| 驼路沟钴矿床地质特征及成因分析 |
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| 引用本文： | 董琳,任鹏奎,曹德智,王燕.驼路沟钴矿床地质特征及成因分析[J].矿产与地质,2008,22(4):306-310. |
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| 作者姓名： | 董琳 任鹏奎 曹德智 王燕 |
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| 作者单位： | 青海省地质调查院,西宁,810012 |
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| 摘 要： | 文章从矿床地质特征、矿体特征及成矿岩系和热水建造等方面进行研究，并对矿床成因进行分析，认为驼路沟钻矿床是典型的海底热水喷气沉积改造成因的钻矿床。
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| 关 键 词： | 钻矿床 矿床特征 成因分析 驼路沟 青海 |
Geological characteristics and genesis of the Tuolugou Co deposit |
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| DONG Lin,REN Peng-kui,CAO De-zhi,WANG Yan.Geological characteristics and genesis of the Tuolugou Co deposit[J].Mineral Resources and Geology,2008,22(4):306-310. |
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| Authors: | DONG Lin REN Peng-kui CAO De-zhi WANG Yan |
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| Institution: | (Qinghai Provincial Geologcial Survey, Xining 810012, China ) |
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| Abstract: | It has studied the deposit from the aspects of geological characteristics, orebodies＇ features, metallogenic rocks series and so on in this paper, and analyzed the genesis of this deposit. It has believed that the Tuolugou Co deposit is formed by typical submarine hydrothermal exhalative-sedimentary alteration. |
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| Keywords: | Co deposit characteristics of the deposit genesis analysis Tuolugou Qinghai |
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