Nonhyperbolic reflection moveout for orthorhombic media
Reflection moveout in azimuthally anisotropic media is not only azimuthally dependent but it is also nonhyperbolic. As a result, the conventional hyperbolic normal moveout (NMO) equation parameterized by the exact NMO (stacking) velocity loses accuracy with increasing offset (i.e., spreadlength)....
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Format: | Technical Report |
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Massachusetts Institute of Technology. Earth Resources Laboratory
2011
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Online Access: | http://hdl.handle.net/1721.1/67847 |