Known mineralization within the project area is spatially associated with calc-alkaline intrusions. Different zones exhibit a combination of geological characteristics and gold-silver grades of both porphyry and epithermal mineralization styles. Collectively the zones may be best characterized as intrusion-related ‘transitional’ deposits. They consist mainly of a hydrothermally altered breccia “pipe”, tabular in shape and similar in nature to other quartz-sulphide gold+/-copper+/-silver epithermal breccia deposits.