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The amplitude of a seismic refraction event is dependent on the properties of the rocks through which the seismic waves travel, the amplitude of the shot, and the offset at which the refraction is recorded. Separation and subsequent analysis of these 3 constituent amplitude terms can provide insight into the physical properties of the near-surface. A comparison between a published method of amplitude separation and a formal, non-linear, inversion scheme is presented using a Vibroseis dataset as the test case.
An assessment of the two methods shows that there is very good correlation for this dataset. Variations in the curves representing lateral changes in physical properties are consistent with each other along most of the extent of the line. The range of values for the non-linear inversion result is consistent with theoretical values for most near- surface geologies.
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