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Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau
Liu, XH (Liu XiaoHui)1,2,3; Xu, Q (Xu Qiang)1,2; Ding, L (Ding Lin)1,2; Liu, XH
Source PublicationSCIENCE CHINA-EARTH SCIENCES
2016
Volume59Issue:11Pages:2105-2120
DOI10.1007/s11430-015-5486-y
AbstractThe surface uplift history of the Tibetan Plateau has provided a key boundary criterion for various geological, climatic, and environmental events since the Cenozoic. The paleoelevation history of the plateau is organically associated with interactions amongst deep geodynamics, earth surface processes, and climate change. Understanding of plateau uplift history has been advanced by the development of a number of paleoaltimetries and their application to studies of the Tibetan Plateau: the paleogeomorphic scenario for the Early Eocene Tibetan Plateau is thought to include two high mountains, the ca. 4500 m Gangdese Mountains to the south, and the ca. 5000 m Qiangtang Center Watershed Mountains to the north. Between these ranges, a low-elevation basin (ca. 2500 m) is thought to have been present. The Himalayas in the southern Tibetan Plateau was close to sea level at this time, while the Hoh Xil Basin in the north reached an elevation of no more than 1500 m. Thus, the so-called "Roof of the World" Tibetan Plateau formed subsequent to the Miocene. Nevertheless,, the uplift histories of the different terranes that comprise this plateau currently remain unclear, which constrains the uplift history reconstruction of the entire Tibetan Plateau. Additional paleoelevation data from different areas, obtained using multi-paleoaltimeters, is required to resolve the forms and processes of Tibetan Plateau uplift and extension.
Subject Area地质学
WOS IDWOS:000387396800003
Language英语
Indexed BySCI
KeywordIndia-asia Collision Hoh Xil Basin Isotope-based Paleoaltimetry Fore-arc Basin Zircon U-pb East-west Extension Southern Tibet Late Miocene Tectonic Evolution Northern Tibet
Cooperation Status国内
Department碰撞与隆升
Citation statistics
Cited Times:7[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7512
Collection图书馆
Corresponding AuthorLiu, XH
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
Recommended Citation
GB/T 7714
Liu, XH ,Xu, Q ,Ding, L ,et al. Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau[J]. SCIENCE CHINA-EARTH SCIENCES,2016,59(11):2105-2120.
APA Liu, XH ,Xu, Q ,Ding, L ,&Liu, XH.(2016).Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau.SCIENCE CHINA-EARTH SCIENCES,59(11),2105-2120.
MLA Liu, XH ,et al."Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau".SCIENCE CHINA-EARTH SCIENCES 59.11(2016):2105-2120.
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