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Tectonometamorphic evolution of the Rehamna massif (Morocco, Variscan belt)

2015
The Morocco Variscan belt is considered to be the south-western continuation of the European Carboniferous orogen on the NW Gondwana margin. The Rehamna Massif, a paleozoic massif located on the Meseta domain which is part of this belt, is affected by three main deformation events (D1, D2 and D3) of variable intensity and geometry, associated with a ...
Wernert, Pauline   +8 more
openaire   +1 more source

The variscan fold belt in the British isles

Journal of Structural Geology, 1983
openaire   +1 more source

The collapse of the Variscan belt: a Variscan lateral extrusion thin-skinned structure in NW Iberia

International Geology Review, 2021
Icaro Dias da Silva   +2 more
exaly  

The Eo-Variscan Domain in the Variscan Belt: New Data from the Sudetes, Southern Poland

Lithos
Mirosław Jastrzębski   +4 more
openaire   +1 more source

Early Metamorphisms and Deformations in the French Variscan Belt

2023
Michel Fauré   +2 more
exaly  

Structural and metamorphic evolution of Variscan basement rocks in the Alps and comparison with the other portions of the European Variscan belt

Évolution structurelle et métamorphique des roches du socle varisque des Alpes en comparaison avec autres domaines de la chaîne varisque européenne L’évolution tectonique de la chaine varisque méridionale est certainement moins comprise que celle de la chaine varisque de l’Europe centrale.
openaire   +1 more source

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