Articles | Volume 7, issue 4
https://doi.org/10.5194/se-7-1043-2016
https://doi.org/10.5194/se-7-1043-2016
Research article
 | 
15 Jul 2016
Research article |  | 15 Jul 2016

Alpine tectonic wedging and crustal delamination in the Cantabrian Mountains (NW Spain)

Jorge Gallastegui, Javier A. Pulgar, and Josep Gallart

Viewed

Total article views: 2,809 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,376 1,176 257 2,809 205 209
  • HTML: 1,376
  • PDF: 1,176
  • XML: 257
  • Total: 2,809
  • BibTeX: 205
  • EndNote: 209
Views and downloads (calculated since 11 Feb 2016)
Cumulative views and downloads (calculated since 11 Feb 2016)

Cited

Latest update: 23 Nov 2024
Download
Short summary
We present the interpretation of deep seismic reflection profile ESCIN-2 across the boundary between the Cantabrian Mountains and the Cenozoic Duero Basin (NW Spain). 2-D seismic modelling allowed us to construct a N-S geological cross section which is compatible with the rest of the geophysical data. This profile shows the importance of the N-S Alpine deformation. A wedge of Cantabrian margin crust indented southwards into the delaminated Iberian crust, forcing its northward subduction.