Methods for the calculation of rays and geometrical spreading of seismic body waves propagating in laterally inhomogeneous media with curved interfaces are suggested. Seismic rays and geometric spreading are des-cribed by a system of ordinary differential equations of the first order. When the ray impinges on an interface, certain quantities of the above system change discontinuously. The initial conditions for these quantities at the interface are derived. Once the geometrical spreading has been determined the computation of ray amplitudes is easy. 1
Seismic wave propagation in laterally heterogeneous anelastic media: Theory and applications to seis...
The interpretation of refraction profiles that traverse laterally varying velocity structures has be...
Earth's heterogeneity near the surface is so severe that surface waves with period 20 s exhibit...
Summary. The most complicated part in the computation of ray amplitudes of seismic body waves in lat...
Boundary conditions are derived for numerical wave simulations that minimize artificial reflections ...
Simulation of wave propagation processes in inhomogeneous media is based on kinematic and dynamic pr...
International audienceWe present a method which combines boundary‐integral equation techniques with ...
The sensitivity of ray and beam theoretical seismograms to changes in velocity models and curved int...
Many situations of practical interest involving seismic wave modelling require curved interfaces and...
The report reviews interdisciplinary problem relevant to the search method hydrocarbon a low-frequen...
This chapter serves as an introduction to seismic wave propagation for those waves commonly observed...
The principle of constructive ray interference is used to derive the dispersion equation for SH-wave...
In this thesis we study wave propagation in inhomogeneous media. Examples of the classical (massless...
In this paper, the main principles of seismic ray theory for isotropic and anisotropic inhomogeneous...
The ray method is a useful tool for investigating the effects of anisotropy and inhomogeneity on the...
Seismic wave propagation in laterally heterogeneous anelastic media: Theory and applications to seis...
The interpretation of refraction profiles that traverse laterally varying velocity structures has be...
Earth's heterogeneity near the surface is so severe that surface waves with period 20 s exhibit...
Summary. The most complicated part in the computation of ray amplitudes of seismic body waves in lat...
Boundary conditions are derived for numerical wave simulations that minimize artificial reflections ...
Simulation of wave propagation processes in inhomogeneous media is based on kinematic and dynamic pr...
International audienceWe present a method which combines boundary‐integral equation techniques with ...
The sensitivity of ray and beam theoretical seismograms to changes in velocity models and curved int...
Many situations of practical interest involving seismic wave modelling require curved interfaces and...
The report reviews interdisciplinary problem relevant to the search method hydrocarbon a low-frequen...
This chapter serves as an introduction to seismic wave propagation for those waves commonly observed...
The principle of constructive ray interference is used to derive the dispersion equation for SH-wave...
In this thesis we study wave propagation in inhomogeneous media. Examples of the classical (massless...
In this paper, the main principles of seismic ray theory for isotropic and anisotropic inhomogeneous...
The ray method is a useful tool for investigating the effects of anisotropy and inhomogeneity on the...
Seismic wave propagation in laterally heterogeneous anelastic media: Theory and applications to seis...
The interpretation of refraction profiles that traverse laterally varying velocity structures has be...
Earth's heterogeneity near the surface is so severe that surface waves with period 20 s exhibit...