This HTML5 document contains 49 embedded RDF statements represented using HTML+Microdata notation.

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

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
n17http://linked.opendata.cz/resource/domain/vavai/vysledek/RIV%2F00025798%3A_____%2F09%3A00000206%21RIV10-MZP-00025798/
n18http://linked.opendata.cz/resource/domain/vavai/projekt/
n14http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n13http://linked.opendata.cz/ontology/domain/vavai/
n11http://linked.opendata.cz/resource/domain/vavai/zamer/
shttp://schema.org/
skoshttp://www.w3.org/2004/02/skos/core#
n3http://linked.opendata.cz/ontology/domain/vavai/riv/
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n4http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n7http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n15http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n5http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n16http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n6http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n10http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F09%3A00000206%21RIV10-MZP-00025798
rdf:type
skos:Concept n13:Vysledek
dcterms:description
The paper describes deformation of the Tepla-Barrandian unit of the Bohemian Massif during the Variscan orogeny. The Late Devonian subduction followed by the Early Carboniferous continental collision of the Saxothuringian and overriding upper-crustal Tepla-Barrandian units led to the growth of a large magmatic arc (the similar to 354-337 Ma Central Bohemian Plutonic Complex) in the central part of the Bohemian Massif. Approaching the magmatic arc margin, the regional structural pattern changes and exhibits significant across- and along-strike variations interpreted as a result of strain partitioning, where the Saxothuringian/Tepla-Barrandian convergence interacted in different ways with the intruding magma pulses. The paper describes deformation of the Tepla-Barrandian unit of the Bohemian Massif during the Variscan orogeny. The Late Devonian subduction followed by the Early Carboniferous continental collision of the Saxothuringian and overriding upper-crustal Tepla-Barrandian units led to the growth of a large magmatic arc (the similar to 354-337 Ma Central Bohemian Plutonic Complex) in the central part of the Bohemian Massif. Approaching the magmatic arc margin, the regional structural pattern changes and exhibits significant across- and along-strike variations interpreted as a result of strain partitioning, where the Saxothuringian/Tepla-Barrandian convergence interacted in different ways with the intruding magma pulses.
dcterms:title
Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif
skos:prefLabel
Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif
skos:notation
RIV/00025798:_____/09:00000206!RIV10-MZP-00025798
n3:aktivita
n5:P n5:Z
n3:aktivity
P(GP205/07/P226), Z(MSM0021620855), Z(MZP0002579801)
n3:cisloPeriodika
1-4
n3:dodaniDat
n10:2010
n3:domaciTvurceVysledku
n14:2387689 n14:8387699
n3:druhVysledku
n6:J
n3:duvernostUdaju
n7:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
315344
n3:idVysledku
RIV/00025798:_____/09:00000206
n3:jazykVysledku
n15:eng
n3:klicovaSlova
Anisotropy of magnetic susceptibility (AMS), Bohemian Massif, Central Bohemian Plutonic Complex, Emplacement, Magmatic arc, Teplá–Barrandian unit
n3:klicoveSlovo
n4:Tepl%C3%A1%E2%80%93Barrandian%20unit n4:Bohemian%20Massif n4:Anisotropy%20of%20magnetic%20susceptibility%20%28AMS%29 n4:Magmatic%20arc n4:Emplacement n4:Central%20Bohemian%20Plutonic%20Complex
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[C0D26732676A]
n3:nazevZdroje
Tectonophysics
n3:obor
n16:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
6
n3:projekt
n18:GP205%2F07%2FP226
n3:rokUplatneniVysledku
n10:2009
n3:svazekPeriodika
469
n3:tvurceVysledku
Dragoun, František Kachlík, Václav Holub, František Verner, Kryštof Chlupáčová, Marta Žák, Jiří
n3:wos
000265990100009
n3:zamer
n11:MZP0002579801 n11:MSM0021620855
s:issn
0040-1951
s:numberOfPages
19