Velocity‐depth ambiguity in the dipping reflector case
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Seismic or acoustic wave velocity is a vital parameter for processing and interpretation of seismic data. Various velocity analysis methods, using traveltime moveout of seismic events, have been described in literature. In certain cases, these methods provide ambiguous results. Hence, there is a need to investigate velocity‐depth ambiguity in such cases.
2010 ◽
Vol 75
(2)
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pp. 151-155
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2019 ◽
Vol 81
(3)
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pp. 223-234
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2002 ◽
pp. 335-347
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2013 ◽
Vol 20
(02)
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pp. 1350017
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