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master's thesis
Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)
Zagreb: University of Zagreb, Faculty of Science, 2015. urn:nbn:hr:217:231388
Hanževački, Sandra
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

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Hanževački, S. (2015). Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk) (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:231388

Hanževački, Sandra. "Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)." Master's thesis, University of Zagreb, Faculty of Science, 2015. https://urn.nsk.hr/urn:nbn:hr:217:231388

Hanževački, Sandra. "Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)." Master's thesis, University of Zagreb, Faculty of Science, 2015. https://urn.nsk.hr/urn:nbn:hr:217:231388

Hanževački, S. (2015). 'Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)', Master's thesis, University of Zagreb, Faculty of Science, accessed 22 November 2024, https://urn.nsk.hr/urn:nbn:hr:217:231388

Hanževački S. Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk) [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2015 [cited 2024 November 22] Available at: https://urn.nsk.hr/urn:nbn:hr:217:231388

S. Hanževački, "Petrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2015. Available at: https://urn.nsk.hr/urn:nbn:hr:217:231388

Metadata
TitlePetrogeneza granita i stijena srednjeg do visokog stupnja metamorfizma u kamenolomu Puklica (Đulovac, Papuk)
Title (english)Petrogenesis of granites and medium-to-high-grade metamorphism rocks in the Puklica quarry (Đulovac, Mt. Papuk)
AuthorSandra Hanževački
MentorDražen Balen (mentor)
Committee memberDražen Balen (predsjednik povjerenstva)
Committee memberMarijan Kovačić (član povjerenstva)
Committee memberBlanka Cvetko Tešović (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2015-09-30, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Abstract
Istraţivani kamenolom nalazi se u blizini malenog naselja Puklica na sjeverozapadnim obroncima Papuka. Stijene u kamenolomu koje ĉine razliĉiti tipovi gnajseva, granita i migmatita zajedno sa stijenama progresivnometamorfnog kompleksa predstavljaju osnovnu graĊevnu jedinicu Papuka i velikog dijela kristaline podloge Panonskog bazena. Na temelju rezultata terenskog istraţivanja, mikrofiziografije stijena i mikrotektonike zakljuĉeno je da su migmatiti nastali parcijalnim taljenjem gnajseva. U kasnijim fazama dolazi do utiskivanja granitne magme i nastanka boranih migmatita u središnjem dijelu kamenoloma. Na temelju rezultata kemijske analize zakljuĉeno je da analizirani graniti predstavljaju granite tipiĉne za gornje dijelove kontinetske kore dok su geotermobarometrijskim metodama okvirno odreĊeni PT-uvjeti tijekom nastanka migmatita.
Abstract (english)
The quarry examined in this research is located near the small village named Puklica on the northwestern slopes od Mt. Papuk. Rocks in the quarry, that are represented by various types of gneiss, granites and migmatites, together with the rocks from progressive metamorphic complex, make the constituent parts of Mt. Papuk and most of the crystallyne basement of the Pannonian Basin. Based on the field research results, microscopy and microtectonics, it is determined that migmatites formed by partial melting of gneiss. Granite emplacement and formation of folded migmatites in the central parts of the quarry took place after the partial melting. Based on the mineral chemsitry results, it is determined that granites in the quarry correspond with granits tipically found in the upper continetnal crust while geothermobarometry provided PT-conditions during the formation of migmatites.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:231388
Study programmeTitle: Graduate university study of 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 on2017-02-27 13:49:27