Page 383 - Acquisition and Processing of Marine Seismic Data
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374                          7. SUPPRESSION OF MULTIPLE REFLECTIONS

           amplitude   spectrum   of  the  seismogram   successive multiples is almost constant in near
           (Fig. 6.12). As the time span between the multi-  offset traces, it progressively increases for far
           ple reflections in the time series increases, the  offsets. This is also evident on the autocorrelo-
           notches in the spectrum get closer to each other.  grams of the shot gather in Fig. 7.9C, in which
              Predictive deconvolution can be used to   the multiple energy is not horizontal but curved
           remove the multiple energy from the seismic  towards the far offsets, indicating that the
           data by predicting and suppressing the multiple  periods of the multiples decrease at far offsets.
           reflection series. A successful predictive decon-  In deconvolution application, an optimal
           volution can remove the complete multiple    selection of prediction lag and operator length
           energy from the seismic data, provided that all  parameters is crucial. Fig. 7.10A shows the atten-
           of the assumptions listed in Section 6.2 are satis-  uation rates of the multiple amplitudes by pre-
           fied. Deconvolution is particularly efficient on  dictive deconvolution for a range of prediction
           short period multiples, and almost ineffective  lag and operator length values. In this example,
           on the multiples with a period larger than   a synthetic seismic trace with one primary reflec-
           approximately 200 ms. This is because the peri-  tion and its multiple is used (Fig. 7.10B), and the
           odicity of the multiples varies with increasing  amplitude suppression rate of the multiple after
           offset due to the normal moveout of the reflec-  each application of predictive deconvolution for
           tion hyperbolas, as schematically shown in   different prediction lag and operator length
           Fig. 7.9A and on a real marine shot gather in  parameters is recorded. According to the auto-
           Fig. 7.9B. Although the time span between the  correlogram of the input synthetic trace shown

































           FIG. 7.9  Illustration of the variations in periodicity of multiples (M 1 , M 2 , and M 3 ) with increasing offset on (A) a schematic
           and (B) a real marine shot gather. (C) Autocorrelograms of the shot in (B) indicating the offset dependency of the multiple
           periods.
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