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

nije evidentirano