"Two types of retrograde metamorphosed eclogite from \u010Cejkov were investigated. The first type is pyroxene-bearing amphibolite with pseudomorphs after garnet (Ca-amphibole, clinopyroxene, plagioclase, orthopyroxene) without a visible structure of the original eclogite. The second type is retrograde metamorphosed eclogite with Ca and Fe-Mg-Mn-Li-amphibole, garnet, plagioclase, clinopyroxene and orthopyroxene that contain abundant clinopyroxene-plagioclase and orthopyroxene-plagioclase symplectites after omphacite (up to c. 75 vol. %). The symplectite rims garnet grains (pseudomorphs after garnet) are a common feature in both rock types and they represent changes from eclogite to amphibolite-granulite facies conditions."@en . . "42565" . "15"^^ . "Retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit od \u010Cejkova u Nov\u00E9ho Rychnova (Moldanubikum, \u010Cesk\u00E1 republika)" . "Bulletin mineralogicko-petrologick\u00E9ho odd\u011Blen\u00ED N\u00E1rodn\u00EDho muzea v Praze" . "RIV/00023272:_____/14:#0002409!RIV15-MK0-00023272" . . "Retrogradely metamorphosed eclogite from \u010Cejkov near Nov\u00FD Rychnov (Moldanubian Zone, Czech Republic)"@en . "1211-0329" . . "CZ - \u010Cesk\u00E1 republika" . "Litochleb, Ji\u0159\u00ED" . "Halodov\u00E1, Patricie" . . "2" . "I" . . "5"^^ . . . "\u0160koda, Radek" . . "Retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit od \u010Cejkova u Nov\u00E9ho Rychnova (Moldanubikum, \u010Cesk\u00E1 republika)" . . . . . "Retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit od \u010Cejkova u Nov\u00E9ho Rychnova (Moldanubikum, \u010Cesk\u00E1 republika)"@cs . "2"^^ . "\u0160reinov\u00E1, Blanka" . . "Retrogradely metamorphosed eclogite from \u010Cejkov near Nov\u00FD Rychnov (Moldanubian Zone, Czech Republic)"@en . "Fi\u0161era, Milan" . "[120B2B39AFF1]" . . "RIV/00023272:_____/14:#0002409" . "retrograde metamorphosed eclogite; symplectite; chemical composition; \u010Cejkov locality; Czech Republic"@en . "P\u0159edm\u011Btem v\u00FDzkumu byly dva typy retrogr\u00E1dn\u011B metamorfovan\u00E9ho eklogitu z \u010Cejkova. Prvn\u00EDm typem je pyroxenick\u00FD amfibolit s pseudomorf\u00F3zami po gran\u00E1tu (Ca-amfibol, klinopyroxen, plagioklas, ortopyroxen) bez viditeln\u00E9 struktury p\u016Fvodn\u00EDho eklogitu. Druh\u00FDm typem je retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit s Ca a Fe-Mg-Mn-Li-amfibolem, gran\u00E1tem, plagioklasem, klinopyroxenem a ortopyroxenem, kter\u00E9 obsahuj\u00ED bohat\u00E9 klinopyroxen-plagioklasov\u00E9 a ortopyroxen-plagioklasov\u00E9 symplektity po omphacitu (a\u017E cca 75 obj. %). Symplektitov\u00E9 okraje gran\u00E1tov\u00FDch zrn (pseudomorf\u00F3zy po gran\u00E1tu) jsou spole\u010Dn\u00FDm rysem obou typ\u016F hornin a reprezentuj\u00ED zm\u011Bny eklogitu v podm\u00EDnk\u00E1ch amfibolit-granulitov\u00E9 facie." . . . . "Retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit od \u010Cejkova u Nov\u00E9ho Rychnova (Moldanubikum, \u010Cesk\u00E1 republika)"@cs . "22" . "P\u0159edm\u011Btem v\u00FDzkumu byly dva typy retrogr\u00E1dn\u011B metamorfovan\u00E9ho eklogitu z \u010Cejkova. Prvn\u00EDm typem je pyroxenick\u00FD amfibolit s pseudomorf\u00F3zami po gran\u00E1tu (Ca-amfibol, klinopyroxen, plagioklas, ortopyroxen) bez viditeln\u00E9 struktury p\u016Fvodn\u00EDho eklogitu. Druh\u00FDm typem je retrogr\u00E1dn\u011B metamorfovan\u00FD eklogit s Ca a Fe-Mg-Mn-Li-amfibolem, gran\u00E1tem, plagioklasem, klinopyroxenem a ortopyroxenem, kter\u00E9 obsahuj\u00ED bohat\u00E9 klinopyroxen-plagioklasov\u00E9 a ortopyroxen-plagioklasov\u00E9 symplektity po omphacitu (a\u017E cca 75 obj. %). Symplektitov\u00E9 okraje gran\u00E1tov\u00FDch zrn (pseudomorf\u00F3zy po gran\u00E1tu) jsou spole\u010Dn\u00FDm rysem obou typ\u016F hornin a reprezentuj\u00ED zm\u011Bny eklogitu v podm\u00EDnk\u00E1ch amfibolit-granulitov\u00E9 facie."@cs .