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Arctic Star Exploration Corp V.ADD

Alternate Symbol(s):  ASDZF

Arctic Star Exploration Corp. is a natural resource company. The Company is a diamond explorer engaged in the acquisition, exploration, and development of mineral properties. Its projects include Diagras Diamond Project and Timantti Diamond Project. Diagras Diamond Project is located in the north-eastern part of the prolific Lac de Gras kimberlite field, approximately 22 kilometers (km) north-northeast of the Diavik diamond mine and 36 km east of the Ekati diamond mine in the northwestern territories of Canada. Diagras Property consists of 58 contiguous claims with an area of approximately 48,346 hectares. The Timantti Project is located in Finland, approximately 17 km away from the town of Kuusamo. The Timantti project, owned 100% by the Company, consists of two Exploration permits, the 243 Ha Exploration Solavaara Permit and the 882 Hectares Vaimouso permit totaling 1125 Ha. The Project is also comprised of two Diamond Bearing Kimberlites: the Black Wolf and White Wolf Kimberlite.


TSXV:ADD - Post by User

Post by rdwwon Apr 22, 2004 11:42am
239 Views
Post# 7388504

SPQ gets 2nd NEW kimber

SPQ gets 2nd NEW kimbertime for MTX to buck up and find one eh! KWG and Spider discover new kimberlite at MacFadyen Spider Resources Inc SPQ Shares issued 156,228,479 Apr 21 close $0.17 Thu 22 Apr 2004 News Release See (KWG) News Release Mr. Michael Newbury of KWG Resources reports A SECOND NEW KIMBERLITE DISCOVERED NEAR PROPOSED VICTOR DIAMOND MINE KWG Resources and joint venture partner Spider Resources have discovered a second new kimberlite pipe on the MacFadyen property located in the Attawapiskat kimberlite cluster, 100 kilometres west of Attawapiskat, Ont., in the James Bay lowlands. All of the MacFadyen kimberlites are within eight kilometres and north of the advanced Victor kimberlite development project of De Beers Canada Exploration Ltd. and 1.5 kilometres east of De Beers's Tango and Tango Extension kimberlites. The new kimberlite was intersected in hole SPQ-04-03 that tested a magnetic anomaly located just south of previously discovered MacFadyen No. 2 kimberlite. Kimberlite was encountered at a depth of 65 metres and the angled hole remained in kimberlite for 32 metres before exiting into very rubbly Paleozoic carbonates, the hole was lost at 104 metres. The first hole in this current program, SPQ-04-01 (announced previously), intersected the Good Friday Kimberlite, which is approximately 100 metres in diameter, and located 300 metres northeast of previously discovered (1994) MacFadyen No. 1 kimberlite and 600 metres northeast of the MacFadyen No. 2 kimberlite. The discovery of this new kimberlite called the MacFadyen No. 2 (south) kimberlite increases the total number of announced kimberlites in the Attawapiskat kimberlite cluster to 21. This new kimberlite may represent two intrusive phases of the same kimberlite (MacFadyen No. 2). Given the proximal position being only 50 metres apart, combined with the magnetic interpretation, it suggests that they are possibly connected at depth. Additional drilling is currently under way in the immediate area of the two new occurrences to test for other potential kimberlites. Furthermore, the first attempt at testing the 250- to 300-metre deep magnetic linear feature traceable for seven kilometres within the joint venture property failed, hole (SPQ-04-02) was lost in the Paleozoic rock when an unconsolidated sand bed was encountered at 72 metres. Another attempt to drill this elusive deep target is planned, as a wrapup to the current drill campaign. This deep linear magnetic feature has been interpreted by the consultants of the KWG-Spider joint venture a possible kimberlite filled fissure or dike. The current drill program at the MacFadyen property is under the field supervision of an independent qualified person (IQP), Roger Thomas, MSc, PEng, PGeo. Mr. Thomas has been logging the drill core and selecting the samples for diamond content processing. The 23 core samples from the first hole in this program were personally delivered by project manager Neil Novak, PGeo, on April 15, to Thunder Bay Diamond Services Laboratory (formerly Kennecott Canada Mineral Processing Laboratory), for a complete diamond content analysis using caustic dissolution. Considering laboratory cue for processing samples, the joint venture anticipates these initial diamond recovery results in late May. The property hosting these four kimberlites (MacFadyen No. 1, MacFadyen No. 2, Good Friday and MacFadyen No. 2 south) consists of five mineral claims totalling 42 units covering 672 hectares. The KWG/Spider own the claims outright, subject to a 25-per-cent clawback entitlement by Ashton Mining of Canada Inc., whereby Ashton can acquire a 25-per-cent interest in the property hosting a kimberlite by paying the joint venture 300 per