Isotopic Geochemical Characteristics and Genetic Analysis of Shuizhuling Cu-Fe-Au-S Deposit,Eastern China

摘要：

　　The Shuizhuling Cu-Fe-Au-S deposit is characterized by a two-layer texture, evidently corresponding to its binary ability and vertical change.The δ34S values of pyrite from the upper stratiform ore bodies vary from +0.9‰ to +5.8‰, that of pyrite from the lower veined ores from +3.2‰ to +6.4‰.The δ34S values of barite from the upper stratiform ore bodies are +19.9‰.The δ18O of calcite from the lower veined ore bodies is +13.3‰, the δ13C of that being 1.2‰, while the δ18O is +14.1‰ and the δ13c is 2.2‰of dolomite from the upper stratiform ore bodies.The mean δ34S of pyrite increase gradually, with the average δ18O and δ13C decreasing progressively, from the upper stratiform ore bodies to the lower veined ore bodies.Studies on geology and isotope characteristics show the Shuizhuling Cu-Fe-S-Au deposit of submarine sedimentary exhalative origin.

关键词： Cu-Fe-Au-S deposit isotope geochemistry two-member texture eastern China Shuizhuling

作者: WANG Likao LI Hongyang GUO Yaojia

作者单位: Shijiazhuang University of Economics

会议类型: 国际会议

会议名称: 第十八届凯洛林国际地质学术研讨会(The 18th Kerulien International Conference on Geological)

会议地点: 石家庄

会议语种:英文

页码: 318-321

在线出版日期: 2013-09-20（万方平台首次上网日期，不代表论文的发表时间）