Depth Imaging
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DownUnder GeoSolutions offers a comprehensive true amplitude and anisotropic depth migration tooklit including Kirchhoff and Gaussian Beaming to solve your imaging problems. |
The Kirchhoff computes travel times through the wavefront reconstruction method and utilises the maximum energy travel times. The amplitude maps for true amplitude migration are calculated using a method based on Dellinger et. al (2000).
Rapid and accurate automated picking of residual moveout and dip, coupled with a robust reflection tomography, ensures efficient iteration and refinement of the velocity model. Faults, horizons and geobodies can be included in the model if required.
