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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10289156%21RIV15-MSM-11310___
rdf:type
skos:Concept n20:Vysledek
dcterms:description
This paper summarizes the current knowledge on the nature, kinematics and timing of movement along major tectonic boundaries in the Bohemian Massif and demonstrates how the Variscan plutonism and deformation evolved in space and time. Four main episodes are recognized: (1) Late Devonian-early Carboniferous subduction and continental underthrusting of the Saxothuringian Unit beneath the Teplá-Barrandian Unit resulted in the orogen-perpendicular shortening and growth of an inboard magmatic arc during c. 354-346 Ma; (2) the subduction-driven shortening was replaced by collapse of the Teplá-Barrandian upper crust, exhumation of the high-grade (Moldanubian) core of the orogen at c. 346-337 Ma and by dextral strike-slip along orogen-perpendicular NW-SE shear zones; (3) following closure of a Rhenohercynian Ocean basin, the Brunia microplate was underthrust beneath the eastern flank of the Saxothuringian/Teplá-Barrandian/Moldanubian 'assemblage'; this process commenced at c. 346 Ma in the NE and ceased at c. 335 Ma in the SW; and (4) late readjustments within the amalgamated Bohemian Massif included crustal exhumation and mainly S-type granite plutonism along the edge of the Brunia indentor at c. 330-327 Ma, and peripheral tectonothermal activity driven by strike-slip faulting and possibly mantle delamination around the consolidated Bohemian Massif's interior until late Carboniferous-earliest Permian times. This paper summarizes the current knowledge on the nature, kinematics and timing of movement along major tectonic boundaries in the Bohemian Massif and demonstrates how the Variscan plutonism and deformation evolved in space and time. Four main episodes are recognized: (1) Late Devonian-early Carboniferous subduction and continental underthrusting of the Saxothuringian Unit beneath the Teplá-Barrandian Unit resulted in the orogen-perpendicular shortening and growth of an inboard magmatic arc during c. 354-346 Ma; (2) the subduction-driven shortening was replaced by collapse of the Teplá-Barrandian upper crust, exhumation of the high-grade (Moldanubian) core of the orogen at c. 346-337 Ma and by dextral strike-slip along orogen-perpendicular NW-SE shear zones; (3) following closure of a Rhenohercynian Ocean basin, the Brunia microplate was underthrust beneath the eastern flank of the Saxothuringian/Teplá-Barrandian/Moldanubian 'assemblage'; this process commenced at c. 346 Ma in the NE and ceased at c. 335 Ma in the SW; and (4) late readjustments within the amalgamated Bohemian Massif included crustal exhumation and mainly S-type granite plutonism along the edge of the Brunia indentor at c. 330-327 Ma, and peripheral tectonothermal activity driven by strike-slip faulting and possibly mantle delamination around the consolidated Bohemian Massif's interior until late Carboniferous-earliest Permian times.
dcterms:title
A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons
skos:prefLabel
A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons
skos:notation
RIV/00216208:11310/14:10289156!RIV15-MSM-11310___
n3:aktivita
n16:Z n16:I n16:S n16:P
n3:aktivity
I, P(GA205/09/0630), P(GAP210/11/1168), S, Z(MSM0021620855)
n3:dodaniDat
n11:2015
n3:domaciTvurceVysledku
n5:7408285 n5:1848941 n5:8387699 n5:3621413 n5:4043790 n5:3319245 n5:7631219 n5:2387689 n5:7243111
n3:druhVysledku
n19:C
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
1041
n3:idVysledku
RIV/00216208:11310/14:10289156
n3:jazykVysledku
n4:eng
n3:klicovaSlova
Bohemina Massif; Teplá-Barrandian Unit; Saxothuringian Unit; Late Devonian-early Permian; Variscan plutonism and deformation; tectonic boundaries
n3:klicoveSlovo
n7:Tepl%C3%A1-Barrandian%20Unit n7:tectonic%20boundaries n7:Variscan%20plutonism%20and%20deformation n7:Bohemina%20Massif n7:Saxothuringian%20Unit n7:Late%20Devonian-early%20Permian
n3:kontrolniKodProRIV
[FA4493315240]
n3:mistoVydani
London
n3:nazevEdiceCisloSvazku
Special Publications, 405
n3:nazevZdroje
The Variscan Orogeny: Extent, Timescale and the Formation of the European Crust
n3:obor
n9:DB
n3:pocetDomacichTvurcuVysledku
9
n3:pocetStranKnihy
406
n3:pocetTvurcuVysledku
10
n3:projekt
n13:GA205%2F09%2F0630 n13:GAP210%2F11%2F1168
n3:rokUplatneniVysledku
n11:2014
n3:tvurceVysledku
Vondrovic, Lukáš Trubač, Jakub Janoušek, Vojtěch Žák, Jiří Holub, František Tomek, Filip Hajná, Jaroslava Kachlík, Václav Finger, Fritz Verner, Kryštof
n3:zamer
n12:MSM0021620855
s:numberOfPages
28
n21:hasPublisher
The Geological Society of London
n10:isbn
978-1-86239-658-6
n17:organizacniJednotka
11310