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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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