| 横山岭铅锌矿床地球化学特征 |
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| 引用本文： | 孙振家.横山岭铅锌矿床地球化学特征[J].中南大学学报(自然科学版),1991(2). |
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| 作者姓名： | 孙振家 |
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| 作者单位： | 中国矿业学院地质系 |
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| 摘 要： | 文中讨论了横山岭铅锌矿床成矿元素地球化学背景、演化、空间分布特征及其富集过程,同时阐明本矿床为一受矿源层、矿源体、构造位控制的多因复成矿床。
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| 关 键 词： | 地球化学 多因复成矿床 铅锌矿 横山岭 |
THE FEATURES OF THE GEOCHEMISTRY OF HENGSHANLING LEAD--ZINC DEPOSITS |
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| Sun Zhenjsa.THE FEATURES OF THE GEOCHEMISTRY OF HENGSHANLING LEAD--ZINC DEPOSITS[J].Journal of Central South University:Science and Technology,1991(2). |
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| Authors: | Sun Zhenjsa |
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| Institution: | Department of Geology |
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| Abstract: | The geochemical setting, evolution, distribution, and mineralization proccesses of the ore-forming elements in Hengshanling lead-zinc deposits are presented and discussed in this paper. It is explained that the deposit is a polygenetic compound ore deposit which was controlled by source rocks and con- structures' positions. |
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| Keywords: | geochemistry polygenetic compound ore deposits lead-zinc deposits Hengshanling |
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