Geochronology and fluid inclusion study of the Jiguanshan porphyry Mo deposit, Inner Mongolia
文献类型：期刊论文
| 作者 | Chen WeiJun1,2; Liu JianMing1; Liu HongTao1; Sun XingGuo1,2; Zhang RuiBin1,2; Zhang ZuoLun1,2; Qin Feng1,2 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2010-05-01 |
| 卷号 | 26期号:5页码:1423-1436 |
| 关键词 | Porphyry Mo Deposit Re-os Isochron Age Fluid Inclusion Jiguanshan Inner Mongolia Xilamulun Molybdenum Metallogenic Belt |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | The Jiguanshan Mo deposit is a very typical porphyry deposit hosted in the Xilamulun molybdenum metallogenic belt. The deposit occurs within the volcanic-intrusive complex. Re-Os isotope dating from five molybdenite samples gives an isochron age of 151. 1 +/- 1. 3Ma, which indicates the deposit formed in the late Jurassic. The Mo mineralization is characterized by a variety of veinlets and disseminated styles. The hydrothermal ore-forming processes can be divided into three stages; stage I-ore-in poor stage, it is characterized by ivory-white quartz veins and minor disseminated pyrites; stage II-the primary Mo mineralization stage, it can be subdivided into two substages: quartz-polymetallic sulfide and fluorite-quartz-polymetallic sulfide substages; stage III-barren stage, it consists of quartzs and carbonates, and it overprints the minerals of the former two stages. Petrographic observation suggests that six major types of fluid inclusion related to mineralization are present in this deposit: gas-rich, liquid-rich, daughter-mineral bearing polyphase. CO(2)-bearing three-phase, pure CO(2) phase and liquid phase inclusions. Fluid inclusions in stage I are mainly gas-rich ones with small amount of CO(2) phase ones, while stage II are multiform inclusions including gas-rich, liquid-rich and daughter-mineral bearing poly-phase inclusions. However, none but liquid-rich fluid inclusions can be observed in stage III. Microthermometric and laser Raman spectroscopic studies indicate that homogenization temperatures of fluid inclusions in quartz-veins from stage I are above 480 degrees C, with the high salinities of above 66. 75% NaClegv. Liquid components are dominated by H(2)O and vapor bubbles mainly composed of CO(2) and H(2)O. Daughter minerals of the poly-phase fluid inclusions include halite, chalcopyrite and hematite representing an oxidizing condition, which indicates the ore-forming fluid is metal-rich magmatic fluid. The stage II fluid inclusions with the temperature range of 320 similar to 480 degrees C in early phase and 180 similar to 320 degrees C in late phase, respectively, and fluid salinities ranging from 4. 65% to 56. 76% NaClegy, reflect Mo mainly mineralized phases. In the stage II, daughter minerals in fluid inclusions, such as halite, calcite, chalcopyrite and minor hematite, also have been recognized. Vapor bubbles are mainly composed of H(2)O and minor CO(2), while liquids generally contain H(2)O. The daughter mineral-bearing inclusions coexist with the gas-and liquid-rich fluid inclusions, and fluid inclusions with contrasting salinities are homogenized to divergent phases at similar homogenization temperatures. The above evidence strongly reveal that fluid-boiling occurred in the stage II. The homogenization temperatures of stage III fluid inclusions fall into 100 similar to 180 degrees C, with corresponding salinities no more than 10. 86% NaClegv. The stage I fluids which are characterized by high temperature, high salinity; high oxygen-fugacity, CO(2)-rich and ore-bearing elements are magmatic fluids. The boiling of fluid occured in the stage II, leading to CO(2)-release, oxygen-fugacity decrease and rapid precipitation of ore-forming materials. During the stage III, the fluids, with input of meteoric water, gradually evolved to those with characteristic of low temperature, low salinity, lack of daughter mineral and poor in CO(2). The boiling is the major mechanism of the ore-deposition. |
| WOS关键词 | ORE-FORMING FLUID ; RE-OS AGES ; COPPER-DEPOSIT ; HYDROTHERMAL EVOLUTION ; MOLYBDENUM DEPOSIT ; HIGH-TEMPERATURE ; MAGMATIC FLUIDS ; GOLD DEPOSITS ; NORTH CHINA ; MINERALIZATION |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000278597800009 |
| 出版者 | SCIENCE CHINA PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/73241]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Chen WeiJun |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen WeiJun,Liu JianMing,Liu HongTao,et al. Geochronology and fluid inclusion study of the Jiguanshan porphyry Mo deposit, Inner Mongolia[J]. ACTA PETROLOGICA SINICA,2010,26(5):1423-1436. |
| APA | Chen WeiJun.,Liu JianMing.,Liu HongTao.,Sun XingGuo.,Zhang RuiBin.,...&Qin Feng.(2010).Geochronology and fluid inclusion study of the Jiguanshan porphyry Mo deposit, Inner Mongolia.ACTA PETROLOGICA SINICA,26(5),1423-1436. |
| MLA | Chen WeiJun,et al."Geochronology and fluid inclusion study of the Jiguanshan porphyry Mo deposit, Inner Mongolia".ACTA PETROLOGICA SINICA 26.5(2010):1423-1436. |
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。