Pore fluid pressure, apparent friction, and Coulomb failure

By N. Beeler, R. Simpson, S. Hickman, D. Lockner. 2000

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Introduction to special section: Stress transfer, earthquake triggering, and time‐dependent seismic hazard (2005, unknown): “Beeler et al. [2000] and Cocco and Rice [2002] have discussed the proper way to correctly include undrained pore pressure changes in Coulomb stress modeling and obtain a general expression for the effective normal stress perturbations.”
Global Omori law decay of triggered earthquakes: Large aftershocks outside the classical aftershock zone (2002, background): “, Beeler et al., 2000]. By calculating only the shear stress component I neglect potential triggering and/or inhibition of earthquakes due to normal stress changes, which in localized studies, have been shown to be important [e.g., Perfettini et al., 1999; Parsons et al., 1999]. However, in other st”
Forecasting the evolution of seismicity in southern California : Animations built on earthquake stress transfer : Stress transfer, earthquake triggering, and time-dependent seismic hazard (2005, background): “, 2000], to local pore fluid effects near the active Coso volcanic and geothermal field [Beeler et al., 2000; Peltzer et al., 1996], or perhaps to locally anomalous rate/state parameters, such as As.”