"..This is a narrow, high-grade vein district. From the cross-sections we’ve seen, you have a real hard time connecting the veins. Continuity is a real real problem there,” Cook said.
Geologically the project is underlain by the Barkerville terrane, which is part of the Omineca belt of the Canadian Cordillera. Barkerville reports that gold mineralization occurs as quartz veins located in shear-type and tension-type fractures in lithologies more brittle than the surrounding lithologies, and as disseminated sulphide zones localized in the nose of secondary local fold structures that have the same northwesterly plunge as the regional, orogeny-related, asymmetrical, overturned, isoclinal fold structures.
Peter George has already been rebuked once for an overly-optimistic resource estimate, with the British Columbia Securities Commission forcing Rubion Minerals (RMX-V) in March 2011 to re-state an estimate prepared by George.."
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