Inženjerskogeološki model klizišta Trstenik (Grad Zagreb)

Bagarić, Josip

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master's thesis

Inženjerskogeološki model klizišta Trstenik (Grad Zagreb)

diplomski rad

Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. urn:nbn:hr:169:655003

Bagarić, Josip

University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Geology and Geological Engineering

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APA 6th Edition

Bagarić, J. (2018). Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : 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:169:655003

MLA 8th Edition

Bagarić, Josip. "Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:655003

Chicago 17th Edition

Harvard

Bagarić, J. (2018). 'Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 17 March 2025, https://urn.nsk.hr/urn:nbn:hr:169:655003

Vancouver

Bagarić J. Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2018 [cited 2025 March 17] Available at: https://urn.nsk.hr/urn:nbn:hr:169:655003

IEEE

J. Bagarić, "Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2018. Available at: https://urn.nsk.hr/urn:nbn:hr:169:655003

Cite this item: https://urn.nsk.hr/urn:nbn:hr:169:655003

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Title	Inženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad
Title (english)	Engineering geological model of the Trstenik landslide (city of Zagreb) : master’s thesis
Author	Josip Bagarić
Mentor	Martin Krkač (mentor)
Committee member	Martin Krkač (predsjednik povjerenstva)
Committee member	Snježana Mihalić Arbanas (član povjerenstva)
Committee member	Željko Arbanas (član povjerenstva)
Granter	University of Zagreb Faculty of Mining, Geology and Petroleum Engineering (Department of Geology and Geological Engineering) Zagreb
Defense date and country	2018-09-14, Croatia
Scientific / art field, discipline and subdiscipline	TECHNICAL SCIENCES Mining, Petroleum and Geology Engineering Geological Engineering
Abstract	Zadatak diplomskog rada bila je interpretacija inženjerskogeološkog modela klizišta Trstenik te analiza uzroka koji su doveli do njegove aktivacije. Inženjerskogeološki model interpretiran je isključivo na temelju podataka inženjerskogeološkog kartiranja. Klizište Trstenik je translacijsko klizište, ukupne duljine 250 m, širine 70 m i interpretirane dubine od 5,5 m. Determinacijom i interpretacijom materijala na izdancima je utvrđeno da istraživanu lokaciju izgrađuju srednje trošni tortonski lapori u podlozi te trošni lapori i koluvijalne naslage na površini. Obzirom na vrste materijala i položaj slojevitosti pretpostavljeno je da je do klizanja došlo na granici srednje trošnih i trošnih lapora. Analiza uzroka klizanja provedena je na podacima o oborinama s meteoroloških stanica Čučerje, Kašina i Zagreb-Rim. Klizište je aktivirano 13.02.2014. Analizom su obuhvaćene mjesečne oborine, koje su za siječanj 2014. iznosile od 22 do 36% više od prosjeka, a za veljaču od 148 do 171% više od prosjeka. Analizom su obuhvaćene i prethodne oborine, koje su uspoređene s regionalnim graničnim vrijednostima.
Abstract (english)	The aim of the thesis was the interpretation of the Trstenik landslide engineering geological model, as well as the analysis of its causes. The engineering geological model is interpreted on the basis of engineering geological mapping. Trstenik landslide is a translational landside with a total length of 250 m, width of 70 m, and interpreted depth of 5.5 m. Determination and interpretation of the material on the outcrops showed different types of engineering geological units, medium weathered tortonian marl in the substrate and weathered marl and colluvial on the surface. Given the type of the material and the bedding orientation, it was assumed that sliding occurred at the boundary of medium weathered and weathered marl. The analysis of the cause of the landslide was carried out on the precipitation data from the meteorological stations of Čučerje, Kašina and Zagreb-Rim. The landslide was activated on 13th February 2014. The analysis showed that monthly precipitation in January 2014 was 22 to 36% higher than the average, while in February it was 148 to 171% higher than the average. The analysis also include previous precipitation which are compared with regional boundary values.
Keywords
Keywords (english)
Language	croatian
URN:NBN	urn:nbn:hr:169:655003
Study programme	Title: Geological engineering; specializations in: Hydrogeology and engineering geology, Environmental geology Course: Hydrogeology and engineering geology Study programme type: university Study level: graduate Academic / professional title: magistar/magistra inženjer/inženjerka geološkog inženjerstva (magistar/magistra inženjer/inženjerka geološkog inženjerstva)
Type of resource	Text
File origin	Born digital
Access conditions	Open access
Terms of use
Repository	Faculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb
Created on	2018-10-25 07:16:21