Geology and ore-forming fluids of Xilekuduke porphyry Cu-Mo deposit in nothern Junggar.
文献类型：期刊论文
| 作者 | Wang LiJuan1,2; Wang JingBin1,2; Wang YuWang1,2; Long LingLi1,2; Wang ShuLai2; Pu KeXin2 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2009-04-01 |
| 卷号 | 25期号:4页码:944-954 |
| 关键词 | Porphyry Xilekuduke Cu-Mo deposit Fluid inclusion Fluid mixing Nothern Junggar |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | The Cu-Mo mineralization of Xilekuduke porphyry Cu-Mo deposits in northern Junggar is related with veins of andesite porphyrite and dacite porphyrite. The alterations include K-feldspar alteration, sericitization, epidotization, the chlorite is developed outward and skarnization is developed in the deep. Mo mineralizations dominate in the shallow and Cu-Mo mineralizations in the deep. Quartz veins from Xilekuduke porphyry Cu-Mo deposit contain fewer fluid inclusions in quantity and smaller in size, also fewer gas inclusions and more CO, gas inclusions and daughter mineral inclusions than the typical porphyry Cu-Mo deposits. Further more, the daughter minerals in Xilekuduke porphyry Cu-Mo deposits mainly are NaCl but not KCl. There occur more boiling CO(2)-rich fluids in the molybdenum-rich region, but more inclusions bearing big daughter minerals without any boiling inclusions in the chalcopyrite-concentrated region. The mineralization of molybdenum chiefly related with the boiling of CO(2)-rich fluids, porphyry alteration and skarn alteration. Molybdenum mainly originates from the crust, and copper is mainly related with the high-salinity magmatic fluid that directly exsoluted from the melting of basic magma and skarn alteration, it chiefly originates from the upper mantle. The mineralization temperature ranges of molybdenum is from 280 to 530 degrees C, mostly between 300 similar to 400 degrees C. The late mineralization temperature is between 180 similar to 300 degrees C, and that of copper mineralization is below 350 degrees C. The characteristics of the ore-forming fluid reflect the features of the fluid mixing between the crust source and the mantle source and the mixing of magmatic hydrothermal fluids and the meteoric water. |
| WOS关键词 | FREEZING-POINT DEPRESSION ; MINERALIZATION ; XINJIANG ; AU |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000265945600018 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/70502]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Wang LiJuan |
| 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 LiJuan,Wang JingBin,Wang YuWang,et al. Geology and ore-forming fluids of Xilekuduke porphyry Cu-Mo deposit in nothern Junggar.[J]. ACTA PETROLOGICA SINICA,2009,25(4):944-954. |
| APA | Wang LiJuan,Wang JingBin,Wang YuWang,Long LingLi,Wang ShuLai,&Pu KeXin.(2009).Geology and ore-forming fluids of Xilekuduke porphyry Cu-Mo deposit in nothern Junggar..ACTA PETROLOGICA SINICA,25(4),944-954. |
| MLA | Wang LiJuan,et al."Geology and ore-forming fluids of Xilekuduke porphyry Cu-Mo deposit in nothern Junggar.".ACTA PETROLOGICA SINICA 25.4(2009):944-954. |
入库方式： OAI收割
来源：地质与地球物理研究所
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