GSP Resource Corporation
GSP Resource Corporation
The Asp 14 Showing – and selected samples from the showing report 2 – 4% copper. One sample was collected, confirming the presence of significant contents copper, gold and palladium and anomalous contents of platinum, nickel and cobalt
Area | 2455.54 hectares
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Location | The property is located in the Interior Plateau area of South Central British Columbia, 25 kilometers northwest of Princeton.
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Property Geology | The claims are underlain by rocks of the Alaskan-type Tulameen Mafic/Ultramafic Complex. The mafic and ultramafic rocks were emplaced into metasedimentary and intermediate metavolcanics rocks belonging to the Upper Triassic Nicola Group during a late Triassic deformational event. This volcanic assemblage evolved during the Late Triassic arc magmatism and these rocks are considered to be co-magmatic with the rocks of the Tulameen mafic-ultramafic suite. |
Target Model | The target model is a Massive copper/nickel sulphide deposit with significant content of platinum, palladium and gold in mafic to ultramafic rock. Placer gold, platinum and palladium have been developed in the Tulameen River and tributaries draining the complex since the mid 1800’s. Bedrock showings of copper, nickel, gold, platinum have been discovered. |
Potential | The Tulameen ultramafic complex is one of the only locales in southern BC that offers the potential of discovering a commercially viable nickel deposit such as those discovered in Voisey’s Bay, Labrador or Norillsk, Russia. This has been an area of exploration activity from major and junior companies. Therefore, the potential of making a discovery in this area is a realistic goal to have
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#1610 – 777 Dunsmuir Street
Vancouver, BC V7Y 1K4
Mobile: +1-604-619-7469
Email: info@gspresource.com
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