About: Gorstian palaeoposition and geotectonic setting of Suchomasty Volcanic Centre (Silurian, Prague Basin, Teplá-Barrandian Unit, Bohemian Massif)     Goto   Sponge   NotDistinct   Permalink

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Description
  • A multidisciplinary palaeomagnetic, whole-rock geochemical and volcanological study was carried out in Gorstian deposits of the Suchomasty Volcanic Centre in the western segment of the Prague Basin (Teplá-Barrandian Unit, Bohemian Massif). Phreato-Strombolian eruptions of alkali basalts, transitional between enriched mid-ocean rift basalt and ocean-island basalt, associated with effusions of lava flows within the lower-middle Scanicus chimaera graptolite Biozone at the Vinařice locality, yield a mean palaeomagnetic direction that allows for computation of a palaeolatitude of 24.4 degrees S. Present data support that the Prague Basin was a continental rift basin, situated on presumed Perunica microplate. The Perunica microplate drifted at southern subtropical palaeolatitudes of 24.4 degrees in Gorstian time and experienced either 170 degrees counter-clockwise or 190 degrees clockwise rotation during the Variscan Orogeny.
  • A multidisciplinary palaeomagnetic, whole-rock geochemical and volcanological study was carried out in Gorstian deposits of the Suchomasty Volcanic Centre in the western segment of the Prague Basin (Teplá-Barrandian Unit, Bohemian Massif). Phreato-Strombolian eruptions of alkali basalts, transitional between enriched mid-ocean rift basalt and ocean-island basalt, associated with effusions of lava flows within the lower-middle Scanicus chimaera graptolite Biozone at the Vinařice locality, yield a mean palaeomagnetic direction that allows for computation of a palaeolatitude of 24.4 degrees S. Present data support that the Prague Basin was a continental rift basin, situated on presumed Perunica microplate. The Perunica microplate drifted at southern subtropical palaeolatitudes of 24.4 degrees in Gorstian time and experienced either 170 degrees counter-clockwise or 190 degrees clockwise rotation during the Variscan Orogeny. (en)
Title
  • Gorstian palaeoposition and geotectonic setting of Suchomasty Volcanic Centre (Silurian, Prague Basin, Teplá-Barrandian Unit, Bohemian Massif)
  • Gorstian palaeoposition and geotectonic setting of Suchomasty Volcanic Centre (Silurian, Prague Basin, Teplá-Barrandian Unit, Bohemian Massif) (en)
skos:prefLabel
  • Gorstian palaeoposition and geotectonic setting of Suchomasty Volcanic Centre (Silurian, Prague Basin, Teplá-Barrandian Unit, Bohemian Massif)
  • Gorstian palaeoposition and geotectonic setting of Suchomasty Volcanic Centre (Silurian, Prague Basin, Teplá-Barrandian Unit, Bohemian Massif) (en)
skos:notation
  • RIV/00216208:11310/14:10290414!RIV15-MSM-11310___
http://linked.open...avai/riv/aktivita
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  • I, P(GAP210/10/2351)
http://linked.open...iv/cisloPeriodika
  • 1
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  • 18487
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  • RIV/00216208:11310/14:10290414
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  • basalt geochemistry; palaeolatitude; Prague Basin; Suchomasty Volcanic Centre; Silurian; Gorstian (en)
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  • SE - Švédské království
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  • [D04309C3DF94]
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  • 136
http://linked.open...iv/tvurceVysledku
  • Frýda, Jiří
  • Janoušek, Vojtěch
  • Manda, Štěpán
  • Pruner, Petr
  • Rapprich, Vladislav
  • Trubač, Jakub
  • Tasáryová, Zuzana
  • Štorch, Petr
  • Schnabl, Petr
  • Čížková, Kristýna
http://linked.open...ain/vavai/riv/wos
  • 000335945500054
issn
  • 1103-5897
number of pages
http://bibframe.org/vocab/doi
  • 10.1080/11035897.2013.879735
http://localhost/t...ganizacniJednotka
  • 11310
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