ABSTRACT In the Iberian Variscides several first order arcuate structures have been
considered. In spite of being highly studied their characterization, formation mechanisms …

Abstract The Variscan belt of Western Europe is part of a large intra-Paleozoic belt
extending on both sides of the Atlantic from the Ouachitas in the US and the Mauritanides in …

The presence of oceanic Paleozoic sequences in the Iberian Variscan Fold Belt is used to
identify and separate suspected exotic terranes from a reference Iberian Autochthon Terrane …

Abstract Ediacaran and Early Cambrian sedimentary rocks from NW Iberia have been
investigated for detrital zircon U–Pb ages. A total of 1,161 concordant U–Pb ages were …

U–Pb geochronology of Variscan granitoid rocks from the West Asturian Leonese Zone of
the NW Iberian belt documents the episodic nature of magmatism in this section of the …

Lower-Middle Cambrian regional stages of the Iberian Peninsula (Cordubian, Ovetian,
Marianian, Bilbilian, Acadoparadoxides and Solenopleuropsidae stages) are now …

The Ossa Morena Zone of SW Iberia represents a continental arc accreted to the Iberian
Autochthon during the Late Proterozoic–Early Cambrian Cadomian orogeny. A subsequent …

Neoproterozoic-early Cambrian successions in Iberia are reexamined. A gradual transition
across the Neoproterozoic-Cambrian boundary is present in Central Iberia, whereas in the …

Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …

The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …