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Title Geochemický model transformácie gabra na rodingit Author info Juraj Butek, Ján Spišiak ... [et al.] Author Butek Juraj 1993- (20%) UMBFP01 - Katedra geografie a geológie
Co-authors Spišiak Ján 1953- (20%) UMBFP01 - Katedra geografie a geológie
Fabre Sébastien (20%)
Duchene Stéphanie (20%)
Grégoire Michel (20%)
Source document Geochémia 2024 : zborník vedeckých príspevkov z konferencie. S. 18-21. - Bratislava : Štátny geologický ústav Dionýza Štúra, 2024 ; Geochémia 2024 medzinárodná vedecká konferencia Keywords geochemické anomálie rodingity - rodingites Form. Descr. príspevky v zborníku - proceedings papers Language Slovak Country Slovak Republic URL Link na plný text Public work category AFD No. of Archival Copy 54426 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ Title Petrochronologická analýza Fe-Ti oxidov z rodingitov z lokality Breznička-Bôrček, severné gemerikum, Západné Karpaty Author info Juraj Butek ... [et al.] Author Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Co-authors Spišiak Ján 1953- (10%) UMBFP01 - Katedra geografie a geológie
Dufourcau Damien (5%)
Duchene Stéphanie (5%)
Laurent Oscar (5%)
Grégoire Michel (5%)
Source document Mineralogická konferencia Vyšná Boca 2023 : zborník abstraktov. Roč., č. (2023), s. 16-17. - Bratislava : Slovenská mineralogická spoločnosť, 2023 ; Mineralogická konferencia Vyšná Boca 2023 konferencia Keywords rodingity - rodingites Headings Geogr. Breznička Západné Karpaty (pohorie) Form. Descr. abstrakty - abstracts Language Slovak Country Slovak Republic URL Link na plný text Public work category BFB No. of Archival Copy 54030 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ Title A petrochronological study of Fe–Ti oxides in rodingites of the Western Carpathians, Slovakia Author info Juraj Butek, Damien Dufourcau ... [et al.] Author Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Co-authors Dufourcau Damien (10%)
Duchene Stéphanie (5%)
Laurent Oscar (1%)
Grégoire Michel (1%)
Spišiak Ján 1953- (13%) UMBFP01 - Katedra geografie a geológie
Source document Lithos. Vol. 460-461 (2023), pp. [1-14]. - Amsterdam : Elsevier B.V., 2023 Keywords rodingity - rodingites geochémia - geochemistry Headings Geogr. Západné Karpaty (pohorie) Form. Descr. články - journal articles Language English Country Netherlands Annotation Rodingitization is the metasomatic transformation of mafic lithologies into rodingite, a Ca-rich and Si-poor rock associated with serpentinized ultramafic bodies. Serpentinization and rodingitization occur simultaneously but it remains challenging to obtain absolute ages on these events in order to identify the geodynamic setting of their formation. In this study, we investigate rodingites from an occurrence in the Western Carpathians with the aim to define the timing of rodingite formation during the tectono-metamorphic evolution of the Carpathian Orogen. The rodingites consist mainly of vesuvianite, diopside, garnet and chlorite. They are noticeably characterized by the presence of Fe–Ti rich aggregates composed of ilmenite, rutile, titanite and calcite. Textural relationships and chemical compositions of the investigated Fe–Ti minerals document their hydrothermal-metamorphic origin. These minerals are characterized by considerable rare earth element (REE) concentrations with prevailing positive Eu anomaly, which presumably derives from the plagioclase-rich protolith of the investigated rodingites. Moreover, the similarity of REE patterns between the analysed phases suggests that the REE concentrations in Fe–Ti minerals are controlled by the immobility and availability of these elements in the system. A particular lamellae texture composed of rutile and calcite originated from titanite destabilization. The titanite destabilization was triggered by cooling, silica leaching and influx of CO2-rich fluids. In situ U–Pb dating of rutile, which have formed by retrograde breakdown of titanite during rodingitization, yields a crystallization age of 102.6 ± 19.9 Ma. This age is in good agreement with Cretaceous ages of the regional alpine metamorphic evolution reported in the literature and suggests that the rodingitization and serpentinization processes took place during the exhumation and cooling of the accretionary wedge resulting from the closure of the Meliata Ocean. URL Link na zdrojový dokument Public work category ADC No. of Archival Copy 53855 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika Title On the origin of vesuvianite-rich rodingites from the Western Carpathians, Slovakia Author info Juraj Butek, Michel Grégorie, Ján Spišiak, Stéphanie Duchene, Richard Kopáčik Author Butek Juraj 1993- (80%) UMBFP01 - Katedra geografie a geológie
