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Seismic attenuation due to wave induced fluid flow in heterogeneous reservoirsNormal access

Authors: T. M. Müller, J. Toms, R. Ciz and B. Gurevich
Event name: 67th EAGE Conference and Exhibition - Workshops
Session: WS 2: Seismic Q: Observations, Mechanisms and Interpretation
Publication date: 13 June 2005
DOI: 10.3997/2214-4609.201405178
Organisations: EAGE
Language: English
Info: Extended abstract, PDF ( 219.25Kb )
Price: € 20

Summary:
One major cause of the attenuation and dispersion of elastic waves in porous fluid-saturated rock is the wave-induced flow. It refers to the flow of fluid which occurs when a passing wave sets up localized pressure gradients between regions of rock having different compliances. This can occur when a rock contains heterogeneities in mineral grains, porosity, permeability, and/or saturating fluid.


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