Dynamic-equivalent medium approach for thinly layered saturated sediments
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/128/1/F1/6070790/128-1-F1.pdf
Reference8 articles.
1. Mechanics of deformation and acoustic propagation in porous media;Biot;J. appl. Phys.,1962
2. The equivalence of quasi-static flow in fluid saturated porous media and Bid's slow wave in the limit of zero frequency;Chandler;J. appl. Phys.,1981
3. Velocity and attenuation of elastic waves in finely layered porous rocks;Gurevich;Geophys. J. Int.,1995
4. Seismic attenuation in finely-layered porous rock: Cumulative effect of fluid flow and scattering, in 65th Ann;Gurevich;Int. Mtg, Soc. Expl. Geophys., Extended Abstracts,1995
5. Low-frequency dispersion and attenuation in partially saturated rocks;Norris;J. acoust. Soc. Am.,1993
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