Nucleation and early seismic propagation of small and large events in a crustal earthquake model

By N. Lapusta, J. Rice. 2003

377 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/55edd2900ec084dbe8b39e04637d29700a8fe1ab

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In Geophysics

Citations in the corpus

Earthquake nucleation on (aging) rate and state faults (2005, background): “In numerical models these are regions of large stressing rate and preferential earthquake nucleation [Lapusta and Rice, 2003].”
Three‐dimensional boundary integral modeling of spontaneous earthquake sequences and aseismic slip (2009, background): “traction (B11) to the strength given by the regularized form of the rate and state friction law [e.g., Rice and Ben-Zion, 1996; Ben-Zion and Rice, 1997; Lapusta et al., 2000; Lapusta and Rice, 2003] results in”
Modern topics and challenges in dynamic fracture (2005, background): “Lapusta and Rice (2003) went on to study nucleation of shear cracks and their early dynamic stages in the context of dynamic shear ruptures.”
Earthquake Initiation From Laboratory Observations and Implications for Foreshocks (2019, background): “Some studies have explored whether nucleation characteristics affect the eventual size of an earthquake (e.g., Beroza & Ellsworth, 1996; Lapusta & Rice, 2003).”
The transition of dynamic rupture styles in elastic media under velocity-weakening friction (2012, background): “…provide a basis for the design and interpretation of future studies that will incorporate more physical, spontaneous nucleation process through earthquake cycle simulations, although at a much higher computational cost [Lapusta and Rice, 2003; Kaneko and Lapusta, 2008; Noda and Lapusta, 2010].”
Aseismic slip transients emerge spontaneously in three-dimensional rate and state modeling of subduction earthquake sequences (2005, background): “D strike slip modeling [Lapusta et al., 2000; Lapusta and Rice, 2003] to produce similar earthquake sequences as for fully elastodynamic modeling, but with somewhat less slip in events, and with sluggish propagation of the rupture front and slip development (e.g., minutes rather than seconds for…”
Precursory Slow Slip and Foreshocks on Rough Faults (2020, positive): “…by theory (Ruina, 1983; Dieterich, 1992; Rubin & Ampuero, 2005; Am-60 puero & Rubin, 2008) and has been observed in laboratory experiments (Dieterich & Kil-61 gore, 1996; McLaskey & Lockner, 2014; McLaskey, 2019) and numerical simulations (e.g. Dieterich, 1992; Lapusta et al., 2000; Lapusta, 2003).”
Modeling afterslip and aftershocks following the 1992 Landers earthquake (2007, neutral): “, 2002] and by theoretical considerations [Rice, 1993; Lapusta and Rice, 2003].”
From Geodetic Imaging of Seismic and Aseismic Fault Slip to Dynamic Modeling of the Seismic Cycle (2015, background): “…depth zd and negative above that, the model can predict long interseismic periods of locking of the updip portion of the interface and occasional rupture of the shallow portion, with transient afterslip within the transition zone (e.g., Lapusta & Rice 2003, Lapusta et al. 2000, Tse & Rice 1986).”
Comparison of finite difference and boundary integral solutions to three‐dimensional spontaneous rupture (2005, positive): “[19] Boundary integral (BI) methods have been widely used to investigate spontaneous propagation of cracks in elastic media [e.g., Das, 1980; Andrews, 1985; Das and Kostrov, 1988; Cochard and Madariaga, 1994; Perrin et al., 1995; Geubelle and Rice, 1995; Ben-Zion and Rice, 1997; Kame and Yamashita, ”
Foreshocks during the nucleation of stick‐slip instability (2013, background): “[7] The foreshocks we record are significantly smaller than the theoretical minimum length scale h* over which an earthquake can nucleate under conditions of quasi-static loading and homogeneous fault friction [Dieterich, 1986; Rice, 1993; Lapusta and Rice, 2003].”
The physics of earthquakes (2001, background): “For a more sophisticated frictional model, the nucleation zone can be as large as 1 m (e.g. Lapusta and Rice (2003)).”
Spectral element modeling of spontaneous earthquake rupture on rate and state faults: Effect of velocity‐strengthening friction at shallow depths (2008, background): “…including earthquake nucleation, postseismic slip, foreshocks, aftershocks, and aseismic transients [e.g., Marone et al., 1991; Dieterich, 1994; Ben-Zion and Rice, 1997; Marone, 1998; Lapusta and Rice, 2003; Liu and Rice, 2005; Kaneko and Lapusta, 2008; Dieterich, 2007, and references therein].”