Clift, Peter D.Hodges, Kip VHeslop, DavidHannigan, RobynVan Long, HoangCalves, Gerome2015-12-081752-0894http://hdl.handle.net/1885/29309Although 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 record200810.1038/ngeo3512015-12-08