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undergraduate thesis
Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori
Zagreb: University of Zagreb, Faculty of Science, 2022. urn:nbn:hr:217:416487
Tomić, Sandro
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Tomić, S. (2022). Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori (Undergraduate thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:416487

Tomić, Sandro. "Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori." Undergraduate thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:416487

Tomić, Sandro. "Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori." Undergraduate thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:416487

Tomić, S. (2022). 'Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori', Undergraduate thesis, University of Zagreb, Faculty of Science, accessed 29 April 2024, https://urn.nsk.hr/urn:nbn:hr:217:416487

Tomić S. Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori [Undergraduate thesis]. Zagreb: University of Zagreb, Faculty of Science; 2022 [cited 2024 April 29] Available at: https://urn.nsk.hr/urn:nbn:hr:217:416487

S. Tomić, "Sedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori", Undergraduate thesis, University of Zagreb, Faculty of Science, Zagreb, 2022. Available at: https://urn.nsk.hr/urn:nbn:hr:217:416487

Metadata
TitleSedimentološke značajke gornjomiocenskih naslaga kod Velikog Trojstva na Bilogori
Title (english)Sedimentological characteristics of Upper Miocene deposits from the Veliko Trojstvo locality, Bilogora Mt.
AuthorSandro Tomić
MentorMarijan Kovačić (mentor)
Committee memberMarijan Kovačić (predsjednik povjerenstva)
Committee memberFrane Marković (član povjerenstva)
Committee memberKarmen Fio Firi (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2022-09-22, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Mineralogy and Petrology
Abstract
Na prostoru zapadnog dijela Bilogore u okolici Velikog Trojstva uzeti su uzorci pijeska miocenske starosti s lokaliteta Manduševac i Lipov Brijeg s ciljem utvrđivanja njihovog granulometrijskog sastava i sastava lake mineralne frakcije. Rezultati granulometrijskih analiza pokazali su da su uzorci s oba lokaliteta izgrađeni od podjednakog udjela čestica pijeska i pelitnih čestica. Analiza lake mineralne frakcije pokazala je da u oba uzorka prevladavaju čestice muskovita i kremena, a relativno su brojne karbonatne čestice. Na temelju analize granulometrijskog sastava i sastava lake mineralne frakcije zaključeno je da su analizirani miocenski pijesci mineraloški i strukturno srednje zreli do zreli i da po tim značajkama odgovaraju pijescima gornjomiocenske starosti sa šireg prostora Sjevernohrvatskog bazena. Porijeklo tih pijesaka veže se uz udaljena izvorišta u istočnim Alpama i Zapadnim Karpatima, a taloženi su na deltnim ušćima u Panonsko jezero.
Abstract (english)
On the territory of the western part of Bilogora in the vicinity of the Veliko Trojstvo, samples of the sand of miocene age were taken from the site of Manduševac and Lipov Brijeg with the aim of determining their granulometric composition and composition of the light mineral fraction. The results of granulometric analyses showed that samples from both sites were built from an equal proportion of sand particles and pelitic particles. Analysis of the light mineral fraction showed that in both samples, muscovite and quartz particles predominate, and there are relatively numerous carbonate particles. Based on the analysis of the granulometric composition and composition of the light mineral fraction, we concluded that the analyzed Miocene sands are mineralogically and structurally medium ripe to mature and that they correspond to the sands of Upper-Miocene age from the wider area of the North Croatian Basin. The origin of these sand is associated with distant terrains in the eastern Alps and western Carpathians, and the deposition took place in the delta systems of the Pannonian lake.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:416487
ProjectNumber: IP-2019-04-7042
Title: Taložni paleobazeni, vodeni prolazi i migracije biote
Title: Sedimentary paleobasins, water corridors and biota migrations
Acronym: SEDBAS
Leader: Marijan Kovačić
Jurisdiction: Croatia
Funder: HRZZ
Funding stream: IP
Study programmeTitle: Undergraduate university study of Geology
Study programme type: university
Study level: undergraduate
Academic / professional title: sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) geologije (sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) geologije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
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Created on2023-01-16 11:50:56