Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)

Volcanism of the Garrotxa area is part of the Neogene volcanism of NE Spain (NE Spain volcanic province, NESVP). This volcanism is a manifestation of the magmatic activity consequence of the rift-type extensional tectonics that affect the eastern margin of Iberia since late Oligocene and that involv...

Descripción completa

Detalles Bibliográficos
Autores: Gisbert Pinto, Guillem, Gimeno Torrente, Domingo, Aulinas Juncà, Meritxell, Fernández Turiel, José Luis, Gasperini, D., Hernández de la Cruz, A.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2011
País:España
Institución:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositorio:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:2445/193560
Acceso en línea:https://hdl.handle.net/2445/193560
Access Level:acceso abierto
Palabra clave:Volcans
Lava
Garrotxa (Catalunya)
Geoquímica
Volcanoes
Garrotxa (Catalonia)
Geochemistry
id ES_43fdbbf5a295278e1bfdff143df01705
oai_identifier_str oai:recercat.cat:2445/193560
network_acronym_str ES
network_name_str España
repository_id_str
spelling Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)Gisbert Pinto, GuillemGimeno Torrente, DomingoAulinas Juncà, MeritxellFernández Turiel, José LuisGasperini, D.Hernández de la Cruz, A.VolcansLavaGarrotxa (Catalunya)GeoquímicaVolcanoesLavaGarrotxa (Catalonia)GeochemistryVolcanism of the Garrotxa area is part of the Neogene volcanism of NE Spain (NE Spain volcanic province, NESVP). This volcanism is a manifestation of the magmatic activity consequence of the rift-type extensional tectonics that affect the eastern margin of Iberia since late Oligocene and that involved the opening of the Valencia trough. Volcanic activity in the NESVP started weakly in the Cadaqués zone 15 Ma ago, (C. Lewis, personal communication), followed by the Empordà (9 to 12 Ma in Alt Empordà, 6 Ma in Baix Empordà), La Selva field (5 to 7 Ma) and the Tordera fault system (2 Ma). Finally, activity took place at the Garrotxa volcanic field (GVF) from 300,000 to 10,000 years ago, with an eruptive episode every 15,000 to 20,000 years approximately (C. Lewis personal communication).Sociedad Española de Mineralogía2023202320112023info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersion2 p.application/pdfhttps://hdl.handle.net/2445/193560Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)InglésReproducció del document publicat a: https://www.semineral.es/websem/PdfServlet?mod=archivos&subMod=publicaciones&archivo=Macla15_101.pdfMACLA. Revista de la Sociedad Española de Mineralogía, 2011, vol. 15, p. 101-102(c) Gisbert Pinto, Guillem et al., 2011info:eu-repo/semantics/openAccessoai:recercat.cat:2445/1935602026-05-29T05:05:01Z
dc.title.none.fl_str_mv Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
title Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
spellingShingle Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
Gisbert Pinto, Guillem
Volcans
Lava
Garrotxa (Catalunya)
Geoquímica
Volcanoes
Lava
Garrotxa (Catalonia)
Geochemistry
title_short Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
title_full Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
title_fullStr Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
title_full_unstemmed Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
title_sort Origin of green clinopyroxene cores of lavas from the garrotxa volcanic field (spain)
dc.creator.none.fl_str_mv Gisbert Pinto, Guillem
Gimeno Torrente, Domingo
Aulinas Juncà, Meritxell
Fernández Turiel, José Luis
Gasperini, D.
Hernández de la Cruz, A.
author Gisbert Pinto, Guillem
author_facet Gisbert Pinto, Guillem
Gimeno Torrente, Domingo
Aulinas Juncà, Meritxell
Fernández Turiel, José Luis
Gasperini, D.
Hernández de la Cruz, A.
author_role author
author2 Gimeno Torrente, Domingo
Aulinas Juncà, Meritxell
Fernández Turiel, José Luis
Gasperini, D.
Hernández de la Cruz, A.
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Volcans
Lava
Garrotxa (Catalunya)
Geoquímica
Volcanoes
Lava
Garrotxa (Catalonia)
Geochemistry
topic Volcans
Lava
Garrotxa (Catalunya)
Geoquímica
Volcanoes
Lava
Garrotxa (Catalonia)
Geochemistry
description Volcanism of the Garrotxa area is part of the Neogene volcanism of NE Spain (NE Spain volcanic province, NESVP). This volcanism is a manifestation of the magmatic activity consequence of the rift-type extensional tectonics that affect the eastern margin of Iberia since late Oligocene and that involved the opening of the Valencia trough. Volcanic activity in the NESVP started weakly in the Cadaqués zone 15 Ma ago, (C. Lewis, personal communication), followed by the Empordà (9 to 12 Ma in Alt Empordà, 6 Ma in Baix Empordà), La Selva field (5 to 7 Ma) and the Tordera fault system (2 Ma). Finally, activity took place at the Garrotxa volcanic field (GVF) from 300,000 to 10,000 years ago, with an eruptive episode every 15,000 to 20,000 years approximately (C. Lewis personal communication).
publishDate 2011
dc.date.none.fl_str_mv 2011
2023
2023
2023
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/193560
url https://hdl.handle.net/2445/193560
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a: https://www.semineral.es/websem/PdfServlet?mod=archivos&subMod=publicaciones&archivo=Macla15_101.pdf
MACLA. Revista de la Sociedad Española de Mineralogía, 2011, vol. 15, p. 101-102
dc.rights.none.fl_str_mv (c) Gisbert Pinto, Guillem et al., 2011
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) Gisbert Pinto, Guillem et al., 2011
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 2 p.
application/pdf
dc.publisher.none.fl_str_mv Sociedad Española de Mineralogía
publisher.none.fl_str_mv Sociedad Española de Mineralogía
dc.source.none.fl_str_mv Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
collection Recercat. Dipósit de la Recerca de Catalunya
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869407062812786688
score 15,81155

Similares en LA Referencia