| 红河车古铁金多金属矿矿化特征及成因探讨 |
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| 引用本文： | 孙玉海,李娜,坚润堂,柴旺,蹇龙,詹关山.红河车古铁金多金属矿矿化特征及成因探讨[J].云南地质,2011,30(4):425-427. |
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| 作者姓名： | 孙玉海 李娜 坚润堂 柴旺 蹇龙 詹关山 |
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| 作者单位： | 中国有色金属工业昆明勘察设计研究院地质研究院,云南昆明,650051 |
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| 摘 要： | 红河县车古铁多金属矿为近期新发现的金矿点,通过矿区已发现的三处矿化体的综合研究,并与典型矿床进行对比,认为本区金矿化体均为热液成因。
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| 关 键 词： | 铁铜金矿化体 地下水热液型 中溢侵入 破碎带赋矿 云南红河车古 |
A PROBE OF METALLOGENETIC CHARACTERISTICS AND GENESIS OF CHEGU MULTIMETALLIC FE-AU ORE SITE IN HONGHE,YUNNAN |
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| SUN Yu-hai,Li Na JIAN Run-tang,CHAI Wang,JIAN Long,ZHAN Mei-shan.A PROBE OF METALLOGENETIC CHARACTERISTICS AND GENESIS OF CHEGU MULTIMETALLIC FE-AU ORE SITE IN HONGHE,YUNNAN[J].Yunnan Geology,2011,30(4):425-427. |
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| Authors: | SUN Yu-hai Li Na JIAN Run-tang CHAI Wang JIAN Long ZHAN Mei-shan |
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| Institution: | (Kunming Institute of Geological Exploration & Design,China Nonferrous Industry,Kunming 650051) |
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| Abstract: | The Chegu multimetallic Fe ore site in Honghe has been discovered in recent years.According to the comprehensive study on discovered 3 metallogenetic bodies and the comparison with the geological characteristics of typical hydrothermal ore deposit,we think that the Au metallogenetic body in this area has the hydrothermal genesis. |
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| Keywords: | Fe-Cu-Au Metallogenetic Body Hydrothermal Type of Underground Water Middle T Intrusion Ore-Bearing Fracture Zone Chegu Honghe Yunnan |
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