SUKDSYN2D - Kirchhoff Depth SYNthesis of 2D seismic data from a migrated seismic section sukdsyn2d infile outfile [parameters] Required parameters: infile=stdin input migrated section outfile=stdout file for output seismic traces ttfile file for input traveltime tables The following 9 parameters describe traveltime tables: fzt= first depth sample nzt= number of depth samples dzt= depth interval fxt= first lateral sample nxt= number of lateral samples dxt= lateral interval fs= x-coordinate of first source ns= number of sources ds= x-coordinate increment of sources The following 6 parameters describe the migration section: fz= first z-coordinate in migrated section dz= vertical spacing of migrated section nz= number of depth points in migrated section fx= first x-coordinate of migrated section dx= horizontal spacing of migrated section nx= number of lateral points in migrated section Optional Parameters: nt=501 number of time samples dt=0.004 time sampling interval (sec) ft=0.0 first time (sec) nxo=1 number of source-receiver offsets dxo=25 offset sampling interval fxo=0.0 first offset nxs=101 number of shotpoints dxs=25 shotpoint sampling interval fxs=0.0 first shotpoint fmax=1/(4*dt) maximum frequency in migration section (Hz) aperx=nxt*dxt/2 modeling lateral aperature angmax=60 modeling angle aperature from vertical v0=1500(m/s) reference velocity value at surface dvz=0.0 reference velocity vertical gradient ls=1 flag for line source jpfile=stderr job print file name mtr=100 print verbal information at every mtr traces Notes: This program takes a migrated seismic section and a set of travel time tables generated using rayt2d for a specific background velocity model and generates synthetic seismic data in the form of common shot gathers. (Common offset gathers may be generated by using nxo=1.) (Demigration.) This program is a tool which may be used for the migration residual statics estimation technique of Tjan, Audebert, and Larner 1994. 1. The traveltime tables are generated by program rayt2d (or other ones) on relatively coarse grids, with dimension ns*nxt*nzt. In the modeling process, traveltimes are interpolated into shot/geophone positions and migration section grids. 2. The input migration section must be an array of binary floats (no SU headers). ", 3. The synthesized traces are output in common-shot gathers in SU format. 4. The memory requirement for this program is about (ns*nxt*nzt+nx*nz+4*nr*nzt+3*nxt*nzt)*4 bytes where nr = 1+min(nxt*dxt,0.5*offmax+aperx)/dxo. Author: CWP: Zhenyue Liu, 07/24/95, Colorado School of Mines References: Tjan, T., F. Audebert, and K. Larner, 1994, Prestack migration for residual statics estimation in complex media (Appeared in 1994 Project Review, CWP-153.) Tjan, T., 1995, Residual statics estimation for data from structurally complex areas using prestack depth migration: M.Sc. thesis, Colorado School of Mines. (In progress.) Larner, K., and Tjan, T., 1995, Simultaneous statics and velocity estimation for data from structurally complex areas. (Appeared in 1995 Project Review, CWP-185.) Trace header fields set: ns, dt, delrt, tracl, tracr, fldr, tracf offset, sx, gx, trid, counit