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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F06%3A00000439%21RIV08-MZP-00025798
rdf:type
skos:Concept n16:Vysledek
dcterms:description
V masívu Blanského lesa byla identifikována rozsáhlá reliktní doména granulitových staveb. Mylonitická stavba z podmínek granulitové facie je diskordantní k převažující stavbě vzniklé v amfibolitové facii v okolních retrográdních granulitech. Mikrostruktury indikují A large-scale relict domain of granulite facies deformation fabrics has been identified within the Blanský les granulite body. The granulite facies mylonitic fabric is discordant to the dominant amphibolite facies structures of the surrounding retrograde granulite. Microstructures indicate grain-size sensitive flow enhanced by the presence of silicate melts at deep crustal levels and a beginning of an exhumation process of low viscosity granulites through a vertical channel. The amphibolite facies fabrics developed at middle crustal levels and their microstructures indicate significant hardening of the retrograde granulite. Increase in the strength of the granulite allowed an active buckling or a rigid body rotation of the granulite sheet, which acted as a strong layer inside the weaker metasediments. A large-scale relict domain of granulite facies deformation fabrics has been identified within the Blanský les granulite body. The granulite facies mylonitic fabric is discordant to the dominant amphibolite facies structures of the surrounding retrograde granulite. Microstructures indicate grain-size sensitive flow enhanced by the presence of silicate melts at deep crustal levels and a beginning of an exhumation process of low viscosity granulites through a vertical channel. The amphibolite facies fabrics developed at middle crustal levels and their microstructures indicate significant hardening of the retrograde granulite. Increase in the strength of the granulite allowed an active buckling or a rigid body rotation of the granulite sheet, which acted as a strong layer inside the weaker metasediments.
dcterms:title
Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root:example of the Blanský les granulite, Bohemian Massif, Czech Republic Kinematický a reologický model exhumace vysokotlakých granulitů ve variském orogenním kořeni: příklad granulitů Blanského lesa, český masiv, Česká republika Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root:example of the Blanský les granulite, Bohemian Massif, Czech Republic
skos:prefLabel
Kinematický a reologický model exhumace vysokotlakých granulitů ve variském orogenním kořeni: příklad granulitů Blanského lesa, český masiv, Česká republika Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root:example of the Blanský les granulite, Bohemian Massif, Czech Republic Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root:example of the Blanský les granulite, Bohemian Massif, Czech Republic
skos:notation
RIV/00025798:_____/06:00000439!RIV08-MZP-00025798
n4:strany
253-276
n4:aktivita
n13:Z n13:P
n4:aktivity
P(GA205/04/2065), Z(MZP0002579801)
n4:cisloPeriodika
3-4
n4:dodaniDat
n7:2008
n4:domaciTvurceVysledku
n5:8764840 n5:6827675
n4:druhVysledku
n15:J
n4:duvernostUdaju
n11:S
n4:entitaPredkladatele
n17:predkladatel
n4:idSjednocenehoVysledku
481643
n4:idVysledku
RIV/00025798:_____/06:00000439
n4:jazykVysledku
n14:eng
n4:klicovaSlova
Variscan granulites, exhumation, tectonics, structural geology
n4:klicoveSlovo
n10:Variscan%20granulites n10:structural%20geology n10:exhumation n10:tectonics
n4:kodStatuVydavatele
AT - Rakouská republika
n4:kontrolniKodProRIV
[37C60E1CBC1B]
n4:nazevZdroje
Mineralogy and Petrology
n4:obor
n12:DB
n4:pocetDomacichTvurcuVysledku
2
n4:pocetTvurcuVysledku
3
n4:projekt
n6:GA205%2F04%2F2065
n4:rokUplatneniVysledku
n7:2006
n4:svazekPeriodika
86
n4:tvurceVysledku
Franěk, Jan Schulmann, K. Lexa, Ondřej
n4:zamer
n8:MZP0002579801
s:issn
0930-0708
s:numberOfPages
24