SEG Technical Program Expanded Abstracts 2005 2005
DOI: 10.1190/1.2148258
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Tomostatics using deformable layer tomography

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“…Another cause of the problems is the presence of low-velocity zone, particularly in desert or loess areas. The loose alluvium, for instance, may have a P-wave velocity value 0.225-0.4 km=s which is slower than the speed of sound (Pralica, 2005). To remove the effects of the near surface and improve the quality of seismic data, we may define a reference datum surface, to which the wavefields are transformed as if they were acquired at this datum.…”
Section: Introductionmentioning
confidence: 99%
“…Another cause of the problems is the presence of low-velocity zone, particularly in desert or loess areas. The loose alluvium, for instance, may have a P-wave velocity value 0.225-0.4 km=s which is slower than the speed of sound (Pralica, 2005). To remove the effects of the near surface and improve the quality of seismic data, we may define a reference datum surface, to which the wavefields are transformed as if they were acquired at this datum.…”
Section: Introductionmentioning
confidence: 99%