"535825" . "Petrogeneze magmatit\u016F s\u00E1zavsk\u00E9ho typu st\u0159edo\u010Desk\u00E9ho plutonick\u00E9ho komplexu" . . "Petrogeneze magmatit\u016F s\u00E1zavsk\u00E9ho typu st\u0159edo\u010Desk\u00E9ho plutonick\u00E9ho komplexu"@cs . . . "Petrogenesis of magmatites of the S\u00E1zava type (Central Bohemian Plutonic Complex"@en . "CZ - \u010Cesk\u00E1 republika" . "13" . "1"^^ . . . . "Petrogeneze magmatit\u016F s\u00E1zavsk\u00E9ho typu st\u0159edo\u010Desk\u00E9ho plutonick\u00E9ho komplexu"@cs . . . "Ren\u00E9, Milo\u0161" . "Bulletin mineralogicko-petrografick\u00E9ho odd\u011Blen\u00ED N\u00E1rodn\u00EDho muzea" . "Z(AV0Z30460519)" . . "Petrogeneze magmatit\u016F s\u00E1zavsk\u00E9ho typu st\u0159edo\u010Desk\u00E9ho plutonick\u00E9ho komplexu" . . . "granite; geochemistry; petrology"@en . "1211-0329" . . . "Petrogenesis of magmatites of the S\u00E1zava type (Central Bohemian Plutonic Complex"@en . "RIV/67985891:_____/05:00044214!RIV07-AV0-67985891" . "[6179C4227356]" . "For intrusive rocks suite of the S\u00E1zava type is significant its metaaluminous to slightly peraluminous character, granodiorite-quartz diorite modal composition and hybrid features. Considerable source of granite melts probably were metabasite comfortable to J\u00EDlov\u00E9 belt metabasites."@en . . "Intruzivn\u00ED horniny s\u00E1zavsk\u00E9ho typu lze charakterizovat metaaluminick\u00FDm a\u017E nev\u00FDrazn\u011B peraluminick\u00FDm charakterem, granodiorit-kvarcdioritov\u00FDm mod\u00E1ln\u00EDm slo\u017Een\u00EDm a hybridn\u00EDm charakterem. V\u00FDznamn\u00FDm zdrojem granitov\u00E9 taveniny byly pravd\u011Bpodobn\u011B metabazity bl\u00EDzk\u00E9 metabazit\u016Fm j\u00EDlovsk\u00E9ho p\u00E1sma."@cs . "-" . "RIV/67985891:_____/05:00044214" . . "199;204" . "Intruzivn\u00ED horniny s\u00E1zavsk\u00E9ho typu lze charakterizovat metaaluminick\u00FDm a\u017E nev\u00FDrazn\u011B peraluminick\u00FDm charakterem, granodiorit-kvarcdioritov\u00FDm mod\u00E1ln\u00EDm slo\u017Een\u00EDm a hybridn\u00EDm charakterem. V\u00FDznamn\u00FDm zdrojem granitov\u00E9 taveniny byly pravd\u011Bpodobn\u011B metabazity bl\u00EDzk\u00E9 metabazit\u016Fm j\u00EDlovsk\u00E9ho p\u00E1sma." . "6"^^ . "1"^^ .