The study of ore-fluid and C-S-Pb isopope of rich in S and poor in S types in epithermal gold deposits Junggar area, Xinjiang
文献类型：期刊论文
| 作者 | Wang, LJ; Wang, JB; Wang, YW; Zhu, HP; Qu, LL |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2005-09-01 |
| 卷号 | 21期号:5页码:1382-1388 |
| 关键词 | Epithermal Gold Deposit Ore-forming Fluids C-s-pb Isotopes Junggar Area Xinjiang |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | Homogeneous temperatures, decrepitation temperatures, as and liquid components Of inclusions, hydrogen and oxygen isotopes, carbon isotope of inclusions of wall-rock and quartz, Sulfur isotope and Lead isotope of pyrite in ore body have been studied on the two typical shallow hydrothermal gold ore deposits in Junggar area of Xinjiang Province, suffur-rich style of Kuoerzhenkuona gold deposit and poor-sulfur style of shiyingtan dold deposit. It shows that ore-forming fluid is characterized in low temperature and low salinites and originates from recurrent meteoric precipitation. Sulfur isotope and Lead isotope of pyrite are all rooted in deep source that indicate plutonic gold Source. And that delta(13)C of CO2 fluid inclusion hosted in quartz is lower than -10 parts per thousand of organic carbon display that the sedimentary strata have involved into the gold-forming procedure. Another, this paper proves that the gold-forming fluids in the sulfur-rich Kuoerzhenkuona Gold Deposit has been mixed by intrusion magmatic hydrothermal fluid. possesses multi-metal ore-forming perspective in its deep part, low-temperature fluid has superposed frequently and, Old mineralization is very strong, which shows that it is medium-scale gold deposit. However, that the ore-forming manner of sulfur-poor Shiyingtan Gold Deposit, without magmatic hydrotherm mixture, is simple, its low-temperature fluid function and Bold mineralization is weak, proves that it is small-scale gold ore deposit. In general, it seems to possesse this rule that the stronger the low-temperature fulid activity, the more Serious the gold mineralization is. |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000233172900008 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/65874]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Wang, LJ |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Beijing Inst Geol Mineral Resources, Beijing 100012, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, LJ,Wang, JB,Wang, YW,et al. The study of ore-fluid and C-S-Pb isopope of rich in S and poor in S types in epithermal gold deposits Junggar area, Xinjiang[J]. ACTA PETROLOGICA SINICA,2005,21(5):1382-1388. |
| APA | Wang, LJ,Wang, JB,Wang, YW,Zhu, HP,&Qu, LL.(2005).The study of ore-fluid and C-S-Pb isopope of rich in S and poor in S types in epithermal gold deposits Junggar area, Xinjiang.ACTA PETROLOGICA SINICA,21(5),1382-1388. |
| MLA | Wang, LJ,et al."The study of ore-fluid and C-S-Pb isopope of rich in S and poor in S types in epithermal gold deposits Junggar area, Xinjiang".ACTA PETROLOGICA SINICA 21.5(2005):1382-1388. |
入库方式： OAI收割
来源：地质与地球物理研究所
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