Seismic wave attenuation and dispersion resulting from wave-induced flow in porous rocks - A review
One major cause of elastic wave attenuation in heterogeneous porous media is wave-induced flow of the pore fluid between heterogeneities of various scales. It is believed that for frequencies below 1 kHz, the most important cause is the wave-induced flow between mesoscopic inhomogeneities, which are...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Society of Exploration Geophysics
2010
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| Online Access: | http://hdl.handle.net/20.500.11937/35921 |