Mantle source heterogeneity beneath the Garrotxa Volcanic Field (NE Spain)
The Neogene volcanism in NE Spain, which is related to the rift-type extensional tectonics affecting the eastern margin of Iberia since late Oligocene, is well represented in the basalts and basanites from the Garrotxa Volcanic Field (GVF).
| Authors: | , , , , , |
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| Format: | article |
| Status: | Published version |
| Publication Date: | 2013 |
| Country: | España |
| Institution: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repository: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:2445/193585 |
| Online Access: | https://hdl.handle.net/2445/193585 |
| Access Level: | Open access |
| Keyword: | Volcans Vulcanisme Mantell terrestre Garrotxa (Catalunya) Volcanoes Volcanism Mantle of the earth Garrotxa (Catalonia) |
| Summary: | The Neogene volcanism in NE Spain, which is related to the rift-type extensional tectonics affecting the eastern margin of Iberia since late Oligocene, is well represented in the basalts and basanites from the Garrotxa Volcanic Field (GVF). |
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