Foreshocks during the nucleation of stick‐slip instability

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Earthquake Initiation From Laboratory Observations and Implications for Foreshocks (2019, background): “Laboratory observations of seismic indicators such as foreshocks and tremors (McLaskey & Kilgore, 2013; Zhuo et al., 2018) will be the focus of a future study, though seismic implications of various nucleation models are considered in section 6.”
Characterization of nucleation during laboratory earthquakes (2013, background): “…was first observed experimentally on Westerly granite [Dieterich, 1978; Okubo and Dieterich, 1984; Ohnaka and Shen, 1999], more recently at an interface between two polycarbonate blocks [Nielsen et al., 2010; Kaneko and Ampuero, 2011] and between Sierra White granite [McLaskey and Kilgore, 2013].”
Preslip and cascade processes initiating laboratory stick slip (2014, background): “For example, McLaskey and Kilgore [2013] showed that increased local stressing rate due to aseismic slip promoted instability (i.”