activity
20182025
most citedFault reactivation by fluid injection: Controls from stress state and injection rate

160 citations · 322 across the 6 of their papers we have counts for

collaborators

6 papers

physics.geo-ph2025★ 3 cited

Direct Estimation of Earthquake Source Properties from a Single CCTV Camera

Soumaya Latour, Mathias Lebihain, Harsha S. Bhat +4

We present a direct measurement of the slip-rate function from a natural coseismic rupture, recorded on March 28, 2025, during the 7.7 Mandalay earthquake (Myanmar). This mea…

physics.geo-ph2024★ 2 cited

Maximum size and magnitude of injection-induced slow slip events

Alexis Sáez, François Passelègue, Brice Lecampion

Fluid injections can induce aseismic slip, resulting in stress changes that may propagate faster than pore pressure diffusion, potentially triggering seismicity at significant dist…

physics.geo-ph2021★ 45 cited

On the scale dependence in the dynamics of frictional rupture: constant fracture energy versus size-dependent breakdown work

Federica Paglialunga, François Passelègue, Nicolas Brantut +3

Potential energy stored during the inter-seismic period by tectonic loading around faults is released during earthquakes as radiated energy, heat and fracture energy. The latter is…

physics.geo-ph2019★ 48 cited

On the origin of thigh-frequency radiation in experimental earthquakes

S. Marty, F. X. Passelègue, J. Aubry +3

We monitor dynamic rupture propagation during laboratory stick-slip experiments performed on saw-cut Westerly granite under upper crustal conditions (10-90 MPa). Spectral analysis…

physics.geo-ph2018★ 160 cited

Fault reactivation by fluid injection: Controls from stress state and injection rate

François. X. Passelègue, Nicolas Brantut, Thomas M. Mitchell

We studied the influence of stress state and fluid injection rate on the reactivation of faults. We conducted experiments on a saw-cut Westerly granite sample under triaxial stress…

physics.geo-ph2018★ 64 cited

Frictional heating processes and energy budget during laboratory earthquakes

J. Aubry, F. X. Passelègue, D. Deldicque +6

During an earthquake, part of the released elastic strain energy is dissipated within the slip zone by frictional and fracturing processes, the rest being radiated away via elastic…