Compared to surface seismic, the increased complexity associated with seafloor seismic data (OBC) requires considerable attention to details if a.
The goal of repeat imaging (detailed studies of prospects as new information is available) using PSDM is to generate new locations for both development.
3-D prestack depth migration is the most time consuming part in velocity model building. To minimize the required iteration of depth migration, we first.
The remarkable improvements in data quality due to rapid advances in processing algorithms and computer technology over the past several years have been.