The early evolution of SW Europe Variscides started by opening of the Rheic ocean at∼ 500
Ma, splitting Avalonia from Armorica/Iberia. Subduction on the SE side of Rheic generated …

I review recent investigations on the electrical conductivity of the lithosphere and
asthenosphere in Europe. The principal method in the reviewed studies is the …

The application of geophysical techniques to massive sulphide deposits exploration has
proven to be a success in the Iberian Pyrite Belt (IPB) metallogenetic province, both in …

We compare recent magnetotelluric investigations of four large fault systems:(i) the actively
deforming, ocean-continent interplate San Andreas Fault (SAF);(ii) the actively deforming …

The western part of the Iberian Peninsula (Iberian Massif) is the best exposed fragment of
the Variscan orogen in Europe. Its southern half was generated by an oblique collision …

The crustal structure in Western Iberia, is the result of a complex geodynamic history. Most of
the surface is covered by rocks dating to the Variscan orogeny, the coastal ranges …

Electrical anisotropy in the Earth's crust and upper mantle has recently gained attention as a
significant linking factor between electrical models and underlying structural and tectonic …

Two wide‐angle seismic transects have been acquired across the SW Iberian Massif. They
crossed three major geological zones (South Portuguese Zone, Ossa‐Morena Zone, and …

The pre‐Mesozoic geodynamic evolution of SW Iberia has been investigated on the basis of
detailed structural analysis, isotope dating, and petrologic study of high‐pressure (HP) …

The Namibian margin is dominated by the late Proterozoic to early Cambrian fold belts of the
Damara Orogen, which wrap around and separate the Congo and Kalahari Cratons. This …