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Variscan ophiolite belts in the Ossa-Morena Zone (Southwest Iberia): Geological...
Ribeiro, A.; Munhá, J.; Fonseca, P. E.; Araújo, A.; Pedro, Jorge; Mateus, A.; Tassinari, C.; Machado, G.; Jesus, A.Abstract At SW Iberia, the boundary between Iberian and South-Portuguese Terranes is traced by a suture recording the closure of Rheic and related oceans through N-NE subduction. The western segment of the suture comprises imbrications of Iberian Terrane Relative Autochthon (Neoproterozoic - Lower Palaeozoic) and Allochthonous Complexes. The Iberian Terrane Relative Autochthon is topped by Lower-Middle Devonian...
Tectonostratigraphy of Middle and Upper Palaeozoic black shales from the Porto-...
Chaminé, H. I.; Pereira, L. C. Gama; Fonseca, P. E.; Moço, L. P.; Fernandes, J. P.; Rocha, F. T.; Flores, D.; Jesus, A. Pinto de; Gomes, C.Middle/late Devonian and early Carboniferous metasedimentary sequences in the northernmost region (Porto-Espinho-Tomar) of the Ossa-Morena Zone (Portuguese Iberian Variscan Massif) contain black shales of very low to low-grade metamorphism. These metasedimentary rocks form a discrete NNW-SSE structure within a major shear zone (Porto-Tomar-Ferreira do Alentejo) and remain subparallel to the observed regional ma...
Tectonostratigraphy of Middle and Upper Palaeozoic black shales from the Porto-...
Chaminé, H. I.; Gama Pereira, L. C.; Fonseca, P. E.; Fernandes, J. P.; Rocha, F. T.; Flores, D.; Pinto de Jesus, A.; Gomes, C.; Soares de Andrade, A. AAbstract Middle/late Devonian and early Carboniferous metasedimentary sequences in the northernmost region (Porto-Espinho-Tomar) of the Ossa-Morena Zone (Portuguese Iberian Variscan Massif) contain black shales of very low to low-grade metamorphism. These metasedimentary rocks form a discrete NNW-SSE structure within a major shear zone (Porto-Tomar-Ferreira do Alentejo) and remain subparallel to the observed re...
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