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Slow-slip phenomena, including afterslips and silent earthquakes, are studiedusing a one-dimensional Burridge--Knopoff model that obeys the rate-and-statedependent friction law. By varying only a few model parameters, this simplemodel allows reproducing a variety of seismic slips within a single framework,including main shocks, precursory nucleation processes, afterslips, and silentearthquakes.

Slow-Slip Phenomena Represented by the One-Dimensional Burridge-Knopoff Model of Earthquakes