| 云南泸水外岩房锡钨矿床地质特征 |
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| 引用本文： | 戚林坤,孔云丽,段红达.云南泸水外岩房锡钨矿床地质特征[J].云南地质,2013(4):439-442. |
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| 作者姓名： | 戚林坤 孔云丽 段红达 |
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| 作者单位： | 云南省有色地质局三一○队,云南大理671000 |
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| 摘 要： | 锡钨矿体产于志本山岩体外接触带、上寒武统核桃坪组下段砂板岩层间破碎带的蚀变闪长—辉长岩脉带中,少数矿体产于岩体内接触带上.矿床成因属于与混合岩化后期派生岩浆有关的高—中温热液矿床.
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| 关 键 词： | 锡钨矿床 高—中温热液型 混合岩化 外接触带 云南泸水外岩房 |
THE GEOLOGICAL FEATURE OF WAIYANFANG SN-W DEPOSIT IN LUSHUI,YUNNAN |
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| QI Lin-kun,KONG Yun-li,DUAN Hong-da.THE GEOLOGICAL FEATURE OF WAIYANFANG SN-W DEPOSIT IN LUSHUI,YUNNAN[J].Yunnan Geology,2013(4):439-442. |
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| Authors: | QI Lin-kun KONG Yun-li DUAN Hong-da |
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| Institution: | (Geological Team 310, Yunnan Bureau of Nonferrous Geology, Dali 671000) |
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| Abstract: | The Sn - W ore body is in the altered diorite - gabbro vein zone in fracture zone of Upper Cambrian Hetaoping Formation Lower Member sandy slate of outer contact of Zhibenshan rock body. A few ore bodies are in the inner contact of the rock body. It belongs to the high - middle T hydrothermal deposit in relation to the later derived magma of migmatization. |
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| Keywords: | Sn- W Ore Deposit High -Middle T Hydrothermal Type Migmatization Outer Contact Waiyanfang Lushui Yunnan |
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