Accelerating seismicity and stress accumulation before large earthquakes

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Foreshocks explained by cascades of triggered seismicity (2002, methodology): “For instance, the ETAS model is different from the receding stress shadow model [Bowman and King, 2001; Sammis and Sornette, 2002], from the critical earthquake model [Bowman et al., 1998; Jaumé and Sykes, 1999; Sammis and Sornette, 2002] and from the pre-slip model [Dodge et al., 1996], which in…”
Statistical physics approach to understanding the multiscale dynamics of earthquake fault systems (2003, background): “[2001], Bowman and King [2001], Zöller and Hainzl [2001, 2002], and Ben-Zion and Lyakhovsky [2002] have provided critical reviews of seismic activation.”
An 8 month slow slip event triggers progressive nucleation of the 2014 Chile megathrust (2017, background): “A first model assumes that the accelerated moment release observed before large earthquakes [Bowman and King, 2001] is triggered by a slow slip event on the fault interface [Bouchon et al., 2013; Ruiz et al., 2014; Dodge et al., 1996].”