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1 Introduction The ophiolites that crop out discontinuously for more than 2000 km along the Yarlung-Zangbo suture zone(YZSZ,also called the Indus-Tsangpo suture)in southern Tibet are the remnants of the Neotethyan oceanic lithosphere,which evolved between the Indian and Eurasian continental plates(Gaetani and Garzanti,1991;
1 Introduction The ophiolites that crop out discontinuously for more than 2000 km along the Yarlung-Zangbo suture zone (YZSZ, also called the Indus-Tsangpo suture) in southern Tibet are the remnants of the Neotethyan oceanic lithosphere, which evolved between the Indian and Eurasian continental plates (Gaetani and Garzanti, 1991;