Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip

By G. Rogers, H. Dragert. Science, 2003

1,220 citations recorded by the source corpus.

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In Geophysics

Citations in the corpus

Dynamics of a velocity strengthening fault region: Implications for slow earthquakes and postseismic slip (2008, positive): “[ 51 ] Slow slip events, such as those observed in the Cascadia subduction zone, seem to be induced by stress perturbations of much smaller wavelengths.”
Spatial and temporal evolution of stress and slip rate during the 2000 Tokai slow earthquake (2006, background): “[48] The recent detection of low-frequency tremors in the Tokai area [Ohta et al., 2004], as was previously found in Cascadia [Rogers and Dragert, 2003] and the Bungo Channel [Obara et al., 2004], is suggestive of the involvement of pore fluids, and in any case is an essential clue which will…”
Machine Learning Predicts Laboratory Earthquakes (2017, background): “This signal bears resemblance to nonvolcanic tremor (Brown et al., 2009; Obara, 2002; Shelly et al., 2007) associated with slow slip (Rogers & Dragert, 2003; Rubinstein et al., 2009), which exhibits ringing characteristics over long periods of time.”
Locking depths estimated from geodesy and seismology along the San Andreas Fault System: Implications for seismic moment release (2011, background): “[27] Recent evidence of nonvolcanic tremor has also been linked to vertical transition zones from fault locking to aseismic slip [Obara et al., 2004; Rogers and Dragert, 2003].”
Statistical physics of fracture, friction, and earthquakes (2011, background): “Synchronized occurrence of short-term SSEs and low-frequency tremors were observed in other regions such as the Cascadia subduction zone, North America (Rogers and Dragert, 2003) and Shikoku, southwestern Japan (Obara et al., 2004).”
Aseismic slip transients emerge spontaneously in three-dimensional rate and state modeling of subduction earthquake sequences (2005, background): “as km/day or more in the Cascadia and Mexico subduction zones [Dragert et al., 2001; Rogers and Dragert, 2003; Kostoglodov et al., 2003].”
Interseismic Coupling, Megathrust Earthquakes and Seismic Swarms Along the Chilean Subduction Zone (38°–18°S) (2016, result): “This interpretation is consistent with observations made on several subduction zones where SSEs have been observed together with swarm seismicity (e.g., ROGERS and DRAGERT 2003; VALLEE et al. 2013); and with recent numerical models (e.g., HETLAND and SIMONS 2010; KANEKO et al. 2010).”