Geological features and ezploration at the southern part of the Jinchuan Cu-Ni mineralization area, Gansu, China
1 IntroductionAs one of the worlds largest magmatic Ni-Cu sulfide deposits, the Jinchuan is well known by the world. Since the deposit was found in 1958, a lot of researches focused on the further exploration in surround areas have been undertaken (e.g., Tang and Li, 1995; Tang et al., 2006; Li, 2006). On the basis of previous studies, three criteria are emphasized during the exploration: 1. ultramafic intrusions; 2. the old metamorphosed Baijiazuizi Formation; and 3. clear magnetic anomalies. Commissioned by the Jinchuan Group Ltd, a detail geological mapping (1:10,000) was carried out in the southern part of the Jinchuan area, where is near the Jinchuan mineralized intrusion, last year. The methods of remote sensing, geochemical exploration, and magnetic survey are also applied. Some new understandings are obtained from the work. Here, we present the results of the study.
Zeng Nanshi Luo Xianrong Peng Qiaoliang Wen Meilan
Key Laboratory of Geological Engineering Centre of Guangxi Province, Guilin University of Technology, Guilin 541004, 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
78-81
2009-09-01（万方平台首次上网日期，不代表论文的发表时间）