Hydrologic Evolution of a Carbonate Aquifer (Dinaric Karst, Croatia) (CROSBI ID 80536)
Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija
Podaci o odgovornosti
Babić, Ljubomir ; Lacković, Damir ; Horvatinčić, Nada
engleski
Hydrologic Evolution of a Carbonate Aquifer (Dinaric Karst, Croatia)
Dinaric Karst terrains contain specific, laminated speleothems, which line all surfaces of subterranean voids. Deposition of these speleothems took place during a phereatic period and Late Quaternary. Phreatic speleothems can be important stratigraphic marker for the cave sediments. The phreatic speleothems indicate a phreatic stage when the ground-water level was very high in the large karst area. During this period the volume of the voids decrease.
karst; hydrology; carbonates; speleothems; cave
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