On the seismic response of a periodic sequence of three thin layers saturated by two-phase fluids
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DOI: 10.1190/geo2020-0668.1
Abstract: The conversion of fast to slow diffusion P waves in fluid-saturated porous media induces attenuation and dispersion of waves at seismic frequencies. This effect, known as wave-induced fluid flow, occurs at mesoscopic scales, which are… read more here.
Keywords: phase; two phase; periodic sequence; thin layers ... See more keywords