. . "tremolite; phlogopite; marble; mineral assemblages; lithology; chemistry; metamorphism; Moldanubicum; Moravicum; Silesicum"@en . "4"^^ . "0"^^ . "4"^^ . "920"^^ . "Tmavo\u0161ed\u00E9 tremolitem bohat\u00E9 mramory p\u0159edstavuj\u00ED specifick\u00FD litotyp v r\u00E1mci metakarbon\u00E1tov\u00FDch hornin \u010Cesk\u00E9ho mas\u00EDvu, termolit tvo\u0159\u00ED velk\u00E9 porfyroblasty a objemov\u011B jednozna\u010Dn\u011B p\u0159eva\u017Euje nad flogopitem. Tyto mramory jsou typicky spjaty s grafitick\u00FDmi horninami a vystupuj\u00ED p\u0159ev\u00E1\u017En\u011B v pestr\u00FDch jednotk\u00E1ch p\u0159i v\u00FDchodn\u00EDm okraji \u010Cesk\u00E9ho mas\u00EDvu (drosendorfsk\u00E1 jednotka, vrat\u011Bn\u00EDnsk\u00E1 jednotka, vranovsk\u00E1 jednotka, ole\u0161nick\u00E1 jednotka, velkovrbensk\u00E1 jednotka). Nejsou zn\u00E1my z dal\u0161\u00EDch jednotek \u010Cesk\u00E9ho mas\u00EDvu s v\u00FDjimkou pestr\u00E9 skupiny moldanubika v okol\u00ED \u010Cesk\u00E9ho Krumlova. Detailn\u00ED litologick\u00E9, petrologick\u00E9 a geochemick\u00E9 studium tremolitov\u00FDch mramor\u016F a s nimi spjat\u00FDch metakarbon\u00E1t\u016F v\u010Detn\u011B vztahu k okoln\u00EDm hornin\u00E1m povede k porovn\u00E1n\u00ED metamorfn\u00ED i p\u0159edmetamorfn\u00ED historie t\u011Bchto specifick\u00FDch hornin v r\u00E1mci r\u016Fzn\u00FDch jednotek, co\u017E m\u016F\u017Ee v\u00FDznamn\u011B p\u0159isp\u011Bt k litostratigrafii a geotektonick\u00FDm model\u016Fm v\u00FDvoje v\u00FDchodn\u00ED \u010D\u00E1sti \u010Cesk\u00E9ho mas\u00EDvu."@cs . . . . . "0"^^ . "Tremolitem bohat\u00E9 mramory jako specifick\u00FD litotyp pro korelace pestr\u00FDch jednotek ve v\u00FDchodn\u00ED \u010D\u00E1sti \u010Cesk\u00E9ho mas\u00EDvu"@cs . . "Tremolite-bearing marbles as a specific lithotype for correlation of metacarbonate-bearing variegated units in the eastern part of the Bohemian Massif"@en . . "2"^^ . "Dark grey tremolite-rich marbles represent a specific lithotype within metacarbonates of the Bohemian Massif (BM) characterized by large tremolite prophyroblast and evident predominance of tremolite over phlogopite. These marbles are typically associated with graphite-rich rocks and almost exclusively occur in several lithotectonic units situated along the eastern margin of Bohemian Massif (Drosendorf Unit, Vran\u011Bn\u00EDn Unit, Vranov Unit, Ole\u0161nice Unit, Velk\u00E9 Vrbno Unit). They are not know from the adjacent geological units except the \u010Cesk\u00FD Krumlov Unit from the Moldanubian Zone. Detailed lithological, petrological, and geochemical study of the tremolite-rich marbles, associated metacarbonates and their host rock lithologies may provide insigh on premetamorphic and metamorphic history of lithologically very similar rocks from distinct units and thus contribute to lithostratigraphic and geotectonic models of the eastern part of Bohemian Massif."@en . "531"^^ . .