Abstract The European Variscan belt is a unique orogen that is covered by comprehensive
sets of seismic and potential field data from the Iberian Peninsula in the west to the Polish …

Mid-Devonian high-pressure (HP) and high-temperature (HT) metamorphism represents an
enigmatic early phase in the evolution of the Variscan Orogeny. Within the Bohemian Massif …

The geochronology of metasediments incorporated to orogenic wedges provides an
important key in understanding the early evolution of collisional systems. This study reveals …

Competing end‐member models for the late Paleozoic Variscan orogeny (ca. 360‐290 Ma)
alternatively suggest moderate 2–3 km elevations underlain by relatively thin crust (< 50 km) …

In this study, U–Pb ages and Hf isotopic composition of detrital zircons from the Precambrian
metasedimentary autochthon of the Brunovistulian Domain in the eastern Bohemian Massif …

Arcuate traces of large structures characterize many mountain chains. The Variscan Belt is
not an exception and traces one of the tightest oroclines on Earth, the Ibero-Armorican Arc …

Synchysite was identified in the Rožná uranium deposit in a quartz–carbonate–sulfide vein,
which is a part of the late (post-uranium and, post-Variscan) stage of the development of the …

Metasandstones from early Cambrian to early Carboniferous stratigraphic successions were
sampled in the Rehamna massif of the Western Meseta in Morocco. The early Cambrian …

The high-grade metamorphic complexes along the northern Moldanubian periphery of the
central Bohemian Massif provide an outstanding structural record of all episodes of the …

A small and isolated hydrothermal vein-type Sb deposit is hosted by a lamprophyre dike
which penetrated Neoproterozoic to early Cambrian volcanosedimentary successions near …