Geodesic
Resonance waves in the media with nonwelded boundaries
Zapiski Nauchnykh Seminarov POMI, Mathematical problems in the theory of wave propagation. Part 37, Tome 354 (2008), pp. 150-156 Cet article a éte moissonné depuis la source Math-Net.Ru

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It is shown that in the layered media with weakened interfaces the resonance waves ($Kr$-waves) are arose. Such waves have the very characteristic frequencies and a lot of other cinematic and dynamic features distinguish them from the well-known Love and Rayleigh type waves. The comparison of the theoretical results with experimental seismic data indicates that $Kr$-waves can be formed in the real geological section. We show theoretically and numerically that in a sedimentary basin of finite lateral extent horizontal $Kr$-wave can be trapped and resonate. This wave has a number of interesting properties: wave spectrum has resonance frequency; wave group velocity is equal to an intermediate value between shear and longitudinal velocities; attenuation of wave increases when the frequency varies from the resonance value. Bibl. – 5 titles, fig. – 5. 
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     title = {Resonance waves in the media with nonwelded boundaries},
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A. P. Krauklis; P. V. Krauklis; A. V. Fat'yanov. Resonance waves in the media with nonwelded boundaries. Zapiski Nauchnykh Seminarov POMI, Mathematical problems in the theory of wave propagation. Part 37, Tome 354 (2008), pp. 150-156. http://geodesic.mathdoc.fr/item/ZNSL_2008_354_a6/

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