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Is Eq. (3) a vslid substitution? Conventional dip-movoout mirrors this birs in the With minor q odificstioas, this inversion based f ins1 stsckod section. Eoro, Do is the roro-offset doto. The vsvo equstion is not considered. This is the operator whioh products the a($ - - dst du (2n)' Equation (7) as written it a 3D formuliam.
- Geophysics > Seismic Surveying > Seismic Processing (0.56)
- Geophysics > Seismic Surveying > Seismic Modeling > Velocity Modeling (0.50)
Green's stress tensor, ni is the unit n d rmal to S, frequencies, bat is superior to the ray method or Computation of the exaot incident field, Green's of what event was caused by what. This approximation has usually been applied to acoustic problems. The C's hide the fcompllaated1 Kirchhoff-Eelmholtx integrals. The iategrand in Bq.(2) oan be interpreted a6 bounded by surfaces of parameter discontinuity. These rays do mot obey Our general approach is similar to Frazer and San Snell'r law except when the phase is stationary.