About: Lithological composition and geodynamic evolution of the south-eastern part of the Šumava Mts.(Moldanubian Zone, Bohemian Massif)     Goto   Sponge   NotDistinct   Permalink

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  • 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. (en)
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) (en)
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) (en)
skos:notation
  • RIV/00025798:_____/10:00000401!RIV11-MZP-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 268694
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/10:00000401
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Šumava Mountains, Bohemian Forest, Variscan orogen, Moldanubian Zone, tectonometamorphic processes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [1266100F0BC7]
http://linked.open...i/riv/nazevZdroje
  • Silva Gabreta
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 16
http://linked.open...iv/tvurceVysledku
  • Franěk, Jan
  • Verner, Kryštof
  • Pertoldová, Jaroslava
http://linked.open...n/vavai/riv/zamer
issn
  • 1211-7420
number of pages
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