"5"^^ . "I" . "Znalost p\u016Fvodn\u00ED, p\u0159eddenuda\u010Dn\u00ED mocnosti nadlo\u017En\u00EDch sediment\u016F m\u00E1 v\u00FDznam pro \u0159e\u0161en\u00ED r\u016Fzn\u00FDch geologick\u00FDch i geotechnick\u00FDch probl\u00E9m\u016F. \u010Cl\u00E1nek shrnuje poznatky o vlivu p\u0159ekonsolidace na horizont\u00E1ln\u00ED nap\u011Bt\u00ED v j\u00EDlovit\u00E9m masivu, dostupn\u00E9 metody pro stanoven\u00ED p\u0159eddenuda\u010Dn\u00ED mocnosti, jejich pou\u017Eit\u00ED a jejich vhodnost z hlediska mechaniky zemin. Oblast\u00ED z\u00E1jmu je karpatsk\u00E1 p\u0159edhlube\u0148 v okol\u00ED m\u011Bsta Brna. Sedimentovaly zde miocenn\u00ED j\u00EDly, zn\u00E1m\u00E9 jako brn\u011Bnsk\u00E9 t\u00E9gly." . "Boh\u00E1\u010D, Jan" . "[294CDA81D189]" . . "CZ - \u010Cesk\u00E1 republika" . "11310" . "Znalost p\u016Fvodn\u00ED, p\u0159eddenuda\u010Dn\u00ED mocnosti nadlo\u017En\u00EDch sediment\u016F m\u00E1 v\u00FDznam pro \u0159e\u0161en\u00ED r\u016Fzn\u00FDch geologick\u00FDch i geotechnick\u00FDch probl\u00E9m\u016F. \u010Cl\u00E1nek shrnuje poznatky o vlivu p\u0159ekonsolidace na horizont\u00E1ln\u00ED nap\u011Bt\u00ED v j\u00EDlovit\u00E9m masivu, dostupn\u00E9 metody pro stanoven\u00ED p\u0159eddenuda\u010Dn\u00ED mocnosti, jejich pou\u017Eit\u00ED a jejich vhodnost z hlediska mechaniky zemin. Oblast\u00ED z\u00E1jmu je karpatsk\u00E1 p\u0159edhlube\u0148 v okol\u00ED m\u011Bsta Brna. Sedimentovaly zde miocenn\u00ED j\u00EDly, zn\u00E1m\u00E9 jako brn\u011Bnsk\u00E9 t\u00E9gly."@cs . "2"^^ . . "1211-913X" . . . . "RIV/00216208:11310/12:10134407" . "2"^^ . "P\u0159eddenuda\u010Dn\u00ED mocnost a p\u0159ekonsolidace brn\u011Bnsk\u00E9ho t\u00E9glu" . "Overburden thickness and overconsolidation of Brno Tegel"@en . . "P\u0159eddenuda\u010Dn\u00ED mocnost a p\u0159ekonsolidace brn\u011Bnsk\u00E9ho t\u00E9glu" . . "160991" . . "P\u0159eddenuda\u010Dn\u00ED mocnost a p\u0159ekonsolidace brn\u011Bnsk\u00E9ho t\u00E9glu"@cs . "neuveden" . . . . "Brno Tegel; overconsolidation; Overburden thickness"@en . "Knowledge of the original overburden thikness overlying sediments is important for solving various geological and geotechnical problems. This article summarizes findings on the influence of overconsolidation on the horizontal stress in clayey mass, the methods available for determining of the overburden thikness, their use and their suitability in terms of soil mechanics. The area of \u200B\u200Binterest is the Carpathian foredeep near the city of Brno. Sedimentation here Miocene clays, known as the Brno Tegel."@en . . "Overburden thickness and overconsolidation of Brno Tegel"@en . "Geotechnika" . "RIV/00216208:11310/12:10134407!RIV14-MSM-11310___" . . . . . "1-2" . "Pavlov\u00E1, Martina" . "P\u0159eddenuda\u010Dn\u00ED mocnost a p\u0159ekonsolidace brn\u011Bnsk\u00E9ho t\u00E9glu"@cs .