摘要
Zambia is one of the most famous copper production places in the world. The copper ore deposits in Zambia include stratabound, sedimentary, metamorphosed-deformation and hydrothermal types, and are dominated by the sedimentary type. Statistics indicate that the sedimentary copper ore resources account for 79% of the whole resources in Zambia. All kinds of the copper ore deposits are controlled by the Luflian arc. The stratabound copper deposits are mainly discovered in the perifornical region, and the ore-bearing rock serious are the Muva megagroup biotite schist and around the anticlines and two-mica quartz schist. The sedimentary copper deposits are mainly distributed around anticlines and the peripheral dome, and the ore-bearing rock series are the lower Katanga megagroup sandstone-shale beds.