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Foreshock and Aftershocks in Simple Earthquake Models
2015
Physical Review Letters
1 Many models of earthquake faults have been introduced that connect Gutenberg-Richter (GR) 2 scaling to triggering processes. However, natural earthquake fault systems are composed of a 3 variety of different geometries and materials and the associated heterogeneity in physical 4 properties can cause a variety of spatial and temporal behaviors. This raises the question of
doi:10.1103/physrevlett.114.088501
pmid:25768785
fatcat:7zwrxjis5vhl5nqaxzp3tiaacq