- Článek:Paragenetická charakteristika ložisek Zn–Pb rud v širším okolí Horního Města u Rýmařova (2007/1–2)Fojt, B., Dolníček, Z., Hoffman, V., Škoda, R., Trdlička, Z., Zeman, J., 2007: Paragenetická charakteristika ložisek Zn–Pb rud v širším okolí Horního Města u Rýmařova. – Acta Mus. Morav., Sci. Geol., 92, 1–2, 3–57 (with English summary)Článek v PDF
...Rhenohercynian Zone at the eastern margin of the Bohemian Massif. The stratiform sulphidic ores form lenticular bodies embedded in the so called “Horní Město volcanic complex” (URBÁNEK and VALENTA 1989). The host rocks are bimodal volcanites, which are characterized by a distinct predominance of trachytes, less rhyolites, and their pyroclastics....
- Článek:Beryl-columbitový pegmatit z Branné, Hrubý Jeseník (2003/1–2)Novák, M., Nepejchal, M., Škoda, R., Urbánek, B., 2003: Beryl-columbitový pegmatit z Branné, Hrubý Jeseník. – Acta Mus. Morav., Sci. Geol., 88, 1–2, 113–122 (with English summary)Článek v PDF
Beryl-columbite pegmatite from Branná, Hrubý Jesenik Mnts., Northern Moravia Granitic pegmatite from Branná represents typical beryl-columbite pegmatite of the Hrubý Jeseník Mts. pegmatite field. Its internal structure, textural-paragenetic units and description of minerals are given. Columbite-tantalite is a typical accessory mineral besides garnet and beryl. Dominant ferrocolumbite is enriched in...