Page 107 - Acquisition and Processing of Marine Seismic Data
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98                            2. MARINE SEISMIC DATA ACQUISITION































           FIG. 2.54  Prestack migration comparison of (A) single azimuth data from a NAZ survey and (B) three-azimuth data from a
           MAZ cube. After Long, A., 2009. Evolutions in seismic azimuth: past, present and future. Geohorizons 4–13.

           • Wide-azimuth surveys (WAZ): One or two     This configuration provides an increased near-
              shooting vessels accompany the single NAZ  offset coverage from a split spread layout with
              vessel along a single azimuth sail line   zero and negative offsets. TopSeis provides a
              (Fig. 2.55C).                             better azimuth distribution and notch diversity,
           • Rich-azimuth surveys (RAZ): A combination of  enabling a higher-resolution data with no ghost
              MAZ and WAZ surveys provides the most     reflection.
              regular azimuth distribution in the survey   Although they are more costly than conven-
              area (Fig. 2.55D).                        tional 3D NAZ acquisitions, the main benefits
           • Coil shooting: One single vessel tows the  of wide-azimuth seismic data are an improved
              streamers and a source array along a circular  target illumination, a better S/N ratio due to
              path (Fig. 2.55E). An extra shooting vessel  the contributions from different azimuths dur-
              may also be used (Fig. 2.55F).            ing the stacking of each 3D azimuth cube, and
                                                        a better multiple attenuation (Moldoveanu,
              Recently, CGG Veritas has tested a specific  2006). As the world’s hydrocarbon exploration
           acquisition technique called TopSeis, where  strategy moves into more challenging areas such
           the seismic sources are towed from a second ves-  as the areas of salt tectonism, or the regions cov-
           sel, positioned above the middle of the streamer  ered by volcanic rocks or carbonates, different
           spread towed by the streamer vessel, which is  types of unconventional surveys which provide
           an innovative source-over-spread acquisition  extra azimuths become more and more popular
           configuration (Whaley, 2017). The streamers  to image complex subsurface targets, particu-
           are towed at approximately 50 m at the center  larly beneath the large salt bodies. MAZ surveys
           of the spread, where the sources are located.  can be performed as complementary surveys to
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