Laboratory-based seismic attenuation in Fontainebleau sandstone: Evidence of squirt flow
Author:
Affiliation:
1. Department of Earth Sciences; ETH Zurich; Zurich Switzerland
2. Institute of Earth Sciences; University of Lausanne; Lausanne Switzerland
3. International Geothermal Centre and Ruhr Universität Bochum; Bochum Germany
Funder
Petrobras
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JB012290/fullpdf
Reference42 articles.
1. Fluid mobility and frequency-dependent seismic velocity-Direct measurements;Batzle;Geophysics,2006
2. The attenuation constant of Earth materials;Born;Geophysics,1941
3. Hydraulic and acoustic properties as a function of porosity in Fontainebleau sandstone;Bourbie;J. Geophys. Res.,1985
4. The influence of fluid-sensitive dispersion and attenuation on AVO analysis;Chapman;Geophys. J. Int.,2006
5. Squirt flow in fully saturated rocks;Dvorkin;Geophysics,1995
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