Tectonic setting, geological features and evaluation of ore-bearing property for magmatic Cu-Ni deposits in eastern Tianshan, NW-China
1 Tectonic setting of Permain magmatic Cu-Ni deposits in Eastern TianshanNorthern Xinjiang in northwestern China is located along the southern margin of the oroclinally folded Altaid or Central Asian Orogenic Belt (CAOB) (Yakubchuk et al., 2002; Xiao et al., 2003, 2004). The CAOB is a vast region of Phanerozoic juvenile crustal growth on the southern side of the Siberian craton. Terranes of the Altay, Junggar and Tianshan areas are a part of the CAOB, which represents one of the largest Phanerozoic orogens of the world.
Qin Kezhang Sun He San Jinzhu Xu Xingwang Tang Dongmei Ding Kuishou Xiao Qinghua Su Benxun
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
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
95-99
2009-09-01(万方平台首次上网日期,不代表论文的发表时间)