Seismotectonics of southeast France: from the Jura mountains to Corsica
The analysis of the seismicity catalog (1996 to 2019) covering the region from the Jura mountains to Corsica provides a first-order image of the distribution of earthquakes, highlighting large structures such as the Briançonnais and Piedmontais seismic arcs, the eastward deepening of the focal depth...
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Académie des sciences
2021-08-01
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Series: | Comptes Rendus. Géoscience |
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Online Access: | https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.69/ |
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author | Larroque, Christophe Baize, Stéphane Albaric, Julie Jomard, Hervé Trévisan, Jenny Godano, Maxime Cushing, Marc Deschamps, Anne Sue, Christian Delouis, Bertrand Potin, Bertrand Courboulex, Françoise Régnier, Marc Rivet, Diane Brunel, Didier Chèze, Jérôme Martin, Xavier Maron, Christophe Peix, Fabrice |
author_facet | Larroque, Christophe Baize, Stéphane Albaric, Julie Jomard, Hervé Trévisan, Jenny Godano, Maxime Cushing, Marc Deschamps, Anne Sue, Christian Delouis, Bertrand Potin, Bertrand Courboulex, Françoise Régnier, Marc Rivet, Diane Brunel, Didier Chèze, Jérôme Martin, Xavier Maron, Christophe Peix, Fabrice |
author_sort | Larroque, Christophe |
collection | DOAJ |
description | The analysis of the seismicity catalog (1996 to 2019) covering the region from the Jura mountains to Corsica provides a first-order image of the distribution of earthquakes, highlighting large structures such as the Briançonnais and Piedmontais seismic arcs, the eastward deepening of the focal depths through the Western Alps, several large active faults (e.g. Belledonne, Middle Durance, Ligure). Over this period the magnitudes are moderate and the focal mechanisms of the main events display a diversity of seismic behaviors that can be explained by the complexity of the different geological domains with a more or less strong structural inheritage, by variable rheological characteristics at the scale of the crust and by the joint action of different mechanisms of deformation. The distribution of the historical events is in fairly good agreement with the instrumental seismicity, but several earthquakes of $M >6$ are highlighted since the 14th century until the beginning of the 20th. |
first_indexed | 2024-03-11T16:14:47Z |
format | Article |
id | doaj.art-fd1cff7927f6482cb86bc140c9cddeae |
institution | Directory Open Access Journal |
issn | 1778-7025 |
language | English |
last_indexed | 2024-03-11T16:14:47Z |
publishDate | 2021-08-01 |
publisher | Académie des sciences |
record_format | Article |
series | Comptes Rendus. Géoscience |
spelling | doaj.art-fd1cff7927f6482cb86bc140c9cddeae2023-10-24T14:24:12ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252021-08-01353S110515110.5802/crgeos.6910.5802/crgeos.69Seismotectonics of southeast France: from the Jura mountains to CorsicaLarroque, Christophe0https://orcid.org/0000-0002-0866-9441Baize, Stéphane1https://orcid.org/0000-0002-7656-1790Albaric, Julie2https://orcid.org/0000-0001-7275-554XJomard, Hervé3https://orcid.org/0000-0002-3878-1215Trévisan, Jenny4https://orcid.org/0000-0002-6755-2737Godano, Maxime5https://orcid.org/0000-0001-7631-8662Cushing, Marc6https://orcid.org/0000-0002-1601-8323Deschamps, Anne7https://orcid.org/0000-0002-6209-9814Sue, Christian8https://orcid.org/0000-0002-2472-5001Delouis, Bertrand9https://orcid.org/0000-0003-1147-5872Potin, Bertrand10https://orcid.org/0000-0002-1332-5985Courboulex, Françoise11https://orcid.org/0000-0002-4467-9102Régnier, Marc12Rivet, Diane13https://orcid.org/0000-0003-4697-4460Brunel, Didier14Chèze, Jérôme15Martin, Xavier16Maron, Christophe17Peix, Fabrice18Géoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceIRSN, PSE-ENV/SCAN/BERSSIN, BP 17, 92 262 Fontenay-aux-roses, FranceCNRS-UMR 6249, Bourgogne-Franche-Comté University, 25 000 Besançon, FranceIRSN, PSE-ENV/SCAN/BERSSIN, BP 17, 92 262 Fontenay-aux-roses, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceIRSN, PSE-ENV/SCAN/BERSSIN, BP 17, 92 262 Fontenay-aux-roses, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceCNRS, IRD, IFSTTAR, ISTerre, University Grenoble Alpes, University Savoie Mont Blanc, 38 000 Grenoble, France; CNRS-UMR 6249, Bourgogne-Franche-Comté University, 25 000 Besançon, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceDepartamento de Geofìsica, Universidad de Chile, Blanco Encalada 2002, Santiago, 8320000, ChileGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceGéoazur, Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, 06 560 Valbonne, FranceThe analysis of the seismicity catalog (1996 to 2019) covering the region from the Jura mountains to Corsica provides a first-order image of the distribution of earthquakes, highlighting large structures such as the Briançonnais and Piedmontais seismic arcs, the eastward deepening of the focal depths through the Western Alps, several large active faults (e.g. Belledonne, Middle Durance, Ligure). Over this period the magnitudes are moderate and the focal mechanisms of the main events display a diversity of seismic behaviors that can be explained by the complexity of the different geological domains with a more or less strong structural inheritage, by variable rheological characteristics at the scale of the crust and by the joint action of different mechanisms of deformation. The distribution of the historical events is in fairly good agreement with the instrumental seismicity, but several earthquakes of $M >6$ are highlighted since the 14th century until the beginning of the 20th.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.69/CorsicaEarthquakesFaultsJura–BresseSoutheast basinWestern AlpsLigurian SeaCorsica |
spellingShingle | Larroque, Christophe Baize, Stéphane Albaric, Julie Jomard, Hervé Trévisan, Jenny Godano, Maxime Cushing, Marc Deschamps, Anne Sue, Christian Delouis, Bertrand Potin, Bertrand Courboulex, Françoise Régnier, Marc Rivet, Diane Brunel, Didier Chèze, Jérôme Martin, Xavier Maron, Christophe Peix, Fabrice Seismotectonics of southeast France: from the Jura mountains to Corsica Comptes Rendus. Géoscience Corsica Earthquakes Faults Jura–Bresse Southeast basin Western Alps Ligurian Sea Corsica |
title | Seismotectonics of southeast France: from the Jura mountains to Corsica |
title_full | Seismotectonics of southeast France: from the Jura mountains to Corsica |
title_fullStr | Seismotectonics of southeast France: from the Jura mountains to Corsica |
title_full_unstemmed | Seismotectonics of southeast France: from the Jura mountains to Corsica |
title_short | Seismotectonics of southeast France: from the Jura mountains to Corsica |
title_sort | seismotectonics of southeast france from the jura mountains to corsica |
topic | Corsica Earthquakes Faults Jura–Bresse Southeast basin Western Alps Ligurian Sea Corsica |
url | https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.69/ |
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