• Biografie:
    Zemřel Doc. Ing. Dušan Němec (2002/1–2)
    Houzar, S., 2002: Zemřel Doc. Ing. Dušan Němec. - Acta Mus. Moraviae, Sci. Geol., 87, 1-2, 221-222

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  • Článek:
    Vysoce hlinité amfibolity Českomoravské vrchoviny (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 part of the Svratka Complex). Their occurrences evidently...

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  • Článek:
    Cummingtonitové amfiboly a jejich postavení v západomoravském moldanubiku (2001/1–2)
    Němec, D., 2001: Cummingtonite amphibolites and their position within the West Moravian Moldanubian Zone. - Acta Mus. Moraviae, Sci. Geol., 86, 1-2, 93-102 (with Czech summary)

    ...a within-plate basalt, while the West Moravian calcic amphibolites are tholeiitic in nature and originally were MORBs. If rocks, which under conditions of the almandine-amphibolite facies yielded cummingtonite amphibolites were in the West Moravian Moldanubian Zone metamorphosed under granulite facies conditions, clinohypersthene-bearing amphibolites originated instead. Different geotectonic setting deduced for...

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  • Článek:
    Vysoce mafické amfibolity moldanubika Českomoravské vrchoviny (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. They are associated with marginal-sea-type metasediments, forming there...

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  • Článek:
    Regionální typizace skarnů Fe Českomoravské vrchoviny (1991/1–2)
    Němec, D., 1991: Regional typization of the iron skarns of the Bohemian-Moravian Heights (Českomoravská vrchovina). - Acta Mus. Moraviae, Sci. Nat., 76, 1-2, 51-82 (with Czech summary)

    ...gneisses, metamorphism took place isochemically. Due to metamorphism the skarns acquired the petrographical characteristics of metamorphic rocks. During regional metamorphism, almandine, grossularite-almandine and hornblende originated. Diopside-hedenbergite, grossularite-andradite, epidote and magnetite are relict minerals. Minerals of the skarns are characterized on the basis of their chemical composition. Chemical equilibria of some...

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