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oa Computing 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
Summary
Head wave amplitudes are dominated by an extremely rapid decrease with increasing source-to-receiver separation. Nevertheless, the standard corrections for geometric spreading are usually quite adequate and are not critical with multi-fold reversed refraction data.
The head wave coefficients (HWC), which are the refraction analogue of the reflection coefficients, are essentially equivalent at coincident sources and receivers. It supports a 2D revision of the standard 1D head wave expression. HWCs can be readily computed with a variety of methods using both the measured head wave amplitudes and full waveform refraction images.
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