Mineralized magmatism of Kalatongke Cu-Ni sulfide deposit in Xinjiang, west China

摘要：

1 IntroductionThe Kalatongke Cu-Ni sulfide deposit in northern Xinjiang, west China is located in the East Junggar terrane. About 11 mafic-ultramafic complexes related to ore-forming in the Kalatongke region were distributed as two corridors along the southern side of the regional Irtysh fault zone, and intruded into slate and tuff of the Lower Carboniferous Nanmingshui Formation. The intrusions ＃1, 2, and 3 host economic Ni-Cu sulfide ores, and are well differentiated and compositionally zoned with the sulfide Re-Os isochron ages of 282.5±4.8 and 290.2±6.9Ma (Zhang et al., 2005), and 305±15Ma (Han et al., 2007).

作者: Fu Piaoer Zhang M J C Li Tang Q Y Li W Y Jia Z Y Shen H F

作者单位: Department of Geology, Lanzhou University, Lanzhou 730000, China Department of Geological Sciences, Indiana University, Bloomington, IN 47405, USA Xian Center of Geological Survey, China Geological Survey, Xian 710000, China

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: 82-84

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）