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).

Detalles Bibliográficos
Autores: Gaperini, D., Gisbert Pinto, Guillem, Gimeno Torrente, Domingo, Aulinas Juncà, Meritxell, Macera, P., Bosch, D.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2013
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/193585
Acceso en línea:https://hdl.handle.net/2445/193585
Access Level:acceso abierto
Palabra clave:Volcans
Vulcanisme
Mantell terrestre
Garrotxa (Catalunya)
Volcanoes
Volcanism
Mantle of the earth
Garrotxa (Catalonia)
Descripción
Sumario: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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