Abstract
Since Kosloff and Baysal (1982) introduced the Fourier or so‐called pseudo‐spectral method to the geophysical industry for solving wave‐equation modeling problems, it has become one of the major tools in computational seismology. Recently, Saatcilar et al. and Saatcilar and Ergintav presented some geophysical applications of the Hartley transform (HT). From their papers, it is clear that the HT is an alternative tool to the Fourier transform (FT).

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