Articles | Volume 7, issue 4
https://doi.org/10.5194/se-7-1043-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-7-1043-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Alpine tectonic wedging and crustal delamination in the Cantabrian Mountains (NW Spain)
Departamento de Geología, Universidad de Oviedo, Jesús Arias
de Velasco s/n, 33005 Oviedo, Spain
Javier A. Pulgar
Departamento de Geología, Universidad de Oviedo, Jesús Arias
de Velasco s/n, 33005 Oviedo, Spain
Josep Gallart
Instituto Ciencias Tierra Jaume Almera-CSIC, Lluís Solé
Sabarís s/n, 08028 Barcelona, Spain
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- Gravitational slope processes triggered by past earthquakes on the Western Cantabrian Mountains (Sierra de la Sobia, Northern Spain) F. Fernández et al. 10.1016/j.geomorph.2021.107867
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- Crustal structure of the North Iberian continental margin from seismic refraction/wide-angle reflection profiles M. Ruiz et al. 10.1016/j.tecto.2017.07.008
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Latest update: 02 Nov 2024
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.
We present the interpretation of deep seismic reflection profile ESCIN-2 across the boundary...