Abstract
Based on the comparison of relief and geological data, the newest structural elements were identified, actively developing in the form of systems of uplifts and depressions, deciphered from satellite images and topographic maps in the form of lineaments predetermined by discontinuous disturbances. As a result of the research, neotectonic shear stress fields have been restored with orientations of the submeridional compression axes of tectonic stresses of the I rank, which is generally in agreement with the subhorizontal compression axes, mainly oriented submeridionally, established in almost all regions of Northern Eurasia.
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