tetradymite
- 网络碲铋矿;辉碲铋矿
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Tetradymite is a Te , Bi sulfide mineral which is usually difficult to form an independent one .
辉碲铋矿是一种较难独立成矿的碲硫化物。
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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 .
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。
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Chemical Analysis of Tetradymite for Major , Minor and Trace Elements
辉碲铋矿单矿物的主次痕量元素分析
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X  ̄ ray powder diffraction analysis of tetradymite
辉碲铋矿的X射线粉晶衍射分析
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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 .
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。
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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 .
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。