The seismic cycle and the difference between foreshocks and aftershocks in a mechanical fault model
Author:
Affiliation:
1. Ben-Gurion University of the Negev; Beer-Sheva Israel
2. École Normale Supérieure; Paris France
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Reference16 articles.
1. Large earthquake cycles and intermittent criticality on heterogeneous faults due to evolving stress and seismicity;Ben-Zion;J. Geopys. Res.,2003
2. Modeling of rock friction, 1. Experimental results and constitutive equations;Dieterich;J. Geophys. Res.,1979
3. Earthquake nucleation on faults with rate- and state- dependent strength;Dieterich;Tectonophysics,1992
4. A constitutive law for rate of earthquake production and its application to earthquake clustering;Dieterich;J. Geophys. Res.,1994
5. Earthquake simulations with time-dependent nucleation and long-range interaction;Dieterich;Nonlinear Proces. Geophys.,1995
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2. Modeling the Impact of the Viscoelastic Layer Thickness and the Frictional Strength to the Lithosphere Deformation in a Strike-Slip Fault: Insight to the Seismicity Pattern along the Great Sumatran Fault;GeoHazards;2022-10-06
3. The thickness of faults: From laboratory experiments to field scale observations;Tectonophysics;2006-10
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