Hydrogeological conditions of the Meshchera depression and their connection with the latest tectonic structure of the region

The article presents the results of a study of the geological structure, recent tectonics and hydrogeological conditions of the central part of the Meshchera depression, located on the border of the Moscow, Ryazan and Vladimir regions. The detailed characterization of the newest structure of the Klepikovsky trough made it possible to identify young growing uplifts that influence the structure and morphology of the trough. The reasons for the intense swampiness of the territory and the change in the orientation of the trough from meridional to latitudinal are determined. The studies carried out proved the influence of the latest tectonics of the trough on the hydrogeological conditions of the territory. It has been established that areas of groundwater recharge and discharge can be localized within the Klepikovsky trough.