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master's thesis
Geološke značajke ponora kod Rašpora na Ćićariji
diplomski rad
Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2014. urn:nbn:hr:169:094787
Korač, Neven
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Mineralogy, Petrology and Mineral Resources

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

Cite this document

Korač, N. (2014). Geološke značajke ponora kod Rašpora na Ćićariji : 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:169:094787

Korač, Neven. "Geološke značajke ponora kod Rašpora na Ćićariji : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2014. https://urn.nsk.hr/urn:nbn:hr:169:094787

Korač, Neven. "Geološke značajke ponora kod Rašpora na Ćićariji : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2014. https://urn.nsk.hr/urn:nbn:hr:169:094787

Korač, N. (2014). 'Geološke značajke ponora kod Rašpora na Ćićariji : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 05 November 2024, https://urn.nsk.hr/urn:nbn:hr:169:094787

Korač N. Geološke značajke ponora kod Rašpora na Ćićariji : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2014 [cited 2024 November 05] Available at: https://urn.nsk.hr/urn:nbn:hr:169:094787

N. Korač, "Geološke značajke ponora kod Rašpora na Ćićariji : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2014. Available at: https://urn.nsk.hr/urn:nbn:hr:169:094787

Metadata
TitleGeološke značajke ponora kod Rašpora na Ćićariji : diplomski rad
Title (english)Geological features of Rašpor cave on Ćićarija : master's thesis
AuthorNeven Korač
MentorUroš Barudžija (mentor)
Committee memberUroš Barudžija
Committee memberIgor Vlahović
Committee memberBruno Tomljenović
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Mineralogy, Petrology and Mineral Resources)
Zagreb
Defense date and country2014-09-30, Croatia
Scientific / art field,
discipline and subdiscipline		TECHNICAL SCIENCES
Mining, Petroleum and Geology Engineering
Geological Engineering
Abstract
Ponor kod Rašpora (Abisso Bertarelli, Žankana jama) nalazi se u neposrednoj blizini sela Rašpor na Ćićariji. Sa svojom dubinom od preko 338 metara najdublji je do sada istražen speleološki objekt na području Istre. Ulaz u jamu izgrađen je od flišolikih naslaga – lapora, pa je zbog toga jama svrstavana u speleološke objekte nastale u 'flišu' i zbog toga je tijekom povijesti smatrana neperspektivnom za daljnja istraživanja. Nakon prvih 50-ak metara dubine kanala dolazi se do kontakta lapora sa paleogenskim foraminiferskim vapnencima koji se nalaze u njihovoj podini i puno su podložniji okršavanju. U stijenama ovakvog tipa razvijen je najveći dio špiljskih kanala. Za izradu ovog diplomskog rada, tijekom terenskog istraživanja vršena su mjerenja strukturnih elemenata i uzimani su geološki uzorci za daljnju analizu u laboratoriju. Uzorci su tada opisani makroskopski, a od dijela uzoraka načinjeni su mikroskopski preparati koji su i mikroskopski opisani. Nakon klasifikacije stijena rezultati su smješteni na odgovarajuće kartografske podloge i na topografski snimak (profil) speleološkog objekta. Tako prikazani odnosno prostorno smješteni podaci o stijenama predstavljaju završni rezultat ovog diplomskog rada.
Abstract (english)
Abstract: Rašpor cave (Abisso Bertarelli, Žankana jama) is located near the village Rašpor on Ćićarija, northern Istria. With its depth of over 338 meters is the deepest so far investigated speleological object in Istria. The entrance to the cave is formed within flysh deposits – mainly marl, and is therefore considered as cave formed in the 'flysch' and therefore has throughout history been considered unpromising for further research. After the first 50 meters depth in channel contact of marl and Paleocene foraminiferal limestones was found. Foraminiferal limestones that lie underneath marl deposits are much more susceptible to karstification and has been found forming most of the cave channel walls. To create this master’s thesis following actions took place. During the fieldwork structural elements (slope layer, and tilt angle) were measured and geological samples were taken for further analysis in the laboratory. The samples were then described macroscopically, and the sample pieces were made that are microscopically described. Following the classification of rocks results are placed in the appropriate cartographic basis and on a topographical survey (profile) of Rašpor cave. This kind of spatial data represents the final result of this thesis.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:169:094787
Study programmeTitle: Geological engineering; specializations in: Hydrogeology and engineering geology, Environmental geology
Course: Environmental 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 conditionsAccess restricted to students and staff of home institution
Terms of useLicence In copyright icon
Created on2016-01-15 14:54:15