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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. (en)
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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)
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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)
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skos:notation
| - RIV/00025798:_____/10:00000401!RIV11-MZP-00025798
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/00025798:_____/10:00000401
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Šumava Mountains, Bohemian Forest, Variscan orogen, Moldanubian Zone, tectonometamorphic processes (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Franěk, Jan
- Verner, Kryštof
- Pertoldová, Jaroslava
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http://linked.open...n/vavai/riv/zamer
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issn
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number of pages
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