Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?

doi:10.1029/2020TC006423

	Zeng, Yun-Chuan 1,2; Xu, Ji-Feng 1,2; Chen, Jian-Lin 3,4; Wang, Bao-Di 4,5,6,7; Huang, Feng 1,2; Xia, Xiao-Ping 3,4; Li, Ming-Jian 1,2
	Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?
Source Publication	TECTONICS
ISSN	0278-7407
	2021-03-01
Volume	40 Issue:3 Pages:22
DOI	10.1029/2020TC006423
Language	英语
WOS Research Area	Geochemistry & Geophysics
WOS ID	WOS:000636359100003
Indexed By	SCI
Citation statistics	Cited Times:21[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/64078
Collection	同位素地球化学国家重点实验室
Corresponding Author	Xu, Ji-Feng
Affiliation	1.China Univ Geosci, Sch Earth Sci & Resources, Beijing, Peoples R China 2.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Peoples R China 4.CAS Ctr Liicellence Deep Earth Sci, Guangzhou, Peoples R China 5.China Geol Survey, Beijing, Peoples R China 6.China Geol Survey, Remote Sensing Ctr Nat Resources, Beijing, Peoples R China 7.China Geol Survey, Chengdu Ctr, Chengdu, Peoples R China
Recommended Citation GB/T 7714	Zeng, Yun-Chuan,Xu, Ji-Feng,Chen, Jian-Lin,et al. Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?[J]. TECTONICS,2021,40(3):22.
APA	Zeng, Yun-Chuan.,Xu, Ji-Feng.,Chen, Jian-Lin.,Wang, Bao-Di.,Huang, Feng.,...&Li, Ming-Jian.(2021).Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?.TECTONICS,40(3),22.
MLA	Zeng, Yun-Chuan,et al."Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?".TECTONICS 40.3(2021):22.

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