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Názov Chromium- and nickel-rich micas and associated minerals in listvenite from the Muranska Zdychava, Slovakia: products of hydrothermal metasomatic transformation of ultrabasic rock Aut.údaje Štefan Ferenc ... [et al.] Autor Ferenc Štefan 1977- (35%) UMBFP01 - Katedra geografie a geológie
Spoluautori Uher Pavel (35%)
Spišiak Ján 1953- (15%) UMBFP01 - Katedra geografie a geológie
Šimonová Viera 1977- (15%) UMBFP01 - Katedra geografie a geológie
Zdroj.dok. Journal of Geosciences. Vol. 61, no. 3 (2016), pp. 239-254. - Prague : Czech Geological Society, 2016 Kľúč.slová mineralizácia - mineralization sulfidické minerály mineralization sulfidická mineralizácia - sulfide mineralization Heslá geogr. Západné Karpaty (pohorie) Muránska Zdychava (Slovensko) Jazyk dok. angličtina Krajina Česká republika Systematika 55 Anotácia The Cr-Ni-rich micas, Ni-Co sulphide phases and associated minerals occur in a small body of listvenite, an extensively altered serpentinite, in Lower Palaeozoic paragneisses near Murnska Zdychava village in Slovensk Rudohorie Mts. (Veporic Superunit, central Slovakia). The main rock-forming minerals of the listvenite are magnesite, dolomite and a serpentine-group mineral, less frequently calcite, quartz and talc. Accessory minerals of the listvenite include Cr-Ni-rich micas, chromite, and Ni-Co-Fe-(Cu-Pb) sulphide minerals (pyrite, pyrrhotite, pentlandite, millerite, polydymite, violarite, siegenite, gersdorffite, cobaltite, chalcopyrite and galena). The micas from the Muranska Zdychava listvenite (Cr-Ni-rich illite to muscovite and Ni-dominant trioctahedral mica) contain the highest Ni concentrations ever reported in the mica-group minerals (up to 22.8 wt. % NiO or 1.46 apfu Ni). The Cr concentrations are also relatively high (up to 11.0 wt. % Cr2O3 or 0.64 apfu). Compositional variations in both Cr-Ni-rich mica minerals are characterized by the negative Cr vs. Ni correlation that indicates a dominant role of 2(O)M(3)+ + (O) = 3(O)M(2)+ and M-O(3)+ + Al-T = M-O(2)+ + Si-T substitution mechanisms. Chromite is dominated by Fe2+ (0.82-0.90 apfu) and Cr (1.38-1.79 apfu). URL Link do databázy WoS Kategória publikačnej činnosti ADC Číslo archívnej kópie 37893 Kategória ohlasu JÉBRAK, Michel - LEBRUN, Charline - ANDRÉ-MAYER, Anne Sylvie - SIMARD, Marjorie. Native antimony emplaced by methane-rich hydrothermal fluid in an orogenic fault-zone. In Terra nova. ISSN 0954-4879, 2017, vol. 29, no. 6, pp. 401-408.
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NAING, Thet - MIN TUN, Myo. The characteristics of nickel-chromite mineralization in Mwetaung-Phataung area, Teddim township, Chin state. In The third Myanmar national conference on earth sciences : MNCES, 2019, Mandalay, 7th-8th November 2019. Mandalay : Yadanabon university, 2019. Pp. 586-598.
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