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

Institutional repository: Faculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb

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Rukavina, D., Saftić, B., Kolenković Močilac, 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 (p. 509). Zagreb: Croatian Geological Society (HGD). Retrieved from 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, p. 509. https://urn.nsk.hr/urn:nbn:hr:169:380262

Rukavina, David, Bruno Saftić, Iva Kolenković Močilac and Marko Cvetković. "Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system." In Abstracts book / 36th International Meeting of Sedimentology, 509. Zagreb: Croatian Geological Society (HGD), 2023. Accessed 2024 November 23. 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, p. 509. Available at: https://urn.nsk.hr/urn:nbn:hr:169:380262 (Accessed 23 November 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. Pp. 509-509. [cited 2024 November 23] Available at: https://urn.nsk.hr/urn:nbn:hr:169:380262

D. Rukavina, B. Saftić, I. Kolenković Močilac and 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] Available at: https://urn.nsk.hr/urn:nbn:hr:169:380262 [Accessed: 23 November 2024]

Metadata
Title (english)Sequence stratigraphy of the Pliocene–Pleistocene infill in the southern part of the Adriatic foredeep system
AuthorDavid Rukavina
AuthorBruno Saftić
AuthorIva Kolenković Močilac
AuthorMarko Cvetković
Author's institutionUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Abstract (english)
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.
Languageenglish
Publication typeScientific paper - Abstract
Publication statusPublished
Peer reviewPeer review - international
Publication versionPublished version
Publication titleAbstracts book / 36th International Meeting of Sedimentology
Numberingp. 509
ISBN978-953-6907-79-3
URN:NBNurn:nbn:hr:169:380262
Publication2023
ConferenceTitle: 36th International Meeting of Sedimentology
Acronym: IAS
Location: Dubrovnik, Croatia
Organizer: Croatian Geological Society (HGD)
Organizer: International Association of Sedimentologists (IAS)
Start date: 2023-06-12
End date: 2023-06-16
Assembly type: Lecture
Document URLhttps://iasdubrovnik2023.org/index.php
Type of resourceText
PublisherCroatian Geological Society (HGD)
Publishing placeZagreb
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2023-09-28 09:51:18