cent of all expenditures incurred on the subject property up until the Ashton election date. McFauld's Lake volcanogenic massive sulphide project update -- exploration continues, three new VMS occurrences discovered Meanwhile, the joint venture is continuing drilling of the McFauld's Lake volcanogenic massive sulphide project, located 150 kilometres to the west of the Attawapiskat diamond project. Downhole geophysics and a large loop TEM (transient electromagnetic survey) lines have been completed on the McFauld's No. 3 occurrence, designed to test this occurrence beyond the depth limitations of the earlier Max Min electromagnetic survey. The final results and interpretation will dictate the positioning of drill holes to test the mineralization at depths below the previous drilling. Since last report on this project, the joint venture has completed five drill holes on a number of additional outlying geophysical targets discovering three new massive sulphide occurrences as follows: L Hole McF-04-36 was located on Grid G, three kilometres south of the McFauld's No. 3 occurrence, to test the northern flank of an extremely high magnetic anomaly. This hole encountered thin pyritic beds spread out over 135 metres in silicified felsic to intermediate volcanic rocks. The pyritic beds were the most dense around 140 to 150 metres downhole. The best assays of samples from this hole returned 0.16 per cent copper over 0.44 metre, followed by 0.44 per cent copper over 3.25 metres. This geology and sulphide mineralogy suggests that this mineralization is distal or somewhat removed from potentially larger sources. Hole McF-04-37 was also located on Grid G to test the same target as hole McF-04-36. McF-04-37 was drilled into the center of a very large magnetic anomaly. After passing through sheared felsic tuffs and a fault contact zone, massive magnetite with other sulphides (pyrite and chalcopyrite) were encountered over a core length of 4.89 metres. The best assay in this hole was 0.862 per cent copper over 1.07 metres. Hole McF-04-38 also located on Grid G and was the second attempt to test a strong Max Min anomaly by the joint venture. This hole successfully reached the target depth and intersected three metres of massive sulphide mineralization between 150.15 metres and 153.5 metres downhole, followed by what appears to be a thin quartz stock-work. Magnetite, chalcopyrite and pyrite have been observed in the mineralized section. Assays are pending for this hole. Hole McF-04-39 undercut hole McF-04-28 (McFauld's No. 3) and intersected similar massive sulphide mineralization over 2.3 metres between 197.95 and 199.25 metres downhole, the samples from this section are currently being assayed. Down the hole geophysical surveys have been completed on these two holes (McF-04-38 and 39) in order to provide a better understand of this new VMS occurrence. It is felt that the two initial test holes in this occurrence may represent the edge of a much larger VMS occurrence. The joint venture awaits the interpretation of the geophysical program and assays from the mineralized sections. Hole McF-04-40 was located on Grid J approximately 15 kilometres southwest of McFauld's No. 3 occurrence. This hole was designed to test a long Max Min anomaly, with high magnetic signature. An 8.6-metre section of semi-massive sulphide was encountered between 120.05 and 128.65 metres. Pyrite interbedded with magnetite and felsic tuff was observed. Further down the hole, sphalerite and chalcopyrite was observed in thin beds over approximately 19 metres (between 140.9 and 159.35 metres). Samples have been selected from both mineralized sections, for assay and results are pending.

The McFauld's project is under the field supervision of James Burns, PEng, as the independent qualified person. Mr. Burns is responsible for the logging of the drill core and the selection of core samples for analysis. All samples are sent the sample processing facility of ALS Chemex in Thunder Bay, Ont., then pulps of the samples are air transported to ALS Chemex Laboratory in Vancouver for multielement analysis using ME-MS61 (four acid digestion -- ICP finish). The McFauld's Lake area drill rig will be moved back to the McFauld's No. 3 occurrence this weekend to complete the last hole of the winter program. The final hole of the winter program is designed to further test the McFauld's No. 3 occurrence at depth and to start the drill followup that the recent down the hole geophysical survey recommended. Both exploration programs will continue for approximately another week, until spring breakup, that happens toward the end of April or beginning of May, in this part of the Canadian north and lasts for four to six weeks. WARNING: The company relies upon litigation protection for "forward-looking" statements. (c) Copyright 2004 Canjex Publishing Ltd. https://www.stockwatch.com

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