RICARDO
ARENAS MARTÍN
Catedrático de universidad
Instituto Geológico y Minero de España
Madrid, EspañaPublicaciones en colaboración con investigadores/as de Instituto Geológico y Minero de España (32)
2024
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A complex accretionary assembly of Pangea developed in the range c. 400–340 Ma: the four successive events of high-P/ultra-high-P metamorphism of the Variscan Orogen
International Geology Review, Vol. 66, Núm. 1, pp. 336-349
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Opening and closure of Cadomian peri-Gondwanan oceans: age and evolution of the Mérida Ophiolite (SW Iberia)
International Geology Review, Vol. 66, Núm. 1, pp. 278-309
2023
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Building and Collapse of the Cadomian Orogen: A Plate-Scale Model Based on Structural Data From the SW Iberian Massif
Tectonics, Vol. 42, Núm. 12
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Variability in the sources of North Gondwana Cadomian basins tracked by Nd isotopic systematics (Iberian Massif)
Precambrian Research, Vol. 397
2022
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Reply to Comment by Azor et al. on “On the Rootless Nature of a Devonian Suture in SW Iberia (Ossa-Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault”
Tectonics
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Tectonostratigraphy of the Mérida Massif reveals a new Cadomian suture zone exposure in Gondwana (SW Iberia)
International Geology Review, Vol. 64, Núm. 3, pp. 405-424
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U-Pb geochronology and isotopic geochemistry of adakites and related magmas in the Ediacaran arc section of the SW Iberian Massif: The role of subduction erosion cycles in peri-Gondwanan arcs
Gondwana Research, Vol. 109, pp. 89-112
2021
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Correlación isotópica (Sm-Nd) entre las series Ediacáricas de Iberia y Bohemia
Geotemas (Madrid), Núm. 18, pp. 453
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Geochemistry and Sm–Nd isotopic sources of Late Ediacaran siliciclastic series in the Ossa–Morena Complex: Iberian–Bohemian correlations
International Journal of Earth Sciences, Vol. 110, Núm. 2, pp. 467-485
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Metapelitas de alta presión de la Unidad de Badajoz-Córdoba (Macizo Ibérico): la sutura del Devónico Superior del Orógeno Varisco
Geotemas (Madrid), Núm. 18, pp. 394
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On the Rootless Nature of a Devonian Suture in SW Iberia (Ossa-Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault
Tectonics, Vol. 40, Núm. 6
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Tectonic setting and isotopic sources (Sm–Nd) of the SW Iberian Autochthon (Variscan Orogen)
Journal of Iberian Geology, Vol. 47, Núm. 1-2, pp. 121-150
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Tectonic setting and isotopic sources, Sm–Nd, of the SW Iberian Autochthon, Variscan Orogen
Journal of iberian geology: an international publication of earth sciences, Vol. 47, Núm. 1, pp. 121-150
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Tracking the Late Devonian high-P metamorphic belt in the Variscan Orogen: New constraints on the PT evolution of eclogites from the Cubito-Moura Unit (SW Iberian Massif)
Lithos, Vol. 386-387
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Two-step obduction of the Porvenir serpentinites: A cryptic Devonian suture in SW Iberian Massif (Ossa-Morena Complex)
Special Paper of the Geological Society of America, Vol. 552, pp. 113-132
2020
2019
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Contrasting isotopic sources (Sm-Nd) of Late Ediacaran series in the Iberian Massif: Implications for the Central Iberian-Ossa Morena boundary
Precambrian Research, Vol. 324, pp. 194-207
2018
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The Calzadilla Ophiolite (SW Iberia) and the Ediacaran fore-arc evolution of the African margin of Gondwana
Gondwana Research, Vol. 58, pp. 71-86
2016
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Allochthonous terranes involved in the Variscan suture of NW Iberia: A review of their origin and tectonothermal evolution
Earth-Science Reviews, Vol. 161, pp. 140-178
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Evolución tectónica del Macizo Ibérico durante la orogenia Varisca: colisión Gondwana - Laurrusia
Geotemas (Madrid), Núm. 16, pp. 215-218