Cyclical one-way continental rupture-drift in the Tethyan evolution: Subduction-driven plate tectonics

查看全文 作　　者：Bo [1]WAN;Fuyuan [1]WU;Ling [1]CHEN;Liang [1]ZHAO;Xiaofeng [1]LIANG;Wenjiao [1]XIAO;Rixiang [1]ZHU

机构地区：[1]State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences

出　　处：《Science China Earth Sciences》索引2019年第62卷第12期,共12页

基　　金：supported by the National Natural Science Foundation of China (Grant Nos. 91855207, 41888101);the Programs of the Chinese Academy of Sciences (Grant Nos. 2013047, GJHZ1776) 摘　　要：Numerous continents have rifted and drifted away from Gondwana to repeatedly open ocean basins over the past-500 millionyears.These Gondwana-derived continents drifted towards and collided with components of the Eurasian continent to successively close the preexisting oceans between the two.Plate tectonics satisfactorily describes the continental drift from Gondwana to Eurasia but does not define the geodynamic mechanism of continuously rifting to collisions of continents in the Tethy an Realm.After reappraisal of geological records of the rift,collision and subduction initiation from the surface and various geophysical observations from depth,we propose that Eurasia-directed subducting oceanic slabs would have driven Tethyan system in the Phanerozoic.The Eurasia-directed subduction would have dragged the passive Gondwana margin to rift and drift northwards,giving birth to new oceans since the Paleozoic.The closure of preexisting oceans between the Gondwana-derived continents and Eurasia led to continental collisions,which would have induced the initiation of oceanic subduction in the Tethyan Realm.Multiple episodic switches between collision-subduction-rift repeatedly led to the separation of continental fragments from Gondwana and dragged them to drift towards Eurasia.The final disappearance of Neo-Tethy s would have induced collision of the Gondwana-derived continents with the Eurasian continent,giving rise to the Cenozoic Alpine-Zagros-Himalayan collisional system.Therefore,the Eurasia-directed oceanic subduction would have acted as a’one-way train’that successively transferred the ruptured Gondwana continental fragments in the south,into the terminal in the north.In this regard,the engine of this'Tethyan one-way train'is the negative buoyancy of subducting oceanic slabs. 关键词：TETHYAN GEODYNAMICS OCEANIC slab SUBDUCTION initiation CONTINENTAL collision CONTINENTAL RIFT

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Cyclical one-way continental rupture-drift in the Tethyan evolution: Subduction-driven plate tectonics

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