Abstract:
The South Caspian Sea (Fig. 1) was only recently opened for exploration to western companies. The number of offshore wells drilled in the past has been limited. The seismic response in the area is generally good, but the geology may be locally complicated. In particular, the presence of undercompacted overpressured shale layers has been reported. Reliable pieces of information relevant to the geophysicist, such as sonic logs or check shot surveys are sparse. Consequently, one often has to rely on seismic data, and more precisely on stacking velocities to estimate the velocities needed for imaging (migration) or for time-to-depth conversion later in the processing-interpretation process. Unfortunately, stacking velocities often diverge dramatically from the needed geological 'propagation' velocities. The many reasons for this are well known and have been documented for a long time in the seismic literature (A1 Chalabi 1994). The South Caspian Sea is no exception, to the rule and strong stacking velocity 'anomalies' were noticed over most of the structures as soon as the first speculative surveys were made available in the area. In this context, improving the control over seismically derived velocities is an important issue in the preparation, acquisition and processing of newly acquired 3D seismic data sets (Robein and Kerimov 1998). This paper presents an approach to this problem applied to a 3D survey shot in 1997 over the Lenkoran-Talysh structure in the Azerbaijan South Caspian Basin, offshore the city of Lenkoran.