1887
ASEG2004 - 17th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

We present a deterministic methodology for mapping the lithology, pore fluid, and porosity from seismic data. The input is the P- and S-wave data volumes that may come, e.g., from acoustic and elastic impedance inversion or cross-well measurements. The output is the pore fluid type (hydrocarbon versus water), total porosity, and clay content. The key element of this methodology is a site-specific rock physics model that provides the needed transforms from the elastic rock properties to the reservoir properties. The model is established by comparing model-based predictions, such as impedance versus porosity, to the relations present in well log data. Once selected, the model is used to identify the presence of hydrocarbons from a combination of the P-wave impedance and Poisson’s ratio. Then the P-wave impedance is used to map porosity and clay content assuming that a deterministic relation exists between the latter two properties. All deterministic equations are calibrated at a well. These equations subsequently are applied to up-scaled well log data to confirm their validity at the seismic scale.

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/content/journals/10.1071/ASEG2004ab138
2004-12-01
2026-01-13
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References

  1. Avseth, P., Dvorkin, I, Mavko, G., and Rykkje, I, 2000, Rock physics diagnostic of North Sea sands: Link between micro structure and seismic properties: Geophysical Research Letters, 27, 2761-2764.
  2. Backus, G. E., 1962, Long-wave elastic anisotropy produced by horizontal layering: Journal of Geophysical Research, 67, 4427-1440.
  3. Castagna, J. P., Batzle, M. L., and Eastwood. R. L., 1985, Relationships between compressional-wave and shear-wave velocities in clastic silicate rocks: Geophysics, 50, 571-581.
  4. Dvorkin, J., and Gutierrez, M. A., 2002, Grain sorting, porosity and elasticity: Petrophysics, 43, 185-196.
  5. Dvorkin, J., and Nur., A, 1996, Elasticity of high-porosity sandstones: Theory for two North Sea datasets: Geophysics, 61,1363-1370.
  6. Gassmann, F., 1951, Uber die Elastizitat poroser Medien: Vier. DerNatur. Gesellschaft in Zurich, 96, 1-23.
  7. Greenberg, M. L., and Castagna, J. P., 1992, Shear-wave velocity estimation in porous rocks: Theoretical formulation, preliminary verification and applications: Geophysical Prospecting, 40, 195-209.
  8. Han, D. -H., 1986, Effects of Porosity and Clay Content on Acoustic properties of Sandstones and Unconsolidated Sediments: Ph.D. dissertation, Stanford University.
  9. Hill, R., 1952, The elastic behavior of crystalline aggregate: Proceedings of the Physical Society of London, A65, 349-372.
  10. Marion, D., 1990, Acoustical, mechanical, and transport properties of sediments and granular materials: Ph.D. thesis, Stanford University.
  11. Mavko, G., Chan, C, and Mukerji, T., 1995, Fluid substitution: Estimating changes in Vp without knowing Vs: Geophysics, 60, 1751-1755.
  12. Mavko G., Mukerji, T., and Dvorkin, J., 1998, The rock physics handbook, Tools for seismic analysis in porous media: Cambridge University Press.
  13. Nur, A., 1969, Effects of stress and fluid inclusions on wave propagation in rock: Ph.D. thesis, MIT.
  14. Raymer, D. S., Hunt, E. R., and Gardner, J. S., 1980, An improved sonic transit time-to-porosity transform, 21st Meeting, SPWLA, Paper P.
  15. Wyllie, M. R. J., Gregory. A. R., and Gardner, L. W., 1956, Elastic wave velocities in heterogeneous and porous media: Geophysics, 27, 569-589.
  16. Yin, H., 1992, Acoustic velocity and attenuation of rocks: Isotropy, intrinsic anisotropy, and stress induced anisotropy: Ph.D. thesis, Stanford University.
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  • Article Type: Research Article
Keyword(s): Characterization; Prediction; Rock Physics
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