Počet záznamov: 1
Garnet-vesuvianite equilibrium in rodingites from Dobšiná (Western Carpathians)
Názov Garnet-vesuvianite equilibrium in rodingites from Dobšiná (Western Carpathians) Aut.údaje Juraj Butek, Ján Spišiak, Stanislava Milovská Autor Butek Juraj 1993- (75%) UMBFP01 - Katedra geografie a geológie
Spoluautori Spišiak Ján 1953- (20%) UMBFP01 - Katedra geografie a geológie
Milovská Stanislava (5%)
Zdroj.dok. Minerals : international, peer-reviewed, open access journal of natural mineral systems, mineral resources, mining, and mineral processing. Vol. 11, no. 2 (2021), pp. [1-16]. - Basel : Multidisciplinary Digital Publishing Institute, 2021 Kľúč.slová minerály - minerals granáty (minerály) - garnets (minerals) chemické kompetencie Heslá geogr. Dobšiná Form.deskr. články - journal articles Jazyk dok. angličtina Krajina Švajčiarsko Anotácia Intensively metasomatized rocks from serpentinized ultramafic tectonic fragments in Dobšiná, Western Carpathians, consist of typical rodingite mineral association: hydrated garnet, vesuvianite, diopside and clinochlore. Electron microprobe analysis (EMPA) and Micro-Raman analyses of the main minerals evidence complex mineralogical evolution and variable mineral chemistry. Garnet solid solution is dominated by grossular-andradite series, which demonstrates a significant degree of hydration, mainly for grossular rich garnet cores. Garnet is locally enriched in TiO2 (up to 13 wt%), possibly indicating a chemical relic of a Ti-oxide mineral. Younger, andradite-richer garnet rims demonstrate a low degree of hydration, suggesting a harder incorporation of an (OH)− anion into its crystal structure. Garnet chemical variations display an ideal negative correlation between Al and (Fe3+ + Ti). The most recent mineral phase is represented by euhedral vesuvianite (± chlorite), which crystallizes at the expense of the garnet solid solution. This reaction shows a well-equilibrated character and indicates a high extent of rodingitization process. Chlorite thermometry models suggest an average temperature of late rodingite (trans) formation of about 265 °C. URL Link na zdrojový dokument Kategória publikačnej činnosti ADC Číslo archívnej kópie 51200 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ Odkazy PERIODIKÁ-Súborný záznam periodika 
článok
Počet záznamov: 1