• Article:
    Barium phlogopite and kinoshitalite-bearing mineral assemblage of forsterite marbles from Rožná uranium deposit, Moldanubicum, western Moravia (2005/1–2)
    Doležalová, H., Houzar, S., Škoda, R., 2005: Minerální asociace forsteritových mramorů s Ba-flogopitem a kinoshitalitem na uranovém ložisku Rožná, moldanubikum, západní Morava. – Acta Mus. Morav., Sci. Geol., 90, 1–2, 75–88 (with English summary)
    Barium phlogopite and kinoshitalite-bearing mineral assemblage of forsterite marbles from Rožná uranium deposit, Moldanubicum, western Moravia Ore-bearing dolomite marbles with rare Ba-micas (kinoshitalite, Ba-phlogopite) were studied in uranium deposit Rožná. Mineral assemblage, chemical…
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  • Article:
    Tourmaline from the mica schist of the Svratka Crystalline Complex (2008/1–2)
    Buriánek, D., Čopjaková, R., 2008: Turmalíny ze svorů svrateckého krystalinika. – Acta Mus. Morav., Sci. Geol., 93, 1–2, 61–79 (with English summary)
    Tourmaline from the mica schist of the Svratka Crystalline Complex Tourmaline is a typical accessory mineral for most of micaschists in the Svratka Crystalline Complex. Based on petrographic and chemical data, two main generations of tourmaline have been distinguished. The first generation…
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  • Article:
    Three genetically different types of garnet-rich rocks from Hlinsko Zone and from Polička Crystalline Complex (2007/1–2)
    Buriánek, D., Otava, J., 2007: Tři geneticky rozdílné typy granátovců z hlinské zóny a poličského krystalinika. – Acta Mus. Morav., Sci. Geol., 92, 1–2, 143–150 (with English summary)
    Three genetically different types of garnet-rich rocks from Hlinsko Zone and from Polička Crystalline Complex The garnet-rich rocks are spatially associated with two metamorphosed volcano-sedimetary complexes at the eastern border of the Bohemian Massiv (Polička Crystalline Complex and…
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  • Article:
    Tourmalinites from the southern part of Svratka Crystalline Complex (2007/1–2)
    Čopjaková, R., Buriánek, D., Škoda, R., Houzar, S., 2007: Turmalinity jižní části svrateckého krystalinika. – Acta Mus. Morav., Sci. Geol., 92, 1–2, 111–130 (with English summary)
    Tourmalinites from the southern part of Svratka Crystalline Complex Tourmalinites from the southern part of the Svratka Crystalline complex form stratiform layers hosted in mica schist. They probably represent a part of metamorphosed volcano-sedimentary complex primary rich in F and B. Whole…
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  • Article:
    Mineralogy, petrography and geology of the Nedvědice marbles, Svratka Crystalline Complex; a review (2006/1–2)
    Houzar, S., Novák, M., Doležalová, H., Hrazdil, V., Pfeiferová, A., 2006: Přehled mineralogie, petrografie a geologie nedvědických mramorů, svratecké krystalinikum. – Acta Mus. Morav., Sci. Geol., 91, 1–2, 3–77 (with English summary)
    Mineralogy, petrography and geology of the Nedvědice marbles, Svratka Crystalline Complex; a review Nedvědice marbles occur in a narrow belt situated along the eastern and northeastern margin of the Svratka Crystalline Complex (Moldanubian Zone). Elongated bodies of calcite marbles up to…
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  • Article:
    Metamorphic evolution of mica-schists and their tectonic position in the Polička Crystalline Complex (2009/1–2)
    Buriánek, D., 2009: Metamorfní vývoj svorů a jejich tektonická pozice v poličském krystaliniku, Acta Mus. Moraviae, Sci. geol., 94, 1-2, 111–128 (with Englis summary)
    Metamorphic evolution of mica-schists and their tectonic position in the Polička Crystalline Complex The Polička Crystalline Complex is situated in the eastern part of the Bohemian Massif. This metamorphosed volcano-sedimentary complex is composed mainly of biotite to two mica gneisses.…
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  • Article:
    Zirconolite in marble at Krahulov and age of HT/LP metamorphism in the contact aureole of the Třebíč Pluton (Moldanubian zone) (2009/1–2)
    Čopjaková, R., Houzar, S., 2009: Zirkonolit v mramoru u Krahulova a stáří HT/LP metamorfózy moldanubika v kontaktní aureole třebíčského plutonu. – Acta Mus. Morav., Sci. Geol., 94, 1–2, 67–76 (with English summary)
    Zirconolite in marble at Krahulov and age of HT/LP metamorphism in the contact aureole of the Třebíč Pluton (Moldanubian zone) Regional-scale contact metamorphism of the Třebíč Pluton led to the formation of distinct zoning manifested typically in dolomite marbles. Inside part of metamorphic…
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  • Article:
    Mineralogy of magnetite-grunerite-siderite ores in Radoškov (Bílý potok Unit, Svratka dome, Moravicum) (2013/2)
    Víšková, E., Fojt, B., Hrazdil, V., Houzar, S., 2013: Mineralogie magnetit-grunerit-sideritového zrudnění z Radoškova (jednotka Bílého potoka, svratecká klenba, moravikum). – Acta Mus. Morav., Sci. Geol., 98, 2, 39–50 (with English summary)
    Mineralogy of magnetite-grunerite-siderite ores in Radoškov (Bílý potok Unit, Svratka dome, Moravicum) Metamorphic iron mineralization was documented in an abandoned adit east of Radoškov, Czech Republic. Siderite-rich ore with magnetite, amphibole asbestos, chlorite and small amounts…
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  • Article:
    Large almandine porphyroblasts from Senorady, western Moravia (2015/2)
    Buriánek, D., Houzar, S., Hrazdil, V., Koníčková, Š., Toman, J., 2015: Velké porfyroblasty almandinu ze Senorad, západní Morava. – Acta Mus. Morav., Sci. Geol., 100, 2, 17–28 (with English summary)
    Large almandine porphyroblasts from Senorady, western Moravia Large garnet crystals (porphyroblasts) occur in migmatized biotite paragneiss near Senorady (Moldanubian Zone, Western Moravia). In their chemical composition prevails almandine komponent (Alm68–72 Sps3–10
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