.M., Morris, T.F. and Crabtree, D.C Kimberlite, base metal and gold exploration targets based upon heavy mineral data derived from surface materials, Opasatika Lake area, northern Ontario; Ontario Geological Survey, Open File Report 5982, 66p. Page -25-

18 REFERENCES Airborne Magnetic Survey, Opasatika, Fergus, Rykert, Caithness Townships, Ontario. Golden Trio Resources, unpublished assessment report. Airborne Magnetic Survey, Ecclestone Twp., Ontario. H. Ferderber Geophysics Ltd. For Golden Trio Resources. Berger, B.R Geology of the Hearst-Kapuskasing area, District of Cochrane: Ontario Geological Survey, Open File Report 5599, 88p. Boissonneau, A.N Glacial history of northeastern Ontario, l. The Cochrane-Hearst area; Canadian Journal of Earth Sciences, v.5, p Dillman, R.J Results of Gemcal's heavy mineral survey for kimberlite indicator minerals on the Kap Property, Ecclestone Twp., Kapuskasing, Ontario: Assessment report. Dillman, R.J Report on additional heavy mineral sampling on the KAP Property, Ecclestone Township, Kapuskasing, Ontario: Assessment report. Fipke, C.E Significance of chromite, ilmenite, G5 Mg-almandine garnet, zircon and tourmaline in heavy mineral detection of diamond bearing lamproite; in Diamonds: Characterization, Genesis and Exploration, Proceedings of the Fifth International Kimberlite Conference, Araxa, Minas Gervais, Brazil, P.366. Gurney, J.J A correlation between garnets and diamonds in kimberlite; in Kimberlite Occurrence and Origin: A Basis for Conceptual Models in Exploration, University of Western Australia, Perth, Western Australia, publication no.8, p Morris, T.F., Carbtree, D.C. and Averil, S.A Kimberlite, base metal and gold exploration targets based upon heavy mineral data derived from surface materials, Kapuskasing, Northeastern Ontario; Ontario Geological Survey, Open File Report 5967, 41 p. Ontario Department of Mines Magliadery Creek; Ontario Department of Mines, aeromagnetic series map 2238 G, scale 1:63,360. Page -22-

19 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-1 LOCATION GRID: GRID J LINE: 2+10 N 2+70 W COLLAR ELEVATION (metres above sea level): 256 m a.b.s. BEARING FROM TRUE NORTH: 285" DECLINATION: 8"W DIP OF HOLE AT COLLAR: 46" TOTAL FOOTAGE (metres) 50m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: February 28, 2001 March 1, 2001 March 1,2001 Robert J. Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Limited DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property TOWNSHIP: Ecclestone Twp. FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT 0-5 Overburden Quartz-feldsparbiotite-hornblende white to grey mottled by black and green specks, alternating white fine to medium grained quartz-plagioclase feldspar rich sections with -^0.5 cm inclusions of biotite rich sections and d.o cm inclusions of green hornblende-chlorite rich sections, moderate to strong gneissosity, several white quartz stringers :1.0 cm wide at random orientations throughout section. Increasing biotite through sections m and m m: strongly folded gneissosity m: waving gneissosity roughly perpendicular to core axis m: several 1 cm fractures 20D C.A., one filled by white quartz m: occasional pinkish feldspar-quartz rich sections, most :10 cm wide some with 1 cm black hornblende clots, hornblende content decreasing down section m: thin well-defined quartz-feldspar rich sections ^ cm wide and biotite-chlorite-quartz-feldspar sections increasing in width down section m: fine grained, weak gneissosity 700 C.A., very fine grained fenitized or ankerite-filled fracture ^.4 cm wide at 35.0 m orientated 850 C.A. Page l of 2

20 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: 285" m. E KAP-1 R- J- Dillman KAP Property DECLINATION: 8"W m 42G/ m N FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Quartz-feldsparbiotite-horn blende m: fenitized fracture 900 C.A m: increasing gneissosity 500 C.A m: increasing silicification down section, stronger marginal to contact with minor brecciation and chloritization Mafic dike dark green mottled by white feldspar, massive, medium to coarse grained, consists of interstitial hornblende-epidoteplagioclase, section cut by several pinkish-white quartzfeldspar-chlorite stringers ^.0 cm wide orientated perpendicular to core axis, largest between m at 800 C.A.. upper contact gradational, lower contact marked by 7 cm ragged quartz-feldspar vein, no defined orientation Quartz-feldsparbiotite-hornblende same as above, white to grey mottled by black and green specks, alternating white fine to medium grained quartzplagioclase feldspar rich sections with ^.5 cm inclusions of biotite rich sections and -clo cm inclusions of green hornblende-chlorite rich sections, moderate to strong gneissosity m moderate gneissosity, minor silicification at contact m: increase in fine grained quartz-feldspar content, possibly mylonitized, decrease in biotite m very fine grained, mylonitized?, little to no biotite or gneissosity m: increasing biotite and gneissosity 450 C.A m: fine grained fenitized section, O.2 cm empty vugs and hairline rusty fractures at various core angles m: increasing quartz-feldspar with green chloritehornblende-biotite inclusions or horizons, hornblende subhedral so. 5 cm crystals. Gneissosity: 5m; 620 C. A., 8m; 450 C. A., 19m; 620 C. A., 32m; 760 C.A., 42m; 760 C.A., 47m; 450 C.A. 50 End of hole Page 2 of 2

