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SUSYNVXZ - SYNthetic seismograms of common offset V(X,Z) media via Kirchhoff-style modeling susynvxz >outfile [optional parameters] Required Parameters: <vfile file containing velocities v[nx][nz] nx= number of x samples (2nd dimension) nz= number of z samples (1st dimension) Optional Parameters: nxb=nx band centered at midpoint nxd=1 skipped number of midponits dx=100 x sampling interval (m) fx=0.0 first x sample dz=100 z sampling interval (m) nt=101 number of time samples dt=0.04 time sampling interval (sec) ft=0.0 first time (sec) nxo=1 number of offsets dxo=50 offset sampling interval (m) fxo=0.0 first offset (m) nxm=101 number of midpoints dxm=50 midpoint sampling interval (m) fxm=0.0 first midpoint (m) fpeak=0.2/dt peak frequency of symmetric Ricker wavelet (Hz) ref="1:1,2;4,2" reflector(s): "amplitude:x1,z1;x2,z2;x3,z3;... smooth=0 =1 for smooth (piecewise cubic spline) reflectors ls=0 =1 for line source; default is point source tmin=10.0*dt minimum time of interest (sec) ndpfz=5 number of diffractors per Fresnel zone verbose=0 =1 to print some useful information Notes: This algorithm is based on formula (58) in Geo. Pros. 34, 686-703, by N. Bleistein. Offsets are signed - may be positive or negative. ", Traveltime and amplitude are calculated by finite differences which is done only in part of midpoints; in the skiped midpoint, interpolation is used to calculate traveltime and amplitude. ", More than one ref (reflector) may be specified. Note that reflectors are encoded as quoted strings, with an optional reflector amplitude: preceding the x,z coordinates of each reflector. Default amplitude is 1.0 if amplitude: part of the string is omitted. CWP: Zhenyue Liu, 07/20/92 Many subroutines borrowed from Dave Hale's program: SUSYNLV Trace header fields set: trid, counit, ns, dt, delrt, tracl. tracr, cdp, cdpt, d2, f2, offset, sx, gx
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