Summary. We present a new method to calculate the SH wavefield produced by a seismic source in a half-space with an irregular buried interface. The diffractiog interface is represented by a distribution of body forces. The Green’s functions needed to solve the boundary conditions are evaluated using the discrete wavenumber method. Our approach relies on the introduc-tion of a periodicity in the source-medium configuration and on the discreti-zation of the interface at regular spacing. The technique developed is applicable to boundaries of arbitrary shapes and is valid at all frequencies. Some examples of calculation in simple configurations are presented showing the capabilities of the method. Key words: seismology, synthetic seismograms, d...
The purpose of the work presented in the paper, is to compute the response of transversely isotropic...
We developed computer codes to synthesize seismograms near a finite fault system with the discrete w...
Summary. For a buried source in a stratified elastic half space, the surface displacements are calcu...
A new discrete wave-number technique for synthetic seismogram calculation is proposed for the case o...
International audienceWe present a method which combines boundary‐integral equation techniques with ...
The accuracy of the finite-difference method for generating synthetic seismo-grams of SH wave propag...
International audienceA semi-analytical, semi-numerical method of seismogram synthesis is presented ...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
International audienceCompressional (P) and shear (S) wave diffraction by free‐surface topography pl...
The finite-difference method is applied to compute the seismic response of 2-D in-homogeneous struct...
Restricted until 11 Dec. 2009.Seismic response of local sites is a significant problem that has been...
Summary. A numerically efficient global matrix approach t o the solution of the wave equation in hor...
This code package of discrete wavenumber method for synthesizing complete seismogram is implemented ...
We present a new method for calculating dynamic and static displacements arising from a buried point...
Expressions for displacements on the surface of a layered half-space due to point force are given in...
The purpose of the work presented in the paper, is to compute the response of transversely isotropic...
We developed computer codes to synthesize seismograms near a finite fault system with the discrete w...
Summary. For a buried source in a stratified elastic half space, the surface displacements are calcu...
A new discrete wave-number technique for synthetic seismogram calculation is proposed for the case o...
International audienceWe present a method which combines boundary‐integral equation techniques with ...
The accuracy of the finite-difference method for generating synthetic seismo-grams of SH wave propag...
International audienceA semi-analytical, semi-numerical method of seismogram synthesis is presented ...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
International audienceCompressional (P) and shear (S) wave diffraction by free‐surface topography pl...
The finite-difference method is applied to compute the seismic response of 2-D in-homogeneous struct...
Restricted until 11 Dec. 2009.Seismic response of local sites is a significant problem that has been...
Summary. A numerically efficient global matrix approach t o the solution of the wave equation in hor...
This code package of discrete wavenumber method for synthesizing complete seismogram is implemented ...
We present a new method for calculating dynamic and static displacements arising from a buried point...
Expressions for displacements on the surface of a layered half-space due to point force are given in...
The purpose of the work presented in the paper, is to compute the response of transversely isotropic...
We developed computer codes to synthesize seismograms near a finite fault system with the discrete w...
Summary. For a buried source in a stratified elastic half space, the surface displacements are calcu...