Radiation of surface Stoneley waves by distributed force sources acting at the solid earth-atmosphere interface

Using the Fourier transform, we find an integral solution describing the excitation of seismoacoustic waves in the solid Earth and the atmosphere by time-dependent forces arbitrarily distributed over the interface between the media. The solid Earth and the atmosphere are modeled by an isotropic soli...

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Veröffentlicht in:	Radiophysics and quantum electronics 2007-07, Vol.50 (7), p.570-582
1. Verfasser:	Razin, A V
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmosphere Atmospheres Classification Earth Excitation Force distribution Fourier transforms Half spaces Mathematical models Solids Stress concentration Time dependence Wave power
Online-Zugang:	Volltext
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