| 江西省兴源冲铜矿床同位素地球化学特征及成矿机制探讨 |
| Received:September 02, 2012 Revised:February 26, 2013 点此下载全文 |
| 引用本文：LIU Ting,LIU ChengDong,YAN ZhaoBin,CHEN YiPing,WU XuLing,FAN XiuJun.2013.Carbon, oxygen and sulfur isotopic geochemistry and metallogenic mechanism of Xingyuanchong copper deposit in Jiangxi Province[J].Mineral Deposits,32(3):614~624 |
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| Author Name | Affiliation | E-mail | | LIU Ting | State Key Laboratory Breeding Base of Nuclear Resources and Environment, Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China Institute of Technology, Nanchang 330013, Jiangxi, China | | | LIU ChengDong | State Key Laboratory Breeding Base of Nuclear Resources and Environment, Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China Institute of Technology, Nanchang 330013, Jiangxi, China | chdliu@ecit.cn | | YAN ZhaoBin | State Key Laboratory Breeding Base of Nuclear Resources and Environment, Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China Institute of Technology, Nanchang 330013, Jiangxi, China | | | CHEN YiPing | State Key Laboratory Breeding Base of Nuclear Resources and Environment, Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China Institute of Technology, Nanchang 330013, Jiangxi, China | | | WU XuLing | Jiangxi Institute of Geological Survey, Nanchang 330030, Jiangxi, China | | | FAN XiuJun | Auhui Technical College of Industry and Economy, Hefei 230051, Anhui, China | |
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| 中文摘要:兴源冲铜矿床地处九岭南缘铜多金属大型矿集区西段的黄茅地区。文章在成矿地质特征的基础上,通过对矿石进行稳定同位素地球化学研究,重点分析了成矿物质来源,探讨了矿床成矿机制。碳、氧同位素分析结果表明,矿区碳酸盐岩δ13CVPDB为-5.4‰~1.9‰,平均为0.6‰,δ18OSMOW变化范围为9.0‰~13.9‰,平均为10.9‰,主要为海相碳酸盐岩,碳、氧同位素图解表明碳可能主要来源于深部,且受高温变质作用和低温蚀变作用明显;矿石硫化物硫同位素δ34S变化范围主要在1.0‰~6.2‰之间,个别样品同位素比值偏大,对比相似矿床,表明该矿床具有海底喷流沉积和后期岩浆热液叠加作用的特征。上述同位素地球化学特征表明,兴源冲铜矿床是在中元古代海底火山沉积基础上,经新元古代晋宁造山期岩浆热液、动力变质叠加成矿作用所形成。 |
| 中文关键词:地球化学 稳定同位素 成矿物质来源 成矿机制 海底火山沉积 兴源冲 |
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| Carbon, oxygen and sulfur isotopic geochemistry and metallogenic mechanism of Xingyuanchong copper deposit in Jiangxi Province |
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| Abstract:The Xingyuanchong copper deposit of Huangmao area is located in the west segment of the South Jiuling large copper polymetallic ore concentration area. In combination with the metallogenic characteristics of the ore deposit, the authors mainly studied stable isotopes of the ores to probe into the sources of metallogenic materials and metallogenic mechanism of the deposit. δ13CVPDB values of carbonates in this area vary in the range of -5.4‰~1.9‰, 0.6‰ on average, whereas δ18OSMOW values range from 9.0‰ to 13.8‰, 10.9‰ on average, indicating that carbonates were mainly marine carbonates. The δ18O-δ13C diagram shows that carbon in the region probably came from the deep earth, and experienced metamorphism at high temperatures and alteration at low temperatures. Except two higher values of δ34S, most δ34S values in this deposit vary in the range of 1.0‰~6.2‰; in comparison with other similar deposits, sulfur of this deposit is characterized by submarine exhalation sedimentation and hydrothermal superimposition. In combination with isotopic data and geological setting, it is proposed that the ore-forming processes of the Xingyuanchong copper deposit could be divided into two stages. At the first stage, submarine volcanic sediments or protore layers were formed in Mesoproterozoic. At the second stage, the pre-existing protores were altered by the hydrothermal fluids and dynamic metamorphism mainly derived from Jinning orogenic period in Late Proterozoic. |
| keywords:geochemistry stable isotope sources of metallogenic materials metallogenic mechanism submarine volcanic sediment Xingyuanchong |
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