Geochemical Features of Danzhai Carlin-Type Gold Deposit,Southeast of Guizhou

摘要：

　　The petrochemistry and trace element data show that the change law of SiO2, Au, As, Sb, CaO, CO2 and MgO contents from unaltered to the most intensely silicified limestones.The REE contents and partition patterns of the altered and mineralized rocks are largely consistent with those of the unaltered host rocks (laminated limestone).The REE content of intensely carbonated rocks is lower, MREE is slightly enriched.The fluid inclusion data indicate that the ore-forming fluids are of the Cl-rich type and that exploding temperatures of fluid inclusions in the quartz and calcite are about 200~338℃.The geochemical study of isotopes such as S, O, H and Pb shows that the medium-water of ore fluids is dominantly of meteoric origin.The ore-forming materials are predominately of crust source with small amounts of mantle component.

关键词： Carlin-type gold deposit Geochemistry Danzhai gold deposit

作者: WU Peng LI Hongyang ZHANG Zongchao

作者单位: Shijiazhuang University of Economics,Shijiazhuang,P.R.China

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: 223-227

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）