Abstract
First of all, what is the nature of the problem to be addressed here? Conventional seismic processing consists of unstacked reflection seismic data as input and, typically, a CDP stacked section in time as output. Except for extremely simple situations, a time migrated section will also be formed. The problem is that the time structure on that final section does not necessarily represent the true depth structure in the earth. This is particularly true when strong lateral velocity variations are present.
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