A model of interseismic fault slip in the presence of asperities
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/101/1/147/2199062/101-1-147.pdf
Reference48 articles.
1. Characterization of barriers on an earthquake fault;Aki;J. geophys. Res.,1979
2. Viscoelastic stress relaxation on deep fault sections as a possible source of very long period elastic waves;Bonafede;J. geophys. Res.,1983
3. Quasi-static crack models and the frictional stress threshold criterion for slip arrest;Bonafede;Geophys. J. R. astr. Soc.,1985
4. Stick-slip as a mechanism for earthquakes;Brace;Science,1966
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1. Effect of fault heterogeneity on rupture dynamics: An experimental approach using ultrafast ultrasonic imaging;Journal of Geophysical Research: Solid Earth;2013-11
2. Three-dimensional characterization of a crustal-scale fault zone: The Pusteria and Sprechenstein fault system (Eastern Alps);Journal of Structural Geology;2010-12
3. Coupling of tectonic loading and earthquake fault slips at subduction zones;Pure and Applied Geophysics PAGEOPH;1995
4. Coupling of Tectonic Loading and Earthquake Fault Slips at Subduction Zones;Mechanics Problems in Geodynamics Part I;1995
5. Propagation of an aseismic dislocation through asperities with smooth borders;Physics of the Earth and Planetary Interiors;1993-10
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