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Location: 45 km E from Reno, Nevada, United States
Suite 201 - 1512 Yew StreetVancouverBritish Columbia, CanadaV6K 3E4
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Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
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The mineralization was divided into the following domains, separated by north-northwest fault, for the purpose of resource modelling.Bear Creek Hanging-Wall Vein System/Domain, bounded by Ripper Fault to south and Cabin Fault to north. The Hanging-Wall vein is comprised predominantly of massive white sulphide poor silica with typical low- sulfidation epithermal textures, including recrystallization, coliform and crustiform banding, adularia bands, amethyst, etc.Bear Creek Footwall Vein System/Domain, bounded by Cabin Fault to south and Talapoosa (South) Fault to the north. The Footwall vein is more sulphide rich, associated with a number of gangue phases including, red hematitic silica, chlorite and minor white to clear silica. Main Zone Vein System/Domain bounded by Talapoosa (South) Fault to the south and Opal/Dyke Fault to the north.The mineralization at both Dyke Adit and East Hill shows similarities in appearance and texture to that of the Hanging-Wall Zone at Bear Creek.The modelling of veins and their bounding faults indicates that the general trend of all mineralization is around 115°, with two prominent dip angles:- Steeply-dipping veins at approximately 70° south, for the Hanging-Wall and Footwall Zones at Bear Creek and for the eastern-most portion of the Main Zone.- Shallowly-dipping veins, at approximately 20 to 40° south for the Dyke Adit, northwest part of the Main Zone (north) and the East Hill Vein. At least in the Main Zone, the flattening of vein dip could be the result of dilatational zones developed between the Talapoosa and Dyke Faults. In the case of the Dyke Adit and East Hill veins the attitude of the veining appears to parallel that of the contact between the hornblende andesite porphyry and the adjacent unit.
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