GIG OpenIR
Liu, Zeyang1,2,3; Selby, David3,4
Deep-water osmium-isotope record of the Permian & ndash;Triassic interval from Niushan, China reveals potential delayed volcanic signal post the mass extinction
Source PublicationGLOBAL AND PLANETARY CHANGE
ISSN0921-8181
2021-05-01
Volume200Pages:8
DOI10.1016/j.gloplacha.2021.103473
Language英语
WOS Research AreaPhysical Geography ; Geology
WOS IDWOS:000640402900003
Indexed BySCI
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Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/62516
Corresponding AuthorLiu, Zeyang
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Peoples R China
2.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
3.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England
4.China Univ Geosci, Sch Earth Resources, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China
Recommended Citation
GB/T 7714
Liu, Zeyang,Selby, David. Deep-water osmium-isotope record of the Permian & ndash;Triassic interval from Niushan, China reveals potential delayed volcanic signal post the mass extinction[J]. GLOBAL AND PLANETARY CHANGE,2021,200:8.
APA Liu, Zeyang,&Selby, David.(2021).Deep-water osmium-isotope record of the Permian & ndash;Triassic interval from Niushan, China reveals potential delayed volcanic signal post the mass extinction.GLOBAL AND PLANETARY CHANGE,200,8.
MLA Liu, Zeyang,et al."Deep-water osmium-isotope record of the Permian & ndash;Triassic interval from Niushan, China reveals potential delayed volcanic signal post the mass extinction".GLOBAL AND PLANETARY CHANGE 200(2021):8.
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