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The Moura Phylonitic Complex: An Accretionary Complex related with obduction in...
Araújo, António Alexandre; Fonseca, Paulo; Munhá, José; Moita, Patrícia; Pedro, Jorge; Ribeiro, AntónioAbstract The structure of the southernmost domain of the Ossa Morena Zone in Portugal (south sector of the Iberian Autochthonous Terrane) is strongly controlled by earlier deformation events. The first two deformation events correspond to tangential strain regimes, marked by sub-horizontal milonitic foliations. These events seem to be directly related with the obduction/subduction process during the Variscan o...
Data: 2005
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Origem: Repositório Científico da Universidade de Évora
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