A hybrid boundary integral equation method for the computation of source time functions for 3-D rupture propagation

Author:

Quin H. R.,Das Shamita X.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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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1. Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domain;Journal of the Mechanics and Physics of Solids;2024-05

2. Spectral boundary integral method for simulating static and dynamic fields from a fault rupture in a poroelastodynamic solid;Geomechanics and Geophysics for Geo-Energy and Geo-Resources;2022-03-25

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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