Translations:Seismic deconvolution/6/en

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On land, the situation became quite different in areas where major multiples originated from near-surface limestone layers. At sea, the situation was different as well — the water layer introduced strong multiple energy in the form of so-called multiple reverberations. At that time, seismograms containing such water-layer-induced reverberations were known as “ringing” or “singing” records.