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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F07%3A00093598%21RIV08-AV0-67985831
rdf:type
n17:Vysledek skos:Concept
dcterms:description
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. Jednoduše popsány a graficky nastíněny jsou rozsáhlé devonské karbonátové bioakumulace z v. části ČR. Obsažena jsou zde základní data o rozloze, mocnosti, složení a architektuře sedimentů. Vápencové útesy a plošiny vč. nosných bloků neoproterozoického krystalinika byly oblopeny hlubokými moři a oceánem při jv. periferii mikrokontinentu brunnia. Plošiny driftovaly na SZ, ca. od 18 po 13 j. rovnoběžku. Implikace faciálního profilu. Postupné trasgresivní překrývání svahu převažovalo až do pozdních dob středního frasnu kdy se střídavě vyvíjely největší mořské záplavové povrchy. Potom už okraje plošin progradovaly ven do moře, prvně s agradovanými klinoformami a následně s nucenou regresí a klinoformami posouvajícími se ven (spolu s erozí břehů a tvorbou zbrázděných ramp), která formovala vrch komplexu. 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.
dcterms:title
Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic Eifelsko až frasnské amfiporové vápence, biostromy a biohermy, Moravský kras, Česká republika
skos:prefLabel
Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic Eifelian-Frasnian Amphipora limestones, biostromes and bioherms, Moravian Karst, Czech Republic Eifelsko až frasnské amfiporové vápence, biostromy a biohermy, Moravský kras, Česká republika
skos:notation
RIV/67985831:_____/07:00093598!RIV08-AV0-67985831
n4:strany
187;189
n4:aktivita
n5:Z n5:P
n4:aktivity
P(IAA300130702), P(IAAX00130702), Z(AV0Z30130516)
n4:dodaniDat
n8:2008
n4:domaciTvurceVysledku
n13:8642702
n4:druhVysledku
n16:C
n4:duvernostUdaju
n9:S
n4:entitaPredkladatele
n14:predkladatel
n4:idSjednocenehoVysledku
419391
n4:idVysledku
RIV/67985831:_____/07:00093598
n4:jazykVysledku
n15:eng
n4:klicovaSlova
reef biofacies; carbonate platform; sequence stratigraphy; Devonian; Moravian Karst
n4:klicoveSlovo
n12:carbonate%20platform n12:Moravian%20Karst n12:reef%20biofacies n12:sequence%20stratigraphy n12:Devonian
n4:kontrolniKodProRIV
[9255517FE936]
n4:mistoVydani
Paris
n4:nazevEdiceCisloSvazku
Mémoires du Muséum national d'histoire naturell...
n4:nazevZdroje
Facies from palaeozoic reefs and bioaccumulations
n4:obor
n6:DB
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
1
n4:projekt
n7:IAAX00130702 n7:IAA300130702
n4:rokUplatneniVysledku
n8:2007
n4:tvurceVysledku
Hladil, Jindřich
n4:zamer
n19:AV0Z30130516
s:numberOfPages
3
n11:hasPublisher
Muséum national d'histoire naturelle
n18:isbn
978-2-85653-593-6