Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi

Meteoric phreatic speleothems and the development of cave stratigraphy: an example from Tounj Cave, Dinarides, Croatia. (CROSBI ID 80532)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Babić, Ljubomir ; Lacković, Damir ; Horvatinčić, Nada Meteoric phreatic speleothems and the development of cave stratigraphy: an example from Tounj Cave, Dinarides, Croatia. // Quaternary science reviews, 15 (1996), 10; 1013-1022

Podaci o odgovornosti

Babić, Ljubomir ; Lacković, Damir ; Horvatinčić, Nada

engleski

Meteoric phreatic speleothems and the development of cave stratigraphy: an example from Tounj Cave, Dinarides, Croatia.

Speleothems occurring in some caves of the carbonate Dinarides line all channel surfaces, and have been deposited from meteoric waters under phreatic conditions. Such phreatic speleothemic deposition modifies common experience (1) that meteoric phreatic conditions cause dissolutional widening of cave voids, and (2) that speleothems imply vadose conditions. The phreatic speleothems described here postdate an early polygenentic evolution of the cave voids, and predate the last, vadose stage. They were likely produced during the late/postglacial warming period, when dissolved carbonate was amply supplied, and when there was much water available for saturation of underground voids. Phreatic speleothems may be used as a tool for time correlation of internal deposits, both within one cave and within a karst region. They indicate an important stage in the history of the ground-water regime of an area. In general, phreatic speleothemx help in better understanding of the development of subterranean voids and related karst/paleokarst.

speleothems; karst; cave; stratigraphy; Dinarides; Quaternary

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

15 (10)

1996.

1013-1022

objavljeno

0277-3791

Povezanost rada

Fizika, Geologija

Indeksiranost