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File:Vol6 Page 028 Image 0001.png
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Rays with different overburden in 3D azimuths. When seismic lines are shot in different directions, the seismic traces may not be identical, even for common reflection points, because of the different overburden encountered. This figure shows two different source-receiver lines with a common reflection point. The reflection characteristics of the horizon observed from a survey shot in one direction may be different from those observed from a survey oriented in a different direction.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:11, 12 December 2012 | | 1,650 × 1,116 (572 KB) | Glenda Smith (Glendasmith) (talk | contribs) | Rays with different overburden in 3D azimuths. When seismic lines are shot in different directions, the seismic traces may not be identical, even for common reflection points, because of the different overburden encountered. This figure shows two diffe... |
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