摘要
In recent years, Chinese geologists have discovered the elluvium-deluvian cobalt deposits in the Central African copper belt. These cobalt deposits are characterized by clear horizontal and vertical zoning, and dominated by heterogenite. They were formed by weathering of altered cataclastite and talc-schist ores in the original copper-cobalt deposits under certain physical-chemical conditions. Researches show that the south of the Katangan copper-cobalt belt between Kolwezi and Likasi in Central Africa is a region of prospecting potential for the elluvium-deluvian cobalt deposits.