Mineral chemical identification of assimilation in the formation of Cu-Ni related layered intrusion: A case study of Hongshishan mafic-ultra mafic intrusion in Beishan area, Xinjiang (NW China)

摘要：

1 IntroductionMagmatic immiscibility and assimilation are the main factors controlling the sulfur saturation which is closely related to the formation of Cu-Ni ore deposit (e.g. Li et al., 2001; Naldrett, 2005). Immiscibility is rarely reserved because of covers from subsequent processes. On the other hand, records of assimilation could be tracked by petrological and geochemical observations. Abundant studies have documented whole-rock compositions (major, trace and isotope) are important references to distinguish assimilation and even its proportion (e.g. Sarkar et al., 2008; Stevenson et al., 2009). In current case study of Hongshishan intrusion, identification of assimilation from mineral chemistry is attemptly established integrating general indicators.

作者: Su Benxun Qin Kezhang Tang Dongmei Sun He Xiao Qinghua Cao Mingjian

作者单位: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Science Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Science

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: 227-230

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）