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南岭地区脉状黑钨矿床的地球化学类型 被引量:16
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作者 谭运金 《地球化学》 CAS 1982年第2期155-161,共7页
In accordance with the characteristics of associated minerals, trace elments in the altered rocks around the veins and the composition of wolframite and mica, the vein wolframite deposits in the Nanling Region can be ... In accordance with the characteristics of associated minerals, trace elments in the altered rocks around the veins and the composition of wolframite and mica, the vein wolframite deposits in the Nanling Region can be divided into two geochemical types:the wolframite-beryl-molybdenite-bismutite (native bismuth) type and the wolframite.cassiterite-sulfide (copper, zine, lead) type. Vein wolframite deposits of these two geochemical types were formed under different conditions. The wolframite-beryl-molybdenite-bismutite (native bismuth) type may be connected with high pH-Eh conditions whereas the wolframite-eassiterite-sulfide (copper, zinc, lead) type with low pH-Eh conditions. It is concluded that the two geochemical types of vein wolframite deposits are genetically related with two different geochemical types of granites in the Nanling Region. 展开更多
关键词 脉状黑钨矿床 地球化学 共生组合 区域构造
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