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1 Δεκ 2023 · The Bohemian Massif (Fig. 1, Fig. 2) exposes the most complete section across the Central European Variscides, from the Rheno-Hercynian (RH) belt with the Mid-German Crystalline High (MGCH) as its southern, active margin, the Saxo-Thuringian (ST) belt, the Teplá-Barrandian (TB) block (“median massif” and zone of structural parting in the ...
1 Ιαν 2023 · Periglacial environments, past and present, of the Central European Variscan ranges show some similarities to those in other rejuvenated Variscan ranges of Europe, especially in the Iberian Peninsula (e.g., Serra da Estrela in Portugal—see Vieira and Nieuwendam, 2020) and the French Massif Central. They too host impressive periglacial ...
The Bohemian Massif (Czech: Česká vysočina or Český masiv, German: Böhmische Masse or Böhmisches Massiv) is a geomorphological province in Central Europe. It is a large massif stretching over most of the Czech Republic, eastern Germany, southern Poland and northern Austria.
1 Νοε 2010 · The Variscan orogeny is the major Middle to Late Palaeozoic tectonometamorphic event in central Europe, and the Bohemian Massif is the largest exposure of rocks deformed during this orogeny. The Bohemian Massif consists of the Saxothuringian, Barrandian and Moldanubian units.
eastern part of the Variscan belt of central Europe. The key profile of this experiment (S01) was 630 km long and extended southwestward from the margin of the East European craton, across the Trans-European suture zone (TESZ) and Sudetes, and across the Bohemian Massif that contains the active Eger (Ohrˇe) rift, which is an element of
Bohemian Massif. High pressure metamorphism. Tectonometamorphic evolution. The Variscan orogenic belt, of which the Bohemian Massif is a part, is typically recognized for its characteristic low pressure, high temperature metamorph.
A Rb–Sr whole-rock isochron of 331 ± 4 Ma from a principal magmatic type of the Central Bohemian pluton confirms the field evidence that the large NE-trending plutons of the Moldanubian zone were emplaced during a late stage of the deformation.
