Natural History Museum-ko ikertzaileekin lankidetzan egindako argitalpenak (19)

2011

  1. Diachronous post-orogenic magmatism within a developing orocline in Iberia, European Variscides

    Tectonics, Vol. 30, Núm. 5

  2. Iberian late-Variscan granitoids: Some considerations on crustal sources and the significance of "mantle extraction ages"

    Lithos, Vol. 123, Núm. 1-4, pp. 121-132

2009

  1. From Rodinia to Pangaea: Ophiolites from NW Iberia as witness for a long-lived continental margin

    Geological Society Special Publication, Vol. 327, pp. 317-341

2008

  1. Detrital Zircon Data from the Eastern Mixteca Terrane, Southern Mexico: Evidence for an Ordovician-Mississippian Continental Rise and a Permo-Triassic Clastic Wedge Adjacent to Oaxaquia

    Middle American Terranes, Potential Correlatives, and Orogenic Processes (CRC Press), pp. 147-161

2007

  1. Provenance of the Granjeno Schist, Ciudad Victoria, México: Detrital zircon U-Pb age constraints and implications for the Paleozoic paleogeography of the Rheic Ocean

    Special Paper of the Geological Society of America

  2. U-Pb chronometry of polymetamorphic high-pressure granulites: An example from the allochthonous terranes of the NW Iberian Variscan belt

    Memoir of the Geological Society of America

2006

  1. A U-Pb study of zircons from a lower crustal granulite xenolith of the Spanish central system: A record of Iberian lithospheric evolution from the Neoproterozoic to the Triassic

    Journal of Geology, Vol. 114, Núm. 4, pp. 471-483

  2. A pre-Rodinian ophiolite involved in the Variscan suture of Galicia (Cabo Ortegal Complex, NW Spain)

    Journal of the Geological Society, Vol. 163, Núm. 5, pp. 737-740

  3. Detrital zircon data from the eastern Mixteca terrane, southern Mexico: Evidence for an Ordovician-Mississippian continental rise and a Permo-Triassic clastic wedge adjacent to Oaxaquia

    International Geology Review, Vol. 48, Núm. 2, pp. 97-111

  4. Geochemistry and U-Pb protolith ages of eclogitic rocks of the Asís Lithodeme, Piaxtla Suite, Acatlán Complex, southern Mexico: Tectonothermal activity along the southern margin of the Rheic Ocean

    Journal of the Geological Society, Vol. 163, Núm. 4, pp. 683-695

  5. Recent advances in in situ U-Pb dating of geological events by laser ablation inductively coupled plasma mass spectrometry

    Spectroscopy Europe, Vol. 18, Núm. 4, pp. 8-14

2005

  1. New data (U-Pb, K-Ar) on the geochronology of the alkaline-carbonatitic association of Fuerteventura, Canary Islands, Spain

    Lithos, Vol. 85, Núm. 1-4 SPEC. ISS., pp. 140-153

2004

  1. Contiguous rather than discrete Paleozoic histories for the Avalon and Meguma terranes based on detrital zircon data

    Geology, Vol. 32, Núm. 7, pp. 585-588

  2. Lithogeochemical and Sm-Nd and U-Pb isotope data from the Silurian-Lower Devonian Arisaig Group clastic rocks, Avalon terrane, Nova Scotia: A record of terrane accretion in the Appalachian-Caledonide orogen

    Bulletin of the Geological Society of America, Vol. 116, Núm. 9-10, pp. 1183-1201

  3. U-Pb (LA-ICP-MS) dating of detrital zircons from Cambrian elastic rocks in Avalonia: Erosion of a Neoproterozoic arc along the northern Gondwanan margin

    Journal of the Geological Society, Vol. 161, Núm. 2, pp. 243-254

2003

  1. Advances in U-Pb geochronology using a frequency quintupled Nd:YAG based laser ablation system (λ = 213 nm) and quadrupole based ICP-MS

    Journal of Analytical Atomic Spectrometry, Vol. 18, Núm. 8, pp. 847-855

  2. Constraints on the provenance of the uppermost allochthonous terrane of the NW Iberian Massif: Inferences from detrital zircon U-Pb ages

    Terra Nova, Vol. 15, Núm. 3, pp. 138-144

  3. Terrane accretion and dispersal in the northern Gondwana margin. An Early Paleozoic analogue of a long-lived active margin

    Tectonophysics, Vol. 365, Núm. 1-4, pp. 221-232

2002

  1. The importance of along-margin terrane transport in northern Gondwana: Insights from detrital zircon parentage in Neoproterozoic rocks from Iberia and Brittany

    Earth and Planetary Science Letters, Vol. 204, Núm. 1-2, pp. 75-88