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中国是世界上锑资源和生产大国。锑矿床划分为喷流沉积改造型、沉积改造型、变质再造型、岩浆热液型、火山热液型和外生堆积型六大类，细分十三亚类。近千个锑矿床（点）主要分布于华南锑矿成矿带、昆仓—秦岭锑成矿带、藏滇锑成矿带和阴山—天山锑成矿带。其中华南锑矿成矿带是最重要的锑成矿带，该带中有三个矿化集中区呈等间距分布。中国锑矿床最重要的成矿期为泥盆纪和侏罗－白垩纪。主要赋矿岩系为泥盆纪细碎屑岩—碳酸盐岩系，其次为元古界浅变质碎屑岩。
China is the world’s antimony resources and producing countries. The antimony deposit is divided into six major categories: jet stream alteration, sedimentary remodeling, metamorphism reformation, magmatic hydrothermal type, volcanic hydrothermal type and exogenous accumulation type, which are subdivided into 13 sub-categories. Nearly a thousand antimony deposits (spots) are mainly distributed in the South China antimony ore belt, the Kunlun-Qinling antimony metallogenic belt, the Tibetian antimony metallogenic belt and the Yinshan-Tianshan antimony metallogenic belt. Among them, the South China antimony ore belt is the most important antimony metallogenic belt, and three mineralized zones are equidistantly distributed. The most important metallogenic stages of China’s antimony deposits are the Devonian and Jurassic-Cretaceous. The main ore-bearing rocks are Devonian fine clastic rocks and carbonate rocks, followed by Proterozoic metamorphic clastic rocks.