TREK Geological Mapping Project, Year 2: Update on Bedrock Geology and Mineralization in the TREK Project Area, Central British Columbia (parts of NTS 093B, C, F, G) J.J. Angen, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC,
[email protected] J.M. Logan, Consulting Geologist, North Saanich, BC C.J.R. Hart, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC R. Kim, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC Angen, J.J., Logan, J.M., Hart, C.J.R. and Kim, R. (2016): TREK geological mapping project, year 2: update on bedrock geology and min- eralization in the TREK project area, central British Columbia (parts of NTS 093B, C, F, G); in Geoscience BC Summary of Activities 2015, Geoscience BC, Report 2016-1, p. 1–16. Introduction The Interior Plateau region of British Columbia is con- sidered to have high exploration potential as it hosts a variety of deposit types including Late Cretaceous and Eocene epithermal Au and Ag deposits (e.g., Blackwa- ter, Capoose and Wolf) and porphyry Cu and Mo depos- its (e.g., Endako and Chu) ranging in age from Late Ju- rassic to Eocene. Exploration activity has historically been hindered by a limited understanding of the charac- ter and distribution of prospective units owing to the masking effects of overlying Eocene and Neogene ba- salt flows and extensive glacial till cover. The Targeting Resources through Exploration and Knowledge (TREK) project is a Geoscience BC initiative to inte- grate geophysical, geological and geochemical data in order to improve our geological understanding and, ul- timately, reduce the risk associated with exploration in such a poorly understood region (Clifford and Hart, 2014).