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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 |
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| Autors principals: | , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Universitat de Barcelona
2017
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| Matèries: | |
| 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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