辉碲铋矿

辉碲铋矿是一种较难独立成矿的碲硫化物。

Tetradymite is a Te , Bi sulfide mineral which is usually difficult to form an independent one .

重选研究发现可以回收一定量的辉碲铋矿，但是总的回收率和精矿碲品位较低。

It was revealed that gravity recovered parts of the tetradymite , but the total recovery rate and the Te grade of gravity concentrates were a little low .

辉碲铋矿的X射线粉晶衍射分析

X ￣ ray powder diffraction analysis of tetradymite

辉碲铋矿单矿物的主次痕量元素分析

Chemical Analysis of Tetradymite for Major , Minor and Trace Elements

矿区主要矿石为含辉碲铋矿的白云石，通过对其碳氧同位素的分析推断其形成可能主要与蚀变作用有关。

Mining ore contains mainly Tetradymite dolomite veins , and the formation of ore may be related with alteration through analysis of carbon and oxygen isotope . 3 .

成矿流体的40Ar/4He比值变化较大，磁黄铁矿黄铁矿阶段的磁黄铁矿为237～379，辉碲铋矿阶段的辉碲铋矿为7～66。

40 Ar / 4 He ratios of metallogenic fluids change greatly , being 237 ~ 379 for pyrrhotite of the pyrrhodtite_pyrite stage and 7 ~ 66 for tetradymite of the tetradymite stage .