Abstract
In the Moscow region, Eopleistocene deformations (1,8 million years) were studied for the first time. The activity of modern geological processes is associated with them. The qualitative and quantitative characteristics of deformations were carried out on the basis of the structural-geodynamic method and morphometric analysis of a large array of GIS data. The stage-by-stage amplitudes and velocities of neotectonic uplifts have been estimated. And the gradient of the strain rate of the Moskvoretskaya zone was calculated.
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