| Novak, M., Skoda, R., Filip, J., Macek, I., Vaculovic, T. (2011) Compositional trends in tourmaline from intragranitic NYF pegmatites of the Trebic pluton, Czech Republic: an electron microprobe, Mossbauer and LA-ICP-MS study. The Canadian Mineralogist, 49 (1) 359-380 doi:10.3749/canmin.49.1.359 | Journal (article/letter/editorial) | INTRAGRANITIC NYF PEGMATITES OF THE TŘEBÍ Č PLUTON, CZECH REPUBLIC: AN ELECTRON MICROPROBE, MÖSSBAUER AND LA–ICP–MS...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic Jan FILIP Regional Centre of Advanced Technologies...University, Šlechtitelů 11, CZ–783 71 Olomouc, Czech Republic Ivo MACEK Department of Geological Sciences...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic Tomáš VACULOVIČ Department of Chemistry, Masaryk...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic Abstract Tourmalines (dravite – schorl – uvite | | Čopjaková, R., Škoda, R., Vašinová Galiová, M., Novák, M. (2013) Distributions of Y + REE and Sc in tourmaline and their implications for the melt evolution; examples from NYF pegmatites of the Třebíč Pluton, Moldanubian Zone, Czech Republic. Journal of GEOsciences, 58 (2) 113-131 | Journal (article/letter/editorial) | from NYF pegmatites of the Třebíč Pluton, Moldanubian Zone, Czech Republic Renata Čopjaková1*, Radek Škoda1...Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic; copjakova@sci.muni.cz Department of Chemistry...Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic Central European Institute of Technology (CEITEC)...Masaryk University, Kamenice 5, 625 00 Brno, Czech Republic Corresponding author Tourmalines from NYF and...(NYF + LCT) pegmatites of the Třebíč Pluton (Moldanubian Zone, Czech Republic) are generally characterized | | Novak, M., Skoda, R., Gadas, P., Krmicek, L., Cerny, P. (2012) Contrasting Origins of the Mixed (NYF + LCT) Signature in Granitic Pegmatites, with Examples from the Moldanubian Zone, Czech Republic. The Canadian Mineralogist, 50 (4) 1077-1094 doi:10.3749/canmin.50.4.1077 | Journal (article/letter/editorial) | PEGMATITES, WITH EXAMPLES FROM THE MOLDANUBIAN ZONE, CZECH REPUBLIC Milan NOVÁK§, Radek ŠKODA and Petr GADAS Department...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic Lukáš KRMÍČEK Department of Geological Sciences...Brno, Czech Republic Petr Černý 4C Minerals, s.r.o. Korunní 29, CZ–120 00 Praha 2, Czech Republic Abstract...LCT) signatures from the Moldanubian Zone, Czech Republic, were examined to determine their origin. On...pegmatite-forming melt derived from the orogenic I-type Třebíč pluton. Geological, petrological, compositional | | | Journal (article/letter/editorial) | examples from NYF pegmatites of the Třebíč Pluton, Czech Republic Adam ZACHAŘ*, Milan NOVÁK, Radek ŠKODA...Masaryk University, Kotlářská 2, Brno 611 37, Czech Republic; adamzachar@seznam.cz * Corresponding author...of the Třebíč Pluton, Moldanubian Zone occurring between Třebíč and Vladislav south of the Třebíč fault...magmatic Be-minerals within a single pegmatite district is exceptional and it is constrained by variable...gadolinite-group minerals, bohseite-bavenite, NYF pegmatites, Třebíč Pluton Received: 15 April 2020; accepted: 21 July | | Sejkora, J., Litochleb, J., Novák, M., Cícha, J., Dolníček, Z. (2020) Nickel-(Bi,Ag) sulphide mineralization from NYF Vepice pegmatite, Milevsko pluton, southern Bohemia (Czech Republic) - a reflection of the parental granite chemistry. Journal of GEOsciences, 65 (3) 187-199 | Journal (article/letter/editorial) | pegmatite, Milevsko pluton, southern Bohemia (Czech Republic) – a reflection of the parental granite chemistry...museum, Cirkusová 1740, CZ-190 00, Prague 9, Czech Republic; jiri.sejkora@nm.cz Department of Geological...611 37 Brno, Czech Republic 3 Prácheň museum, Velké náměstí 114, 397 24 Písek, Czech Republic * Corresponding...parkerite, pentlandite, EPMA data, NYF pegmatite, Czech Republic Received: 22 March 2020; accepted: 25 August...as Sn (e.g., stannite, kesterite, černýite, herzenbergite; Kissin et al. 1978; Smeds 1993; Losos et al |
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