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GEOPHYSICS RESEARCH DIRECTORATE AIR FORCE CAMBRIDGE RESEARCH CENTER
Abstract
A matrix formalism developed by W. T. Thomson is used to obtain the phase velocity dispersion equations for elastic surface waves of Rayleigh and Love type on multilayered solid media. The method is used to compute phase and group velocities of Rayleigh waves for two assumed three-layer models and one two-layer model of the earth's crust in the continents. The computed group velocity curves are compared with published values of the group velocities at various frequencies of Rayleigh waves over continental paths. The scatter of the observed values is larger than the difference between the three computed curves. It is believed that not all of this scatter is due to observational errors, but probably represents a real horizontal heterogeneity of the continental crusts.
Footnotes
* Manuscript received for publication June 5, 1951.
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F. SCHWAB and L. KNOPOFF Love waves and the torsional free modes of a multilayered anelastic sphere Bulletin of the Seismological Society of America, June 1, 1973; 63(3): 1107 - 1117. [Abstract] [PDF]
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R. P. MASSE, D. G. LAMBERT, and D. G. HARKRIDER Precision of the determination of focal depth from the spectral ratio of Love/Rayleigh surface waves Bulletin of the Seismological Society of America, February 1, 1973; 63(1): 59 - 100. [Abstract] [PDF]
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L. A. DRAKE Rayleigh waves at a continental boundary by the finite element method Bulletin of the Seismological Society of America, October 1, 1972; 62(5): 1259 - 1268. [Abstract] [PDF]
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R. M. LASTRICO, C. M. DUKE, and Y. OHTA Effects of site and propagation path on recorded strong earthquake motions Bulletin of the Seismological Society of America, August 1, 1972; 62(4): 933 - 954. [Abstract] [PDF]
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