Abstract
Absence of granite in the crust under the central part of the Black Sea depression is confirined by the two methods. The sediments are underlain by basalt; granite is detectable only on the depression's periphery. Boundaries of the granite-free zone are clearly defined in the north and east of the sea; so far, no deep seismic sounding has been conducted in the west (fig. 5) where the wedging-Out of granite, toward the center of the depression, outside the competence of unaided seismological analysis, has been indicated on geomorphological premises (fig. 1).--V.P.Sokoloff.
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