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DOI10.1126/sciadv.adh3058
Upward and outward growth of north-central Tibet: Mechanisms that build high-elevation, low-relief plateaus
Li, Lin; Garzione, Carmala N.
发表日期2023
ISSN2375-2548
卷号9期号:27
英文摘要Large orogenic plateaus, such as the Tibetan Plateau, are characterized by high-elevation, low-relief topography, in contrast to the rugged terrains of narrower mountain belts. A key question is how low-elevation hinterland basins, characteristic of broad regions of shortening, were raised while regional relief was flattened. This study uses the Hoh Xil Basin in north-central Tibet as an analogue for late-stage orogenic plateau formation. The precipitation temperatures of lacustrine carbonates deposited between similar to 19 and similar to 12 million years ago record an early to middle Miocene phase of surface uplift of 1.0 +/- 0.7 km. The results of this study demonstrate the contribution of sub-surface geodynamic processes in driving regional surface uplift and redistribution of crustal material to flatten plateau surfaces during the late stage of orogenic plateau formation.
英文关键词HOH XIL BASIN; FENGHUOSHAN GROUP; LACUSTRINE CARBONATES; TECTONIC EVOLUTION; ASIAN MONSOONS; KUNLUN FAULT; LATE-EOCENE; UPLIFT; ISOTOPE; RECORD
WOS研究方向Multidisciplinary Sciences
WOS记录号WOS:001030983100019
来源期刊SCIENCE ADVANCES
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/283096
作者单位University of Arizona; University of Rochester
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GB/T 7714
Li, Lin,Garzione, Carmala N.. Upward and outward growth of north-central Tibet: Mechanisms that build high-elevation, low-relief plateaus[J],2023,9(27).
APA Li, Lin,&Garzione, Carmala N..(2023).Upward and outward growth of north-central Tibet: Mechanisms that build high-elevation, low-relief plateaus.SCIENCE ADVANCES,9(27).
MLA Li, Lin,et al."Upward and outward growth of north-central Tibet: Mechanisms that build high-elevation, low-relief plateaus".SCIENCE ADVANCES 9.27(2023).
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