STRUCTURAL EVOLUTION AND METALLOGENY OF SOUTH XINJIANG METALLOGENIC BELT, JIANGXI, SOUTH CHINA

来源期刊：中南大学学报(英文版)1996年第1期

论文作者：Liu Jishun Wu Yanzhi Li Peizheng

文章页码：50 - 53

Key words：structural evolution: Cathysia basement; rift: metallogeny;Cu-polymetal; Jiangxi

Abstract: South Xinjian Cu-Au-Ag Metallogenic Belt is located near the boundary between Jiangnan Terrane and Cathysia Terrane. It has the cathysia type of crystalline basement, and experienced basin opening (rifting) for three times and the basin closing for three times since Proterozoicage. In correspondance with the structural evolution the belt has developed three sets of ore-forming rock series and happened reformed metallization for three_times. The emplacement of large deposits has been controlled by the crossing of many different geological factors.