Abstract
This is shown in diagrammatic form in Figure 9.1. Since we are considering only one homogeneous layer, of constant velocity V, between the surface and the inclined reflecting surface, the usual distinctions between average velocity, root mean square velocity and interval velocity do not arise in this case.
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© 1985 Springer Science+Business Media Dordrecht
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Cordier, JP. (1985). Investigation of the Influence of Dip on Velocity Analyses. In: Velocities in Reflection Seismology. Seismology and Exploration Geophysics, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3641-1_9
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DOI: https://doi.org/10.1007/978-94-017-3641-1_9
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-8416-3
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