prikaz prve stranice dokumenta Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia
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Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia
International Journal of Earth Sciences, 112 (2023), 3; 1023-1041. https://doi.org/10.1007/s00531-023-02290-w
Špelić, Marko; Kovács, Ádám; Saftić, Bruno; Sztanó, Orsolya

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Špelić, M., Kovács, Á., Saftić, B. i Sztanó, O. (2023). Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia. International Journal of Earth Sciences, 112. (3), 1023-1041. doi: 10.1007/s00531-023-02290-w

Špelić, Marko, et al. "Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia." International Journal of Earth Sciences, vol. 112, br. 3, 2023, str. 1023-1041. https://doi.org/10.1007/s00531-023-02290-w

Špelić, Marko, Ádám Kovács, Bruno Saftić i Orsolya Sztanó. "Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia." International Journal of Earth Sciences 112, br. 3 (2023): 1023-1041. https://doi.org/10.1007/s00531-023-02290-w

Špelić, M., et al. (2023) 'Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia', International Journal of Earth Sciences, 112(3), str. 1023-1041. doi: 10.1007/s00531-023-02290-w

Špelić M, Kovács Á, Saftić B, Sztanó O. Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia. International Journal of Earth Sciences [Internet]. 24.01.2023. [pristupljeno 28.02.2025.];112(3):1023-1041. doi: 10.1007/s00531-023-02290-w

M. Špelić, Á. Kovács, B. Saftić i O. Sztanó, "Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia", International Journal of Earth Sciences, vol. 112, br. 3, str. 1023-1041, Siječanj 2023. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:924634. [Citirano: 28.02.2025.]

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Podaci o radu
Naslov (engleski)Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia
AutorMarko Špelić
AutorÁdám Kovács
AutorBruno Saftić
AutorOrsolya Sztanó
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 thick Lake Pannon sedimentary record provides insights into the downdip and lateral development of stratigraphic surfaces through the analysis of the basin-scale clinoform progradation. The clinoform architecture from the eastern part of the Drava Basin (Pannonian Basin System) was interpreted to reflect the base-level changes. A major downlap surface interpreted as a flooding event followed by rejuvenation of slope progradation was recognized on 2D seismic sections. Detailed 3D seismic interpretation combined with well data revealed that the large sigmoidal and the overlying small oblique clinoform sets that downlap the large one only apparently produce the geometry of a maximum flooding surface. Instead, the 3D mapping revealed the influence of two competing slope systems arriving from the north and northwest. Lateral switching of sediment input, similar to many recent deltaic systems. e.g., Danube and Po rivers led to the variability of stratigraphic surfaces, lithology, and thickness, which resulted in non-uniform shelf-edge migration. These observations were supported by forward stratigraphic modeling simulating different scenarios, which led to the generation of the depositional architecture with an apparent maximum flooding surface. This study also implies the potential pitfalls in basin analysis based only on scarce 2D seismic and emphasizes the role of lateral variations in sediment input controlling the depositional architecture.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaInternational Journal of Earth Sciences
Brojčani podacivol. 112, br. 3, str. 1023-1041
p-ISSN1437-3254
e-ISSN1437-3262
DOIhttps://doi.org/10.1007/s00531-023-02290-w
URN:NBNurn:nbn:hr:169:924634
Datum objave publikacije2023-01-24
ProjektŠifra: 809943
Naziv (engleski): Strengthening research in the Croatian Geological Survey: Geoscience-Twinning to develop state-of-the-art subsurface modelling capability and scientific impact
Kratica: GeoTwinn
Pravna nadležnost: eu
Financijer: Europska unija
Linija financiranja: Horizon 2020
ProjektŠifra: UIP-2019-04-3846
Naziv (hrvatski): GEOloška karakterizacija podzemlja istočnog dijela Dravske depresije s ciljem procjene Energetskog Potencijala
Naziv (engleski): GEOlogical characterization of the Eastern part of the Drava depression subsurface intended for the evaluation of Energy Potentials
Kratica: GEODEP
Voditelj: Marko Cvetković
Pravna nadležnost: Hrvatska
Financijer: Hrvatska zaklada za znanost
Linija financiranja: Installation Research Projects
URL dokumentahttps://link.springer.com/10.1007/s00531-023-02290-w
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje 4.0 međunarodna (CC BY 4.0)
Datum i vrijeme pohrane2025-02-28 08:54:04