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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F10%3A00000401%21RIV11-MZP-00025798
rdf:type
n15:Vysledek skos:Concept
dcterms:description
The SE part of the Šumava Mts. (i.e. Bohemian Forest) offers a unique opportunity to observe the interaction of deformations in high-grade metamorphic rocks with development of magmatic fabrics in contemporaneous intrusions in a fluid state, proceeding at temperatures above ~700 °C and pressures corresponding to depths of ~20–30 km. The geological history is related to the Variscan orogenic processes, which, in this region of the so-called Moldanubian Zone, can be divided into (1) Exhumation of the deep-seated rocks at ~343–335 Ma associated with ascent of ultrapotassic, Mg-K-rich (durbachite) intrusions, immediately followed by an LP–HT metamorphic event and anatexis; (2) Intrusion of large volumes of high-K I-type Weinsberg granitoids into the partially exhumed Moldanubian rock syntectonic with distinct younger deformations at ~340–325 Ma, followed by emplacement of peraluminous S-type Eisgarn posttectonic granites contemporaneous with the activity of the Pfahl Shear Zone at ~325 Ma. The SE part of the Šumava Mts. (i.e. Bohemian Forest) offers a unique opportunity to observe the interaction of deformations in high-grade metamorphic rocks with development of magmatic fabrics in contemporaneous intrusions in a fluid state, proceeding at temperatures above ~700 °C and pressures corresponding to depths of ~20–30 km. The geological history is related to the Variscan orogenic processes, which, in this region of the so-called Moldanubian Zone, can be divided into (1) Exhumation of the deep-seated rocks at ~343–335 Ma associated with ascent of ultrapotassic, Mg-K-rich (durbachite) intrusions, immediately followed by an LP–HT metamorphic event and anatexis; (2) Intrusion of large volumes of high-K I-type Weinsberg granitoids into the partially exhumed Moldanubian rock syntectonic with distinct younger deformations at ~340–325 Ma, followed by emplacement of peraluminous S-type Eisgarn posttectonic granites contemporaneous with the activity of the Pfahl Shear Zone at ~325 Ma.
dcterms:title
Lithological composition and geodynamic evolution of the south-eastern part of the Šumava Mts.(Moldanubian Zone, Bohemian Massif) Lithological composition and geodynamic evolution of the south-eastern part of the Šumava Mts.(Moldanubian Zone, Bohemian Massif)
skos:prefLabel
Lithological composition and geodynamic evolution of the south-eastern part of the Šumava Mts.(Moldanubian Zone, Bohemian Massif) Lithological composition and geodynamic evolution of the south-eastern part of the Šumava Mts.(Moldanubian Zone, Bohemian Massif)
skos:notation
RIV/00025798:_____/10:00000401!RIV11-MZP-00025798
n3:aktivita
n9:Z n9:I
n3:aktivity
I, Z(MZP0002579801)
n3:cisloPeriodika
3
n3:dodaniDat
n5:2011
n3:domaciTvurceVysledku
n6:2431858 n6:2387689 n6:6827675
n3:druhVysledku
n16:J
n3:duvernostUdaju
n17:S
n3:entitaPredkladatele
n11:predkladatel
n3:idSjednocenehoVysledku
268694
n3:idVysledku
RIV/00025798:_____/10:00000401
n3:jazykVysledku
n12:eng
n3:klicovaSlova
Šumava Mountains, Bohemian Forest, Variscan orogen, Moldanubian Zone, tectonometamorphic processes
n3:klicoveSlovo
n8:tectonometamorphic%20processes n8:%C5%A0umava%20Mountains n8:Moldanubian%20Zone n8:Variscan%20orogen n8:Bohemian%20Forest
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[1266100F0BC7]
n3:nazevZdroje
Silva Gabreta
n3:obor
n14:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n5:2010
n3:svazekPeriodika
16
n3:tvurceVysledku
Pertoldová, Jaroslava Verner, Kryštof Franěk, Jan
n3:zamer
n13:MZP0002579801
s:issn
1211-7420
s:numberOfPages
22