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 Alkhalifah, T., Fomel, S., and Biondi, B., 1997, Timedomain anisotropic processing in arbitrarily inhomogeneous media: SEP95, 7799.

 Fomel, S., 1997, A variational formulation of the fast marching eikonal solver: SEP95, 127147.

 Hatton, L., Larner, K. L., and Gibson, B. S., 1981, Migration of seismic data from inhomogeneous media: Geophysics, 46, no. 5, 751767.

 Hubral, P., 1977, Time migration  some ray theoretical aspects: Geophys. Prosp., 25, no. 4, 738745.

 Larner, K. L., Hatton, L., Gibson, B. S., and Hsu, I. C., 1981, Depth migration of imaged time sections: Geophysics, 46, no. 5, 734750.

 Raynaud, B. A., and Thore, P., 1993, Real time migration operators simulated by anisotropic ray tracing: 55th Mtg. Eur. Assoc. Expl Geophys., Abstracts.

 Sethian, J. A., and Popovici, A. M., 1997, Threedimensional traveltime computation using the fast marching method: submitted to Geophysics.

 Stork, C., and Clayton, R. W., 1991, Linear aspects of tomographic velocity analysis: Geophysics, 56, no. 4, 483495.

Comptomoflat
Figure 5 Linearization errors for the deep reflector
at zero offset (thick) and 3.2 km offset (thin):
solid lines for domain tomography
and dashed lines for domain tomography.
Comptomoanom
Figure 6 Linearization errors for the shallow reflector
at zero offset (thick) and 3.2 km offset (thin):
solid lines for domain tomography
and dashed lines for domain tomography.
Movezdip
Figure 7 True velocity model in domain with
a superimposed a contour plot of the starting velocity model.
The reflector geometries and a few zerooffset raypaths are superimposed
onto the model.
Movetaudip
Figure 8 True velocity model in domain with
a superimposed a contour plot of the starting velocity model.
The reflector geometries and a few zerooffset raypaths are superimposed
onto the model.
Comptomodippos
Figure 9 Linearization errors for the positive anomaly case
at zero offset (thick) and 2 km offset (thin)
(solid lines for domain tomography
and dashed lines for domain tomography).
Comptomodipneg
Figure 10 Linearization errors for the negative anomaly case
at zero offset (thick) and 2 km offset (thin)
(solid lines for domain tomography
and dashed lines for domain tomography).
A
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Stanford Exploration Project
10/10/1997