Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)

Detalhes bibliográficos
Autor(a) principal: Pereira, M.F.
Data de Publicação: 2020
Outros Autores: Gama, C., Dias da Silva, I., Fuenlabrada, J.M., Silva, J.B., Medina, J.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/32765
https://doi.org/10.1144/SP503-2019-163
Resumo: New Rb–Sr isotopic data from South Portuguese Zone (SPZ) turbidites show that the 87Sr/86Sr(t) ratio increases from the basal Mértola Formation (Visean–Serpukhovian: 0.706–0.707), through the Mira Formation (Serpukhovian–Bashkirian: 0.706–0.712) to the uppermost Brejeira Formation (Bashkirian– Moscovian: 0.713–0.715). In addition, estimated Nd TDM model ages for the Mértola (1.29–1.09 Ga), Mira (1.58–1.1 Ga) and Brejeira (1.73–1.37 Ga) formations indicate inverted stratigraphy for their isotopic sources. The isotope geochemical data indicate significant changes in the sources from which the SPZ Carboniferous turbidites are derived, consistent with the progressive denudation of a continental magmatic arc built on the Laurussian margin. Mértola turbidites inherited their geochemical and isotopic characteristics from an adjacent dissected Middle–Late Devonian continental magmatic arc with an intermediate–felsic composition: that is a Laurussian (Rheic magmatic arc)-type source. The progressive erosion of its plutonic roots and older host continental basement rocks are indicated in the Mira and Brejeira formations by the increasing contribution of recycled ancient continental crust. The pronounced similarity between the Nd TDM model ages and the detrital zircon populations of the Mira and Brejeira formations (SW Iberia) suggest that they share a common Laurussian (West Avalonia/Meguma terrane)-type source but a contribution from Gondwanan (Ossa-Morena)- type sources cannot be discarded.
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spelling Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)Rb-Sr - Sm-Nd isotopesCarboniferous flyschSouth-Portuguese ZoneSW IberiaNew Rb–Sr isotopic data from South Portuguese Zone (SPZ) turbidites show that the 87Sr/86Sr(t) ratio increases from the basal Mértola Formation (Visean–Serpukhovian: 0.706–0.707), through the Mira Formation (Serpukhovian–Bashkirian: 0.706–0.712) to the uppermost Brejeira Formation (Bashkirian– Moscovian: 0.713–0.715). In addition, estimated Nd TDM model ages for the Mértola (1.29–1.09 Ga), Mira (1.58–1.1 Ga) and Brejeira (1.73–1.37 Ga) formations indicate inverted stratigraphy for their isotopic sources. The isotope geochemical data indicate significant changes in the sources from which the SPZ Carboniferous turbidites are derived, consistent with the progressive denudation of a continental magmatic arc built on the Laurussian margin. Mértola turbidites inherited their geochemical and isotopic characteristics from an adjacent dissected Middle–Late Devonian continental magmatic arc with an intermediate–felsic composition: that is a Laurussian (Rheic magmatic arc)-type source. The progressive erosion of its plutonic roots and older host continental basement rocks are indicated in the Mira and Brejeira formations by the increasing contribution of recycled ancient continental crust. The pronounced similarity between the Nd TDM model ages and the detrital zircon populations of the Mira and Brejeira formations (SW Iberia) suggest that they share a common Laurussian (West Avalonia/Meguma terrane)-type source but a contribution from Gondwanan (Ossa-Morena)- type sources cannot be discarded.The Geological society of London2022-11-17T16:29:23Z2022-11-172020-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10174/32765http://hdl.handle.net/10174/32765https://doi.org/10.1144/SP503-2019-163engPEREIRA, M.F., Gama, C., Dias da Silva, Í., Fuenlabrada, J.M., Silva, J.B., Medina, J. (2020). Isotope geochemistry evidence for Laurussian-type sources of South-Portuguese Zone Carboniferous turbidites (Variscan orogeny). In: Pannotia to Pangea: Neoproterozoic and Paleozoic orogenic cycles in the circum-North Atlantic region (eds) J.B. Murphy, R.A. Strachan, C., Quesada. GEOLOGICAL SOCIETY OF LONDON SPECIAL PUBLICATIONS, 503.ndndndndndnd250Pereira, M.F.Gama, C.Dias da Silva, I.Fuenlabrada, J.M.Silva, J.B.Medina, J.info: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:RCAAP2024-01-03T19:33:23Zoai:dspace.uevora.pt:10174/32765Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:21:31.956639Repositório 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 Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
title Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
spellingShingle Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
Pereira, M.F.
