"An extensive Devonian carbonate bioaccumulation in eastern part of the Czech Republic is simply described and visualized. The basic data about area, average thickness, biofacies, architecture and composition of sediments are involved. The Middle Eifelian - Late Frasnian assemblages of platforms and reef-related limestone structures with their Neoproterozoic crystalline basement blocks were originally environed by deep seas and ocean, SE periphery of the Brunnia microcontinent. These platforms drifted toward the NW, from palaeolatitude about 18* to 13* S. Implications of the facies section (picture): Retrogradational onlapping on the slopes prevailed up to the end-Middle Frasnian times when maximum flooding surfaces alternately occurred. After, the prograding onlapping architecture with aggraded clinoforms developed, and subsequently, the forced regression of prograding clinoforms (onshore erosion, later also ravinment on carbonate ramps) formed the uppermost parts." . . "Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic" . . "187;189" . . "Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic"@en . . . "419391" . "RIV/67985831:_____/07:00093598!RIV08-AV0-67985831" . "Mus\u00E9um national d'histoire naturelle" . "reef biofacies; carbonate platform; sequence stratigraphy; Devonian; Moravian Karst"@en . "[9255517FE936]" . . . "Paris" . . "Facies from palaeozoic reefs and bioaccumulations" . "Eifelsko a\u017E frasnsk\u00E9 amfiporov\u00E9 v\u00E1pence, biostromy a biohermy, Moravsk\u00FD kras, \u010Cesk\u00E1 republika"@cs . "RIV/67985831:_____/07:00093598" . . . . "Hladil, Jind\u0159ich" . "M\u00E9moires du Mus\u00E9um national d'histoire naturell..." . . . "Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic" . . . . "Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic"@en . . . "Eifelsko a\u017E frasnsk\u00E9 amfiporov\u00E9 v\u00E1pence, biostromy a biohermy, Moravsk\u00FD kras, \u010Cesk\u00E1 republika"@cs . "Jednodu\u0161e pops\u00E1ny a graficky nast\u00EDn\u011Bny jsou rozs\u00E1hl\u00E9 devonsk\u00E9 karbon\u00E1tov\u00E9 bioakumulace z v. \u010D\u00E1sti \u010CR. Obsa\u017Eena jsou zde z\u00E1kladn\u00ED data o rozloze, mocnosti, slo\u017Een\u00ED a architektu\u0159e sediment\u016F. V\u00E1pencov\u00E9 \u00FAtesy a plo\u0161iny v\u010D. nosn\u00FDch blok\u016F neoproterozoick\u00E9ho krystalinika byly oblopeny hlubok\u00FDmi mo\u0159i a oce\u00E1nem p\u0159i jv. periferii mikrokontinentu brunnia. Plo\u0161iny driftovaly na SZ, ca. od 18 po 13 j. rovnob\u011B\u017Eku. Implikace faci\u00E1ln\u00EDho profilu. Postupn\u00E9 trasgresivn\u00ED p\u0159ekr\u00FDv\u00E1n\u00ED svahu p\u0159eva\u017Eovalo a\u017E do pozdn\u00EDch dob st\u0159edn\u00EDho frasnu kdy se st\u0159\u00EDdav\u011B vyv\u00EDjely nejv\u011Bt\u0161\u00ED mo\u0159sk\u00E9 z\u00E1plavov\u00E9 povrchy. Potom u\u017E okraje plo\u0161in progradovaly ven do mo\u0159e, prvn\u011B s agradovan\u00FDmi klinoformami a n\u00E1sledn\u011B s nucenou regres\u00ED a klinoformami posouvaj\u00EDc\u00EDmi se ven (spolu s eroz\u00ED b\u0159eh\u016F a tvorbou zbr\u00E1zd\u011Bn\u00FDch ramp), kter\u00E1 formovala vrch komplexu."@cs . "978-2-85653-593-6" . "1"^^ . . "1"^^ . "An extensive Devonian carbonate bioaccumulation in eastern part of the Czech Republic is simply described and visualized. The basic data about area, average thickness, biofacies, architecture and composition of sediments are involved. The Middle Eifelian - Late Frasnian assemblages of platforms and reef-related limestone structures with their Neoproterozoic crystalline basement blocks were originally environed by deep seas and ocean, SE periphery of the Brunnia microcontinent. These platforms drifted toward the NW, from palaeolatitude about 18* to 13* S. Implications of the facies section (picture): Retrogradational onlapping on the slopes prevailed up to the end-Middle Frasnian times when maximum flooding surfaces alternately occurred. After, the prograding onlapping architecture with aggraded clinoforms developed, and subsequently, the forced regression of prograding clinoforms (onshore erosion, later also ravinment on carbonate ramps) formed the uppermost parts."@en . . "P(IAA300130702), P(IAAX00130702), Z(AV0Z30130516)" . "3"^^ .