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Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data

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Resumo:This work addresses the present-day (<100 ka) mantle heterogeneity in the Azores region through the study of two active volcanic systems from Terceira Island. Our study shows that mantle heterogeneities are detectable even when "coeval" volcanic systems (Santa Barbara and Fissural) erupted less than 10 km away. These volcanic systems, respectively, reflect the influence of the Terceira and D. Joao de Castro Bank end-members defined by Beier et at (2008) for the Terceira Rift Santa Barbara magmas are interpreted to be the result of mixing between a HIMU-type component, carried to the upper mantle by the Azores plume, and the regional depleted MORB magmas/source. Fissural lavas are characterized by higher Ba/Nb and Nb/U ratios and less radiogenic Pb-206/Pb-204, Nd-143/Nd-144 and Hf-176/Hf-177, requiring the small contribution of delaminated sub-continental lithospheric mantle residing in the upper mantle. Published noble gas data on lavas from both volcanic systems also indicate the presence of a relatively undegassed component, which is interpreted as inherited from a lower mantle reservoir sampled by the ascending Azores plume. As inferred from trace and major elements, melting began in the garnet stability field, while magma extraction occurred within the spinel zone. The intra-volcanic system's chemical heterogeneity is mainly explained by variable proportions of the above-mentioned local end-members and by crystal fractionation processes.
Autores principais:Madureira, Pedro
Outros Autores:Mata, João; Mattielli, Nadine; Queiroz, Gabriela; Silva, Pedro
Assunto:Ocean island basalts Small-scale mantle heterogeneity Terceira Island Azores
Ano:2011
País:Portugal
Tipo de documento:artigo
Tipo de acesso:acesso aberto
Instituição associada:Instituto Politécnico de Lisboa
Idioma:inglês
Origem:Repositório Científico do Instituto Politécnico de Lisboa
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author Madureira, Pedro
author2 Mata, João
Mattielli, Nadine
Queiroz, Gabriela
Silva, Pedro
author2_role author
author
author
author
author_facet Madureira, Pedro
Mata, João
Mattielli, Nadine
Queiroz, Gabriela
Silva, Pedro
author_role author
contributor_name_str_mv RCIPL
country_str PT
creators_json_txt [{\"Person.name\":\"Madureira, Pedro\"},{\"Person.name\":\"Mata, João\",\"Person.identifier.orcid\":\"0000-0001-5769-7708\"},{\"Person.name\":\"Mattielli, Nadine\",\"Person.identifier.orcid\":\"0000-0002-7170-1520\"},{\"Person.name\":\"Queiroz, Gabriela\"},{\"Person.name\":\"Silva, Pedro\",\"Person.identifier.orcid\":\"0000-0002-9178-3623\"}]
datacite.contributors.contributor.contributorName.fl_str_mv RCIPL
datacite.creators.creator.creatorName.fl_str_mv Madureira, Pedro
Mata, João
Mattielli, Nadine
Queiroz, Gabriela
Silva, Pedro
datacite.date.Accepted.fl_str_mv 2011-10-01T00:00:00Z
datacite.date.available.fl_str_mv 2013-02-15T16:18:19Z
datacite.date.embargoed.fl_str_mv 2013-02-15T16:18:19Z
datacite.rights.fl_str_mv http://purl.org/coar/access_right/c_abf2
datacite.subjects.subject.fl_str_mv Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
datacite.titles.title.fl_str_mv Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
dc.contributor.none.fl_str_mv RCIPL
dc.creator.none.fl_str_mv Madureira, Pedro
Mata, João
Mattielli, Nadine
Queiroz, Gabriela
Silva, Pedro
dc.date.Accepted.fl_str_mv 2011-10-01T00:00:00Z
dc.date.available.fl_str_mv 2013-02-15T16:18:19Z
dc.date.embargoed.fl_str_mv 2013-02-15T16:18:19Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv http://hdl.handle.net/10400.21/2211
dc.language.none.fl_str_mv eng
dc.publisher.none.fl_str_mv Elsevier
dc.rights.none.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.subject.none.fl_str_mv Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
dc.title.fl_str_mv Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
dc.type.none.fl_str_mv http://purl.org/coar/resource_type/c_6501
description This work addresses the present-day (<100 ka) mantle heterogeneity in the Azores region through the study of two active volcanic systems from Terceira Island. Our study shows that mantle heterogeneities are detectable even when "coeval" volcanic systems (Santa Barbara and Fissural) erupted less than 10 km away. These volcanic systems, respectively, reflect the influence of the Terceira and D. Joao de Castro Bank end-members defined by Beier et at (2008) for the Terceira Rift Santa Barbara magmas are interpreted to be the result of mixing between a HIMU-type component, carried to the upper mantle by the Azores plume, and the regional depleted MORB magmas/source. Fissural lavas are characterized by higher Ba/Nb and Nb/U ratios and less radiogenic Pb-206/Pb-204, Nd-143/Nd-144 and Hf-176/Hf-177, requiring the small contribution of delaminated sub-continental lithospheric mantle residing in the upper mantle. Published noble gas data on lavas from both volcanic systems also indicate the presence of a relatively undegassed component, which is interpreted as inherited from a lower mantle reservoir sampled by the ascending Azores plume. As inferred from trace and major elements, melting began in the garnet stability field, while magma extraction occurred within the spinel zone. The intra-volcanic system's chemical heterogeneity is mainly explained by variable proportions of the above-mentioned local end-members and by crystal fractionation processes.
