General characteristics of fluid inclusions in magmatic Ni-Cu-PGE sulfide deposits

摘要：

1 IntroductionMagmatic Ni-Cu-platinum group element(PGE)ores result from liquid immiscibility between sulfide and silicate magmas(Naldrett, 1989); however, it is clear that hydrothermal processes also play a role in PGE and base-metal. especially Cu enrichment in some magmatic ore deposits (Watkinson, 1990; Farrow, 1994). The purpose of this paper is to evaluate the possible role of fluids in enrichment of copper, nickel and PGE.

作者: Qin Zhipeng Wang Xiongwu Zhou Yun Zhou Qiang Zeng Qiang

作者单位: College of Earth Science, Chengdu University of Technology, Chengdu 610059, China Faculty of Materials and Metallurgical Engineering,Kunming University of Science and Technolog, Kunm Regional geogical investigative team of Sichuan geologic mineral nerambulative development bureau, C

会议类型: 国际会议

会议名称: Xian International Ni-Cu(Pt) Deposit Symposium 2009(2009 西安·Ni-Cu(Pt)岩浆矿床国际学术研讨会)

会议地点: 西安

会议语种:英文

页码: 24-25

在线出版日期: 2009-09-01（万方平台首次上网日期，不代表论文的发表时间）