Constant sliding velocity (i.e. rate of rotation) friction experiments on mm-thick layers of glass beads, under room temperature and humidity conditions. Stick-slip in sheared granular aggregates is considered to be an analog for the intermittent deformation of the earth’s lithosphere via earthquakes. Stick-slip can be regular, i.e. periodic and of consistent amplitude, or irregular, i.e. aperiodic and of varying amplitude. In the context of seismology, the former behavior resembles the Characteristic Earthquake Model, whereas the latter is equivalent to the Gutenberg-Richter Model. This publication contains mechanical and acoustic emission (AE) data from sliding experiments on aggregates of soda-lime glass beads. By tuning certain parame...
Simple axi-symmetric uni-axial compression tests have been realized on dry loose samples of glass be...
International audienceEarthquakes or fault core sliding occur naturally in response to long-term def...
We propose a theory of shear flow in dense granular materials. A key ingredient of the theory is an ...
Constant sliding velocity (i.e. rate of rotation) friction experiments on mm-thick layers of glass b...
The goal of predicting earthquakes remains elusive despite decades of instrumental observations and ...
Seismological observations in the past few decades have revealed a diversity of slip behaviors of fa...
Probabilistic seismic hazard analysis (PSHA) is the standard method used for designing earthquake-re...
International audienceDrained triaxial axisymmetric compression tests are performed on water-saturat...
Currently, it is unknown how seismic and aseismic slip influences the recurrence and magnitude of ea...
Currently, it is unknown how seismic and aseismic slip influences the recurrence and magnitude of ea...
International audienceTo determine the processes responsible for slip-weakening in clayey gouge zone...
We monitor the stick-slip displacements of a very slowly driven moveable perforated top plate which...
The release of stress in the lithosphere along active faults shows a wide range of behaviors spannin...
Simple axi-symmetric uni-axial compression tests have been realized on dry loose samples of glass be...
International audienceEarthquakes or fault core sliding occur naturally in response to long-term def...
We propose a theory of shear flow in dense granular materials. A key ingredient of the theory is an ...
Constant sliding velocity (i.e. rate of rotation) friction experiments on mm-thick layers of glass b...
The goal of predicting earthquakes remains elusive despite decades of instrumental observations and ...
Seismological observations in the past few decades have revealed a diversity of slip behaviors of fa...
Probabilistic seismic hazard analysis (PSHA) is the standard method used for designing earthquake-re...
International audienceDrained triaxial axisymmetric compression tests are performed on water-saturat...
Currently, it is unknown how seismic and aseismic slip influences the recurrence and magnitude of ea...
Currently, it is unknown how seismic and aseismic slip influences the recurrence and magnitude of ea...
International audienceTo determine the processes responsible for slip-weakening in clayey gouge zone...
We monitor the stick-slip displacements of a very slowly driven moveable perforated top plate which...
The release of stress in the lithosphere along active faults shows a wide range of behaviors spannin...
Simple axi-symmetric uni-axial compression tests have been realized on dry loose samples of glass be...
International audienceEarthquakes or fault core sliding occur naturally in response to long-term def...
We propose a theory of shear flow in dense granular materials. A key ingredient of the theory is an ...