Geochemical Characteristics of Shimenkou CuFeAuS Deposit,
///The Shimenkou Cu-Fe-Au-S deposit was presented by the upper stratiform ore beds and the lower disseminated-veinlet ores. The Re-Os isotopic model age of pyrites in the ores was 303±33 Ma. The geological-geochemical features show the Shimenkou Cu-Fe-S-Au deposit is of submarine sedimentary exhalative origin.