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master's thesis
Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara
Zagreb: University of Zagreb, Faculty of Science, 2023. urn:nbn:hr:217:791316
Maljković, Ana
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Maljković, A. (2023). Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:791316

Maljković, Ana. "Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara." Master's thesis, University of Zagreb, Faculty of Science, 2023. https://urn.nsk.hr/urn:nbn:hr:217:791316

Maljković, Ana. "Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara." Master's thesis, University of Zagreb, Faculty of Science, 2023. https://urn.nsk.hr/urn:nbn:hr:217:791316

Maljković, A. (2023). 'Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara', Master's thesis, University of Zagreb, Faculty of Science, accessed 03 October 2024, https://urn.nsk.hr/urn:nbn:hr:217:791316

Maljković A. Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2023 [cited 2024 October 03] Available at: https://urn.nsk.hr/urn:nbn:hr:217:791316

A. Maljković, "Mineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2023. Available at: https://urn.nsk.hr/urn:nbn:hr:217:791316

Metadata
TitleMineraloška obilježja eocenskih lapora iz flišne serije područja Baške (otok Krk) i jugozapadne obale otoka Hvara
Title (english)MINERALOGICAL PROPERTIES OF EOCENE MARLS FROM FLYSCH SEQUENCES OF THE BAŠKA AREA (KRK ISLAND) AND SOUTHWEST COAST OF HVAR ISLAND
AuthorAna Maljković
MentorNenad Tomašić (mentor)
Committee memberNenad Tomašić (predsjednik povjerenstva)
Committee memberDražen Kurtanjek (član povjerenstva)
Committee memberVlasta Ćosović (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2023-02-22, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Mineralogy and Petrology
Abstract
U ovom radu istraženi su uzorci srednjoeocenskih lapora s tri lokaliteta na otocima Krk i Hvar. Metodama kalcimetrije i rendgenske difrakcije utvrđen je volumni udio karbonata, te mineralni sastav kojeg čine kalcit, kvarc i plagioklasi, te minerali glina klorit, illit, illit/smektit, dioktaedarski vermikulit i kaolinit. Mineraloška svojstva su proučavana s ciljem pronalaženja dokaza o tragovima srednjoeocenskih klimatskih optimuma. Rezultati ne upućuju direktno na uvjete tople i vlažne klime. Veća prisutnost illita i klorita ukazuje na prevladavajuće fizičko trošenje. Prisutnost kaolinita u pojedinim uzorcima može upućivati na djelomice povećano kemijsko trošenje, a time i na nešto vlažniju i topliju klimu, dok prisutnost smektita ukazuje na sezonalnost klime.
Abstract (english)
In this study, samples of Middle Eocene marls from three localities on the islands of Krk and Hvar were investigated. Calcimetry and X-ray diffraction methods were used to determine the volume fraction of carbonates, and the mineral composition of the samples. The marl samples contain calcite, quartz and plagioclase, as well as clay minerals chlorite, illite, illite/smectite, dioctahedral vermiculite and kaolinite. Mineralogical properties were studied in order to find evidence of traces of the Middle Eocene climatic optima. The results do not significantly imply warm and humid climate conditions. Prevailing content of illite and chlorite indicates predominant physical weathering. The presence of kaolinite in some samples could point to partly increased chemical weathering, and thus to a more humid and warmer climate, and occurrence of smectite implies climate seasonality.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:791316
ProjectNumber: IP-2019-04-5775
Title: Dinaridski predgorski bazen između dva eocenska termalna optimuma: mogući scenarij za sjevernojadranski bazen
Title: Dinaridic foreland basin between two Eocene thermal optima: a possible scenario for the Northern Adriatic
Acronym: BREEMECO
Leader: Vlasta Ćosović
Jurisdiction: Croatia
Funder: HRZZ
Funding stream: IP
Study programmeTitle: Graduate university study of Environmental 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 on2023-06-21 10:58:48