气候变化领域集成服务门户(CCPortal): Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau

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DOI	10.1007/s11430-015-5486-y
	Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau
	Liu XiaoHui; Xu Qiang; Ding Lin
通讯作者	Liu, XH (通讯作者)
发表日期	2016
ISSN	1674-7313
EISSN	1869-1897
起始页码	2105
结束页码	2120
卷号	59 期号:11
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.
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
英文关键词	Paleoelevation; Differential surface uplift; Cenozoic; Tibetan Plateau
语种	英语
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000387396800003
来源期刊	SCIENCE CHINA-EARTH SCIENCES
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/258653
推荐引用方式 GB/T 7714	Liu XiaoHui,Xu Qiang,Ding Lin. Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau[J]. 中国科学院青藏高原研究所,2016,59(11).
APA	Liu XiaoHui,Xu Qiang,&Ding Lin.(2016).Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau.SCIENCE CHINA-EARTH SCIENCES,59(11).
MLA	Liu XiaoHui,et al."Differential surface uplift: Cenozoic paleoelevation history of the Tibetan Plateau".SCIENCE CHINA-EARTH SCIENCES 59.11(2016).