PGE enrichment regularity in Cu-Ni deposits hosted in small mafic-ultramafic intrusions, eastern Xinjiang
The Eastern Tienshan in Xinjiang is a very important tectonic belt. It separates the Sibria plate to the north from the Tarim plate to the south. From the early Paleozoic to the late Paleozoic, the eastern Tienshan was controlled by Siberain and Tarim plates movement mechanism and accompanied by mantle-originated magma ascending to the crust which formed two paralled trench-arc-back-are basin composite tectonic systems (Qin et al., 2002; Li et al., 2006). The eastern Xinjiang region also is one of the most important Ni-Cu-Co metallogenic belts in China. There are many medium sized to large-scale mgmatic Ni-Cu deposits occurred in this region and adjacent areas.
Tang Dongmei Qin Kezhang Sun He Su Benxun Xiao Qinghua
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
国际会议
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)
西安
英文
112-114
2009-09-01（万方平台首次上网日期，不代表论文的发表时间）