Publicaciones en colaboración con investigadores/as de Universidad Complutense de Madrid (30)

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. A conceptual model for the evolution of a magmatic system based on U-Pb zircon studies on the Devonian granites of Sierra de San Luis, Argentina

    International Geology Review, Vol. 66, Núm. 9, pp. 1794-1814

  3. 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

  4. 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

  1. Comments on Bahlburg (2021), A Silurian-Devonian active margin in the proto- Andes –new data on an old conundrum: International Geology Review doi.org/10.1080/00206814.2021.2012719

    International Geology Review, Vol. 65, Núm. 3, pp. 489-490

  2. Exploring paleoproterozoic metamorphism in the western Río de la Plata craton from drill-core evidence

    Journal of South American Earth Sciences, Vol. 131

  3. Geochemistry of metasedimentary rocks from the Eastern Pyrenees (Iberian Peninsula): Implications for correlation of Ediacaran terranes along the Gondwanan margin

    Precambrian Research, Vol. 397

  4. Petrogenetic evolution and thermobarometry of the Late Jurassic La Hoya pluton, early stages of the North Patagonian batholith, southwestern Argentina

    International Journal of Earth Sciences, Vol. 112, Núm. 6, pp. 1687-1716

2022

  1. The Andaluca plutonic unit, Vinquis Intrusive Complex, Argentina: An assessment of mantle role in the genesis of Early Carboniferous weakly peraluminous A-type granites in the pre-Andean SW Gondwana margin

    Lithos, Vol. 434-435

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. A review of Devonian–Carboniferous magmatism in the central region of Argentina, pre-Andean margin of SW Gondwana

    Earth-Science Reviews, Vol. 221

  3. Early Ordovician magmatism in the Sierra de Ancaján, Sierras Pampeanas (Argentina): implications for the early evolution of the proto-Andean margin of Gondwana

    Journal of Iberian Geology, Vol. 47, Núm. 1-2, pp. 39-63

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

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

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

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

  6. Geochemistry and geochronology of intermediate volcanic rocks from the Compostela area, Nayarit, Mexico: Implications for petrogenesis and tectonic setting

    Geological Journal, Vol. 56, Núm. 8, pp. 4401-4428

  7. 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

  8. Sheeted intrusion of granitic magmas in the upper crust – Emplacement and thermal evolution of the Guandacolinos pluton, NW Argentina

    Tectonophysics, Vol. 816

  9. 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

2020

  1. A combined zircon Hf isotope and whole-rock Nd and Sr isotopes study of Carboniferous A-type granites, Sierras Pampeanas of Argentina

    Journal of South American Earth Sciences, Vol. 100

  2. 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

    International Geology Review, pp. 1-24