Building the Tibetan plateau during the collision between the India and Asia Plates

Anne Replumaz, Cécile Lasserre, Stéphane Guillot, Marie Luce Chevalier, Fabio A. Capitanio, Francesca Funiciello, Fanny Goussin, Shiguang Wang

Research output: Chapter in Book/Report/Conference proceedingChapter (Book)Otherpeer-review

Abstract

The Tibetan Plateau is the highest and widest orogenic plateau on Earth, towering over the world at an average altitude of 4,500 m and over 800 km. While far from being an exhaustive review of the existing data and models, this chapter presents some recent constraints and models that provide an integrated and improved understanding of the enigmatic plateau building. It also presents some analogue and numerical models at the lithospheric/upper mantle scale to better understand the dynamics of subduction, mantle flow and the formation of the plateau as a result. In Tibet, the global positioning system velocity field relative to Eurasia shows a dominant north-eastward motion of the plateau. At depth, seismic profiles are used to constrain the deformation of the lower crust and of the lithospheric mantle beneath Tibet.

Original languageEnglish
Title of host publicationHimalaya, Dynamics of a Giant 1
Subtitle of host publicationGeodynamic Setting of the Himalayan Range
EditorsRodolphe Cattin, Jean-Luc Epard
Place of PublicationLondon UK
PublisherWiley-ISTE
Chapter2
Pages33-55
Number of pages23
Volume1
ISBN (Electronic)9781394228584
ISBN (Print)9781789451290
DOIs
Publication statusPublished - 8 Aug 2023

Publication series

NameGeoscience: Dynamics of the Continental Lithosphere
PublisherWiley-ISTE
Volume1

Keywords

  • Analogue models
  • Eurasia
  • Global positioning system
  • Lithospheric mantle
  • Mantle flow
  • Numerical models
  • Tibetan Plateau

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