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Thursday, July 12, 2012 10:16:48 AM
Property Geology
The AU/WEN Property is chiefly underlain by a folded and faulted succession of steeply- dipping, northerly trending Upper Triassic Nicola Group. The dominant lithologies are volcanics, volcaniclastics and interbedded siltstone and flow breccias. On the AU claims, the lithologies mapped by Preto (1979) as confirmed by Freeze (1986) consists of greenish grey augite porphyry flows and related breccia intruded by microdiorite dykes as off shoots of the Pennask batholith. Similar lithologies occur on the MAL claim with the addition of siltstone and tuffaceous volcanics and on the WEN claim with the addition of flow breccia. The TOE claims are underlain by Upper Triassic Nicola volcanics, which at the northern part of the claim is in contact with quartz diorite of the Pennask Batholith. Dioritic intrusions inside the TOE claims may be related to the Pennask batholith.
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