Page 376 - Acquisition and Processing of Marine Seismic Data
P. 376

7. SUPPRESSION OF MULTIPLE REFLECTIONS                 367

























           FIG. 7.2  (A) Schematic display of multiple reflection ray paths in the case of an inclined seabed; (B) an example marine
           stack section from an inclined seafloor. Multiples can be regarded as primary reflections from apparent reflectors lying at
           the subsurface in the case of an inclined seafloor.

           expression of a seabed multiple of mth order for  • Multiples are predictable, yet primaries
           a seafloor with an inclination angle of θ is    are not.
           given by                                     • Multiples appear at regular time intervals, at
                                                           least for near offsets on shot gathers.
                        2
                       x +4h  4hxsin m +1Þθ
                             2
                 2                   ð
                 t xðÞ ¼          2               (7.2)  • Multiples always have higher moveout times
                                 V
                                                           than the primary reflections of the same zero
           where h is the perpendicular distance from source  offset arrival time.
           to the specific apparent multiple reflector  • Lower velocities are required to flatten the
           (Fig. 7.2A). Eq. (7.2) indicates that the inclination  multiple reflection hyperbolas during normal
           of each consecutive multiple increases on the zero  moveout (NMO) correction.
           offsetsections.Iftheinclinationoftheseafloorisθ,  • The inclination of a multiple reflection
           then the inclination of the mth order multiple will  produced by an inclined reflector is higher
           be mθ. This situation prevents the complete suc-  than the inclination of the primary reflection
           cess of most demultiple approaches.             from the same reflector.
              The multiples can be suppressed if one of  • Amplitudes of primary and multiple
           their characteristics, such as velocity or periodic-  reflections with same zero-offset time are
           ity, meets the theoretical basis of the existing  generally different.
           multiple removal approaches. Some of the     • Polarity of seabed multiple reflections is
           demultiple methods are based on specific differ-  reversed with respect to the polarity of the
           entiations between primaries and multiples,     seafloor reflection.
           such as moveout differences, while the others
                                                           Several different methods to predict and
           try to model or predict the multiples and then
                                                        remove multiple reflections have been devel-
           subtract from the input data. These differences
                                                        oped based on their characteristics given in
           between primaries and multiples regarding
                                                        the preceding list. For instance, predictive
           their main specifications are as follows:
   371   372   373   374   375   376   377   378   379   380   381