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Cenozoic eastward growth of the Tibetan Plateau controlled by tearing of the Indian slab - Nature Geoscience

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Cenozoic eastward growth of the Tibetan Plateau controlled by tearing of the Indian slab - Nature Geoscience

Formation of the Tibetan Plateau is generally ascribed to the Cenozoic India–Asia collision. However, the origin of along-strike deformation of the Indian mantle lithosphere, especially beneath the eastern Tibetan Plateau region, and its effect on the plateau's eastward growth remain unclear. Here, we conduct multiscale seismic tomography to provide a revised structure of the Indian mantle lithosphere beneath the eastern Tibetan Plateau region.

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Cenozoic eastward growth of the Tibetan Plateau controlled by tearing of the Indian slab - Nature Geoscience

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Cenozoic eastward growth of the Tibetan Plateau controlled by tearing of the Indian slab - Nature Geoscience

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