Pilar Andonaegui, Rubén Díez Fernández, Jacobo Abati- Time-resolved geochemical data from the orthogneisses of the basal units of the Allochthonous complexes … Más
Etiqueta: Díez Fernández-R.
A unique blueschist facies metapelite with Mg-rich chloritoid from the Badajoz-Córdoba Unit (SW Iberian Massif): correlation of Late Devonian high-pressure belts along the Variscan Orogen
R. Arenas (et al.)- The Badajoz-Córdoba Unit (BCU, SW Iberian Massif) is a Variscan high-P unit mainly constituted by metapelites, … Más
Reconstruction of the prograde PT history of high‐P migmatitic paragneisses via melt‐reintegration approach and thermodynamic modelling (Allochthonous Complexes, NW Iberian Massif)
Irene Novo‐Fernández (et al.)- The Upper Units of the allochthonous complexes of the NW Iberian Massif constitute a terrane with … Más
Single subduction zone for the generation of Devonian ophiolites and high‐P metamorphic belts of the Variscan Orogen (NW Iberia)
Rubén Díez Fernández (et al.)- Within the Variscan Orogen, Early Devonian and Late Devonian high‐P belts separated by mid‐Devonian ophiolites … Más
Geochemical and isotopic (SmNd) provenance of Ediacaran-Cambrian metasedimentary series from the Iberian Massif. Paleoreconstruction of the North Gondwana margin
José Manuel Fuenlabrada (et al.)- The geochemical and isotopic (SmNd) features of the Ediacaran-Cambrian siliciclastic series from the Central Iberian … Más
Contrasting isotopic sources (Sm-Nd) of Late Ediacaran series in the Iberian Massif: Implications for the Central Iberian-Ossa Morena boundary
Esther Rojo-Pérez (et a.)- In the Iberian Massif, westernmost sector of the Variscan Orogen, the nature of the boundary between the … Más
Re-folded structure of syn-orogenic granitoids (Padrón dome, NW Iberia): Assessing rheological evolution of cooling continental crust in a collisional setting
Rubén Díez Fernández, Francisco J. Rubio Pascual, Luis Miguel Martín Parra – This contribution discusses about the rheological, kinematic and dynamic frameworks … Más
Ediacaran Obduction of a Fore‐Arc Ophiolite in SW Iberia: A Turning Point in the Evolving Geodynamic Setting of Peri‐Gondwana
Rubén Díez Fernández (et al.)- The Calzadilla Ophiolite is an ensemble of mafic and ultramafic rocks that represents the transition … Más
Combined zircon UPb and LuHf isotopes study of magmatism and high-P metamorphism of the basal allochthonous units in the SW Iberian Massif (Ossa-Morena complex)
Jacobo Abati (et al.)- UPb and LuHf isotope ratios measured in zircon crystals from magmatic and metamorphic rocks provide crucial information to understand the origin and tectonothermal evolution … Más
The Calzadilla Ophiolite (SWIberia) and the Ediacaran fore-arc evolution of the African margin of Gondwana
Ricardo Arenas (et al.)- In the Ossa Morena Domain of SW Iberia, the Calzadilla Ophiolite is formed by an ensemble of ultramafic and mafic … Más
S-type granite generation and emplacement during a regional switch from extensional to contractional deformation (Central Iberian Zone, Iberian autochthonous domain, Variscan Orogeny)
M. F. Pereira (et al.)- Zircon grains extracted from S-type granites of the Mêda-Escalhão-Penedono Massif (Central Iberian Zone, Variscan Orogen) constrain the … Más