"Metamorfn\u00ED v\u00FDvoj svor\u016F a jejich tektonick\u00E1 pozice v poli\u010Dsk\u00E9m krystaliniku" . "RIV/00025798:_____/09:00000122" . . . "[0B32261AB463]" . . . "CZ - \u010Cesk\u00E1 republika" . "1"^^ . "94" . "Metamorphic evolution of mica-schists and their tectonic position in the Poli\u010Dka Crystalline Complex"@en . . "Z(MZP0002579801)" . "Metamorphic evolution of mica-schists and their tectonic position in the Poli\u010Dka Crystalline Complex"@en . "Metamorfn\u00ED v\u00FDvoj svor\u016F a jejich tektonick\u00E1 pozice v poli\u010Dsk\u00E9m krystaliniku"@cs . "1"^^ . . "metamorphism, mineralogy, mica-schist, Poli\u010Dka Crystalline Complex, Bohemian Massif"@en . . . "Metamorfn\u00ED v\u00FDvoj svor\u016F a jejich tektonick\u00E1 pozice v poli\u010Dsk\u00E9m krystaliniku" . "RIV/00025798:_____/09:00000122!RIV10-MZP-00025798" . "Acta Musei Moraviae, Scientae geologicae" . "325624" . . . "srpen" . "1211-8796" . "Metamorfn\u00ED v\u00FDvoj svor\u016F a jejich tektonick\u00E1 pozice v poli\u010Dsk\u00E9m krystaliniku"@cs . . . . . . . "Dvojsl\u00EDdn\u00E9 svory s miner\u00E1ln\u00ED asociac\u00ED obsahuj\u00EDc\u00ED Grt +- St +- Sil +- Ky nejsou sou\u010D\u00E1st\u00ED litologie poli\u010Dsk\u00E9ho krystalinika. Svou mineralogi\u00ED a stupn\u011Bm metamorf\u00F3zy maj\u00ED bl\u00EDzko k hornin\u00E1m okoln\u00EDch jednotek. Svory pod\u00E9l z\u00E1padn\u00ED hranice jsou podobn\u00E9 svor\u016Fm ze svrateck\u00E9ho krystalinika. Svory p\u0159i v\u00FDchodn\u00ED hranici vykazuj\u00ED \u0159adu podobnost\u00ED se svory z letovick\u00E9ho krystalinika. Do dne\u0161n\u00ED pozice se svory dostaly b\u011Bhem varisk\u00E9 orogeneze. V obou p\u0159\u00EDpadech je kontakt svor\u016F s rulami poli\u010Dsk\u00E9ho krystalinika modifikov\u00E1n tektonicky. P\u2013T podm\u00EDnky vm\u00EDst\u011Bn\u00ED svoru do dne\u0161n\u00ED tektonick\u00E9 pozice byl podobn\u00E9 na obou kontaktech a pohybovaly se kolem 640\u2013660 \u00B0C a 7\u20138 kbar. Mezi horninami poli\u010Dsk\u00E9ho a svrateck\u00E9ho krystalinika neexistoval v t\u00E9 dob\u011B \u017E\u00E1dn\u00FD v\u00FDrazn\u00FD kontrast v P\u2013T podm\u00EDnk\u00E1ch. Naproti tomu miner\u00E1ln\u00ED asociace horniny letovick\u00E9ho krystalinika vznikala za vy\u0161\u0161\u00EDch tlak\u016F a na kontaktu svor\u016F s rulami poli\u010Dsk\u00E9ho krystalinika pozorujeme retrogr\u00E1dn\u00ED metamorf\u00F3zu svor\u016F."@cs . . "Buri\u00E1nek, David" . "Dvojsl\u00EDdn\u00E9 svory s miner\u00E1ln\u00ED asociac\u00ED obsahuj\u00EDc\u00ED Grt +- St +- Sil +- Ky nejsou sou\u010D\u00E1st\u00ED litologie poli\u010Dsk\u00E9ho krystalinika. Svou mineralogi\u00ED a stupn\u011Bm metamorf\u00F3zy maj\u00ED bl\u00EDzko k hornin\u00E1m okoln\u00EDch jednotek. Svory pod\u00E9l z\u00E1padn\u00ED hranice jsou podobn\u00E9 svor\u016Fm ze svrateck\u00E9ho krystalinika. Svory p\u0159i v\u00FDchodn\u00ED hranici vykazuj\u00ED \u0159adu podobnost\u00ED se svory z letovick\u00E9ho krystalinika. Do dne\u0161n\u00ED pozice se svory dostaly b\u011Bhem varisk\u00E9 orogeneze. V obou p\u0159\u00EDpadech je kontakt svor\u016F s rulami poli\u010Dsk\u00E9ho krystalinika modifikov\u00E1n tektonicky. P\u2013T podm\u00EDnky vm\u00EDst\u011Bn\u00ED svoru do dne\u0161n\u00ED tektonick\u00E9 pozice byl podobn\u00E9 na obou kontaktech a pohybovaly se kolem 640\u2013660 \u00B0C a 7\u20138 kbar. Mezi horninami poli\u010Dsk\u00E9ho a svrateck\u00E9ho krystalinika neexistoval v t\u00E9 dob\u011B \u017E\u00E1dn\u00FD v\u00FDrazn\u00FD kontrast v P\u2013T podm\u00EDnk\u00E1ch. Naproti tomu miner\u00E1ln\u00ED asociace horniny letovick\u00E9ho krystalinika vznikala za vy\u0161\u0161\u00EDch tlak\u016F a na kontaktu svor\u016F s rulami poli\u010Dsk\u00E9ho krystalinika pozorujeme retrogr\u00E1dn\u00ED metamorf\u00F3zu svor\u016F." . "18"^^ . "Mica-schists are present only as small lenses or bodies within gneisses, which represent typical rocks of the Poli\u010Dka Crystalline Complex. Based on the geological position, two types of mica-schists were recognized: (i) Mica-schists with mineral assemblage Qtz + Ms + Bt + Grt +- Pl +- Sill are situated along the contact with the Svratka Crystalline Complex (W boundary Poli\u010Dka Crystalline Complex). These mica-schists yield PT conditions of 642 +- 124 \u00B0C and 8 +- 2 kbar. (ii) Mica-schists with mineral assemblage Qtz + Ms + Bt +- Pl +- St +- Grt +- Pl +- Ky form several N-S oriented stripes between villages Sta\u0161ov, Hamry and Jedlov\u00E1 on NE margin of the Poli\u010Dka Crystalline Complex. Mica-schists in this part of the Poli\u010Dka Crystalline Complex indicate peak P\u2013T conditions of ~650 \u00B0C and ~8 kbar and younger decrease of pressure to about 7 kbar and 660 \u00B0C, related to thrusting of the Letovice Crystalline Complex over the Poli\u010Dka Crystalline Complex."@en .