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f Resolution by migration after stack
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 54th EAEG Meeting, Jun 1992, cp-45-00261
- ISBN: 978-90-73781-04-7
Abstract
For smnplicity profile data is considered and the migrated section will be considered as a sampled function f(x,z) (x= coordinate along profile, z= depth) . In practice time (t= TWT) instead of depth (z) is more common, but this will be neglected as being a matter of "scaling" .