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master's thesis
Amfibolitne leće u filonitiziranim gnajsevima Krndije
diplomski rad
Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. urn:nbn:hr:169:123632
Ostrelič, Damjan
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

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Ostrelič, D. (2018). Amfibolitne leće u filonitiziranim gnajsevima Krndije : 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:169:123632

Ostrelič, Damjan. "Amfibolitne leće u filonitiziranim gnajsevima Krndije : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:123632

Ostrelič, Damjan. "Amfibolitne leće u filonitiziranim gnajsevima Krndije : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:123632

Ostrelič, D. (2018). 'Amfibolitne leće u filonitiziranim gnajsevima Krndije : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 23 May 2024, https://urn.nsk.hr/urn:nbn:hr:169:123632

Ostrelič D. Amfibolitne leće u filonitiziranim gnajsevima Krndije : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2018 [cited 2024 May 23] Available at: https://urn.nsk.hr/urn:nbn:hr:169:123632

D. Ostrelič, "Amfibolitne leće u filonitiziranim gnajsevima Krndije : 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:169:123632

Metadata
TitleAmfibolitne leće u filonitiziranim gnajsevima Krndije : diplomski rad
Title (english)Amphibolite lenses in phyllonitized paragneisses of Mt. Krndija : master’s thesis
AuthorDamjan Ostrelič
MentorVesnica Garašić (mentor)
Committee memberVesnica Garašić (predsjednik povjerenstva)
Committee memberDunja Aljinović (član povjerenstva)
Committee memberBruno Tomljenović (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Mineralogy, Petrology and Mineral Resources)
Zagreb
Defense date and country2018-09-07, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Mineralogy and Petrology
Abstract
Istraživane amfibolitne leće uložene u filonitizirane paragnajseve Krndije pripadaju Psunjsko-kutjevačkom metamorfnom kompleksu slavonskih planina. Na terenu je prikupljeno sedam uzoraka amfibolita te dva uzorka filonitiziranih gnajseva. Metodama polarizacijske mikroskopije i rendgenske difrakcije određen je mineralni sastav i petrografskse karakteristike svih uzoraka, a kemijskim metodama emisijske i masene spektrometrije s induktivno spregnutom plazmom (ICP–ES i ICP–MS) određen je kemijski sastav pet odabranih uzoraka amfibolita i jednog uzorka filonitiziranog paragnajsa. Uzorci amfibolita su prema petrografskim karakteristikama određeni kao trakasti i „porfiroblastični“ amfiboliti, dok su gnajsevi određeni kao filonitizirani paragnajsevi. Na temelju kemijskog sastava protoliti amfibolita određeni su kao toleiitski bazalti do bazalt-andeziti zalučnog bazena, a protoliti paragnajseva kao sedimentne stijene nastale trošenjem felzičnih stijena kalcijsko–alkalijske magmatske serije peraluminijskog karaktera nastalih na aktivnom kontinentalnom rubu. Predloženi petrogenetski model protolitnih stijena je zalučni bazen iza zone subdukcije u kojem se taložio klastični materijal deriviran iz kontinentalne kore istovremeno s povremenim izljevima bazaltnih lava.
Abstract (english)
The investigated amphibolite lenses in phyllonitized paragneisses of Mt. Krndija are a part of the Psunj-kutjevo metamorphic complex of the Slavonian mountains. Seven amphibolite field samples were taken along with two samples of paragneisses. Using polarised microscopy and X-ray diffraction, the mineral composition and petrographic characteristics of all samples were determined. Chemical composition of five selected amphibolite samples and one paragneiss sample were obtained using mass and emission spectrometry with inductively coupled plasma (ICP–MS and ICP–ES). The investigated amphibolites were determined as linated or „porphyroblastic“ amphibolites based on their petrography, while the gneiss samples were determined as phyllonitized paragneisses. Based on the chemical composition of amphibolites, their protolith was determined as tholeiitic basalt to andesite–basalt formed in a back arc basin. The protolith of paragneisses was determined as a sedimentary rock formed by erosion of calc–alkali felsic rocks of peraluminous character at an active continental margin. The proposed petrogenetic model of protolith rocks is a back arc basin in which siliciclastic material of continental originwas being deposited simultaneously with periodic effusions of basaltic lavas.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:169:123632
Study programmeTitle: Geology; specializations in: Geology of mineral resources and geophysical explorations
Course: Geology of mineral resources and geophysical explorations
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 on2018-10-25 08:25:38