Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)

The Manzalvos-Castromil massif (NW Iberian Hercynian Belt) is mainly composed of granitoids that define an alumino-potassic association. Magmatic microgranular enclaves and scattered amphibole-biotite intermediate rocks are present in the massif. These rocks are later intruded by some two micas gran...

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Detalles Bibliográficos
Autores: Bellido Mulas, F., Gallastegui, G., Díez Montes, Alejandro
Tipo de recurso: artículo
Fecha de publicación:2002
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/9368
Acceso en línea:http://hdl.handle.net/10272/9368
Access Level:acceso abierto
Palabra clave:Granitoids
Basic Enclaves
Manzalvos-Castromil
Central Iberian Zone
Hercynian Belt
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spelling Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)Petrology of the Manzalvos-Castromil granitic massif (NW Central Iberian Zone)Bellido Mulas, F.Gallastegui, G.Díez Montes, AlejandroGranitoidsBasic EnclavesManzalvos-CastromilCentral Iberian ZoneHercynian BeltThe Manzalvos-Castromil massif (NW Iberian Hercynian Belt) is mainly composed of granitoids that define an alumino-potassic association. Magmatic microgranular enclaves and scattered amphibole-biotite intermediate rocks are present in the massif. These rocks are later intruded by some two micas granites and leucogranites that result in hybrid contact zones. Field relationships point out to a quasi-simultaneous intrusion of both basic magmas and granitoids. The hybrid nature of the calcoalkaline basic magma is deduced from its petrological, mineralogical and geochemical characteristics. They are derived from a basic magma evolving by assimilation and contamination with crustal components in the middle continental crustSociedad Geológica de España20022002-01-0120022002-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9368reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/93682026-06-02T14:58:11Z
dc.title.none.fl_str_mv Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
Petrology of the Manzalvos-Castromil granitic massif (NW Central Iberian Zone)
title Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
spellingShingle Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
Bellido Mulas, F.
Granitoids
Basic Enclaves
Manzalvos-Castromil
Central Iberian Zone
Hercynian Belt
title_short Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
title_full Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
title_fullStr Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
title_full_unstemmed Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
title_sort Petrología del macizo granítico de Manzalvos-Castromil (NO de la Zona Centro-Ibérica)
dc.creator.none.fl_str_mv Bellido Mulas, F.
Gallastegui, G.
Díez Montes, Alejandro
author Bellido Mulas, F.
author_facet Bellido Mulas, F.
Gallastegui, G.
Díez Montes, Alejandro
author_role author
author2 Gallastegui, G.
Díez Montes, Alejandro
author2_role author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Granitoids
Basic Enclaves
Manzalvos-Castromil
Central Iberian Zone
Hercynian Belt
topic Granitoids
Basic Enclaves
Manzalvos-Castromil
Central Iberian Zone
Hercynian Belt
description The Manzalvos-Castromil massif (NW Iberian Hercynian Belt) is mainly composed of granitoids that define an alumino-potassic association. Magmatic microgranular enclaves and scattered amphibole-biotite intermediate rocks are present in the massif. These rocks are later intruded by some two micas granites and leucogranites that result in hybrid contact zones. Field relationships point out to a quasi-simultaneous intrusion of both basic magmas and granitoids. The hybrid nature of the calcoalkaline basic magma is deduced from its petrological, mineralogical and geochemical characteristics. They are derived from a basic magma evolving by assimilation and contamination with crustal components in the middle continental crust
publishDate 2002
dc.date.none.fl_str_mv 2002
2002-01-01
2002
2002-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/9368
url http://hdl.handle.net/10272/9368
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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