Structure of an intraplate fold-and-thrust belt: The Iberian Chain. A synthesis
The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence between the Eurasian, Iberian and African plates during the late Eocene to the Miocene. The main trend of its contractional structures is NW-SE, but E-W, NE-SW and N-S-trending structures are also present....
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| Udgivet i: | Geologica Acta: an international earth science journal |
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| Hovedforfatter: | |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Universitat de Barcelona
2018
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| Fag: | |
| Online adgang: | https://www.redalyc.org/articulo.oa?id=50559030006 https://www.redalyc.org/journal/505/50559030006/ https://www.redalyc.org/journal/505/50559030006/html/ https://www.redalyc.org/journal/505/50559030006/50559030006.epub https://www.redalyc.org/journal/505/50559030006/movil https://doi.org/10.1344/GeologicaActa2018.16.4.6 |
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