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renewal, which is below a depth of 1.5 km at Sijarinska Banja and below 1.3 km at Selters Banja.Key words: spread, fault zone, distance of recharge zone, depth, hydrodynamic zoning, mineral water. Апстракт. Циљ овог рада

mineral water sites. Many authors haveprovided brief geological and hydrogeological descriptions of the immediate spread of the hydrogeologic structures in which such water occurs, and presented results of physicochemical, radioactivity

there were nomanifestations on the ground surface. The hydrogeologic structures were studied in termsof their spread between recharge zones, depth, andpoints of discharge of mineral water, along with thepost-infiltration residence