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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10290414%21RIV15-MSM-11310___
rdf:type
skos:Concept n20:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.1080/11035897.2013.879735
dcterms: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.
dcterms: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)
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)
skos:notation
RIV/00216208:11310/14:10290414!RIV15-MSM-11310___
n3:aktivita
n13:I n13:P
n3:aktivity
I, P(GAP210/10/2351)
n3:cisloPeriodika
1
n3:dodaniDat
n4:2015
n3:domaciTvurceVysledku
n5:7292546 n5:2705176 n5:7243111 n5:3621413 n5:4056124
n3:druhVysledku
n14:J
n3:duvernostUdaju
n6:S
n3:entitaPredkladatele
n19:predkladatel
n3:idSjednocenehoVysledku
18487
n3:idVysledku
RIV/00216208:11310/14:10290414
n3:jazykVysledku
n16:eng
n3:klicovaSlova
basalt geochemistry; palaeolatitude; Prague Basin; Suchomasty Volcanic Centre; Silurian; Gorstian
n3:klicoveSlovo
n8:Prague%20Basin n8:Silurian n8:basalt%20geochemistry n8:palaeolatitude n8:Suchomasty%20Volcanic%20Centre n8:Gorstian
n3:kodStatuVydavatele
SE - Švédské království
n3:kontrolniKodProRIV
[D04309C3DF94]
n3:nazevZdroje
GFF
n3:obor
n18:DB
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
10
n3:projekt
n17:GAP210%2F10%2F2351
n3:rokUplatneniVysledku
n4:2014
n3:svazekPeriodika
136
n3:tvurceVysledku
Tasáryová, Zuzana Janoušek, Vojtěch Trubač, Jakub Štorch, Petr Pruner, Petr Schnabl, Petr Manda, Štěpán Čížková, Kristýna Rapprich, Vladislav Frýda, Jiří
n3:wos
000335945500054
s:issn
1103-5897
s:numberOfPages
4
n15:doi
10.1080/11035897.2013.879735
n9:organizacniJednotka
11310