| 新疆温泉县喇嘛苏铜多金属矿床成因初探 |
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| 引用本文： | 赖健清,彭省临,钟运鄂,邵拥军,王核.新疆温泉县喇嘛苏铜多金属矿床成因初探[J].岩土工程界,1998(5). |
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| 作者姓名： | 赖健清 彭省临 钟运鄂 邵拥军 王核 |
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| 作者单位： | 中南工业大学地质系 |
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| 摘 要： | 喇嘛苏铜多金属矿床产于浅变质的库西姆切克群碳酸盐岩和海西期酸性岩体的接触带附近，属于沉积变质富集、岩浆改造型多因复成矿床。地质及地球化学特征分析表明，该矿床的形成过程可以总结为沉积－火山喷流沉积富集、区域变质富集和岩浆改造成矿等三个步骤。
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| 关 键 词： | 喇嘛苏 铜矿床 新疆 |
ON THE GENESIS OF THE LAMASU COPPER-POLYMETALLIC DEPOSIT IN WENQUAN, XINJIANG |
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| Abstract: | Occuring near the contact between Kuximqiek carbonate rocks and Hercynian acidic bodies, the Lamasu copper-polymetallic deposit is a polygenetic deposit formed by sedimentary-metamorphism and magmatic reworking. Its geology and geochemistry indicate that it was formed in three steps which are sedimentary and volcanic-exhalation, regional metamorphism and magmatic metallogenesis. |
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| Keywords: | polygenetic copper deposit Lamasu Xinjiang |
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