Articles | Volume 35, issue 5
https://doi.org/10.5194/ejm-35-845-2023
https://doi.org/10.5194/ejm-35-845-2023
Research article
 | 
18 Oct 2023
Research article |  | 18 Oct 2023

Contrasting appinites, vaugnerites and related granitoids from the NW Iberian Massif: insight into mantle and crustal sources

Gumer Galán, Gloria Gallastegui, Andrés Cuesta, Guillermo Corretgé, Ofelia Suárez, and Luis González-Menéndez

Viewed

Total article views: 1,403 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
871 472 60 1,403 122 65 142
  • HTML: 871
  • PDF: 472
  • XML: 60
  • Total: 1,403
  • Supplement: 122
  • BibTeX: 65
  • EndNote: 142
Views and downloads (calculated since 18 Oct 2023)
Cumulative views and downloads (calculated since 18 Oct 2023)

Viewed (geographical distribution)

Total article views: 1,402 (including HTML, PDF, and XML) Thereof 1,402 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Jun 2026
Download
Short summary
Two examples of granites in the Variscan Iberian Massif were studied because they are associated with mafic rocks (appinites and vaugnerites), which raise the question of the role of mantle magma in the formation of granitic rocks. We conclude that appinites and vaugnerites derived from melting of different mantle sources, both previously modified by interaction with crustal materials. Subsequent differentiation of appinites and vaugnerites was influenced by contamination with coeval granites.
Share