• Article:
    Highly mafie amphibolites in the Moldanaubian Zone of the Bohemian-Moravian Heights (Českomoravská vrchovina) (1998/1–2)
    Němec, D., 1998: Vysoce mafické amfibolity moldanubika Českomoravské vrchoviny. - Acta Mus. Moraviae, Sci. Geol., 83, 1-2, 59-71 (with Czech summary)
    Highly mafie amphibolites in the Moldanaubian Zone of the Bohemian-Moravian Heights (Českomoravská vrchovina) In the Chýnov zone which encompasses the area E of the town of Tábor and belongs to the Moldanubian Varied series, highly mafie amphibolites occur that are almost monomineral.…
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  • Article:
    High-Al amphibolites of the Bohemian-Moravian Heights (1997/1–2)
    Němec, D., 1997: High-Al amphibolites of the Bohemian-Moravian Heights. - Acta Mus. Moraviae, Sci. Geol., 82, 1-2, 63-72 (with Czech summary)
    High-Al amphibolites of the Bohemian-Moravian Heights In the Bohemian-Moravian Heights high-Al amphibolites having 21-22 wt % Alp, were observed in four amphibolite complexes (at Kozlov, Račice and Rožná in the Strážek subdivision of the Moldanubian Complex, and at Kasany in the southernmost…
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  • Article:
    Metamorphic evolution of Upper Moravian Nappe in the South part of the Svratka Dome (2011/1)
    Buriánek, D., 2011: Metamorfní vývoj svrchního příkrovu moravika v jižním křídle svratecké klenby. – Acta Mus. Moraviae, Sci. geol., 96, 1, 33–46 (with English summary)
    Metamorphic evolution of Upper Moravian Nappe in the South part of the Svratka Dome The southern part of the Svratka Dome is built two crystalline napes overlying Cadomian basement (Brunovistulicum) and its Devonian cover. The Upper Moravian Nappe consists of orthogneisses, muscovite to muscovite-biotite…
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