Scientific response to the 2021–2022 seismic swarm in the Monts Dore volcanic province (France): structural insights from punctual surveys (1/2)

Long-dormant volcanic provinces remain excellent proxies in studying active edifices. The Monts Dore volcanic province (French Massif Central) has been recently the site of a unique seismic episode. Geophysical surveys were conducted at different horizontal and vertical spatial scales. Magnetic anomalies highlight mechanical heterogeneities consistent with the regional tectonic context. Low-conductive structures imaged suggest the presence of fluid rising along main paths at various depths. Although we cannot strictly exclude a purely tectonic explanation, our data seem to support the origin of seismicity as being linked to the injection of fluids at depth controlled by internal structural constraints.

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Publication Details

Journal
Comptes Rendus Géoscience
Published
2025-05-05
DOI
https://doi.org/10.5802/crgeos.284
Citations
2
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
3.73

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article

Scientific response to the 2021–2022 seismic swarm in the Monts Dore volcanic province (France): structural insights from punctual surveys (1/2)

Charley Merciecca, Vincent Boulenger, Lydie Gailler, Solène Buvat et al.
2 citations
Comptes Rendus Géoscience
earthquake and tectonic studies
3.73
article

Scientific response to the 2021–2022 seismic swarm in the Monts Dore volcanic province (France): structural insights from punctual surveys (1/2)

Charley Merciecca, Vincent Boulenger, Lydie Gailler, Solène Buvat, Cyril Aumar, Valentin Freret-Lorgeril, Philippe Labazuy, Victoria Rafflin, Guillaume Boudoire, Erwan Thébault, Nicolas Cluzel, Jean Battaglia, Jean-Michel Douchain, Marc Grunberg, Romain Guillard, Clément Grace, Thierry Souriot, Jehoji Kuzamba
article en
2 citations

Abstract

Long-dormant volcanic provinces remain excellent proxies in studying active edifices. The Monts Dore volcanic province (French Massif Central) has been recently the site of a unique seismic episode. Geophysical surveys were conducted at different horizontal and vertical spatial scales. Magnetic anomalies highlight mechanical heterogeneities consistent with the regional tectonic context. Low-conductive structures imaged suggest the presence of fluid rising along main paths at various depths. Although we cannot strictly exclude a purely tectonic explanation, our data seem to support the origin of seismicity as being linked to the injection of fluids at depth controlled by internal structural constraints.

Comptes Rendus GéoscienceVol. 357(G1)
Centre National de la Recherche Scientifique (FR), Royal Holloway University of London (GB), Université Clermont Auvergne (FR), Istituto Nazionale di Geofisica e Vulcanologia (IT), Observatoire de Physique du Globe de Clermont-Ferrand (FR), Laboratoire Magmas et Volcans (FR), Institut de Recherche pour le Développement (FR), Université de Strasbourg (FR)
Centre National d’Etudes Spatiales, Bureau de Recherches Géologiques et Minières, Université Clermont-Auvergne, European Regional Development Fund
Openalex Percentile: Top 9%
earthquake and tectonic studies
3.73
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