Deep Long Period Earthquakes Beneath Volcanoes of the French Massif Central

Abstract The recent installation of new broadband seismic stations in the French Massif Central (FMC) has resulted in the detection of a few “deep” earthquakes located near the crust‐mantle boundary beneath volcanic regions. Analysis of the spectral content of the respective waveforms has shown that the spectra of these “deep” earthquakes are significantly depleted in high frequencies. Based on these observations of anomalous depth and spectral content, these earthquakes can be classified as Deep Long Period (DLP) events. This is a specific class of volcanic seismicity observed beneath many active volcanoes around the World. While the exact physical origin of this type of earthquakes is still debated, they are often considered as indicators of the presence of magma near the crust‐mantle boundary. Therefore, observation of DLP earthquakes can bring new insights into understanding the state and the activity of the recent FMC volcanoes.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-06-18
DOI
https://doi.org/10.1029/2025gl114904
Citations
1
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
1.87

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Deep Long Period Earthquakes Beneath Volcanoes of the French Massif Central

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Deep Long Period Earthquakes Beneath Volcanoes of the French Massif Central

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article en
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Abstract

Abstract The recent installation of new broadband seismic stations in the French Massif Central (FMC) has resulted in the detection of a few “deep” earthquakes located near the crust‐mantle boundary beneath volcanic regions. Analysis of the spectral content of the respective waveforms has shown that the spectra of these “deep” earthquakes are significantly depleted in high frequencies. Based on these observations of anomalous depth and spectral content, these earthquakes can be classified as Deep Long Period (DLP) events. This is a specific class of volcanic seismicity observed beneath many active volcanoes around the World. While the exact physical origin of this type of earthquakes is still debated, they are often considered as indicators of the presence of magma near the crust‐mantle boundary. Therefore, observation of DLP earthquakes can bring new insights into understanding the state and the activity of the recent FMC volcanoes.

Geophysical Research LettersVol. 52(12)
Centre National de la Recherche Scientifique (FR), Université Toulouse III - Paul Sabatier (FR), Université Clermont Auvergne (FR), Geological Survey of Denmark and Greenland (DK), Istituto Nazionale di Geofisica e Vulcanologia (IT), Institut des Sciences de la Terre (FR), Observatoire Midi-Pyrénées (FR), Laboratoire Magmas et Volcans (FR), Université Gustave Eiffel (FR), Institut de Recherche pour le Développement (FR), Université Savoie Mont Blanc (FR), Université Grenoble Alpes (FR)
Agence Nationale de la Recherche, HORIZON EUROPE European Research Council
Openalex Percentile: Top 17%
earthquake and tectonic studies
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