Page 421 - Acquisition and Processing of Marine Seismic Data
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412                                8. CDP SORT AND BINNING

























           FIG. 8.7  Schematic representation of traces forming the CDP gathers using reflections from only one horizontal reflector
           along a 3D seismic bin grid, which is divided into several cells, termed bins. Here, d is inline bin size, and a is distance between
           the streamers for 3D surveys.


           standard acquisition technique for conventional  negatively affect the acquisition geometry,
           3D surveys today. Each bin has several reflec-  including the streamer feathering, sail line
           tions from different gun arrays to various chan-  obstructions, navigation errors, etc., and the sub-
           nels of different streamers, which results in  surface midpoint locations of the traces deviate
           groups of traces with different azimuths and dif-  from their preplanned positions. Therefore, the
           ferent offsets. These traces are schematically  number of traces within each bin is not constant
           illustrated as circular trace groups for each bin  and fold distribution is not regular. Fig. 8.8
           in Fig. 8.7. Although each individual trace is  shows a small portion of a bin grid with the mid-
           reflected from a different point within a CDP  points of the recorded traces from eight
           bin, and hence normally has a random reflection  streamers slightly feathering to the left. Each
           point distribution within the bins, all of these  trace falling into a bin is assigned to the center
           traces are assigned to the bin centers. Similarly  of that specific bin.
           to the 2D case, fold decreases towards the edges  In 3D exploration, it is preferred that all bins
           of the 3D bin grid.                          have traces with all offsets, near and far channel
              As the vessel shoots along the predefined sail  traces together, in ideal conditions. However,
           lines, bins within the bin grid are filled by the  feathering of the streamers due to rough
           traces reflected from the subsurface areas   weather conditions during the surveys may
           defined by individual bins. Each bin then has  cause irregular fold distributions at the end of
           several traces from different shots and recorded  the survey, which results in degradation of sub-
           at different receivers, and the number of traces  sequent processing steps, such as migration,
           within a bin defines the fold of that particular  DMO or velocity analysis. If there are large gaps
           bin. In ideal conditions, each bin should have  in the fold coverage, reshooting is generally
           an equal number of traces reflected exactly at  applied in these areas to fill in the data gaps,
           the center of the bins. However, this cannot be  which ultimately affects the total cost of the
           achieved since there are several factors that  survey.
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