Pregled bibliografske jedinice broj: 649353
Lower Cretaceous carbonate gravity-flow deposits from the Bohinj area (NW Slovenia) : evidence of a lost carbonate platform in the Internal Dinarides
Lower Cretaceous carbonate gravity-flow deposits from the Bohinj area (NW Slovenia) : evidence of a lost carbonate platform in the Internal Dinarides // Bulletin de la Société géologique de France, 183 (2012), 4; 383-392 doi:10.2113/gssgfbull.183.4.383 (međunarodna recenzija, članak, znanstveni)
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Naslov
Lower Cretaceous carbonate gravity-flow deposits from the Bohinj area (NW Slovenia) : evidence of a lost carbonate platform in the Internal Dinarides
Autori
Kukoč, Duje ; Goričan, Špela ; Košir, Adrijan
Izvornik
Bulletin de la Société géologique de France (0037-9409) 183
(2012), 4;
383-392
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Biancone limestone; Calcareous breccia; Radiolarians; Berriasian; Bled basin; Bohinj Formation
Sažetak
In the Bohinj area (NW Slovenia), a distinctive interval of carbonate gravity-flow deposits overlying the pelagic Biancone limestone was analyzed for microfacies and dated with radiolarians. This interval, newly described as the Bohinj Formation, consists of a 3-m-thick carbonate breccia capped by a 4-m-thick massive calcarenite. The breccia is composed of clasts of carbonate platform facies, isolated ooids and oncoids, and bioclasts of shallow-marine benthos. Intraclasts of pelagic calpionellid wackestone and rare chert clasts are also present. Radiolarians from the pelagic limestone below indicate a latest Tithonian to earliest Berriasian age, and those above indicate a Berriasian to Early Valanginian age. Paleogeographically, the area was part of the Bled Basin, which had a relatively distal position on the Adriatic continental margin. This position is suggested by flysch-type deposits in the area that are Early Cretaceous in age and thus correlate with the Bosnian Flysch in the central Dinarides. The Bohinj Formation provides evidence of a carbonate platform that must have been located more internally but is now not preserved. This inferred platform (named the Bohinj Carbonate Platform) may have developed on top of a nappe stack, which formed during the early emplacement of the internal Dinaric units onto the continental margin. The platform correlates regionally with genetically similar isolated carbonate platforms of the Alpine – Dinaride – Carpathian orogenic system, e.g., with the Plassen Carbonate Platform in the Northern Calcareous Alps and the Kurbnesh Carbonate Platform in Albania.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119-1191152-1171 - Uloga taložnih prekida u karbonatnim sukcesijama Krških Dinarida (Bucković, Damir, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Duje Kukoč
(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