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A STUDY ON THE METALLOGENETIC CONDITION OF TONGCHANGHE CU DEPOSIT IN NINGLANG, YUNNAN
Author(s): 
Pages: 46-58
Year: Issue:  1
Journal: YUNNAN GEOLOGY

Keyword:  宁蒗铜厂河铜矿床控矿构造矿体空间分带成矿模式;
Abstract: 宁蒗铜厂河铜矿床系喜马拉雅期隐伏斑岩体外接触带玄武岩系热液型铜矿床,其主要含矿层位为上二叠统玄武岩组三段(P2β3)与黑泥哨组(P2h).主干控矿构造为南北向断裂体系,铜矿化均产于NW向F1断裂的下盘(南盘).矿区具显著的成矿多期、多阶段性和矿化体水平、垂直分带性规律.通过对碳、氧、硫等稳定同位素和包裹体分析及成矿热液演化特征探讨,建立了铜厂河铜矿热液成矿模式.
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