Articles | Volume 12, issue 4
https://doi.org/10.5194/se-12-835-2021
https://doi.org/10.5194/se-12-835-2021
Research article
 | 
15 Apr 2021
Research article |  | 15 Apr 2021

A tectonic carpet of Variscan flysch at the base of a rootless accretionary prism in northwestern Iberia: U–Pb zircon age constrains from sediments and volcanic olistoliths

Emilio González Clavijo, Ícaro Dias da Silva, José R. Martínez Catalán, Juan Gómez Barreiro, Gabriel Gutiérrez-Alonso, Alejandro Díez Montes, Mandy Hofmann, Andreas Gärtner, and Ulf Linnemann

Viewed

Total article views: 2,588 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,701 813 74 2,588 389 59 68
  • HTML: 1,701
  • PDF: 813
  • XML: 74
  • Total: 2,588
  • Supplement: 389
  • BibTeX: 59
  • EndNote: 68
Views and downloads (calculated since 15 Oct 2020)
Cumulative views and downloads (calculated since 15 Oct 2020)

Viewed (geographical distribution)

Total article views: 2,588 (including HTML, PDF, and XML) Thereof 2,481 with geography defined and 107 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 01 Apr 2025
Download
Short summary
In northwest Iberia, a low-grade unit separates the unrooted accretionary prism from the autochthon. It was divided into Upper (preorogenic) and Lower (synorogenic) parautochthons around the Morais Complex. A review of the sedimentary sequence characteristics, supported by U–Pb ages in 17 new samples of synorogenic sediments and volcanic olistoliths, proposes this model to show the Galicia–Trás-os-Montes Zone forming a tectonic carpet exposed in most of the Parautochthon–Autochthon limit.
Share