中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Rhenium-Osmium isotope systematics of an Early Mesoproterozoic SEDEX polymetallic pyrite deposit in the North China Craton: Implications for geological significance and the marine osmium isotopic record

文献类型:期刊论文

作者Gao, Bingyu1,2,3; Zhang, Lianchang1,2,3; Jin, Xindi1,2; Li, Zhiquan1,2,3; Li, Wenjun1,2,3
刊名ORE GEOLOGY REVIEWS
出版日期2020-02-01
卷号117页码:10
关键词Gaobanhe deposit SEDEX Pyrite Re-Os isotopes Marine Os isotopic record
ISSN号0169-1368
DOI10.1016/j.oregeorev.2020.103331
英文摘要The rhenium-osmium (Re-Os) isotopic system preserved in ancient seafloor hydrothermal sulfide deposits can be used to gain insight into the Os composition of ancient seawater. In particular, the age of sedimentary exhalative (SEDEX) deposits can be determined by measuring Re-Os isotopes in syn-depositional pyrite, a common constituent of SEDEX deposits. Here we report on the Gaobanhe sediment-hosted, polymetallic pyrite deposit which is hosted within the Gaoyuzhuang Formation in the central part of the northern margin of the North China Craton (NCC). Re-Os isotopic data from syn-depositional pyrite yield an isochron age of 1505 +/- 55 Ma, constraining the timing of primary mineralization, as well as the minimum age of the host sediments to the Mesoproterozoic. Analyzed pyrite grains indicate an initial Os-187/Os-188 (Os-i) value of 0.181 +/- 0.066, suggesting that the mineralizing fluids were an admixture of seawater and submarine hydrothermal fluids, with the Os being primarily derived from seawater. The Os-i value is slightly higher than that of Paleoproterozoic seawater (similar to 0.13), suggesting that there was a radiogenic riverine flux to the oceans and that atmospheric oxygen must have been sufficiently high at that time to drive this increased, continental radiogenic Os input to the oceans. We propose that the Re-Os isotopic system, as recorded by these SEDEX deposits, may provide key insights when examining changes in the Os isotopic composition of seawater throughout the Precambrian.
WOS关键词RE-OS ; BROOKS RANGE ; BLACK SHALES ; OCEAN ; CONSTRAINTS ; GEOCHRONOLOGY ; BENEATH ; SULFATE ; ROCKS ; BASIN
资助项目National Natural Science General Project[41603016] ; Nation Key R&D Program of China[2016YFC0600106]
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000515206900025
出版者ELSEVIER
资助机构National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; National Natural Science General Project ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China ; Nation Key R&D Program of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/95606]  
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
通讯作者Zhang, Lianchang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Gao, Bingyu,Zhang, Lianchang,Jin, Xindi,et al. Rhenium-Osmium isotope systematics of an Early Mesoproterozoic SEDEX polymetallic pyrite deposit in the North China Craton: Implications for geological significance and the marine osmium isotopic record[J]. ORE GEOLOGY REVIEWS,2020,117:10.
APA Gao, Bingyu,Zhang, Lianchang,Jin, Xindi,Li, Zhiquan,&Li, Wenjun.(2020).Rhenium-Osmium isotope systematics of an Early Mesoproterozoic SEDEX polymetallic pyrite deposit in the North China Craton: Implications for geological significance and the marine osmium isotopic record.ORE GEOLOGY REVIEWS,117,10.
MLA Gao, Bingyu,et al."Rhenium-Osmium isotope systematics of an Early Mesoproterozoic SEDEX polymetallic pyrite deposit in the North China Craton: Implications for geological significance and the marine osmium isotopic record".ORE GEOLOGY REVIEWS 117(2020):10.

入库方式: OAI收割

来源:地质与地球物理研究所

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