prikaz prve stranice dokumenta Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)
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Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)
U: Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD), 2023. str. 295. urn:nbn:hr:169:167178
Kovačić, Marijan; Pavelić, Davor; Tibljaš, Darko; Galić, Ivo; Marković, Frane; Pavičić, Ivica

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Kovačić, M., Pavelić, D., Tibljaš, D., Galić, I., Marković, F. i Pavičić, I. (2023). Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia). Abstracts book / 36th International Meeting of Sedimentology (str. 295). Zagreb: Croatian Geological Society (HGD). Preuzeto s https://urn.nsk.hr/urn:nbn:hr:169:167178

Kovačić, Marijan, et al. "Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)." Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), 2023, str. 295. https://urn.nsk.hr/urn:nbn:hr:169:167178

Kovačić, Marijan, Davor Pavelić, Darko Tibljaš, Ivo Galić, Frane Marković i Ivica Pavičić. "Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)." U Abstracts book / 36th International Meeting of Sedimentology, 295. Zagreb: Croatian Geological Society (HGD), 2023. Citirano 13.10.2024.. https://urn.nsk.hr/urn:nbn:hr:169:167178

Kovačić, M., et al. (2023) 'Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)', Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), Zagreb, str. 295. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:169:167178 (Datum pristupa: 13.10.2024.)

Kovačić M, Pavelić D, Tibljaš D, Galić I, Marković F, Pavičić I. Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia). Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD); 2023. Str. 295-295. [pristupljeno 13.10.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:167178

M. Kovačić, D. Pavelić, D. Tibljaš, I. Galić, F. Marković i I. Pavičić, "Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)", Abstracts book / 36th International Meeting of Sedimentology Zagreb: Croatian Geological Society (HGD), 2023. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:167178 [Citirano: 13.10.2024.]

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Naslov (engleski)Sedimentological evidence of climatic changes during the Miocene Climatic Optimum in the North Croatian Basin (SW Pannonian Basin System, Croatia)
AutorMarijan Kovačić
AutorDavor Pavelić
AutorDarko Tibljaš
AutorIvo Galić
AutorFrane Marković
AutorIvica Pavičić
Autorova ustanovaSveučilište u Zagrebu
Prirodoslovno-matematički fakultet
(Geološki odsjek)
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za geologiju i geološko inženjerstvo)
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za rudarstvo i geotehniku)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
The North Croatian Basin (NCB) occupies the south-western part of the Pannonian Basin System, and belongs to the Central Paratethys realm. Detailed sedimentological field studies and mineralogical and petrological analyses showed that a 40 m thick section composed of well-bedded mixed, carbonate–siliciclastic deposits with occurrence of pyroclastics indicate three evolutional stages of lake development. The first evolutionary stage evolved in the late Early Miocene. It was characterised by mainly dolomite precipitation directly from the water body, and are associated with tuffites and marls, together with minerals such as analcime, hydrous Ca-bearing magnesium carbonate, and natrolite. This indicates deposition in a shallow, hydrologically closed lake of highly alkaline waters controlled by an arid climate. The second evolutionary stage is represented by the intercalation of dolomites and sandstones, indicating changes of hydrologically open and closed lacustrine environments as result of the frequent alternation arid and humid climates. The third stage, characterized by deposition of siliciclastics by gravity flows indicates the formation of a long-lived, hydrologically open lake that probably commenced in the Middle Miocene. The whole investigated lacustrine depositional sequence coincides with the Miocene Climatic Optimum generally characterized by hot and warm, and humid climates. However, the evolution of the closed lake that is correlative with similar lakes in northern Bosnia and central Serbia, indicates the existence of an arid zone in the region that was confined by areas characterized by a more humid climate in the late Early Miocene.
Jezikengleski
Vrsta publikacijeZnanstveni rad - Sažetak
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov zbornikaAbstracts book / 36th International Meeting of Sedimentology
Brojčani podacistr. 295
ISBN978-953-6907-79-3
URN:NBNurn:nbn:hr:169:167178
Datum objave publikacije2023
SkupNaziv: 36th International Meeting of Sedimentology
Kratica: IAS
Lokacija: Dubrovnik, Hrvatska
Organizator: Croatian Geological Society (HGD)
Organizator: International Association of Sedimentologists (IAS)
Datum početka: 2023-06-12
Datum završetka: 2023-06-16
Vrsta izlaganja: Postersko izlaganje
URL dokumentahttps://iasdubrovnik2023.org/index.php
Vrsta resursaTekst
IzdavačCroatian Geological Society (HGD)
Mjesto izdavanjaZagreb
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Zaštićeno autorskim pravom.
Datum i vrijeme pohrane2023-09-27 12:52:22