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赛钦铜钴矿大地构造位置属秦祁昆地槽褶皱系所属Ⅱ级构造单元—昆仑华力西地槽褶皱带之柴南缘断褶带与东昆仑隆起带的交合部位,昆中深大断裂东段北侧,铜钴矿化赋矿岩性为晚三叠世陆相火山岩建造中的次安山岩。赛钦铜钴矿的形成具有其独特的地质环境和物化条件,而且成矿过程复杂多变,矿床成因与火山—次火山热液有密切的联系,其矿床成因类型为次火山热液型铜钴矿床。
The tectonic setting of the Saiqin copper-cobalt deposit is located at the intersection of the Qaidam fault and the East Kunlun uplift in the Qilun-Kunqin gneiss fold belt. On the north side of the segment, the lithology of copper-cobalt mineralization is sub-andesite in the Late Triassic continental volcanic rock. The formation of the Saiqin copper-cobalt deposit has its unique geological environment and physicochemical conditions, and the metallogenetic process is complicated and changeable. The genesis of the deposit is closely related to volcanic-subvolcanic hydrothermal. The genetic type of the deposit is subvolcanic hydrothermal copper Cobalt deposit.