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Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen include where the India–Asia convergence was accommodated and how the plateau grew. To clarify these problems, we review the deformations and their role in the plateau's growth. Our results show that ~1630km of shortening occurred across the Tibetan–Himalayan orogen since ~55Ma, with more than ~1400km accommodated by...
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