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Published in 2017 at "Journal of Geophysical Research"
DOI: 10.1002/2017jb014558
Abstract: Many researchers have analyzed seismic attenuation and velocity dispersion due to wave-induced fluid flow (WIFF) related to the presence of fluid-saturated fractures embedded in an isotropic porous background. Most fractured formations do, however, exhibit some…
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Keywords:
seismic attenuation;
background;
background anisotropy;
intrinsic background ... See more keywords