About: Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias

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About: Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Breccias with phosphorites constitute a distinct lithology in Lower Carboniferous of the Moravo-Silesian basin. This facies constitutes lens-like bodies sandwiched between preorogenic sediments and younger synorogenic turbidites (“Culm” facies). This facies represents a key lithology in our understanding of the transition from the passive margin to the foreland basin stage of the MSB. Detailed description of facies, allochem composition and biostratigraphy indicate that the breccias were deposited on toes of submarine slopes and contain significant proportion of reworked material. The onset of breccia sedimentation was diachronous within the interval from middle Tournaisian to early Viséan. The breccias are always underlain by Famennian carbonates suggesting there is always a distinct hiatus associated with their basal surface. The breccias are in places accompanied by neptunian dikes filled with upper Tournaisian detrital sediments. Breccias with phosphorites constitute a distinct lithology in Lower Carboniferous of the Moravo-Silesian basin. This facies constitutes lens-like bodies sandwiched between preorogenic sediments and younger synorogenic turbidites (“Culm” facies). This facies represents a key lithology in our understanding of the transition from the passive margin to the foreland basin stage of the MSB. Detailed description of facies, allochem composition and biostratigraphy indicate that the breccias were deposited on toes of submarine slopes and contain significant proportion of reworked material. The onset of breccia sedimentation was diachronous within the interval from middle Tournaisian to early Viséan. The breccias are always underlain by Famennian carbonates suggesting there is always a distinct hiatus associated with their basal surface. The breccias are in places accompanied by neptunian dikes filled with upper Tournaisian detrital sediments. (en)
Title	Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias (en)
skos:prefLabel	Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias Differential subsidence in the Variscan foreland of Moravia, biostratigraphy, facies and conodont reworking in Mississippian gravity-flow carbonate breccias (en)
skos:notation	RIV/00216224:14310/06:00017151!RIV10-MSM-14310___
http://linked.open...avai/riv/aktivita	Z
http://linked.open...avai/riv/aktivity	Z(MSM0021622412)
http://linked.open...vai/riv/dodaniDat	2010
http://linked.open...aciTvurceVysledku	Bábek, Ondřej Kalvoda, Jiří
http://linked.open.../riv/druhVysledku	D - Článek ve sborníku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Masarykova univerzita / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	471657
http://linked.open...ai/riv/idVysledku	RIV/00216224:14310/06:00017151
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	breccias; stratigraphy; sedimentology; synsedimentary tectonics; foreland basin (en)
http://linked.open.../riv/klicoveSlovo	foreland basin sedimentology stratigraphy breccias synsedimentary tectonics
http://linked.open...ontrolniKodProRIV	[F086CEBCC08C]
http://linked.open...v/mistoKonaniAkce	Koeln
http://linked.open...i/riv/mistoVydani	Koeln
http://linked.open...i/riv/nazevZdroje	Koelner Forum fuer Geologie und Palaeontologie
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	2 (xsd:int)
http://linked.open...cetTvurcuVysledku	2 (xsd:int)
http://linked.open...UplatneniVysledku	2006
http://linked.open...iv/tvurceVysledku	Bábek, Ondřej Kalvoda, Jiří
http://linked.open...vavai/riv/typAkce	WRD - Světová
http://linked.open.../riv/zahajeniAkce	2006-10-04 (xsd:date)
http://linked.open...n/vavai/riv/zamer	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)
number of pages	1 (xsd:int)
http://purl.org/ne...btex#hasPublisher	Institut fuer Geologie und Mineralogie der Universitaet zu Koeln
https://schema.org/isbn	3-934027-18-0
http://localhost/t...ganizacniJednotka	14310

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