Understanding and modeling seismic wave propagation is important in regional and exploration seismology. Ray tracing is a powerful and popular method for this purpose. Wavefront construction (WFC) method handles wavefronts instead of individual rays, thereby controlling proper ray density on the wavefront. By adaptively controlling rays over a wavefront, it efficiently models wave propagation. Algorithms for a quasi-P wave wavefront construction method and a new coordinate system used to generate wavefront construction mesh are proposed and tested for numerical properties and modeling capabilities. Traveltimes, amplitudes, and other parameters, which can be used for seismic imaging such as migrations and synthetic seismograms, are computed ...
For seismic imaging of complex 3-D structures by e.g. prestack Kirchhoff depth migration large amoun...
A study of two-point seismic-ray tracing problems in a heterogeneous isotropic medium and how to sol...
The physical world consists of spatially varying media, such as the atmosphere and the ocean, in whi...
Understanding and modeling seismic wave propagation is important in regional and exploration seismol...
The wavefront construction (WFC) method is an effective tool to compute seismic ray fields and has w...
We present a novel method which can perform the fast computation of the times of arrival of seismic ...
The research described in this thesis covers various aspects of the forward calculation of seismic r...
Ray tracing technique is an important tool not only to forward but also for inverse problems in Geop...
Two methods for tracing seismic rays between 2 given end points through three dimensional, continuou...
Wavefield travel time tomography is used for a variety of purposes in acoustics, geophysics and non-...
Ray methods have been used extensively in seismology and seis-ic exploration to study propagation of...
Wavelet estimation, ray tracing, and traveltime inversion are fundamental problems in seismic explo...
Wavefront construction (WF) ray tracing in tetrahedral models-Application to 3-D traveltime and ray ...
textRay theory plays an important role in seismic imaging and velocity model building. Although rays...
Acoustic rays do not travel in straight raypaths in nonhomogeneous media. This causes difficulty in ...
For seismic imaging of complex 3-D structures by e.g. prestack Kirchhoff depth migration large amoun...
A study of two-point seismic-ray tracing problems in a heterogeneous isotropic medium and how to sol...
The physical world consists of spatially varying media, such as the atmosphere and the ocean, in whi...
Understanding and modeling seismic wave propagation is important in regional and exploration seismol...
The wavefront construction (WFC) method is an effective tool to compute seismic ray fields and has w...
We present a novel method which can perform the fast computation of the times of arrival of seismic ...
The research described in this thesis covers various aspects of the forward calculation of seismic r...
Ray tracing technique is an important tool not only to forward but also for inverse problems in Geop...
Two methods for tracing seismic rays between 2 given end points through three dimensional, continuou...
Wavefield travel time tomography is used for a variety of purposes in acoustics, geophysics and non-...
Ray methods have been used extensively in seismology and seis-ic exploration to study propagation of...
Wavelet estimation, ray tracing, and traveltime inversion are fundamental problems in seismic explo...
Wavefront construction (WF) ray tracing in tetrahedral models-Application to 3-D traveltime and ray ...
textRay theory plays an important role in seismic imaging and velocity model building. Although rays...
Acoustic rays do not travel in straight raypaths in nonhomogeneous media. This causes difficulty in ...
For seismic imaging of complex 3-D structures by e.g. prestack Kirchhoff depth migration large amoun...
A study of two-point seismic-ray tracing problems in a heterogeneous isotropic medium and how to sol...
The physical world consists of spatially varying media, such as the atmosphere and the ocean, in whi...