prikaz prve stranice dokumenta Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore
Embargo period 2025-02-20
master's thesis
Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore
Zagreb: University of Zagreb, Faculty of Science, 2023. urn:nbn:hr:217:335187
Schneller, Dario
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Schneller, D. (2023). Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:335187

Schneller, Dario. "Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore." Master's thesis, University of Zagreb, Faculty of Science, 2023. https://urn.nsk.hr/urn:nbn:hr:217:335187

Schneller, Dario. "Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore." Master's thesis, University of Zagreb, Faculty of Science, 2023. https://urn.nsk.hr/urn:nbn:hr:217:335187

Schneller, D. (2023). 'Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore', Master's thesis, University of Zagreb, Faculty of Science, accessed 08 June 2024, https://urn.nsk.hr/urn:nbn:hr:217:335187

Schneller D. Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2023 [cited 2024 June 08] Available at: https://urn.nsk.hr/urn:nbn:hr:217:335187

D. Schneller, "Indikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2023. Available at: https://urn.nsk.hr/urn:nbn:hr:217:335187

Metadata
TitleIndikatori parcijalnog taljenja u metapelitnim stijenama Moslavačke gore
Title (english)Indicators of partial melting in metapelites from Moslavačka Gora
AuthorDario Schneller
MentorZorica Petrinec (mentor)
Committee memberZorica Petrinec (predsjednik povjerenstva)
Committee memberDražen Balen (član povjerenstva)
Committee memberKarmen Fio Firi (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2023-02-20, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Mineralogy and Petrology
Abstract
Kristalin Moslavačke gore predstavlja magmatsko-metamorfni kompleks kojeg čine granitoidne stijene, metamorfne stijene srednjeg stupnja metamorfizma te migmatitne stijene. Dosadašnja istraživanja kao migmatite dominantno opisuju različite varijetete migmatiziranih gnajseva. Cilj ovoga rada je potkrijepiti hipotezu da je pojava parcijalnog taljenja zabilježena i u metapelitima Moslavačke gore, na što ukazuju dosadašnja geotermobarometrijska istraživanja. U tu svrhu optičkim istraživanjima obuhvaćeno je pet uzoraka metapelita Moslavačke gore te je analizirana velika količina mikrostrukturnih indikatora parcijalnog taljenja. Glavne mikrostrukturne indikatore predstavljaju zrna peritektičkog i retrogradnog cordijerita koja su zaobljena u kontaktu sa „zašiljenim“ volumenima felsičnih minerala. Navedena kombinacija indikatora potvrđuje da je u metapelitnim stijenama bila prisutna taljevina, odnosno, da se u migmatizirane stijene Moslavačke gore, uz gnajseve, mogu ubrojiti i metapelitne stijene.
Abstract (english)
Moslavačka Gora crystalline represents a magmatic-metamorphic complex consisting of granitoid rocks, medium-grade metamorphic rocks, and migmatitic rocks. Previous research predominantly describes different varieties of migmatised gneisses as migmatites. The aim of this work is to support the hypothesis that the occurrence of partial melting was also recorded in the metapelites of Moslavačka Gora, as indicated by previous geothermobarometric research. For this purpose, five samples of metapelites from Moslavačka Gora were included in optical research, and a large number of microstructural indicators of partial melting were analyzed. The main microstructural indicators are peritectic and retrograde cordierite grains that were rounded in contact with pointed volumes of felsic minerals. The aforementioned combination of indicators confirms that melt was present in metapelitic rocks, i.e., that metapelitic rocks can be regarded as migmatites of Moslavačka Gora, along with gneisses.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:335187
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 conditionsEmbargoed access
Embargo expiration date: 2025-02-20
Terms of useLicence In copyright icon
Created on2023-06-21 09:11:35