prikaz prve stranice dokumenta Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system
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Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system
U: Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD), 2023. str. 509. urn:nbn:hr:169:380262
Rukavina, David; Saftić, Bruno; Kolenković Močilac, Iva; Cvetković, Marko

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Rukavina, D., Saftić, B., Kolenković Močilac, I. i Cvetković, M. (2023). Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system. Abstracts book / 36th International Meeting of Sedimentology (str. 509). Zagreb: Croatian Geological Society (HGD). Preuzeto s https://urn.nsk.hr/urn:nbn:hr:169:380262

Rukavina, David, et al. "Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system." Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), 2023, str. 509. https://urn.nsk.hr/urn:nbn:hr:169:380262

Rukavina, David, Bruno Saftić, Iva Kolenković Močilac i Marko Cvetković. "Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system." U Abstracts book / 36th International Meeting of Sedimentology, 509. Zagreb: Croatian Geological Society (HGD), 2023. Citirano 28.04.2024.. https://urn.nsk.hr/urn:nbn:hr:169:380262

Rukavina, D., et al. (2023) 'Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system', Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), Zagreb, str. 509. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:169:380262 (Datum pristupa: 28.04.2024.)

Rukavina D, Saftić B, Kolenković Močilac I, Cvetković M. Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system. Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD); 2023. Str. 509-509. [pristupljeno 28.04.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:380262

D. Rukavina, B. Saftić, I. Kolenković Močilac i M. Cvetković, "Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system", Abstracts book / 36th International Meeting of Sedimentology Zagreb: Croatian Geological Society (HGD), 2023. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:380262 [Citirano: 28.04.2024.]

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Naslov (engleski)Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system
AutorDavid Rukavina
AutorBruno Saftić
AutorIva Kolenković Močilac
AutorMarko Cvetković
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za geologiju i geološko inženjerstvo)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
The evolution of the foreland basin sediments in the Adriatic (Messinian–Quaternary) foredeep system was controlled by the Meso and Neoalpine emersed chain. Croatia’s southern part of this system comprises the Palagruža Trough and South Adriatic Basin filled with marine clastic succession. Our study, in this area, aims to reconstruct the shelf-edge trajectories and sequence stratigraphy to describe the migration of the depositional systems. The study integrates published geological maps, well logs and reports, and 2D seismic sections. Mappable seismic facies are defined and correlated with sedimentological facies and depositional processes. Both, ascending and descending shelf-edge trajectories are defined. Ascending trajectories are associated with transgressive and highstand system tracts. Descending trajectories are associated with forced regression and the presence of extensive erosional surface on the shelf. Overall progradation characterizes Pliocene and Pleistocene sediments, first filling the Palagruža Trough in the SW direction and then SE progradation towards the South Adriatic Basin. The progradation pattern is interrupted by a base-level rise at the end of the Pliocene. Analysing the main sediment transport directions, the two third-order unconformity-bounded stratigraphic units are interpreted. Especially interesting are results about nearby Pliocene–Pleistocene clastic depositional systems and processes that shaped the southern part of the Adriatic Sea. These results highlight the stratigraphic and tectonic evolution of the Adriatic foredeep’s southern part, providing the records of the regional and global controls driven by the local tectonics and emersion, basin migration and subsequent basin infill.
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. 509
ISBN978-953-6907-79-3
URN:NBNurn:nbn:hr:169:380262
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: Predavanje
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 pohrane2023-09-28 09:51:18