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undergraduate thesis
Računalno 3D modeliranje geološke građe okolice Drniša
Zagreb: University of Zagreb, Faculty of Science, 2022. urn:nbn:hr:217:436612
Novak, Laura
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Novak, L. (2022). Računalno 3D modeliranje geološke građe okolice Drniša (Undergraduate thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:436612

Novak, Laura. "Računalno 3D modeliranje geološke građe okolice Drniša." Undergraduate thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:436612

Novak, Laura. "Računalno 3D modeliranje geološke građe okolice Drniša." Undergraduate thesis, University of Zagreb, Faculty of Science, 2022. https://urn.nsk.hr/urn:nbn:hr:217:436612

Novak, L. (2022). 'Računalno 3D modeliranje geološke građe okolice Drniša', Undergraduate thesis, University of Zagreb, Faculty of Science, accessed 29 April 2024, https://urn.nsk.hr/urn:nbn:hr:217:436612

Novak L. Računalno 3D modeliranje geološke građe okolice Drniša [Undergraduate thesis]. Zagreb: University of Zagreb, Faculty of Science; 2022 [cited 2024 April 29] Available at: https://urn.nsk.hr/urn:nbn:hr:217:436612

L. Novak, "Računalno 3D modeliranje geološke građe okolice Drniša", Undergraduate thesis, University of Zagreb, Faculty of Science, Zagreb, 2022. Available at: https://urn.nsk.hr/urn:nbn:hr:217:436612

Metadata
TitleRačunalno 3D modeliranje geološke građe okolice Drniša
Title (english)Geological 3D computer modeling of the Drniš area.
AuthorLaura Novak
MentorBorna Lužar-Oberiter (mentor)
Committee memberBorna Lužar-Oberiter (predsjednik povjerenstva)
Committee memberKatarina Gobo (član povjerenstva)
Committee memberDražen Kurtanjek (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
Geology and Paleontology
Abstract
Cilj ovog rada bio je, kroz izradu računalnog 3D modela kompleksne strukturne geološke građe okolice Drniša, objasniti rad u softveru MOVE. Model je izrađen u četiri koraka: unos podataka, vektoriziranje položaja slojeva i geoloških granica, konstrukcija i digitalizacija profila te na kraju spajanje profila i izrada 3D prikaza. Dobiveni model prikazuje dio rasjeda Split-Karlovac koji odjeljuje regionalnu tektonsku jedinicu Visokog krša na dvije podjedinice odnosno Donji visoki krš i Gornji visoki krš. Na njihovom kontaktu nalazi se kao dekolmanski horizont naslaga evaporita koja je dijapirskim kretnjama aktivirala njihovo navlačenje i time izmijenila tektonski režim duž južnog dijela rasjeda.
Abstract (english)
The aim of this study was to explain how to use software MOVE through 3D modeling of the complex geological structure of the Drniš area. The model was made in four steps: data input, vectorization of layers and geological boundaries, construction and digitalization of cross-sections and finally combining sections and making the 3D model. The model is a representation of the southern part of the Split-Karlovac fault that dissects the regional tectonic unit of High Karst into two subunits called Upper High Karst and Lower High Karst. The contact between these two subunits is marked by a decollement horizon generated by evaporite diapirs, which caused the activation of the tectonic regime along the southern part of the Split-Karlovac fault.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:436612
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
Terms of useLicence In copyright icon
Created on2023-01-16 11:16:13