Pregled bibliografske jedinice broj: 583965
Jurassic carbonates of western Gorski kotar (Karst Dinarides - Croatia) as sedimentary signature of geodynamics within the inner Adriatic carbonate platform realm
Jurassic carbonates of western Gorski kotar (Karst Dinarides - Croatia) as sedimentary signature of geodynamics within the inner Adriatic carbonate platform realm // 20th International Karstological School “Classical Karst” ; Karst Forms and Processes, Guide Book & Abstracts / Mihevc, Andrej ; Gabrovšek, Franci (ur.).
Postojna: Karst Research Institute - ZRC SAZU, 2012. (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Jurassic carbonates of western Gorski kotar (Karst Dinarides - Croatia) as sedimentary signature of geodynamics within the inner Adriatic carbonate platform realm
Autori
Bucković, Damir ; Markić, Ana
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
20th International Karstological School “Classical Karst” ; Karst Forms and Processes, Guide Book & Abstracts
/ Mihevc, Andrej ; Gabrovšek, Franci - Postojna : Karst Research Institute - ZRC SAZU, 2012
Skup
20th International Karstological School “Classical Karst”
Mjesto i datum
Postojna, Slovenija, 18.06.2012. - 22.06.2012
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Jurassic; Karst Dinarides; geodynamics; Adriatic carbonate platform; Croatia
Sažetak
The Jurassic succession of Gorski Kotar reveals typical sedimentary signature of inner Adriatic carbonate platform realm. Due to its facies characteristics, eleven informal lithofacies units can be distinguished. Their origin is grouped into three depositional settings that alternated over the spacious Adriatic platform area during the Jurassic. These are: (1) subtidal below the fair-weather wave-base to higher-energy subtidal above the fair-weather wave-base ; (2) subtidal below the fair-weather wave-base with episodic higher-energy influences ; (3) peritidal. The alteration of depositional settings reflects periods of intensive regional large-scale tectonic movements during the geodynamic evolution of the Western Neo-Tethys region, such as the opening/closing of the Dinaridic branch of the Neo-Tethys and opening of the Adriatic basin.
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:
Damir Bucković
(autor)