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

doi:10.1016/j.chemgeo.2018.08.016

	Yin, Lu 1,2; Li, Jie1,3 ; Tian, Hui1 ; Long, Xiaoping 4
	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 Publication	CHEMICAL GEOLOGY
ISSN	0009-2541
	2018-11-05
Volume	499 Pages:26-42
DOI	10.1016/j.chemgeo.2018.08.016
Language	英语
WOS Research Area	Geochemistry & Geophysics
WOS ID	WOS:000447407300002
Indexed By	SCI
Citation statistics	Cited Times:28[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/36652
Collection	同位素地球化学国家重点实验室
Corresponding Author	Li, Jie
Affiliation	1.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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