A hybrid boundary integral equation method for the computation of source time functions for 3-D rupture propagation
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/96/1/163/1615984/96-1-163.pdf
Reference16 articles.
1. Fault impedance and earthquake energy in the Fourier transform domain;Andrews;Bull. seism. Soc. Am.,1980
2. 3-D numerical simulations of dynamic faulting in a half space;Archuleta;Bull. seism. Soc. Am.,1978
3. Tectonic stress and the spectra of seismic shear-waves from earthquakes;Brune;J. geophys. Res.,1970
4. Admissible speeds for plane strain self-similar shear-cracks with friction but lacking cohesion;Burridge;Geophys. J. R. astr. Soc.,1973
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3. Parameters for Earthquake Rupture Dynamics;Zisin (Journal of the Seismological Society of Japan. 2nd ser.);2009
4. A Pseudo-Dynamic Approximation to Dynamic Rupture Models for Strong Ground Motion Prediction;Bulletin of the Seismological Society of America;2004-12-01
5. Strong Ground-Motion Prediction from Stochastic-Dynamic Source Models;Bulletin of the Seismological Society of America;2003-02-01
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