Page 500 - Acquisition and Processing of Marine Seismic Data
P. 500

10.5 QC IN NMO CORRECTION AND STACKING                  491

           limit percentage reduces, even removes, these  stretch mute percentage. The gap always occurs
           amplitudes (Fig. 10.34B). Consequently, there  only at the start-of-line side (Fig. 10.35A). This is
           may be a trade-off between the data loss and  because the traces in the very first CDP gathers
           stack quality by means of the NMO stretch mute  located at the start-of-line side are always far off-
           percentage. Too-small values result in the loss of  set traces, whereas the traces in the very last
           far (even near) offsets, whereas too-high limits  CDP gathers located at the end-of-line side are
           incorporate noise amplitudes in the stack.   all near offset traces. Since the early arrivals of
              In shallow water data, there is a triangular  far offset traces are automatically muted out
           data gap located at one border of the seismic line  by NMO stretch mute, the early arrivals of the
           due to the NMO stretch mute. The size of this  traces at the very first CDPs of the lines, which
           area is inversely proportional to the NMO    consist of only far offsets, are removed. This is















































           FIG. 10.35  (A) In shallow waters, NMO stretch mute results in a triangular data gap located at the start-of-line side.
           Schematic representation of the ray paths of the traces for (B) the very first CDPs at the start-of-line, and (C) the very last CDPs
           at the end-of-line. The traces in CDPs 1, 2, and 3 in (B) are composed of only far offset traces, whereas the traces in CDPs 10, 11,
           and 12 in (C) are composed of only near offset traces. Because NMO stretch mute removes early arrivals of far offsets, this part in
           the very first CDPs is completely muted out. That is why the gap in (A) always occurs only at the start-of-line side. Here, (D) and
           (E) show real data examples from the first and last CDPs of a small-spread marine seismic line with a 693-m maximum offset,
           where the trace offsets range from 662 to 693 m in the first six CDPs, while they are between 100 and 131 m in the last six CDPs.
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