"Z(MZP:N03/98:00)" . . "Lower Badenian sand-clayey rhytmites are folded by asymetric folds of Xm order of northern vergency, after eroded at the top and overlain by gravels deposited probably in braided rivers.Lower Badenian sand-clayey rhytmites are folded by asymetric folds of Xm order of northern vergency, after eroded at the top and overlain by gravels deposited probably in braided rivers."@en . . . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na)" . . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na)"@cs . . "CZ - \u010Cesk\u00E1 republika" . "Petrov\u00E1, Pavla" . . . "GEOLOGICK\u00C9 V\u00DDZKUMY na Morav\u011B a ve Slezsku v roce 2003" . . . . "Geological documentation of the railway cut west of B\u011Blot\u00EDn (Moravian gate)"@en . "RIV/00025798:_____/04:00000076!RIV/2005/MZP/N03005/N" . "2003.00" . "Carpathian Foredeep, Quaternary, Lower Badenian, tectonics, provenance"@en . . . . . "[BC5BA81B833B]" . "18-23" . "RIV/00025798:_____/04:00000076" . "Geological documentation of the railway cut west of B\u011Blot\u00EDn (Moravian gate)"@en . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na)"@cs . . "4"^^ . "6"^^ . "Geologick\u00E1 dokumentace z\u00E1\u0159ezu \u017Eelezni\u010Dn\u00EDho koridoru z\u00E1padn\u011B B\u011Blot\u00EDna (Moravsk\u00E1 br\u00E1na)" . "Rytmicky ukl\u00E1dan\u00E9 p\u00EDsky a j\u00EDly spodn\u00EDho b\u00E1denu byly posti\u017Eeny vr\u00E1sn\u011Bn\u00EDm (asymetrick\u00E9 vr\u00E1sy Xm \u0159\u00E1du a severn\u00ED vergence), pot\u00E9 \u010D\u00E1ste\u010Dn\u011B erodovan\u00E9 a p\u0159ekryt\u00E9 obl\u00E1zky, kter\u00E9 byly deponovan\u00E9 pravd\u011Bpodobn\u011B v divok\u00FDch toc\u00EDch."@cs . "565478" . "4"^^ . "1212-6209" . . "11.00" . . "Rytmicky ukl\u00E1dan\u00E9 p\u00EDsky a j\u00EDly spodn\u00EDho b\u00E1denu byly posti\u017Eeny vr\u00E1sn\u011Bn\u00EDm (asymetrick\u00E9 vr\u00E1sy Xm \u0159\u00E1du a severn\u00ED vergence), pot\u00E9 \u010D\u00E1ste\u010Dn\u011B erodovan\u00E9 a p\u0159ekryt\u00E9 obl\u00E1zky, kter\u00E9 byly deponovan\u00E9 pravd\u011Bpodobn\u011B v divok\u00FDch toc\u00EDch." .