## Computation of high-frequency seismic wavefileds
in 3-D laterally inhomogeneous anisotropic media

**Dirk Gajewski ** **&**
**Ivan Psencik **
### Summary

An algorithm for the computation of travel times, ray amplitudes
and ray synthetic seismograms in 3-D laterally inhomogeneous media
composed of isotropic and anisotropic layers is described. All 21
independent elastic parameters may vary within the anisotropic
layers. Rays and travel times are evaluated by numerical solution
of the ray tracing equations. Ray amplitudes are determined by
evaluating reflection/transmission coefficients and the geometrical
spreading along individual rays. The geometrical spreading is
computed approximately by numerical measurement of the cross-sectional
area of the ray tube formed by three neighbouring rays.
A similar approximate procedure is used for the determination of
coefficients of the paraxial approximation. The ray paraxial
approximation makes computation of synthetic seismograms on the
surface of the model very efficient. Examples of ray synthetic
seismograms computed with a program package based on the described
algorithm are presented.

*Geophys. J. R. astr. Soc.*, **91** (1987), 383-411.

SW3D
- main page of consortium ** Seismic Waves in Complex 3-D Structures **.