"0028-3649" . "Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Ro\u017En\u00E1 uranium deposit, Western Moravia, Czech Republic"@en . "RIV/00216224:14310/06:00016622!RIV10-MSM-14310___" . "Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Ro\u017En\u00E1 uranium deposit, Western Moravia, Czech Republic" . . . . . "481682" . . . "Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Ro\u017En\u00E1 uranium deposit, Western Moravia, Czech Republic" . "\u0160koda, Radek" . . . . . . . . "Laud\u00E1tov\u00E1, Hana" . . "RIV/00216224:14310/06:00016622" . "14310" . . "Neues Jahrbuch fur Mineralogie, Abhandlungen" . . "Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Ro\u017En\u00E1 uranium deposit, Western Moravia, Czech Republic"@en . "Ba-micas including magnesian kinoshitalite (XMg more than 0.99) were found in sulphide-rich dolomite marbles at the Ro\u017En\u00E1 uranium deposit, Moldanubicum, Czech Republic. The Ba-micas (phlogopite with Ba > 0.280 apfu and kinoshitalite with Ba from 0.869 to 1.244 apfu) are Mn, Fe and Ti-poor in comparison to other Ba-micas described up to date. The main substitution mechanism in Ba-micas is (Ba2+,Ca2+) (Al3+) (K+,Na+)-1 Si4+-1. Relatively high content of Mn in silicates and carbonates from the host marble is in contrast to the chemistry of Ba-micas. Barium and manganese show distinct behaviour during metamorphism. Manganese and iron were probably partitioned to metamorphic sphalerite and pyrrhotite relative to (Mn, Fe)-poor Ba-micas. Barium concentrated in mica minerals and the system was evidently Ba-depleted in late stages." . . "182/2006" . "7"^^ . "2" . "DE - Spolkov\u00E1 republika N\u011Bmecko" . . "Losos, Zden\u011Bk" . . . "Ba-micas including magnesian kinoshitalite (XMg more than 0.99) were found in sulphide-rich dolomite marbles at the Ro\u017En\u00E1 uranium deposit, Moldanubicum, Czech Republic. The Ba-micas (phlogopite with Ba > 0.280 apfu and kinoshitalite with Ba from 0.869 to 1.244 apfu) are Mn, Fe and Ti-poor in comparison to other Ba-micas described up to date. The main substitution mechanism in Ba-micas is (Ba2+,Ca2+) (Al3+) (K+,Na+)-1 Si4+-1. Relatively high content of Mn in silicates and carbonates from the host marble is in contrast to the chemistry of Ba-micas. Barium and manganese show distinct behaviour during metamorphism. Manganese and iron were probably partitioned to metamorphic sphalerite and pyrrhotite relative to (Mn, Fe)-poor Ba-micas. Barium concentrated in mica minerals and the system was evidently Ba-depleted in late stages."@en . "4"^^ . . "3"^^ . "Z(MSM0021622410), Z(MSM0021622412)" . "[7045D5F902F7]" . "Houzar, Stanislav" . . "kinoshitalite; Ba-micas; sphalerite; marble; Ro\u017En\u00E1 uranium deposit; Moldanubicum; Bohemian Massif; Czech Republic"@en . .