The non-cylindrical character of the Variscan Belt is established via a description of its most
salient geological characteristics and correlations among the main and relatively minor …

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 …

The well-known Variscan basement areas of Europe contain relic terranes with a pre-
Variscan evolution testifying to their peri-Gondwanan origin (eg, relics of Neoproterozoic …

The Trans-European Suture Zone (TESZ) is a broad and complex zone of terrane accretion
separating ancient lithosphere of the Baltic Shield and East European Craton (EEC) from the …

The geological inventory of the Variscan Bohemian Massif can be summarized as a result of
Early Devonian subduction of the Saxothuringian ocean of unknown size underneath the …

Abstract The Late Paleozoic Variscan Orogen of Europe and North Africa comprises
reworked Neoproterozoic to Early Paleozoic crust of the northern Gondwanan shelf that …

The structure and evolution of the Polish part of the Variscan Orogenic Belt is reviewed,
based on published data and interpretations. The Sudetic segment of the Variscides …

Key lithological units of the high-grade eastern margin of the Bohemian Massif were dated
using the U-Pb and Pb-Pb methods on zircons in order to establish a chronological …

In order to portray the main differences and similarities between the Northeastern Variscan
segments (French Massif Central (FMC), Vosges, Black Forest and Bohemian Massif (BM)) …

The Brunovistulian terrane represents a microcontinent of enigmatic Proterozoic provenance
that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan …