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In the middle Okinawa Trough, the two last phases of extension are dated Pleistocene and late Pleistocene-Holocene. Using seismic, 3.5 kHz and swath bathymetric data acquired during the Donghai cruise, the characteristics of the two families of faults have been established and directions of extension have been deduced by comparison with analog modelling.Les deux dernieres phases d'extension identifiees...
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