Late Cambrian magmatic arc activity in peri-Gondwana: geochemical evidence from the Basal Allochthonous Units of NW Iberia

Late Cambrian magmatic arc activity in peri-Gondwana: geochemical evidence from 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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Bibliographic Details
Main Authors: P. ANDONAEGUI, J. ABATI, R. DÍEZ FERNÁNDEZ
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2017-10-01
Series:Geologica Acta
Subjects:
Convergent margin
Subduction
Magmatism
Whole rock geochemistry
NW Iberian Massif
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/17459

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/17459

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