Publicaciones en las que colabora con RUBÉN DÍEZ FERNÁNDEZ (64)

2024

  1. 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

  2. Cadomia origins: paired Ediacaran ophiolites from the Iberian Massif, the opening and closure record of peri-Gondwanan basins

    Geological Society Special Publication, Vol. 542, Núm. 1, pp. 507-526

  3. Exhumation of high-pressure rocks: role of late faulting (Eastern Ossa–Morena Complex, Iberian Massif)

    Geological Society Special Publication, Vol. 542, Núm. 1, pp. 527-548

  4. Frontier of the Paleo-Tethys Ocean in the western Mediterranean: Isotopic (Sm-Nd) constraints on sources of Devonian units from Menorca Island

    Geoscience Frontiers, Vol. 15, Núm. 5

  5. Mega-Folding of a Basement During Incipient Intra-Plate Continental Subduction (Alpine Central Iberia)

    Tectonics, Vol. 43, Núm. 4

  6. 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

  7. Origin and evolution of Cadomian magmatism in SW Iberia: from subduction onset and arc building to a tectonic switching

    International Geology Review, Vol. 66, Núm. 10, pp. 1885-1909

2023

  1. 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

  2. Variability in the sources of North Gondwana Cadomian basins tracked by Nd isotopic systematics (Iberian Massif)

    Precambrian Research, Vol. 397

2022

  1. 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

  2. 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

  3. 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

  1. 100 MYR cycles of oceanic lithosphere generation in peri-gondwana: Neoproterozoic–devonian ophiolites from the NW african–iberian margin of gondwana and the variscan orogen

    Geological Society Special Publication (Geological Society of London), pp. 169-184

  2. Correlación isotópica (Sm-Nd) entre las series Ediacáricas de Iberia y Bohemia

    Geotemas (Madrid), Núm. 18, pp. 453

  3. Evolución tectonotermal de paragneises de alta-P y alta-T (sutura Varisca, NO del Macizo Ibérico)

    Geotemas (Madrid), Núm. 18, pp. 1056

  4. Generación de litosfera oceánica en ciclos de 100 Ma en peri-Gondwana: Ofiolitas de Marruecos e Iberia

    Geotemas (Madrid), Núm. 18, pp. 1041

  5. 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

  6. 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

  7. 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

  8. 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