The contribution of hydrothermal activities to Jinchuan Ni-Cu-PGE sulfide deposit
The Jinchuan intrusion hosts one of the largest magmatic Ni-Cu sulfide deposits in the world. Since the discovery of the deposit, many experts think that it is the magmatic differentiated sulfide deposit, but field mapping and petrological-geochemical investigation of the Jinchuan intrusion suggest that it is not only the result of magmatic differentiated effection, but also in the process of diagenesis and tectonic metamorphism, hydrothermal activity has an important contribution to mineralization. Cu-PGE-rich ores are domain characterized by vein, which is a direct result of the hydrothermalism.
Xie Xie Li Wenyuan
College of Earth Science and Land Recourses, Changan University, Xian 710054, China Xian Center of China Geological Survey, CGS, Xian 710054 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
72-73
2009-09-01（万方平台首次上网日期，不代表论文的发表时间）