Petrogenesis of the Late Triassic diorites in the Hoh Xil area, northern Tibet: Insights into the origin of the high-Mg# andesitic signature of continental crust

doi:10.1016/j.lithos.2017.12.007

	Wang, Jun 1,2; Gou, Guo-Ning 1; Wang, Qiang1,2,3 ; Zhang, Chunfu 4; Dan, Wei1,3 ; Wyman, Derek A.5; Zhang, Xiu-Zheng 1
	Petrogenesis of the Late Triassic diorites in the Hoh Xil area, northern Tibet: Insights into the origin of the high-Mg# andesitic signature of continental crust
Source Publication	LITHOS
ISSN	0024-4937
	2018-02-01
Volume	300 Pages:348-360
DOI	10.1016/j.lithos.2017.12.007
Language	英语
WOS Research Area	Geochemistry & Geophysics ; Mineralogy
WOS ID	WOS:000425577000021
Indexed By	SCI
Citation statistics	Cited Times:11[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/36732
Collection	同位素地球化学国家重点实验室
Corresponding Author	Wang, Qiang; Dan, Wei
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.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 4.Ft Hays State Univ, Dept Geosci, Hays, KS 67601 USA 5.Univ Sydney, Sch Geosci, Sydney, NSW 2006, Australia
Recommended Citation GB/T 7714	Wang, Jun,Gou, Guo-Ning,Wang, Qiang,et al. Petrogenesis of the Late Triassic diorites in the Hoh Xil area, northern Tibet: Insights into the origin of the high-Mg# andesitic signature of continental crust[J]. LITHOS,2018,300:348-360.
APA	Wang, Jun.,Gou, Guo-Ning.,Wang, Qiang.,Zhang, Chunfu.,Dan, Wei.,...&Zhang, Xiu-Zheng.(2018).Petrogenesis of the Late Triassic diorites in the Hoh Xil area, northern Tibet: Insights into the origin of the high-Mg# andesitic signature of continental crust.LITHOS,300,348-360.
MLA	Wang, Jun,et al."Petrogenesis of the Late Triassic diorites in the Hoh Xil area, northern Tibet: Insights into the origin of the high-Mg# andesitic signature of continental crust".LITHOS 300(2018):348-360.

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