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The document summarizes a preliminary structural study of the gold-bearing shear zone system at the Seabee Mine in northern Saskatchewan. The Seabee gold deposit is hosted by deformed gabbroic rocks intruded by felsic dykes. The gold-bearing veins occur in narrow, steeply dipping shear zones composed of foliated mylonites characterized by a steep foliation and mineral lineation. Auriferous veins occur as Riedel shears oriented at low angles to the foliation, as well as fault fill and extension veins. Kinema

Author

Rivai Anwar

Language

EN