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 …

It is still a matter of debate what were the protoliths of the felsic HP granulites; arguments for
major HP melting period giving rise to these rocks and the alternative view of the granulites …

This paper presents a model for the genesis of migmatites and granites during orogenic
evolution based on the analysis of several Phanerozoic crustal segments and a review of …

This paper summarizes the current knowledge on the nature, kinematics and timing of
movement along major tectonic boundaries in the Bohemian Massif and demonstrates how …

Convergent plate boundaries are characterized by the development of crustal orogenic
wedges and orogenic plateaus but also by gravitational collapse of previously thickened …

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)) …

A large database of structural, geochronological and petrological data combined with a
Bouguer anomaly map is used to develop a two‐stage exhumation model of deep‐seated …

The Bavarian Phase (330–315 Ma) represents a fully independent stage of the Variscan
orogeny in the Bohemian Massif. It is defined by a significant reheating (LP–HT regional …

The structure of the Moldanubian domain is marked by felsic granulites of Ordovician
protolith age forming the cores of domes that are separated from mid‐crustal Neoproterozoic …

The classical concept of collisional orogens suggests that mountain belts form as a crustal
wedge between the downgoing and overriding plates. However, this orogenic style is not …