Fault reactivation during fluid pressure oscillations: transition from stable to unstable slip

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While sliding at seismic slip-rates of ∼1 m/s, natural faults undergo an abrupt decrease of shear stress called dynamic weakening. Asperity-scale processes related to flash heating and weakening and, meso-scale (mm-cm) processes involving shear across the ...

Fault reactivation during fluid pressure oscillations: transition from stable to unstable slip

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Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks

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Determination of Parameters Characteristic of Dynamic Weakening Mechanisms During Seismic Faulting in Cohesive Rocks