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Tectonometamorphic evolution of the Rehamna massif (Morocco, Variscan belt)
2015The 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
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The variscan fold belt in the British isles
Journal of Structural Geology, 1983openaire +1 more source
The collapse of the Variscan belt: a Variscan lateral extrusion thin-skinned structure in NW Iberia
International Geology Review, 2021Icaro Dias da Silva +2 more
exaly
The Eo-Variscan Domain in the Variscan Belt: New Data from the Sudetes, Southern Poland
LithosMirosław Jastrzębski +4 more
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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.
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