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oa Inverting the head wave coefficient with multi-fold near-surface seismic refraction data
- Australian Society of Exploration Geophysicists
- Source: ASEG Extended Abstracts, Volume 2019, Issue 2nd Australasian Exploration Geoscience Conference: Data to Discovery, Dec 2019, p. 1 - 4
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- 01 Dec 2019
Abstract
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.