Tectonic tremor is associated with seismic signals in the 2–8 Hz frequency band whose durations are up to several minutes, and that can be correlated between stations separated by distances of up to a hundred kilometers or so. Since its discovery in Japan by Obara (2002), spontaneous and dynamically triggered (i.e., induced by transient seismic waves) tectonic tremor has been observed in many subduction zone environments (e.g., Gomberg et al., 2008; Peng and Chao, 2008; Peng et al., 2009; Rubinstein et al., 2009; Fry et al., 2011). Outside subduction zones,...

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.