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Rpt on Airborne Geophys Surv Nipigon Plate Prop

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o */.y -; P vnrn Vj,4 1 i, ij i.UD J GECSCSEMCE ASSi-SCMENT __ OFFiCE A Report on Airborne Geophysical Survey on the Nipigon Plate Property, of CANADIAN GOLDEN DRAGON RESOURCES LTD Vanguard Claim Group, Kashabowie Area Thunder Bay Mining Division, Ontario Province of Ontario for Canadian Golden Dragon Resources Ltd 500 - 20 Maud Street Toronto, Ontario M5V 2M5 May 20lh, 2003 Roger J Caven, BASc, P Eng, Consulting Geophysicist RR# 5, 479 Ocean View Drive, Gibsons, British Columbia, CANADA VON l V5 Tel/Fax: (604) 886-0479, e-mail: rogerj^avei^telus.net (Sunshine Coast) 52B09NW2018 2.25700 KASHABOWIE LAKE 010 TABLE OF CONTENTS Summary Page 3 Introduction 3 Location and Access 3 Previous Work 3 Property - Description and Location 4 Geology of the Claim Group and area 5 Airborne EM - Magnetic Survey 5 Discussion of Results 6 Distribution of Work Performed ,t ,,t .., ^ p /* 6 Conclusions and Recommendations ©©-©f.©\ ^ ^©j l \J\J7 References Reports 8 Maps 9 Certificate of Author 10 Table 12.5 Metamorphic mineral assemblages of the Shebandowan greenstone belt, 2 pages. Report of the Helicopter-borne Time Domain Electromagnetic Geophysical Survey, Vanguard Property, Kashabowie Area, Thunder Bay Area, Ontario, for Canadian Golden Dragon Resources Ltd, by Geotech Ltd. Claim Map Scale 1:50,000, Approximate Reduced Total Field Magnetic Map Scale 1:40,000, Approximate Reduced Airborne EM Profiles Scale 1:40,000, Approximate In Pocket Airborne EM Profile Map Scale 1:20,000 Airborne Magnetic Contour Map Scale 1:20,000 SUMMARY Canadian Golden Dragon Resources Ltd, holds several groups of claims, including the 320 claim units in 47 claims within the Kashabowie area within the Shebandowan greenstone belt, about 88 km WNW of Thunder Bay, Ontario. This report deals with the recent airborne geophysical survey over the Vanguard claims group. On February 11 th to 12th Geotech Ltd flew the Vanguard property with the Helicopter-borne time domain electromagnetic/ magnetic survey system. This survey was intended to outline electromagnetic conductors and to obtain detail magnetic information for the purpose of outlining the subsurface geology. Results of the survey are appended as maps. INTRODUCTION Recently Canadian Golden Dragon Resources has been directing its attention to greenstone belts in addition to its interest in ultramafic intrusives. The Kashabowie area is in the Shebandowan greenstone belt in the Wawa subprovince. The Archean age Superior Province includes several greenstone belts with iron formations and sulphide occurrencies, many with economic basemetal mineralization. Although the greenstone belts have been subject to exploration for many years, newer geophysical techniques have improved the discrimination of conductive features as well as providing a better depth penetration. Although helicopter borne geophysical surveys have been used for many years, they have been based on frequency domain systems which have limited depth penetration, although generally resolution of near surface features have been good. The move to time domain electromagnetic systems began in the 1960©s with the Barringer Research INPUT system. INPUT improved depth penetration, although resolution was less. Several time domain systems have been developed since, among them the Fugro (formerly Geoterrex) Megatem system with high power and very good depth penetration. Recently Geotech Ltd has developed and tested the helicopter borne Dream Catcher Time Domain Electromagnetic system. Test flights by Megatem and Dream Catcher TDEM have shown comparable depth penetrations but better lateral resolution for the latter. Canadian Golden Dragon decided to use the Dream Catcher TDEM system for a detail look at the Kashabowie area of the Shebandowan greenstone belt. LOCATION AND ACCESS The Vanguard property is road accessible via Hwy 11 to Kashabowie situated ~88 km WNW of Thunder Bay. Local and forestry roads branch off the highway south to the property. PREVIOUS WORK Previous work on the property and surrounding areas are described in the references. Additional work is to be found among assessment work reports. PROPERTY- DESCRIPTION AND LOCATION VANGUARD PROPERTY The Company has acquired a 320 claim unit group covering parts of the Burchell Lake, Crayfish Lake, Greenwater Lake, and Kashabowie Lake townships, at 480 37© N latitude and 900 30© W longitude (~ centre), approximately 88 km WNW of Thunder Bay, in the Thunder Bay Mining Division. The property is accessed from Hwy 11 via roads to the south. Claim no Units Claim Map Recorded Due Date 1064687 06 Burchell Lake 02 Aug 2001 02 Aug 2003 1064688 11 Burchell Lake 27 Jul 2001 27 Jul 2003 1064689 07 Kashabowie Lake 07 Aug 2001 07 Aug 2003 1187559 01 Burchell Lake 08 Mar 2002 08 Mar 2004 C,-V~- 