Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling

doi:10.1002/gj.2531

GIG OpenIR

	Zhang, Daohan 1; Wei, Junhao 1; Fu, Lebing 1; Chen, Huayong2 ; Tan, Jun 1; Li, Yanjun 1; Shi, Wenjie 1; Tian, Ning 1
	Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling
Source Publication	GEOLOGICAL JOURNAL
ISSN	0072-1050
	2015-03-01
Volume	50 Issue:2 Pages:122-138
DOI	10.1002/gj.2531
Language	英语
WOS ID	WOS:000350909700002
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/344008/31662
Collection	中国科学院广州地球化学研究所
Corresponding Author	Zhang, Daohan
Affiliation	1.China Univ Geosci, Fac Earth Resources, Wuhan 430074, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou, Guangdong, Peoples R China
Recommended Citation GB/T 7714	Zhang, Daohan,Wei, Junhao,Fu, Lebing,et al. Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling[J]. GEOLOGICAL JOURNAL,2015,50(2):122-138.
APA	Zhang, Daohan.,Wei, Junhao.,Fu, Lebing.,Chen, Huayong.,Tan, Jun.,...&Tian, Ning.(2015).Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling.GEOLOGICAL JOURNAL,50(2),122-138.
MLA	Zhang, Daohan,et al."Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling".GEOLOGICAL JOURNAL 50.2(2015):122-138.

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