Geological-Geochemical Prospecting Model for the Rexiang Copper Deposit in Western Sichuan Province
详细信息
- 责任者：Fei Guangchun (College of Earth Sciences ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Youguo
- 刊名：Geophysical and Geochemical Exploration
- 出版年：2010
- 卷期：34(1)
- 关键词：铜矿 ; copper ores ; 四川 ; Sichuan Province
- 页码：p.19-23
- 图表：4 illus., 3 tables, 14 refs.
- 分类号：1600
- issnNo：ISSN1000-8918
- isbnNo：CN11-1906/P
摘要
The Rexiang copper deposit is located in the secondary syncline core of Niangyongfu syncline on the hanging wall of Xiangcheng fault and occurs in granodiorite dikes. According to researches on the ore body, ores and content of major and trace elements, the authors preliminarily hold that the Rexiang ore deposit is a hydrothermal copper deposit formed by magmatic intrusion in faults resulting from intracontinental strike-slip. On the basis of a comprehensive analysis, the authors have constructed a geological-geochemical ore-prospecting model for the Rexiang copper deposit.