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master's thesis
Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.
Zagreb: University of Zagreb, Faculty of Science, 2020. urn:nbn:hr:217:088549
Zadravec, Jure
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Zadravec, J. (2020). Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore. (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:088549

Zadravec, Jure. "Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.." Master's thesis, University of Zagreb, Faculty of Science, 2020. https://urn.nsk.hr/urn:nbn:hr:217:088549

Zadravec, Jure. "Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.." Master's thesis, University of Zagreb, Faculty of Science, 2020. https://urn.nsk.hr/urn:nbn:hr:217:088549

Zadravec, J. (2020). 'Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.', Master's thesis, University of Zagreb, Faculty of Science, accessed 29 April 2024, https://urn.nsk.hr/urn:nbn:hr:217:088549

Zadravec J. Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore. [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2020 [cited 2024 April 29] Available at: https://urn.nsk.hr/urn:nbn:hr:217:088549

J. Zadravec, "Usporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2020. Available at: https://urn.nsk.hr/urn:nbn:hr:217:088549

Metadata
TitleUsporedba petrografskog sastava paleogenskih pješčenjaka Banovine i Požeške gore.
Title (english)Comparison of petrographic composition of Paleogene sandstones from Banovina and Požeška gora.
AuthorJure Zadravec
MentorBorna Lužar-Oberiter (mentor)
Committee memberBorna Lužar-Oberiter (predsjednik povjerenstva)
Committee memberKatarina Gobo (član povjerenstva)
Committee memberMarijan Kovačić (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2020-02-28, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
Glavni cilj ovoga rada je usporedba sastava uzoraka pješčenjaka sa Zrinske i Požeške gore, sličnih sedimentoloških karakteristika te paleogenske starosti, koja pruža bitan uvid u njihove provenijencije. Analizirani su uzorci pješčenjaka uzeti sa izdanaka paleogenskih naslaga u blizini Gornje Bačuge kod Petrinje i u dolini potoka Stupnica na Zrinskoj gori, te sela Škrabutnik na Požeškoj gori. Iz uzoraka su izrađeni petrografski preparati na kojima je provedena kvantitativna analiza petrografskog sastava Gazzi- Dickinson-ovom metodom. Napravljena je usporedba rezultata mikroskopiranja te brojanja zrna iz uzoraka sa dva istraživana područja te su podaci interpretirani u smislu regionalnog geotektonskog smještaja. Rezultatima je dokazano da istraživani paleogenski pješčenjaci imaju slična izvorišta materijala, koji većinom potječe od erodiranog vulkanskog luka. Te naslage ugradile su se u akrecijsku prizmu koju danas predstavlja Sava zona. Također, postoji mogućnost da su naslage formirane u istom taložnom bazenu.
Abstract (english)
The main objective of this thesis is the composition comparison of the seemingly similar sanstone samples of Paleogene age from Požeška and Zrinska gora, which provides important insights into their provenance. The collected sandstone samples from the Palaeogene deposits of Gornja Bačuga in the vicinity of Petrinja, the and the village of Škrabutnik atop the Požeška gora were analysed. The samples were processed into thin sections, which were quantitively analysed using the Gazzi-Dickinson method. The final results from the two researched areas were compared, and the data interpreted in a way it would provide useful information about the regional geotectonic setting. The results have proven that the researched sandstones have had similar provenance. The detrital material is mostly made up from an eroded magmatic arc. The deposits have been embed into an accretionary prism, which is today represented by the Sava zone. There is also a possibility that the deposits were formed in the same sedimentation basin.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:088549
Study programmeTitle: Graduate university study of Geology
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geologije (magistar/magistra geologije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2020-03-10 11:56:22