Aftershock triggering by complete Coulomb stress changes

By D. Kilb, J. Gomberg, P. Bodin. 2002

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EARTHQUAKE TRIGGERING BY STATIC, DYNAMIC, AND POSTSEISMIC STRESS TRANSFER (2005, background): “In a related study, Kilb et al. (2002b) suggests that large peak dynamic stresses following the Landers earthquake could have played a role in the eventual triggering of the Hector Mine earthquake.”
New constraints on mechanisms of remotely triggered seismicity at Long Valley Caldera (2005, background): “[3] As pointed out by previous studies, in these longrange, rapid triggering cases, the seismic waves are the immediate cause of the earthquakes rather than the largescale static stress change or viscoelastic stresses [e.g., Hill et al., 1993; Kilb et al., 2002 ].”
Introduction to special section: Stress transfer, earthquake triggering, and time‐dependent seismic hazard (2005, background): “A correlation between seismicity rate changes and rupture directivity has been noted in cases of triggering at remote distances [Mohamad et al., 2000; Gomberg et al., 2001; Kilb et al., 2002; Kilb, 2003; Gomberg et al., 2004] and in the near field [Gomberg et al., 2003].”