| 云南金顶铅锌矿床成因研究 |
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| 引用本文： | 赵兴元.云南金顶铅锌矿床成因研究[J].地球科学,1989,14(5):523-530. |
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| 作者姓名： | 赵兴元 |
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| 作者单位： | China University of Geosciences，Wuhan 430074 |
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| 摘 要： |
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| 关 键 词： | 铅锌矿床 矿床成因 层控矿床 |
ON THE GENESIS OF THE JINDING LEAD-ZINC ORE DEPOSIT IN YUNNAN |
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| Zhao Xingyuan.ON THE GENESIS OF THE JINDING LEAD-ZINC ORE DEPOSIT IN YUNNAN[J].Earth Science-Journal of China University of Geosciences,1989,14(5):523-530. |
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| Authors: | Zhao Xingyuan |
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| Abstract: | Based on the geological setting, characteristics and some other mineralization information of the deposit, the deposit is considered to be of stratabound type. Depneumatolysis of the mantle source and hydrothermal-sedimentary processes predominate in the mineralization. The ore-location is formed in diagenesis , and reformed in epigenesis. The main ore-forming metals are derived from the upper mantle, a few of them from the crust; sulfur comes mainly from marine sediments, organic materials in continent facies and sulfide in the strata. There is a little deep-seated sulfur in the deposit. |
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| Keywords: | stratabound deposit geological setting mineralization information depneumatolysis of the mantle source Yunnan province |
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