The Kenbridge nickel deposit is hosted by an oval shaped gabbroic suite and has a distinct “breccia pipe” appearance. Interpretation of outcrop lithological information is slightly complicated by deformation and metamorphism (regionally up to upper greenschist facies and with overprints of local contact metamorphism), and selective exposure within the project area. The following general rock descriptions have been modified from previous detailed outcrop mapping and reports (circa 1950’s).
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