Go to the list of seismic processes.
Go to SIOSEIS introduction.
This example shows how "inner" and "outer" mutes may be applied
to moved-out data. The nmo velocity function also causes some weird
looking data because the NMO time goes backwards.
input data plot (see script below)
Notice that the ranges are from 182m to over 6000m. NMO created
some weird affects on the long range traces with velocities:
vtp 1495 4.85 1515 5.0 1555 5.167 2100 5.567 3500 6.567 end
The NMO time actually decreased and the increased, causing some data
to be mirrored.
plot of mirrored data
SIOSEIS process NMO zeroes data when time decreases.
data plot with nmo
The long ranges are normally muted at long ranges because of NMO
stretch and low signal-to-noise ratio. e.g.
mute
xtp 2000 4.8 3000 5.2 6000 8. end
end
data plot with nmo and outer mute data
Sometimes the traces close to the ship (small ranges) are noisy
later in time. An inner (close to the ship) mute may be used. e.g.
smute
xtp 0 5.5 3000 9 end
end
data plot with nmo and outer and inner mute data
sioseis << eof
procs diskin nmo mute smute agc plot end
diskin
ipath line23.g.3116.3120 fno 3116 lno 3116
end
end
nmo
vtp 1495 4.85
1515 5.0
1555 5.167
2100 5.567
3500 6.567 end
end
mute
xtp 2000 4.8 3000 5.2 6000 8. end
end
smute
xtp 0 5.5 3000 9 end
end
plot
ann range taginc 5
srpath sunfil nibs 75 nsecs 5 vscale 2.5 def .05 trpin 10
end
end
agc
winlen .5 end
end
end
eof
xloadimage -r 90 sunfil &
Go to the list of seismic processes.
Go to SIOSEIS introduction.