Characteristics of Ore-Forming Fluid in the Zhenyuan Gold Orefield, Yunnan Province, China
文献类型：期刊论文
| 作者 | Zhao Yan1; Wang Qingfei1; Sun Xiang1; Li Gongjian1 |
| 刊名 | JOURNAL OF EARTH SCIENCE
 |
| 出版日期 | 2013 |
| 卷号 | 24期号:2页码:203-211 |
| 关键词 | DEPOSIT MINERALIZATION MANTLE BELT METALLOGENESIS fluid inclusion (FI) ore-forming fluid Ailaoshan orogenic belt Zhenyuan gold orefield |
| ISSN号 | 1674-487X |
| 其他题名 | Characteristics of Ore-Forming Fluid in the Zhenyuan Gold Orefield, Yunnan Province, China |
| 英文摘要 | The Zhenyuan gold orefield is located in the Ailaoshan gold belt, Sanjiang metallogenic region, China. The fluid inclusions (FIs) in mineralized quartz samples, collected from four deposits, i.e., Laowangzhai, Donggualin, Kudumu, and Daqiaoqing, in the orefield, were studied to reveal ore-forming process. Only aqueous-type and H2O-NaCl-type FIs were observed in the samples. Two generations of FIs are identified due to the spatial occurrences of FIs in host minerals. The early generation is located in the internal zone of quartz crystal, and it has higher homogenization temperatures varying from 180 to 255 degrees C and salinities ranging from 8.7% to 11%; the late generation, often with beating bubbles under room temperature, is developed in the quartz margin, its homogenization temperatures is lower within 95 to 160 degrees C. After elimination of the late generation of FIs, early generation FIs compositions were tested. Gaseous phases in the FIs were H2O and CO2, with low contents of N-2, CH4, and C2H6, and the liquids mainly contains Na+, K+, Ca2+, Mg2+, Cl-, and SO42-. The reappraisal of the previously published hydrogen and oxygen isotope results suggested that the early generation of ore-forming fluid was mainly primary magma hydrothermal, while the late generation fluid contains large amounts of meteoric water. Thus, the result showed that Zhenyuan gold orefield may differ from typical orogenic deposits, which contains abundant CO2-dominated FIs. The two generations FIs developed as quartz grew displaying a continuous evolution of the ore-forming fluids. |
| 资助项目 | [National Key Basic Research Development Program] ; [Century Training Program Foundation for the Talents of Humanities and Social Science by the State Education Commission] ; [Program of Introducing Talents of Discipline to Universities of China] |
| 语种 | 英语 |
| CSCD记录号 | CSCD:4793505 |
| 源URL | [http://ir.imr.ac.cn/handle/321006/144155]  |
| 专题 | 金属研究所_中国科学院金属研究所 |
| 作者单位 | 1.China University Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China 2.中国科学院金属研究所 |
| 推荐引用方式 GB/T 7714 | Zhao Yan,Wang Qingfei,Sun Xiang,et al. Characteristics of Ore-Forming Fluid in the Zhenyuan Gold Orefield, Yunnan Province, China[J]. JOURNAL OF EARTH SCIENCE,2013,24(2):203-211. |
| APA | Zhao Yan,Wang Qingfei,Sun Xiang,&Li Gongjian.(2013).Characteristics of Ore-Forming Fluid in the Zhenyuan Gold Orefield, Yunnan Province, China.JOURNAL OF EARTH SCIENCE,24(2),203-211. |
| MLA | Zhao Yan,et al."Characteristics of Ore-Forming Fluid in the Zhenyuan Gold Orefield, Yunnan Province, China".JOURNAL OF EARTH SCIENCE 24.2(2013):203-211. |
入库方式： OAI收割
来源：金属研究所
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