HYDROGEOLOGICAL ROLE OF GEODYNAMIC ACTIVE ZONES
Structural-geological conditions and geodynamic (neotectonic) activity play a key role in the formation of the hydrogeological conditions in the western part of the Siberian platform in the zone of active water exchange – it is established as a result of structural and hydrogeological and lineament-geodynamic analysis. Geospatial relationship of areas of high geodynamic activity with areas of high concentration of groundwater flow and groundwater chemical drain are installed. Most local tectonic uplifts in geodynamic active zones are characterized by elevated hydrogeological parameters. The main hydrogeological role geodynamic active zones are in the distribution of groundwater flow; the formation of the hydrogeological and hydrogeochemical anomalies, as well as in the formation of specific hydro-geological, geo-environmental and geotechnical conditions and the formation of mineral deposits.