prikaz prve stranice dokumenta Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg)
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master's thesis
Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg)
diplomski rad
2013. urn:nbn:hr:169:074592
Arežina, Tamara
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Geology and Geological Engineering

Cite this document

Arežina, T. (2013). Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : 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:169:074592

Arežina, Tamara. "Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2013. https://urn.nsk.hr/urn:nbn:hr:169:074592

Arežina, Tamara. "Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2013. https://urn.nsk.hr/urn:nbn:hr:169:074592

Arežina, T. (2013). 'Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 18 November 2024, https://urn.nsk.hr/urn:nbn:hr:169:074592

Arežina T. Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2013 [cited 2024 November 18] Available at: https://urn.nsk.hr/urn:nbn:hr:169:074592

T. Arežina, "Litostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2013. Available at: https://urn.nsk.hr/urn:nbn:hr:169:074592

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Metadata
TitleLitostratigrafske značajke karbonatnih breča na prijelazu donja/gornja kreda u ležištu arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) : diplomski rad
Title (english)Lithostratigraphic characteristics of Upper Albian carbonate breccia in dimension stone quarry Tvrda Ljut (Široki Brijeg) : master's thesis
AuthorTamara Arežina
MentorIvan Dragičević (mentor)
Committee memberIvan Dragičević
Committee memberUroš Barudžija
Committee memberIvo Galić
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Zagreb
Defense date and country2013-07-11, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
Terenskim istraživanjem i mikropetrografskom analizom unutar karbonatnih breča iz ležišta arhitektonsko-građevnog kamena Tvrda Ljut (Široki Brijeg) definirano je pet različitih litofacijesa klasta: (a) foraminiferskog grejnstona (biosparita), (b) mikrita i djelomice (de)dolomitiziranog mikrita, (c) mikrita s ostrakodima/ostrakodnog mikrita (djelomice (de)dolomitiziranog) (d) rekristaliziranog/(de)dolomitiziranog pelsparita; te (e) dolomita-dedolomita. Na temelju determinacije mikrofacijesa klasta i ostalih karakteristika karbonatnih breča utvrđen je plitkomorski okoliš formiranja ležišta, uz djelovanje tektonike te vjerojatno padinskih ili gravitacijskih procesa. Analizom prisutnih fosilnih ostataka u klastima određena je gornjoalbska starost brečiranih naslaga.
Abstract (english)
Abstract: Five different lithofacies of carbonate breccia clasts in dimension stone quarry Tvrda Ljut (Široki Brijeg) have been determined by field work and micropetrographic analysis: (a) foraminiferal grainstone (biosparite), (b) micrite and partially (de)dolomitized micrite, (c) micrite with ostracods/ostracodal micrite (partially (de)dolomitized), (d) recrystallized/(de)deolomitized pelsparite and (e) dolomite-dedolomite. Based on the determination of microfacies of clasts and other charachteristics of carbonate breccia it has been determined that the quarry was formed in the shallow-marine environment, with the activity of tectonics, as well as the slope and gravitational processes. By analysing fossil remains in clasts it has been determined that the brecciated deposits are of Upper Albian age.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:169:074592
Study programmeTitle: Geology
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geologije (magistar/magistra geologije)
Type of resourceText
File originBorn digital
Access conditionsAccess restricted to students and staff of home institution
Terms of useLicence In copyright icon
Created on2016-01-19 14:30:09