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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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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

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

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

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 24 April 2024, https://urn.nsk.hr/urn:nbn:hr:169:655003

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 2024 April 24] Available at: https://urn.nsk.hr/urn:nbn:hr:169:655003

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

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Metadata
TitleInženjerskogeološki model klizišta Trstenik (Grad Zagreb) : diplomski rad
Title (english)Engineering geological model of the Trstenik landslide (city of Zagreb) : master’s thesis
AuthorJosip Bagarić
MentorMartin Krkač (mentor)
Committee memberMartin Krkač (predsjednik povjerenstva)
Committee memberSnježana Mihalić Arbanas (član povjerenstva)
Committee memberŽeljko Arbanas (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Zagreb
Defense date and country2018-09-14, 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)
Languagecroatian
URN:NBNurn:nbn:hr:169:655003
Study programmeTitle: 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 resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
RepositoryFaculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb
Created on2018-10-25 07:16:21

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