Abstract:Shewushan gold deposit occured in overtured anticline and double thrust tectonic which were mainly composed of Cambrian-Ordovician Carbonatite, and belong to epithermal ore deposit (primary gold deposit).The Shallow orebody, that is primary gold deposit occured in gently dipping fault tectonite underwent near a hundred million years' weathering-Leaching transformation, and became strippable weathering gold deposit.Ore grade is low. Gold appeared in micro-fine grained impregnation state. Compared with Carlin type gold deposit, Shewushan goid deposit belong to Carlin type and can be divided into two subtypes:primary and weathering gold deposit.
刘施民, 黎家祥. 湖北蛇屋山卡林型金矿地质及成因[J]. 地质与资源, 1995, 4(3): 184-192.
Liusbimin, Lei Jiaxiang. GEOLOGY AND GENESIS OF SHEWUSHAN CARLIN TYDE OF GOLD DEPOSIT IN HUBEI PROVINCE. GEOLOGY AND RESOURCES, 1995, 4(3): 184-192.