Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia
文献类型：期刊论文
| 作者 | Liu, W; Li, XJ; Tan, J |
| 刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
 |
| 出版日期 | 2003-07-01 |
| 卷号 | 46期号:7页码:652-663 |
| 关键词 | fluid mixing fluid inclusion quadrupole mass spectrometer stable isotope Dajing ore deposit |
| ISSN号 | 1006-9313 |
| 文献子类 | Article |
| 英文摘要 | Dajing Cu-Sn-Ag-Pb-Zn ore deposit, in the Inner Mongolia Autonomous Region of China, is a fissure-filling hydrothermal ore deposit. The deltaD values of quartz-hosted inclusion water are centered at -100parts per thousand - -130parts per thousand. The delta(34)S values of sulfide ore minerals and delta(13)C values of carbonate gangue minerals vary from -0.3parts per thousand to 2.6parts per thousand and from -2.9parts per thousand to -7.0parts per thousand, respectively. Integrated' isotopic data point to two major contributions to the mineralizing fluid that include a dominant meteoric-derived groundwater, and sulfur and carbon species from hypogene magma. Linear trends are exhibited on the gaseous H2O versus CO2 plot, and plots of CO, N-2, CH4, and C2H6. It is shown by quantitative simulation that magma degassing cannot explain the linear trends. Hence, these linear trends are interpreted in terms of mixing Of CO2-rich magmatic fluid with meteoric-derived groundwater. The groundwater circulated in Paleozoic sedimentary rocks and absorbed CO, N-2, CH4, C2H6 and radiogenic Ar from organic matter. Cooling effects resulting from mixing have caused the precipitation of ore minerals. |
| WOS关键词 | ISOTOPE FRACTIONATION ; TUNGSTEN DEPOSITS ; NORTHERN XINJIANG ; STABLE ISOTOPE ; ALKALI GRANITE ; OXYGEN ; INCLUSION ; EXCHANGE ; CARBON ; HYDROGEN |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000183283600002 |
| 出版者 | SCIENCE CHINA PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/78477]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Liu, W |
| 作者单位 | Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100101, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu, W,Li, XJ,Tan, J. Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2003,46(7):652-663. |
| APA | Liu, W,Li, XJ,&Tan, J.(2003).Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,46(7),652-663. |
| MLA | Liu, W,et al."Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 46.7(2003):652-663. |
入库方式： OAI收割
来源：地质与地球物理研究所
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