This HTML5 document contains 56 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%2F00216208%3A11310%2F12%3A10128650%21RIV13-GA0-11310___/
n6http://localhost/temp/predkladatel/
n8http://linked.opendata.cz/resource/domain/vavai/projekt/
n4http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n21http://linked.opendata.cz/resource/domain/vavai/subjekt/
n20http://linked.opendata.cz/ontology/domain/vavai/
n15http://linked.opendata.cz/resource/domain/vavai/zamer/
shttp://schema.org/
skoshttp://www.w3.org/2004/02/skos/core#
rdfshttp://www.w3.org/2000/01/rdf-schema#
n3http://linked.opendata.cz/ontology/domain/vavai/riv/
n19http://bibframe.org/vocab/
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n7http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n10http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n16http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n11http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n18http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n14http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n5http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F12%3A10128650%21RIV13-GA0-11310___
rdf:type
skos:Concept n20:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.1016/j.jsg.2011.12.011
dcterms:description
The similar to 354-336 Ma Central Bohemian Plutonic Complex is a Variscan magmatic arc that developed in the central Bohemian Massif in response to subduction of the Saxothuringian lithosphere beneath the Tepla-Barrandian microplate. Magmatic to solid state fabrics in the most voluminous portion of this arc (the similar to 346 Ma Blatna pluton) record two superposed orogenic events: dextral transpression associated with arc-parallel stretching and arc-perpendicular shortening, and normal shearing associated with exhumation of the high-grade core of the orogen (Moldanubian unit). This kinematic switch is an important landmark in the evolution of this segment of the Variscan belt for it marks the cessation of subduction-related compressive forces in the upper crust giving way to gravity-driven normal movements of the Tepla-Barrandian hanging wall block relative to the high-grade Moldanubian footwall. We use thermal modeling to demonstrate that the emplacement of huge volumes of arc magmas and their slow cooling produced a thermally softened domain in the upper crust and that the magmatic arc granitoids may have played a major role in initiating the orogenic collapse in the Bohemian Massif through lubrication and reactivation of a pre-existing lithospheric boundary and decreasing the overall strength of the rigid orogenic lid. The similar to 354-336 Ma Central Bohemian Plutonic Complex is a Variscan magmatic arc that developed in the central Bohemian Massif in response to subduction of the Saxothuringian lithosphere beneath the Tepla-Barrandian microplate. Magmatic to solid state fabrics in the most voluminous portion of this arc (the similar to 346 Ma Blatna pluton) record two superposed orogenic events: dextral transpression associated with arc-parallel stretching and arc-perpendicular shortening, and normal shearing associated with exhumation of the high-grade core of the orogen (Moldanubian unit). This kinematic switch is an important landmark in the evolution of this segment of the Variscan belt for it marks the cessation of subduction-related compressive forces in the upper crust giving way to gravity-driven normal movements of the Tepla-Barrandian hanging wall block relative to the high-grade Moldanubian footwall. We use thermal modeling to demonstrate that the emplacement of huge volumes of arc magmas and their slow cooling produced a thermally softened domain in the upper crust and that the magmatic arc granitoids may have played a major role in initiating the orogenic collapse in the Bohemian Massif through lubrication and reactivation of a pre-existing lithospheric boundary and decreasing the overall strength of the rigid orogenic lid.
dcterms:title
Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif
skos:prefLabel
Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif
skos:notation
RIV/00216208:11310/12:10128650!RIV13-GA0-11310___
n20:predkladatel
n21:orjk%3A11310
n3:aktivita
n11:Z n11:P n11:I
n3:aktivity
I, P(GA205/09/0630), P(GAP210/11/1168), Z(MSM0021620855), Z(MSM6840770003)
n3:cisloPeriodika
3
n3:dodaniDat
n5:2013
n3:domaciTvurceVysledku
n4:1848941 n4:8387699 n4:2387689
n3:druhVysledku
n14:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
147735
n3:idVysledku
RIV/00216208:11310/12:10128650
n3:jazykVysledku
n16:eng
n3:klicovaSlova
Variscan orogeny; Tepla-Barrandian unit; Gravitational collapse; Granite; Exhumation; Bohemian Massif
n3:klicoveSlovo
n7:Gravitational%20collapse n7:Bohemian%20Massif n7:Granite n7:Variscan%20orogeny n7:Tepla-Barrandian%20unit n7:Exhumation
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[7F71F7B0BCD7]
n3:nazevZdroje
Journal of Structural Geology
n3:obor
n18:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
6
n3:projekt
n8:GAP210%2F11%2F1168 n8:GA205%2F09%2F0630
n3:rokUplatneniVysledku
n5:2012
n3:svazekPeriodika
36
n3:tvurceVysledku
Chlupácová, Marta Verner, Kryštof Žák, Jiří Halodová, Patricie Kabele, Petr Holub, František
n3:wos
000301630600004
n3:zamer
n15:MSM0021620855 n15:MSM6840770003
s:issn
0191-8141
s:numberOfPages
16
n19:doi
10.1016/j.jsg.2011.12.011
n6:organizacniJednotka
11310