Page 127 - Acquisition and Processing of Marine Seismic Data
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118                           2. MARINE SEISMIC DATA ACQUISITION

              Depth of the streamer(s) should be controlled  2.5.1.3 Group Interval
           carefully, especially for high-resolution surveys  Group interval is the distance between the cen-
           where the streamer is towed at relatively shal-  ters of two adjacent recording channels. In marine
           low depths. In high-salinity warmer waters,  seismic equipment, the group interval isdesigned
           streamer trimming with specific weights may  during production and cannot be modified later
           be necessary. If some sections of the streamer  except that it can be increased by trace summing
           are shallower than the remaining sections, then  option provided by digital seismic streamers.
           the channels in shallow sections record too  Since a smaller interval provides a smaller inline
           much swell noise. If they are deeper, however,  binsize(whichalwaysequalsthehalfgroupinter-
           this results in distinct phase distortions along  val, as shown in Fig. 2.72), and hence better inline
           the reflections. Fig. 2.71 shows an interesting  resolution, it is always preferred to use a group
           example shot gather for this situation. The tail  interval as small as possible. Today, a 6.25 or
           sections of the streamer, which involve approx-  12.5 m group interval is typical for conventional
           imately last 64 channels, are much deeper than  2D or 3D exploration, while a 3.125 m interval is
           the remaining frontal part of the cable. This  used for high-resolution seismic systems.
           causes significant phase distortions, both on   Group interval defines the largest spatial sam-
           the sea floor and subsurface reflections, which  pling that prevents aliasing during the migration
           cannot be handled during the processing.     process. According to sampling theory, a




































           FIG. 2.71  An example shot gather illustrating the effect of depth variations along the streamer on the recorded data. Depth
           of the last 64 channels is twice the rest of the streamer depth, which results in distinct phase distortions in the area, shown by a
           dashed ellipse.
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