| Bačík, P., Uher, P., Cempírek, J., Vaculovič, T. (2012) Magnesian tourmalines from plagioclase-muscovite-scapolite metaevaporite layers in dolomite marble near Prosetín (Olešnice Unit, Moravicum, Czech Republic) Journal of GEOsciences, 57 (3) 143-153 | Journal (article/letter/editorial) | layers in dolomite marble near Prosetín (Olešnice Unit, Moravicum, Czech Republic) Peter BAČÍK1,*, Pavel UHER1...Petrology, Mlynská dolina, 842 15 Bratislava, Slovak Republic; bacikp@fns.uniba.sk 2 Department of Mineralogy...Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic 3 Department of Earth and Ocean Sciences, University...Masaryk University, Kamenice 5, 625 00 Brno, Czech Republic * Corresponding author 1 Radial aggregates...layers in dolomite marble near Prosetín (Olešnice Unit, Moravicum, Czech Republic). It occurs in association | | Gadas, Petr, Novák, Milan, Cempírek, Jan, Filip, Jan, Vašinová Galiová, Michaela, Groat, Lee A., Všianský, Dalibor (2014) Mineral assemblages, compositional variation, and crystal structure of feruvitic tourmaline from a contaminated anatectic pegmatite at Mirošov near Strážek, Moldanubian zone, Czech Republic. The Canadian Mineralogist, 52 (2) 285-301 doi:10.3749/canmin.52.2.285 | Journal (article/letter/editorial) | AT MIROŠOV NEAR STRÁŽEK, MOLDANUBIAN ZONE, CZECH REPUBLIC Petr GADAS§ and Milan NOVÁK Department of Geological...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic Jan CEMPÍREK Department of Earth, Ocean and...Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic Jan FILIP Regional Centre of Advanced Technologies...University, 17. listopadu 12, CZ–771 46, Olomouc, Czech Republic Michaela VAŠINOVÁ GALIOVÁ Department of Chemistry...Masaryk University, Kotlářská 2, CZ–611 37 Brno, Czech Republic and Central European Institute of Technology | | Ertl, Andreas, Topa, Dan, Giester, Gerald, Rossman, George R., Tillmanns, Ekkehart, Konzett, Jürgen (2019) Sr-bearing high-pressure tourmaline from the Kreuzeck Mountains, Eastern Alps, Austria. European Journal of Mineralogy, 31 (4) 791-798 doi:10.1127/ejm/2019/0031-2863 | Journal (article/letter/editorial) | Hughes (2002) on Fe-bearing olenite and on Al-rich schorl also showed substantial amounts of [4]B. “Oxy-rossmanite”...analyses in the core region (crystal structure see Tables 1–3); Zone 2, 5 analyses (core region); Zone 3, 5 analyses...analyses (rim region); Zone 4, 2 analyses (rim region). Li (16–30 ppm) was determined on a bulk sample...metaevaporite layers in dolomite marble near Prosetín (Moravicum, Czech Republic), blue-grey Mg-rich tourmalines were...layers in dolomite marble near Prosetín (Olešnice Unit, Moravicum, Czech Republic). J. Geosci., 57, 143–153 | | Bačík, P., Uher, P., Dikej, J., Puškelová, Ľ. (2018) Tourmalines from the siderite-quartz-sulphide hydrothermal veins, Gemeric unit, western Carpathians, Slovakia: crystal chemistry and evolution. Mineralogy and Petrology, 112 (1) 45-63 doi:10.1007/s00710-017-0500-8 | Journal (article/letter/editorial) | mentioned deposits belong mostly to the alkali group, schorl to dravite series, rarely dominant X-site vacant...of tourmaline precipitation in the entire ore district, and the possible fluid sources, as essentially...on the large-scale processes acting in the ore district. Geological settings The investigated tourmaline-bearing...Museum, London and Geological Survey of the Slovak Republic, Bratislava. Operating conditions were set at... Dobšiná TU-1 schorl Dobšiná TU-1 schorl Vlachovo TU-2 foitite Vlachovo TU-2 schorl R. Bystré TU-3 | | Bačík, Peter, Dikej, Jakub, Fridrichová, Jana, Miglierini, Marcel, Števko, Martin (2017) Chemical composition and evolution of tourmaline-supergroup minerals from the Sb hydrothermal veins in Rožňava area, Western Carpathians, Slovakia. Mineralogy and Petrology, 111 (4) 609-624 doi:10.1007/s00710-017-0507-1 | Journal (article/letter/editorial) | Peter-Pavol are almost homogeneous with intermediate schorl-dravite composition. Čučma – Gabriela tourmaline...Technology, Ilkovičova 3, 812 19 Bratislava, Slovak Republic formula