. . "Neuvedeno."@en . "GA105/04/0884" . . . . "The Karvin\u00E1 sub-basin (part of the Upper Silesian Coal Basin) is traditionally described as the area with simple tectonic architecture (so call tafrogenic style) and absolutely dominant normal faults tectonics. Only rarely, in the western part of Karvin\u00E1sub-basin, there was known thrust structures localized in the zone of the Central Thrust. In eastern basin area there were thrusts and genetically associated deformations with vertical amplitude, which does not exceed coal seam thickness. However, in thelast decade low angle thrusts with vertical uplift up-to first ten meters order were proved on the base of mine drilling, galleries digging and coal exploitation in deeper structure and stratigraphic levels. These thrusts substantially complicate exploitation of coal seams. The prediction and cross-section construction of down dip continuation above mentioned thrusts in-to lower seams defied generally known structure geology rules and experiences of mine geologists. The aim of the project is the"@en . . "2007-10-16+02:00"^^ . "1"^^ . . . "Structure analysis of Karvin\u00E1 subbbasin (upper Silesian coal basin - Czech Republic) in relation to the coal seams mineability from deeper structure levels"@en . . . "0"^^ . "4"^^ . . "4"^^ . "http://www.isvav.cz/projectDetail.do?rowId=GA105/04/0884"^^ . . "Tradi\u010Dn\u011B je karvinsk\u00E1 d\u00EDl\u010D\u00ED p\u00E1nev popisov\u00E1na jako oblast s jednoduchou tzv. tafrogenn\u00ED strukturn\u011B-tektonickou stavbou, v n\u00ED\u017E zcela dominuje jednoduch\u00E1 tektonika poklesov\u00E9ho charakteru. Jenom v\u00FDjime\u010Dn\u011B, v z. \u010D\u00E1sti, byly popisov\u00E1ny m\u00E9n\u011B v\u00FDznamn\u00E9 struktury p\u0159esmykov\u00E9ho charakteru v z\u00F3n\u011B tzv. centr\u00E1ln\u00EDho p\u0159esmyku. Ve v. \u010D\u00E1sti p\u00E1nve byly zn\u00E1my p\u0159esmyky s velikosti zdvihu nep\u0159esahuj\u00EDc\u00ED mocnost posti\u017Een\u00E9 sloje. B\u011Bhem posledn\u00EDho desetilet\u00ED byly d\u016Fln\u00EDmi vrty, d\u016Fln\u00EDmi d\u00EDly a p\u0159i postupu porubn\u00EDch front v souvislosti s exploatac\u00ED ve st\u00E1le v\u011Bt\u0161\u00EDch hloubk\u00E1ch ov\u011B\u0159eny p\u0159esmykov\u00E9 struktury, u nich\u017E se v\u00FD\u0161ka zdvihu pohybovala v mocnostech sloj\u00ED, ale i struktury s v\u00FD\u0161kou zdvihu v \u0159\u00E1dech prvn\u00EDch des\u00EDtek metr\u016F, kter\u00E9 v\u00FDznamn\u011B komplikuj\u00ED vyt\u011B\u017Eitelnost uheln\u00FDch z\u00E1sob. Jejich predikce do ni\u017E\u0161\u00EDch slojov\u00FDch \u00FArovn\u00ED se p\u0159itom vymyk\u00E1 b\u011B\u017En\u00FDm z\u00E1sad\u00E1m konstrukce prostorov\u00E9ho pr\u016Fb\u011Bhu dislokac\u00ED. C\u00EDlem projektu proto je komplexn\u00ED anal\u00FDza strukturn\u011B-tektonick\u00FDch pom\u011Br\u016F karvinsk\u00E9 d\u00EDl\u010D\u00ED p\u00E1nve s d\u016Frazem na v\u00FDvoj tektoniky v" . "0"^^ . "Anal\u00FDza strukturn\u011B-tektonick\u00FDch pom\u011Br\u016F karvinsk\u00E9 d\u00EDl\u010D\u00ED p\u00E1nve (hornoslezsk\u00E1 p\u00E1nev) ve vztahu k vyt\u011B\u017Eitelnosti sloj\u00ED s postupem t\u011B\u017Eby do v\u011Bt\u0161\u00EDch hloubek" . . . . "Karvinsk\u00E1 d\u00EDl\u010D\u00ED p\u00E1nev popisov\u00E1na jako oblast s jednoduchou tzv. tafrogenn\u00ED strukturn\u011B-tektonickou stavbou, v n\u00ED\u017E zcela dominuje jednoduch\u00E1 tektonika poklesov\u00E9ho charakteru. Jenom v\u00FDjime\u010Dn\u011B, v z. \u010D\u00E1sti, byly popisov\u00E1ny m\u00E9n\u011B v\u00FDznamn\u00E9 struktury p\u0159esmykov\u00E9ho"@cs . . . . "The Karvin\u00E1 sub-basin (part of the Upper Silesian Coal Basin) is traditionally described as the area with simple tectonic architecture (so call tafrogenic style) and absolutely dominant normal faults tectonics. Only rarely, in the western part of Karvin\u00E1"@en . . .