Abstract
On the example of loamy-chalky Upper Cretaceous strata (K2cm) of Sviatogirsk brachyanticline it has been found out that carbonate karst forms with the participation of different on dynamics and chemical composition kinds of groundwater.Basic chemical reactions that lead to leaching and dissolution of carbonate rocks during their interaction with groundwater have been characterized. Geological, hydrogeological and geochemical conditions of formation of various morphogenetic types of karst - surface (epikarst) and deep (hypokarst) have been well-grounded.
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