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Bulletin of the Seismological Society of America; April 1967; v. 57; no. 2; p. 191-198
© 1967 Seismological Society of America
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Body waves as normal and leaking modes. Part I: Introduction

J. CL. DE BREMAECKER

DEPARTMENT OF GEOLOGY RICE UNIVERSITY, HOUSTON, TEXAS

Abstract

Realistic artificial seismograms may be computed by considering body waves as sums of normal or leaking modes of surface waves: the S wave and those arriving after S may be considered as sums of higher normal modes of Rayleigh waves (RiN) and Love waves (LiN); in this case the apparent velocity c < ßn. Earlier arrivals are generally due to the first kind of leaking modes of Rayleigh waves (RiL1) for which ßn < c < {alpha}n. Deep reflections in seismic prospecting are RiL2 for which c > {alpha}n. Synthetic seismograms can be computed by double Fourier transformation in those two last cases. Alternately the method of residues followed by a single Fourier (or Laplace) transformation may be used in all cases. Earth-stretching approximations should give excellent results for SH waves and may give satisfactory results for P and SV waves.




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Bulletin of the Seismological Society of AmericaHome page
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Leaking modes in a crust with a surface layer
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