. "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na). - Geol. v\u00FDzk Mor.Slez. v r. 2003, 18-23. Brno."@cs . . "Otava, Ji\u0159\u00ED" . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na). - Geol. v\u00FDzk Mor.Slez. v r. 2003, 18-23. Brno." . . "Masarykova univerzita" . . . . "Geologick\u00E9 v\u00FDzkumy na Morav\u011B a ve Slezsku v roce 2003" . . . "Geological documentation of the railway cut west of B\u011Blot\u00EDn (Moravian gate)"@en . "80-210-3466-1" . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na). - Geol. v\u00FDzk Mor.Slez. v r. 2003, 18-23. Brno."@cs . "V z\u00E1padn\u00ED \u010D\u00E1sti cca 2 km defil\u00E9 v z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru B\u011Blot\u00EDn byly zasti\u017Eeny nezvr\u00E1sn\u011Bn\u00E9 sedimenty, m\u00EDsty s drobn\u00FDmi poklesov\u00FDmi dislokacemi. Ve st\u0159edn\u00ED a v\u00FDchodn\u00ED \u010D\u00E1sti defil\u00E9 jsou spodnobadensk\u00E9 rytmity posti\u017Eeny kompresn\u00ED deformac\u00ED nar\u016Fstaj\u00EDc" . "18-23" . "RIV/00025798:_____/04:00000072" . . "Carpathian foredeep, Quaternary, Lower Badenian, tectonics, provenance"@en . "V z\u00E1padn\u00ED \u010D\u00E1sti cca 2 km defil\u00E9 v z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru B\u011Blot\u00EDn byly zasti\u017Eeny nezvr\u00E1sn\u011Bn\u00E9 sedimenty, m\u00EDsty s drobn\u00FDmi poklesov\u00FDmi dislokacemi. Ve st\u0159edn\u00ED a v\u00FDchodn\u00ED \u010D\u00E1sti defil\u00E9 jsou spodnobadensk\u00E9 rytmity posti\u017Eeny kompresn\u00ED deformac\u00ED nar\u016Fstaj\u00EDc"@cs . "Brno" . "Brno" . "6"^^ . . . . "4"^^ . "[13137028B6C2]" . "Geological documentation of the railway cut west of B\u011Blot\u00EDn (Moravian gate)"@en . . "565479" . . . "4"^^ . . "Western part of the railway cut west of B\u011Blot\u00EDn outcrops non folded sediments with local normal faults. The central and eastern parts is characterized by compessionally deformed (folded) rhythmites of claystones and sandstones (Lower Badenian). The deforWestern part of the railway cut west of B\u011Blot\u00EDn outcrops non folded sediments with local normal faults. The central and eastern parts is characterized by compessionally deformed (folded) rhythmites of claystones and sandstones (Lower Badenian). The defor"@en . "RIV/00025798:_____/04:00000072!RIV/2005/MZP/N03005/N" . "2004-04-25+02:00"^^ . "Z(MZP:N03/98:00)" . . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na). - Geol. v\u00FDzk Mor.Slez. v r. 2003, 18-23. Brno." . .