1887
2nd Australasian Exploration Geoscience Conference: Data to Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

The head wave coefficient (HWC), the refraction analogue of the reflection coefficient, is a complex function of the densities and the P- and S-wave velocities in both the weathered and sub-weathered regions. In general, the HWC increases with increasing P- and S-wave velocities in the weathered layer, but it decreases with increasing P- and S-wave seismic velocities in the sub-weathered layer.

Unscaled S-wave velocities in the weathered and sub-weathered regions can be computed with the HWCs for each interface and the detailed P-wave seismic velocities in each layer, using various approximations for the HWC. In general, there is excellent agreement between the measured and computed HWCs. However, some form of traveltime-based estimate of the S-wave velocities is required to calibrate the amplitude-based estimates.

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/content/journals/10.1080/22020586.2019.12072941
2019-12-01
2026-01-25
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References

  1. Červený, V., Ravindra, R., 1971, Theory of seismic head waves, Toronto, University of Toronto Press.
  2. Cox, M. J. G., 1999, Static corrections for seismic reflection surveys. Society of Exploration Geophysicists, Tulsa.
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  4. Meulenbroek, A. M., 2016. Inversion of seismic refraction amplitudes for near-surface velocity control. M Ph thesis, Univ. of Queensland, 313p.
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  8. Sheriff, R. E., and Geldart, L. P., 1995, Exploration seismology: Cambridge Univ. Press.
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/content/journals/10.1080/22020586.2019.12072941
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  • Article Type: Research Article
Keyword(s): amplitudes; head wave coefficient; inversion; refraction; S-wave velocities
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