湖南柿竹园钨-钼-铋-锡矿床中锡石的产状与成因
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MODE OF OCCURRENCE AND ORIGIN OF CASSITERITE IN THE SHIZHUYUAN SKARN W-Mo-Bi-Sn DEPOSIT,HUNAN PROVINCE
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摘要:
笔者通过电子探针观察在湖南省柿竹园夕卡岩型钨—钼—铋—锡矿床中找到了大量微米粒级的锡石。这些锡石在空间上与磁铁矿共生,在成因上却与早期含锡夕卡岩的交代蚀变作用有关。本文根据矿物组合特征和锡石产出形式讨论了锡石的形成过程,并且提出了本区含锡磁铁矿夕卡岩中锡石的成因模式。
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陈骏,C. Halls, C. J. Stanley.1992.湖南柿竹园钨-钼-铋-锡矿床中锡石的产状与成因[J].地质论评,38(2):164-172,[DOI].
Chen Jun, C. Halls, C. J. Stanley Department of Earth Sciences, Nanjing University, Nanjing Department of Geology, Royal School of Mines, Imperial College Department of Mineralogy, British Museum: Natural History.1992. MODE OF OCCURRENCE AND ORIGIN OF CASSITERITE IN THE SHIZHUYUAN SKARN W-Mo-Bi-Sn DEPOSIT, HUNAN PROVINCE[J]. Geological Review,38(2):164-172.
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