From the fields of regional crust-mantle structure, metallogentic settings, history of tectonic-magmatic activity, distribution of high antimony anomaly, characteristics of deposit, origin of ore-forming materials (including Sb, C, Si, S, solution and associated elements), black dikes, the relation of deposit and mantle metasomatism fluid is expounded by means of geology and geophysics. Xikuangshan antimony deposit is proved to be a typical vein deposit formed by mantle metasomatism fluid. On the basis of this knowledge, the prospecting criteria of blind orebody of the deposit are given as follows: extensive structuer which indicating the activities of mantle metasomatism fluid, change of host rocks (especially exsisting shale barrier bed), silication and carbonization alteration.

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At the same time, import agent titanium dioxide, ultra-white ultra-fine calcined kaolin, Brightener, magnesium hydroxide, carbon black, white carbon black gas, and has made three zinc Hunan Antimony Trioxide Antimony Industry Co., Ltd. in east China general agent, the company has a independent right to import and export products are exported to India, Korea, Singapore and other countries.

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antimony trisulfide：化學(xué)名:三硫化銻

antimony black 俗名:銻黑 | antimony trisulfide 化學(xué)名:三硫化銻 | antimony bloom 俗名:銻華

antimony orange：銻桔黃 銻橙

antimony black 銻黑 | antimony orange 銻桔黃;銻橙 | antimony oxide 銻白

ocher; bismuth：鉍華

"銻赭石;黃銻礦","ocher; antimony" | "鉍華","ocher; bismuth" | "黑赭石;錳土","ocher; black"