Ray tracing computations in the smoothed SEG/EAGE Salt Model. Part 2: Sources in the well

Vaclav Bucha

Summary

Two-point rays of refracted and reflected P-waves in the smoothed SEG/EAGE Salt Model are computed for two sources situated in a well. The source-receiver configuration is derived from the original SEG/EAGE Phase A Acquisition. One profile is used for generation of the ray-theory seismograms.

Keywords

Velocity model, ray tracing, seismic waves, synthetic seismograms, well

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In: Seismic Waves in Complex 3-D Structures, Report 14, pp. 27-34, Dep. Geophys., Charles Univ., Prague, 2004.
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