Translations:Gap deconvolution of a mixed-delay wavelet/2/en

Suppose various signature-deconvolution procedures are used to remove the source signature, absorption, and instrument response from a seismic trace. However, the process is not perfect, so a short causal nonminimum-delay residual wavelet u remains in their place. Thus, the resulting trace is $x=u*m*\varepsilon$, where m is the minimum-delay multiple and $\varepsilon$ is the white reflectivity. Suppose the multiple consists only of the water-layer reverberation given above — that is, $m=b$. For example, suppose the reverberation is