Recent geophysical research has made widespread use of depth migration and velocity analysis in our efforts to improve seismic images in structurally complex areas. Such structural exploration problems include the imaging of salt intrusions and faulted structures from offshore Newfoundland, and the delineation of thrust faulted structures from the Alberta foothills. We show that methods such as reverse-time migration and Kirchhoff migration can lead to significant improvements in our knowledge of geological formations. We are increasingly convinced that structural interpretation of intermediate processing results should play an important role in the development of the seismic velocity model for further iterations.
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