prikaz prve stranice dokumenta Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System
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Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System
Marine and Petroleum Geology, 152 (2023); 106235. https://doi.org/10.1016/j.marpetgeo.2023.106235
Rukavina, David; Saftić, Bruno; Matoš, Bojan; Kolenković Močilac, Iva; Premec Fuček, Vlasta; Cvetković, Marko

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Rukavina, D., Saftić, B., Matoš, B., Kolenković Močilac, I., Premec Fuček, V. i Cvetković, M. (2023). Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System. Marine and Petroleum Geology, 152.. doi: 10.1016/j.marpetgeo.2023.106235

Rukavina, David, et al. "Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System." Marine and Petroleum Geology, vol. 152, 2023. https://doi.org/10.1016/j.marpetgeo.2023.106235

Rukavina, David, Bruno Saftić, Bojan Matoš, Iva Kolenković Močilac, Vlasta Premec Fuček i Marko Cvetković. "Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System." Marine and Petroleum Geology 152 (2023). https://doi.org/10.1016/j.marpetgeo.2023.106235

Rukavina, D., et al. (2023) 'Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System', Marine and Petroleum Geology, 152. doi: 10.1016/j.marpetgeo.2023.106235

Rukavina D, Saftić B, Matoš B, Kolenković Močilac I, Premec Fuček V, Cvetković M. Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System. Marine and Petroleum Geology [Internet]. 06.2023. [pristupljeno 27.02.2025.];152. doi: 10.1016/j.marpetgeo.2023.106235

D. Rukavina, B. Saftić, B. Matoš, I. Kolenković Močilac, V. Premec Fuček i M. Cvetković, "Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System", Marine and Petroleum Geology, vol. 152, Lipanj 2023. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:241938. [Citirano: 27.02.2025.]

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Naslov (engleski)Tectonostratigraphic analysis of the syn-rift infill in the Drava Basin, southwestern Pannonian Basin System
AutorDavid Rukavina
AutorBruno Saftić
AutorBojan Matoš
AutorIva Kolenković Močilac
AutorVlasta Premec Fuček
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 Drava Basin in the SW Pannonian Basin System (PBS) was initially formed by passive rifting with accompanying sedimentary infill. Although this has been the subject of much previous work, an account of tectonic control has been lacking. Based on cores, wire logging, and seismic data, the tectonostratigraphic interpretation, depositional systems, and control on depositional systems of the syn-rift infill of the eastern part of the Drava Basin were studied. The rifting phase is characterised by the formation of half-grabens, grabens, a sag, and supradetachment basin structures with structural ramp and structural highs. The syn-rift infill can be divided into second-order tectonostratigraphic sequences corresponding to the early and late rift stages. The second-order sequences are further subdivided into third-order tectonostratigraphic sequences formed in response to higher-order tectonic events associated with local rift migration. In contrast to the early-stage structures, the latestage rift structures are primarily controlled by extensional detachments that represent parts of the Drava Rift Fault System (DRFS). The early syn-rift is characterised by continental deposition through alluvial fans, fan deltas, and lacustrine environments. The late syn-rift stage is characterised by marine deposition in shallow water, fan deltas, and submarine slope-aprons, with deep marine sedimentation and intense volcanic activity. The ramp, basin slopes, and fault scarp slopes represent the major sediment transport pathways involved in the formation of alluvial fans, fan deltas, or submarine slope-aprons. Basinal sedimentation and major depocenters are located within synforms formed by structural lows in the geometry of extensional detachments. This study gives an example of syn-rift tectonic control for the SW part of the PBS and the influence of detachment geometry on basin fill. We have presented an approach based on 3D seismostratigraphic interpretation of tectonostratigraphic sequences, and the correlation of seismic facies with depositional environments developed in a back-arc setting.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaMarine and Petroleum Geology
Brojčani podacivol. 152, 106235
p-ISSN0264-8172
DOIhttps://doi.org/10.1016/j.marpetgeo.2023.106235
URN:NBNurn:nbn:hr:169:241938
Datum objave publikacije2023-06
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
ProjektŠifra: 653718
Naziv (engleski): ENabling Onshore CO2 Storage in Europe
Kratica: ENOS
Pravna nadležnost: eu
Financijer: EC
Linija financiranja: H2020
URL dokumentahttps://linkinghub.elsevier.com/retrieve/pii/S0264817223001411
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje-Nekomercijalno-Bez prerada 4.0 međunarodna (CC BY-NC-ND 4.0)
Datum i vrijeme pohrane2025-02-27 11:35:31