This HTML5 document contains 55 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
n8http://linked.opendata.cz/ontology/domain/vavai/riv/typAkce/
dctermshttp://purl.org/dc/terms/
n19http://localhost/temp/predkladatel/
n16http://purl.org/net/nknouf/ns/bibtex#
n15http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n12http://linked.opendata.cz/ontology/domain/vavai/
n14http://linked.opendata.cz/resource/domain/vavai/zamer/
n7https://schema.org/
shttp://schema.org/
skoshttp://www.w3.org/2004/02/skos/core#
n3http://linked.opendata.cz/ontology/domain/vavai/riv/
n13http://linked.opendata.cz/resource/domain/vavai/vysledek/RIV%2F00216224%3A14310%2F06%3A00017189%21RIV08-MSM-14310___/
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n5http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n18http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n20http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n11http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n9http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n6http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n17http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F06%3A00017189%21RIV08-MSM-14310___
rdf:type
n12:Vysledek skos:Concept
dcterms:description
The Brunovistulian terrane represents a microcontinent of an enigmatic Proterozoic provenance that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan orogeny, it represented the southern passive margin of Laurussia, in this respect resembling the Istanbul Zone to the east and the Avalonian terrane to the west. Nevertheless, the presence of a Silurian-Devonian back-arc basin cannot be excluded at the southermost margin of the terrane. The early Variscan phase was characterized the by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. The development of the Moravo-Silesian The Brunovistulian terrane represents a microcontinent of an enigmatic Proterozoic provenance that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan orogeny, it represented the southern passive margin of Laurussia, in this respect resembling the Istanbul Zone to the east and the Avalonian terrane to the west. Nevertheless, the presence of a Silurian-Devonian back-arc basin cannot be excluded at the southermost margin of the terrane. The early Variscan phase was characterized the by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. The development of the Moravo-Silesian Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika
dcterms:title
Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane
skos:prefLabel
Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane
skos:notation
RIV/00216224:14310/06:00017189!RIV08-MSM-14310___
n3:strany
53-54
n3:aktivita
n20:Z
n3:aktivity
Z(MSM0021622412)
n3:dodaniDat
n17:2008
n3:domaciTvurceVysledku
n15:1283987 n15:7162286 n15:6213405 n15:6504507 n15:3032744
n3:druhVysledku
n6:D
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
503212
n3:idVysledku
RIV/00216224:14310/06:00017189
n3:jazykVysledku
n11:eng
n3:klicovaSlova
stratigraphy; Brunovistulian terrane; Rhenohercynian zone; Variscan orogeny; tectonostratigraphy; Devonian; Carboniferous
n3:klicoveSlovo
n5:tectonostratigraphy n5:stratigraphy n5:Devonian n5:Rhenohercynian%20zone n5:Brunovistulian%20terrane n5:Variscan%20orogeny n5:Carboniferous
n3:kontrolniKodProRIV
[614408C8F6EB]
n3:mistoKonaniAkce
Köln
n3:mistoVydani
Köln
n3:nazevZdroje
Carboniferous Conference Cologne. From Platform to Basin, Sept. 4-10 2006. Kölner Forum für Geologie und Paläontologie, 15.
n3:obor
n9:DB
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n17:2006
n3:tvurceVysledku
Melichar, Rostislav Špaček, Petr Leichmann, Jaromír Kalvoda, Jiří Bábek, Ondřej
n3:typAkce
n8:WRD
n3:zahajeniAkce
2006-09-04+02:00
n3:zamer
n14:MSM0021622412
s:numberOfPages
2
n16:hasPublisher
Institut für Geologie und Mineralogie der Universität zu Köln
n7:isbn
3-934027-18-0
n19:organizacniJednotka
14310