He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources

Detalhes bibliográficos
Autor(a) principal: Madureira, Pedro
Data de Publicação: 2011
Outros Autores: Moreira, Manuel, Nunes, João Carlos, Lourenço, Nuno, Gautheron, Cécile, Carvalho, Maria do Rosário, Mata, João, Pinto de Abreu, Manuel
Tipo de documento: Artigo de conferência
Idioma: por
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/3219
Resumo: We present He and Ne isotopic data from subaerial and submarine samples collected along the Terceira Rift. Graciosa Island as well as the western end of S. Miguel Island and D. João de Castro Bank display 4He/3He ratios similar to those observed along the MAR segments located to the north of the Azores Triple Junction area. Conversely, samples from the south Hirondelle Basin display a 4He/3He ratio similar to that of the MAR segments located to the south of the Azores Plateau. The Terceira Rift is thus characterized by the mingling of two different mantle domains referred as ‘Eurasia’ and ‘Nubia’ type. He and Ne systematics shows that the influence of the relatively primitive source sampled by the Azores plume can be followed along the Terceira Rift from the Graciosa Island towards the south Hirondelle Basin. Moreover, samples from the south Hirondelle Basin, D. João de Castro Bank and Graciosa Island cannot be explained by the same hyperbolic mixing model that encloses Terceira data.
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spelling He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sourcesNoble Gases (He, Ne)Terceira RiftWe present He and Ne isotopic data from subaerial and submarine samples collected along the Terceira Rift. Graciosa Island as well as the western end of S. Miguel Island and D. João de Castro Bank display 4He/3He ratios similar to those observed along the MAR segments located to the north of the Azores Triple Junction area. Conversely, samples from the south Hirondelle Basin display a 4He/3He ratio similar to that of the MAR segments located to the south of the Azores Plateau. The Terceira Rift is thus characterized by the mingling of two different mantle domains referred as ‘Eurasia’ and ‘Nubia’ type. He and Ne systematics shows that the influence of the relatively primitive source sampled by the Azores plume can be followed along the Terceira Rift from the Graciosa Island towards the south Hirondelle Basin. Moreover, samples from the south Hirondelle Basin, D. João de Castro Bank and Graciosa Island cannot be explained by the same hyperbolic mixing model that encloses Terceira data.2012-01-10T17:09:29Z2012-01-102011-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjecthttp://hdl.handle.net/10174/3219http://hdl.handle.net/10174/3219pornaonaosimpedro@uevora.ptmoreira@ipgp.frjcnunes@notes.uac.ptnlourenco@am-em.orgcecile.gautheron@u-psud.frmdrcarvalho@fc.ul.ptjmata@fc.ul.ptmapabreu@am-em.org247Madureira, PedroMoreira, ManuelNunes, João CarlosLourenço, NunoGautheron, CécileCarvalho, Maria do RosárioMata, JoãoPinto de Abreu, Manuelinfo: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:RCAAP2023-08-08T03:46:25ZPortal AgregadorONG
dc.title.none.fl_str_mv He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
title He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
spellingShingle He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
Madureira, Pedro
Noble Gases (He, Ne)
Terceira Rift
title_short He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
title_full He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
title_fullStr He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
title_full_unstemmed He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
title_sort He and Ne isotopic ratios from the Terceira Rift (Azores): Constraints on the boundary between Eurasia and Nubia mantle sources
author Madureira, Pedro
author_facet Madureira, Pedro
Moreira, Manuel
Nunes, João Carlos
Lourenço, Nuno
Gautheron, Cécile
Carvalho, Maria do Rosário
Mata, João
Pinto de Abreu, Manuel
author_role author
author2 Moreira, Manuel
Nunes, João Carlos
Lourenço, Nuno
Gautheron, Cécile
Carvalho, Maria do Rosário
Mata, João
Pinto de Abreu, Manuel
author2_role author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Madureira, Pedro
Moreira, Manuel
Nunes, João Carlos
Lourenço, Nuno
Gautheron, Cécile
Carvalho, Maria do Rosário
Mata, João
Pinto de Abreu, Manuel
dc.subject.por.fl_str_mv Noble Gases (He, Ne)
Terceira Rift
topic Noble Gases (He, Ne)
Terceira Rift
description We present He and Ne isotopic data from subaerial and submarine samples collected along the Terceira Rift. Graciosa Island as well as the western end of S. Miguel Island and D. João de Castro Bank display 4He/3He ratios similar to those observed along the MAR segments located to the north of the Azores Triple Junction area. Conversely, samples from the south Hirondelle Basin display a 4He/3He ratio similar to that of the MAR segments located to the south of the Azores Plateau. The Terceira Rift is thus characterized by the mingling of two different mantle domains referred as ‘Eurasia’ and ‘Nubia’ type. He and Ne systematics shows that the influence of the relatively primitive source sampled by the Azores plume can be followed along the Terceira Rift from the Graciosa Island towards the south Hirondelle Basin. Moreover, samples from the south Hirondelle Basin, D. João de Castro Bank and Graciosa Island cannot be explained by the same hyperbolic mixing model that encloses Terceira data.
publishDate 2011
dc.date.none.fl_str_mv 2011-01-01T00:00:00Z
2012-01-10T17:09:29Z
2012-01-10
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moreira@ipgp.fr
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cecile.gautheron@u-psud.fr
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