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刚果(金)堪苏祁铜钴矿床位于东非大裂谷中段西侧NW向分支内,属于加丹加铜钴铀矿带一部分。该矿床具有2种成矿类型:一种是沉积岩型铜钴矿,以铜为主,伴生钴,铜矿早期受沉积型砂页岩地层的控制,钴矿赋存于韧脆性剪切构造带中,受后期构造的控制,剪切构造面理是钴矿的主要富集场所;另一种是后期伴随韧脆性剪切带生成的热液型钴铜矿,以钴的品位较高为特征。根据成矿地质条件及EH4物探解译成果分析,矿区深部及外围尚有该类型矿床的找矿潜力。
The Kansuqi copper-cobalt deposit in the DRC is located in NW NW of the middle section of the Great Rift Valley in East Africa and belongs to part of the Katanga copper-cobalt-uranium ore belt. The deposit has two metallogenic types: one is a sedimentary-type copper-cobalt ore, mainly copper, associated cobalt and copper deposits controlled by sedimentary sand-shale formations, and the cobalt deposits occur in the ductile-brittle shear zone , Controlled by later tectonics, and the shear tectonics is the main enrichment site for cobalt ore. The other is the hydrothermal cobalt-copper deposit formed in the later period accompanied by ductile-brittle shear zones, characterized by high cobalt grade. According to the analysis of metallogenic geological conditions and interpretation results of EH4 geophysical prospecting, the prospecting potential of this type of deposit is still found in the deep and the periphery of the mine.