The collision between Gondwana and Laurussia that formed the latest supercontinent,
Pangea, occurred during Devonian to Early Permian times and resulted in large-scale …

The Escoural gold district belongs to the Montemor-Ficalho metallogenic belt which is part of
the Portuguese section of Ossa-Morena Zone (OMZ), at the SW of Iberia. The Escoural gold …

A Cambro-Ordovician palaeogeographical restoration of the southwestern European margin
of Gondwana is proposed based on the relative positions of Variscan tectonostratigraphic …

The volcanism in the Iberian Pyrite Belt migrated from the present day west/southwest to the
east/northeast during Devonian/Carboniferous times. Evidence is here discussed based in …

Abstract The Variscan Orogen in Iberia and the Anti-Atlas Mountains in Morocco contains a
set of ophiolites formed between Neoproterozoic and Devonian times, during the complex …

The recently discovered massive and stockwork sulphide mineralization of Semblana-Rosa
Magra and Monte Branco, situated ESE of the Neves–Corvo volcanogenic massive sulphide …

The comprehensive mapping of resistivities in depth and its interpretation is of great
importance to unravel the electrical properties of deep‐seated rocks, providing significant …

Abstract The Azenhas and Alvito Fe-deposits are located at SW of the Iberian Variscan belt,
in a wide Fe-Zn ore district (Montemor-Ficalho Belt), part of the Ossa-Morena Zone. Both …

Magma‐poor rifted margins can be affected by magmatic occurrences coeval with rifting and
post‐rifting. Understanding the geological processes that originated these magmatic events …

In this work, we report the first palynological age for the base strata of the Silves Sandstones
of the Silves Group in the Algarve Basin, located in Southern Portugal. The group is the …