1887
ASEG2001 - 15th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Multi-component OBC data relies on mode conversion from p-wave to s-wave in the subsurface to obtain information about the elastic properties of the earth. Since the energy converted to s-wave is now missing from the p-wave an alternative to recording OBC multi-component data is to examine p-wave data for the missing energy. Since the conversion is dependent upon the incident angle and occurs most at wider angles of incidence, long offset p-wave data is necessary for this technique.

A non-linear, wide angle (including post critical) AVO inversion has been developed that allows elastic properties to be extracted from long offset p-wave data. In order to extract amplitudes at long offsets for this inversion it is necessary to image the data correctly, including correcting for higher order moveout.

The higher order moveout may itself be inverted to yield additional information about the anisotropy of the subsurface.

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/content/journals/10.1071/ASEG2001ab148
2001-12-01
2026-01-23
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References

  1. Hawkins, K., Leggott, R., & Williams, R.G., 2000, P-wave VTI anisotropy measurements for long offset data: a case history from W. Africa, SEG Extended Abstracts
  2. Leggott, R., Cheadle, S., Whiting, P., and Williams, R.G., 2000, Analysis of higher order moveout in terms of vertical velocity variation and VTI anisotropy, ASEG meeting Perth
  3. MacLeod, M.K., Hanson, R.A., Bell, C.R. and McHugo, S., 1999, The Alba Field ocean bottom cable seismic survey: Impact on development, The Leading Edge, 18, 1306-1311.
  4. Roberts, G., 2000, Wide Angle AVO, EAGE Extended Abstracts
  5. Shuey, R. T., 1985, A simplification of the Zoeppritz equations, Geophysics, 50, 609-614
/content/journals/10.1071/ASEG2001ab148
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  • Article Type: Research Article
Keyword(s): Anisotropy; AVO; Long offset; OBC; Shear wave
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