SUDATUMK2DR - Kirchhoff
datuming of receivers for 2D prestack data (shot gathers are the input)
sudatumk2dr
infile= outfile= [parameters]
Required parameters:
infile=stdin file
for input seismic traces
outfile=stdout file for common offset migration output
ttfile file
for input traveltime tables
The following 9 parameters describe
traveltime tables:
fzt first
depth sample in traveltime table
nzt number
of depth samples in traveltime table
dzt depth
interval in traveltime table
fxt first
lateral sample in traveltime table
nxt number
of lateral samples in traveltime table
dxt lateral
interval in traveltime table
fs x-coordinate
of first source
ns number
of sources
ds x-coordinate
increment of sources
fxi x-coordinate of the first surface location
dxi
horizontal spacing on surface
nxi
number of input surface locations
sgn Sign of the datuming process
(up=-1 or down=1)
Optional Parameters:
dt= or from header (dt) time sampling interval of input data
ft= or from header (ft) first
time sample of input data
surf="0,0;99999,0" The first surface defined the recording
surface
surf="0,0;99999,0"
and the second one, the new datum.
"x1,z1;x2,z2;x3,z3;...
fzo=fzt z-coordinate
of first point in output trace
dzo=0.2*dzt vertical
spacing of output trace
nzo=5*(nzt-1)+1 number of points in output trace ",
fxso=fxt x-coordinate
of first shot
dxso=0.5*dxt shot horizontal spacing
nxso=2*(nxt-1)+1 number of shots
fxgo=fxt x-coordinate
of first receiver
dxgo=0.5*dxt receiver
horizontal spacing
nxgo=nxso number
of receivers per shot
fmax=0.25/dt frequency-highcut
for input traces
offmax=99999 maximum
absolute offset allowed in migration
aperx=nxt*dxt/2 migration lateral
aperature
angmax=60 migration angle aperature from vertical
v0=1500(m/s) reference
velocity value at surface
dvz=0.0
reference velocity vertical
gradient
antiali=1 Antialiase filter (no-filter = 0)
jpfile=stderr job
print file name
mtr=100
print verbal information at
every mtr traces
ntr=100000 maximum
number of input traces to be migrated
Notes:
1. Traveltime tables were generated by
program rayt2d (or other ones)
on relatively coarse grids, with dimension
ns*nxt*nzt. In the
datuming process, traveltimes are
interpolated into shot/gephone
positions and output grids.
2. Input traces must be SU format and
organized in common rec. gathers
3. If the offset value of an input trace is not in the offset
array
of output, the nearest one in the array is chosen.
4. Amplitudes are computed using the reference velocity profile,
v(z),
specified by the
parameters v0= and dvz=.
5. Input traces must specify source and receiver
positions via the header
fields
tr.sx and tr.gx. Offset is computed automatically.
Author: Trino Salinas,
05/01/96, Colorado School of
Mines
This code is based on
sukzmig2d.c written by Zhenyue Liu, 03/01/95.
Subroutines from Dave Hale's modeling library were adapted
in
this code to define topography
using cubic splines.
This
code implements a Kirchhoff extraplolation operator that allows to
transfer data from one reference surface to
another. The formula used in
this application is a far field approximation
of the Berryhill's original
formula (Berryhill, 1979).
This equation is the result of a stationary
phase analysis to get an analog asymptotic
expansion for the two-and-one
half
dimensional extrapolation formula (Bleistein, 1984).
The extrapolation formula permits the
downward continuation of upgoing
waves and upward
continuation of downgoing waves. For upward conti-
nuation of upgoing waves and downward continuation of downgoing
waves,
the conjugate transpose of
the equation is used (Bevc, 1993).
References :
Berryhill, J.R., 1979, Wave equation datuming: Geophysics,
44, 1329--1344.
_______________, 1984, Wave equation datuming
before stack
(short note) :
Geophysics, 49, 2064--2067.
Bevc, D., 1993, Data parallel wave equation datuming with
irregular acquisition topography : 63rd Ann. Internat.
Mtg., SEG, Expanded Abstracts,
197--200.
Bleistein, N.,
1984, Mathematical methods for wave phenomena,
Academic Press Inc. (Harcourt Brace Jovanovich Publishers),
New York.