On optimal NMO and generalised Dix equations for velocity determination and depth conversion
he classical Earth model used to process seismic data assumes plane layers and a velocity analysis based on a hyperbolic approximation of the reflection events, where basically one parameter (the stacking velocity) is used to perform the normal move-out (NMO) correction to obtain the stacked sect...
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| Format: | Article |
| Published: |
2014
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| Subjects: | |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S092698511300284X http://eprints.utp.edu.my/12191/ |
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| Summary: | he classical Earth model used to process seismic data assumes plane layers and
a velocity analysis based on a hyperbolic approximation of the reflection events, where
basically one parameter (the stacking velocity) is used to perform the normal move-out
(NMO) correction to obtain the stacked section. |
|---|