Seismic attenuation due to wave-induced fluid flow in a porous rock with spherical heterogeneities

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Seismic attenuation due to wave-induced fluid flow in a porous rock with spherical heterogeneities

Most natural porous rocks have heterogeneities at nearly all scales. Heterogeneities of mesoscopic scale that is, much larger than the pore size but much smaller than wavelength can cause significant attenuation and dispersion of elastic waves due to wave induced flow between more compliant and...

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Bibliographic Details
Main Authors:	Ciz, Radim, Gurevich, Boris, Markov, M.
Format:	Journal Article
Published:	Blackwells / Wiley 2006
Subjects:	attenuation scattering poroelastic media wave propagation Biot's slow wave
Online Access:	http://hdl.handle.net/20.500.11937/12745

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