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Authordc.contributor.authorLarroque, Christophe
Authordc.contributor.authorBaize, Stéphane
Authordc.contributor.authorAlbaric, Julie
Authordc.contributor.authorJomard, Hervé
Authordc.contributor.authorTrévisan, Jenny
Authordc.contributor.authorGodano, Maxime
Authordc.contributor.authorCushing, Marc
Authordc.contributor.authorDeschamps, Anne
Authordc.contributor.authorSue, Christian
Authordc.contributor.authorDelouis, Bertrand
Authordc.contributor.authorPotin, Bertrand
Authordc.contributor.authorCourboulex, Francoise
Authordc.contributor.authorRégnier, Marc
Authordc.contributor.authorRivet, Diane
Authordc.contributor.authorBrunel, Didier
Authordc.contributor.authorCheze, Jerome
Authordc.contributor.authorMartin, Xavier
Authordc.contributor.authorMaron, Christophe
Authordc.contributor.authorPeix, Fabrice
Admission datedc.date.accessioned2022-03-23T19:28:28Z
Available datedc.date.available2022-03-23T19:28:28Z
Publication datedc.date.issued2021
Cita de ítemdc.identifier.citationComptes Rendus Géoscience — Sciences de la Planète 2021, 353, no. S1, p. 105-151es_ES
Identifierdc.identifier.other10.5802/crgeos.69
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/184408
Abstractdc.description.abstractThe 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.es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherCentre Mersenne pour l’édition scientifique ouvertees_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
Sourcedc.sourceComptes Rendus Géosciencees_ES
Keywordsdc.subjectEarthquakeses_ES
Keywordsdc.subjectFaultses_ES
Keywordsdc.subjectJura–Bressees_ES
Keywordsdc.subjectSoutheast basines_ES
Keywordsdc.subjectWestern Alpses_ES
Keywordsdc.subjectLigurian Seaes_ES
Keywordsdc.subjectCorsicaes_ES
Títulodc.titleSeismotectonics of southeast France: from the Jura mountains to Corsicaes_ES
Document typedc.typeArtículo de revistaes_ES
dc.description.versiondc.description.versionVersión publicada - versión final del editores_ES
dcterms.accessRightsdcterms.accessRightsAcceso abiertoes_ES
Catalogueruchile.catalogadorcrbes_ES
Indexationuchile.indexArtículo de publícación WoSes_ES


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Attribution-NonCommercial-NoDerivs 3.0 United States
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States