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青海省哈尔汗铜-钴矿床地质特征及成因探讨

Shang-li XU,Jun-min LI,Peng-kui REN,Wen-shan LIN

MINERAL RESOURCES AND GEOLOGY（2005）

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Abstract
哈尔汗(督冷沟)铜-钴矿床位于东昆仑多金属成矿带东段.该矿床地质工作及研究程度极低,铜钴矿体明显受万保沟群基性火山岩层位及断裂构造控制.根据矿床地质特征及同位素特征分析,认为该矿床成因为火山喷气-沉积-热液叠加改造复合型矿床,具中-大型远景规模.
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