21 DRILL HOLE KAP-2 DATE HOLE STARTED: March 1,2001 LOCATION GRID: GRID J LINE: 1+72 N 2+70 W DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO -^ COLLAR ELEVATION (metres above sea level): 258 m a.b.s. DATE HOLE FINISHED: March 3, 2001 BEARING FROM TRUE NORTH: 15" DECLINATION: 8"W DATE LOGGED: March 3, 2001 DIP OF HOLE AT COLLAR: 45" LOGGED BY: TOTAL FOOTAGE (metres) 78m Robert J. Dillman MAP REFERENCE: 42G/7 DATE SUBMITTED: March 25, 2001 U.T.M. COORDINATES: m. E m. N. SIG CLAIM : EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Limited DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property TOWNSHIP: Ecclestone Twp. FOOTAGE (metres) 0-6 Overburden Quartz-feldsparbiotite-homblende ROCK TYPE DESCRIPTION SAMPLE pinkishish-white alternating with greyish biotite rich bands and blackish green hornblende-biotite clots or inclusions, moderate gneissosity: 8m; 360 C.A m: minor folding, contorted gneissosity Diabase Dike dark green mottled by white plagioclase feldspar, minor green epidote, fine grained, upper contact sharp at 400 C.A., lower contact gradational less defined 720 C.A., weakly magnetite Quartz-feldsparbiotite-hornblende same as above, alternating sections of silicified-mylonitized and non-deformed/altered sections of varying wides m: silicified gneiss, no foliation, pinkish-white, coarse grained with ^.0 cm wide dull green hornblende-chlorite clots m: strong gneissosity 360 C.A m: brecciated silicified section, very fine grained mylonitized, pinkish green, some epidote, upper contact sharp at 280 C.A., lower contact sharp at 420 C.A m: increasing thin fine grained silicified and thin blackish-orange grano-diorite intervals down section. Gneissosity: 21m; 40" C.A., 27m; 31 0 C.A., 29m; 400 C.A., 30m; weak folding 860 C.A. INTERVAL FROM TO ASSAY RESULT Page l of 3

22 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: m. E KAP-2 R- J- Dillman KAP Property DECLINATION: 8"W 45" 78 m 42G/ m N FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Quartz-feldsparbiotite-hornblende m: fine grained silicified and brecciated section, sharp parallel contacts 460 C. A m: blackish-orange-white diorite?, medium grained, moderate contorted gneissosity C. A m: brecciated silicified section, fine grained, upper contact 900 C. A., lower contact 200 C. A m: gneiss, minor zones of contortion and alterationbrecciation and silicification ^0 cm wide m: massive silicified section, very fine grained quartzfeldspar, weak to no gneissosity, trace very fine biotite m: gneiss, contorted, upper contact sharp 900 C.A., lower contact sharp 450 C. A m: alternating fine grained orange-white quartzfeldspar sections and gneissic sections with moderate gne ssosity 220 C.A m: 3 cm light-green fine grained gauge filled fracture 390 C. A., occasional similar hairline fracture associated with strong silicified and brecciated sections through m Mafic dike medium grained dark green mottled by white feldspar, massive, consists of interstitial hornblende-epidote-plagioclase-quartz, decreasing plagioclase-quartz down section, similar to mafic dike in KAP-1, upper contact gradational, dark green medium grained pyroxenite above lower contact, sharp at 520 C. A Quartz-feldsparbiotite-horn blende same as above, white to grey mottled by black and green specks, alternating fine grained weakly brecciated massive sections with moderate gneissic sections Gneissosity: 53m; 380 C.A., 62m; 300 C.A m: chlorite-hornblende-biotite clots in medium grained quartz-feldspar matrix m: increasing mega-brecciation, some large pinkish sugary very fine grained fragments through 64-65m, 1-20Xo fine Page 2 of 3

23 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-2 LOGGED BY: R. J. Dillman PROPERTY NAME: KAP Property BEARING FROM TRUE NORTH: 15" DECLINATION: S'W DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) MAP REFERENCE: 78 m 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Quartz-feldsparbiotite-homblende m: alternating gneiss and fine grained silicified/mylonitized sections, gneissic section increasing down section, occasional hornblende-chlorite-rich section which also increase in association with gneissosity. Gneissosity: 67m; 380 C.A m: orange feldspar minor quartz, massive, medium grained, cut by blackish grey hairline fractures 420 C. A m: gneiss, moderate gneissosity. Gneissosity: 70m; 320 C. A., 77m; 220 C.A. 78 End of Hole Page 3 of 3

24 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO^^^ DRILL HOLE KAP-3A LOCATION GRID: GRID J LINE: 1+20N 4+20E COLLAR ELEVATION (metres above sea level): 257 m a.b.s. BEARING FROM TRUE NORTH: 1250 DECLINATION: s'w DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 22.6m abandoned MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: March 3, 2001 March 4, 2001 March 5, 2001 Robert J. Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Limited DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property TOWNSHIP: Ecclestone Twp. FOOTAGE (metres) 0-10 Overburden Quartz-feldsparbiotite-hornblende ROCK TYPE DESCRIPTION SAMPLE white quartz-feldspar sections alternating with grey sections mottled by disseminated fine black biotite rich bands and blackish green hornblende-chlorite-biotite clots or inclusions, moderate gneissosity, occasional section with pinkish-orangered rusty? Halo surrounding mica inclusions. Gneissosity: 14m; 360 C.A Diabase Dike fine grained, dark green mottled by white plagioclase feldspar, well foliated parallel contacts, minor green epidote, upper contact sharp at 380 C.A., lower contact 370 C.A., weakly magnetic Quartz-feldsparbiotite-hornblende 22.6 End of Hole Abandoned due to caving. same as above, alternating sections grey sections mottled by disseminated fine black biotite rich bands and blackish green hornblende-chlorite-biotite clots or inclusions, moderate gneissosity. 16.8m: 3 cm epidote veinlet 400 C.A. perpendicular gneissosity at320 C.A m: occasional hornblende-biotite rich inclusion/ clot m: several hornblende-biotite rich inclusion/ clot. INTERVAL ASSAY RESULT Page l of l

