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对汞矿成因,国内外争论已久,主要有沉积、升华、岩浆低温热液三种观点。近代以热液说占统治地位。最近数十年,尤其是60年代以来,随着地质工作不断地深入和发展,岩浆低温热液成矿论,遇到了难以克服的困难,而“沉积-热液改造”,“多源多成因”等观点,则普遍被人们所接受和赞赏。本文主要是在研究贵州省汞矿的基础上,试以综合多因素的方法,对贵州及其邻区的汞矿成因作初步探讨。不当之处,望批评指正。
The cause of mercury deposits, the controversy at home and abroad for a long time, there are three main deposition, sublimation, magma cryogenic hydrothermal. In modern times, said hydrothermal fluid dominated. In recent decades, especially since the 1960s, with the continuous deepening and development of geological work, magmatic low-temperature hydrothermal mineralization met with insurmountable difficulties. However, “sedimentary-hydrothermal transformation”, “multi-source and multi-genesis ”And other points of view, then generally accepted and appreciated by people. Based on the study of mercury deposits in Guizhou Province, this article attempts to make a preliminary discussion on the origin of mercury deposits in Guizhou and its adjacent areas by a comprehensive and multi-factor approach. Inappropriate, hope criticism correction.