| Názov | Chromium- and nickel-rich micas and associated minerals in listvenite from the Muranska Zdychava, Slovakia: products of hydrothermal metasomatic transformation of ultrabasic rock
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| Aut.údaje | Štefan Ferenc ... [et al.]
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| Autor | Ferenc Štefan 1977- (35%) UMBFP01 - Katedra geografie a geológie
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| Spoluautori | Uher Pavel (35%)
Spišiak Ján 1953- (15%) UMBFP01 - Katedra geografie a geológie
Šimonová Viera 1977- (15%) UMBFP01 - Katedra geografie a geológie
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| Zdroj.dok. | Journal of Geosciences. Vol. 61, no. 3 (2016), pp. 239-254. - Prague : Czech Geological Society, 2016
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| Kľúč.slová |
mineralizácia - mineralization
sulfidické minerály
sulfidická mineralizácia - sulfide mineralization
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| Heslá geogr. | Západné Karpaty (pohorie)
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| Muránska Zdychava (Slovensko)
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| Jazyk dok. | angličtina
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| Krajina | Česká republika
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| Systematika | 55
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| 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).
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| Kategória publikačnej činnosti | ADC
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| Číslo archívnej kópie | 37893
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| Katal.org. | BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
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| Báza dát | xpca - PUBLIKAČNÁ ČINNOSŤ
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| Odkazy | PERIODIKÁ-Súborný záznam periodika
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