FN Archimer Export Format PT J TI First direct observation of coseismic slip and seafloor rupture along a submarine normal fault and implications for fault slip history BT AF ESCARTIN, Javier LECLERC, Frederique OLIVE, Jean-Arthur MEVEL, Catherine CANNAT, Mathilde PETERSEN, Sven AUGUSTIN, Nico FEUILLET, Nathalie DEPLUS, Christine BEZOS, Antoine BONNEMAINS, Diane CHAVAGNAC, Valerie CHOI, Yujin GODARD, Marguerite HAAGA, Kristian A. HAMELIN, Cedric ILDEFONSE, Benoit JAMIESON, John W. JOHN, Barbara E. LELEU, Thomas MACLEOD, Christopher J. MASSOT-CAMPOS, Miguel NOMIKOU, Paraskevi PAQUET, Marine ROMMEVAUX-JESTIN, Celine ROTHENBECK, Marcel STEINFUEHRER, Anja TOMINAGA, Masako TRIEBE, Lars CAMPOS, Ricard GRACIAS, Nuno GARCIA, Rafael ANDREANI, Muriel VILASECA, Geraud AS 1:1;2:2;3:3;4:1;5:1;6:4;7:4;8:1;9:1;10:5;11:1;12:6;13:1;14:7;15:8;16:8;17:7;18:4;19:9;20:6;21:10;22:11;23:12;24:1;25:1;26:4;27:4;28:13;29:2;30:14;31:;32:;33:15;34:1; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:;31:;32:;33:;34:; C1 CNRS UMR7154, Inst Phys Globe Paris, Paris, France. Earth Observ Singapore, Singapore, Singapore. Lamont Doherty Earth Observ, Palisades, NY USA. GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany. Univ Nantes, Nantes, France. CNRS UMR5563, Geosci Environm Toulouse, Toulouse, France. Univ Montpellier, Geosci Montpellier, Montpellier, France. Univ Bergen, Bergen, Norway. Univ Wyoming, Laramie, WY 82071 USA. Cardiff Univ, Cardiff, S Glam, Wales. Univ Balearic Isl, Palma De Mallorca, Spain. Univ Athens, Athens, Greece. Texas A&M Univ, College Stn, TX USA. Univ Girona, Girona, Spain. Univ Lyon, Lyon, France. C2 CNRS, FRANCE EARTH OBSERV SINGAPORE, SINGAPORE LDEO, USA HELMHOLTZ CTR OCEAN RES, GERMANY UNIV NANTES, FRANCE CNRS, FRANCE UNIV MONTPELLIER, FRANCE UNIV BERGEN, NORWAY UNIV WYOMING, USA UNIV CARDIFF, UK UNIV ILLES BALEARS, SPAIN UNIV ATHENS, GREECE UNIV TEXAS A&M, USA UNIV GIRONA, SPAIN UNIV LYON, FRANCE IF 4.409 TC 21 UR https://archimer.ifremer.fr/doc/00344/45500/45051.pdf https://archimer.ifremer.fr/doc/00344/45500/45052.csv LA English DT Article CR BATHYSAINTES ODEMAR BO Pourquoi pas ? DE ;submarine fault;surface rupture;earthquake;fault slip;neotectonics;microbathymetry AB Properly assessing the extent and magnitude of fault ruptures associated with large earthquakes is critical for understanding fault behavior and associated hazard. Submarine faults can trigger tsunamis, whose characteristics are defined by the geometry of seafloor displacement, studied primarily through indirect observations (e.g., seismic event parameters, seismic profiles, shipboard bathymetry, coring) rather than direct ones. Using deep-sea vehicles, we identify for the first time a marker of coseismic slip on a submarine fault plane along the Roseau Fault (Lesser Antilles), and measure its vertical displacement of ∼0.9 m in situ. We also map recent fissuring and faulting of sediments on the hangingwall, along ∼3 km of rupture in close proximity to the fault's base, and document the reactivation of erosion and sedimentation within and downslope of the scarp. These deformation structures were caused by the 2004 Mw 6.3 Les Saintes earthquake, which triggered a subsequent tsunami. Their characterization informs estimates of earthquake recurrence on this fault and provides new constraints on the geometry of fault rupture, which is both shorter and displays locally larger coseismic displacements than available model predictions that lack field constraints. This methodology of detailed field observations coupled with near-bottom geophysical surveying can be readily applied to numerous submarine fault systems, and should prove useful in evaluating seismic and tsunamigenic hazard in all geodynamic contexts. PY 2016 PD SEP SO Earth And Planetary Science Letters SN 0012-821X PU Elsevier Science Bv VL 450 UT 000381535600010 BP 96 EP 107 DI 10.1016/j.epsl.2016.06.024 ID 45500 ER EF