25 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO-^ DRILL HOLE KAP-3B LOCATION GRID: GRID J LINE: 1+20N 4+19E COLLAR ELEVATION (metres above sea level): 257 m a.b.s. BEARING FROM TRUE NORTH: 125" DECLINATION: DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 150m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: SIGNATURE March 4, 2001 March 5, 2001 March 7, 2001 Robert J. Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Limited FOOTAGE (metres) 0-10 Overburden DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property ROCKTYPE DESCRIPTION SAMPLE TOWNSHIP: Ecclestone Twp. INTERVAL FROM l TO ASSAY RESULT Quartz-feldsparbiotite-horn blende Feldspar-quartzfuchsite? shear zone white feldspar plus quartz mottled by dark grey and grey hornblende and fine biotite, fine to medium grained, weak to moderate gneissosity, finer grained section show weaker gneissosity, occasional disseminated biotite and/or dull green hornblende-chlorite rich section usually ^0 cm wide, occasional pinkish red rusty? halo surrounding some biotite mica grains increases down section. 16.7m: 5 cm of fine dull green hornblende-chlorite 280 C.A m: 1 cm epidote veinlet 450 C.A., fenitized margins m: minor brecciated sections cut by hairline fractures 520 C.A. perpendicular to gneissosity at 280 C.A m: massive, very weak to no gneissosity, fine grained, some biotite 'peppered' through core, occasional hornblendeclot some with epidote, slight increase in hornblende-epidote down section. Gneissosity: 12m; 28" C.A., 16m; 400 C.A., 22m; 580 C.A., 32m;600 C.A., 49m; 35" C.A. well foliated shear 150 C.A., fine grained, sugary, dull orangebrown white and bright green, strong degree of brecciation, milling and recrystallization, S-20% bright green fuchsite? on Page l of 4

26 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: m. E KAP-3B Robert J. KAP Property DECLINATION: 45" 150m 42G/ m N Dillman 8"W FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Feldspar-quartzfuchsite? shear zone planar cleavages in wall rock cm marginal either side of shear, S-15% fuchsite associate with carbonated fragments in shear, contacts sharp, parallel, 150 C.A Quartz-feldsparbiotite-hornblende same as above, slight increase in biotite-hornblende rich horizons, weak gneissosity m: 10^0 fine cubic pyrite with hornblende-biotite rich segment m: greyish-white very fine grained quartz vein 400 C. A. orientated perpendicular gneissosity at 320 C. A., contacts sharp, trace fine pyrite on lower contact m: occasional hornblende-biotite rich section with trace of pyrite m: fine grained grey quartz vein, parallel gneissosity at 340 C, A., contacts sharp, scattered fine biotite throughout, trace pyrite magnet te m: strong gnessosity, increase in biotite content, several quartz-feldspar ^ cm at random core angles through 82-83m m: hornblende-biotite rich phase, 80 0Xo fine to medium grained, dark green mottled by fine white feldspar m: occasional hornblende-rich interval ^ cm wide, strong gneissosity, contorted C.A. through m with hornblende-biotite clots m: alternating brecciated and gneissic sections -^1.0 m wide, gradational contacts, weak brecciation with no gneissosity due to fine grain silicification and mylonitization. Gneissosity: 62m; 250 C.A., 65m; 300 C.A., 72m; 34" C.A., 78m; 41 0 C.A Lamprophyre dike porphyritic, SO-40% bright green euhedral to pellet shaped clinopyroxene crystals up to 1 cm in diameter, ^007o light blue pellet to shapeless :1 cm grains of amphibole, 1 07o black O.5 cm pellet shaped unknown mineral, dark greyish black KAP-3B KAP-3B Microprobe Digestion see microprobe results Cr diopside Cr amphibole Page 2 of 4

27 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: 1250 KAP-3B Robert J. KAP Property DECLINATION: 45" 150m 42G/7 Dillman 8"W U.T.M. CLAIM : COORDINATES: m. E m. N. FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Lamprophyre dike very fine grained matrix of serpentine (greasy feel), fine black mica and carbonate, moderate magnetism, upper contact sharp 260 C. A. perpendicular to gneissosity at 200 C. A., lower contact sharp 260 C. A. perpendicular to gneissosity at 200 C. A., no alteration to wallrock marginal dike, several hairline calcite filled fractures cutting dike C. A.. Biotite/ phlogopiteserpentinized carbonated matrix Quartz-feldsparbiotite-hornblende same as above, alternating gneissic and weakly macro brecciated to fine grained-mylonitized intervals, gradational contacts m: hornblende-biotite rich section, dull green, subhedral crystals of hornblende O.5 cm. Gneissosity: 98m; 400 C.A., 100m; 45" C.A Lamprophyre dike same as above, darker black matrix, less light blue amphibole, abundant bright green clinopyroxene, upper contact sharp 61 0 C.A. cuts gneissosity, similar lower contact 61 0 C. A Quartz-feldsparbiotite-homblende same as above m: several O.3 cm light green aplite dikes 120 C.A m: several ^.S cm light green aplite dikes C.A.., no alteration marginal dikes m: several 2 cm light green aplite dike C.A.., brecciation and mylonitization marginal dikes, increasing homblende-biotite rich intervals down section m: mafic section, fine to medium grained, dark green hornblende mottle by fine white plagioclase, well foliated 11 0 C.A m: light orange-pink feldspar dike 380 C.A, 1 cm orange coloured alteration marginal dike. Gneissosity: 104m; 350 C.A., 112m; 150 C.A., 119m; 300 C.A. Page 3 of 4

