Abstract In the Franco-Cantabrian region and Catalonia, the Upper Palaeolithic begins with
three assemblage-types found in stratigraphic order through the interval between 45,000 …

The Iberian microcontinent stands out because of its intense Alpine intraplate deformation.
This is reflected in a large number of Cenozoic basins of very different sizes. Most of the …

Thomsen, KJ, Murray, AS, Jain, M., Bøtter-Jensen, L.[2008. Laboratory fading rates of
various luminescence signals from feldspar-rich sediment extracts. Radiat. Meas. 43, 1474 …

Abstract Late Cenozoic (and especially Quaternary) fluvial deposits and related landforms
provide valuable information about landscape evolution, not just in terms of changing …

The late persistence in Southern Iberia of a Neandertal-associated Middle Paleolithic is
supported by the archeological stratigraphy and the radiocarbon and luminescence dating …

The Portuguese mainland, located in western Iberia, represents a key area for
understanding the evolution of the European Atlantic margin during the Cenozoic and the …

Two clearly differentiated techno-complexes can be recognised in the Iberian Peninsula
during the second half of the Middle Pleistocene: the Acheulean and the Middle Palaeolithic …

The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and
deformation belts with a wide variety of structural trends. The Spanish‐Portuguese Central …

This work analyses the chronology of fluvial terrace sequences of the two most important
fluvial basins from central Spain draining to the Atlantic Ocean (Upper Tagus and Duero …

This paper presents a synthesis of the neotectonic studies performed in mainland Portugal
that address the “recent”(post Piacenzian,~ 3 Ma) tectonic evolution of the Portuguese …