GIG OpenIR  > 同位素地球化学国家重点实验室  > 期刊论文
Yin, Lu1,2; Li, Jie1,3; Tian, Hui1; Long, Xiaoping4
Rhenium-osmium and molybdenum isotope systematics of black shales from the Lower Cambrian Niutitang Formation, SW China: Evidence of a well oxygenated ocean at ca. 520 Ma
Source PublicationCHEMICAL GEOLOGY
Corresponding AuthorLi, Jie(jieli@gig.ac.cn)
ISSN0009-2541
2018-11-05
Volume499Pages:26-42
DOI10.1016/j.chemgeo.2018.08.016
Indexed BySCI
Language英语
WOS Research AreaGeochemistry & Geophysics
WOS IDWOS:000447407300002
Funding OrganizationNational Science Foundation of China ; Chinese Academy of Sciences
Citation statistics
Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/36652
Collection同位素地球化学国家重点实验室_期刊论文
Corresponding AuthorLi, Jie
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
4.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
Recommended Citation
GB/T 7714
Yin, Lu,Li, Jie,Tian, Hui,et al. Rhenium-osmium and molybdenum isotope systematics of black shales from the Lower Cambrian Niutitang Formation, SW China: Evidence of a well oxygenated ocean at ca. 520 Ma[J]. CHEMICAL GEOLOGY,2018,499:26-42.
APA Yin, Lu,Li, Jie,Tian, Hui,&Long, Xiaoping.(2018).Rhenium-osmium and molybdenum isotope systematics of black shales from the Lower Cambrian Niutitang Formation, SW China: Evidence of a well oxygenated ocean at ca. 520 Ma.CHEMICAL GEOLOGY,499,26-42.
MLA Yin, Lu,et al."Rhenium-osmium and molybdenum isotope systematics of black shales from the Lower Cambrian Niutitang Formation, SW China: Evidence of a well oxygenated ocean at ca. 520 Ma".CHEMICAL GEOLOGY 499(2018):26-42.
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