Influence of pore‐pressure on the event‐size distribution of induced earthquakes

By Corinne Bachmann, S. Wiemer, B. Goertz-Allmann, J. Woessner. 2012

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Fluid‐faulting evolution in high definition: Connecting fault structure and frequency‐magnitude variations during the 2014 Long Valley Caldera, California, earthquake swarm (2016, background): “In natural faulting, these mechanisms are often intertwined, particularly when fluid pressure perturbations are involved [e.g., Wiemer and McNutt, 1997; Wiemer et al., 1998; Bachmann et al., 2012].”
Data‐driven spatial b value estimation with applications to California seismicity: To b or not to b (2015, background): “…of various faulting regimes [Wiemer and Wyss, 1997, 2002], as a proxy for shear stress and pore pressure [Scholz, 1968; Schorlemmer et al., 2005; Bachmann et al., 2012], as an indicator of material heterogeneity [Mogi, 1962; Mori and Abercrombie, 1997], or even as precursors of future rupture…”
Acoustic emissions document stress changes over many seismic cycles in stick‐slip experiments (2013, background): “…doi:10.1002/grl.50507, 2013 Acoustic emissions document stress changes over many seismic cycles in stick-slip experiments T. H. W. Goebel,1 D. Schorlemmer,2 T. W. Becker,1 G. Dresen,3 and C. G. Sammis1 Received 25 February 2013; revised 19 April 2013; accepted 25 April 2013; published 31 May 2013.”