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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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Publicat a:Geologica Acta: an international earth science journal
Autors principals: P. ANDONAEGUI, J. ABATI, R. DÍEZ FERNÁNDEZ
Format: Artigo
Idioma:Inglês
Publicat: Universitat de Barcelona 2017
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Accés en línia:https://www.redalyc.org/articulo.oa?id=50553843005
https://www.redalyc.org/journal/505/50553843005/
https://www.redalyc.org/journal/505/50553843005/html/
https://www.redalyc.org/journal/505/50553843005/50553843005.epub
https://www.redalyc.org/journal/505/50553843005/movil
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