FN Archimer Export Format PT J TI Sedimentary markers in the Provençal Basin (western Mediterranean): a window into deep geodynamic processes BT AF LEROUX, Estelle ASLANIAN, Daniel RABINEAU, Marina MOULIN, Maryline GRANJEON, Didier GORINI, Christian DROZ, Laurence AS 1:1,2;2:3;3:2;4:3;5:4;6:1;7:2; FF 1:;2:PDG-REM-GM-LGG;3:;4:PDG-REM-GM-LGG;5:;6:;7:; C1 Univ Paris 06, UPMC, ISTEP, UMR 7193, F-75005 Paris, France. IUEM UBO, CNRS, UMR6538, Domaines Ocean, F-29280 Plouzane, France. IFREMER, Ctr Brest, GM, F-29280 Plouzane, France. IFP Energies Nouvelles, F-92852 Rueil Malmaison, France. C2 UNIV PARIS 06, FRANCE CNRS, FRANCE IFREMER, FRANCE IFP ENERGIES NOUVELLES, FRANCE SI BREST SE PDG-REM-GM-LGG UM LGO IN WOS Ifremer jusqu'en 2018 copubli-france copubli-univ-france IF 2.758 TC 13 UR https://archimer.ifremer.fr/doc/00253/36466/37817.pdf LA English DT Article CR AM-MED-1 SARDINIA BO Le Suroît L'Atalante AB Deep Earth dynamics impact so strongly on surface geological processes that we can use sediment palaeo-markers as a window into the deeper Earth. Derived from climatic and tectonic erosive actions on the continents, and related to eustasy, subsidence and isostasy, the sediment in a deep basin is the main recorder of these processes. Nevertheless, defining and quantifying the relative roles of parameters that interact to give the final sedimentary architecture is not a simple task. Using a 3D-grid of seismic and wide-angle data, boreholes and numerical stratigraphic modelling, we propose here a quantification of post-rift vertical movements in the Provençal Basin (West Mediterranean) involving three domains of subsidence: seaward tilting on the platform and the slope and purely vertical subsidence in the deep basin. These domains fit the deeper crustal domains highlighted by previous geophysical data. Post-break-up sedimentary markers may therefore be used to identify the initial hinge lines of the rifting phase and the subsidence laws. PY 2015 PD APR SO Terra Nova SN 0954-4879 PU Wiley-blackwell VL 27 IS 2 UT 000351872600005 BP 122 EP 129 DI 10.1111/ter.12139 ID 36466 ER EF