The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”

Detalhes bibliográficos
Autor(a) principal: Soares, António F.
Data de Publicação: 1993
Outros Autores: Rocha, Rogério B., Elmi, Serge, Henriques, Maria Helena, Mouterde, René, Almeras, Yves, Ruget, Christiane, Marques, Júlio, Duarte, Luís, Carapito, Maria Cristina, Kullberg, José Carlos
Tipo de documento: Artigo
Idioma: fra
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10316/20072
Resumo: The North-Lusitanian Subbasin has sustained a complex evolution whichcart be divided into five main stages: 1. Liassic Distension leading to the differentiation of the Arunca-Montemor lineament; 2. Lower Liassic Rifting with development of endemic ammonites-faunas (Upper Sinemurian); 3. Differential Subsidence (Middle Liassic to Lower Aalenian): eustatic changes were complicated by a strong acceleration of the differential subsidence; 4. Progradation of a carbonate platform (Middle Aalenian to Lower Callovian); 5. The closure of the subbasin began during the Middle Callovian and was followed by emersions.
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spelling The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”The North-Lusitanian Subbasin has sustained a complex evolution whichcart be divided into five main stages: 1. Liassic Distension leading to the differentiation of the Arunca-Montemor lineament; 2. Lower Liassic Rifting with development of endemic ammonites-faunas (Upper Sinemurian); 3. Differential Subsidence (Middle Liassic to Lower Aalenian): eustatic changes were complicated by a strong acceleration of the differential subsidence; 4. Progradation of a carbonate platform (Middle Aalenian to Lower Callovian); 5. The closure of the subbasin began during the Middle Callovian and was followed by emersions.Académie des sciences1993info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10316/20072http://hdl.handle.net/10316/20072fraSoares, António F. [et. al.] - The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”. "Comptes rendus de l'Académie des sciences". ISSN 0764-4450. 317:12 (1993) 1659-16660764-4450Soares, António F.Rocha, Rogério B.Elmi, SergeHenriques, Maria HelenaMouterde, RenéAlmeras, YvesRuget, ChristianeMarques, JúlioDuarte, LuísCarapito, Maria CristinaKullberg, José Carlosinfo: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:RCAAP2021-08-25T09:21:44Zoai:estudogeral.uc.pt:10316/20072Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:55:12.054375Repositório 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 The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
title The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
spellingShingle The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
Soares, António F.
title_short The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
title_full The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
title_fullStr The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
title_full_unstemmed The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
title_sort The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”
author Soares, António F.
author_facet Soares, António F.
Rocha, Rogério B.
Elmi, Serge
Henriques, Maria Helena
Mouterde, René
Almeras, Yves
Ruget, Christiane
Marques, Júlio
Duarte, Luís
Carapito, Maria Cristina
Kullberg, José Carlos
author_role author
author2 Rocha, Rogério B.
Elmi, Serge
Henriques, Maria Helena
Mouterde, René
Almeras, Yves
Ruget, Christiane
Marques, Júlio
Duarte, Luís
Carapito, Maria Cristina
Kullberg, José Carlos
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Soares, António F.
Rocha, Rogério B.
Elmi, Serge
Henriques, Maria Helena
Mouterde, René
Almeras, Yves
Ruget, Christiane
Marques, Júlio
Duarte, Luís
Carapito, Maria Cristina
Kullberg, José Carlos
description The North-Lusitanian Subbasin has sustained a complex evolution whichcart be divided into five main stages: 1. Liassic Distension leading to the differentiation of the Arunca-Montemor lineament; 2. Lower Liassic Rifting with development of endemic ammonites-faunas (Upper Sinemurian); 3. Differential Subsidence (Middle Liassic to Lower Aalenian): eustatic changes were complicated by a strong acceleration of the differential subsidence; 4. Progradation of a carbonate platform (Middle Aalenian to Lower Callovian); 5. The closure of the subbasin began during the Middle Callovian and was followed by emersions.
publishDate 1993
dc.date.none.fl_str_mv 1993
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10316/20072
http://hdl.handle.net/10316/20072
url http://hdl.handle.net/10316/20072
dc.language.iso.fl_str_mv fra
language fra
dc.relation.none.fl_str_mv Soares, António F. [et. al.] - The North-Lusitanian Subbasin (Portugal) from the Triassic to the Middle Jurassic: a model of an “aborted rift”. "Comptes rendus de l'Académie des sciences". ISSN 0764-4450. 317:12 (1993) 1659-1666
0764-4450
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dc.publisher.none.fl_str_mv Académie des sciences
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dc.source.none.fl_str_mv reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
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