RICARDO
ARENAS MARTÍN
Catedrático de universidad
José Ramón
Martínez Catalán
Publicaciones en las que colabora con José Ramón Martínez Catalán (54)
2015
2014
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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
2013
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Thickening and exhumation of the Variscan roots in the Iberian Central System: Tectonothermal processes and 40Ar/39Ar ages
Tectonophysics, Vol. 587, pp. 207-221
2012
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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
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The Corredoiras orthogneiss (NW Iberian Massif): Geochemistry and geochronology of the Paleozoic magmatic suite developed in a peri-Gondwanan arc
Lithos, Vol. 128-131, pp. 84-99
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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
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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
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One- and two-dimensional models are equally effective in monitoring the crust's thermal response to advection by large-scale thrusting during orogenesis
Computers and Geosciences, Vol. 37, Núm. 8, pp. 1205-1207
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Tectonic evolution of a continental subduction-exhumation channel: Variscan structure of the basal allochthonous units in NW Spain
Tectonics, Vol. 30, Núm. 3
2010
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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
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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
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A rootless suture and the loss of the roots of a mountain chain: The Variscan belt of NW Iberia
Comptes Rendus - Geoscience
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Textural record of an intra-oceanic subduction.: the Careon ophiolite (NW Spain)
Trabajos de geología, Núm. 29, pp. 303-304
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Use of thermal modeling to assess the tectono-metamorphic history of the Lugo and Sanabria gneiss domes, Northwest Iberia
Bulletin de la Societe Geologique de France, Vol. 180, Núm. 3, pp. 179-197
2007
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Careón ophiolite, NW Spain: Suprasubduction zone setting for the youngest rheic ocean floor
Geology, Vol. 35, Núm. 1, pp. 53-56
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Geochemistry of two associated ophiolites from the Cabo Ortegal Complex (Variscan belt of NW Spain)
Memoir of the Geological Society of America
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Paleozoic ophiolites in the Variscan suture of Galicia (northwest Spain): Distribution, characteristics, and meaning
Memoir of the Geological Society of America
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Space and time in the tectonic evolution of the northwestern Iberian Massif: Implications for the Variscan belt
Memoir of the Geological Society of America
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Tectonic evolution of the upper allochthon of the Órdenes complex (northwestern Iberian Massif): Structural constraints to a polyorogenic peri-Gondwanan terrane
Special Paper of the Geological Society of America
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The Vila de Cruces ophiolite: A remnant of the early Rheic Ocean in the Variscan suture of Galicia (northwest Iberian Massif)
Journal of Geology, Vol. 115, Núm. 2, pp. 129-148