Closure of Tethys ocean, collision of India and Asia, and subsequent evolution of the Himalaya was a multistage process involving the accretion of more than one terrane. It has been proposed that the Paleogene Liuqu Conglomerates, which crop out discontinuously for many kms along strike along the Yarlung-Tsangpo suture zone between the Indian and Asian plates record the history of collision between India and an intra-oceanic arc.
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