| 浅析贵州二叠系锰矿与峨眉山玄武岩之关系 |
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| 引用本文： | 韩忠华,潘家州. 浅析贵州二叠系锰矿与峨眉山玄武岩之关系[J]. 贵州地质, 2007, 24(3): 197-201 |
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| 作者姓名： | 韩忠华 潘家州 |
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| 作者单位： | 贵州省地矿局106地质大队,贵州,遵义,563000;贵州省地质调查院,贵州,贵阳,550004 |
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| 摘 要： | 贵州遵义-水城地区中二叠纪茅口组第二段顶部产出的原生碳酸锰和氧化锰矿床,为贵州二叠系锰矿主要矿床。贵州中西部有大量的峨眉山玄武岩分布。本文就贵州二叠系锰矿与峨眉山玄武岩之关系进行探讨。
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| 关 键 词： | 峨眉山玄武岩 二叠系 锰矿 贵州 |
| 文章编号： | 1000-5943（2007）03-0197-05 |
| 修稿时间： | 2007-03-07 |
Relationship Analysis on Permian Manganese and Emeishan Basalt in Guizhou |
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| HAN Zhong-hua,PAN Jia-zhou. Relationship Analysis on Permian Manganese and Emeishan Basalt in Guizhou[J]. Guizhou Geology, 2007, 24(3): 197-201 |
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| Authors: | HAN Zhong-hua PAN Jia-zhou |
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| Abstract: | Primary carbonate manganese and manganese oxide,hosted at the top of second section of Permian Maokou Formation in the Zhunyi-Shuicheng areas of Guizhou,are a majority of manganese deposits of the Permian.Widespread Emeishan basalt covers in western Guizhou area.Correlation between Permian manganese ores and Emeishan basalt is introduced. |
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| Keywords: | Emeishan basalt Permian manganese ores Guizhou |
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