【摘 要】
：
The ＞2000-km-long Indus-Tsangpo suture zone(ITSZ)in southern Tibet marks the boundary between the India and Eurasia plates and contains the remnants of the Neotethyan oceanic lithosphere,ophiolitic mé
【机 构】
：
State Key Laboratory of Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of G
【出 处】
：
International Workshop on: Ophiolites, Mantle Processes and
论文部分内容阅读
The ＞2000-km-long Indus-Tsangpo suture zone(ITSZ)in southern Tibet marks the boundary between the India and Eurasia plates and contains the remnants of the Neotethyan oceanic lithosphere,ophiolitic mélanges,flysch units and continental rocks.Field-based structural analyses and drill core observations from the Luobusa Scientific Drilling Project indicate a complex crustal architecture of superposed deformation fabrics resulted from the ophiolite emplacement and the subsequent continental collision.The late Jurassic-early Cretaceous suprasubduction zone ophiolites were emplaced onto the northern margin of the proto-Indian plate along S-directed thrust faults in the late Cretaceous.
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