Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet

GIG OpenIR > 中科院广州地化所(-2008)

	Xu YG; Lan JB; Yang QJ; Huang XL; Qiu HN
	Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet
Source Publication	Chemical Geology
ISSN	0009-2541
	2008
Volume	255 Issue:3-4 Pages:439-453
Language	英语
WOS ID	WOS:000260919600012
Indexed By	sci
Citation statistics	Cited Times:144[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/14161
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Xu YG,Lan JB,Yang QJ,et al. Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet[J]. Chemical Geology,2008,255(3-4):439-453.
APA	Xu YG,Lan JB,Yang QJ,Huang XL,&Qiu HN.(2008).Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet.Chemical Geology,255(3-4),439-453.
MLA	Xu YG,et al."Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet".Chemical Geology 255.3-4(2008):439-453.

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