SEISMIC ATTENUATION FOR RESERVOIR CHARACTERIZATION.
In fully-saturated rock and at ultrasonic frequencies, the microscopic squirt flow induced between the stiff and soft parts of the pore space by an elastic wave is responsible for velocity-frequency dispersion and attenuation. In the seismic frequency range, it is the macroscopic cross-flow between...
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| Language: | English |
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Pittsburgh, Pa. ; Morgantown, W.Va. : Oak Ridge, Tenn. :
National Energy Technology Laboratory (U.S.) ; Distributed by the Office of Scientific and Technical Information, U.S. Department of Energy,
2002.
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| Physical Description: | 12 pages. |
| Format: | Electronic eBook |