This paper discusses several aspects of the calculation of theoretical seismograms for two-dimensional inhomogeneous media with the method of Gaussian beams. The most important steps of this method, kinematic and dynamic ray tracing, can be performed very efficiently, if the model cross-section is subdivided into triangles with linear velocity laws. Each Gaussian beam is characterized by a complex beam constant ∈ which determines its width and phase-front curvature. Various possibilities to choose ∈ are discussed, including cases where beam properties at the beam endpoint (and not at the beginning) are prescribed; for instance, the beam width at the endpoint can be specified. In such cases the beam constant is a function of the radiation angle at the source, and the decomposition of a cylindrical wave into beams has to take this into account by weighting the beams differently, at least in principle. The exact weight function is derived and shown to be reasonably well approximated by the weight function, corresponding to angle-independent ∈ Theoretical seismograms are presented for a laterally heterogeneous model of the crust—mantle transition which is characterized by complications in the reflection from the transition and in the refraction from below. These complications are modelled by and large with success. The seismograms, however, depend to a certain extent on the choice of the beam constant. Moreover, according to the reciprocity principle calculations with source and receiver interchanged should have the same results as calculations for the original configuration. In practice this is not so, and the difference increases with the strength of lateral heterogeneities. Hence, for a successful application of Gaussian beams the model should not vary too strongly in lateral direction.
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