"Pertoldov\u00E1, Jaroslava" . "Lithological composition and geodynamic evolution of the south-eastern part of the \u0160umava Mts.(Moldanubian Zone, Bohemian Massif)" . . . "Lithological composition and geodynamic evolution of the south-eastern part of the \u0160umava Mts.(Moldanubian Zone, Bohemian Massif)"@en . "\u0160umava Mountains, Bohemian Forest, Variscan orogen, Moldanubian Zone, tectonometamorphic processes"@en . . . "Lithological composition and geodynamic evolution of the south-eastern part of the \u0160umava Mts.(Moldanubian Zone, Bohemian Massif)"@en . . . "Verner, Kry\u0161tof" . "Silva Gabreta" . "Lithological composition and geodynamic evolution of the south-eastern part of the \u0160umava Mts.(Moldanubian Zone, Bohemian Massif)" . "CZ - \u010Cesk\u00E1 republika" . "268694" . "[1266100F0BC7]" . "1211-7420" . "Fran\u011Bk, Jan" . . "The SE part of the \u0160umava 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 \u00B0C and pressures corresponding to depths of ~20\u201330 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\u2013335 Ma associated with ascent of ultrapotassic, Mg-K-rich (durbachite) intrusions, immediately followed by an LP\u2013HT 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\u2013325 Ma, followed by emplacement of peraluminous S-type Eisgarn posttectonic granites contemporaneous with the activity of the Pfahl Shear Zone at ~325 Ma."@en . . . "I, Z(MZP0002579801)" . . "The SE part of the \u0160umava 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 \u00B0C and pressures corresponding to depths of ~20\u201330 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\u2013335 Ma associated with ascent of ultrapotassic, Mg-K-rich (durbachite) intrusions, immediately followed by an LP\u2013HT 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\u2013325 Ma, followed by emplacement of peraluminous S-type Eisgarn posttectonic granites contemporaneous with the activity of the Pfahl Shear Zone at ~325 Ma." . "RIV/00025798:_____/10:00000401!RIV11-MZP-00025798" . "22"^^ . . . . . "3"^^ . "RIV/00025798:_____/10:00000401" . "3"^^ . . . . . . "3" . . "16" .