Abstract
On the basis of medium-scale mapping of the pre-Mesozoic surface of Donbas and the southeastern part of the DDZ, the use of the results of seismostratigraphic and gravimetric works, the analysis of scientific research, publications and innovative hypotheses, the geological and geotectonic unity of Donbas and the DDZ is substantiated. The features of the geological structure of the fringes and their central part were specified, and 16 alpine uplifts and downlifts of the northeastern trend were identified and mapped for the first time, including 5 drops in DDZ and 4 - in Donbass and 4 drops each to DDZ and Donbass.
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