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独山锑矿田位于独山箱状背斜核部近倾伏端，矿床、矿体的产出严格受断裂控制，其半坡式锑矿呈脉状产于下泥盆统、志留系碎屑岩的陡倾斜断裂中；其巴年式的锑矿呈层状产于中泥盆统碎屑岩与碳酸盐岩之间的层间滑动带中。成矿温度低，矿石组分和围岩蚀变简单，锑主要来源于下伏地层，硫主要来源于赋矿地层．成矿流体主要为大气降水，构造动力成矿作用导致锑矿床的形成，矿床类型为一典型的构过动对热液矿床。
The Dushan antimony ore field is located at the downturn near the core of the Dushan box-like anticline. The output of the ore deposit and ore body is strictly controlled by the fault. The semi-slope antimony ore is vein-shaped in the lower Devonian and Silurian Clastic rocks in the steep-sloping fault; the Barian-type antimony ore is stratified in the Middle Devonian clastic rocks and carbonate strata between the slip band. Low metallogenic temperature, simple alteration of ore components and wall rocks, antimony mainly comes from underlying strata, and sulfur mainly comes from ore-bearing strata. The ore-forming fluid is mainly the precipitation of the atmosphere, the tectonic dynamic mineralization led to the formation of the antimony deposit, and the deposit type is a typical over-active-hydrothermal deposit.