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master's thesis
Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski
Zagreb: University of Zagreb, Faculty of Science, 2022. urn:nbn:hr:217:878808
Mateša, Karlo
University of Zagreb
Faculty of Science
Department of Geology

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Mateša, K. (2022). Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:878808

Mateša, Karlo. "Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski." Master's thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:878808

Mateša, Karlo. "Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski." Master's thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:878808

Mateša, K. (2022). 'Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski', Master's thesis, University of Zagreb, Faculty of Science, accessed 19 January 2025, https://urn.nsk.hr/urn:nbn:hr:217:878808

Mateša K. Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2022 [cited 2025 January 19] Available at: https://urn.nsk.hr/urn:nbn:hr:217:878808

K. Mateša, "Usporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2022. Available at: https://urn.nsk.hr/urn:nbn:hr:217:878808

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Metadata
TitleUsporedba recentnih dravskih sedimenata sa sedimentima dravske riječne terase na lokalitetu Novigrad Podravski
Title (english)COMPARISON OF RECENT DRAVA RIVER SEDIMENTS WITH THE SEDIMENTS OF THE DRAVA RIVER TERRACE AT THE NOVIGRAD PODRAVSKI SITE
AuthorKarlo Mateša
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 country2022-02-23, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
Glavni cilj ovog diplomskog rada bio je usporediti recentne dravske sedimente sa sedimentima na lokalitetu Novigrad Podravski te im utvrditi porijeklo. U tu je svrhu obiđen i snimljen teren, uzorkovani su šljunci i pijesci te su napravljene granulometrijska i petrografska analiza te analiza teške mineralne frakcije. Rezultati petrografske analize i analize teških minerala ukazuju da porijeklo recentnih sedimenata rijeke Drave i četvrte dravske terase (pleistocen) odgovara geologiji istočnih Alpa koje su građene od neoproterozojskih i fanerozojskih metamorfnih stijena. Sastav valutica ukazuje i na prisutnost vulkanskih stijena u izvorišnom području. Ne isključuje se mogućnost da je dio materijala četvrte dravske terase pretaložen s okolnih gora čije je uzdizanje započelo u pliocenu, što je potkrijepljeno većom zrelošću teške frakcije te povećanim udjelima epidota, cirkona, rutila i turmalina u pojedinim uzorcima.
Abstract (english)
The main goal of this Thesis was to compare recent Drava river sediments with sediments of Novigrad Podravski and determine their provenance. For that purpose river and excavation sites were visited and surveyed where gravel and sand were sampled. This was followed granulometric, petrographic and quantitative heavy mineral analysis. Results show that the recent Drava river sediments and the 4th Drava river terrace (Pleistocen) to some degree have similar characteristics, and are ultimately derived from a common source area in the Eastern Alps largely built of neoproterozoic and phanerozoic metamorphic rocks. Composition of pebbles indicates the presence of volcanic rocks in the source area. It is not not excluded that a part of 4th Drava river terrace sediments represent redeposited material from surrounding hills and mountains uplifted since the Pliocen, which is substantiated by the maturity of THM fraction and increased proportions of epidot group minerals, zircon, rutile and tourmaline in some specimens.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:878808
Study programmeTitle: Graduate university study of Environmental 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
RepositoryRepository of the Faculty of Science
Created on2022-10-06 11:31:44

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