28 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP.. ONTARIO DRILL HOLE KAP-3B LOGGED BY: Robert J. Oldman PROPERTY NAME: KAP Property BEARING FROM TRUE NORTH: 125" DECLINATION ^"w DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 150m MAP REFERENCE: 42G/7 U.T.M. COORDINATE S: m. E m. N. CLAIM : FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Feldspar dike light orange-pink to white, fine grained feldspar, some fine grey to white quartz 100Xo, banded 420 C. A., upper contact sharp 200 C. A., parallel gneissosity, lower contact sharp 500 C. A. cut gneissosity 250 C. A., minor deformation to wallrock marginal to lower contact, cut by dark greenish black hairline fracture parallel to lower contact Quartz-feldsparbiotite-homblende same as above. Gneissosity: 121m; 320 C.A Diorite? fine to very fine grained, whitish-pink feldspar and lesser quartz mottled by dark green hornblende-biotite-chlorite clots -so.s cm wide, weak to no gneissosity, gradational upper contact. Gneissosity: 125m; 250 C.A Lamprophyre dike same as above, dark black matrix, abundant bright green clinopyroxene, upper contact sharp 420 C. A., lower contact 400 C.A.. KAP-3B m Digestion Diorite? same as above, occasional gneissic section, increasing grain size down section. Gneissosity: 141m; 190 C.A. 150 End of hole. Page 4 of 4

29 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO^^^ DRILL HOLE KAP-4 LOCATION GRID: GRID A LINE: 8+30W 3+80N COLLAR ELEVATION: (metres above sea level) 263m a.s.l. BEARING FROM TRUE NORTH: 140" DECLINATION: DIP OF HOLE AT COLLAR: 450 TOTAL FOOTAGE (metres) 150m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: March March 9, 2001 March 10, 2001 Robert J Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Ltd. DRILLING COMPANY: Major Dominik Drilling, Timmins CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property TOWNSHIi Ecclestone Twp. FOOTAGE (metres) FROM l TO 0-6 Overburden ROCK TYPE DESCRIPTION SAMPLE INTERVAL FROM TO ASSAY RESULT Amphibolitized metasedimentary schist greyish green, fine grained pelagic metasediment, weak to moderate schistosity, chlorite slickened cleavages with fine anhedral pyrite, trace over section, occasionally cut by hairline to ^.2 cm wide white calcite stringer, stringers at random orientation, occasional section of brecciation and fracturing m: white quartz vein 450 C.A., trace pyrite on lower contact m: moderate brecciation, mega fragments, dark hairline matrix, occasional :1 cm wide quartz stringer at random orientations, some with traces of pyrite and replaced by fine pyrite stringes, trace - 2 0Xo pyrite over section. Schistosity: 9m; 280 C.A., 12m; 400 C.A Basalt grey mottle white, fine grained, massive, upper contact sharp, ragged and brecciated 550 C.A., lower contact sharp 450 C.A Brecciated metasedimentary schist Brecciated metabasalt same as above, moderate brecciated, thin dark hairline matrix, milled clastes. same as above, brecciated, thin dark hairline matrix of milled clastes, upper contact sharp 480 C.A. Kap-4-1 Kap-4-2 Kap m 1.2m 14-15m 1.0m m 1.3m Page l of 3

30 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: KAP-4 Robert J 140" m. E Dillman KAP Property DECLINATION: 45" 150m 42G/ m N 8"W FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Brecciated metasedimentary schist same as above, brecciated pelagic metasedimentary schist, zones of good schistosity and destroyed schistosity by brecciation and fracturing, sections of multiple fracturing and ground core, S-5% loss, hairline stringers and clots of calcite associated with sections of fracturing and brecciation with chlorite slickened cleavages, increasing brecciation and fracturing down section m: calcite-ankerite stringer stockwork and brecciation, 620 CA. 40m: fractures at 280 C. A., rusty and amphibolitized with calcite m: ground core, 50Xo lost, calcite-ankerite stringer stockwork 72" C.A m: chlorite slickened fractures 550 C.A., 2 cm quartz vein at 44.7m orientated 560 C.A m: increasing brecciation down section, decreasing schistosity. Schistosity: 30m; 420 C.A Peridotite? dark grey to black, very fine grained to aphanitic, massive, homogeneous appearance to entire section, some minor brecciation with micro thin black matrix of milled rock, section cut by 1-3 per metre greenish-white serpentinized fractures at random core angles ^ cm wide with traces of fine anhedral smears of yellow pyrite, moderate magnetism through out section, occasional small clot of magnet te, upper contact lost, could be gradational, possibly marked by a series serpentinized fractures orientated 50-72" C. A., lower contact also lost. Kap-4-4 Kap-4-5 Kap-4-6 Kap-4-7 Kap-4-8 Kap m 6.4m 66-74m 8.0m 74-83m 9.0m m 8.0m 91-99m 8.0m m 5.0m Mafic Meta volcanic Basalt? fine grained/ aphanitic, dark greyish-green, massive, cut by numerous randomly orientated hairline fractures of light green epidote some preferred orientations at 800 C. A., some interstitial fine quartz and white O.2 cm disseminated pop-corn Page 2 of 3

31 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-4 LOGGED BY: Robert J Dillman PROPERTY NAME: KAP Property BEARING FROM TRUE NORTH: 1400 DECLINATION: 8^ DIP OF HOLE AT COLLAR: 450 TOTAL FOOTAGE (metres) 150m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Mafic Metavolcanic Basalt? like white feldspar grains, upper contact lost by fracturing and ground core, fracturing at 780 C. A., increasing quartz replacing epidote through m m: quartz + epidote hairline stringers with ^"/o fine pyrite m: 13 cm white quartz vein at 320 C.A m: increasing brecciation and epidote-calcite hairline stringers at random core angles. Schistosity: 135m; 240 C.A., 140m; 360 C.A. 150 End of Hole Page 3 of 3

