Aseismic slip transients emerge spontaneously in three-dimensional rate and state modeling of subduction earthquake sequences

By Yajing Liu, J. Rice. 2005

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View Paper: https://www.semanticscholar.org/paper/6349b0bb646e6e0929e1e9ecf7454aa0a229b496

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In Geophysics

Citations in the corpus

Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, background): “…used inmodels of fault slip nucleation and propagation both for quasi-static, slow slip (e.g. Kuroki et al., 2004; Yoshida and Kato, 2003; Liu and Rice, 2005; Rubin, 2008) and dynamic slip (e.g. Rice and Tse, 1986; Dieterich, 1992; Fukuyama and Madariaga, 1998; Bizzarri and Cocco, 2003)…”
Three‐dimensional boundary integral modeling of spontaneous earthquake sequences and aseismic slip (2009, background): “Such large values of h* may be realistic under some conditions, e.g., if effective normal stress s is very low due to fluid overpressure [e.g., Liu and Rice, 2005; Suppe and Yue, 2007] or if steady state velocity-weakening properties are close to velocity neutral.”
Earthquake Initiation From Laboratory Observations and Implications for Foreshocks (2019, background): “Earthquake nucleation is intimately related to stability, so this study may also have relevance to our understanding of slow earthquakes, which might be considered unsuccessful earthquake nucleation attempts (e.g., Liu & Rice, 2005).”
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].”
Earthquake nucleation on rate and state faults - Aging and slip laws (2008, background): “[51] Dropping the effective normal stress to 1 MPa, as advocated by Liu and Rice [2007], could increase the aging law nucleation length to tens of kilometers.”
Spatial and temporal evolution of stress and slip rate during the 2000 Tokai slow earthquake (2006, background): “The second mechanism on the other hand, involves spatial variations in the frictional parameters and, according to Liu and Rice [2005], some degree of along-strike stress heterogeneity.”
Afterslip and aftershocks in the rate‐and‐state friction law (2007, methodology): “, 1991], slow earthquakes [e.g., Yoshida and Kato, 2003; Liu and Rice, 2005], and seismic activity [e.”