Lower crustal foundering drove the uplift of southern Tibet during the Paleocene
Abstract The growth of the Tibetan Plateau is traditionally attributed to the India-Asia collision and subsequent convergence. However, recent paleo-elevation reconstructions suggest that Gangdese arc in southern Tibetan Plateau reached >4.0 km before or alongside the collision. Here we reconstru...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-05-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-025-02269-2 |
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