Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone)
Main Author: | |
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Publication Date: | 2025 |
Other Authors: | , |
Format: | Article |
Language: | eng |
Source: | Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) |
Download full: | http://hdl.handle.net/10400.9/5663 |
Summary: | ABSTRACT: This study is dedicated to the presentation and interpretation of whole-rock geochemical data concerning a few mafic subvolcanic dykes located in northern Portugal, related to the late to posttectonic stages of the Variscan orogeny. Overall, the analyzed rocks are reasonably fresh, ultrabasic to intermediate, metaluminous to moderately peraluminous, and calc-alkaline or alkaline. There is no evidence implying the occurrence of crustal contamination, but crystal fractionation is likely to have played either a minor or more meaningful role on the petrogenetic evolution. While most dykes were probably generated from subduction-modified, metasomatically-enriched lithospheric sources, others possibly derived from the asthenosphere. There are also important differences regarding the residual mineralogy of the sources, as well as the melting degrees. |
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Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone)Heterogeneidade composicional dos ciques máficos subvulcânicos, tardi a pós-variscos do norte de Portugal (Zona Centro Ibérica)LamprophyresDoleritesDykesVariscan orogenyLamprófirosDoleritosDiquesMagmatismoOrogenia VariscaABSTRACT: This study is dedicated to the presentation and interpretation of whole-rock geochemical data concerning a few mafic subvolcanic dykes located in northern Portugal, related to the late to posttectonic stages of the Variscan orogeny. Overall, the analyzed rocks are reasonably fresh, ultrabasic to intermediate, metaluminous to moderately peraluminous, and calc-alkaline or alkaline. There is no evidence implying the occurrence of crustal contamination, but crystal fractionation is likely to have played either a minor or more meaningful role on the petrogenetic evolution. While most dykes were probably generated from subduction-modified, metasomatically-enriched lithospheric sources, others possibly derived from the asthenosphere. There are also important differences regarding the residual mineralogy of the sources, as well as the melting degrees.RESUMO: O presente trabalho dedica-se à apresentação e interpretação de dados de geoquímica de rocha total sobre alguns diques subvulcânicos máficos, localizados no norte de Portugal, associados às fases tardi a pós-tectónicas da orogenia Varisca. Em geral, as rochas analisadas são razoavelmente frescas, ultrabásicas a intermédias, metaluminosas a moderadamente peraluminosas, e calcoalcalinas ou alcalinas. Não existem evidências a favor da ocorrência de contaminação crustal, mas a cristalização fracionada deverá ter desempenhado um papel mais ou menos significativo sobre a evolução petrogenética. Embora a maioria dos diques tenha provavelmente sido gerada a partir de fontes litosféricas, modificadas por subducção e enriquecidas metassomaticamente, os restantes possivelmente derivaram da astenosfera. Existem ainda diferenças importantes no que diz respeito à mineralogia residual das fontes, assim como sobre os respetivos graus de fusão.LNEG - Laboratório Nacional de Energia e GeologiaRepositório do LNEGOliveira, AntónioMartins, HelenaSant'Ovaia, H.2025-05-09T15:24:36Z2025-042025-04-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.9/5663eng0873-948X10.34637/7dm2-f386info:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2025-05-18T04:48:37Zoai:repositorio.lneg.pt:10400.9/5663Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T07:13:41.650984Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse |
dc.title.none.fl_str_mv |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) Heterogeneidade composicional dos ciques máficos subvulcânicos, tardi a pós-variscos do norte de Portugal (Zona Centro Ibérica) |
title |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
spellingShingle |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) Oliveira, António Lamprophyres Dolerites Dykes Variscan orogeny Lamprófiros Doleritos Diques Magmatismo Orogenia Varisca |
title_short |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
title_full |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
title_fullStr |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
title_full_unstemmed |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
title_sort |
Compositional heterogeneity of late to post-Variscan, mafic subvolcanic dykes from northern Portugal (Central Iberian Zone) |
author |
Oliveira, António |
author_facet |
Oliveira, António Martins, Helena Sant'Ovaia, H. |
author_role |
author |
author2 |
Martins, Helena Sant'Ovaia, H. |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
Repositório do LNEG |
dc.contributor.author.fl_str_mv |
Oliveira, António Martins, Helena Sant'Ovaia, H. |
dc.subject.por.fl_str_mv |
Lamprophyres Dolerites Dykes Variscan orogeny Lamprófiros Doleritos Diques Magmatismo Orogenia Varisca |
topic |
Lamprophyres Dolerites Dykes Variscan orogeny Lamprófiros Doleritos Diques Magmatismo Orogenia Varisca |
description |
ABSTRACT: This study is dedicated to the presentation and interpretation of whole-rock geochemical data concerning a few mafic subvolcanic dykes located in northern Portugal, related to the late to posttectonic stages of the Variscan orogeny. Overall, the analyzed rocks are reasonably fresh, ultrabasic to intermediate, metaluminous to moderately peraluminous, and calc-alkaline or alkaline. There is no evidence implying the occurrence of crustal contamination, but crystal fractionation is likely to have played either a minor or more meaningful role on the petrogenetic evolution. While most dykes were probably generated from subduction-modified, metasomatically-enriched lithospheric sources, others possibly derived from the asthenosphere. There are also important differences regarding the residual mineralogy of the sources, as well as the melting degrees. |
publishDate |
2025 |
dc.date.none.fl_str_mv |
2025-05-09T15:24:36Z 2025-04 2025-04-01T00:00:00Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10400.9/5663 |
url |
http://hdl.handle.net/10400.9/5663 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
0873-948X 10.34637/7dm2-f386 |
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info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
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application/pdf |
dc.publisher.none.fl_str_mv |
LNEG - Laboratório Nacional de Energia e Geologia |
publisher.none.fl_str_mv |
LNEG - Laboratório Nacional de Energia e Geologia |
dc.source.none.fl_str_mv |
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Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) |
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