“…(3) The Yarlung Zangbo suture zone marks the contact between India and Asia, and includes ophiolites and tectonic mélange with serpentinite or shale matrix (Cai et al, 2012;Chan et al, 2015;Xu et al, 2015). (4) The Tethyan Himalayan sedimentary sequence is generally subdivided into southern and northern zones, separated by the Gyirong-Kangmar thrust and representing proximal and distal northern Indian continentalmargin depozones, respectively.…”