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金山金矿床位于赣东北深大断裂北西盘，金成矿作用与区域构造演化关系密切；构造对该矿床具多级控制的特点：①赣东北深大断裂是区域上一级控矿构造，控制着金成矿带的空间展布；②金山—西蒋韧性剪切带是引导成矿流体运移的矿田（床）构造；③剪切带中非连续变形晚期脆性断裂系统是主要的容矿构造
The Jinshan gold deposit is located in the northwestern plate of the deep fault of northeastern Jiangxi and the gold mineralization is closely related to regional tectonic evolution. The multi-level control of the ore deposit is characterized by the following features: (1) The spatial distribution of the gold metallogenic belt; ② the Jinshan-Xijiang ductile shear zone is the orefield structure that leads the migration of ore-forming fluids; ③ the late brittle fracture system of discontinuous deformation in the shear zone is the major ore-hosting structure