"Ultramaphic rock was found at Varied unit of Moldanubicum near Loukovice (western Moravia). It composed predominately by chlorite and amphibole, locally rich in ferroan spinel and serpentinised magnesian olivine (Fo = 73\u201381 mol. %). Their current mineral assemblage corresponds to polyphase metamorphosed spinel peridotite in conditions of amphibolite facie. Older mineral assemblage Ol + Cpx + Opx + Sp indicates the temperature 786\u2013804\u00B0C for pressures near 10 kbar. Amphibole (magnesiohornblende) and chlorite (clinochlore) formed in the retrograde phase of metamorphism at temperatures of 714 \u00B1 34 \u00B0C at the expected pressure around 8 kbar or less."@en . "19" . . "V pestr\u00E9 jednotce moldanubika u Loukovic (z\u00E1padn\u00ED Morava) byla zji\u0161t\u011Bna metamorfovan\u00E1 ultramafick\u00E1 hornina, kterou by bylo mo\u017En\u00E9 petrograficky nejp\u0159esn\u011Bji klasifikovat jako chloritick\u00FD hornblendit se spinelem a oliv\u00EDnem. Jej\u00ED sou\u010Dasn\u00E1 miner\u00E1ln\u00ED asociace odpov\u00EDd\u00E1 polyf\u00E1zov\u00E9 metamorf\u00F3ze peridotitu v podm\u00EDnk\u00E1ch vy\u0161\u0161\u00ED amfibolitov\u00E9 facie. Star\u0161\u00ED miner\u00E1ln\u00ED asociace Ol + Cpx + Opx + Sp indikuje teploty 786\u2013804 \u00B0C (p\u0159i p\u0159edpokl\u00E1dan\u00E9m tlaku kolem 10 kbar). Amfibol a chlorit vznikaly v n\u00E1sleduj\u00EDc\u00ED f\u00E1zi metamorf\u00F3zy za teplot 714 \u00B1 34 \u00B0C p\u0159i p\u0159edpokl\u00E1dan\u00E9m tlaku kolem 8 kbar nebo ni\u017E\u0161\u00EDm. Zji\u0161t\u011Bn\u00E9 metamorfn\u00ED teploty t\u00E9to metamorf\u00F3zy jsou podobn\u00E9 jako vrcholn\u00E9 podm\u00EDnky vypo\u010Dten\u00E9 pro horniny pestr\u00E9 skupiny v rakousk\u00E9 \u010D\u00E1sti moldanubika a drosendorfsk\u00E9ho okna 650\u2013800 \u00B0C a 7\u20139 kbar (Petrakakis, 1986; B\u00FCttner a Kruhl, 1997; Petrakakis, 1997; Racek et al. 2006). Nejpravd\u011Bpodobn\u011Bji jde o polymetamorfovanou horninu p\u016Fvodem ze svrchn\u00EDho pl\u00E1\u0161t\u011B, tektonicky importovanou do st\u0159edn\u00ED k\u016Fry p\u0159i varisk\u00E9 orogenezi."@cs . . "Chloritick\u00FD hornblendit s oliv\u00EDnem a spinelem z Loukovic u Moravsk\u00FDch Bud\u011Bjovic (moldanubikum, z\u00E1padn\u00ED Morava)."@cs . "1"^^ . "RIV/00094862:_____/12:#0001386!RIV13-MK0-00094862" . "CZ - \u010Cesk\u00E1 republika" . . . "I" . "2"^^ . "127037" . . "Chloritick\u00FD hornblendit s oliv\u00EDnem a spinelem z Loukovic u Moravsk\u00FDch Bud\u011Bjovic (moldanubikum, z\u00E1padn\u00ED Morava)." . "Buri\u00E1nek, David" . "Olivine- and spinel-bearing chlorite hornblendite from Loukovice near Moravsk\u00E9 Bud\u011Bjovice (Moldanubicum, western Moravia)."@en . "[92F5431F5A5C]" . . "Houzar, Stanislav" . . . "spinel; olivine; chlorite hornblendite; P-T conditions; Varied Group; Moldanubicum"@en . "Geologick\u00E9 v\u00FDzkumy na Morav\u011B a ve Slezsku" . "Chloritick\u00FD hornblendit s oliv\u00EDnem a spinelem z Loukovic u Moravsk\u00FDch Bud\u011Bjovic (moldanubikum, z\u00E1padn\u00ED Morava)."@cs . . . "RIV/00094862:_____/12:#0001386" . . "Chloritick\u00FD hornblendit s oliv\u00EDnem a spinelem z Loukovic u Moravsk\u00FDch Bud\u011Bjovic (moldanubikum, z\u00E1padn\u00ED Morava)." . . . "1212-6209" . . "Olivine- and spinel-bearing chlorite hornblendite from Loukovice near Moravsk\u00E9 Bud\u011Bjovice (Moldanubicum, western Moravia)."@en . . "5"^^ . "V pestr\u00E9 jednotce moldanubika u Loukovic (z\u00E1padn\u00ED Morava) byla zji\u0161t\u011Bna metamorfovan\u00E1 ultramafick\u00E1 hornina, kterou by bylo mo\u017En\u00E9 petrograficky nejp\u0159esn\u011Bji klasifikovat jako chloritick\u00FD hornblendit se spinelem a oliv\u00EDnem. Jej\u00ED sou\u010Dasn\u00E1 miner\u00E1ln\u00ED asociace odpov\u00EDd\u00E1 polyf\u00E1zov\u00E9 metamorf\u00F3ze peridotitu v podm\u00EDnk\u00E1ch vy\u0161\u0161\u00ED amfibolitov\u00E9 facie. Star\u0161\u00ED miner\u00E1ln\u00ED asociace Ol + Cpx + Opx + Sp indikuje teploty 786\u2013804 \u00B0C (p\u0159i p\u0159edpokl\u00E1dan\u00E9m tlaku kolem 10 kbar). Amfibol a chlorit vznikaly v n\u00E1sleduj\u00EDc\u00ED f\u00E1zi metamorf\u00F3zy za teplot 714 \u00B1 34 \u00B0C p\u0159i p\u0159edpokl\u00E1dan\u00E9m tlaku kolem 8 kbar nebo ni\u017E\u0161\u00EDm. Zji\u0161t\u011Bn\u00E9 metamorfn\u00ED teploty t\u00E9to metamorf\u00F3zy jsou podobn\u00E9 jako vrcholn\u00E9 podm\u00EDnky vypo\u010Dten\u00E9 pro horniny pestr\u00E9 skupiny v rakousk\u00E9 \u010D\u00E1sti moldanubika a drosendorfsk\u00E9ho okna 650\u2013800 \u00B0C a 7\u20139 kbar (Petrakakis, 1986; B\u00FCttner a Kruhl, 1997; Petrakakis, 1997; Racek et al. 2006). Nejpravd\u011Bpodobn\u011Bji jde o polymetamorfovanou horninu p\u016Fvodem ze svrchn\u00EDho pl\u00E1\u0161t\u011B, tektonicky importovanou do st\u0159edn\u00ED k\u016Fry p\u0159i varisk\u00E9 orogenezi." . . . . "1-2" .