32 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-5 LOCATION GRID: GRID A LINE: 6+30W 1+70S COLLAR ELEVATION: (metres above sea level) 258m a.s.l. BEARING FROM TRUE NORTH: 1400 DECLINATION: S'W DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 123m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: March 9, 2001 March 10, 2001 March 11, 2001 Robert J Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Ltd. FOOTAGE (metres) DRILLING COMPANY: Major Dominik Drilling, Timmins CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property ROCK TYPE DESCRIPTION SAMPLE 0-19 Overburden 13-19m: basal till, regolith, light greenish-brown, non-stratified, unconsolidated, hard packed till with various sized clastes of different compositions, some local metavolcanic and metasedimentary rock fragments and distal limestone and red arkose sediments Amphibolitized metasedimentary schist grey green, fine grained pelagic metasediment, nonschistose due to strong fracturing with chlorite slickened cleavages orientated C.A. and brecciation, trace pyrite over section m: 1-20Xo fine silver subhedral pyrite. TOWNSHIP/ Ecclestone Twp. INTERVAL FROM TO KAP m 6m ASSAY RESULT Diabase dark greyish black mafic minerals mottle greyish white anhedral plagioclase, medium grained, massive, occasional weakly rusty fracture at no preferred orientation, magnetic, upper contact sharp, 450 C.A., lower contact sharp 450 C.A Gneissic metasediment moderate gneissosity increasing down section, fine grained, grey mottled by white plagioclase? and darker fine biotite rich sections m: brecciated weak to no foliation or gneissosity, 10 cm contact alteration zone of recrystallization and silicification. Page l of 2

33 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY. ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-5 LOGGED BY: Robert J Dillman PROPERTY NAME: KAP Property BEARING FROM TRUE NORTH: 140" DECLINATION: 8"W DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 123m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Gneissic metasediment m: increasing gneissosity, some contortion, decreasing brecciation and recrystallization, 0.3 cm chlorite slickened fracture 520 C. A. at 102.1m m: numerous randomly orientated hairline fractures, light green, some brecciation, weak banding of light and dark minerals Gneissosity: 103m; 450 C.A., 104m; 90 C.A., 108m; 480 C.A Mafic Dike Peridotite? black, very fine grained to aphanitic, massive, homogeneous across section, greasy-serpentinized feel, orientated 130 C. A. contacts sharp Mafic Dike Diabase? fine grained, dark green, consists of interstitial plagioclaseamphibole and biotite, massive, cut by numerous randomly orientated light green calcite-chlorite filled fractures, lower contact sharp 170 C. A Quartz-feldsparbiotite medasedimentary gneiss same as above, fine grained aphanitic, weak bands of light silicate minerals and darker biotite, section cut by numerous chloritized hairline fractures most C. A.. Gneissosity: 113m; 480 C.A., 116m; 45" C.A., 120m; 480 C.A End of Hole Page 2 of 2

34 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILL HOLE KAP-6 LOCATION GRID: GRID E LINE: 2+75W 1+37S COLLAR ELEVATION: 254 m a.s.l BEARING FROM TRUE NORTH: 225" DECLINATION: 8"W DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 168m MAP REFERENCE: 42G/2 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: March 12, 2001 March 14, 2001 March 14, 2001 R. J. Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Ltd DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CSR14, claim , GRID E 0+20W, 0+25S PROPERTY NAME: KAP Property TOWNSHIP/ Ecclestone Twp FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE 0-16 Overburden 11-16m: basal till, light brown, sandy matrix with unsorted cobbles of local and distill rock fragments Quartz-feldsparhorn blende-biotite Pink feldsparquartz-biotite vein Quartz-feldsparhomblende-biotite alternating white quartz-feldspar rich sections and dull green hornblende-epidote-biotite rich intervals, fine-moderate grained, moderate to strong gneissosity. Gneissosity: 18m; 700 CA, 21m; 580 CA, 30m; 680 CA. fine grained, sugary, pinkish-white peppered with fine black biotite, contacts sharp, parallel gneissosity, upper 320 CA, lower 450 CA., at least one 5 cm wallrock inclusion in vein. same as above. Gneissosity: 39m; 740 C.A., 42m; 61" C.A Lamprophyre dike dark grey, very fine grained matrix of biotite and serpentine, subtle light and dark pellet shaped grains "d cm wide of various minerals consisting of 10"Xo blue amphibole, ^00Xo clinopyroxene, fine black mica and possibly yellow olivine some of which have a reddish stain or rust, weakly magnetic, similar to dikes in KAP-3b but not as porphyritic, trace fine disseminated silver pyrite, 3 cm secondary pink feldspar veinlet at 44.7m orientated 390 C.A, dike contacts sharp, upper contact KAP-6-1 KAP-6 KAP-6-3 INTERVAL FROM l TO 5m Heavy mineral separation m Microprobe m Digestion ASSAY RESULT Page l of 4

35 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP NAME: TRUE NORTH: 2250 COLLAR: (metres) REFERENCE: KAP-6 R. J. Dillman KAP Property DECLINATION: 45" 168m 42G/2 8^ U.T.M. CLAIM : COORDINATES: m. E m. N. FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Lamprophyre dike 620 C.A. perpendicular gneissosity at 650 C. A., lower contact sharp, 240 C.A., brecciated wallrock, possibly by earlier shearing, no alteration either side of dike Quartz-feldsparhornblende-biotite same as above m: hornblende-chlorite-biotite rich horizon, grains cfj.s cm, well foliated 530 C. A. Gneissosity: 51m; 78C) C. A Diabase dike light greenish grey pyroxene mottled by fine white plagioclase feldspar, fine-medium grained, massive, upper contact sharp 520 CA, lower contact sharp 680 C.A., cutting gneissosity Quartz-feldsparhornblende-biotite same as above, section cut by several pink feldspar-quartzbiotite veins m: K feldspar vein, 650 CA m: K feldspar vein, 430 CA m: K feldspar vein, upper contact 440 C. A., lower contact gradational m: K feldspar vein, upper contact 820 C. A., lower contact gradational brecciated feldspar vein, section cut by randomly orientated chlorite-biotite slickened fractures, upper contact sharp 580 CA, stronger brecciation at lower contact 420 CA m: brecciated section with black slickened hairline fractures 25" C. A., lower contact gradational, 83.45m 2 cm K feldspar vein parallel fracturing m: non-deformed gneiss, moderate gneissosity. Gneissosity: 69m; 450 CA, 75m; 520 CA, 80m; 600 CA., 84m; 70" C A Brecciated mafic dike. (Diabase?) dark green mottled by fine white plagioclase, fine grained, similar to dike at m, many black slickened hairline fractures at random core angles and parallel contact, Page 2 of 4