unit). Based on Mössbauer spectra, the...fluids forming tourmaline. Keywords Tourmaline . Schorl-dravite . Feruvite . Magnesio-foitite . Hydrothermal...in granitic rocks and their derivatives with the schorl-foitite composition (Broska et al. 1999). It also...tourmaline composition varies mainly between foitite and schorl, rarely dravite, fluordravite to fluor-uvite and | | Bačík, Peter, Koděra, Peter, Uher, Pavel, Ozdín, Daniel, Jánošík, Michal (2015) Chlorine-Enriched Tourmalines In Hydrothermally Altered Diorite Porphyry From the Biely Vrch Porphyry Gold Deposit (Slovakia) The Canadian Mineralogist, 53 (4) 673-691 doi:10.3749/canmin.1500013 | Journal (article/letter/editorial) | Petrology, Mlynská dolina, 842 15 Bratislava, Slovak Republic PETER KODĚRA Comenius University in Bratislava...Deposits, Mlynská dolina, 842 15 Bratislava, Slovak Republic PAVEL UHER AND DANIEL OZDÍN Comenius University...Petrology, Mlynská dolina, 842 15 Bratislava, Slovak Republic MICHAL JÁNOŠÍK Comenius University in Bratislava...Deposits, Mlynská dolina, 842 15 Bratislava, Slovak Republic ABSTRACT Chlorine-enriched tourmaline was found...magnesio-foitite, and foitite), alkali (oxy-schorl, schorl), and calcic (feruvite) tourmaline. The variation | | | Journal (article/letter/editorial) | tourmalines are mainly dravite with a prevalent schorl end-member with average XMg values over 0.6. Apart...and are therefore classified as minerals of the schorl-dravite series [35,36]. In igneous rocks, tourmaline...analysed tourmalines can be classified as of the schorl–dravite series (Figure 6). cases its concentrations...analysed tourmalines can be classified as of the schorl–dravite series (Figure 6). The high XMg = Mg/(Mg...remaining 18 grains, the inner core was enriched in Fe (schorl-like cores, not show a clear pattern in chemical | | Cempírek, J., Houzar, S., Novák, M., Groat, L. A., Selway, J. B., Šrein, V. (2013) Crystal structure and compositional evolution of vanadium-rich oxy dravite from graphite quartzite at Bítovánky, Czech Republic. Journal of GEOsciences, 58 (2) 149-162 | Journal (article/letter/editorial) | oxy‑dravite from graphite quartzite at Bítovánky, Czech Republic Jan Cempírek1,2,*, Stanislav Houzar2, Milan...Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic; jcempirek@mzm.cz Department of Geological...Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic Caracle Creek International Consulting Inc... P3C 4Y9, Canada Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic Corresponding author...(a joint facility of Masaryk University and the Czech Geological Survey). The compositional data were | | Dzikowski, Tashia J., Cempírek, Jan, Groat, Lee A., Dipple, Gregory M., Giuliani, Gaston (2014) Origin of gem corundum in calcite marble: The Revelstoke occurrence in the Canadian Cordillera of British Columbia. Lithos, 198. 281-297 doi:10.1016/j.lithos.2014.03.030 | Journal (article/letter/editorial) | Mineralogy, Moravian Museum, Zelný trh 6, Brno, Czech Republic, 61137 NU IRD et CRPG/CNRS, Centre de Recherches...The Omineca Belt is a northwest trending uplifted region of metamorphic and plutonic rocks separating accreted...apfu, , WO ≤ 0.46 apfu) and Ca,Fe-enriched rims of schorl-dravite, Na-rich uvite and fluor-uvite (XMg=0.46-0...and G.M.D., by the Ministry of Culture of the Czech Republic (as part of its long-term conceptual development...tourmaline in metacherts from PT Chvojnica, Slovak Republic: crystal chemistry and multistage evolution. Canadian | | | Conference Proceedings (Volume) | Neoproterozoic rocks in the Lufilian belt, Domes region, Zambia .........................................through polycyclic orogeny: the example of the Litsa district, Russia Anne-Sylvie André-Mayer, Michel Cuney...mantle-crustal ore-forming systems of the Pechenga ore district (Fennoscandian shield) ........................mineralization of Manono-Kitotolo (Katanga, Democratic Republic of Congo): current state of knowledge . . .....Moravian archaeological site Břeclav-Pohansko, Czech republic ......................................... |
|