Co-authors Grégoire Michel (1%)
Spišiak Ján 1953- (15%) UMBFP01 - Katedra geografie a geológie
Duchene Stéphanie (1%)
Kopáčik Richard 1995- (3%) UMBFP01 - Katedra geografie a geológie
Source document Lithos. Vol. 432-433 (2022), pp. 1-19, art. no. 106902. - Amsterdam : Elsevier B.V., 2022 Keywords vezuvianity - vesuvianites metasomatóza - metasomatism rodingitizácia - rodingitization Headings Geogr. Západné Karpaty (pohorie) Form. Descr. články - journal articles Language English Country Netherlands Annotation Rodingite represents a particular metasomatic rock type that occurs as dykes or lenses in association with serpentinized ultramafic rocks and typically consists of Ca-rich, often hydrated silicate minerals. Rodingites have been recognized as a source of information on fluid compositions and their circulation in both ocean floor and subduction environments. Yet, the nature of the protoliths, the chemistry and the origin of fluids, the details of fluid-rock interaction, and the metamorphic context remain often obscure. This work investigates some of these questions in the case of rodingites from the Western Carpathians through petrological, mineralogical and geochemical studies. Rodingites are here associated in the field with serpentinized tectonically dismembered bodies of ultramafic rocks embeded into Carboniferous metasediments. They mostly consist of vesuvianite, diopside, and hydrated garnet with minor titanite, chlorite, epidote, calcite and Fe–Ti oxides. Three successive hydrothermal events were recognized: 1) formation of diopside, vesuvianite and garnet, 2) formation of a second generation of vesuvianite and garnet together with titanite and minor chlorite, and 3) formation of a mineral assemblage consisting of epidote, chlorite and calcite. The first two events represent a pervasive and intense rodingitization process, whereas the third one represents late, channeled, fluid circulation under greenschist facies conditions. The presence of Fe–Ti oxides influences the mineralogy and the whole rock chemistry of the investigated rodingites. Rutile and ilmenite are commonly associated with titanite and garnet, and whole rock analyses can reach up to 9.2 wt% TiO2. Vesuvianite and garnet also incorporate a significant amount of titanium. The lack of primary minerals, the mineral composition as well as high CaO and low SiO2 contents demonstrate high extent of Ca-metasomatism. The high modal amount of vesuvianite and the immobility of Al during metasomatic processes suggest that the protolith was relatively Al-rich. Taking into account the REE patterns of whole-rock and minerals, the high TiO2 content and the local Fe-Ti-rich accumulations, we suggest that the protoliths were more or less Fe-Ti-rich gabbroic rocks initially occurring in association with the serpentinized ultramafic body. URL Link na plný text Public work category ADC No. of Archival Copy 52676 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika Title Petrology of Fe-Ti-rich rodingites from Western Carpathians Author info Juraj Butek ... [et al.] Author Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Co-authors Duchene Stéphanie (10%)
Grégoire Michel (10%)
Spišiak Ján 1953- (10%) UMBFP01 - Katedra geografie a geológie
Source document 27e réunion des sciences de la terre : livre des résumés : abstracts. S. 254. - Paríž : Société Géologique de France, 2021 ; Réunion des Sciences de la Terre kongres Keywords geochémia - geochemistry mineralógia - mineralogy rodingity - rodingites Headings Geogr. Západné Karpaty (pohorie) Form. Descr. abstrakty - abstracts Language English Country France URL Link na zdrojový dokument Link na konferenciu Public work category BFA No. of Archival Copy 51237 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