[HTML][HTML] The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

JRM Catalan, K Schulmann, JF Ghienne - Earth-Science Reviews, 2021 - Elsevier
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 …

[HTML][HTML] An Andean type Palaeozoic convergence in the Bohemian massif

K Schulmann, J Konopásek… - Comptes …, 2009 - comptes-rendus.academie-sciences …
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 …

Magma-mixing in the genesis of Hercynian calc-alkaline granitoids: an integrated petrographic and geochemical study of the Sázava intrusion, Central Bohemian …

V Janoušek, CJR Braithwaite, DR Bowes, A Gerdes - Lithos, 2004 - Elsevier
The Devonian–early Carboniferous (354.1±3.5 Ma: conventional zircon U–Pb age) Sázava
intrusion (biotite-amphibole quartz diorite, tonalite and granodiorite) of the Central …

A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons

J Žák, K Verner, V Janoušek, FV Holub… - Geological Society …, 2014 - lyellcollection.org
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 …

Post-Variscan (end Carboniferous-Early Permian) basin evolution in western and central Europe

T McCann, C Pascal, MJ Timmerman… - Geological Society …, 2006 - lyellcollection.org
The Variscan orogeny, resulting from the collision of Laurussia with Gondwana to form the
supercontinent of Pangaea, was followed by a period of crustal instability and re …

Origin and physical-chemical control of topaz crystallization in felsic igneous rocks: Contrasted effect of temperature on its OH–F substitution

M Soufi - Earth-Science Reviews, 2021 - Elsevier
In highly evolved F-rich felsic igneous rocks, topaz Al 2 SiO 4 (F, OH) 2 forms in different
genetic stages: orthomagmatic, pegmatitic, transitional magmatic-hydrothermal, and …

Correlation of allochthonous terranes and major tectonostratigraphic domains between NW Iberia and the Bohemian Massif, European Variscan belt

JR Martínez Catalán, S Collett, K Schulmann… - International Journal of …, 2020 - Springer
Abstract The NW Iberian Allochthon and the Teplá-Barrandian and Moldanubian zones
represent the internal parts of the Variscan belt in their respective domains. A correlation …

Heat sources and trigger mechanisms of exhumation of HP granulites in Variscan orogenic root

O Lexa, K Schulmann, V Janoušek… - Journal of …, 2011 - Wiley Online Library
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 …

Structural characteristics of epicentral areas in Central Europe: study case Cheb Basin (Czech Republic)

P Bankwitz, G Schneider, H Kämpf, E Bankwitz - Journal of Geodynamics, 2003 - Elsevier
The earthquake distribution pattern of Central Europe differs systematically from the
neighbouring areas of NW and southern Europe regarding the fault plane kinematics. Within …

U–Pb zircon provenance of Moldanubian metasediments in the Bohemian Massif

J Košler, J Konopásek, J Sláma… - Journal of the Geological …, 2014 - lyellcollection.org
Detrital zircon U–Pb age data from the Moldanubian part of the Bohemian Massif obtained
by laser ablation inductively coupled plasma mass spectrometry show variations between …