Affiliation:
1. Institute of Technology Saint Louis University St. Louis, Missouri
Abstract
abstract
The surface motion arising from a plane dilatational wave striking the base of a layered system is obtained by Fourier synthesis using the frequency dependent transmission coefficients which may be computed by the Haskell-Thomson matrix method. Theoretical seismograms illustrating the effect of thin, low-velocity surface layers on the surface motion are constructed from the transmission coefficients of four crustal models.
Publisher
Seismological Society of America (SSA)
Subject
Geochemistry and Petrology,Geophysics
Cited by
11 articles.
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1. Lake Superior seismic experiment: Frequency spectra and absorption1;The Earth Beneath the Continents;2013-04-03
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3. On the rotational components of seismic motion;Earthquake Engineering & Structural Dynamics;1989-08
4. Bibliography;Developments in Solid Earth Geophysics;1979
5. References;Spectral Analysis in Geophysics;1974