KONÍČKOVÁ, Šárka, Zdeněk LOSOS, Vladimír HRAZDIL, Stanislav HOUZAR a Dalibor VŠIANSKÝ. Mineralogy of "eye-like" opals from Nová Ves near Oslavany (Moldanubian zone, Bohemian Massif). Online. In Joint 5th Central-European Mineralogical Conference and 7th Mineral Sciences in the Carpathians Conference. 2018, [citováno 2024-04-24]
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Základní údaje
Originální název Mineralogy of "eye-like" opals from Nová Ves near Oslavany (Moldanubian zone, Bohemian Massif)
Autoři KONÍČKOVÁ, Šárka, Zdeněk LOSOS, Vladimír HRAZDIL, Stanislav HOUZAR a Dalibor VŠIANSKÝ
Vydání Joint 5th Central-European Mineralogical Conference and 7th Mineral Sciences in the Carpathians Conference, 2018.
Další údaje
Originální jazyk angličtina
Typ výsledku Konferenční abstrakt
Stát vydavatele Česká republika
Utajení není předmětem státního či obchodního tajemství
Organizační jednotka Přírodovědecká fakulta
Klíčová slova anglicky eye-like concentric opal;quartz;mineralogy;weathering;serpentinite
Změnil Změnil: doc. RNDr. Zdeněk Losos, CSc., učo 2470. Změněno: 31. 7. 2018 14:15.
Anotace
The locality Nová Ves near Oslavany, situated in Moldanubian zone of western Moravia, represents the only known occurrence of zonal "eye-like" (concentric) opals in Bohemian Massif. This specific type of opal is characterized by a concentric zonal texture with white core ("eye"), brown massive translucent inner rim and locally also white porous outer rim. These opals occur in residual sediments in a small area along the contact of serpentinized peridotite and granulite. White and grey "eye" and brown inner zone contains mainly opal-CT. Quartz and moganite are present in part in white aggregates of the "eye" only. White outer rim of opals is composed of calcite with disseminated opal relics and this zone is younger as core and inner rim (calcite replaces opal). X-ray powder diffraction analyses proved presence of sepiolite admixture in brown part and accessory amount of sepiolite and chlorite in white rim.
VytisknoutZobrazeno: 24. 4. 2024 00:57