摘要
Katanga copper-cobalt metallogenic belt in Congo (DRC) is western extension part of the world’s famous Congo (DRC)-Zambia’s copper-cobalt metallogenic belt. Roan Group of Katanga rocks is the main ore-bearing strata. Due to folds and nappe tectonics, so deeply buried ore-bearing strata were pushed to the surface cover, thus forming rich-shallow copper-cobalt metallogenic belt along fold distribution in Lufilian arch.