. . "Filip, Jan" . "2"^^ . . . "Intragranitic, euxenite type NYF pegmatite Ko\u017Eichovice II derived from ultrapotassic orogenic T\u0159eb\u00ED\u010D Pluton (syenogranite) contains pale green prismatic crystals of primary beryl Ienclosed in massive quartz. Beryl I is locally altered to the secondary mineral assemblage beryl II + bavenite + bazzite + smectite. Secondary mineral assemblage after beryl I including common bavenite and elevated Ca in bazzite suggest high activity of Ca in late fluids. The temperature slightly below 250 to 350 C and neutral to slightly alkaline conditions for the formation of the secondary assemblage are suggested." . "[2F73C6698B9E]" . "0008-4476" . . . "RIV/00216224:14310/10:00049273!RIV11-GA0-14310___" . "P(GA205/07/1159), Z(MSM6198959218)" . "Unusual Na,Mg enriched beryl and its breakdown products (beryl II, bazzite, bavenite) from euxenite type NYF pegmatite related to the orogenic ultrapotassic T\u0159eb\u00ED\u010D Pluton, Czech Republic" . "2"^^ . "3" . . "Nov\u00E1k, Milan" . "CA - Kanada" . "14"^^ . . "Unusual Na,Mg enriched beryl and its breakdown products (beryl II, bazzite, bavenite) from euxenite type NYF pegmatite related to the orogenic ultrapotassic T\u0159eb\u00ED\u010D Pluton, Czech Republic"@en . "48" . . . . "The Canadian Mineralogist" . "Unusual Na,Mg enriched beryl and its breakdown products (beryl II, bazzite, bavenite) from euxenite type NYF pegmatite related to the orogenic ultrapotassic T\u0159eb\u00ED\u010D Pluton, Czech Republic"@en . . . . "Unusual Na,Mg enriched beryl and its breakdown products (beryl II, bazzite, bavenite) from euxenite type NYF pegmatite related to the orogenic ultrapotassic T\u0159eb\u00ED\u010D Pluton, Czech Republic" . . "RIV/00216224:14310/10:00049273" . "14310" . "Intragranitic, euxenite type NYF pegmatite Ko\u017Eichovice II derived from ultrapotassic orogenic T\u0159eb\u00ED\u010D Pluton (syenogranite) contains pale green prismatic crystals of primary beryl Ienclosed in massive quartz. Beryl I is locally altered to the secondary mineral assemblage beryl II + bavenite + bazzite + smectite. Secondary mineral assemblage after beryl I including common bavenite and elevated Ca in bazzite suggest high activity of Ca in late fluids. The temperature slightly below 250 to 350 C and neutral to slightly alkaline conditions for the formation of the secondary assemblage are suggested."@en . "294425" . "Beryl bazzite bavenite electron microprobe M\u00F6ssbauer spectroscopy granitic pegmatite T\u0159eb\u00ED\u010D Pluton Czech Republic"@en . .