Dictionary:Normal moveout (NMO)
The difference in reflection arrival time because the geophone is not located at the source point, i.e., because of source-to-geophone distance (offset). Usually applied to common-midpoint gathers, it is the additional traveltime required because of offset, assuming that the reflecting bed is not dipping and that raypaths are straight lines. This leads to a hyperbolic shape for a reflection. Because the raypath actually curves as the velocity changes, fitting a hyperbola assumes that the actual velocity distribution is equivalent to a constant NMO velocity, but the NMO velocity changes with the offset. However, the assumption often provides an adequate solution for offsets less than the reflector depth.
The NMO correction applied to long-offset data generally creates a ‘‘hockey-stick’’ effect giving long-offset traveltimes that are too small and causing waveshape broadening and loss of resolution. For long-offsets the reflection curvature becomes nonhyperbolic because of vertical changes in velocity and anisotropy and a nonhyperbolic normal-moveout analysis (q.v.) has to be used. Reflector dip also has effects that often require a DMO correction. The functions of the NMO and DMO operations are illustrated graphically in Figure D-20e.
- main page: Reflection_moveout
- Step-by-step NMO correction by Leonardo Uieda - February 2017
- ↑ Deregowski, S. M. (1986). "What is DMO". First Break 4 (7): 7–24. doi:10.3997/1365-2397.1986014.