Nd-Hf Isotopic Decoupling of the Silurian-Devonian Granitoids in the Chinese Altai: A Consequence of Crustal Recycling of the Ordovician Accretionary Wedge?

doi:10.1007/s12583-019-1217-x

	Huang, Yanqiong 1,2; Jiang, Yingde1 ; Yu, Yang 1; Collett, Stephen 3; Wang, Sheng 1,2; Shu, Tan 1,2; Xu, Kang 1,2
	Nd-Hf Isotopic Decoupling of the Silurian-Devonian Granitoids in the Chinese Altai: A Consequence of Crustal Recycling of the Ordovician Accretionary Wedge?
Source Publication	JOURNAL OF EARTH SCIENCE
ISSN	1674-487X
	2020-02-01
Volume	31 Issue:1 Pages:102-114
DOI	10.1007/s12583-019-1217-x
Language	英语
WOS Research Area	Geology
WOS ID	WOS:000511477000009
Indexed By	SCI
Citation statistics	Cited Times:10[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/48747
Collection	同位素地球化学国家重点实验室
Affiliation	1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Czech Geol Survey, Ctr Lithospher Res, Prague, Czech Republic
Recommended Citation GB/T 7714	Huang, Yanqiong,Jiang, Yingde,Yu, Yang,et al. Nd-Hf Isotopic Decoupling of the Silurian-Devonian Granitoids in the Chinese Altai: A Consequence of Crustal Recycling of the Ordovician Accretionary Wedge?[J]. JOURNAL OF EARTH SCIENCE,2020,31(1):102-114.
APA	Huang, Yanqiong.,Jiang, Yingde.,Yu, Yang.,Collett, Stephen.,Wang, Sheng.,...&Xu, Kang.(2020).Nd-Hf Isotopic Decoupling of the Silurian-Devonian Granitoids in the Chinese Altai: A Consequence of Crustal Recycling of the Ordovician Accretionary Wedge?.JOURNAL OF EARTH SCIENCE,31(1),102-114.
MLA	Huang, Yanqiong,et al."Nd-Hf Isotopic Decoupling of the Silurian-Devonian Granitoids in the Chinese Altai: A Consequence of Crustal Recycling of the Ordovician Accretionary Wedge?".JOURNAL OF EARTH SCIENCE 31.1(2020):102-114.

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