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在很长时间里,汞-锑成矿的岩浆-热液(低温热液)假说在矿床成因中占着统治地位。现在,把汞矿与地下(地幔)汞的来源联系起来的超低温热液成矿假说又得到了发展。 在研究土耳其斯坦-阿拉依锑-汞矿之初,我们区分了汞锑矿化岩浆派生的低温热液性质和成矿物质岩浆来源这样两个不同的概念。此后,所搜集的大量资料表明,汞锑矿化的物质来源是围岩,特别是寒武纪、志留纪、泥盆纪和石炭纪的碳酸岩。岩浆源是造成成
For a long time, the magmatic-hydrothermal (cryogenic hydrothermal) hypothesis of mercury-antimony mineralization dominated the genesis of the deposit. Now, the hypothermia hydrothermal mineralization hypothesis linking mercury deposits to the source of subsurface (mantle) mercury has been developed. At the beginning of the study of the antimony-mercury deposits in Turkestan-Alray, we made a distinction between the two different concepts of the low-temperature hydrothermal properties derived from mercury-antimony-bearing mineralized magmas and the origin of ore-forming material magma. Since then, the large amount of information collected indicates that the sources of mercury-antimony mineralization are the surrounding rocks, especially the Cambrian, Silurian, Devonian and Carboniferous carbonates. Magma source is caused into