36 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: m. E KAP-6 R. J. Dillman KAP Property DECLINATION: 45" 168m 42G/ m N 8^ FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Brecciated mafic dike. (Diabase?) brecciation significant, fragments long and thin by shearing ^x2 cm, orientated by shearing 250 CA, upper contact brecciated sharp at 280 C.A., 1 cm K feldspar stringer at upper contact, lower contact stronger brecciation 480 C. A Pink feldsparquartz-biotite vein fine grained, sugary, pinkish-white peppered with fine black biotite, lower contact 480 C. A Quartz-feldsparhornblende-biotite same as above. Gneissosity: 90m; 520 C.A Diatreme dike? light grey siliceous very fine grained aphanitic matrix, one 5 cm wide angular fragment of syenite well preserved, several small fragments of wall rock, similar to diatreme dike found on this grid at 0+50W, 12+75N and in outcrop on Grid J, no mica visible Quartz-feldsparhorn blende-biotite same as above. Gneissosity: 99m; 500 C.A Lamprophyre dike dark greyish black, very fine grained, similar to dike at m, much less mineral inclusions especially bright green clinopyroxene, -slo^/o small discrete blue amphibole, trace of black mica pellet shaped grains O.2 cm, massive, upper contact sharp 450 CA, brecciated section at lower contact between m similar to brecciated section at m, possible dike is superimposed on previous shear, lower contact of dike and brecciate 450 C.A.., dike is weakly magnetic. KAP m Digestion Quartz-feldsparhomblende-biotite same as above m: 2 cm very fine grained aphanitic mafic dike, dark grey, 500 C.A. Page 3 of 4

37 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP.. ONTARIO DRILL HOLE KAP-6 LOGGED BY: R. J. Dillman PROPERTY NAME: KAP Property BEARING FROM TRUE NORTH: 225" DECLINATION: DIP OF HOLE AT COLLAR: 450 TOTAL FOOTAGE (metres) 168m MAP REFERENCE: 42G/2 U.T.M. COORDINATES: m. E m. N. CLAIM : FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Quartz-feldsparhornblende-biotite m: K feldspar vein parallel gneissosity, 560 C.A m: white quartz K feldspar vein parallel foliation at 420 C.A m: increasing folding down section m: white quartz K feldspar vein 440 C.A., several 0. 5 cm clots of biotite m: white quartz K feldspar vein 440 C.A m: white quartz K feldspar vein 460 C.A., coarser grained, 1 cm clots of biotite chlorite. Gneissosity: 108m; 720 C.A., 114m; 620 C.A., 123m; 620 C.A., 159m; 570 CA, 165m; 700 CA. 168 End of Hole Page 4 of 4

38 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO^ DRILL HOLE KAP-7 LOCATION GRID: GRID J LINE: 3+62N 4+12E COLLAR ELEVATION (metres above sea level): 252 m a.s.l. BEARING FROM TRUE NORTH: 300" DECLINATION: 8"W DIP OF HOLE AT COLLAR: 45" TOTAL FOOTAGE (metres) 135m MAP REFERENCE: 42G/7 U.T.M. COORDINATES: m. E m. N. CLAIM : DATE HOLE STARTED: DATE HOLE FINISHED: DATE LOGGED: LOGGED BY: DATE SUBMITTED: March 15, 2001 March 17, 2001 March 17, 2001 Robert J. Dillman March 25, 2001 EXPLORATION COMPANY, OWNER, OPTIONEE: G. Silverman Diadem Resources Limited DRILLING COMPANY: Major Dominik Drilling CORE STORAGE LOCATION: end of access road CRS 14, claim , Grid E PROPERTY NAME: KAP Property TOWNSHIP: Ecclestone Twp. FOOTAGE (metres) FROM l TO ROCK TYPE DESCRIPTION SAMPLE INTERVAL FROM TO ASSAY RESULT 0-6 Overburden Quartz-feldsparbiotite-horn blende white feldspar plus quartz mottled by dark grey and green hornblende and fine biotite, fine to medium grained, weak to moderate gneissosity, some sections contorted, occasional disseminated biotite and/or dull green hornblende-chlorite rich section or zenolith up to 20 cm wide, Gneissosity: 15m; 51 0 C.A., 24m; 660 C.A., 42m; 670 C.A., 47m; 580 C.A Lamprophyre dike porphyritic, 30~4007o bright green euhedral to pellet shaped clinopyroxene crystals up to 1 cm in diameter, 5 0Xo light blue pellet to shapeless ^ cm grains of amphibole, ^% black -^0.5 cm pellet shaped unknown mineral, dark greenish grey very fine grained matrix of serpentine (greasy feel), fine black mica and carbonate, moderate magnetism, contacts sharp and parallel 690 C.A., no alteration to wallrock marginal dike Quartz-feldsparbiotite-horn blende same as above, significant degree of contortion or folding of gneissosity. Gneissosity: 48m; 58" C.A., 49m; 220 C.A. KAP m Heavy mineral separation Page l of 3

