By J. Fertig, P. Krajewski (auth.), R. Marschall (eds.)
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Extra info for Aspects of Seismic Reflection Data Processing
The model for computing the actual data examples is introduced in the next section. R. Germany. In the following section, the synthetic common shot gathers for line sources are shown, representing the measured data, followed by a section showing the gathers after PIS-wave separation. In the last section, the transient plane-wave seismograms are shown, representing the plane-wave decomposed PIS separated gathers, being the input data to a future inversion algorithm. All synthetic material, even the gathers simulating results from processing steps, are computed directly from the model parameters and not via the related processing steps from the common shot gathers.
Cross-line horizontal component seismogram for the elastic model due to a SH-wave line sourcc with strong SH-SH reflection events labelled 5 and 6. -G. 3 Ii ~ \. 2 ~ 0 10 20 30 40 :0 :0 0 0 90 ? 0 Fig. 7. Vertical component seismogram for the elastic model due to SV-wave line source with strong SV-SV reflection events labelled 5 and 7 and a strong SV-P reflection event labelled 6. 0 Fig. 8. In-line horizontal component seismogram for the elastic model due to a SV-wave line source with strong SV-SV reflection events labelled 5 and 7.
Another big advantage of the prestack depth-migration is a good velocity control for migration: after resorting to common midpoint (CMP) gathers, the PS reflections can be stacked coherently at their correct depth position, provided the 128 o au.. J. FERTIG AND P. 500 2. 500 3. 000 Fig. 17. Common Conversion Point (CCP) Stack of inline horizontal component of converted PSwaves. , I ' I ,I ~ 20 I I I I I I 10 I' I, I ,I, "I I o I, I' ,1"1" I, I 9 40 30 I I I I I 2740 II II II II II I I I I I I \ I I 11'1 I I I I' I !
Aspects of Seismic Reflection Data Processing by J. Fertig, P. Krajewski (auth.), R. Marschall (eds.)