广东官田黄铁矿矿床物质组分分布规律的研究 |
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引用本文: | 黄富荣.广东官田黄铁矿矿床物质组分分布规律的研究[J].化工矿产地质,1997,19(4):227-232. |
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作者姓名: | 黄富荣 |
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作者单位: | 化学工业部化学矿产地质研究院 |
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摘 要: | 官田黄铁矿矿床为一浅成低温水热脉状黄铁矿矿床,物质成分复杂,伴生有Cu、Au、Ag、Te、Bi等多种有益组分。矿床外围有铅、锌、钼等共生矿产。这些有益主元素或伴生元素的分布规律与大气降水成矿作用、两种不同性质溶液在运移途中相遇造成成矿元素淀积的成矿作用及构造变动密切相关。
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关 键 词: | 硫 伴生组分 分布 大气降水 成矿作用 构造变动 |
DISTRIBUTION OF MATERIAL COMPOSITIONS IN GUANTIAN PYRITE DEPOSIT OF GUANGDONG |
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Institution: | MCI Geological Institute for Chemical Minerals |
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Abstract: | Guantian pyrite deposit is known as a epithermal vein pyrite deposit with complicated material compositions including many accompanying useful components Cu, Au, Ag, Te, Bi,etc. In addition,in the periphery of the deposit there are a nember of coexsiting elements Pb, Zn, Mo and the like. Distribution of all these useful and accompanying elements was controlled, to a large extent, by multisource processes, such as introduction of meteorological water, meeting and precipitation of different elements while migrating,and comtemporary tectonic events. |
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Keywords: | sulfur associated component meteorological water mineralization tectonic event |
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