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    eröffnet am 01.04.08 14:52:13 von
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      Avatar
      schrieb am 01.04.08 14:52:13
      Beitrag Nr. 1 ()
      Mit Goldcliff Ressources habe ich einen neuen Wert in meine Watchlist aufgenommen, da er mir sehr vielversprechend erscheint.

      http://www.goldcliff.com/

      Letzte Meldung:


      Goldcliff Discovers New-Ainsworth Silver TargetsGOLDCLIFF RESOURCE CORP GCN 3/28/2008 1:37:15 PMVANCOUVER, BRITISH COLUMBIA, Mar 28, 2008 (Marketwire via COMTEX News Network) --
      Leonard W. Saleken, Chairman of Goldcliff Resource Corporation (TSX VENTURE:GCN) is pleased to report the discovery of five new silver exploration targets on the Ainsworth Silver claims. Located on the west side of Kootenay Lake within the historical Ainsworth silver camp in British Columbia, the Ainsworth Silver claims are 100%-owned by the Company and consist of one contiguous block that totals 18,176 hectares (44,896 acres). Goldcliff's discovery of new exploration targets in the old silver district has revived interest in Ainsworth's silver potential for new deposits.

      Historically, silver production in the Ainsworth camp came from four mines -- No.One, Highland, Highlander and Kootenay-Florence -- that produced 4.40 million ounces of silver (Minfile). Located on Goldcliff's claims, the No.One mine produced 1.99 million ounces of silver and was the premium historic producer in the camp. From 1889 to 1924, the No.One produced 40,169 tons of silver ore with an average grade of 49.64 ounces silver per ton. Modern multi parameter airborne exploration methods were used by Goldcliff to identify important new exploration targets in this promising silver region.

      New Exploration Targets (TG)

      The TG-1 target zone contains two separate geophysical anomalies, each of which covers an area of 0.5 square kilometres. The target zone contains strong airborne electro-magnetic (EM), northern-trending conductors, a prominent east-west trending magnetic feature and two historic silver mines. Until now these anomalies have been hidden by overburden. The TG-1 target has road access and is rated as high-priority.

      The TG-2 target zone contains two separate geophysical anomalies, each of which covers an area of one square kilometre. The target zone contains two moderate to weak airborne EM conductors that are related to a north-south fault. TheTG-2 target zone contains the historic No.One mine and other past silver producers. The two anomalies are located approximately 1,000 metres west of the No.One mine. The TG-2 target has road access and is rated as high-priority.

      The TG-3 target zone contains three separate geophysical anomalies, each of which covers an area of 0.4 square kilometres. The anomalies are aligned along an east-west trend that extends over two kilometres. The target zone contains weak to moderate airborne EM, northern-trending conductors, and several prominent north-south trending magnetic features. The anomalies are related to north-south faults. There are no recorded mineral showings in the target zone. The TG-3 target has road access and is rated as medium-priority.

      The TG-4 target zone contains two separate geophysical anomalies that are 1,000 metres apart. The anomalies each cover an area of one square kilometre. The target zone contains weak airborne EM, northern-trending conductors, and prominent north-south trending magnetic features. There are no recorded mineral showings in the target zone. The TG-4 target has road access and is rated as medium-priority.

      The TG-5 target zone contains three separate geophysical anomalies that are aligned along a north-west trend of four kilometres. The anomalies each cover an area of one square kilometre. The target zone contains weak to strong airborne EM, north-west trending conductors, and prominent north-west trending magnetic features. There are no recorded mineral showings in the target zone. The TG-5 target has no road access and is rated as low-priority due to the inaccessibility of the target area.

      Conclusions

      The TG-1 and TG-2 target zones are the high-priority targets for 2008 ground follow-up. They contain historical silver mines that have produced over 1.99 million ounces of silver. The TG-1 and TG-2 target zones are new discoveries in close proximity to these mines. The targets represent excellent exploration potential for silver deposits.

