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master's thesis
Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije
diplomski rad
Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2015. urn:nbn:hr:169:833692
Rukavina, David
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Geology and Geological Engineering

Institutional repository: Faculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb

Cite this document

Rukavina, D. (2015). Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad (Master's thesis). Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering. Retrieved from https://urn.nsk.hr/urn:nbn:hr:169:833692

Rukavina, David. "Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2015. https://urn.nsk.hr/urn:nbn:hr:169:833692

Rukavina, David. "Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2015. https://urn.nsk.hr/urn:nbn:hr:169:833692

Rukavina, D. (2015). 'Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 15 July 2024, https://urn.nsk.hr/urn:nbn:hr:169:833692

Rukavina D. Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2015 [cited 2024 July 15] Available at: https://urn.nsk.hr/urn:nbn:hr:169:833692

D. Rukavina, "Strukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2015. Available at: https://urn.nsk.hr/urn:nbn:hr:169:833692

Metadata
TitleStrukturna analiza i interpretacija tektonske evolucije istočnog dijela Savske depresije : diplomski rad
Title (english)Structural analysis and interpretation of tectonic evolution in the eastern part of Sava depresion : master’s thesis
AuthorDavid Rukavina
MentorBruno Tomljenović (mentor)
Committee memberBruno Tomljenović
Committee memberBruno Saftić
Committee memberDavor Pavelić
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Zagreb
Defense date and country2015-04-17, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
U ovom radu analizirani su i interpretirani 2D seizmički profili i bušotinski podatci na temelju kojih je određena geometrija, kinematske značajke i prostorni raspored rasjeda i pratećih struktura u istočnom dijelu Savske depresije. Seizmički profili i bušotinski podatci, ustupljeni od tvrtke INA Industrija nafte, d.d. Zagreb, analizirani su primjenom računalnog paketa PetrelTM Seismic to Simulation, pomoću kojeg je konstruiran strukturni model koji je omogućio izradu strukturnih karata po plohama podloge neogena, podloge panona i podloge plio-kvartara, trima regionalnim stratigrafskim horizontima koji odražavaju važne promjene u tektonskoj evoluciji dijela Panonskog bazenskog sustava na području Hrvatske. Rekonstruirane su i glavne deformacijske strukture koje su prikazane na strukturnim kartama, čiji je postanak interpretiran tijekom faze otvaranja Savske depresije uslijed regionalne ekstenzije i za vrijeme tektonske inverzije tijekom pliocena i kvartara. Pomoću strukturnih karata definirano je pet glavnih strukturnih jedinica u istraživanom području. Homokline Prosare i Motajice dio su magmatsko-metamorfniih kompleksa Prosare i Motajice koji su inicijalno formirani prije otvaranja Savske depresije. Sinklinale Roždanik i Nova Gradiška nastale su otvaranjem taložnog prostora Savske depresije u ekstenzijskoj fazi. Strukturna jedinica Novska-Batrina na karti po podlozi neogenskih naslaga definirana kao homoklina, a na kartama po podlozi panonskih i pliokvartarnih naslaga kao antiklinala, izdignuta je sustavom reversnih rasjeda pružanja SZ-JI nagiba generalno prema SI, aktivnih za vrijeme tektonske inverzije. Na temelju interpretiranih podataka napravljen je model formiranja istraživanog dijela Savske depresije prema kojem je ona stvorena normalnim rubnim rasjedima u fazi intenzivne ekstenzije, na koju se nastavlja glavna faza zapunjavanja i blažeg normalnog rasjedanja. U zadnjoj fazi dolazi do snažne inverzije kada reversni rasjedi, uz sjeverni rub depresije, presjecaju prijašnje normalne rasjede i izdižu podlogu bazena u svojim krovinskim krilima. Inverzija također uzrokuje formiranje lokalnih „pop-up“ struktura i reaktivaciju ranije nastalih normalnih rasjeda.
Abstract (english)
Abstract: Interpretation of 2D sesmic reflection sections together with well data enabled determination of the geometry, kinematics and spatial distribution of faults and associated structures in eastern part of Sava depression. Seismic sections and well data, made available by INA Plc, Zagreb, were analyzed using the PetrelTM Seismic to Simulation software package. The constructed structural model consists of the strucural maps - Base Neogene, Base Pannonian and Base Plio-Quaternary, three regional stratigraphic horizons that represent important changes in tectonic evolution in the Croatian part of Pannonian basin system. Main deformation structures were also reconstructed. These structures were firstly created during the phase of opening of the Sava depression, as a result of regional extension and then changed during tectonic inversion that occured in Pliocene and Quaternary. Five major strucutral units are defined on structural maps. The Prosara and Motajica homoclines are parts of magmatic-metamorphic complexes of Mt. Prosara and Mt. Motajica which were initially formed before opening of the Sava depression. The Roždanik and Nova Gradiška synclines were formed in the extensional phase. Structural unit named Novska-Batrina on the Base Neogene map is shaped as a homocline while on the Base Pannonian and Base Plio-Quaternry it acquired a shape of an anticline uplifted by the system of reverse faults. Mentioned faults strike NW-SE generaly and are inclined to NE, and it is proven that they were active during tectonic inversion. Based on interpreted data the structural evolution of the eastern part of Sava depression is reconstructed. According to that model, depression was formed by normal faulting in phase of intensive extension which is followed by main infill of depresion and mild normal extension. In the last phase, strong inversion occured with reverse faulting along the northern edge of depression crossing previous normal faults and uplifting the base of basin fill. Inversion also caused formation of local pop-up structures and reactivation of the pre-existing normal faults.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:169:833692
Study programmeTitle: 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 on2015-12-15 13:42:37