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$Modeling 3-D anisotropic fractal mediaa$

20 Sava <strong>Madagascar</strong> Documentation In zero-offset migration, we use the observed data to backprogate the wavefields using the data as boundary conditions. The image is the wavefield at time zero. Since we can acquire data at different locations in space, the reconstructed wavefields depend on the acquisition geometry, thus limiting the illumination in the subsurface. Therefore, the migrated images depend on the acquisition array, as illustrated in Figures 6(a) and 6(b) for the horizontal and vertical arrays, respectively. We can also obtain images by migrating the data observed in both the horizontal and vertical arrays, as illustrated in Figure 7, thus increasing the acquisition aperture and the subsurface illumination. CONCLUSIONS The combination of L A TEX and madagascar allows geoscientists to generate reproducible documents where the numeric examples can be verified by any user with the same computer setup. This allows for transparent peer-review, for recursive development and for transfer of technology between collaborative research groups. ACKNOWLEDGMENTS The reproducible numeric examples in this paper use the madagascar open-source software package freely available from http://www.reproducibility.org. REFERENCES Clærbout, J. F., 1985, Imaging the Earth’s interior: Blackwell Scientific Publications.
<strong>Madagascar</strong> Documentation WSI tutorial 21 Figure 6: Migrated images for data acquired in (a) the horizontal array and (b) the vertical array. school/sigsbee imgH,imgV
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