Triggering of Seismicity by Pore-pressure Perturbations: Permeability-related Signatures of the Phenomenon

By Serge A Shapiro, R. Patzig, E. Rothert, J. Rindschwentner. Pure and Applied Geophysics, 2003

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Introduction to special section: Stress transfer, earthquake triggering, and time‐dependent seismic hazard (2005, methodology): “Diffusive processes of pore pressure relaxation in fractured and saturated rocks have been proposed to explain both earthquakes [Noir et al., 1997; Bosl and Nur, 2002] and induced seismicity [see Shapiro et al., 2003; Paroditis et al., 2005, and references therein].”
A thermal pressurization model for the spontaneous dynamic rupture propagation on a three‐dimensional fault: 1. Methodological approach (2006, background): “They can also trigger aftershocks controlling the patterns of seismicity both in space and time [e.g., Nur and Booker, 1972; Miller et al., 1996, 2004; Yamashita, 1998; Shapiro et al., 2003; Antonioli et al., 2006].”