Earthquakes as multiscale dynamic ruptures with heterogeneous fracture surface energy

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Preslip and cascade processes initiating laboratory stick slip (2014, methodology): “This model produces a population of event sizes that is roughly consistent with the power law which describes surface roughness (i.e., a GutenbergRichter distribution) [Ide and Aochi, 2005].”
Earthquake Initiation From Laboratory Observations and Implications for Foreshocks (2019, background): “Hierarchical models (Aochi & Ide, 2004; Ide & Aochi, 2005) would be more appropriate, especially if they include rate‐dependent effects.”
Earthquake source characteristics from dynamic rupture with constrained stochastic fault stress (2007, background): “If fracture energy is heterogeneous, however, a stress distribution with smallamplitude variations or even homogeneous stress also can produce globally subshear ruptures, as demonstrated by Ide and Aochi [2005] .”