The example in [[:file:seismic-migration_fig6.png|Figure 6]] shows imaging of reflections from steep faults. While migration of CMP-stacked data (not shown here) shows the faulting, reflections from ''the faults themselves'' are absent. Details of the fault reflections seen on the DMO-processed result can be diagnostic of sealing along the faults. | The example in [[:file:seismic-migration_fig6.png|Figure 6]] shows imaging of reflections from steep faults. While migration of CMP-stacked data (not shown here) shows the faulting, reflections from ''the faults themselves'' are absent. Details of the fault reflections seen on the DMO-processed result can be diagnostic of sealing along the faults. |