Pregled bibliografske jedinice broj: 13126
Hydrologic evolution of a carbonate aquifer (Dinaric Karst, Croatia).
Hydrologic evolution of a carbonate aquifer (Dinaric Karst, Croatia). // Geologia Croatica : journal of the Institute of Geology Zagreb and the Croatian Geological Society, 50 (1997), 2. (međunarodna recenzija, članak, znanstveni)
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Naslov
Hydrologic evolution of a carbonate aquifer (Dinaric Karst, Croatia).
Autori
Babić, Ljubomir ; Lacković, Damir ; Horvatinčić, Nada
Izvornik
Geologia Croatica : journal of the Institute of Geology Zagreb and the Croatian Geological Society (1330-030X) 50
(1997), 2;
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
karst; hydrology; carbonates; speleothems; cave
Sažetak
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.
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Geologija
POVEZANOST RADA
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Scopus
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