引文
Aki, K., and Richards, P. G., 1980, Quantitative seismology:W. H. Freeman & Co.
Biot, M. A., 1956a, Theory of propagation of elastic wavesin a fluid saturated porous solid - I: low frequency range:J. Acoust. Soc. Am., 28, 168 – 178.
Biot, M. A., 1956b, Theory of propagation of elastic wavesin a fluid saturated porous solid - II: high frequencyrange: J. Acoust. Soc. Am., 28, 179 – 191.
Biot, M. A., 1962, Generalized theory of acoustic propagation in porous dissipative media: J. Acoust. Soc.Am., 34, 1254 – 1264.
Castagna, J. P., 1993, Petrophysical imaging using AVO:The Leading Edge, 12, 172 – 178.
Castagna, J. P., Sun, S. and Seigfried, R.W., 2003,Instantaneous spectral analysis: Detection of low-frequency shadows associated with hydrocarbons: TheLeading Edge, 22, 120 – 127.
Chapman, M., Zatsepin, S. V., and Crampin, S., 2002,Derivation of a microstructural poroelasticity model:Geophys. J. Int., 151, 427 – 451.
Chapman, M., 2003, Frequency dependent anisotropydue to meso-scale fractures in the presence of equantporosity: Geophysical Prospecting, 51, 369 – 379.
Chapman, M., Liu, E., and Li, X. Y., 2005, The influence of abnormally high reservoir attenuation on the AVOsignature: The Leading Edge, 24, 1120 – 1125.
Chapman, M., Liu, E., and Li, X. Y., 2006, The influence of fluid-sensitive dispersion and attenuation on AVOanalysis: Geophys. J. Int., 167, 89 – 105.
Ebrom, D., 2004, The low-frequency gas shadow onseismic sections: The Leading Edge, 23, 772.
Gassmann, F., 1951, über die Elastizit t poroser Medien:Veirteljahrsschrift der Naturforschenden Gesellschaft inZürich, 96, 1 – 23.
Goloshubin, G., and Schuyver, C. V., 2006, Reservoirimaging using low frequencies of seismic reflections:The Leading Edge, 25, 527 – 531.
Kan, T. K., Batzle, M. L., and Gaiser, J. E., 1983,Attenuation measured from VSP: Evidence of frequency-dependent Q: 53rd Ann. Internat. Mtg., Soc. Explor.Geophys., Expanded Abstracts, 589 – 590.
Korneev, V., Goloshubin, G., Daley, T., and Silin, D., 2004,Seismic low-frequency effects in monitoring fluid-saturated reservoirs: Geophysics, 69, 522 – 532.
Liu, E., and Chapman, M., 2006, Comparison of spectral decomposition techniques for evaluating frequency-dependent variations in seismic data: EdinburghAnisotropy Project Annual Report, Section C: Frequency-dependent anisotropy.
Mavko , G., and Nur, A., 1975, Melt squirt in the asthenosphere: J. Geophys. Res., 80, 1444 – 1448.
Murphy, W. F., 1984, Acoustic measures of partial gassaturation in tight sandstones: J. Geophys. Res., 89,11549 – 11559.
Odebeatu, E., Zhang, J., Chapman, M., Liu, E., and Li, X. Y.,2006, Application of spectral decomposition to detectionof dispersion anomalies associated with gas saturation:The Leading Edge, 25, 206 – 210.
Partyka, G., Gridley, J., and Lopez, J., 1999, Interpretationalapplications of spectral decomposition in reservoircharacterization: The Leading Edge, 18, 353 – 360.
Swan, H., 1991, Amplitude-versus-offset measure menterrors in a finely layered medium: Geophysics, 56, 41 –49.
Taner, M. T., Koehler, F., and Sheriff, R. E., 1979, Complexseismic trace analysis: Geophysics, 44, 1041 – 1063.
Wu, X., and Liu, T., 2009, Time-frequency analysis on Wigner-Ville distribution of seismic signal basedon time-frequency rearrangement: Oil GeophysicalProspecting, 44(2), 201 – 205.
Zhao, B., Johnston, D., and Gouvela, W., 2006, Spectralde composition of 4D seismic data: 76th Ann. Internat.Mtg., Soc. Expl. Geophys., Expanded Abstracts, 3235 –3239.