Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip

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Foreshocks during the nucleation of stick‐slip instability (2013, background): “On average, interevent times are ~25min for stick-slip events preceded by a reset stage and ~8min for those without reset.”
Dynamics of a velocity strengthening fault region: Implications for slow earthquakes and postseismic slip (2008, neutral): “Deep low-frequency earthquakes have also been observed in coincidence with tremor and episodic slow slip in subduction zones, with focal mechanism and location consistent with interplate slip [ Shelly et al. , 2006, 2007].”
Scaling of small repeating earthquakes explained by interaction of seismic and aseismic slip in a rate and state fault model (2009, background): “Recent observations suggest that similar interaction occurs on larger spatial scales, with aseismic slip transients and seismic tremor discovered on several seismogenic faults [Kao et al., 2005; Shelly et al., 2006; Schwartz and Rokosky, 2007].”