. "5"^^ . "Manifestations of late quaternary tectonics within the sudetic marginal fault zone"@en . "quaternary tectonics; active tectonics; morphotectonics; paleoseismology; natural hazards"@en . . "The goal of the project is study of manifestations of Late Quaternary tectonics in relief and geology within the zone of Sudetic Marginal Fault (SMF), where Late Pleistocene to Holocene movements were found out. Basing on geomorphological mapping, detailed field work in selected sites, and methods of paleoseismological research - particularly trenching, the youngest tectonic development will be determined. Also dynamism of the development will be evaluated. The obtained knowledge concerning paleoseismicity/paleotectonics can be of special importance for hazard assessment within the studied area. This topic have not been studied yet from this point of view within the area nor the effective methods of paleoseismology (trenching etc.) have been used in the Czech Republic. Moreover, the obtained data will be compared with the youngest geological evolution of the adjacent area and with results of research carried out in the Polish part of the SMF zone. In addition, the results will be"@en . "1145"^^ . . . "1145"^^ . "0"^^ . . . "C\u00EDlem projektu je hled\u00E1n\u00ED projev\u016F mladokvart\u00E9rn\u00ED tektoniky v\u00A0reli\u00E9fu a geologii v\u00A0\u010Desk\u00E9 \u010D\u00E1sti z\u00F3ny okrajov\u00E9ho sudetsk\u00E9ho zlomu (OSZ), kde byly dokumentov\u00E1ny svrchn\u011Bpleistocenn\u00ED a\u017E holocenn\u00ED pohyby, jako\u017E i sou\u010Dasn\u00E9 pohyby potvrzen\u00E9 monitoringem. Na z\u00E1klad\u011B geomorfologick\u00E9ho mapov\u00E1n\u00ED, detailn\u00EDch ter\u00E9nn\u00EDch prac\u00ED ve vybran\u00FDch lokalit\u00E1ch a metod paleoseismick\u00E9ho v\u00FDzkumu, zejm\u00E9na zemn\u00EDch r\u00FDh a jejich dokumentace v\u010Detn\u011B datace z\u00EDskan\u00E9ho vhodn\u00E9ho materi\u00E1lu, bude formulov\u00E1n nejmlad\u0161\u00ED tektonick\u00FD v\u00FDvoj a posouzena dynamika v\u00FDvoje modelov\u00FDch lokalit. Takto z\u00EDskan\u00E9 nov\u00E9 poznatky mohou m\u00EDt velk\u00FD v\u00FDznam pro zhodnocen\u00ED ohro\u017Een\u00ED zkouman\u00E9 oblasti tektonickou/seismickou aktivitou. Tato problematika z\u00A0tohoto pohledu nebyla v\u00A0dan\u00E9 oblasti je\u0161t\u011B \u0159e\u0161ena a ani velmi \u00FA\u010Dinn\u00E9 metody paleoseismick\u00E9ho ter\u00E9nn\u00EDho v\u00FDzkumu nebyly u n\u00E1s dosud pou\u017E\u00EDv\u00E1ny. Zji\u0161t\u011Bn\u00E9 poznatky budou d\u00E1le srovn\u00E1ny s nejmlad\u0161\u00EDm geologick\u00FDm v\u00FDvojem \u0161ir\u0161\u00EDho okol\u00ED a zasazeny do celkov\u00E9ho neotektonick\u00E9ho v\u00FDvoje reli\u00E9fu, kter\u00FD bude porovn\u00E1n s\u00A0v\u00FDsledky"@cs . . . . "2008-01-01+01:00"^^ . "Projevy mladokvart\u00E9rn\u00ED tektoniky v z\u00F3n\u011B okrajov\u00E9ho sudetsk\u00E9ho zlomu"@cs . . "2010-12-31+01:00"^^ . . "1"^^ . "0"^^ . "5"^^ .