Abstract
The signature generated by an array of marine seismic sources is an important input to many seismic processing algorithms. Several methods have been proposed for determining the source signature from a single source or a source array (see e.g., Ziolkowski et al., 1982; Hargreaves, 1984; Loewenthal and Shtivelman, 1989; Carrion et al., 1990; Weglein and Secrest, 1990; Tygel et al., 1991; Landrø and Sollie, 1992, and Amundsen, 1993).
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