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

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 in...

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Main Authors: Jean-Xavier Dessa, Marie-Odile Beslier, Laure Schenini, Nicolas Chamot-Rooke, Nicolà Corradi, Matthias Delescluse, Jacques Déverchère, Christophe Larroque, Serge Sambolian, Albane Canva, Stéphane Operto, Alessandra Ribodetti, Hans Agurto-Detzel, Cédric Bulois, Caroline Chalumeau, Laure Combe
Format: Article
Language:English
Published: MDPI AG 2020-03-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/10/3/108
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author Jean-Xavier Dessa
Marie-Odile Beslier
Laure Schenini
Nicolas Chamot-Rooke
Nicolà Corradi
Matthias Delescluse
Jacques Déverchère
Christophe Larroque
Serge Sambolian
Albane Canva
Stéphane Operto
Alessandra Ribodetti
Hans Agurto-Detzel
Cédric Bulois
Caroline Chalumeau
Laure Combe
author_facet Jean-Xavier Dessa
Marie-Odile Beslier
Laure Schenini
Nicolas Chamot-Rooke
Nicolà Corradi
Matthias Delescluse
Jacques Déverchère
Christophe Larroque
Serge Sambolian
Albane Canva
Stéphane Operto
Alessandra Ribodetti
Hans Agurto-Detzel
Cédric Bulois
Caroline Chalumeau
Laure Combe
author_sort Jean-Xavier Dessa
collection DOAJ
description 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.
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spelling doaj.art-fd9e4e27fa21489c9cf9bd0333773e6a2022-12-22T03:15:35ZengMDPI AGGeosciences2076-32632020-03-0110310810.3390/geosciences10030108geosciences10030108Seismic 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 CruiseJean-Xavier Dessa0Marie-Odile Beslier1Laure Schenini2Nicolas Chamot-Rooke3Nicolà Corradi4Matthias Delescluse5Jacques Déverchère6Christophe Larroque7Serge Sambolian8Albane Canva9Stéphane Operto10Alessandra Ribodetti11Hans Agurto-Detzel12Cédric Bulois13Caroline Chalumeau14Laure Combe15CNRS, IRD, Université Côte d’Azur, Sorbonne Université, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceLaboratoire de Géologie, École Normale Supérieure, PSL Research University, CNRS, F 75231 Paris, FranceDISTAV, Universita di Genova, Corso Europa, 26, 16132 Genova, ItalyLaboratoire de Géologie, École Normale Supérieure, PSL Research University, CNRS, F 75231 Paris, FranceCNRS, Laboratoire Géosciences Océan, Univ. Brest, F 29280 Plouzané, FranceCNRS, IRD, Université Côte d’Azur, Université de Reims, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceCNRS, IRD, Université Côte d’Azur, Observatoire de la Côte d’Azur, Géoazur, 250 rue Albert Einstein, CS 10269, F 06905 Sophia-Antipolis CEDEX, FranceThe 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.https://www.mdpi.com/2076-3263/10/3/108western mediterraneanligurian basintectonic inversionsalt tectonicscrustal geophysical explorationmultichannel seismic imagingwide-angle seismic recording
spellingShingle Jean-Xavier Dessa
Marie-Odile Beslier
Laure Schenini
Nicolas Chamot-Rooke
Nicolà Corradi
Matthias Delescluse
Jacques Déverchère
Christophe Larroque
Serge Sambolian
Albane Canva
Stéphane Operto
Alessandra Ribodetti
Hans Agurto-Detzel
Cédric Bulois
Caroline Chalumeau
Laure Combe
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
Geosciences
western mediterranean
ligurian basin
tectonic inversion
salt tectonics
crustal geophysical exploration
multichannel seismic imaging
wide-angle seismic recording
title 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
title_full 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
title_fullStr 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
title_full_unstemmed 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
title_short 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
title_sort 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
topic western mediterranean
ligurian basin
tectonic inversion
salt tectonics
crustal geophysical exploration
multichannel seismic imaging
wide-angle seismic recording
url https://www.mdpi.com/2076-3263/10/3/108
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