Results of our DMO program

We now return to the field data from the Gulf of Mexico, which we have processed earlier in this chapter and in chapter .

 

wgdmostk
Figure 26 Stack after the dip-moveout correction. Compare this result with Figure . This one has fault plane reflections to the right of the faults.

 

wgdmomig
Figure 27 Kirchhoff migration of the previous figure. Now the fault plane reflections jump to the fault.