Petrological, Geochemical and the Origin of the Cuobuzha Peridotite in the Western Yarlung Zangbo Suture Zone


FENG Guangying;YANG Jingsui;XIONG Fahui;LIU Fei;NIU Xiaolu;LIAN Dongyang;WANG Yunpeng;ZHAO Yijue;


<正>Ophiolites are fragments of ancient oceanic lithosphere emplaced onto continental margins,accretionary prisms,or island arcs during plate collisions(Dilek and Furnes,2011).The well-preserved ophiolitic sequence provides important information on melt extraction,melting,and melt-rock interaction in the upper mantle of paleo-oceanic lithosphere(e.g.Kelemen et al.,1992;Zhou et al.,2005;Arai et al.,2007;Dilek et al.,2007;Dai et al.,2011),and


rock;Petrological;Geochemical and the Origin of the Cuobuzha Peridotite in the Western Yarlung Zangbo Suture Zone;


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Total: 10 articles

  • [1] YANG JingSui1,XIONG FaHui1,GUO GuoLin2,LIU Fei1,LIANG FengHua1,Chen SongYong1,LI ZhaoLi1 and ZHANG LiWen3 1.State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China 2.State Key Laboratory Breeding Base of Nuclear Resources and Environment,East China Institute of Technology,Nanchang 330013,China 3.China University of Geosciences,Beijing 100083,China, The Dongbo ultramafic massif:A mantle peridotite in the western part of the Yarlung Zangbo suture zone,Tibet,with excellent prospects for a major chromite deposit, Acta Petrologica Sinica,
  • [2] J.A. Pearce;;P.T. Robinson, The Troodos ophiolitic complex probably formed in a subduction initiation, slab edge setting, Gondwana Research,
  • [3] Yildirim Dilek;;Harald Furnes;;Minella Shallo, Suprasubduction zone ophiolite formation along the periphery of Mesozoic Gondwana, Gondwana Research,
  • [4] Shoji Arai;;Natsue Abe;;Satoko Ishimaru, Mantle peridotites from the Western Pacific, Gondwana Research,


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