line-level: 2" class=MsoNormal>Geochemical Features and Minerogenic Potentiality of Granite Aplite in Zhujiding Copper Deposit in
详细信息
- 责任者：Fei Guangchun (College of Earth Sciences ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Youguo
- 刊名：Xinjiang Geology
- 出版年：2010
- 卷期：28(2)
- 关键词：geochemical exploration ; 铜矿 ; copper ores ; 四川 ; Sichuan Province
- 页码：p.204-208
- 图表：6 illus., 2 tables, 17 refs.
- 分类号：1500
- issnNo：ISSN1000-8845
- isbnNo：CN65-1092/P
摘要
Zhujiding copper deposit locates in the core of Sidaoqiao-Zhujiding anticline and Sandaoqiao-Qingda anticline in hanging walls of Xiangcheng fault, which is a newly founded copper deposit in the middle of the Yidun island arc and the genesis is closely related to the granite aplite. The content of metal metallogenic element is higher than upper crust. Combined with the research of oxygen fugacity, volatile component and wall rock alteration, it is suggested that the Zhujiding granite aplite have greater copper minerogenic potentiality.