Pregled bibliografske jedinice broj: 611062
Fluviokarst and classical karst: Examples from the Dinarics (Krk Island, Northern Adriatic, Croatia)
Fluviokarst and classical karst: Examples from the Dinarics (Krk Island, Northern Adriatic, Croatia) // Geomorphology, 184 (2013), 64-73 doi:10.1016/j.geomorph.2012.11.016 (međunarodna recenzija, članak, znanstveni)
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Naslov
Fluviokarst and classical karst: Examples from the Dinarics (Krk Island, Northern Adriatic, Croatia)
Autori
Benac, Čedomir ; Juračić, Mladen ; Matičec, Dubravko ; Ružić, Igor ; Pikelj, Kristina
Izvornik
Geomorphology (0169-555X) 184
(2013);
64-73
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
classical karst; Fluviokarst; coastal geomorphology; Terra rossa; Dinarics; Adriatic Sea
(classical karst; Fluviokarst; Coastal geomorphology; Terra rossa; Dinarics; Adriatic Sea)
Sažetak
In order to contribute to the debate on the role of fluvial erosion in the shaping of karst, two nearby areas with different karstic landscapes were compared. Areas A and B are located relatively close to each other on the southern side of the Krk Island (Adriatic Sea, Croatia). Both areas are composed of similar limestone with a very high CaCO3 content. Area A is a typical doline or polygonal type (“classical”) of karst with numerous dolines (up to 57/km2) covered with terra rossa (red soil) and Mediterranean maquis shrubland. Dolines are located in zones which correspond to the strike of the main geological structures. Dry karstic valleys are visible only on gently inclined coastal slopes bordering the karstic plateau. In contrast, area B is typical of a bare karst landscape with a strong (palaeo)fluvial imprint. The dolines are absent, and the bedrock is only sporadically covered with terra rossa. Palaeogene marls have been observed in a few elongated depressions and in the coastal zone of area B. Along steep coastal slopes, valleys (up to 460 m/km2) are cut into the carbonates. The traces of episodic surface flows are visible in some of these valleys, in contrast to the valleys in area A. Remnants of a disrupted ancient fluvial network are clearly visible on the elevated karstic plateau in area B. Differences in the recent morphology are attributed mainly to varying thicknesses of the Palaeogene impermeable marly cover, and the intensity of tectonics in the two areas.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Projekti:
114-0822695-2568 - Procjena, umanjivanje i upravljanje geološkim hazardom u području Kvarnera (Benac, Čedomir, MZOS ) ( CroRIS)
119-1191152-1169 - Recentni sedimenti i fosilni okoliši jadranskog priobalja (Juračić, Mladen, MZOS ) ( CroRIS)
181-0000000-3199 - Građa facijesa i sekvencijalna stratigrafija Promina formacije u Dalmaciji (Matičec, Dubravko, MZOS ) ( CroRIS)
Ustanove:
Građevinski fakultet, Rijeka,
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut
Profili:
Igor Ružić
(autor)
Čedomir Benac
(autor)
Mladen Juračić
(autor)
Kristina Pikelj
(autor)
Dubravko Matičec
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus
Uključenost u ostale bibliografske baze podataka::
- Geobase
- Cambridge Scientific Abstracts
- PASCAL/CNRS
- Research Alert
- SCISEARCH
- Science Citation Index
- Scopus