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Links Between Lithospheric Structure and Topography SE Tibet

AB: The Himalaya and high Tibetan Plateau, one of the most remarkable topographic features on Earth, are widely taken to be the classic example of continent-continent collision. Across the northeastern margin of the Indian plate in southeastern Tibet, the Himalayan orogen terminates abruptly. Collisional processes responsible for the elevation of Tibet and the tectonics of the main Himalayan range are replaced by the strike-slip tectonics of the eastern Himalayan syntaxis as lithospheric material, enters the clockwise deformation regime of the eastern syntaxis. As part of a larger multidisciplinary study we deployed a broadband temporary seismic array extending east from Lhasa, through the eastern Himalayan syntaxis, to the eastern margin of the Tibetan plateau to examine how changes in lithospheric structure and rheology are linked to changes in topography and lithospheric mechanics. A denser short period array was deployed in the core of the syntaxis around the Gyala Peri – Namche Barwa Massif, the site of high