Add to ORKGWe developed computer codes to synthesize seismograms near a finite fault system with the discrete wave-number method. Besides we synthesized seismograms in two dimensional space, formulations in three dimension are also provided. The discrete wave-number method which regarded circular wave from epicenter as a sum of plane waves propagating any direction is useful in introducing a rectangular fault source and a stratified medium. 1
Broadband synthetic time histories for central and eastern United States are generated using a propo...
The kinematical finite source is considered as stacking of dynamic point sources based on the dynami...
In asymptotic ray theory, the solution for particle motion is assumed to be an infinite power series...
This code package of discrete wavenumber method for synthesizing complete seismogram is implemented ...
A new discrete wave-number technique for synthetic seismogram calculation is proposed for the case o...
The accuracy of the finite-difference method for generating synthetic seismo-grams of SH wave propag...
Multiple methods exist for modeling with synthetic seismograms, each with its own characteristic app...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
A three dimensional, second order finite difference method was used to create synthetic seismograms...
A finite-difference algorithm is used to generate synthetic seismograms for waves propagating throug...
International audienceA semi-analytical, semi-numerical method of seismogram synthesis is presented ...
Abstract In this paper, numerical computations are carried out to investigate the seismo-electromagn...
Synthetic seismograms are a computer-generated aid in the search for hydrocarbons. Heretofore the so...
Summary. A numerically efficient global matrix approach t o the solution of the wave equation in hor...
Summary. We present a new method to calculate the SH wavefield produced by a seismic source in a hal...
Broadband synthetic time histories for central and eastern United States are generated using a propo...
The kinematical finite source is considered as stacking of dynamic point sources based on the dynami...
In asymptotic ray theory, the solution for particle motion is assumed to be an infinite power series...
This code package of discrete wavenumber method for synthesizing complete seismogram is implemented ...
A new discrete wave-number technique for synthetic seismogram calculation is proposed for the case o...
The accuracy of the finite-difference method for generating synthetic seismo-grams of SH wave propag...
Multiple methods exist for modeling with synthetic seismograms, each with its own characteristic app...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
A three dimensional, second order finite difference method was used to create synthetic seismograms...
A finite-difference algorithm is used to generate synthetic seismograms for waves propagating throug...
International audienceA semi-analytical, semi-numerical method of seismogram synthesis is presented ...
Abstract In this paper, numerical computations are carried out to investigate the seismo-electromagn...
Synthetic seismograms are a computer-generated aid in the search for hydrocarbons. Heretofore the so...
Summary. A numerically efficient global matrix approach t o the solution of the wave equation in hor...
Summary. We present a new method to calculate the SH wavefield produced by a seismic source in a hal...
Broadband synthetic time histories for central and eastern United States are generated using a propo...
The kinematical finite source is considered as stacking of dynamic point sources based on the dynami...
In asymptotic ray theory, the solution for particle motion is assumed to be an infinite power series...