Titlebook: Seismic Love Waves; Z. S. Andrianova,A. L. Levshin,M. G. Neigauz Book 1967 Consultants Bureau 1967 Storm.energy.seismic

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Book 1967placements of particles in Rayleigh waves are parallel, and the displacements in Love waves perpendicular, to the vertical plane containing the direction of propagation (some variation from this polarization is possible close to the source or in the presence of horizontal inhomogeneities in the medi

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,Love Waves in the Earth’s Crust,ropagated mainly in the earth’s crust and in which they practically never penetrate into the mantle (i.e., their phase velocities are lower than the velocities of transverse waves in the mantle — see pp. 20–21).

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e usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished by their dispersion and reso- nance, and are used in many investigations - in the determination of the structure of the medium (the existen

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