Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences

The Ubaye Region is the most seismically active region in the Western Alps, with earthquakes that were commonly felt by the population and that even damaged local villages and cities. Since the first testimonies in 1844, this area has been regularly struck by seismic swarms with a high number of eve...

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Main Authors: Baques, Marion, De Barros, Louis, Duverger, Clara, Jomard, Hervé, Godano, Maxime, Courboulex, Françoise, Larroque, Christophe
Format: Article
Language:English
Published: Académie des sciences 2021-09-01
Series:Comptes Rendus. Géoscience
Subjects:
Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.76/
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author Baques, Marion
De Barros, Louis
Duverger, Clara
Jomard, Hervé
Godano, Maxime
Courboulex, Françoise
Larroque, Christophe
author_facet Baques, Marion
De Barros, Louis
Duverger, Clara
Jomard, Hervé
Godano, Maxime
Courboulex, Françoise
Larroque, Christophe
author_sort Baques, Marion
collection DOAJ
description The Ubaye Region is the most seismically active region in the Western Alps, with earthquakes that were commonly felt by the population and that even damaged local villages and cities. Since the first testimonies in 1844, this area has been regularly struck by seismic swarms with a high number of events, such as in 2003–2004 or 2012–2015, or by mainshock–aftershock sequences with a magnitude up to ML 5.3 in 1959. In this paper, we analysed both historical records and instrumental seismicity in the light of geological observations. Some earthquakes could be associated with known faults, even if most of them occurred on blind, unknown faults that reveal a highly fractured basement. The abnormal level of seismicity, together with its peculiar behaviour, suggests complex driving processes involving not only tectonic loading but also fluid pressure.
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spelling doaj.art-782a97e530b74f93a4593cda542e24572023-10-24T14:24:12ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252021-09-01353S153555910.5802/crgeos.7610.5802/crgeos.76Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequencesBaques, Marion0https://orcid.org/0000-0003-3078-0223De Barros, Louis1https://orcid.org/0000-0002-5541-9162Duverger, Clara2https://orcid.org/0000-0002-7814-1546Jomard, Hervé3https://orcid.org/0000-0002-3878-1215Godano, Maxime4https://orcid.org/0000-0001-7631-8662Courboulex, Françoise5https://orcid.org/0000-0002-4467-9102Larroque, Christophe6https://orcid.org/0000-0002-0866-9441Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, FranceUniversité Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, FranceCEA, DAM, DIF, F-91297 Arpajon, FranceBureau d’évaluation des risques sismiques pour la sûreté des installations, Institut de Radioprotection et Sûreté Nucléaire, Fontenay-aux-Roses, FranceUniversité Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, FranceUniversité Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, FranceUniversité Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, FranceThe Ubaye Region is the most seismically active region in the Western Alps, with earthquakes that were commonly felt by the population and that even damaged local villages and cities. Since the first testimonies in 1844, this area has been regularly struck by seismic swarms with a high number of events, such as in 2003–2004 or 2012–2015, or by mainshock–aftershock sequences with a magnitude up to ML 5.3 in 1959. In this paper, we analysed both historical records and instrumental seismicity in the light of geological observations. Some earthquakes could be associated with known faults, even if most of them occurred on blind, unknown faults that reveal a highly fractured basement. The abnormal level of seismicity, together with its peculiar behaviour, suggests complex driving processes involving not only tectonic loading but also fluid pressure.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.76/Mainshock-aftershocks sequencesEarthquake swarmsFluid-driven processUbaye regionFrench Western AlpsMainshock-aftershocks sequences
spellingShingle Baques, Marion
De Barros, Louis
Duverger, Clara
Jomard, Hervé
Godano, Maxime
Courboulex, Françoise
Larroque, Christophe
Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
Comptes Rendus. Géoscience
Mainshock-aftershocks sequences
Earthquake swarms
Fluid-driven process
Ubaye region
French Western Alps
Mainshock-aftershocks sequences
title Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
title_full Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
title_fullStr Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
title_full_unstemmed Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
title_short Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
title_sort seismic activity in the ubaye region french alps a specific behaviour highlighted by mainshocks and swarm sequences
topic Mainshock-aftershocks sequences
Earthquake swarms
Fluid-driven process
Ubaye region
French Western Alps
Mainshock-aftershocks sequences
url https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.76/
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