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《GEOCHIMICA》 1996-04
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LiuAiping;ZhongZichuan;TangJianwu (Chengdu Institute of Technology,Chengdu 610059)(Sichuan Research Institute of Petroleum Exploration and Development, Chengdu 610051)  
The geochemical features of the first tellurium deposit in the world are studied in this paper. The key point is placed on the geochemical condition of trace-dispersed element Te concentrating in the deposit. This deposit is a hydrothermal deposit which belong to the Te-Bi-Au-Ag association type. The ore bodies are the carbonate veins and pyrrhotite veins with the average grades of 5.98% Te, 8.02% Bi, 9.73 10-6 Au and 37.45 x 10-6 Ag.The ore-forming elements (Te, Au and Ag) mainly come from the deep hydrothermal fluid rich in CO2 and S. When the hydrothermal fluid raised along the abyssal fault to shallow crust,the ore-forming elements Bi and Fe were extracted from the surrounding rocks. The Sexsited in the fluid combined firstly with Fe, forming the pyrrhotite.As a result,the S concentration in the fluid was reduced. This made the trece-dispersed element Te combining with the precipitating agents such as Bi, Ag and Au and forming the tetradymite, tsumoite, joseite-B, hessile and calaverite. At last the deposit was formed.
【Fund】: 中国科学院矿床地球化学开放研究实验室资助
【CateGory Index】: P618.83
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