"Anal\u00FDza synkinematick\u00E9 mineralizace na Drahansk\u00E9 vrchovin\u011B" . "Anal\u00FDza synkinematick\u00E9 mineralizace na Drahansk\u00E9 vrchovin\u011B"@cs . "Analysis of synkinematic mineralization in the Drahany upland"@en . . . "1"^^ . . "Anal\u00FDza synkinematick\u00E9 mineralizace na Drahansk\u00E9 vrchovin\u011B" . "1"^^ . . "Richtrov\u00E1, Dagmar" . "RIV/00216224:14310/13:00068319!RIV14-MSM-14310___" . . "Moravian Paleozoicum; Drahany Upland; Lower Carboniferous; tectonic fault; paleostress; hydrothermal mineralization; Alpine paragenesis; zeolites; laumontite"@en . . . . . . "Kulmsk\u00E9 slepence v kamenolomu v Lul\u010Di jsou protknuty tektonick\u00FDmi zlomy, na jejich\u017E ploch\u00E1ch je vyvinuta k\u0159emen-kalcit-laumontitov\u00E1 mineralizace. P\u0159evl\u00E1daj\u00EDc\u00ED siln\u011B kompresn\u00ED re\u017Eim v oblasti zap\u0159\u00ED\u010Dinil vznik zlom\u016F a nadlo\u017En\u00ED kra se za\u010Dala sunout sm\u011Brem na V. Tepl\u00E1 fluida se nabohatila v\u00E1pn\u00EDkem z rozkl\u00E1daj\u00EDc\u00EDch se plagioklas\u016F v okoln\u00EDch valounech granulit\u016F. Ochlazov\u00E1n\u00EDm t\u011Bchto roztok\u016F se na ploch\u00E1ch trhlin vyvinuly miner\u00E1ly alpsk\u00E9 parageneze. Mineralizace vznikala synkinematicky za n\u00EDzk\u00FDch tlak\u016F a teplot v rozmez\u00ED 145\u2013180 stup\u0148\u00FA Celsia v hloubce 3\u20134,8 km pod povrchem."@cs . . . . . "P(EE2.4.31.0019), S" . "Kulmsk\u00E9 slepence v kamenolomu v Lul\u010Di jsou protknuty tektonick\u00FDmi zlomy, na jejich\u017E ploch\u00E1ch je vyvinuta k\u0159emen-kalcit-laumontitov\u00E1 mineralizace. P\u0159evl\u00E1daj\u00EDc\u00ED siln\u011B kompresn\u00ED re\u017Eim v oblasti zap\u0159\u00ED\u010Dinil vznik zlom\u016F a nadlo\u017En\u00ED kra se za\u010Dala sunout sm\u011Brem na V. Tepl\u00E1 fluida se nabohatila v\u00E1pn\u00EDkem z rozkl\u00E1daj\u00EDc\u00EDch se plagioklas\u016F v okoln\u00EDch valounech granulit\u016F. Ochlazov\u00E1n\u00EDm t\u011Bchto roztok\u016F se na ploch\u00E1ch trhlin vyvinuly miner\u00E1ly alpsk\u00E9 parageneze. Mineralizace vznikala synkinematicky za n\u00EDzk\u00FDch tlak\u016F a teplot v rozmez\u00ED 145\u2013180 stup\u0148\u00FA Celsia v hloubce 3\u20134,8 km pod povrchem." . . "14310" . "Culm conglomerates in the quarry in Lule\u010D are intersected by tectonic fault. Quartz-calcite-laumontite mineralization is formed on their planes. The dominant compressed mode caused formation of fault and overlying landscape began to shift in the direction of East. Warm fluids were enriched by calcium from decomposing plagioclase from the surrounding boulders granulites. Alpine paragenesis minerals were developed by cooling of these solutions on the planes of the faults. This mineralization was formed synkinematically at low pressures and temperatures in the range 145\u2013180 degrees of Celsius at the depths between 3\u20134,8 km below the surface."@en . . "Analysis of synkinematic mineralization in the Drahany upland"@en . "RIV/00216224:14310/13:00068319" . . "[C266F812D290]" . . . . "61076" . "Anal\u00FDza synkinematick\u00E9 mineralizace na Drahansk\u00E9 vrchovin\u011B"@cs . . . .