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- Valeri A. Korneev
- Lawrence Berkeley National Laboratory 1 , Berkeley, California, . E-mail: vakorneev@lbl.gov .
書誌事項
- 公開日
- 2011-11-01
- DOI
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- 10.1190/geo2011-0086.1
- 公開者
- Society of Exploration Geophysicists
この論文をさがす
説明
<jats:title>ABSTRACT</jats:title> <jats:p>The Krauklis wave is a slow dispersive wave mode that propagates in a fluid layer bounded by elastic media. In a model of alternating fluid and elastic layers, two interface waves can exist at low frequencies: The first wave propagates mostly in the elastic layer and has little dispersion, while the second wave can have strong dispersion and propagates as a Krauklis wave for some parameter combinations. Analytical conditions predict appearance of the Krauklis wave for higher frequencies and low porosities. Interface-wave velocities depend on model porosity, which potentially can be used for fracture mapping.</jats:p>
収録刊行物
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- Geophysics
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Geophysics 76 (6), N47-N53, 2011-11-01
Society of Exploration Geophysicists
