| 云南勐腊龙巴河小红桥组构造角砾岩型铜矿 |
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| 引用本文： | 和松文,刘仕军.云南勐腊龙巴河小红桥组构造角砾岩型铜矿[J].云南地质,2014(1):127-129. |
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| 作者姓名： | 和松文 刘仕军 |
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| 作者单位： | 云南地矿国际矿业公司,云南昆明650051 |
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| 摘 要： | 矿体赋存于中侏罗统小红桥组（花开左组下部）上段近东西向断裂破碎带中.已圈定V1、V2两个矿体,分别受F1、F2断裂控制,伴生Pb、Zn、Ag、Co、Ni,矿石以辉铜矿、黑黝铜矿为主,应属受断裂破碎带控制的构造角砾岩热液型铜矿床.
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| 关 键 词： | 辉铜矿黑黝铜矿 构造角砾岩型 断裂破碎带控制 中侏罗统小红桥组 云南勐腊龙巴河 |
LONGBAHE CU DEPOSIT OF XIAOHONGQIAO FORMATION STRUCTURE BRECCIA TYPE IN MENGLA,YUNNAN |
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| HE Song-wen,LIU Shi-jun.LONGBAHE CU DEPOSIT OF XIAOHONGQIAO FORMATION STRUCTURE BRECCIA TYPE IN MENGLA,YUNNAN[J].Yunnan Geology,2014(1):127-129. |
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| Authors: | HE Song-wen LIU Shi-jun |
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| Institution: | ( Yunnan International Mining Company of Geology and Mineral Resources, Kunming 650051 ) |
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| Abstract: | The orebody is in the nearly EW fault Fracture zone of Middle Jurassic Xiaohongqiao Formation （ Lower Huakaizuo Formation） Upper Member. 2 orebodies V1 and V2 have been outlined, which are separately controlled by fault F1 and F2. The main associated Pb, Zn, Ag, Co, Ni ores are chalcocite, etc, which must be the hydrothermal Cu deposit of structure breccia controlled by fault fracture zone. |
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| Keywords: | Chalcocite Structure Breccia Type Fault Fracture Zone Control Middle Turassic Xiao-hongqiao Formation Longbahe Mengla Yunnan |
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