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GEOLOGICALGEOCHEMICAL PROSPECTING MODEL
FOR THE REXIANG COPPER DEPOSIT IN WESTERN SICHUAN |
| FEI Guangchun1 ,LI Youguo1 ,WEN Chunqi 1,CHEN Xu 2,DUAN Qiong 3 |
| 1. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China; 2. College of Environment and Civil Engineering, Chengdu University of Technology, Chengdu 610059, China; 3. Wangpu Middle School in Beibei District, Chongqing 400717, China |
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Abstract 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 strikeslip. On the basis of a comprehensive analysis, the authors have constructed a geologicalgeochemical oreprospecting model for the Rexiang copper deposit.
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Published: 10 February 2010
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