Morphotectonic significance of the main lineaments in the Iberian Massif (Portugal and Spain)
Vegas, Ramon +2 more
openaire +1 more source
Quarry mining or nature conservation, emerging conflicts in Serra de Aire e Candeeiros Natural Park (Portugal). [PDF]
Diaz MG, Carreira Dos Santos L.
europepmc +1 more source
Niche expansion of polyploid cytotypes shaped the phylogeographical history of the Salix retusa complex in the European Alpine System. [PDF]
Pittet L +3 more
europepmc +1 more source
The José Planellas Herbarium (Herbarium BCN). [PDF]
Guardia R, Soriano I.
europepmc +1 more source
<i>Cistus ladanifer</i> L.: Essential Oils, Volatiles, By-Products, and Their Biological Properties. [PDF]
Gago C +3 more
europepmc +1 more source
Human-Deer Relations during Late Prehistory: The Zooarchaeological Data from Central and Southern Portugal in Perspective. [PDF]
Almeida NJ +4 more
europepmc +1 more source
Seismic imaging of the western Iberian crust using ambient noise: Boundaries and internal structure of the Iberian Massif [PDF]
We present new Rayleigh-wave dispersion maps of the western Iberian Peninsula for periods between 8 and 30. s, obtained from correlations of seismic ambient noise, following the recent increase in seismic broadband network density in Portugal and Spain ...
Graça Silveira +2 more
exaly +5 more sources
The Galicia–Ossa-Morena Zone: Proposal for a new zone of the Iberian Massif. Variscan implications [PDF]
Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) exposed in the NW and SW of the Iberian Massif, is used to propose a new geotectonic zone in the southern branch of the Variscan Orogen: the Galicia–Ossa ...
Ricardo Arenas +2 more
exaly +2 more sources
Integrated in the national inventory of geological heritage in Portugal, the “Iberian Massif Landscape and Fluvial Network” was selected as one of the geological frameworks with international relevance.
Diamantino Insua Pereira +2 more
exaly +2 more sources
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An arcuate structure, comparable in size with the Ibero-Armorican arc, is delineated by Variscan folds and magnetic anomalies in the Central Iberian Zone of the Iberian Massif. Called the Central Iberian arc, its sense of curvature is opposite to that of the Ibero-Armorican arc, and its core is occupied by the Galicia-Tras-os-Montes Zone of NW Iberia ...
JOSÉ R Martínez Catalan
exaly +2 more sources

