Rubén Díez Fernández-rekin lankidetzan egindako argitalpenak (19)

2016

  1. Relationships between syn-orogenic sedimentation and nappe emplacement in the hinterland of the Variscan belt in NW Iberia deduced from detrital zircons

    Geological Magazine, Vol. 153, Núm. 1, pp. 38-60

2015

  1. 2-D thermal modeling of HT-LP metamorphism in NW and Central Iberia: Implications for Variscan magmatism, rheology of the lithosphere and orogenic evolution

    Tectonophysics, Vol. 657, pp. 21-37

2014

  1. Correlation of the nappe stack in the Ibero-Armorican arc across the Bay of Biscay: A joint French-Spanish project

    Geological Society Special Publication, Vol. 405, Núm. 1, pp. 77-113

  2. The late variscan HT/LP metamorphic event in NW and Central Iberia: Relationships to crustal thickening, extension, orocline development and crustal evolution

    Geological Society Special Publication, Vol. 405, Núm. 1, pp. 225-247

2013

  1. Crustal thickening and attenuation as revealed by regional fold interference patterns: Ciudad Rodrigo basement area (Salamanca, Spain)

    Journal of Structural Geology, Vol. 46, pp. 115-128

  2. Rheological control on the tectonic evolution of a continental suture zone: The Variscan example from NW Iberia (Spain)

    International Journal of Earth Sciences, Vol. 102, Núm. 5, pp. 1305-1319

2012

  1. Age constraints on Lower Paleozoic convection system: Magmatic events in the NW Iberian Gondwana margin

    Gondwana Research, Vol. 21, Núm. 4, pp. 1066-1079

  2. Extensional flow during gravitational collapse: A tool for setting plate convergence (padrón migmatitic dome, Variscan belt, NW Iberia)

    Journal of Geology, Vol. 120, Núm. 1, pp. 83-103

  3. Stretching lineations in high-pressure belts: The fingerprint of subduction and subsequent events (Malpica-Tui complex, NW Iberia)

    Journal of the Geological Society, Vol. 169, Núm. 5, pp. 531-543

  4. The onset of the assembly of Pangaea in NW Iberia: Constraints on the kinematics of continental subduction

    Gondwana Research, Vol. 22, Núm. 1, pp. 20-25

  5. U-Pb detrital zircon analysis of the lower allochthon of NW iberia: Age constraints, provenance and links with the variscan mobile belt and Gondwanan cratons

    Journal of the Geological Society, Vol. 169, Núm. 6, pp. 655-665

2011

  1. Tectonic evolution of a continental subduction-exhumation channel: Variscan structure of the basal allochthonous units in NW Spain

    Tectonics, Vol. 30, Núm. 3

2010

  1. Evolución estructural y cinemática De una corteza continental subducida: la unidad de Malpica-Tui (no del Macizo Ibérico)

    Evolución estructural y cinemática De una corteza continental subducida: la unidad de Malpica-Tui (no del Macizo Ibérico)

  2. U-Pb ages of detrital zircons from the Basal allochthonous units of NW Iberia: Provenance and paleoposition on the northern margin of Gondwana during the Neoproterozoic and Paleozoic

    Gondwana Research, Vol. 18, Núm. 2-3, pp. 385-399

  3. Upper crust reworking during gravitational collapse: The Bembibre-Pico Sacro detachment system (NW Iberia)

    Journal of the Geological Society, Vol. 167, Núm. 4, pp. 769-784

2009

  1. 3D Analysis of an Ordovician igneous ensemble: A complex magmatic structure hidden in a polydeformed allochthonous Variscan unit

    Journal of Structural Geology, Vol. 31, Núm. 3, pp. 222-236

  2. A rootless suture and the loss of the roots of a mountain chain: The Variscan belt of NW Iberia

    Comptes Rendus - Geoscience

  3. Variscan recumbent folding of Ordovician plutons in the Malpica-Tui Unit (NW Iberia) .

    Trabajos de geología, Núm. 29, pp. 234-236

2006

  1. Plegamiento recumbente en la Serra do Galiñeiro (Pontevedra, NO España)

    Geogaceta, Núm. 40, pp. 3-6