. "2" . . "1"^^ . "RIV/00025798:_____/11:00000465!RIV12-MZP-00025798" . . . . "Metamorphic evolution OF Upper Moravian Nappe in the South part of the Svratka Dome"@en . "1"^^ . . "96" . . . . . "14"^^ . "Buri\u00E1nek, David" . "Metamorfn\u00ED v\u00FDvoj svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00EDm k\u0159\u00EDdle svrateck\u00E9 klenby"@cs . . "Acta Musei Moraviae, Scientae geologicae" . . "Metamorfn\u00ED v\u00FDvoj hornin svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00ED \u010D\u00E1sti svrateck\u00E9 klenby moravika byl roz\u010Dlen\u011Bn na t\u0159i hlavn\u00ED metamorfn\u00ED f\u00E1ze. Nejstar\u0161\u00ED f\u00E1zi p\u0159edstavuje syntektonick\u00E1 metamorf\u00F3za M1 (520-620 \u00B0C pro tlak 9 kbar). Druhou metamorfn\u00ED etapu (M2) indikuje syntektonick\u00E1 miner\u00E1ln\u00ED asociace v matrix svor\u016F(~ 600\u2013670 \u00B0C a ~ 8\u201310 kbar). V mramorech vznikla miner\u00E1ln\u00ED asociace Tr + Cal \u00B1 Dol. Tato miner\u00E1ln\u00ED asociace musela za dan\u00FDch P-T podm\u00EDnek vznikat v rovnov\u00E1ze s fluidy o slo\u017Een\u00ED XCO2 = 0,1\u20130,6. Vrcholn\u00E1 miner\u00E1ln\u00ED asociace v\u00E1penatosilik\u00E1tov\u00FDch hornin (Qtz + Pl + Di \u00B1 Cal), kter\u00E9 jsou s mramory asociov\u00E1ny, naopak indikuje koexistenci s fluidy o slo\u017Een\u00ED XCO2 <0,2. Nejmlad\u0161\u00ED metamorfn\u00ED f\u00E1ze (M3) se ve svorech projevuje vznikem st\u0159i\u017En\u00FDch p\u00E1s\u016F v nich\u017E nach\u00E1z\u00EDme rekrystalovan\u00FD muskovit a chlorit. V mramorech se tato metamorf\u00F3za projevuje vznikem mastku. Tyto sekund\u00E1rn\u00ED miner\u00E1ly umo\u017E\u0148uj\u00ED odhadnou horn\u00ED teplotn\u00ED limit metamorf\u00F3zy M3 na 450 \u00B0C pro tlak 2 kbar." . "[4E2BE2CB5842]" . "CZ - \u010Cesk\u00E1 republika" . . . "The southern part of the Svratka Dome is built two crystalline napes overlying Cadomian basement and its Devonian cover. The Upper Moravian Nappe consists of orthogneisses, muscovite to muscovite-biotite micas chists and gneisses with layers or boudins of amphibolites, quartzites, calc-silicate rocks and marbles. Study of mineral chemistry in these rocks, resulted in distinguishing three metamorphic stages of the P-T evolution. First syntectonic metamorphic assemblage M1 is preserved only as relicts in central parts of some garnet or amphibole porphyroblasts garnets and is considered to have occurred at T 520\u2013620 \u00B0C and P ~ 9 kbar. The following metamorphic event (M2) indicates peak conditions of T = 600\u2013670 \u00B0C and P = 8\u201310 kbar. The mineral assemblages in marbles (Tr + Cal \u00B1 Dol) indicate XCO2 in fluid between 0.1 and 0.6, while calc-silicate rocks (Qtz + Pl + Di \u00B1 Cal) reflect XCO2 < 0.2. The temperature of a low-grade metamorphic event (M3) was established at ~450 \u00B0C for pressure 2 kbar."@en . "RIV/00025798:_____/11:00000465" . . "211727" . "I, Z(MZP0002579801)" . "Metamorfn\u00ED v\u00FDvoj svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00EDm k\u0159\u00EDdle svrateck\u00E9 klenby" . . "Metamorfn\u00ED v\u00FDvoj hornin svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00ED \u010D\u00E1sti svrateck\u00E9 klenby moravika byl roz\u010Dlen\u011Bn na t\u0159i hlavn\u00ED metamorfn\u00ED f\u00E1ze. Nejstar\u0161\u00ED f\u00E1zi p\u0159edstavuje syntektonick\u00E1 metamorf\u00F3za M1 (520-620 \u00B0C pro tlak 9 kbar). Druhou metamorfn\u00ED etapu (M2) indikuje syntektonick\u00E1 miner\u00E1ln\u00ED asociace v matrix svor\u016F(~ 600\u2013670 \u00B0C a ~ 8\u201310 kbar). V mramorech vznikla miner\u00E1ln\u00ED asociace Tr + Cal \u00B1 Dol. Tato miner\u00E1ln\u00ED asociace musela za dan\u00FDch P-T podm\u00EDnek vznikat v rovnov\u00E1ze s fluidy o slo\u017Een\u00ED XCO2 = 0,1\u20130,6. Vrcholn\u00E1 miner\u00E1ln\u00ED asociace v\u00E1penatosilik\u00E1tov\u00FDch hornin (Qtz + Pl + Di \u00B1 Cal), kter\u00E9 jsou s mramory asociov\u00E1ny, naopak indikuje koexistenci s fluidy o slo\u017Een\u00ED XCO2 <0,2. Nejmlad\u0161\u00ED metamorfn\u00ED f\u00E1ze (M3) se ve svorech projevuje vznikem st\u0159i\u017En\u00FDch p\u00E1s\u016F v nich\u017E nach\u00E1z\u00EDme rekrystalovan\u00FD muskovit a chlorit. V mramorech se tato metamorf\u00F3za projevuje vznikem mastku. Tyto sekund\u00E1rn\u00ED miner\u00E1ly umo\u017E\u0148uj\u00ED odhadnou horn\u00ED teplotn\u00ED limit metamorf\u00F3zy M3 na 450 \u00B0C pro tlak 2 kbar."@cs . "marbles, calc-silicate rocks, amphibolites, mica schist, P-T conditions, Upper Moravian Nappe"@en . . . . . "Metamorfn\u00ED v\u00FDvoj svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00EDm k\u0159\u00EDdle svrateck\u00E9 klenby" . "Metamorfn\u00ED v\u00FDvoj svrchn\u00EDho p\u0159\u00EDkrovu moravika v ji\u017En\u00EDm k\u0159\u00EDdle svrateck\u00E9 klenby"@cs . "1211-8796" . "Metamorphic evolution OF Upper Moravian Nappe in the South part of the Svratka Dome"@en .