Translations:Synthetic seismogram without multiples/15/en

From SEG Wiki
Jump to navigation Jump to search

In summary, when we convolve a wavelet with a reflectivity function, we obtain the synthetic multiple-free trace shown in Figure 7. In other words, the reflectivity represents the primaries-only impulse response of the subsurface. The synthetic trace (without multiples) is the convolution of this impulse response with the seismic wavelet.