Abstract：Kanggul gold deposit occurs in a second-order shear zone within a large-size ductile shear zone on the northern margin of Carboniferous island arc volcanic area.Orebodies,hosted by altered phyllonite and mylonitized volcanic rocks,are parallel to the steep-dipping mylonite zone.The wall rock alterations include silicification,chloritization,sericitization and pyritization.Geological studies show that the tectonic altered metallogenic characteristics have zoning phenomenon.The doposit is a product of polyphase evolution.The ore materials were derived from volcanic rocks.The ductile shearing is not only an ore controlling structure,but also a kind of mineralization by its ductile deformation and metamophism.A model of metollogenesis of ductile shear zone gold deposit of Kanggul is established.
张连昌, 曾章仁, 杨兴科, 姬金生, 赵伦山. 康古尔韧性剪切带型金矿构造地球化学特征[J]. 地质与资源, 1997, 6(1): 13-21.
Zhang Lianchang, Zeng Zhangren, Yang Xingke, Ji Jinsheng, Zhao Lunshan. TECTONO-GEOCHEMICAL CHARACTERISTICS OF THE DUCTILE SHEAR ZONE TYPE GOLD DEPOSIT IN KAN GGUL, XINJIAN G. GEOLOGY AND RESOURCES, 1997, 6(1): 13-21.
1997, Vol. 6 
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