- Článek:Výskyt a mineralogie zeleného chalcedonu (plazmy) v reziduích moravských serpentinitů (moldanubikum, Český masiv) (2014/2)Koníčková, Š., 2014: Výskyt a mineralogie zeleného chalcedonu (plazmy) v reziduích moravských serpentinitů (moldanubikum, Český masiv). – Acta Musei Moraviae, Sci. geol., 99, 2, 3–36 (with English summary)Článek v PDF
Occurence and mineralogy of green chalcedony (plasma) in serpentinite residues at Moravia (Moldanubian Zone, Bohemian Massif) Massive green chalcedony (plasma) represents a specific mineral in the weathering zone at serpentinized peridotites of western Moravia (Moldanubian Zone, Bohemian Massif). Plasma consists mainly of microand non-crystalline silica minerals with different proportions of...
- Článek:Velké porfyroblasty almandinu ze Senorad, západní Morava (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)Článek v PDF
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 Prp16–22 Grs0–6 Adr1–6). Only weak diffuse zonation (Mn-rich core and Mg-rich rim) and inclusions of quartz, ilmenite, apatite and...