Clara Duverger
YOU?
Author Swipe
View article: Annual variations in Nepalese seismicity: <i>b</i>-values and seismicity rates
Annual variations in Nepalese seismicity: <i>b</i>-values and seismicity rates Open
SUMMARY Seasonal variations in Nepalese seismicity have been reported with varying degrees of confidence. We re-investigate these claims by analysing 20 yr of Nepalese seismicity before the 2015 Gorkha earthquake, as detected by the Nepale…
View article: Local to moment earthquake magnitude conversion in mainland France and implications for seismic hazard assessment
Local to moment earthquake magnitude conversion in mainland France and implications for seismic hazard assessment Open
Modern ground motion prediction equations used in probabilistic seismic hazard assessment studies are now almost exclusively expressed as a function of moment magnitude MW. Yet, earthquake catalogues produced by seismic observatories often…
View article: Fluid-driven swarms and mainshock-aftershocks sequences in the Ubaye Region (Western Alps).
Fluid-driven swarms and mainshock-aftershocks sequences in the Ubaye Region (Western Alps). Open
The Ubaye Region, located in the French Western Alps, is one of the most seismically active regions in France. It is regularly hit by mainshock-aftershocks sequences (1959, ML5.3), seismic swarms (2003-2004), and complex sequences (2012-20…
View article: Update on the seismogenic potential of the Upper Rhine Graben southern region
Update on the seismogenic potential of the Upper Rhine Graben southern region Open
The Upper Rhine Graben (URG), located in France and Germany, is bordered by north–south-trending faults, some of which are considered active, posing a potential threat to the dense population and infrastructures on the Alsace plain. The la…
View article: Supplementary material to "Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region"
Supplementary material to "Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region" Open
DECLUSTERING FROM MARSAN ET AL
View article: Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region
Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region Open
The Upper Rhine Graben (URG), located in France and Germany, is bordered by north-south trending faults, some of them considered active, posing a potential threat to dense population and infrastructures from the Alsace plain. The largest h…
View article: Swarms and mainshock–aftershocks sequences are both triggered by fluids in the Ubaye Region (Western Alps)
Swarms and mainshock–aftershocks sequences are both triggered by fluids in the Ubaye Region (Western Alps) Open
SUMMARY The Ubaye Region (French Western Alps) is one of the most seismically active regions in France. It is regularly struck by mainshock–aftershocks sequences like in 1959 (ML 5.3), seismic swarms (2003–2004), and complex sequences (201…
View article: Susceptibility of Microseismic Triggering to Small Sinusoidal Stress Perturbations at the Laboratory Scale
Susceptibility of Microseismic Triggering to Small Sinusoidal Stress Perturbations at the Laboratory Scale Open
Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth's crust, these stress perturbations can be caused by various sources such as the passage of seismic waves, forcing by tides, or hydrological seasonal…
View article: How to discriminate between area-source models for probabilistic seismic hazard assessment in a more objective manner?
How to discriminate between area-source models for probabilistic seismic hazard assessment in a more objective manner? Open
We propose a methodology to assist in the selection or definition of weights for components of seismic hazard models, which are combinations of seismic source models and ground motion models, in the context of probabilistic seismic hazard …
View article: Microseismic triggering by small sinusoidal stress perturbations at the laboratory scale
Microseismic triggering by small sinusoidal stress perturbations at the laboratory scale Open
Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth's crust, these stress perturbations can be caused by various sources such as the passage of seismic waves, tidal forcing, or hydrological seasonal lo…
View article: Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region
Update of the Seismogenic Potential of the Upper Rhine Graben Southern Region Open
The Upper Rhine Graben (URG), located in France and Germany, is bordered by north-south trending faults, some of them considered active, posing a potential threat to dense population and infrastructures from the Alsace plain. The largest h…
View article: Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale"
Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale" Open
List of data contained within this repository. Total weight = ~ 40GB --- Raw data : -For all experiments (control and oscillation experiments): Mechanical data files (460 MB); Acoustic emission waveforms (40 GB). --- Derived data: -For the…
View article: Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale"
Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale" Open
List of data contained within this repository. Total weight = ~ 40GB --- Raw data : -For all experiments (control and oscillation experiments): Mechanical data files (460 MB); Acoustic emission waveforms (40 GB). --- Derived data: -For the…
View article: Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale"
Data Availibility for "Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale" Open
List of data contained within this repository. Total weight = ~ 40GB --- Raw data : -For all experiments (control and oscillation experiments): Mechanical data files (460 MB); Acoustic emission waveforms (40 GB). --- Derived data: -For the…
View article: Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale
Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale Open
Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth’s crust, these stress perturbations can be caused by various sources such as the passage of seismic waves, forcing by tides, or hydrological seasonal…
View article: Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale&#160;
Susceptibility of microseismic triggering to small sinusoidal stress perturbations at the laboratory scale  Open
<div> <p><span>Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth's crust, these transient stress changes can be caused by various sources : passing of seismic waves, forcing by tide…
View article: Seismic swarms in Tricastin, lower Rhône Valley (France): review of historical and instrumental seismicity and models
Seismic swarms in Tricastin, lower Rhône Valley (France): review of historical and instrumental seismicity and models Open
The Tricastin region in the lower Rhône Valley (France) is affected by an atypical seismic activity characterised by the development of long-lasting and recurrent seismic swarms. Indeed, since the 16th century, hundreds of seismic events s…
View article: Seismic swarms in Tricastin, lower Rhône Valley (France) : review of historical and instrumental seismicity and models
Seismic swarms in Tricastin, lower Rhône Valley (France) : review of historical and instrumental seismicity and models Open
Dans le cadre de l’intégration aux dispositions européens EPOS, Résif s'est transformé en octobre 2023 en Epos-France, une nouvelle infrastructure de recherche aux contours thématiques plus larges et en accord avec ceux de sa grande sœur e…
View article: Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences
Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences Open
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…
View article: The Western Gulf of Corinth (Greece) 2020–2021 Seismic Crisis and Cascading Events: First Results from the Corinth Rift Laboratory Network
The Western Gulf of Corinth (Greece) 2020–2021 Seismic Crisis and Cascading Events: First Results from the Corinth Rift Laboratory Network Open
We investigate a seismic crisis that occurred in the western Gulf of Corinth (Greece) between December 2020 and February 2021. This area is the main focus of the Corinth Rift Laboratory (CRL) network, and has been closely monitored with lo…
View article: Seismicity in far western Nepal reveals flats and ramps along the Main Himalayan Thrust
Seismicity in far western Nepal reveals flats and ramps along the Main Himalayan Thrust Open
SUMMARY Unravelling relations between lateral variations of mid-crustal seismicity and the geometry of the Main Himalayan Thrust (MHT) system at depth is a key issue in seismotectonic studies of the Himalayan range. These relations can rev…
View article: Complex behaviour highlighted by earthquake aftershock and swarm sequences in Ubaye Region (French Western Alps).&#160;
Complex behaviour highlighted by earthquake aftershock and swarm sequences in Ubaye Region (French Western Alps).  Open
<p>The Ubaye Region, where the city of Barcelonnette is settled, is the most seismically active region in the French Western Alps since at least two centuries. Seismicity in this area exhibits a dual behaviour, with mainshock-aftersh…
View article: A decade of seismicity in metropolitan France (2010–2019): the CEA/LDG methodologies and observations
A decade of seismicity in metropolitan France (2010–2019): the CEA/LDG methodologies and observations Open
We summarize ten years of the French seismicity recorded by the Geophysical and Detection Laboratory (LDG) of the French Alternative Energies and Atomic Energy Commission (CEA) network from 2010 to 2019. During this period, 25 265 natural …
View article: Full characterization of the ML 5.4 2019/11/11 Le Teil earthquake in France based on a multi-technology approach
Full characterization of the ML 5.4 2019/11/11 Le Teil earthquake in France based on a multi-technology approach Open
<p>Metropolitan France is a region of slow tectonic deformation rates with sparse historical and instrumental seismicity, and where geodesy is not able to reach the required resolution in order to resolve the tectonic loadings. The f…
View article: Dynamics of microseismicity and its relationship with the active structures in the western Corinth Rift (Greece)
Dynamics of microseismicity and its relationship with the active structures in the western Corinth Rift (Greece) Open
International audience
View article: Seismicity, seismic-aseismic couplings and transient deformation processes in an active fault system : the Corinth rift, Greece
Seismicity, seismic-aseismic couplings and transient deformation processes in an active fault system : the Corinth rift, Greece Open
View article: Sismicité, couplages sismique-asismiques et processus transitoires de déformation dans un système de failles actives : le rift de Corinthe, Grèce
Sismicité, couplages sismique-asismiques et processus transitoires de déformation dans un système de failles actives : le rift de Corinthe, Grèce Open
The western part of the Corinth Rift in Greece is opening at about 15 mm per year, generating one of the highest deformation rates in the world, some destructive earthquakes of magnitude M>6 per decade, and high microseismic activity irreg…
View article: Seismicity, seismic-aseismic coupling and transient deformation processes in an active fault system: the Corinth Rift, Greece
Seismicity, seismic-aseismic coupling and transient deformation processes in an active fault system: the Corinth Rift, Greece Open
View article: The 2003–2004 seismic swarm in the western Corinth rift: Evidence for a multiscale pore pressure diffusion process along a permeable fault system
The 2003–2004 seismic swarm in the western Corinth rift: Evidence for a multiscale pore pressure diffusion process along a permeable fault system Open
Microseismic multiplets occurring in the western Corinth rift, Greece, during a large swarm are analyzed to retrieve their spatiotemporal characteristics. These multiplets activated small subfaults at depth (∼7 km), up to 1 km long, at the…