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THE IMPORTANCE OF LOCALLY CONVERTED WAVES ON THE ELASTIC INVERSION OF COMPRESSIONAL DATA

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Figure 1 – Four-layer model: a water layer and a sedimentary section composed of a 50 m sandstone encased in shales.
Figure 3 – Seismic events propagating through a thin layer: a) only primary P waves; b) P S wave originated at the base of thin layer; c) P S wave originated at top of thin layer and SS reflection at the base; d) P waves through thin layer
Figure 4 – Seismic events reflecting at the bottom of sandstone in Figure 1 in the τ − p domain
Figure 6 – Reference data; data from complete response inversion model; and data residuals for the 50 m sandstone model.
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