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Isotopic and geochemical record of the active to passive margin transition in NW Iberia during the Cambrian-Ordovician : vestiges of a waning continental arc
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Late Cambrian magmatic arc activity in peri-Gondwana : geochemical evidence from metagranitoid rocks of the Basal Allochthonous Units of NW Iberia. (2017) Vol. 15 Núm. 4 Pág. 305-321 |