Výsledky vyhľadávania
Názov Geochemický model transformácie gabra na rodingit Aut.údaje Juraj Butek, Ján Spišiak ... [et al.] Autor Butek Juraj 1993- (20%) UMBFP01 - Katedra geografie a geológie
Spoluautori Spišiak Ján 1953- (20%) UMBFP01 - Katedra geografie a geológie
Fabre Sébastien (20%)
Duchene Stéphanie (20%)
Grégoire Michel (20%)
Zdroj.dok. Geochémia 2024 : zborník vedeckých príspevkov z konferencie. S. 18-21. - Bratislava : Štátny geologický ústav Dionýza Štúra, 2024 ; Geochémia 2024 medzinárodná vedecká konferencia Kľúč.slová geochemické anomálie rodingity - rodingites Form.deskr. príspevky v zborníku - proceedings papers Jazyk dok. slovenčina Krajina Slovenská republika URL Link na plný text Kategória publikačnej činnosti AFD Číslo archívnej kópie 54426 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ 
kniha
Názov A petrochronological study of Fe–Ti oxides in rodingites of the Western Carpathians, Slovakia Aut.údaje Juraj Butek, Damien Dufourcau ... [et al.] Autor Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Spoluautori Dufourcau Damien (10%)
Duchene Stéphanie (5%)
Laurent Oscar (1%)
Grégoire Michel (1%)
Spišiak Ján 1953- (13%) UMBFP01 - Katedra geografie a geológie
Zdroj.dok. Lithos. Vol. 460-461 (2023), pp. [1-14]. - Amsterdam : Elsevier B.V., 2023 Kľúč.slová rodingity - rodingites geochémia - geochemistry Heslá geogr. Západné Karpaty (pohorie) Form.deskr. články - journal articles Jazyk dok. angličtina Krajina Holandsko Anotácia 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 Kategória publikačnej činnosti ADC Číslo archívnej kópie 53855 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ Odkazy PERIODIKÁ-Súborný záznam periodika 
článok
Názov Petrochronologická analýza Fe-Ti oxidov z rodingitov z lokality Breznička-Bôrček, severné gemerikum, Západné Karpaty Aut.údaje Juraj Butek ... [et al.] Autor Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Spoluautori Spišiak Ján 1953- (10%) UMBFP01 - Katedra geografie a geológie
Dufourcau Damien (5%)
Duchene Stéphanie (5%)
Laurent Oscar (5%)
Grégoire Michel (5%)
Zdroj.dok. Mineralogická konferencia Vyšná Boca 2023 : zborník abstraktov. Roč., č. (2023), s. 16-17. - Bratislava : Slovenská mineralogická spoločnosť, 2023 ; Mineralogická konferencia Vyšná Boca 2023 konferencia Kľúč.slová rodingity - rodingites Heslá geogr. Breznička Západné Karpaty (pohorie) Form.deskr. abstrakty - abstracts Jazyk dok. slovenčina Krajina Slovenská republika URL Link na plný text Kategória publikačnej činnosti BFB Číslo archívnej kópie 54030 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ článok
Názov On the origin of vesuvianite-rich rodingites from the Western Carpathians, Slovakia Aut.údaje Juraj Butek, Michel Grégorie, Ján Spišiak, Stéphanie Duchene, Richard Kopáčik Autor Butek Juraj 1993- (80%) UMBFP01 - Katedra geografie a geológie
Spoluautori Grégoire Michel (1%)
Spišiak Ján 1953- (15%) UMBFP01 - Katedra geografie a geológie
Duchene Stéphanie (1%)
Kopáčik Richard 1995- (3%) UMBFP01 - Katedra geografie a geológie
Zdroj.dok. Lithos. Vol. 432-433 (2022), pp. 1-19, art. no. 106902. - Amsterdam : Elsevier B.V., 2022 Kľúč.slová vezuvianity - vesuvianites metasomatóza - metasomatism rodingitizácia - rodingitization Heslá geogr. Západné Karpaty (pohorie) Form.deskr. články - journal articles Jazyk dok. angličtina Krajina Holandsko Anotácia 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 Kategória publikačnej činnosti ADC Číslo archívnej kópie 52676 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ Odkazy PERIODIKÁ-Súborný záznam periodika článok
Názov Petrology of Fe-Ti-rich rodingites from Western Carpathians Aut.údaje Juraj Butek ... [et al.] Autor Butek Juraj 1993- (70%) UMBFP01 - Katedra geografie a geológie
Spoluautori Duchene Stéphanie (10%)
Grégoire Michel (10%)
Spišiak Ján 1953- (10%) UMBFP01 - Katedra geografie a geológie
Zdroj.dok. 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 Kľúč.slová geochémia - geochemistry mineralógia - mineralogy rodingity - rodingites Heslá geogr. Západné Karpaty (pohorie) Form.deskr. abstrakty - abstracts Jazyk dok. angličtina Krajina Francúzsko URL Link na zdrojový dokument Link na konferenciu Kategória publikačnej činnosti BFA Číslo archívnej kópie 51237 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ článok