Geophysical Journal | 2001 volume 23 4

A quasi-3D geoelectrical model of West Ukraine

© T.K. Burakhovich, S.N. Kulik, 2001

At the north-west of the Ukrainian Shield a Korostenian - Thernovtsy high conductivity anomaly with the integral longitudinal conductivity from 500 to 1000 S has been observed within the limits of the Volynian and Podolian blocks at depth of 15 km. There is some evidence of a conductivity layer with S of ca 2000 S at a depth of 70 km in the upper mantle. Thus, all data consistently shows a boundary separating the mantle of Ukrainian Shield at the longitude of 30-32 degree.

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