中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Fluid processes of a heavy metallogenesis at Jinding, Lanping, SW-China

文献类型:期刊论文

作者Xue, CJ; Zeng, R; Gao, YB; Zhu, HP; Zhao, SH; Li, YQ
刊名ACTA PETROLOGICA SINICA
出版日期2006-04-01
卷号22期号:4页码:1031-1039
关键词various mineralization stage fluid inclusions rare elements fluid processes Jinding giant deposit
ISSN号1000-0569
文献子类Article
英文摘要The Jinding ore deposit is the Youngest and the only giant deposit hosted in continental sedimentary rocks in the world, and followed with interests. The Jinding fluid mineralization experienced three stages, they are quartz-sphalerite-galena, sphalerite-galena-celestite and galena-calcite-celestite-gypsum, according to the intergrowth of minerals in the Jinding ores. Pyrite occurs in each stage, and various generations of minerals can be distinguished by their occurrence, texture and assemblage relations. Rare element compositions in fluid inclusions are an important indicator of the large-scale fluid metallogenic processes because the REE patterns and rare element distributions of the fluid inclusions in minerals of various mineralization stages do not evidently change in different hosted minerals. From the first to the third mineralization stage of the fluid mineralization processes, Sigma REE (1.34 x 10(-9) similar to 6.28 x 10(-9) similar to 297.03 x 10(-9)) and LREE/HREE increased in the ore-forming fluid respectively, and the fluid system became more oxidizing, the rare element assemblage of the ore-forming fluid became more complex, the metallogenic element (zinc changing from 13.594 x 10(-9) to 29331. 810 x 10-9) was richer and richer (zinc being 0.16 x 10(-3) similar to 0.20 x 10(-3) times, 0.041 similar to 0.193 times and 0.028 similar to 0.341 times of China continental crust) in the ore-forming fluid. The fluid mineralization may be quick during the early-middle stage and slower during the middle-late stage. A mixing of a deep- and a shallow-fluid may be the essentials for the large-scale mineralization in the Jinding.
WOS关键词DEPOSITS ; YUNNAN ; HELIUM ; QUARTZ ; XENON
WOS研究方向Geology
语种英语
WOS记录号WOS:000238367700027
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/66642]  
专题中国科学院地质与地球物理研究所
通讯作者Xue, CJ
作者单位1.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
2.Changan Univ, Fac Earth Sci & Land Resources, Xian 710054, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
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Xue, CJ,Zeng, R,Gao, YB,et al. Fluid processes of a heavy metallogenesis at Jinding, Lanping, SW-China[J]. ACTA PETROLOGICA SINICA,2006,22(4):1031-1039.
APA Xue, CJ,Zeng, R,Gao, YB,Zhu, HP,Zhao, SH,&Li, YQ.(2006).Fluid processes of a heavy metallogenesis at Jinding, Lanping, SW-China.ACTA PETROLOGICA SINICA,22(4),1031-1039.
MLA Xue, CJ,et al."Fluid processes of a heavy metallogenesis at Jinding, Lanping, SW-China".ACTA PETROLOGICA SINICA 22.4(2006):1031-1039.

入库方式: OAI收割

来源:地质与地球物理研究所

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