Abstract
The Tibetan Plateau serves as a model for understanding the possible influence of middle and lower crustal flow on the geomorphic and tectonic evolution of a continental plateau. Arguments are presented in favor of a weak middle (and, in some areas, lower) crust beneath the plateau, and the development of tectonic models of the Himalayan-Tibetan orogenic system that incorporate lateral flow of this weak crust under the influence of gravity are explored. Many long- and short-wavelength features of Tibetan and Himalayan landscapes are reasonably explained as a consequence of such flow.
Original language | English (US) |
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Title of host publication | Tectonic Geomorphology |
Publisher | Elsevier Inc. |
Pages | 350-369 |
Number of pages | 20 |
Volume | 5 |
ISBN (Print) | 9780080885223 |
DOIs | |
State | Published - Mar 2013 |
Keywords
- Channel flow
- Climate
- Continental plateaus
- Crustal flow
- Crustal rheology
- Himalaya
- Karakoram
- Orographic precipitation
- Tectonics
- Tibet
- Tibetan plateau
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences