Characteristic frequencies of seismic attenuation due to wave-induced fluid flow in fractured porous media
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/166/2/574/1501850/166-2-574.pdf
Reference14 articles.
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2. A model for P-wave attenuation and dispersion in a porous medium permeated by aligned fractures;Brajanovski;Geophys. J. Int.,2005
3. The equivalence of quasistatic flow in fluid-saturated porous media and Biot's slow wave in the limit of zero frequency;Chandler;J. Appl. Phys.,1981
4. Dynamic poroelasticity of thinly layered structures;Gelinsky;Internat. J. Solids Structures.,1998
5. Attenuation of longitudinal waves in a saturated porous medium with random inhomogeneities;Gurevich;Doklady Earth Science Sections,1985
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