A further twist to the latter is that one such capture event, that of the Yarlung Tsangpo by the Brahmaputra, has potentially resulted in extremely rapid recent exhumation of the Indian plate metamorphic rocks of the Namche Barwa Eastern syntaxis by focused weakening of the crust due to very rapid fluvial incision and erosive thinning of strong upper crust due to the capture event (erosion-tectonic coupling model, Zeitler et al.
et al., 2004, U-Pb zircon constraints on the tectonic evolution of Southeastern Tibet, Namche Barwa Area, American J.
and Zeitler, P.K., 2009, Constraints on the metamorphic evolution of the eastern Himalayan syntaxis from geochronologic and petrologic studies of Namche Barwa, Geological Soc.
et al., 1998, The Namche Barwa syntaxis: evidence for exhumation related to compressional crustal folding, J.
Metamorphic characteristics of HP granulite facies in the Namche Barwa region and its tectonic application.
Geochronology and Precambrian tectonic evolution of the Namche Barwa complex from the eastern Himalayan syntaxis, Tibet.