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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

The North African section of the Gondwana margin was the site of voluminous, arc-related magmatism during the Late Neoproterozoic (Avalonian–Cadomian orogen). The lower (and older) metasedimentary sequence that constitutes the Basal Units of the Allochthonous Complexes of NW Iberia was deposited in...

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Detalhes bibliográficos
Publicado no:Geologica Acta: an international earth science journal
Main Authors: P. ANDONAEGUI, J. ABATI, R. DÍEZ FERNÁNDEZ
Formato: Artigo
Idioma:Inglês
Publicado em: Universitat de Barcelona 2017
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Acesso em linha:https://www.redalyc.org/articulo.oa?id=50553843005
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