Abstract:The Dishui copper deposit in Xinjiang Uygur Autonomous Region, a typical Cenozoic lacustrine sedimentary rock-hosted deposit, lies in the southwestern margin of Kuqa depression basin. The ore bodies occur as stratiform, between the overlying grey marl and the underlying greyish white medium-grained sandstone. The copper grade is positively related to Fe2+ while negatively to Fe3+. Cuprite is the major ore mineral. The synthetic research indicates that the Dishui copper deposit experienced several genetic stages such as syn-sedimentary, diagenetic reformation and oxidation leaching. The deposit belongs to sedimentary transformation lacustrine sedimentary rock-hosted copper deposit.
时文革, 姚玉增, 巩恩普, 褚亦功, 张永利, 赵纯福. 新疆滴水陆相砂岩型铜矿成因浅析[J]. 地质与资源, 2016, 25(1): 60-68.
SHI Wen-ge, YAO Yu-zeng, GONG En-pu, CHU Yi-gong, ZHANG Yong-li, ZHAO Chun-fu. RESEARCH ON METALLOGENY OF THE DISHUI LACUSTRINE SEDIMENTARY ROCK-HOSTED COPPER DEPOSIT IN XIJIANG REGION. GEOLOGY AND RESOURCES, 2016, 25(1): 60-68.