摘要
///Dimma Cu-Co deposit is located in the northwest end of Cu-Co ore belt in Luffilian fold arc at boundary between Congo(Kinshasa) and Zambia. It is related to volcanism and syn-sedimentary faulting and reworked by folding, fracturing,metamorphism and secondary enrichment in late orogenic process. Therefore, it is a polygenous Cu-Co deposit controlled by multi-factors.