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云南武定荒箐铁铜多金属矿矿床成因
引用本文:朱晖,周元昆,李迅,周丽英,赵云.云南武定荒箐铁铜多金属矿矿床成因[J].云南地质,2010,29(1):53-55,52.
作者姓名:朱晖  周元昆  李迅  周丽英  赵云
作者单位:云南省有色地质局312队,云南,安宁市,650300
摘    要:矿床产于断层破碎带中,受断层和地层层位控制,与迤纳厂矿床具有一定的相似性。铁矿为中低温热液裂隙充填型脉状矿床,而铜矿床应为沉积——变质型。

关 键 词:昆阳群铁铜矿床  断裂背景  构造复合部位  改造富集  云南武定荒箐

THE GENESIS OF HUANGQING FE-CU MULTIMETALLIC DEPOSIT IN WUDING,YUNNAN
ZHU Hui,ZHOU Yuan-kun,LI Xun,Zhou Li-ying,ZHAO Yun.THE GENESIS OF HUANGQING FE-CU MULTIMETALLIC DEPOSIT IN WUDING,YUNNAN[J].Yunnan Geology,2010,29(1):53-55,52.
Authors:ZHU Hui  ZHOU Yuan-kun  LI Xun  Zhou Li-ying  ZHAO Yun
Institution:(Geological Team 312, Yunnan Bureau of Nonferrous Geology, Arming 650300)
Abstract:The ore deposit in fault fracture zone is controlled by the fault and stratigraphic horizon, with a certain similarity to the Yinachang ore deposit. The Fe deposit belongs to the middle - low T hydrothermal fissure filling type, but the Cu deposit belongs to the sedimentary -metamorphic one.
Keywords:Fe - Cu Deposit of Kunyang Group  Fault Background  Structure Composite Part  Reforma- tion Enrichment  Huangqing  Wuding  Yunnan
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