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湖南沃溪钨—锑—金矿床的矿石组构学特征及其成因意义
顾雪祥; OskarSchulz; FranzVavtar; 刘建明; 郑明华
Corresponding Author顾雪祥
2003
Source Publication矿床地质
ISSN0258-7106
Volume22Issue:2Pages:107-120
Abstract通过对湖南沃溪矿床的宏观至微观尺度上的矿石组构学研究,揭示出矿床系同生热水沉积成因。层状矿体、细脉状矿化以及围岩蚀变之间的空间关系,指示了矿石与其所赋存的围岩同时形成。矿床形成后的变质—变形作用,主要使矿物发生重结晶、碎裂、位错以及小范围的再活化等。
metadata_83矿床地球化学国家重点实验室
Keyword湖南 钨-锑-金矿床 矿石组构学 围岩 空间关系 同生热水沉积 变质-变形作用
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:1328685
Citation statistics
Cited Times:20[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/773
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Corresponding Author顾雪祥
Recommended Citation
GB/T 7714
顾雪祥,OskarSchulz,FranzVavtar,等. 湖南沃溪钨—锑—金矿床的矿石组构学特征及其成因意义[J]. 矿床地质,2003,22(2):107-120.
APA 顾雪祥,OskarSchulz,FranzVavtar,刘建明,&郑明华.(2003).湖南沃溪钨—锑—金矿床的矿石组构学特征及其成因意义.矿床地质,22(2),107-120.
MLA 顾雪祥,et al."湖南沃溪钨—锑—金矿床的矿石组构学特征及其成因意义".矿床地质 22.2(2003):107-120.
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