Abstract
We consider theoretical seismographs of a wave field passing through an elastic layer with high propagation velocity. We note the presence of a low-frequency part of the seismogram for longitudinal waves. It is shown that the propagation time of low-frequency vibrations is equal to that of longitudinal disturbances screened by the layer.
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Translated from Zapiski Nauchnykh Seminarov Leningradskogo Otdeleniya Matematicheskogo Instituta im. V. A. Steklova, AN SSSR, Vol. 173, pp. 134–141, 1988.
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Smirnova, N.S. Wave propagation through a high-velocity elastic layer. J Math Sci 55, 1741–1746 (1991). https://doi.org/10.1007/BF01098213
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DOI: https://doi.org/10.1007/BF01098213