1187652 03 Burchell Lake 19Nov2001 19Nov2003 C©Ti f* \z. ^ 1218593 08 Kashabowie Lake 28 May 2001 28 May 2003 ^ 1218594 14 Crayfish Lake 06 Jun 2001 06 Jun 2003 1218595 16 Kashabowie Lake 06 Dec 2001 06 Dec 2003 1218596 14 Crayfish Lake 06 Dec 2001 06 Dec 2003 1218597 03 Burchell Lake 06 Aug 2002 06 Aug 2004 1238679 01 Burchell Lake 17 Feb 2003 17 Feb 2005 (Holder K R Kukkee) 1239688 01 Burchell Lake 17 Feb 2003 17 Feb 2005 (Holder K R Kukkee) 1240532 04 Kashabowie Lake 01 Jun 2000 01 Jun 2005 1240533 04 Kashabowie Lake 01 Jun 2000 01 Jun 2005 1242495 04 Kashabowie Lake 19 Dec 2000 19 Dec 2003 1242496 02 Kashabowie Lake 19 Dec 2000 19 Dec 2003 1242497 05 Kashabowie Lake 21 Feb 2001 21 Feb 2004 1242498 07 Kashabowie Lake 21 Mar 2001 21 Mar 2004 1242499 01 Kashabowie Lake 27 Apr 2001 27 Apr 2004 1242500 03 Kashabowie Lake 27 Apr 2001 27 Apr 2004 1242511 02 Burchell Lake 18 Dec 2001 18 Dec 2003 1242602 14 Burchell Lake 18 Jun 2001 18 Jun 2003 1242603 02 Kashabowie Lake 18 Dec 2001 18 Dec 2003 1242608 04 Kashabowie Lake 18 Dec 2001 18 Dec 2003 1242609 11 Crayfish Lake 26 Mar 2001 26 Mar 2004 1245728 03 Burchell Lake 26 Mar 2001 26 Mar 2004 1245729 04 Crayfish Lake 26 Mar 2001 26 Mar 2004 1246763 06 Kashabowie Lake 29 Mar 2001 29 Mar 2004 1246772 16 Crayfish Lake 06 Jun 2001 06 Jun 2003 1249547 12 Green Water Lake 07 Feb 2002 07 Feb 2004 1249548 2 Green Water Lake 07 Feb 2002 07 Feb 2004 3001508 11 Burchell Lake 15 May 2002 15 May 2004 3001509 08 Burchell Lake 15 May 2002 15 May 2004 3001510 09 Burchell Lake 15 May 2002 15 May 2004 3001588 02 Crayfish Lake 11 Jul 2002 11 Jul 2004 3001590 07 Kashabowie Lake 15 Aug 2002 15 Aug 2004 3001591 04 Kashabowie Lake 02 Jul 2002 02 Jul 2004 3005088 16 Crayfish Lake 27 Jan 2003 27 Jan 2005 3005089 06 Crayfish Lake 27 Jan 2003 27 Jan 2005 3005090 15 Crayfish Lake 27 Jan 2003 27 Jan 2005 3005091 01 Crayfish Lake 27 Jan 2003 27 Jan 2005 3010484 02 Crayfish Lake 16 Sep 2002 16 Sep 2004 3010485 01 Burchell Lake 23 Sep 2002 23 Sep 2004 3010486 02 Burchell Lake 23 Sep 2002 23 Sep 2004 3011123 15 Kashabowie Lake 27 Jan 2003 27 Jan 2005 3011124 15 Crayfish Lake 27 Jan 2003 27 Jan 2005 3011125 15 Crayfish Lake 27 Jan 2003 27 Jan 2005 Total 47 claims 320 units GEOLOGY OF THE CLAIM GROUP AND AREA The Vanguard claims in the Kashabowie area are in the Shebandowan greenstone belt of the Wawa Subprovince of the Superior Province. The age is Archean. The Shebandowan greenstone belt is arcuate in shape reflecting the curvature of the Quetico - Shebandowan greenstone belt boundary, approximately WSW - ENE as shown by the magnetic trends. The Shebandowan greenstone belt is subdivided into the Burchell and Greenwater assemblages, with a third suite of rocks, the Shebandowan assemblage, consisting of sedimentary and volcanic rocks which overlie unconformably the Burchell - Greenwater boundary, locally straddling it. The Burchell assemblage is divided into three cycles, with cycle 1 intruded by the Shebandowan Lake intrusion. The lower part of cycle 1 comprises massive basalt flows locally altered to chlorite schist. Pillow lava underlies the dacite and rhyolithic units in the upper parts of the cycle. Near the base of this cycle are tabular, serpentinized, peridotite units that contain copper - nickel mineralization. Cycle 1 contains the most extensive basic intrusions in the greenstone belt. Cycle 2 also contains numerous mafic intrusions, but also distinguished by a thick unit of rhyolite to dacite which extends along the northern part of the belt. The main mass of this felsic unit located in and south of the Burchell area is displaced and separated from the more tuffaceous eastern part by right-handed transcurrent movement on the Crayfish Creek fault. (The geology information has been abstracted from "Geology of Ontario; OGS Special Volume 4, Pt1, 1991.) Appended is a two-page table: Table 12.5. Metamorphic mineral assemblages of the Shebandowan greenstone belt. Geology of Ontario; OGS Special Volume 4. Numerous mineral occurrencies have been found on the property. AIRBORNE TIME DOMAIN MAGNETIC - ELECTROMAGNETIC SURVEY On February 11th to 12th, 2003, a helicopter borne geophysical survey was flown over the property with a newly developed time domain electromagnetic system named "Dream Catcher TDEM system". A total of 527.7 km as flown, some of it outside the claims for operational purposes as well to keep the boundaries of flying area manageable. Navigation was by GPS and radar altimetry. The flying height was maintained at 80 m above ground, with sensor at 35 m above ground, and aircraft velocity was nominally 70 km/hour. The low altitude of the sensor and relatively slow speed of he aircraft, coupled with the superior depth penetration and sensitivity of a time domain electromagnetic system has produced survey results where closely located conductors have been discriminated.
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