Rb-Sr - Sm-Nd isotopes
Carboniferous flysch
South-Portuguese Zone
SW Iberia
title_short Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
title_full Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
title_fullStr Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
title_full_unstemmed Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
title_sort Isotope geochemistry evidence for Laurussian-type sources of South Portuguese Zone Carboniferous turbidites (Variscan Orogeny)
author Pereira, M.F.
author_facet Pereira, M.F.
Gama, C.
Dias da Silva, I.
Fuenlabrada, J.M.
Silva, J.B.
Medina, J.
author_role author
author2 Gama, C.
Dias da Silva, I.
Fuenlabrada, J.M.
Silva, J.B.
Medina, J.
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Pereira, M.F.
Gama, C.
Dias da Silva, I.
Fuenlabrada, J.M.
Silva, J.B.
Medina, J.
dc.subject.por.fl_str_mv Rb-Sr - Sm-Nd isotopes
Carboniferous flysch
South-Portuguese Zone
SW Iberia
topic Rb-Sr - Sm-Nd isotopes
Carboniferous flysch
South-Portuguese Zone
SW Iberia
description New Rb–Sr isotopic data from South Portuguese Zone (SPZ) turbidites show that the 87Sr/86Sr(t) ratio increases from the basal Mértola Formation (Visean–Serpukhovian: 0.706–0.707), through the Mira Formation (Serpukhovian–Bashkirian: 0.706–0.712) to the uppermost Brejeira Formation (Bashkirian– Moscovian: 0.713–0.715). In addition, estimated Nd TDM model ages for the Mértola (1.29–1.09 Ga), Mira (1.58–1.1 Ga) and Brejeira (1.73–1.37 Ga) formations indicate inverted stratigraphy for their isotopic sources. The isotope geochemical data indicate significant changes in the sources from which the SPZ Carboniferous turbidites are derived, consistent with the progressive denudation of a continental magmatic arc built on the Laurussian margin. Mértola turbidites inherited their geochemical and isotopic characteristics from an adjacent dissected Middle–Late Devonian continental magmatic arc with an intermediate–felsic composition: that is a Laurussian (Rheic magmatic arc)-type source. The progressive erosion of its plutonic roots and older host continental basement rocks are indicated in the Mira and Brejeira formations by the increasing contribution of recycled ancient continental crust. The pronounced similarity between the Nd TDM model ages and the detrital zircon populations of the Mira and Brejeira formations (SW Iberia) suggest that they share a common Laurussian (West Avalonia/Meguma terrane)-type source but a contribution from Gondwanan (Ossa-Morena)- type sources cannot be discarded.
publishDate 2020
dc.date.none.fl_str_mv 2020-01-01T00:00:00Z
2022-11-17T16:29:23Z
2022-11-17
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/10174/32765
http://hdl.handle.net/10174/32765
https://doi.org/10.1144/SP503-2019-163
url http://hdl.handle.net/10174/32765
https://doi.org/10.1144/SP503-2019-163
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv PEREIRA, M.F., Gama, C., Dias da Silva, Í., Fuenlabrada, J.M., Silva, J.B., Medina, J. (2020). Isotope geochemistry evidence for Laurussian-type sources of South-Portuguese Zone Carboniferous turbidites (Variscan orogeny). In: Pannotia to Pangea: Neoproterozoic and Paleozoic orogenic cycles in the circum-North Atlantic region (eds) J.B. Murphy, R.A. Strachan, C., Quesada. GEOLOGICAL SOCIETY OF LONDON SPECIAL PUBLICATIONS, 503.
nd
nd
nd
nd
nd
nd
250
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv The Geological society of London
publisher.none.fl_str_mv The Geological society of London
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)
repository.name.fl_str_mv Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
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