论贵州汞矿成因——地幔（裂隙）喷气成矿

ORIGIN OF MERCURY DEPOSITS OF GUIZHOU—FORMATION OF MANTLE （CRACK） EMANATION DEPOSITS

摘要: 笔者曾参加贵州汞元素分布特征的研究,并据贵州汞矿的一些地质资料,反映出汞成矿主要是与地壳内部构造活动有关,而表生聚汞作用是不明显的。笔者认为,贵州汞矿与深断裂有一定的依附性,与地幔物质有联系性,受构造层的控制,并且矿化还显现出分带性。从而提出贵州汞矿成因上属沿深断裂导上的地幔汞喷气,在地壳上部适当有利的地方的热水体中的成矿作用。

Abstract: Accroding to the distribution characteristics of mercury and geological data from mercury, deposits of Guizhou, origin of mercury is mainly due to structural activity,and hypergene cnrichment of mercury is not evident. The author considers that the formation mercury deposits of Guizhon depends on deep faults and is related to the mantle-derived naterials.They are controlled by structural layering and their mineralization shows zoral bution.Thus it follows that mereury deposits of Guizhou formed by emanation of mercury along deep faults up to sites favourable to localization of hydrothermal fluids.