Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan

By K. Obara. Science, 2002

1,304 citations recorded by the source corpus.

Subfields: Artificial Intelligence, Geophysics

View Paper: https://www.semanticscholar.org/paper/890b82978412b30bca6aa8dff9c01aa91f5644f8

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Citations in the corpus

The geophysics, geology and mechanics of slow fault slip (2018, background): “Res., Solid Earth, 122 (2017), pp. 3739-3753, 10.1002/2017JB014047 Shelly et al., 2006 D.R. Shelly, G.C. Beroza, S. Ide, S. NakamulaLow-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip Nature, 442 (2006), pp. 188-191 Shibazaki et al., 2011 B. Shibazaki, T. ”
Seismic Wave Propagation and Scattering in the Heterogeneous Earth : Second Edition (2012, methodology): “Assuming that those signals mainly consisted of S-waves continuously radiated from a source, Obara (2002) first determined the location of tremor source by measuring differential travel time between stations estimated from the cross correlation of seismogram envelopes.”
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.”
Dynamics of a velocity strengthening fault region: Implications for slow earthquakes and postseismic slip (2008, positive): “Moreover, their occurrence often coincides with nonvolcanic seismic tremor [ Obara , 2002; Rogers and Dragert , 2003; Obara et al. , 2004], probably induced by fluid circulation [ Chouet , 1992; Kao et al. , 2005].”
Aseismic slip transients emerge spontaneously in three-dimensional rate and state modeling of subduction earthquake sequences (2005, background): “Rather, because fluid released from metamorphic dehydration reactions has been proposed as playing an important role in causing silent slip events [Obara, 2002; Rogers and Dragert, 2003; Kodaira et al., 2004], we had assumed that an extension of the modeling, which we still plan, to include…”
Foreshocks during the nucleation of stick‐slip instability (2013, background): “Solid Earth, 118, 2982–2997, doi:10.1002/jgrb.50232.”
A scaling law for slow earthquakes (2007, background): “Assuming a constant D for all events, equations (1) and (3) lead to a relation between L and T:”