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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。
The Harhan (Duolingou) copper-cobalt deposit is located in the eastern section of the eastern Kunlun polymetallic metallogenic belt. The geological work and research level of this deposit is very low. The copper and cobalt ore bodies are obviously controlled by the basic volcanic layers and faults in the Wanbaoogou Group. According to the geological characteristics and isotopic characteristics of the deposit, it is believed that the genesis of the deposit belongs to the composite deposit of volcanic jet-sedimentary-hydrothermal superimposition and transformation, with medium-large scale.