1887

Abstract

The technique of obtained synthetic gathers using time section traces is explained. Based on these traces, stacking velocities were calculated into interval velocities. Generating depth-velocity models for depth migration when initial seismograms are absent as well as a possibility of re-processing of synthetic gathers with the purpose of enhancing seismic record resolution are considered.

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/content/papers/10.3997/2214-4609-pdb.38.F301
2003-09-01
2020-10-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.38.F301
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