Actividade ígnea pós-paleozóica no continente português (elementos para uma síntese crítica)
Autor(a) principal: | |
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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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Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
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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 |
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/10362/1513 |
url |
http://hdl.handle.net/10362/1513 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
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1777302867138314240 |