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矿床地质  2003 

湖南沃溪钨-锑-金矿床的矿石组构学特征及其成因意义

Keywords: 地质学,矿石组构,沉积喷流,同生成因,钨锑金矿床,沃溪,湖南

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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。

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