Using IWAVE - Madagascar

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$Modeling 3-D anisotropic fractal mediaa$

12 Figure 3: 2D shot record, (2,4) staggered grid scheme, ∆x = ∆z = 5 m, appropriate ∆t, 301 traces: shot x = 3300 m, shot z = 40 m, receiver x = 100 - 6100 m, receiver z = 20 m, number of time samples = 1501, time sample interval = 2 ms. Source pulse = zero phase trapezoidal [0.0, 2.4, 15.0, 20.0] Hz bandpass filter.
13 Figure 4: Trace 100 (receiver x = 2100 m) for ∆x = ∆z = 20 m (black), 10 m (blue), 5 m (green), and 2.5 m (red). Note arrival time discrepancy after 1 s: this is the interface error discussed in (Symes and Vdovina, 2009). Except for the 20 m result, grid dispersion error is minimal.
Page 1 and 2: Using IWAVE William. W. Symes 1 ABS
Page 3 and 4: 3 mechanical parameters which shed
Page 5 and 6: 5 one uses the basic IWAVE commands
Page 7 and 8: 7 that associated with the bulk mod
Page 9 and 10: 9 ACKNOWLEDGEMENTS IWAVE has been a
Page 11: 11 Figure 2: Dome density model
Page 15 and 16: 15 Figure 6: 2D shot record, (2,8)
Page 17 and 18: 17 Figure 8: Trace 100 detail, 1.8-
Page 19 and 20: 19 which is the value associated to
Page 21: 21 The parameters described here re

Using IWAVE - Madagascar

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