Page 14 - Acquisition and Processing of Marine Seismic Data
P. 14

1. INTRODUCTION                                 5


                                                SegD/SegY raw data
                                                   Data loading

                                                  Demultiplexing

                            Observer logs        Geometry loading
                            Navigation logs

                                                  Band-pass filter
                                                                        Near trace section
                                                   Gain recovery
                                                                        Brute stack section
                                               Track kill / Edit / Muting

                                                    f-k Dip filter

                                                     Multiple
                                                   suppression

                                                   Deconvolution
                                                  Band-pass filter

                                                 CDP sort / Binning
                                                                           First velocity analysis
                                                                                 NMO
                       Prestack migration         Velocity analysis
                                                                           Dip moveout (DMO)
                                                                              Inverse NMO
                            Gain                   NMO - Stack            Second velocity analysis
                                                                                 NMO
                                                                                 Stack
                          Top mute               Poststack migration
                         SEGY output              Gain / top mute

           FIG. 1.3  A conventional seismic data-processing flow for marine seismic data.

           performed on the very first shots of the line  in Fig. 1.4. Here, the dataset used has 500 shots
           instead of applying the filter to the whole seis-  with 480 recording channels, resulting in a total
           mic line. After determination of all parameters  of 240,000 traces and 120-fold seismic data. Sam-
           for each step, the flow is run for the whole line  pling rate and maximum recording time are
           using approved parameters, which is known    1 ms and 6 s, respectively. Apart from the hard-
           as production processing.                    ware specifications used to prepare this illustra-
              Each of these steps is of a specific run time con-  tion, the relative time span for each processing
           trolled bydatavolume, processing hardware, and  step is remarkable. In general, the processes per-
           the algorithm implemented. As an example, nec-  formed on prestack data require much more run
           essary rendering times in seconds for different  time thanthose applied to poststack data,because
           steps for the same 2D seismic dataset are shown  the data volume is significantly reduced after
   9   10   11   12   13   14   15   16   17   18   19