Translations:Piecemeal convolutional model/2/en

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An observed seismogram can be subdivided into time intervals (called windows). The boundaries of those windows are established by the arrival times of the major primaries. At such boundaries, the dynamic structure of a seismic trace changes. We will show that within any window, the dynamics remain essentially the same. Admittedly, this is just an approximation, but it clarifies how the mathematics of deconvolution works.