,Discovery of Late Cretaceous-Paleocene faulted basins developed on the Yandang Low Uplift, East Chi

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1.ObjectiveThe East China Sea Shelf Basin (ECSSB) is a typical Meso-Cenozoic superimposed basin which consists several tectonic units including the Changjiang Sag, Oujiang Sag,Hupijiao Uplift, Haijiao Uplift, Yandang Low Uplift (YDLU),Minjiang Sag, Taipei Low Uplift, Xihu Sag, Jilong Sag and so on.It has been successively involved into the tectonic evolution of the Tethyan and Pacific domains since Early Mesozoic and recorded the detailed evidences on the tectonic evolution and transition among different types of continentalmargins in East Asia (Zhang GW et al., 2013).
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