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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


Kukoč, Duje; Goričan, Špela; Košir, Adrijan
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:

Avatar Url Duje Kukoč (autor)

Poveznice na cjeloviti tekst rada:

doi bsgf.geoscienceworld.org bsgf.geoscienceworld.org

Citiraj ovu publikaciju:

Kukoč, Duje; Goričan, Špela; Košir, Adrijan
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)
Kukoč, D., Goričan, Š. & Košir, A. (2012) 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 (4), 383-392 doi:10.2113/gssgfbull.183.4.383.
@article{article, author = {Kuko\v{c}, Duje and Gori\v{c}an, \v{S}pela and Ko\v{s}ir, Adrijan}, year = {2012}, pages = {383-392}, DOI = {10.2113/gssgfbull.183.4.383}, keywords = {Biancone limestone, Calcareous breccia, Radiolarians, Berriasian, Bled basin, Bohinj Formation}, journal = {Bulletin de la Soci\'{e}t\'{e} g\'{e}ologique de France}, doi = {10.2113/gssgfbull.183.4.383}, volume = {183}, number = {4}, issn = {0037-9409}, title = {Lower Cretaceous carbonate gravity-flow deposits from the Bohinj area (NW Slovenia) : evidence of a lost carbonate platform in the Internal Dinarides}, keyword = {Biancone limestone, Calcareous breccia, Radiolarians, Berriasian, Bled basin, Bohinj Formation} }
@article{article, author = {Kuko\v{c}, Duje and Gori\v{c}an, \v{S}pela and Ko\v{s}ir, Adrijan}, year = {2012}, pages = {383-392}, DOI = {10.2113/gssgfbull.183.4.383}, keywords = {Biancone limestone, Calcareous breccia, Radiolarians, Berriasian, Bled basin, Bohinj Formation}, journal = {Bulletin de la Soci\'{e}t\'{e} g\'{e}ologique de France}, doi = {10.2113/gssgfbull.183.4.383}, volume = {183}, number = {4}, issn = {0037-9409}, title = {Lower Cretaceous carbonate gravity-flow deposits from the Bohinj area (NW Slovenia) : evidence of a lost carbonate platform in the Internal Dinarides}, keyword = {Biancone limestone, Calcareous breccia, Radiolarians, Berriasian, Bled basin, Bohinj Formation} }

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


Citati:





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