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>New timing of the Indosinian intracontinental deformation from the Triassic growth strata in the Kuqa Depression,Southern Tianshan,China
New timing of the Indosinian intracontinental deformation from the Triassic growth strata in the Kuqa Depression,Southern Tianshan,China
1.Objectives In the Indosinian duration,series of Gondwana-related plates pieced together and formed the geological sketch of China for the first time,i.e.the Yangtze,Sino Korean,Tarim plates,and other sub-plates that had been isolated for a long time.Subduction and collision among the Tarim,Qaidam,and Qiangtang blocks in Triassic,as well as the closure of the Paleo-Tethys Ocean,reactivated Late Paleozoic suture zones in the Tianshan orogen region(Hendrix MS et al.,1992).
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机译:seasonal and size-dependent variations in the phytoplankton growth and microzooplankton grazing in the southern south China sea under the influence of the East asian monsoon