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...
| Main Author: | Ayman N Qadrouh, José M Carcione, Marco AB Botelho, Zuhar Zahir, . |
|---|---|
| Format: | Article |
| Institution: | Universiti Teknologi Petronas |
| Record Id / ISBN-0: | utp-eprints.12191 / |
| Published: |
2014
|
| Subjects: | |
| Online Access: |
http://www.sciencedirect.com/science/article/pii/S092698511300284X http://eprints.utp.edu.my/12191/ |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| 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. |
|---|