Laeticia Jacquemond

ORCID: 0009-0004-1481-9970
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Seismic Imaging and Inversion Techniques
  • Geological and Geophysical Studies Worldwide
  • High-pressure geophysics and materials
  • Landslides and related hazards
  • Earthquake Detection and Analysis
  • Seismology and Earthquake Studies

Université Côte d'Azur
2024

Observatoire de la Côte d’Azur
2024

Institut de Recherche pour le Développement
2024

Centre National de la Recherche Scientifique
2024

Université Toulouse III - Paul Sabatier
2024

Observatoire Midi-Pyrénées
2024

Géoazur
2023

SUMMARY The Lacq area in southwest France has been associated with continuous moderate induced seismic activity since 1969. However, the mechanisms driving this seismicity are not fully understood: reservoir depletion proposed as main factor, and more recently wastewater injection suggested to play a important role. interpretation of these relies heavily on quality earthquake locations, which we prove be weak due lack local instrumentation for several years. In order provide most complete...

10.1093/gji/ggae119 article EN cc-by Geophysical Journal International 2024-03-29

Abstract The 2020 Alex storm in southern France led to localized extreme rainfall exceeding 600 mm less than 24 hr. In the 100 days following storm, a series of small earthquakes swarm occurred beneath Tinée valley, region characterized by low background deformation. To gain insight into mechanisms controlling evolution, we used an enhanced seismic catalog detect 188 events. These events exhibited magnitudes comprised between −1.03 and 2.01, 78 them were relocated using relative locations at...

10.1029/2024ea003528 article EN cc-by-nc-nd Earth and Space Science 2024-06-01

The geodynamic complexity of the Southwestern Alps (France, Italy) comes from its strong tectonic inheritage due to European-African plates convergence. motion being currently mainly accommodated along Maghrebides, this region only registers small moderate seismicity linked low-deformation rates (convergence 0.3-0.9 mm/yr). Hence until now, geometry active faults in remains unclear and imprecise. Yet, a better knowledge these is prerequisite for establishment regional deformation model...

10.5194/egusphere-egu23-3365 preprint EN 2023-02-22

On 2nd October 2020, an unusual extreme rainfall event (600 mm) associated with the devastating “Alex storm” occurred in less than 24 hours Tinée valley, a low strain rate area (convergence rates of 0.3-0.9 mm/yr) Southern French Alps, located 20 kilometers from Nice city. This transitional zone between Argentera Mercantour exhumed Alpine massif and Nice/Castellane Arc, mainly filled Cenozoic sediments covering inherited structures, has no clear active faults...

10.5194/egusphere-egu23-3067 preprint EN 2023-02-22
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