Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)

Detalhes bibliográficos
Autor(a) principal: Aires-Barros, L.
Data de Publicação: 2008
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10362/1513
Resumo: The Author presents a synopsis about the post-Paleozoic igneous activity in continental Portugal. Subvolcanic massifs of Sintra, Sines and Monchique and the basaltic complex of Lisbon-Mafra are interpreted. The large network of dikes and sills occuring at north of Tagus river in Lisbon- Torres Vedras region as the dikes of Algarve and also those of diapiric formation are studied and compared. Also the doleritic dikes cuting the Hesperic Massif and the Great dike of Alentejo are studied. The Author presents an attempt of petrological and geochemical correlation-among these post-Paleozoic igneous rocks. For this more than 350 chemical analysis are used in order to elaborate several diagrams and some general conclusions are derived from them. The correlation between the origin of these igneous rocks and the opening of North Atlantic and the counter-clockwise rotation of the Iberia are also tried.
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spelling Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)Igneous activityPost-PaleozoicPortugalThe Author presents a synopsis about the post-Paleozoic igneous activity in continental Portugal. Subvolcanic massifs of Sintra, Sines and Monchique and the basaltic complex of Lisbon-Mafra are interpreted. The large network of dikes and sills occuring at north of Tagus river in Lisbon- Torres Vedras region as the dikes of Algarve and also those of diapiric formation are studied and compared. Also the doleritic dikes cuting the Hesperic Massif and the Great dike of Alentejo are studied. The Author presents an attempt of petrological and geochemical correlation-among these post-Paleozoic igneous rocks. For this more than 350 chemical analysis are used in order to elaborate several diagrams and some general conclusions are derived from them. The correlation between the origin of these igneous rocks and the opening of North Atlantic and the counter-clockwise rotation of the Iberia are also tried.RUNAires-Barros, L.2008-07-282008-07-28T00:00:00Z2008-07-28T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10362/1513porinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-07-10T15:23:08ZPortal AgregadorONG
dc.title.none.fl_str_mv Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
title Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
spellingShingle Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
Aires-Barros, L.
Igneous activity
Post-Paleozoic
Portugal
title_short Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
title_full Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
title_fullStr Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
title_full_unstemmed Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
title_sort Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
author Aires-Barros, L.
author_facet Aires-Barros, L.
author_role author
dc.contributor.none.fl_str_mv RUN
dc.contributor.author.fl_str_mv Aires-Barros, L.
dc.subject.por.fl_str_mv Igneous activity
Post-Paleozoic
Portugal
topic Igneous activity
Post-Paleozoic
Portugal
description The Author presents a synopsis about the post-Paleozoic igneous activity in continental Portugal. Subvolcanic massifs of Sintra, Sines and Monchique and the basaltic complex of Lisbon-Mafra are interpreted. The large network of dikes and sills occuring at north of Tagus river in Lisbon- Torres Vedras region as the dikes of Algarve and also those of diapiric formation are studied and compared. Also the doleritic dikes cuting the Hesperic Massif and the Great dike of Alentejo are studied. The Author presents an attempt of petrological and geochemical correlation-among these post-Paleozoic igneous rocks. For this more than 350 chemical analysis are used in order to elaborate several diagrams and some general conclusions are derived from them. The correlation between the origin of these igneous rocks and the opening of North Atlantic and the counter-clockwise rotation of the Iberia are also tried.
publishDate 2008
dc.date.none.fl_str_mv 2008-07-28
2008-07-28T00:00:00Z
2008-07-28T00:00:00Z
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10362/1513
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dc.language.iso.fl_str_mv por
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