39 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP NAME: TRUE NORTH: 3000 COLLAR: (metres) REFERENCE: KAP-7 Robert J. KAP Property DECLINATION: 45" 135m 42G/7 Dillman S'W U.T.M. CLAIM : COORDINATES: m. E m. N. FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Lamprophyre dike same as above, similar to lamprophyre dike in KAP-3b, strong porphyritic appearance, ^ cm euhedral crystals and pellet shaped grains of bright green clinopyroxene, lesser pellets and shapeless blue amphibole in black mica-serpentinized fine grained matrix, coarser grained in center of dike, weakly banded towards lower contact parallel contact, upper contact sharp 450 C. A., lower contact sharp 480 C. A., weakly magnetic. KAP m Digestion Pink feldsparquartz-biotite vein very fine grain, foliated parallel contacts, orangy-white mottle by black biotite, upper contact 480 C. A., lower contact lost, ground core Quartz-feldsparbiotite-horn blende same as above. Gneissosity: 55m; 480 C. A., 63m; 380 C. A Lamprophyre dike same as above, good chrome diopside content, 3 cm very fine grained grey dike at upper contact 570 C. A., lower contact 57" C.A. perpendicular gneissosity at 70" C.A. KAP Quartz-feldsparbiotite-homblende same as above Lamprophyre dike same as above, 1 cm dike, good bright green clinopyroxene content with grains ^ cm wide, 600 C.A Quartz-feldsparbiotite-hornblende same as above. Gneissosity: 81m; 660 C.A., 92m; 750 C.A Pink feldsparquartz-biotite vein same as above, white-orange with black specks of biotite, fine grained, upper contact 550 C. A., Cr-clinopyroxene dike at lower contact. Page 2 of 3

40 DIAMOND DRILL LOG GEMCAL PROSPECTING SYNDICATE-DIADEM RESOURCES LTD. KAP PROPERTY, ECCLESTONE TWP., ONTARIO DRILLHOLE LOGGED BY: PROPERTY BEARING FROM DIP OF HOLE AT TOTAL FOOTAGE MAP U.T.M. CLAIM : NAME: TRUE NORTH: COLLAR: (metres) REFERENCE: COORDINATES: 300" m. E KAP-7 Robert J. KAP Property DECLINATION: m 42G/ m N Dillman 8"W FOOTAGE (metres) ROCK TYPE DESCRIPTION SAMPLE INTERVAL ASSAY RESULT Lamprophyre dike same as above, 3 cm dike 540 C.A Quartz-feldsparbiotite-horn blende same as above Lamprophyre dike contacts weakly brecciated with small angular pieces of gneiss, upper 57" C. A., lower 600 C. A., section cut by several cm wide calcite-serpentine filled fractures with black slickened contacts C.A. KAP m Digestion Quartz-feldsparbiotite-hornblende same as above, decrease in hornblende-biotite rich segments, fine grained sections with pinkish-red rust? associated with small black mica inclusions, decreasing gneissosity down section m: coarsegrained K feldspar-quartz-biotite vein, brecciated margins, upper contact 450 C.A. cutting 590 C.A. gneiss, lower contact gradational, some epidote at lower contact. Gneissosity: 100m; 330 C.A Mafic dike very fine grained, apanitic, dark grey matrix with whistish-grey shapeless to soft-edged pellets of plagioclase? -^0.3 cm wide, section cut by several quartz stringers O.2 cm wide orientated C. A., upper contact sharp 390 C. A., lower contact 450 C. A., 1-2 cm wide recrystallized aureole in wall rock surrounding dike Quartz-feldsparbiotite-horn blende same as above, some zoning between coarse and fine minerals giving candy-striped appearance to section. Gneissosity: 117m; 460 C.A. 135 End of Hole. Page 3 of 3

41 CLINOPYROXENE, R. DILLMAN, KAP - DIADEM, March 19, 2001, R.L.B. 1 SI TI02.18 A C FEO 2.97 MGO MNO.12 CAO K20.02 NA20.42 SUM SI AL AL.012 TI.005 CR.019 FE.090 MG.972 MN.004 CA.868 NA.029 K ENST FER t t t t t K t t F/M.096 F/FM SAMPLE KAP 38, CPX 2 SAMPLE KAP 3B, CPX 3 SAMPLE KAP 3B, CPX 4 SAMPLE KAP 3B, CPX 5 SAMPLE KAP 38, CPX 6 SAMPLE KAP 3B, CPX 7 SAMPLE KAP 38, CPX 8 SAMPLE KAP 38, CPX 1, CENTRAL 2, ANOTHER CENTRAL 2, NEAR MARGIN 3, ANOTHER CPX CENTRAL 4, ANOTHER GRAIN 5, ANOTHER GRAIN 6, ANOTHER GRAIN 7, ANOTHER GRAIN CENTRAL CENTRAL CENTRAL CENTRAL

42 CLINOPYROXENE, R. DILLMAN, KAP - DIADEM, March 19, 2001, R.L.8. 9 SI TI02.30 A C FEO 3.06 MGD UNO.06 CAO K20.00 NA20.44 SUM , SI AL AL II CR FE MG MN CA NA K ENST WO FER F/M.099 F/FM SAMPLE KAP 38, CPX IN GDMASS 10 SAMPLE KAP 38, CPX IN GOMASS 11 SAMPLE KAP 38, ANOTHER CPX IN GDMASS 12 SAMPLE KAP 38, ANOTHER CPX IN GOMASS 13 SAMPLE KAP 38, AT MARGIN CPX 14 SAMPLE KAP 3B, CHROME-RICH CENTRAL AGAIN

43 Wo l l aston i te 90/10 30/10 Diopside 50/50 80/20 70/30 SO/10 80/20 70/30 60/10 so/so Hedenbergite 10/90 20/80 30/70 W&Q 50/50" Enstatite 20 90/10 J/IO Ferros i i ite CLINOPYROXENE - DIADEM SAMPLE KAP 3B (March 7, 2001)

44 CLINOPYROXENE - DIADEM SAMPLE KAP 3B (March 7, 2001) q, wt % Na 2O o RLB

45 AMPHIBOLE, R. DILLMAN, KAR - DIADEH, March 19, 2001, R.L.B. SI02 TI02 A203 C203 FED MGD MNO CAO K20 NA20 SUM SI AL AL TI CR FE MG MN CA K HA FE MG , , , F/M F/FM l SAMPLE KAR 38, OVER CPX IN GROUNDMASS

