FN Archimer Export Format
PT J
TI Seismic Exploration of the Deep Structure and Seismogenic Faults in the Ligurian Sea by Joint Multi Channel and Ocean Bottom Seismic Acquisitions: Preliminary Results of the SEFASILS Cruise
BT 
AF Dessa, Jean-Xavier
   Beslier, Marie-Odile
   Schenini, Laure
   Chamot-Rooke, Nicolas
   Corradi, Nicolà
   Delescluse, Matthias
   Déverchère, Jacques
   Larroque, Christophe
   Sambolian, Serge
   Canva, Albane
   Operto, Stéphane
   Ribodetti, Alessandra
   Agurto-Detzel, Hans
   Bulois, Cédric
   Chalumeau, Caroline
   Combe, Laure
AS 1:1;2:2;3:2;4:3;5:4;6:3;7:5;8:6;9:2;10:2;11:2;12:2;13:2;14:2;15:2;16:2;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;
C1 Université Côte d'Azur, Sorbonne Université, CNRS, IRD, Observatoire de la Côte d'Azur, Géoazur, 250 rue Albert Einstein - CS 10269 - F 06905 Sophia-Antipolis CEDEX, France
   Université Côte d'Azur, CNRS, IRD, Observatoire de la Côte d'Azur, Géoazur, 250 rue Albert Einstein - CS 10269 - F 06905 Sophia-Antipolis CEDEX, France
   Laboratoire de Géologie, École Normale Supérieure, PSL Research University, CNRS - F 75231 Paris, France
   DISTAV, Universita di Genova, Corso Europa, 26 - 16132 Genova, Italy
   Univ. Brest, CNRS, Laboratoire Géosciences Océan - F 29280 Plouzané, France
   Université Côte d'Azur, Université de Reims, CNRS, IRD, Observatoire de la Côte d'Azur, Géoazur, 250 rue Albert Einstein - CS 10269 - F 06905 Sophia-Antipolis CEDEX, France
C2 UNIV SORBONNE, FRANCE
   UNIV NICE, FRANCE
   ENS, FRANCE
   UNIV GENOVA, ITALY
   UBO, FRANCE
   UNIV REIMS, FRANCE
UM LGO
IN DOAJ
TC 5
UR https://archimer.ifremer.fr/doc/00615/72690/71694.pdf
LA English
DT Article
CR SEFASILS
BO Pourquoi pas ?
DE ;Western Mediterranean;Ligurian basin;tectonic inversion;salt tectonics;crustal geophysical exploration;multichannel seismic imaging;wide-angle seismic recording
AB The north Ligurian margin is a complex geological area in many ways. It has witnessed several phases of highly contrasting deformation styles, at both crustal scale and that of shallower cover tectonics, simultaneously or in quick succession, and with significant spatial variability. This complex interplay is mirrored in the resulting intricate structures that make it hard to identify active faults responsible for both, the significant seismicity observed, and the tectonic inversion undergone by the margin, identified at longer time scales on morphostructural grounds. We present here the first preliminary results of the leg 1 of SEFASILS cruise, conducted in 2018 offshore Monaco, in an effort to answer these questions by means of modern deep seismic acquisitions, using multichannel reflection and wide-angle sea-bottom records. Some first interpretations are provided and point towards an active basement deformation that focuses at the limits between main crustal domains. 
PY 2020
PD MAR
SO Geosciences
SN 2076-3263
PU MDPI AG
VL 10
IS 3
UT 000523701300003
DI 10.3390/geosciences10030108
ID 72690
ER

EF