When considering spatially inhomogeneous media with smooth variability, it is natural to admit local anisotropy – a non-spherical indicatrix – in place of a more restrictive assumption of isotropy. On that basis, ray dynamics and the eikonal equation that govern geometric optics (and geometric acoustics) in inhomogeneous media are formulated to take into account the dependence of local propagation velocity on the direction of the ray. All the equations reduce to classical forms when anisotropy vanishes.
Summary. The limitations of asymptotic wave theory and its geometrical manifestations are newly form...
In this report the equations for acoustic ray trajectories are derived using Fermat’s prin-ciple. Fi...
Elliptical anisotropy may be considered a more general case of isotropy, in which the medium has bee...
Karal and Keller [1] developed the geometrical acoustics for wave propagation in a heterogeneous iso...
Karal and Keller [1] developed the geometrical acoustics for wave propagation in a heterogeneous iso...
Ray theory is developed for elastic waves propagating in inhomogeneously oriented anisotropic solids...
The present investigation is concerned with the propagation of inhomogeneous plaine waves in anisotr...
The combined effects of acoustic nonlinearity and diffraction on the propagation of intense acoustic...
The first motion approximation has been used to calculate synthetic seisnograms in transversely isot...
International audienceWe propose approximate equations for P-wave ray theory Green's function for sm...
We derive equations describing the path and traveltime of a coherent elastic wave propagating in an ...
In the geometric optics approximation for inhomogeneous, nonstationary, anisotropic and dispersive m...
Summary. The most complicated part in the computation of ray amplitudes of seismic body waves in lat...
Conditions on the elastic stiffnesses of anisotropic crystals are derived such that circularly polar...
The relative geometric spreading along the raypath contributes to the amplitude decay of the seismic...
Summary. The limitations of asymptotic wave theory and its geometrical manifestations are newly form...
In this report the equations for acoustic ray trajectories are derived using Fermat’s prin-ciple. Fi...
Elliptical anisotropy may be considered a more general case of isotropy, in which the medium has bee...
Karal and Keller [1] developed the geometrical acoustics for wave propagation in a heterogeneous iso...
Karal and Keller [1] developed the geometrical acoustics for wave propagation in a heterogeneous iso...
Ray theory is developed for elastic waves propagating in inhomogeneously oriented anisotropic solids...
The present investigation is concerned with the propagation of inhomogeneous plaine waves in anisotr...
The combined effects of acoustic nonlinearity and diffraction on the propagation of intense acoustic...
The first motion approximation has been used to calculate synthetic seisnograms in transversely isot...
International audienceWe propose approximate equations for P-wave ray theory Green's function for sm...
We derive equations describing the path and traveltime of a coherent elastic wave propagating in an ...
In the geometric optics approximation for inhomogeneous, nonstationary, anisotropic and dispersive m...
Summary. The most complicated part in the computation of ray amplitudes of seismic body waves in lat...
Conditions on the elastic stiffnesses of anisotropic crystals are derived such that circularly polar...
The relative geometric spreading along the raypath contributes to the amplitude decay of the seismic...
Summary. The limitations of asymptotic wave theory and its geometrical manifestations are newly form...
In this report the equations for acoustic ray trajectories are derived using Fermat’s prin-ciple. Fi...
Elliptical anisotropy may be considered a more general case of isotropy, in which the medium has bee...