Correlation of Himalayan exhumation rates and Asian monsoon intensity
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Clift, Peter D.
Hodges, Kip V
Heslop, David
Hannigan, Robyn
Van Long, Hoang
Calves, Gerome
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Nature Publishing Group
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Although most data suggest that the India-Eurasia continental collision began 45-55 Myr ago, the architecture of the Himalayan-Tibetan orogen is dominated by deformational structures developed in the Neogene period (<23 Myr ago). The stratigraphic record
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Nature Geoscience
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2037-12-31
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