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SUMIGGBZOAN - MIGration via Gaussian beams ANisotropic media (P-wave) sumiggbzoan <infile >outfile vfile= nt= nx= nz= [optional parameters] Required Parameters: a3333file= name of file containing a3333(x,z) nx= number of inline samples (traces) nz= number of depth samples Optional Parameters: dt=tr.dt time sampling interval dx=tr.d2 inline sampling interval (trace spacing) dz=1.0 depth sampling interval fmin=0.025/dt minimum frequency fmax=10*fmin maximum frequency amin=-amax minimum emergence angle; must be > -90 degrees amax=60 maximum emergence angle; must be < 90 degrees bwh=0.5*vavg/fmin beam half-width; vavg denotes average velocity Files for general anisotropic parameters confined to a vertical plane: a1111file= name of file containing a1111(x,z) a1133file= name of file containing a1133(x,z) a1313file= name of file containing a1313(x,z) a1113file= name of file containing a1113(x,z) a3313file= name of file containing a3313(x,z) For transversely isotropic media Thomsen's parameters could be used: deltafile= name of file containing delta(x,z) epsilonfile= name of file containing epsilon(x,z) a1313file= name of file containing a1313(x,z) if anisotropy parameters are not given the program considers ", the medium to be isotropic. Credits: CWP: Tariq Alkhalifah, based on MIGGBZO by Dave Hale CWP: repackaged as an SU program by John Stockwell, April 2006 Technical Reference: Alkhailfah, T., 1993, Gaussian beam migration for anisotropic media: submitted to Geophysics. Cerveny, V., 1972, Seismic rays and ray intensities in inhomogeneous anisotropic media: Geophys. J. R. Astr. Soc., 29, 1--13. Hale, D., 1992, Migration by the Kirchhoff, slant stack, and Gaussian beam methods: CWP,1992 Report 121, Colorado School of Mines. Hale, D., 1992, Computational Aspects of Gaussian Beam migration: CWP,1992 Report 121, Colorado School of Mines.
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