46 MICA, R. DILLMAN, KAP - DIAOEH, Harch 19, 2001, R.L.B. SI02 TI02 A203 C203 FEO 1160 UNO CAO K20 NA20 SUM SI AL AL TI CR FE MG MN CA K NA , FE MG F/M.349 F/FM l SAMPLE KAP 38, MICA l, CENTRAL 2 SAMPLE'KAP SB,...MICA i, AT MARGIN

47 Work Report Summary MINISTRY OF NORTHERN DEVELOPMENT AND MINES Transaction No: W Status: APPROVED Recording Date: 2001-MAR-30 Work Done from: 2001-FEB-25 Approval Date: 2001-JUL-17 to: 2001-MAR-17 Client(s): SILVERMAN, GEORGE CHARLES Survey Type(s): PDRILL Work Report Details: Claim P P P P P P P P P P P P Perform 58,334 S S SO SO SO SO SO SO SO so Perform Approve 55,834 S11,919 S11,501 SO SO SO SO SO SO SO Applied 50 so SO S , ,200 56,400 53,200 51,600 S3.200 S3.200 Applied Approve SO S , ,200 56,400 S ,600 53,200 53,200 Assign so so so so so so so so so so so so Assign Approve Reserve S , ,001 SO 50 SO SO SO SO SO so so Reserve Approve 55, , SEP ,501 Due Date 2001-SEP OCT-22 SO 2002-MAR-31 SO 2002-MAR-31 SO 2002-MAR-31 SO 2002-MAR-31 SO 2002-MAR MAR MAR MAR MAR-31 P ,336 S33,836 SO SO 534,400 33,600 S JUL ,090 S63, , ,400 S , , ,690 External Credits: SO Reserve: S28,690 (538,690) (510,000) Reserve of Work Report: W Applied by W JUN-21 Total Remaining Status of claim is based on information currently on record. 42G07SW ECCLESTONE Aug-14 10:18 Armstrong-d Page 1 of 1

48 Ministry of Northern Development and Mines Date:2001-JUL-18 Ministers du Developpement du Nord et des Mines Ontario GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5 GEORGE CHARLES SILVERMAN 75 ACTON AVENUE DOWNSVIEW, ONTARIO M3H 4H2 CANADA Tel: (888) Fax:(877) Dear Sir or Madam Submission Number: Transaction Number(s): W 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. Assessment work credit has been approved as outlined on the AMENDED Declaration of Assessment Work Form received July 17, If you have any question regarding this correspondence, please contact or by phone at (705) BRUCE GATES by at Yours Sincerely, Ron Gashinski Supervisor, Geoscience Assessment Office Cc: Resident Geologist George Charles Silverman (Claim Holder) Assessment File Library George Charles Silverman (Assessment Office) Visit our website at Page: 1 Correspondence 10:16135

49 i ^ L u. L. u l MINING LAND TENURE MAP Date/Time of Issue Apr B 2001 TOWNSHIP/AREA ECCLESTONE 12:52h Eastern PLAN G ''V- X i ~ J,..Vj -~j 12 ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Land Tilled/Registry Division Ministry o( Natural Resources District TOPOGRAPHIC i O,,... ; "i l. J.,. p,-,-, n,,,-., J1. Porcupine COCHRANE HEARST LAND TENURE (D D Q Q : ; i B 0 Q LAND TENURE WITHDRAWALS IMPORTANT NOTICES LAND TENURi WITHDRAWAL DESCRIPTIONS. '.. T t ' '. ' ^^..J IdiMiHu.....Ijjjt.. Date.. DcicrtUoii an Wn Jn 1 wu it DSF'QiwL Mi UUI H.K iuhl 2CW1?i;t Wxn Sun 1 Htflj M fi w ^.Fl.JlM.t). dl.ns ijsj wph Jdi l itfll Pmun-fl utau a on untth tno VLt. wrn IMPORTANT NOTICES trtwihu WU i)ilnrd devil an mint iwiinllai S { 42G07SW ECCLESTONE 200..,..! -,,,..xi,;,.;x,. f A itikiiiii^inuiitivrti inncfl r I ha uun. Thom-4 i mnul ill idrt, lu^ nwqmi.ind auiu'v.-'i 1lil1HI ijw-ihlniilloii pnip iab M IHituriiniriiiliriii ^nm+iniihn in up la i iimpnm lin in "^IIIJLI l Mn loiv Ao li obtdnbj ihinunl.lln? hi rf i n.js TkHL c, r nuin, r Q-frk:r, in tt i e Milklrv iirndiii al RHUI,,, General Information and Limitations MflB OaTiiin. HH flj,,,,, murijttnn iir'lljhil /Kit liilhmil filini th C. l r, tin Aim CM) Linrl inniin iiiwllidi lentil-:'oi miihitil li er r-hlly In Wnhr inlnlnj i Itfhns niriy mr n

50 360000mE360000mE r~\x 2M^ AGRiO Chromite \\\ PicroilmenitA V\ Pyrope-^1- Chrome Diopside Chrome Diopside (questionable source).' 3 2 l Kimberlite Mineral Location Suspected Kimberlite Minerals (No microprobe analyses) Barren Sample Site Ground Magnetic Anomaly Area of Outcrop Diabase Granite Metasedimentary Rock Mafic Metavolcanic Rock Esker Glacial Striation KoCC ' i' DRILL HOLE LOCATION O 500 1,000 metres 42G07SW ECCLESTONE A 7 DIAMOND DRILL HOLE LOCATIONS KAR PROPERTY ECCLESTONE TWP., ONTARIO GEMCAL PROSPECTING SYNDICATE DIADEM RESOURCES LIMITED SCALE 1:10,000 MAP No.: DDH-2001 NTS: 42G Date: March 25, 2001 DRAWN BY: RJD Revised: