. "1212-6209" . "Moravo-Silesian Zone; Devonian; Carboniferous; conodont biostratigraphy; Variscan tectonics"@en . . . . "Geologick\u00E9 v\u00FDzkumy na Morav\u011B a ve Slezsku v roce 2005" . "RIV/00216224:14310/06:00015926" . "Biostratigrafick\u00E9 doklady pro tence \u0161upinovitou stavbu hranick\u00E9ho paleozoika, moravskoslezsk\u00E1 z\u00F3na"@cs . . . . "P(GA205/03/0967), Z(MZP0002579801)" . . "Biostratigrafick\u00E9 doklady pro tence \u0161upinovitou stavbu hranick\u00E9ho paleozoika, moravskoslezsk\u00E1 z\u00F3na" . . "CZ - \u010Cesk\u00E1 republika" . "2"^^ . "Na profilu \u010Cernot\u00EDn v hranick\u00E9m paleozoiku, moravskoslezsk\u00E1 z\u00F3na, st\u0159edn\u00ED Morava byla nalezena cca 2m mocn\u00E1 \u010Do\u010Dka brekci\u00ED s fosfority st\u00E1\u0159\u00ED st\u0159edn\u00ED tournai (sp. Si. crenulata a\u017E spodn\u00ED \u010D\u00E1sti Si. isosticha \u2013 sv. Si. crenulata) uvnit\u0159 stratigrafick\u00E9ho sledu pl\u00E1stevnat\u00FDch hn\u011Bvot\u00EDnsk\u00FDch v\u00E1penc\u016F st\u00E1\u0159\u00ED svrchn\u00ED famen (?Pa. marginifera \u2013 Pa. expansa). Vzhledem ke skute\u010Dnosti, \u017Ee mlad\u0161\u00ED karbon\u00E1ty jsou uzav\u0159eny ve star\u0161\u00EDch, nelze tuto situaci pova\u017Eovat za p\u0159irozenou stratigrafickou inkluzi, ale za p\u0159\u00EDklad biostratigrafick\u00E9 inverze. Tato inverze je vyvinuta v z\u00F3n\u011B karbon\u00E1tov\u00FDch mylonit\u016F s v\u00FDraznou foliac\u00ED o st\u0159edn\u00EDm \u00FAklonu 40st. k ZSZ. Biostratigrafickou inverzi a mylonitizaci proto lze pova\u017Eovat za spole\u010Dn\u00FD v\u00FDsledek tektonick\u00E9ho zvr\u00E1sn\u011Bn\u00ED a ze\u0161upinat\u011Bn\u00ED obou karbon\u00E1tov\u00FDch litotyp\u016F na jedn\u00E9 ze st\u0159i\u017En\u00FDch z\u00F3n publikovan\u00FDch d\u0159\u00EDv\u011Bj\u0161\u00EDmi autory, kter\u00E9 maj\u00ED v hranick\u00E9m paleozoiku stejnou orientaci." . "4"^^ . . . "B\u00E1bek, Ond\u0159ej" . . "Otava, Ji\u0159\u00ED" . "13" . "2"^^ . . "Na profilu \u010Cernot\u00EDn v hranick\u00E9m paleozoiku, moravskoslezsk\u00E1 z\u00F3na, st\u0159edn\u00ED Morava byla nalezena cca 2m mocn\u00E1 \u010Do\u010Dka brekci\u00ED s fosfority st\u00E1\u0159\u00ED st\u0159edn\u00ED tournai (sp. Si. crenulata a\u017E spodn\u00ED \u010D\u00E1sti Si. isosticha \u2013 sv. Si. crenulata) uvnit\u0159 stratigrafick\u00E9ho sledu pl\u00E1stevnat\u00FDch hn\u011Bvot\u00EDnsk\u00FDch v\u00E1penc\u016F st\u00E1\u0159\u00ED svrchn\u00ED famen (?Pa. marginifera \u2013 Pa. expansa). Vzhledem ke skute\u010Dnosti, \u017Ee mlad\u0161\u00ED karbon\u00E1ty jsou uzav\u0159eny ve star\u0161\u00EDch, nelze tuto situaci pova\u017Eovat za p\u0159irozenou stratigrafickou inkluzi, ale za p\u0159\u00EDklad biostratigrafick\u00E9 inverze. Tato inverze je vyvinuta v z\u00F3n\u011B karbon\u00E1tov\u00FDch mylonit\u016F s v\u00FDraznou foliac\u00ED o st\u0159edn\u00EDm \u00FAklonu 40st. k ZSZ. Biostratigrafickou inverzi a mylonitizaci proto lze pova\u017Eovat za spole\u010Dn\u00FD v\u00FDsledek tektonick\u00E9ho zvr\u00E1sn\u011Bn\u00ED a ze\u0161upinat\u011Bn\u00ED obou karbon\u00E1tov\u00FDch litotyp\u016F na jedn\u00E9 ze st\u0159i\u017En\u00FDch z\u00F3n publikovan\u00FDch d\u0159\u00EDv\u011Bj\u0161\u00EDmi autory, kter\u00E9 maj\u00ED v hranick\u00E9m paleozoiku stejnou orientaci."@cs . "RIV/00216224:14310/06:00015926!RIV10-GA0-14310___" . . . . "467128" . "-" . . "Biostratigraphic evidence for thin-skinned structure of the Hranice Palaeozoic, Moravo-Silesian Zone"@en . . "The first conodont-supported outcrop evidence of biostratigraphic inversion in the Hranice Palaeozoic, NE Moravo-Silesian Zone, is presented in this paper. About 2m thick lense of Middle Tournaisian skeletal calcarenite and calcirudite with phosphorite fragments (L. Si. crenulata to Si. isosticha \u2013 U. Si. crenulata) is enclosed in Upper Famennian calcimylonites (?Pa. marginifera Zone to Pa. expansa Zone) at the \u010Cernot\u00EDn section. The lense is oriented parallel to deformation cleavage whose orientation is consistent with that of the shear zones described from other parts of the Hranice Palaeozoic by previous authors. The newly-described biostratigraphic inversion very well fits in the previously proposed models of thin-skinned structure of the Brunovistulicum and its sedimentary cover in the NE Moravo-Silesian Zone, derived from interpretation of borehole and seismic data."@en . "Biostratigraphic evidence for thin-skinned structure of the Hranice Palaeozoic, Moravo-Silesian Zone"@en . "Biostratigrafick\u00E9 doklady pro tence \u0161upinovitou stavbu hranick\u00E9ho paleozoika, moravskoslezsk\u00E1 z\u00F3na" . "Biostratigrafick\u00E9 doklady pro tence \u0161upinovitou stavbu hranick\u00E9ho paleozoika, moravskoslezsk\u00E1 z\u00F3na"@cs . "[795518F0B098]" . . "14310" . .