prikaz prve stranice dokumenta Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)
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Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)
U: Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin / Korbar, Tvrtko; Kovačić, Marijan; Vlahović, Igor (ur.). Zagreb: Hrvatsko geološko društvo (HGD), 2023. str. 143-158. urn:nbn:hr:245:631625
Korbar, Tvrtko; Belak, Mirko; Fuček, Ladislav; Španiček, Jelena; Steuber, Thomas

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Korbar, T., Belak, M., Fuček, L., Španiček, J. i Steuber, T. (2023). Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia). U T. Korbar, (Ur.), M. Kovačić, (Ur.), I. Vlahović, (Ur.), Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin (str. 143-158). Zagreb: Hrvatsko geološko društvo (HGD). Preuzeto s https://urn.nsk.hr/urn:nbn:hr:245:631625

Korbar, Tvrtko, et al. "Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)." Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, Ur. Tvrtko Korbar, Ur. Marijan Kovačić, Ur. Igor Vlahović, Hrvatsko geološko društvo (HGD), 2023, str. 143-158. https://urn.nsk.hr/urn:nbn:hr:245:631625

Korbar, Tvrtko, Mirko Belak, Ladislav Fuček, Jelena Španiček i Thomas Steuber. "Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)." U Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, ur. Tvrtko Korbar, ur. Marijan Kovačić, ur. Igor Vlahović, 143-158. Zagreb: Hrvatsko geološko društvo (HGD), 2023. https://urn.nsk.hr/urn:nbn:hr:245:631625

Korbar, T., et al. (2023) 'Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)' u Korbar, T. (ur.), Kovačić, M. (ur.), Vlahović, I. (ur.) Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin Zagreb: Hrvatsko geološko društvo (HGD), str. 143-158. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:245:631625 (Datum pristupa: 10.05.2024.)

Korbar T, Belak M, Fuček L, Španiček J, Steuber T. Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia). U: T. Korbar, ur., M. Kovačić, ur., I. Vlahović, ur. Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin. Zagreb: Hrvatsko geološko društvo (HGD); 2023. Str. 143-158. [pristupljeno 10.05.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:245:631625

T. Korbar, M. Belak, L. Fuček, J. Španiček i T. Steuber, "Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)", Sedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, T. Korbar, M. Kovačić i I. Vlahović, Ur. Zagreb: Hrvatsko geološko društvo (HGD), 2023, str. 143-158. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:245:631625

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Naslov (engleski)Volcano-sedimentary-evaporitic rocks from an aborted Triassic rift and Cretaceous to Palaeogene Adriatic Carbonate Platform successions: OAEs, K–Pg boundary and the Palaeocene platform top (central Dalmatian islands, Croatia)
AutorTvrtko Korbar
AutorMirko Belak
AutorLadislav Fuček
AutorJelena Španiček
AutorThomas Steuber
UrednikTvrtko Korbar
UrednikMarijan Kovačić
UrednikIgor Vlahović
Autorova ustanovaHrvatski geološki institut
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Geologija i paleontologija
Sažetak (engleski)
The central Adriatic Vis archipelago was in 2019 recognized as a UNESCO Global Geopark. The islands are characterized by the oldest and the youngest rocks in the Adriatic, owing to salt tectonics that characterize the area. Salt diapirs are the most prominent subsurface tectonic structures in the central part of the Adriatic, built of once deeply buried volcano-sedimentary-evaporitic rocks deposited during the middle Triassic rifting stage of the Adriatic microplate (Adria). The subtropical Adriatic Carbonate Platform (AdCP) existed during most of the Mesozoic in the central part of the then more spacious Adria. The NE part of the AdCP has been incorporated into the Dinarides fold-and-thrust belt during the Palaeogene while the SW part remained relatively undeformed within the Adriatic foreland, which is mostly covered by the Neogene clastic deposits and by the sea since the Holocene. The diapirs include complexes of various Triassic rocks, which in places uplifted, and even pierced, a few kilometres thick AdCP succession, e.g., Komiža Bay on the island of Vis. As a consequence, an up to 1500 m-thick succession of the Cretaceous shallow- water carbonates is exposed on the flanks of the Komiža diapir. While pre- and post-Aptian successions are characterized by monotonous peritidal cycles, the Lower Aptian is marked by prominent facies diversification because of the perturbations related to the onset of the Ocean Anoxic Event 1a (OAE 1a), and the upper part is characterized by a regional subaerial exposure. OAE 2 is only incompletely recorded within the Cenomanian–Turonian succession on the islands of Vis and Biševo, as a consequence of local emergence of the platform top during the event, that is followed by a relatively short period of deposition until the Coniacian, when the SW part of the AdCP emerged. In the NE part of the platform the deposition continued until the Maastrichtian, and in places even into the Palaeocene. Thus, the Cretaceous–Palaeogene (K–Pg) boundary event is recorded within rare successions deposited on tidal flats (Hvar island) or in inner-platform lagoons (Brač island), but there is still debate on the origin of the specific boundary layer. The AdCP top is characterized by a major subaerial exposure, during which distinct discontinuity surfaces have been formed, and it is unconformably overlain by diachronous Eocene Foraminiferal Limestones that were deposited on a distal ramp of the once migrating Dinaric foreland basin.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Poglavlje u knjizi
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov knjigeSedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin
Brojčani podacistr. 143-158
ISBN978-953-6907-80-9
URN:NBNurn:nbn:hr:245:631625
Datum objave publikacije2023-06-12
Vrsta resursaTekst
IzdavačHrvatsko geološko društvo (HGD)
Mjesto izdavanjaZagreb
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Zaštićeno autorskim pravom.
Datum i vrijeme pohrane2024-01-24 08:20:50