odre usal.es

ODRE

Provenance variability along the Early Ordovician north Gondwana margin Paleogeographic and tectonic implications of U-Pb detrital zircon ages from the Armorican Quartzite of the Iberian Variscan belt. J Shaw, G. Gutiérrez-Alonso, S.T. Johnston and D. Pastor Galán. Tectonic evolution of NW Iberia during the Paleozoic inferred from the geochemical record of detrital rocks in the Cantabrian Zone. J Fernández-Suárez G. Gutiérrez-Alonso D. Pastor-Galán M. Hofmann J. B. Murphy U. Linn.S T Johnston, A.B.
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ODRE

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Provenance variability along the Early Ordovician north Gondwana margin Paleogeographic and tectonic implications of U-Pb detrital zircon ages from the Armorican Quartzite of the Iberian Variscan belt. J Shaw, G. Gutiérrez-Alonso, S.T. Johnston and D. Pastor Galán. Tectonic evolution of NW Iberia during the Paleozoic inferred from the geochemical record of detrital rocks in the Cantabrian Zone. J Fernández-Suárez G. Gutiérrez-Alonso D. Pastor-Galán M. Hofmann J. B. Murphy U. Linn.S T Johnston, A.B.

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This site odre.usal.es has the following on the site, "Provenance variability along the Early Ordovician north Gondwana margin Paleogeographic and tectonic implications of U-Pb detrital zircon ages from the Armorican Quartzite of the Iberian Variscan belt." Our analyzers noticed that the webpage also said " Tectonic evolution of NW Iberia during the Paleozoic inferred from the geochemical record of detrital rocks in the Cantabrian Zone."

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