Ray tracing computations in the smoothed SEG/EAGE Salt Model, Part 3: Maps of reflections

Vaclav Bucha


The paper presents computation of two-point rays of the P-wave reflected from the flat bottom interface in the smoothed SEG/EAGE Salt Model. Six shot-receiver configurations derived from the original Phase A Acquisition are used for generation of reflection point maps, colour coded according to amplitudes.


Velocity model, ray tracing, seismic waves, reflection maps

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In: Seismic Waves in Complex 3-D Structures, Report 14, pp. 35-42, Dep. Geophys., Charles Univ., Prague, 2004.
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