2026-06-27T23:17:06Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/237082023-08-28T13:23:42Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Díez Fernández, Rubén
author
Arenas Martín, Ricardo
2023-06-18T05:59:26Z
2023-06-18T05:59:26Z
2015-07
0040-1951
10.1016/j.tecto.2015.05.001 0040-1951
https://hdl.handle.net/20.500.14352/23708
https://www.sciencedirect.com/journal/tectonophysics/vol/654/suppl/C
http:// www.elsevier.com/locate/tecto
Correlation of three high-P and low to intermediate-T belts from NW and SW Iberia allows recognition of a single terrane affected by Late Devonian continental subduction during the Variscan orogeny. This terrane is located in the lower part of the allochthonous complexes of NW Iberia, and in a lower position in most of the Ossa Morena Zone that, therefore, emerges as another allochthonous complex of Iberia. The Ossa Morena Complex together with the allochthonous complexes of NW Iberia form a huge rootless nappe that was transported towards the Variscan foreland during final assembly of Pangea.
eng
The Late Devonian Variscan suture of the Iberian Massif: A correlation of high-pressure belts in NW and SW Iberia
journal article
URL
https://docta.ucm.es/bitstreams/46b788f7-cb20-4d4b-bd05-50d13e40346a/download
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d480c24b78d69eccf41f675d5e15cf02
1261443
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The Late Devonian Variscan suture of the Iberian.pdf