Geological characteristics and mineralization fluid of Hongyuan Mo deposit in the West Junggar, Xinjiang
文献类型：期刊论文
| 作者 | Yan YuHong1; Wang JunNian2; Shen Ping1; Pan HongDi3; Zhong ShiHua1; Li Jing4 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2015-02-01 |
| 卷号 | 31期号:2页码:491-504 |
| 关键词 | Fluid Inclusion Stable Isotope Electronic Probe Hongyuan Mo Deposit West Junggar Xinjiang |
| 文献子类 | Article |
| 英文摘要 | The Hongyuan Mo deposit is a newly discovered porphyry-type deposit in the West Junggar region, Xinjiang, which occurs fine vein and disseminated mineralization. Main ore mineral is molybdenite, followed by chalcopyrite and pyrite. It develops hydrothermal alteration. Based on fluid inclusion studies, we find it different from typical porphyry Mo deposit, with the existence of CH, in ore-forming fluid, belonging to NaCl-H2O-CO2-CH4 fluid system. Geochemical data of biotite shows a slightly high oxygen fugacity in the granite crystallization stage. The C isotope data of CH, in ore-forming fluid is ranging from -31. 08 parts per thousand to - 26.44 parts per thousand, indicating the source of crustal organic carbon. Stage I, the early stage of mineralization, the homogenization temperature mainly is 340 similar to 360 degrees C, with high temperature-high salinity and low salinity fluids, weakly reduced fluid, Mo, Cu and other metal minerals are enriched in fluid, with little Mo, Cu mineralization, developing muscovite alteration at high temperature. Stage If, the main stage of mineralization, the homogenization temperature mainly is 280 similar to 300 degrees C, low salinity, the combined action of boiling, atmospheric water and reducing environment causes a large amount of precipitation of Mo, Cu and other metal minerals, forming the main ore body, with sericitization alteration. Stage III, the late-mineralization stage, the homogenization temperature mainly is 160 similar to 180 degrees C, fluid changes to low temperature and low salinity, with weakened mineralization and carbonatization alteration of wall rock. |
| WOS关键词 | NW CHINA ; MOLYBDENUM DEPOSITS ; PORPHYRY ; EVOLUTION ; SYSTEM |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000350616100015 |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62550]  |
| 专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Xinjiang Bur Geol & Mineral Resources, Geol Party 7, Wusu 833300, Peoples R China 3.Changan Univ, Sch Earth Sci & Resources, Xian 710054, Peoples R China 4.Hebei United Univ, Tangshan 063009, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yan YuHong,Wang JunNian,Shen Ping,et al. Geological characteristics and mineralization fluid of Hongyuan Mo deposit in the West Junggar, Xinjiang[J]. ACTA PETROLOGICA SINICA,2015,31(2):491-504. |
| APA | Yan YuHong,Wang JunNian,Shen Ping,Pan HongDi,Zhong ShiHua,&Li Jing.(2015).Geological characteristics and mineralization fluid of Hongyuan Mo deposit in the West Junggar, Xinjiang.ACTA PETROLOGICA SINICA,31(2),491-504. |
| MLA | Yan YuHong,et al."Geological characteristics and mineralization fluid of Hongyuan Mo deposit in the West Junggar, Xinjiang".ACTA PETROLOGICA SINICA 31.2(2015):491-504. |
入库方式： OAI收割
来源：地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。