prikaz prve stranice dokumenta Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System
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Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System
Geologica Carpathica, 74 (2023), 2; 155-179. https://doi.org/10.31577/GeolCarp.2023.06
Matošević, Mario; Marković, Frane; Bigunac, Dijana; Šuica, Sanja; Krizmanić, Krešimir; Perković, Adaleta; Kovačić, Marijan; Pavelić, Davor

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Matošević, M., Marković, F., Bigunac, D., Šuica, S., Krizmanić, K., Perković, A. ... Pavelić, D. (2023). Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System. Geologica Carpathica, 74. (2), 155-179. doi: 10.31577/GeolCarp.2023.06

Matošević, Mario, et al. "Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System." Geologica Carpathica, vol. 74, br. 2, 2023, str. 155-179. https://doi.org/10.31577/GeolCarp.2023.06

Matošević, Mario, Frane Marković, Dijana Bigunac, Sanja Šuica, Krešimir Krizmanić, Adaleta Perković, Marijan Kovačić i Davor Pavelić. "Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System." Geologica Carpathica 74, br. 2 (2023): 155-179. https://doi.org/10.31577/GeolCarp.2023.06

Matošević, M., et al. (2023) 'Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System', Geologica Carpathica, 74(2), str. 155-179. doi: 10.31577/GeolCarp.2023.06

Matošević M, Marković F, Bigunac D, Šuica S, Krizmanić K, Perković A, i sur.. Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System. Geologica Carpathica [Internet]. 01.06.2023. [pristupljeno 21.03.2025.];74(2):155-179. doi: 10.31577/GeolCarp.2023.06

M. Matošević, et al., "Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System", Geologica Carpathica, vol. 74, br. 2, str. 155-179, Lipanj 2023. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:393697. [Citirano: 21.03.2025.]

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Naslov (engleski)Petrography of the Upper Miocene sandstones from the North Croatian Basin : understanding the genesis of the largest reservoirs in the southwestern part of the Pannonian Basin System
AutorMario Matošević
AutorFrane Marković
AutorDijana Bigunac
AutorSanja Šuica
AutorKrešimir Krizmanić
AutorAdaleta Perković
AutorMarijan Kovačić
AutorDavor Pavelić
Autorova ustanovaSveučilište u Zagrebu
Prirodoslovno-matematički fakultet
(Geološki odsjek)
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)
This paper presents a petrographic study of the Upper Miocene sandstones from exploration wells in the Sava and Drava Depressions in the North Croatian Basin (SW of the Pannonian Basin System), Central Europe. These sandstones represent the most important reservoir rocks for oil and gas in Croatia. A total of 130 core samples from depths of more than 3000 m were examined. The sandstones generally have a feldspatho–litho–quartzose (fLQ) composition. The modal composition of samples from the Sava... Više Depression is Q39.2–61.0F8.9–26.0L26.1–42.3, and Q40.6–63.5F6.6–23.3L20.9–42.3 for those from the Drava Depression. Lithic fragments are dominated by extrabasinal carbonates with subordinate metamorphic grains (mostly schists) and less frequent magmatics (granitoids). Garnet, tourmaline, apatite, rutile, epidote, clinozoisite, zoisite, titanite, zircon, staurolite, and opaque minerals form the heavy mineral association and imply an area of provenance dominated by metamorphic rocks. The tectonic setting of the sandstones corresponds to recycled orogen, i.e., a subduction complex or fold-thrust belt. There are no significant compositional differences between the sandstone samples from the two depressions, thus indicating a common main source area and similar diagenetic processes in the subsurface. The sandstones originated from eroded parts of the uplifted Alpine–Carpathian fold belt and are distinct from the Lower and Middle Miocene sandstones in the North Croatian Basin. Observed variations in the sandstones’ composition with regards to geographic location and depth are associated with variations in the erosion of parent rocks, including subsequent modification of detrital sediment during transport, mixing, and deposition, as well as burial diagenesis. The Sava and Drava Depressions were part of Lake Pannon in the Late Miocene with no significant topographical obstacles between them for the inflow of the detritus. The study will therefore help with the correlation of the Upper Miocene reservoir rocks in various parts of the North Croatian Basin (as well as adjacent parts of the Pannonian Basin System) and thereby assist with future hydrocarbon exploration in this area. Sakrij dio sažetka
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaGeologica Carpathica
Brojčani podacivol. 74, br. 2, str. 155-179
p-ISSN1335-0552
DOIhttps://doi.org/10.31577/GeolCarp.2023.06
URN:NBNurn:nbn:hr:169:393697
Datum objave publikacije2023-06-01
ProjektŠifra: IP-2019-04-7042
Naziv (hrvatski): Taložni paleobazeni, vodeni prolazi i migracije biote
Naziv (engleski): Sedimentary paleobasins, water corridors and biota migrations
Kratica: SEDBAS
Voditelj: Marijan Kovačić
Pravna nadležnost: Hrvatska
Financijer: Hrvatska zaklada za znanost
Linija financiranja: Research Projects
URL dokumentahttps://geologicacarpathica.com/browse/archive/?journal_article_no=30713
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje-Nekomercijalno-Bez prerada 4.0 međunarodna (CC BY-NC-ND 4.0)
Datum i vrijeme pohrane2025-02-24 09:41:09
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