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Injection of Indian crust into Tibetan lower crust: A two‐dimensional finite element model study
We propose a model in which the stronger Indian crust injects into the weaker lower crust of Tibet. If the viscosity of the Tibetan lower crust is below a critical value, the continuous advancing of… Expand
Uplift of Tibetan Plateau
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… Expand
Preferential rifting of continents: A source of displaced terranes
Lithospheric rifting, while prevalent in the continents, rarely occurs in oceanic regions. To explain this preferential rifting of continents, we compare the total strength of different lithospheres… Expand