      The TG-3, TG-4 and TG-5 target zones are in uncharted exploration territory. The targets are in the northern portion of Goldcliff's claims. The targets are in an area of heavy overburden and contain favourable geology for the discovery of silver deposits. There are no reported old mines or silver showings in the area. Logging road access to the area is fairly recent and estimated to be within the last 40 years. The peak of mining activity in the Ainsworth silver camp was from 1889 to the 1940s. Goldcliff considers all targets to be very significant and represent excellent exploration potential for silver deposits in both past producing and new exploration territory.

      The geophysical interpretation of airborne, multi-parameter geophysical survey that was conducted on Goldcliff's claims between the Ainsworth silver camp and Kaslo was very successful in defining 19 geophysical anomalies. Twelve of these geophysical anomalies are contained in the five priority exploration target zones and will be further evaluated in the field in 2008.

      The silver exploration target map is posted on Goldcliff's website, www.goldcliff.com.

      Leonard W. Saleken, PGeo (geologist), and Edwin R. Rockel, PGeo (geophysicist), are the qualified person as defined by National Instrument 43-101 who supervised the preparation and verification of the technical information in this release.

      GOLDCLIFF RESOURCE CORPORATION

      Leonard W. Saleken, Pgeo, Chairman, CEO, Director

      SOURCE: Goldcliff Resource Corporation

      Goldcliff Resource Corporation George Sanders President (250) 764-8879 or Toll Free at 1-866-769-4802 (604) 261-8994 (FAX) Email: sanders@goldcliff.com Website: www.goldcliff.com
      Avatar
      schrieb am 01.04.08 14:59:23
      Beitrag Nr. 2 ()
      Avatar
      schrieb am 17.04.08 19:36:24
      Beitrag Nr. 3 ()
      Goldcliff Resource Corporation

      TSX VENTURE: GCN
      Apr 17, 2008 13:20 ET
      Goldcliff Acquires Large Platinum-Gold Land Position

      VANCOUVER, BRITISH COLUMBIA--(Marketwire - April 17, 2008) - George W. Sanders, President of Goldcliff Resource Corporation (TSX VENTURE:GCN), is pleased to report that Company has acquired a large platinum-gold land position in the Princeton mining region in south-central British Columbia. The Tulameen claims are 100%-owned by the Company and consist of one contiguous block that totals 45,245 hectares (111,755 acres). Located in the historical Princeton mining region, the Goldcliff claim area is situated between the Tulameen platinum district and the Copper Mountain district. The Tulameen platinum district was an important historic producer of placer platinum (20,000 ounces) and the Copper Mountain district was a significant producer of copper and gold (168 million tonnes).

      The Goldcliff claims cover several of the historic placer producing platinum-gold creeks, copper-gold showings and outcrops of intrusive and country rocks that are favourable for mineral deposits in the Princeton mining region. The Tulameen platinum district, which contains several lode platinum occurrences (Minfile), has a reported historic placer platinum production of 20,000 ounces platinum. The potential economic platinum values associated with the lode occurrences range from 2.5 to 16.0 grams platinum per tonne. The Copper Mountain district has a historic production of 168 million tonnes of ore with an average grade of 0.46% copper and 0.14 grams per tonne gold.

      The modern data base has enhanced the exploration potential of Goldcliff's claims in the Princeton mining region with respect to platinum, gold and copper. Readily accessed by road, the Goldcliff claims are ideally positioned for exploration in the Princeton mining region.

      Tulameen Platinum District

      From 1889 to 1936, the Tulameen platinum district was recognized as the most important producer of placer platinum and gold in North America. Several of the creeks in the Princeton mining region had 20,000 ounces of reported platinum production. The Goldcliff claims cover the majority of the creeks that produced placer platinum and gold.

      Referred to as the Tulameen Complex, the lode platinum occurrences in the Tulameen platinum district are associated with ultramafic-mafic intrusive rocks. The Tulameen Complex contains several lode platinum occurrences that have platinum values ranging from 2.5 to 16.0 grams platinum per tonne. The placer platinum deposits in the creeks are the result of the de-gradation and erosion of the lode platinum occurrences in the Tulameen Complex.

