Structural inversion exercises
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Series | Investigations in Geophysics |
---|---|
Author | Öz Yilmaz |
DOI | http://dx.doi.org/10.1190/1.9781560801580 |
ISBN | ISBN 978-1-56080-094-1 |
Store | SEG Online Store |
Exercise 10-1. Does a zero-offset wavefield modeled from exploding reflectors contain multiples?
Exercise 10-2. Consider two image sections derived from (a) time migration, and (b) depth migration followed by scaling from depth to time. To perform the depth-to-time scaling, you may use an interval velocity field based on the rms velocity field to do the time migration or the velocity-depth model to do the depth migration. Which option would make the two image sections in time more compatible?
See also
- Introduction to structural inversion
- Subsalt imaging in the North Sea
- Subsalt imaging in the Gulf of Mexico
- Imaging beneath irregular water bottom in the Northwest Shelf of Australia
- Imaging beneath volcanics in the West of the Shetlands of the Atlantic Margin
- Imaging beneath shallow gas anomalies in the Gulf of Thailand
- 3-D structural inversion applied to seismic data from the Southern North Sea
- 3-D structural inversion applied to seismic data from the Central North Sea
- 3-D structural inversion applied to seismic data from offshore Indonesia
- 3-D structural inversion applied to seismic data from the Northeast China
- Seismic modeling