caa a22 4500 445364831 CHVBK 20180317142926.0 cr unu---uuuuu 170323e20110901xx s 000 0 eng 10.1007/s11001-011-9114-4 doi (NATIONALLICENCE)springer-10.1007/s11001-011-9114-4 Structural evolution of the northern East China Sea Shelf Basin interpreted from cross-section restoration [Elektronische Daten] [Deniz Cukur, Senay Horozal, Gwang Lee, Dae Kim, Hyun Han, Moo Kang] The northern East China Sea Shelf Basin consists of three depressions (the Domi, Jeju, and Socotra Depressions), separated by basement highs or rises. Reconstruction of depth-converted seismic reflection profiles from these depressions reveals that the northern East China Sea Shelf Basin experienced two phases of rifting, followed by regional subsidence. Initial rifting in the Late Cretaceous was driven by the NW-SE crustal stretching of the Eurasian plate, caused by the subduction of the Pacific plate beneath the plate margin. Major extension (~15km) took place during the early phase of basin formation. The initial rifting was terminated by regional uplift in the Late Eocene-Early Oligocene, which was probably due to reorganization of plate boundaries. Rifting resumed in the Early Oligocene; the magnitude of extension was mild (<1km) during this period. A second phase of uplift in the Early Miocene terminated the rifting, marking the transition to the postrift phase of regional subsidence. Up to 2,600m of sediments and basement rock were removed by erosion during and after the second phase of uplift. An inversion in the Late Miocene interrupted the postrift subsidence, resulting in an extensive thrust-fold belt in the eastern part of the area. Subsequent erosion removed about 900m of sediments. The regional subsidence has dominated the area since the Late Miocene. Springer Science+Business Media B.V., 2011 East China Sea Shelf Basin nationallicence Reconstruction nationallicence Rifting nationallicence Extension nationallicence Cukur Deniz Leibniz Institute for Marine Sciences, Wischhofstrasse 1-3, 24148, Kiel, Germany aut Horozal Senay Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut Lee Gwang Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut Kim Dae Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut Han Hyun Korea Institute of Geoscience and Mineral Resources, 305-350, Daejon, South Korea aut Kang Moo Korea Institute of Geoscience and Mineral Resources, 305-350, Daejon, South Korea aut Marine Geophysical Research Springer Netherlands 32/3(2011-09-01), 363-381 0025-3235 32:3<363 2011 32 11001 https://doi.org/10.1007/s11001-011-9114-4 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/s11001-011-9114-4 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Cukur Deniz Leibniz Institute for Marine Sciences, Wischhofstrasse 1-3, 24148, Kiel, Germany aut NATIONALLICENCE 700 1- Horozal Senay Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut NATIONALLICENCE 700 1- Lee Gwang Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut NATIONALLICENCE 700 1- Kim Dae Department of Energy Resources Engineering, Pukyong National University, 608-737, Busan, South Korea aut NATIONALLICENCE 700 1- Han Hyun Korea Institute of Geoscience and Mineral Resources, 305-350, Daejon, South Korea aut NATIONALLICENCE 700 1- Kang Moo Korea Institute of Geoscience and Mineral Resources, 305-350, Daejon, South Korea aut NATIONALLICENCE 773 0- Marine Geophysical Research Springer Netherlands 32/3(2011-09-01), 363-381 0025-3235 32:3<363 2011 32 11001 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer