prikaz prve stranice dokumenta Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System
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Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System
U: Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD), 2023. str. 520. urn:nbn:hr:169:931588
Baketarić, Tomislav; Vranjković, Alan; Majstorović-Bušić, Ana; Marić-Đureković, Željka; Pavelić, Davor

Institucijski repozitorij: Repozitorij Rudarsko-geološko-naftnog fakulteta Sveučilišta u Zagrebu

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Baketarić, T., Vranjković, A., Majstorović Bušić, A., Marić Đureković, Ž. i Pavelić, D. (2023). Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System. Abstracts book / 36th International Meeting of Sedimentology (str. 520). Zagreb: Croatian Geological Society (HGD). Preuzeto s https://urn.nsk.hr/urn:nbn:hr:169:931588

Baketarić, Tomislav, et al. "Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System." Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), 2023, str. 520. https://urn.nsk.hr/urn:nbn:hr:169:931588

Baketarić, Tomislav, Alan Vranjković, Ana Majstorović Bušić, Željka Marić Đureković i Davor Pavelić. "Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System." U Abstracts book / 36th International Meeting of Sedimentology, 520. Zagreb: Croatian Geological Society (HGD), 2023. Citirano 01.12.2024.. https://urn.nsk.hr/urn:nbn:hr:169:931588

Baketarić, T., et al. (2023) 'Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System', Abstracts book / 36th International Meeting of Sedimentology, Croatian Geological Society (HGD), Zagreb, str. 520. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:169:931588 (Datum pristupa: 01.12.2024.)

Baketarić T, Vranjković A, Majstorović Bušić A, Marić Đureković Ž, Pavelić D. Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System. Abstracts book / 36th International Meeting of Sedimentology. Zagreb: Croatian Geological Society (HGD); 2023. Str. 520-520. [pristupljeno 01.12.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:931588

T. Baketarić, A. Vranjković, A. Majstorović Bušić, Ž. Marić Đureković i D. Pavelić, "Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System", Abstracts book / 36th International Meeting of Sedimentology Zagreb: Croatian Geological Society (HGD), 2023. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:931588 [Citirano: 01.12.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:931588
Podaci o radu
Naslov (engleski)Seismic geomorphology of Pannonian clastic reservoirs in Drava and Zala Basins, Pannonian Basin System
AutorTomislav Baketarić
AutorAlan Vranjković
AutorAna Majstorović-Bušić
AutorŽeljka Marić-Đureković
AutorDavor Pavelić
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)
Mature basins provide a wealth of data for the reconstruction and mapping of their sedimentary evolution and architecture as well as regional paleo-geographic changes. In turn, these often lead to a better understanding of geological processes and thus provide a basis for novel concepts in exploration of subsurface. The Neogene Pannonian Basin System (PBS) nested between the Dinarides, Alps and the Carpathian arc in Central Europe is such a mature area with more than a century hydrocarbon exploration and production history. The upper Miocene to Pliocene sediments, referred to as Pannonian Stage, were initially deposited in an under-filled lake basin displaying gradual transgression followed by a powerful regression characterized by prograding and aggrading clinoforms on reflection seismic data. Relative chronostratigraphic framework was defined by clinoform sets mapped along with their rollover points across Drava and Zala basins. Based on seismic attributes, log patterns and available core data, clastic depositional features and architectures were delineated across different depositional environments within lake basin clinoforms. Each depositional feature is described upon its position within clinoforms, type of clinoform trajectory and typical log pattern. Finally, depositional features are described in their typical sizes (based on 3D seismic data) and reservoir quality. Integrating various data resulted in more complete temporal and spatial development of depositional environments during clinoform deposition as well as depositional features. Mapping of the depositional features across clinoforms resulted in considerable range of reservoir sandbody types that can be recognized on 3D seismic within Pannonian Basin System.
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. 520
ISBN978-953-6907-79-3
URN:NBNurn:nbn:hr:169:931588
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 10:15:00