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Mechanical energy dissipation during seismic dynamic weakening in calcite‐bearing faults
Earthquakes are frictional instabilities caused by the shear stress decrease, that is, dynamic
weakening, of faults with slip and slip rate. During dynamic weakening, shear stress …
weakening, of faults with slip and slip rate. During dynamic weakening, shear stress …
Bonded nanoparticles restrengthen faults during earthquake slip
Faults are the primary sources of seismicity worldwide, yet the mechanisms of fault
weakening and recovery remain controversial. This study examines the microstructures and …
weakening and recovery remain controversial. This study examines the microstructures and …