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Mechanics of frictional healing
Mechanics of frictional healing
The frictional properties of rocks depend on temperature, switching from stable to unstable at various temperatures. We explain this behavior by the activation of competing healing mechanisms with the gouge layer.
Lithosphere dynamics
Lithosphere dynamics
Seismic cycles in a viscoelastic medium
Numerical modeling
Numerical modeling
Review of numerical methods for seismic cycle modeling
Fault dynamics
Fault dynamics
Rock mechanics
Granite friction
Granite friction
Rock mechanics
Mediterranean tectonics
Mediterranean tectonics
Geodetic modeling
California tectonics
California tectonics
Geodetic modeling
Main Himalayan thrust
Main Himalayan thrust
Seismic cycle modeling
Fault-bend folds
Fault-bend folds
Seismic cycle modeling
Thermal instabilities
Thermal instabilities
Crustal dynamics
Boundary integral method
Boundary integral method
Numerical methods
Parkfield earthquakes
Parkfield earthquakes
Seismic cycle modeling
Viscoelastic flow
Viscoelastic flow
Postseismic relaxation modeling