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The article presents factual material substantiating the mixed supply regime of the ore-bearing aquifer at uranium deposits of the Khiagda ore field. There are two competing flows: infiltration of oxygen-containing meteoric waters and exfiltration of deep carbonate bicarbonate–magnesium groundwaters containing epigenetic reducing agents in the form of gases and dissolved organic matter of the petroleum series. Exfiltration prevails over infiltration. Carbonate groundwater containing epigenetic reducing agents forms a constantly acting reductive geochemical barrier that works as an ore-preserving factor.

Carbonate Groundwater—An Ore-Preserving Factor at Uranium Deposits of The Khiagda Ore Field (Republic of Buryatia)