Results 111 to 120 of about 1,932 (208)
Variscan deformation of the Hesperian massif in the Lousã mountain range (central Portugal) [PDF]
[Abstract] The occidental region of the Central-Iberian Zone of the Variscan Iberian massif, in the central part of Portugal (Lousã mountain range), has a Variscan tectonostructural organization as the one recognized in the occidental border of the ...
Gomes, E. M. C. +2 more
core
The North African section of the Gondwana margin was the site of voluminous, arc-related magmatism during the Late Neoproterozoic (Avalonian–Cadomian orogen).
P. ANDONAEGUI +2 more
doaj
Como se ha descrito en la primera parte del trabajo (Moita et al. en este volumen), el Macizo de Hospitais pertenece a una serie magmática sinorogénica Varisca intruida en un complejo de gneises y migmatitas perteneciente a los Terrenos de Alto-grado Metamórfico de Évora. Se han utilizado datos geoquímicos de las tonalitas, de los enclaves dioríticos y
Moita, P., Santos, J. F., Pereira, M. F.
openaire +2 more sources
New SHRIMP U-Pb zircon ages for the Portalegre and Alcáçovas orthogneisses document a complex pre- Variscan history for the Iberian basement in Portugal. The available geochemical and geochronological data for the Alcáçovas orthogneiss (ca.
Cordani Umberto G. +6 more
doaj
A two-stage collision in the origin of Pangea: Evidences in NW Iberian Massif
Abstract of an oral presentation in a ...
Arenas, R. +6 more
openaire +1 more source
Fluid inclusions in magmatic ilmenite record degassing in basic magmas
Magmatic volatile phases play a major role in igneous systems, but indirect sampling of the magmatic fluid, especially for basic magmas, remains challenging to document.
Anthony Pochon +10 more
doaj +1 more source
The penultimate temperate period, 127–110 ka before present (BP), bracketed by abrupt shifts of the global climate system initiating and terminating it, is considered as an analogue of the Holocene because of a similar low global ice‐volume.
Rietti-Shati, M +7 more
core
Structural contributions on the Tamames syncline: Schist and Greywacke Domain of the Central Iberian Zone (Iberian Massif) [PDF]
Un estudio estructural del sector oriental del sinclinal de Tamames, en la Zona Centro Ibérica (ZCI) del Macizo Ibérico, evidencia que la foliación tectónica asociada a los pliegues mayores es una crenulación que, por su relación temporal con el ...
Gómez Barreiro, Juan +3 more
core
Correlation of hercynian units of the Iberian massif and southeastern France
The Olio de sapo anliform in the northwest Iberian Massif is made up of superposed allochthonous units of Paleozoic metasediments and Ordovician orthogneisses, similar to gneissic domes in the eastern Pyrenees and in the Montagne Noire of southern France.
openaire +1 more source
Silurian conodonts of the Obejo-Valsequillo Domain (SW of the Iberian Massif)
Peer ...
Aragonés-Illanas, Pau +2 more
openaire +1 more source

