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Uplift of Tibetan Plateau

Zhao, Wu‐Ling, Morgan, W. Jason·1985·Tectonics

Abstract

A history of the elevation and crustal thickness of the Tibetan Plateau since the continental collision at 45 Ma has been computed using a kinematic model based on plate tectonic reconstructions and conservation of crustal volume. In our reconstructions, the Indochina block was attached to the southern margin of Eurasia before being “extruded” to the southeast as evidenced by the opening of the South China Sea. This opening affected the mass input into Tibet so that Tibet did not uplift to an elevation higher than 1 km until early Miocene (when spreading of the South China Sea ceased). The model then gives a steady rise of Tibet from Middle Miocene to its present elevation.

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Metadata

Authors
Zhao, W., & Morgan, W. J.
Venue
Tectonics
Published
1985-06
Volume
4
Issue
4
Pages
359-369
ISSN
  • 0278-7407 (ISSN-L)
  • 1944-9194
OpenAlex
W1997020239
Cited by
183
References
0
FWCI
10.52
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Uplift of Tibetan Plateau. https://app.cochat.ai/papers/10.1029/tc004i004p00359
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Zhao, W., & Morgan, W. J. (1985). Uplift of Tibetan Plateau. Tectonics. https://doi.org/10.1029/tc004i004p00359

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.