Plateau Uplift, Regional Warping, and Subsidence

J. Babault; J. Van Den Driessche

doi:10.1016/B978-0-12-374739-6.00087-7

Plateau Uplift, Regional Warping, and Subsidence

J. Babault, J. Van Den Driessche

Department of Geology

Research output: Chapter in Book › Chapter › Research › peer-review

6 Citations (Scopus)

Abstract

The authors present the physiognomic and deep characteristics of the seven largest plateaus on Earth. In the second part, the evidence used by the Earth science's community to infer rock and/or surface uplifts of plateaus are reviewed. Finally, the authors briefly present the debate between the feedbacks between plateaus uplift and global climate change. Some of the results contained in this chapter are still under debate and ongoing research is still needed to confirm them because different studies invoke for a same object contradictory processes, in that they result in conflicting uplift history. © 2013 Elsevier Inc. All rights reserved.

Original language	English
Title of host publication	Treatise on Geomorphology
Pages	93-128
Number of pages	35
Volume	5
DOIs	https://doi.org/10.1016/B978-0-12-374739-6.00087-7
Publication status	Published - 1 Mar 2013

Keywords

Afar plateau
Altiplano
Andes
Climate
Colorado plateau
East African plateau
Eastern Anatolian plateau
Erosion
Erosional surface
Ethiopian plateau
Low-relief erosional landscapes
Paleoaltimetry
Paleoelevation
Plateau
Relict landscape
Rock uplift
Southern African plateau
Surface uplift
Tibet

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title = "Plateau Uplift, Regional Warping, and Subsidence",

abstract = "The authors present the physiognomic and deep characteristics of the seven largest plateaus on Earth. In the second part, the evidence used by the Earth science's community to infer rock and/or surface uplifts of plateaus are reviewed. Finally, the authors briefly present the debate between the feedbacks between plateaus uplift and global climate change. Some of the results contained in this chapter are still under debate and ongoing research is still needed to confirm them because different studies invoke for a same object contradictory processes, in that they result in conflicting uplift history. {\textcopyright} 2013 Elsevier Inc. All rights reserved.",

keywords = "Afar plateau, Altiplano, Andes, Climate, Colorado plateau, East African plateau, Eastern Anatolian plateau, Erosion, Erosional surface, Ethiopian plateau, Low-relief erosional landscapes, Paleoaltimetry, Paleoelevation, Plateau, Relict landscape, Rock uplift, Southern African plateau, Surface uplift, Tibet",

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AB - The authors present the physiognomic and deep characteristics of the seven largest plateaus on Earth. In the second part, the evidence used by the Earth science's community to infer rock and/or surface uplifts of plateaus are reviewed. Finally, the authors briefly present the debate between the feedbacks between plateaus uplift and global climate change. Some of the results contained in this chapter are still under debate and ongoing research is still needed to confirm them because different studies invoke for a same object contradictory processes, in that they result in conflicting uplift history. © 2013 Elsevier Inc. All rights reserved.

KW - Afar plateau

KW - Altiplano

KW - Andes

KW - Climate

KW - Colorado plateau

KW - East African plateau

KW - Eastern Anatolian plateau

KW - Erosion

KW - Erosional surface

KW - Ethiopian plateau

KW - Low-relief erosional landscapes

KW - Paleoaltimetry

KW - Paleoelevation

KW - Plateau

KW - Relict landscape

KW - Rock uplift

KW - Southern African plateau

KW - Surface uplift

KW - Tibet

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BT - Treatise on Geomorphology

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