📄 ela2d.out
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E L A 2 D . X (start)
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Highest P-wave velocity in the model: 2800.000000
Lowest S-wave velocity in the model: 1700.000000
WARNING : dx/dz may not represent shortest wavelength suffic
iently!
wavelet length: 2250 time steps
grid rows 75
grid columns 150
source point [GP] 51 4
[m] 300.000000 18.000000
number of receivers 46
source type 1
( 1=dilatational source
2=vertical displacement
3=horizontal displacement )
wavelet type 1
( 1=2nd deriv. of Gauss-function
2=Kosloff wavelet
3=Ricker wavelet
4=Kuepper wavelet )
free surface (1=on) 1
first row of comput. 1
dx between cols 1&2 6.000000
dz between lines 1&2 6.000000
central frequency 30.000000
dissipative boundary-zone 26 [GP]
or 150.000000 [m]
max. taper factor 9.691378E-01
Higdon-Boundary-Cond. 1 1=on
write SeisSample each 1 Timestep
ZeitIntegration of 4th order
number of time steps 400
runtime 5.000000E-01 s
time-intervall dt 1.250000E-03 s
SnapShots :
nSnaps = 6 SnapShots
Delay = 80 timesteps
or 1.000000E-01 seconds
Intervall = 64 timesteps
or 8.000000E-02 seconds
snapmax = 400 timesteps
!!! BEGIN of the time loop !!!
TimeStep 25 of 400
TimeStep 50 of 400
TimeStep 75 of 400
SNAPSHOT No. 1 : max. amplitudes (Ux, Uz)
3968.812000 3329.287000
at timestep 80 of 400
TimeStep 100 of 400
TimeStep 125 of 400
SNAPSHOT No. 2 : max. amplitudes (Ux, Uz)
2318.868000 2304.165000
at timestep 144 of 400
TimeStep 150 of 400
TimeStep 175 of 400
TimeStep 200 of 400
SNAPSHOT No. 3 : max. amplitudes (Ux, Uz)
1921.842000 2433.631000
at timestep 208 of 400
TimeStep 225 of 400
TimeStep 250 of 400
SNAPSHOT No. 4 : max. amplitudes (Ux, Uz)
1627.037000 2478.411000
at timestep 272 of 400
TimeStep 275 of 400
TimeStep 300 of 400
TimeStep 325 of 400
SNAPSHOT No. 5 : max. amplitudes (Ux, Uz)
774.697900 1137.745000
at timestep 336 of 400
TimeStep 350 of 400
TimeStep 375 of 400
TimeStep 400 of 400
SNAPSHOT No. 6 : max. amplitudes (Ux, Uz)
70.136080 40.746190
at timestep 400 of 400
!!! END of the time loop !!!
CLOSED snapshot files !
CLOSED seismic files !
401 samples have been written to seismic traces
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E L A 2 D . X (END)
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