Seismic attenuation due to wave-induced flow

Seismic attenuation due to wave-induced flow [electronic resource]

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Analytical expressions for three P-wave attenuation mechanisms in sedimentary rocks are given a unified theoretical framework. Two of the models concern wave-induced flow due to heterogeneity in the elastic moduli at mesoscopic scales (scales greater than grain sizes but smaller than wavelengths). I...

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Bibliographic Details
Online Access: Online Access
Corporate Author: Lawrence Berkeley National Laboratory (Researcher)
Format: Government Document Electronic eBook
Language:English
Published: Berkeley, Calif. : Oak Ridge, Tenn. : Lawrence Berkeley National Laboratory ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 2003.
Subjects:
Water.
Mixtures.
Grain Size.
Porosity.
Attenuation.
Sedimentary Rocks.
Wavelengths.
Lithology.
Clays.
Scale Models.
Air.
Geosciences.

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Holdings details from Online
Call Number: E 1.99:lbnl--53898
E 1.99:lbnl--53898 Available

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