      Tulameen Claims Regional Geology

      The Tulameen claims cover an area of 45,000 hectares of geology that is favourable for the exploration of platinum, palladium, gold and copper deposits. The claims have extensive overburden. The Tulameen platinum district is located to the northwest and the Copper Mountain copper-gold porphyry-deposits are located to the southeast of the claim block. In the Tulameen platinum district, the Tulameen Complex containing the lode platinum occurrences is partially exposed. There are similar Tulameen Complex rocks that occur on Goldcliff's claims.

      The Tulameen Complex of ultramafic-mafic intrusive rocks is classified as an Uralian-Alaskan-type complex. The Uralian-Alaskan complexes are a major contributor of platinum group metals (PGM) in the world (Google).

      In the Tulameen district, the platinum metal is a mineral alloy that was identified in 1974 as tulameenite (BC Geology). Tulameenite occurs in other Uralian-Alaskan complexes in the world that are associated with platinum production. Tulameenite is a ferronickelplatinum alloy with a mineralogical composition of Pt-Fe-Cu-(Ni).

      World Platinum Producers

      Globally, the Uralian-Alaskan complexes are a significant source of platinum group metals (PGM). In Alaska, the Goodnews Bay Complex had 647,500 ounces of platinum recovered from its placers. The Salt Chuck lode mine produced 661,771 ounces of platinum and palladium as a by-product of copper ore from the Salt Chuck Complex.

      In Russia, the Ural region is a significant placer and lode producer of PGM from a Uralian-Alaskan complex. The placer deposits were discovered in the Ural Mountains in 1823 and have been producing PGM continuously up to the present. The historic PGM production from placer and lode deposits is not well documented but is considered significant. In the late 1980s, lode deposits reached peak platinum production of around 4.0 million ounces of palladium and 1.0 million ounces of platinum. In 2005, the lode deposits reported production of 751,000 ounces of platinum and 3,133 million ounces of palladium in the Ural region (Google).

      The other important producers of PGM in the world are in South Africa (Bushveld Complex) and in the USA (Stillwater Complex). The South Africa grades of PGM metal are typically between 3 and 6 grams per tonne. The USA grades of PGM metal are typically between 10 and 20 grams per tonne (Google).

      In the Princeton mining region, the Tulameen placer-platinum deposits have produced a reported 20,000 ounces of platinum. The lode platinum occurrences in the Tulameen platinum district range in values from 2.5 to 16.0 grams platinum per tonne.

      Conclusions

      The Goldcliff claims are located in the Princeton mining region which has favourable geology for multiple mineral deposits discoveries of platinum, gold and copper.

      The Goldcliff claims in the Princeton mining region are 100%-owned and are readily accessed by road.

      The Tulameen Project claim acquisition is consistent with Goldcliff's management policy to acquire high quality exploration projects.

      The Tulameen project area map, which includes the claims, is posted on Goldcliff's website www.goldcliff.com.

      Leonard W. Saleken, PGeo (geologist) is the qualified person as defined by National Instrument 43-101 who supervised the preparation and verification of the technical information in this release.

      GOLDCLIFF RESOURCE CORPORATION

      George W. Sanders, President

      The TSX Venture Exchange has not reviewed and does not accept responsibility for the adequacy or the accuracy of this news release, gcnnews2804.
      Avatar
      schrieb am 17.04.08 19:39:38
      Beitrag Nr. 4 ()
      das ding wird ja nur in B gehandelt... :confused:

      Avatar
      schrieb am 21.04.08 15:31:31
      Beitrag Nr. 5 ()
      Antwort auf Beitrag Nr.: 33.911.736 von Zockii am 17.04.08 19:39:38na und?:confused:

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      Avatar
      schrieb am 10.07.08 13:45:28
      Beitrag Nr. 6 ()
      hallo leute hat sich schon mal einer mit diesem wert auseinandergesetzt? kling soweit nicht schlecht für meine geschmack


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