📄 proc
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#! /bin/sh# use zero-velocity layer and wave-equation datuming# to datum data from topography to a horizontal surface#static shift data from topography to a horizontal surface above###################################################################sustatic < demo.su > demo.su_zstat hdrs=2 sign=-1 sou_file=zsou.b \rec_file=zrec.b ns=320 nr=320 no=1#################################################################### wave-equation datum from this horizontal surface to another# horizontal surface located at a depth of 600 m (see Cshot# plot of model) - two velocity fields are used: the thin lens# velocity backs out the static shift introduced above, and the # diffraction term doesn't "turn on" until the original topographic# surface is reached###################################################################sudatumfd < demo.su_zstat > demo.su_zstat_dat \nt=501 nx=320 nz=161 nsx=1 dz=10.0 dx=50.0 buff=10 tap_len=5 \mx=360 mz=161 vfile1=vfp1.b vfile2=vfp2.b dt=0.004 x_0=0.0#################################################################### The velocity models given with vfp1.b and vfp2.b start at the# lateral position 0.0, so the value x_0 is set to 0.0.exit 0
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