Acoustic and petrophysical relationships in low‐shale sandstone reservoir rocks

References

1. BestA.I. and McCannC.1995. Seismic attenuation and pore‐fluid viscosity in clay‐rich reservoir sandstones. Geophysics60, 1386–1397.
   [Google Scholar]
2. BestA.I., McCannC. and SothcottJ.1994. The relationships between the velocities, attenuations and petrophysical properties of reservoir sedimentary rocks. Geophysical Prospecting42, 151–178.
   [Google Scholar]
3. BiotM.A.1956a. Theory of propagation of elastic waves in a fluid‐saturated porous solid (I. Low frequency range). Journal of the Acoustical Society of America28, 168–178.
   [Google Scholar]
4. BiotM.A.1956b. Theory of propagation of elastic waves in a fluid‐saturated porous solid (II. Higher frequency range). Journal of the Acoustical Society of America28, 179–191.
   [Google Scholar]
5. CastagnaJ.P., BatzleM.L. and EastwoodR.L.1985. Relationships between compressional‐wave and shear‐wave velocities in clastic silicate rocks. Geophysics50, 571–581.
   [Google Scholar]
6. ChristensenN.I. and WangH.F.1985. The influence of pore pressure and confining pressure on dynamic elastic properties of Berea sandstone. Geophysics50, 207–213.
   [Google Scholar]
7. DomenicoS.N.1974. Effect of water saturation on seismic reflectivity of sand reservoirs encased in shale. Geophysics39, 759–769.
   [Google Scholar]
8. DomenicoS.N.1984. Rock lithology and porosity determination from shear and compressional wave velocity. Geophysics54, 76–81.
   [Google Scholar]
9. DvorkinJ., MavkoG. and NurA.1995. Squirt flow in fully saturated rocks. Geophysics60, 97–107.
   [Google Scholar]
10. Eberhart‐PhillipsD., HanD.H. and ZobackM.D.1989. Empirical relationships among seismic velocity, effective pressure, porosity, and clay content in sandstone. Geophysics54, 82–89.
    [Google Scholar]
11. GardnerG.H.F. and HarrisM.H.1968. Velocity and attenuation of the lunar interior. In: Lunar Science VII , pp. 181–183. Lunar Science Institute, Houston , TX .
    [Google Scholar]
12. GassmannF.1951. Über die Elastizität poröser Medien. Vierteljahrsschrift der Naturforschenden Gesellschaft in Zürich96, 1–23.
    [Google Scholar]
13. HanD., NurA. and MorganF.D.1986. Effects of porosity and clay content on wave velocities in sandstones. Geophysics51, 2093–2107.
    [Google Scholar]
14. JohnstonD.H. and ToksözM.N.1980. Ultrasonic P and S wave attenuation in dry and saturated rocks under pressure. Journal of Geophysical Research85, 925–936.
    [Google Scholar]
15. JonesS.M., McCannC., AstinT.R. and SothcottJ.1998. The effects of pore‐fluid salinity on ultrasonic wave propagation in sandstones. Geophysics63, 928–934.
    [Google Scholar]
16. KingM.S.1966. Wave velocities in rocks as a function of changes in overburden pressure and pore fluid saturates. Geophysics31, 50–73.
    [Google Scholar]
17. KlimentosT. and McCannC.1990. Relationships between compressional wave attenuation, porosity, clay content and permeability of sandstones. Geophysics55, 998–1014.
    [Google Scholar]
18. KlinkenbergL.J.1941. The permeability of porous media to liquids and gases. Drilling and Production Practice2, 200–213.
    [Google Scholar]
19. MavkoG.M. and NurA.1979. Wave attenuation in partially saturated rocks. Geophysics44, 161–178.
    [Google Scholar]
20. A.Hurst
    McCannC. and SothcottJ.1992. Techniques for the accurate measurement of the seismic properties of rocks in the laboratory. In: Geological Applications of Wireline Logging (eds A.Hurst , C.M.Griffiths and P.Worthington ), pp. 285–299. Geological Society , Bath. ISBN 09033178X.
    [Google Scholar]
21. MorrowC.A. and LocknerD.A.1994. Permeability differences between surface‐driven and deep drilled core samples. Geophysical Research Letters21, 2151–2154.
    [Google Scholar]
22. O'ConnellR.J. and BudianskyB.1977. Viscoelastic properties of fluid‐saturated cracked solids. Journal of Geophysical Research82, 5719–5736.
    [Google Scholar]
23. O'HaraS.G.1989. Elastic wave attenuation in fluid‐saturated Berea Sandstone. Geophysics54, 785–788.
    [Google Scholar]
24. PeacockS., McCannC., SothcottJ. and AstinT.R.1994. Seismic velocities in fractured rocks: an experimental verification of Hudson's theory. Geophysical Prospecting42, 27–80.
    [Google Scholar]
25. ShatiloA.P., SondergeldC. and RaiC.S.1998. Ultrasonic attenuation in Glen Pool rocks, north‐eastern Oklahoma. Geophysics63, 465–478.
    [Google Scholar]
26. TaoG., KingM.S. and Nabi‐BidhendiM.1995. Ultrasonic wave propagation in dry and brine‐saturated sandstones as a function of effective stress: laboratory measurements and modelling. Geophysical Prospecting43, 299–327.
    [Google Scholar]
27. TathamR.H.1982. VP/VS and lithology. Geophysics47, 336–344.
    [Google Scholar]
28. WangZ., BatzleM.L. and NurA.1990. Effect of different pore fluids on seismic velocities in rocks. Canadian Journal of Exploration Geophysics26, 104–112.
    [Google Scholar]
29. WangZ. and NurA.1990. Wave velocities in hydrocarbon‐saturated rocks: Experimental results. Geophysics55, 723–733.
    [Google Scholar]
30. WhiteJ.E.1986. Biot‐Gardner theory of extensional waves in porous rods. Geophysics51, 742–745.
    [Google Scholar]
31. WinklerK.W.1985. Dispersion analysis of velocity and attenuation in Berea sandstone. Journal of Geophysical Research90, 6793–6800.
    [Google Scholar]
32. WinklerK. and PlonaT.J.1982. Technique for measuring ultrasonic velocity and attenuation spectra in rocks under pressure. Journal of Geophysical Research87, 10776–10780.
    [Google Scholar]