About: Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane     Goto   Sponge   NotDistinct   Permalink

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Description
  • Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika (cs)
  • 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 (en)
Title
  • Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane
  • Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane (en)
  • Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika (cs)
skos:prefLabel
  • Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane
  • Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane (en)
  • Tektonostratigrafický vývoj devonu a karbonu brunovistulického teránu, Česká republika (cs)
skos:notation
  • RIV/00216224:14310/06:00017189!RIV08-MSM-14310___
http://linked.open.../vavai/riv/strany
  • 53-54
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM0021622412)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 503212
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/06:00017189
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • stratigraphy; Brunovistulian terrane; Rhenohercynian zone; Variscan orogeny; tectonostratigraphy; Devonian; Carboniferous (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [614408C8F6EB]
http://linked.open...v/mistoKonaniAkce
  • Köln
http://linked.open...i/riv/mistoVydani
  • Köln
http://linked.open...i/riv/nazevZdroje
  • Carboniferous Conference Cologne. From Platform to Basin, Sept. 4-10 2006. Kölner Forum für Geologie und Paläontologie, 15.
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Bábek, Ondřej
  • Kalvoda, Jiří
  • Leichmann, Jaromír
  • Melichar, Rostislav
  • Špaček, Petr
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
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  • Institut für Geologie und Mineralogie der Universität zu Köln
https://schema.org/isbn
  • 3-934027-18-0
http://localhost/t...ganizacniJednotka
  • 14310
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