Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros

Detalhes bibliográficos
Autor(a) principal: Ruget, Ch.
Data de Publicação: 2010
Outros Autores: Thierry, J., Rocha, R. B., Delance, J. H., Laurin, B., Mouterde, R., Tintant, H.
Tipo de documento: Artigo
Idioma: fra
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10362/3290
Resumo: New elements about the stratigraphy of the Serra de Candeeiros Dogger and Lower «Lusitanian» are presented. The Lower Aalenian was recognized for the first time. Bathonian (more than 50 metres thick) is dated on brachiopods and foraminifera. It corresponds to a series of massive micritic, biodetritical, coral-reef, chaetetid, bryozoa and oolitic-limestones. Callovian (120 m) begins by whitish or yellowish limestones with ammonites and brachiopods of the Gracilis zone. It is followed by regressive limestone sequences ending with thick oncolitic layers. The «Lusitanian» base is formed by greyish lagoon brackish limestones; it lies unconformably on the Dogger, with or without angular and/or cartographic unconformity. This radical facies change is related to tectonic deformation of several blocks between the Nazaré and Tagus faults during Oxfordian times.
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spelling Stratigraphie du Dogger et crise lusitanienne dans la Serra de CandeeirosStratigraphyDogger«Lusitanian»Serra de CandeeirosNew elements about the stratigraphy of the Serra de Candeeiros Dogger and Lower «Lusitanian» are presented. The Lower Aalenian was recognized for the first time. Bathonian (more than 50 metres thick) is dated on brachiopods and foraminifera. It corresponds to a series of massive micritic, biodetritical, coral-reef, chaetetid, bryozoa and oolitic-limestones. Callovian (120 m) begins by whitish or yellowish limestones with ammonites and brachiopods of the Gracilis zone. It is followed by regressive limestone sequences ending with thick oncolitic layers. The «Lusitanian» base is formed by greyish lagoon brackish limestones; it lies unconformably on the Dogger, with or without angular and/or cartographic unconformity. This radical facies change is related to tectonic deformation of several blocks between the Nazaré and Tagus faults during Oxfordian times.RUNRuget, Ch.Thierry, J.Rocha, R. B.Delance, J. H.Laurin, B.Mouterde, R.Tintant, H.2010-03-25T12:33:20Z2010-03-25T12:33:20Z2010-03-25info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10362/3290frainfo: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:RCAAP2024-03-11T03:31:35Zoai:run.unl.pt:10362/3290Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T03:14:45.865957Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
title Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
spellingShingle Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
Ruget, Ch.
Stratigraphy
Dogger
«Lusitanian»
Serra de Candeeiros
title_short Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
title_full Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
title_fullStr Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
title_full_unstemmed Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
title_sort Stratigraphie du Dogger et crise lusitanienne dans la Serra de Candeeiros
author Ruget, Ch.
author_facet Ruget, Ch.
Thierry, J.
Rocha, R. B.
Delance, J. H.
Laurin, B.
Mouterde, R.
Tintant, H.
author_role author
author2 Thierry, J.
Rocha, R. B.
Delance, J. H.
Laurin, B.
Mouterde, R.
Tintant, H.
author2_role author
author
author
author
author
author
dc.contributor.none.fl_str_mv RUN
dc.contributor.author.fl_str_mv Ruget, Ch.
Thierry, J.
Rocha, R. B.
Delance, J. H.
Laurin, B.
Mouterde, R.
Tintant, H.
dc.subject.por.fl_str_mv Stratigraphy
Dogger
«Lusitanian»
Serra de Candeeiros
topic Stratigraphy
Dogger
«Lusitanian»
Serra de Candeeiros
description New elements about the stratigraphy of the Serra de Candeeiros Dogger and Lower «Lusitanian» are presented. The Lower Aalenian was recognized for the first time. Bathonian (more than 50 metres thick) is dated on brachiopods and foraminifera. It corresponds to a series of massive micritic, biodetritical, coral-reef, chaetetid, bryozoa and oolitic-limestones. Callovian (120 m) begins by whitish or yellowish limestones with ammonites and brachiopods of the Gracilis zone. It is followed by regressive limestone sequences ending with thick oncolitic layers. The «Lusitanian» base is formed by greyish lagoon brackish limestones; it lies unconformably on the Dogger, with or without angular and/or cartographic unconformity. This radical facies change is related to tectonic deformation of several blocks between the Nazaré and Tagus faults during Oxfordian times.
publishDate 2010
dc.date.none.fl_str_mv 2010-03-25T12:33:20Z
2010-03-25T12:33:20Z
2010-03-25
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url http://hdl.handle.net/10362/3290
dc.language.iso.fl_str_mv fra
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