The curves of deep magnetotelluric soundings at sites located along the south-western border of the East-European platform have been combined with the magnetovariational one from the Lviv geomagnetic observatory. The apparent resistivity and phase curves in the period from 9 - 100 sup to <$E 3,4~cdot~10 sup 8> s are used for the 1D modelling. The one-dimensional inversion results have shown increasing the total lateral conductivity of the upper mantle from 1 400 - 2 200 S under the East Europe platform up to more than 3 000 S under the Teisseyre-Tornquist zone.

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