Solid Earth
Solid Earth
SE
Articles | Volume 13, issue 3
Articles | Volume 13, issue 3
https://doi.org/10.5194/se-13-659-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-13-659-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 13, issue 3
Research article
 | 
21 Mar 2022
Research article |  | 21 Mar 2022

Radial anisotropy and S-wave velocity depict the internal to external zone transition within the Variscan orogen (NW Iberia)

Jorge Acevedo, Gabriela Fernández-Viejo, Sergio Llana-Fúnez, Carlos López-Fernández, Javier Olona, and Diego Pérez-Millán

Viewed

Total article views: 2,841 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,991 770 80 2,841 201 96 133
  • HTML: 1,991
  • PDF: 770
  • XML: 80
  • Total: 2,841
  • Supplement: 201
  • BibTeX: 96
  • EndNote: 133
Views and downloads (calculated since 11 Oct 2021)
Cumulative views and downloads (calculated since 11 Oct 2021)

Viewed (geographical distribution)

Total article views: 2,841 (including HTML, PDF, and XML) Thereof 2,652 with geography defined and 189 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 Nov 2025
Download
Short summary
The NW Iberian Peninsula provides one of the most complete Variscan sections in Europe, showing the transition between a sedimentary domain with folds and thrust and a metamorphic domain with igneous intrusions. By processing the seismic ambient noise recorded by several seismograph networks in this area, new 3-D S-wave velocity and radial anisotropy models were created. These models reveal the limit between the two domains, delineating the core of the large western European Variscan Belt.
Read more
Share