On the physical mechanism of silent slip events along the deeper part of the seismogenic zone

By B. Shibazaki, Y. Iio. 2003

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Statistical physics of fracture, friction, and earthquakes (2011, methodology): “Repeating slow earthquakes at transition depths from shallow locked zone to deeper stable sliding zone were simulated in Shibazaki and Iio (2003) and Shibazaki and Shimamoto (2007).”
Spatial and temporal evolution of stress and slip rate during the 2000 Tokai slow earthquake (2006, methodology): “Shibazaki and Iio [2003] performed a three dimensional simulation using Dietrich-Ruina friction law with a small cutoff velocity to an evolution effect in the friction law at depths below seismogenic zone and were able to reproduce slow slip events.”
Afterslip and aftershocks in the rate‐and‐state friction law (2007, methodology): “…used the rate-and-state friction law to model slow earthquakes [Boatwright and Cocco, 1996; Belardinelli, 1997; Reinen, 2000; Du et al., 2003; Shibazaki and Iio, 2003; Yoshida and Kato, 2003; Hirose and Hirahara, 2004; Liu and Rice, 2005, 2007; Lowry, 2006; Mitsui and Hirahara, 2006;…”