Add to ORKGNa área de Abrantes (Zona Ossa Morena), o extremo NW da Zona de Cisalhamento de Tomar-Badajoz-Córdoba termina contra a Zona de Cisalhamento Porto-Tomar-Ferreira do Alentejo. Mantos de carreamento de soco Cadomiano foram transportados para NE durante a orogenia Varisca; granulitos de pressão intermédia/baixa contrastam com associações cadomianas de alta pressão na zona axial da ZCTBC, devido à presença de uma sutura Cadomiana. O sistema intraplacas de mantos de soco da ZOM é conectado via a paleotransformante PTFA com os mantos de soco do sistema interplacas da sutura transportada do NW Ibérico
The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence betwee...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...
Na área de Abrantes (Zona Ossa Morena), o extremo NW da Zona de Cisalhamento de Tomar-Badajoz-Córdob...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
The Ossa-Morena Zone (SW Iberian Massif) was affected by continuous orogen-parallel transcurrent con...
The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and deformation...
A cartografia geológica da região Tomar-Sardoal-Ferreira do Zêzere permitiu individualizar sucessões...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
NW Iberia includes a rather complete section of the Variscan suture, where different terranes with c...
The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and deformation...
The Variscan Fold Belt SW suture zone involves several very different units when analysed from the t...
Abstract At SW Iberia, the boundary between Iberian and South-Portuguese Terranes is traced by a sut...
The lithosphere of Iberia has been formed through a number of processes of continental collision and...
The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence betwee...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...
Na área de Abrantes (Zona Ossa Morena), o extremo NW da Zona de Cisalhamento de Tomar-Badajoz-Córdob...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
The Ossa-Morena Zone (SW Iberian Massif) was affected by continuous orogen-parallel transcurrent con...
The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and deformation...
A cartografia geológica da região Tomar-Sardoal-Ferreira do Zêzere permitiu individualizar sucessões...
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) ...
NW Iberia includes a rather complete section of the Variscan suture, where different terranes with c...
The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and deformation...
The Variscan Fold Belt SW suture zone involves several very different units when analysed from the t...
Abstract At SW Iberia, the boundary between Iberian and South-Portuguese Terranes is traced by a sut...
The lithosphere of Iberia has been formed through a number of processes of continental collision and...
The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence betwee...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...
Abstract The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and de...