Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau

doi:10.1016/j.jseaes.2019.103909

GIG OpenIR

	Pang, Jianzhang 1; Yu, Jingxing 1,2; Zheng, Dewen 1,3; Wang, Yizhou 1; Zhang, Huiping 1; Li, Chaopeng 1; Wang, Weitao 4; Hao, Yuqi 1
	Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau
Source Publication	JOURNAL OF ASIAN EARTH SCIENCES
ISSN	1367-9120
	2019-09-01
Volume	181 Pages:10
DOI	10.1016/j.jseaes.2019.103909
Language	英语
WOS Research Area	Geology
WOS ID	WOS:000482496600022
Indexed By	SCI
Citation statistics	Cited Times:24[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/47182
Collection	中国科学院广州地球化学研究所
Corresponding Author	Yu, Jingxing
Affiliation	1.China Earthquake Adm, State Key Lab Earthquake Dynam, Inst Geol, Beijing 100029, Peoples R China 2.Univ Oxford, Dept Earth Sci, Ctr Observat & Modelling Earthquakes Volcanoes &, Oxford OX1 3AN, England 3.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China 4.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangzhou 510275, Guangdong, Peoples R China
Recommended Citation GB/T 7714	Pang, Jianzhang,Yu, Jingxing,Zheng, Dewen,et al. Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,181:10.
APA	Pang, Jianzhang.,Yu, Jingxing.,Zheng, Dewen.,Wang, Yizhou.,Zhang, Huiping.,...&Hao, Yuqi.(2019).Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau.JOURNAL OF ASIAN EARTH SCIENCES,181,10.
MLA	Pang, Jianzhang,et al."Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau".JOURNAL OF ASIAN EARTH SCIENCES 181(2019):10.

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