| 试论岩溶在沉积—改造铅锌矿床形成中的作用 |
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| 引用本文： | 刘功余,邓自强.试论岩溶在沉积—改造铅锌矿床形成中的作用[J].矿产与地质,1993,7(2):102-107. |
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| 作者姓名： | 刘功余 邓自强 |
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| 作者单位： | 地质部岩溶地质研究所 桂林541004
(刘功余，邓自强，张美良)，地质部岩溶地质研究所 桂林541004(林玉石) |
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| 摘 要： | 在碳酸盐岩地区广泛分布着一些沉积—改造铅锌矿床.其主要改造作用目前一般概括为地下(热)水作用.本文通过比较地下水改造成矿作用与岩溶作用之间的关系,论证岩溶在矿床形成中起着重要作用,即地下水改造富积成矿作用主要为岩溶作用.
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| 关 键 词： | 岩溶 沉积 铅锌矿床 地下水 |
DISCUSSION ON THE KARST AS A FACTOR IN THE FORMATION OF SEDIMENTARY-TRANSFORMATION Pb-Zn DEPOSITS |
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| Liu Gongyu,Deng Ziqiang,Zhang Meiliang,Lin Yushi.DISCUSSION ON THE KARST AS A FACTOR IN THE FORMATION OF SEDIMENTARY-TRANSFORMATION Pb-Zn DEPOSITS[J].Mineral Resources and Geology,1993,7(2):102-107. |
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| Authors: | Liu Gongyu Deng Ziqiang Zhang Meiliang Lin Yushi |
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| Abstract: | In the carbonate rock area ,there are some sedimentary -transformation Pb-Zn deposits. The transformation ore -forming processes are usually summarized as underground (hot)water processes. Comparing the karst processes with the transformation ore-forming processes in their development course. It is considered that the karst plays an important role in the formation of the deposits . That is to say .actually karst processes make the transformation, accumulation, concentration ore-forming processes of underground water in the carbonate rock area. |
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| Keywords: | Karst Sedimentary-transformation Pb-Zn deposits Underground water Carbonate rock |
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