"0"^^ . "Morfostrukturn\u00ED a strukturn\u011B-geologick\u00E1 anal\u00FDza vz\u00E1jemn\u00E9ho ovlivn\u011Bn\u00ED varisk\u00E9ho a alpinsk\u00E9ho tektog\u00E9nu moravskoslezsk\u00E9 oblasti vych\u00E1zela jednak z klasick\u00E9 strukturn\u011B-tektonick\u00E9 a paleonap\u011B\u0165ov\u00E9 anal\u00FDzy jednak z anal\u00FDzy digit\u00E1ln\u00EDch model\u016F reli\u00E9fu a mapov\u00FDch"@cs . "Morphostructural relationships and mutual tectonic influence of the Variscan and Alpine orogeny in the Moravosilesian area of the Bohemian Massif"@en . . . . . "Moravsko-slezsk\u00E1 oblast reprezentuje ojedin\u011Bl\u00FD p\u0159\u00EDklad strukturn\u00ED interference dvou tektogen\u016F. D\u00EDky tomu se zde setk\u00E1v\u00E1me se superpozic\u00ED t\u0159\u00ED strukturn\u00EDch et\u00E1\u017E\u00ED: kadomsk\u00E9 (brunovistulikum), varisk\u00E9 (rhenohercynsk\u00E1 a subvarisk\u00E1 z\u00F3na) a alp\u00EDnsk\u00E9 (p\u0159\u00EDkrovy Vn\u011Bj\u0161\u00EDch Karpat a \u010Deln\u00ED p\u0159edhlube\u0148). Strukturn\u00ED pl\u00E1n a kinematika alpinsk\u00FDch n\u00E1sun\u016F byly ovliv\u0148ov\u00E1ny zd\u011Bd\u011Bn\u00FDmi epivarisk\u00FDmi strukturami jv. okraje \u010Cesk\u00E9ho masivu. Tentonick\u00E9 a gravita\u010Dn\u00ED zat\u011B\u017Eov\u00E1n\u00ED jv. svah\u016F \u010Cesk\u00E9ho masivu n\u00E1suny vn\u011Bkarpatsk\u00FDch p\u0159\u00EDkrov\u016F sou\u010Dasn\u011B v\u00FDznamn\u00FDm zp\u016Fsobem modifikovalo strukturn\u00ED pl\u00E1n epivarisk\u00E9ho fundamentu, v\u010Detn\u011B uhlonosn\u00E9 molasy hornoslezsk\u00E9 p\u00E1nve. Prost\u0159ednictv\u00EDm srovn\u00E1vac\u00EDho studia varisk\u00E9 a alp\u00EDnsk\u00E9 strukturn\u00ED et\u00E1\u017Ee chceme podrobn\u011Bji klasifikovat a kvantifikovat deforma\u010Dnprojevy jednotliv\u00FDch varisk\u00FDch a alp\u00EDnsk\u00FDch deforma\u010Dn\u00EDch f\u00E1z\u00ED. Tyto vztahy budou studov\u00E1ny s vyu\u017Eit\u00EDm komplexn\u00EDho zpracov\u00E1n\u00ED strukturn\u011B-geologick\u00FDch datab\u00E1z\u00ED v prost\u0159ed\u00ED GIS a po\u010D\u00EDta\u010Dov\u00E9 grafiky (prostorov\u00E1 3D vizualizace strukturn\u00EDch ploch, DTM a" . . . "Morfostrukturn\u00ED vztahy a vz\u00E1jemn\u00E9 tektonick\u00E9 ovlivn\u011Bn\u00ED varisk\u00E9ho a alp\u00EDnsk\u00E9ho orog\u00E9nu - moravskoslezsk\u00E1 oblast \u010Cesk\u00E9ho masivu" . "1"^^ . "Neuvedeno."@en . . "0"^^ . . "The Moravosilesian area represents a unique example of structural interference between two principal tectogens. Therefore, a superposition of three structure levels can be found here: Cadomian (Brunovistulicum), Variscan (Rhenohercynian and Sub-Variscan zone) and Alpine (nappes of Outer Carpathians and Alpine foredeep). Structural framework and kinematics of Alpine thrusts were influenced by inherited epi-Variscan structures on the southeast boundary of the Bohemian Massif. At the same time, tectonic angravitational loading of the southeast slopes of the Bohemian Massif by the thrusts of the Outer-Carpathian nappes modified the structural framework of the epi-Variscan fundament considerably, including the coal-bearing molasse of the Upper Silesian basin. By means of a comparative study of the Variscan and Alpine structural levels, we aim to classify and quantify deformational demonstrations of individual Variscan and Alpine deformational phases detailedly. These relationships will be studied using"@en . . "2008-05-19+02:00"^^ . . . . . "9"^^ . . "9"^^ . . "http://www.isvav.cz/projectDetail.do?rowId=GA205/00/1182"^^ . "GA205/00/1182" . . .