Tectonic evolution of Variscan Iberia: gondwana–Laurussia collision revisited

RD Fernández, R Arenas, MF Pereira… - Earth-Science …, 2016 - Elsevier
An integrated interpretation of the late Paleozoic structural and geochronological record of
the Iberian Massif is presented and discussed under the perspective of a Gondwana …

[PDF][PDF] As regiões central e sul da Zona de Ossa-Morena

AA Araújo, JP Almeida, J Borrego, J Pedro, T Oliveira - 2006 - dspace.uevora.pt
1990). Mais recentemente foi introduzido o conceito de sector, que visa a melhor
compreensão dos vários depocentros, independentemente dos seus limites geográficos …

The Beja layered gabbroic sequence (Ossa-Morena Zone, Southern Portugal): geochronology and geodynamic implications

AP Jesus, J Munhá, A Mateus, C Tassinari… - Geodinamica …, 2007 - Taylor & Francis
The Beja Igneous Complex (BIC) is a major geological feature in SW Iberian Variscides,
consisting of three main units developed during different stages of the oblique collision …

[PDF][PDF] Tectonoestratigrafia da faixa de cisalhamento de Porto–Albergaria-a-Velha–Coimbra–Tomar, entre as Zonas Centro-Ibérica e de Ossa-Morena (Maciço Ibérico …

HI Chaminé, LC Pereira, PE Fonseca, F Noronha… - 2003 - ruc.udc.es
Indeed, tectonical, petrological and palynological evidences from Albergaria-a-Velha–
Coimbra–Espinhal revealed, for the very first time in this OMZ sector, an imbrication of black …

Evolução Geodinâmica dos sectores setentrionais da Zona de Ossa-Morena no contexto do Varisco Ibérico

N Moreira - 2017 - dspace.uevora.pt
Os estudos levados a cabo na região Abrantes-Tomar permitiram reconhecer dois domínios
distintos: um domínio Este com claras afinidades litoestratigráficas, estruturais e …

The Moura Phyllonitic Complex: an accretionary complex related with obduction in the Southern Iberia Variscan Suture

A Araújo, P Fonseca, J Munhá, P Moita, J Pedro… - Geodinamica …, 2005 - Taylor & Francis
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 …

Unraveling middle‐crust conductive layers in Paleozoic Orogens through 3D modeling of magnetotelluric data: The Ossa‐Morena Zone case study (SW Iberian …

G Munoz, A Mateus, J Pous, W Heise… - Journal of …, 2008 - Wiley Online Library
In recent years a number of magnetotelluric (MT) surveys have been carried out in the
southern branch of the Iberian Variscan Massif, namely in the Ossa Morena Zone (OMZ) and …

3-D electromagnetic imaging of a Palaeozoic plate-tectonic boundary segment in SW Iberian Variscides (S Alentejo, Portugal)

NV Da Silva, A Mateus, FAM Santos, EP Almeida… - Tectonophysics, 2007 - Elsevier
In SW Iberian Variscides, the boundary between the South Portuguese Zone (SPZ) and the
Ossa Morena Zone (OMZ) corresponds to a major tectonic suture that includes the Beja …

Evidence for coupled reverse and normal active faulting in W Iberia: The Vidigueira–Moura and Alqueva faults (SE Portugal)

AB da Silveira, J Cabral, H Perea, A Ribeiro - Tectonophysics, 2009 - Elsevier
The Vidigueira–Moura fault (VMF) is a 65 km long, E–W trending, N dipping reverse left-
lateral late Variscan structure located in SE Portugal (W Iberia), which has been reactivated …

A case study of two and three‐dimensional inversion of dipole‐dipole data: the Enfermarías Zn‐Pb (Ag, Sb, Au) Prospect (Moura, Portugal)

P Represas, FAM Santo, A Mateus, J Figueiras… - Near Surface …, 2005 - earthdoc.org
ABSTRACT The Enfermarías Zn‐Pb (Ag, Sb, Au) prospect, located in the Moura‐Ficalho
region (Alentejo, Portugal), was intensively explored during 1980s. A drilling programme …