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学科主题: 地球科学::地质学
题名: Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau
作者: Liu, XH (Liu XiaoHui)1, 2, 3; Xu, Q (Xu Qiang)1, 2; Ding, L (Ding Lin)1, 2
通讯作者: Liu, XH
关键词: INDIA-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
刊名: SCIENCE CHINA-EARTH SCIENCES
发表日期: 2016
DOI: 10.1007/s11430-015-5486-y
卷: 59, 期:11, 页:2105-2120
收录类别: SCI
合作性质: 国内
文章类型: Article
部门归属: 碰撞与隆升
英文摘要: The 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.
语种: 英语
WOS记录号: WOS:000387396800003
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.itpcas.ac.cn/handle/131C11/7512
Appears in Collections:图书馆_期刊论文

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作者单位: 1.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:
Liu, XH ,Xu, Q ,Ding, L . Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau[J]. SCIENCE CHINA-EARTH SCIENCES,2016,59(11):2105-2120.
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