Alpine tectonic wedging and crustal delamination in the Cantabrian Mountains (NW Spain)
The Cantabrian Mountains have been interpreted as a Paleozoic basement block uplifted during an Alpine deformation event that led to the partial closure of the Bay of Biscay and the building of the Pyrenean range in the Cenozoic. A detailed interpretation of deep seismic reflection profile ESCIN-2 a...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-07-01
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| Series: | Solid Earth |
| Online Access: | http://www.solid-earth.net/7/1043/2016/se-7-1043-2016.pdf |