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eu_rights_str_mv openAccess
format article
fulltext.url.fl_str_mv https://repositorio.ipl.pt/bitstreams/6f0029fd-227d-4658-8a04-35441f7475f9/download
id ripl_ff4d673d7ffce7280b398b7397fa6aec
identifier.url.fl_str_mv http://hdl.handle.net/10400.21/2211
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institution Instituto Politécnico de Lisboa
instname_str Instituto Politécnico de Lisboa
language eng
network_acronym_str ripl
network_name_str Repositório Científico do Instituto Politécnico de Lisboa
oai_identifier_str oai:repositorio.ipl.pt:10400.21/2211
organization_str_mv urn:organizationAcronym:ipl
person_str_mv Madureira, Pedro
Mata, João
Mata, João
https://www.ciencia-id.pt/4312-8A60-15E3
4312-8A60-15E3
http://orcid.org/0000-0001-5769-7708
0000-0001-5769-7708
Mattielli, Nadine
Mattielli, Nadine
http://orcid.org/0000-0002-7170-1520
0000-0002-7170-1520
Queiroz, Gabriela
Silva, Pedro
Silva, Pedro
https://www.ciencia-id.pt/C314-1157-FD0C
C314-1157-FD0C
http://orcid.org/0000-0002-9178-3623
0000-0002-9178-3623
publishDate 2011
publisher.none.fl_str_mv Elsevier
reponame_str Repositório Científico do Instituto Politécnico de Lisboa
repository_id_str urn:repositoryAcronym:ripl
service_str_mv urn:repositoryAcronym:ripl
spelling engElsevierporThis work addresses the present-day (<100 ka) mantle heterogeneity in the Azores region through the study of two active volcanic systems from Terceira Island. Our study shows that mantle heterogeneities are detectable even when "coeval" volcanic systems (Santa Barbara and Fissural) erupted less than 10 km away. These volcanic systems, respectively, reflect the influence of the Terceira and D. Joao de Castro Bank end-members defined by Beier et at (2008) for the Terceira Rift Santa Barbara magmas are interpreted to be the result of mixing between a HIMU-type component, carried to the upper mantle by the Azores plume, and the regional depleted MORB magmas/source. Fissural lavas are characterized by higher Ba/Nb and Nb/U ratios and less radiogenic Pb-206/Pb-204, Nd-143/Nd-144 and Hf-176/Hf-177, requiring the small contribution of delaminated sub-continental lithospheric mantle residing in the upper mantle. Published noble gas data on lavas from both volcanic systems also indicate the presence of a relatively undegassed component, which is interpreted as inherited from a lower mantle reservoir sampled by the ascending Azores plume. As inferred from trace and major elements, melting began in the garnet stability field, while magma extraction occurred within the spinel zone. The intra-volcanic system's chemical heterogeneity is mainly explained by variable proportions of the above-mentioned local end-members and by crystal fractionation processes.application/pdfporMantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) dataMadureira, PedroPersonalMata, JoãoDSpacehttp://dspace.org/items/7be0beb3-e47d-4ff0-befa-01dd05c93942DSpacehttp://dspace.org/items/7be0beb3-e47d-4ff0-befa-01dd05c93942MataJoãoCiência IDhttps://www.ciencia-id.pt4312-8A60-15E3ORCIDhttp://orcid.org0000-0001-5769-7708Researcher IDhttps://www.researcherid.comI-3352-2012Scopus Author IDhttps://www.scopus.com7102806167PersonalMattielli, NadineDSpacehttp://dspace.org/items/c370049a-3a1a-45c2-842a-82df39aea180DSpacehttp://dspace.org/items/c370049a-3a1a-45c2-842a-82df39aea180MattielliNadineORCIDhttp://orcid.org0000-0002-7170-1520Queiroz, GabrielaPersonalSilva, PedroDSpacehttp://dspace.org/items/54c96e27-8c3a-42d9-b751-ebc637c2f478DSpacehttp://dspace.org/items/54c96e27-8c3a-42d9-b751-ebc637c2f478SilvaPedroCiência IDhttps://www.ciencia-id.ptC314-1157-FD0CORCIDhttp://orcid.org0000-0002-9178-3623Researcher IDhttps://www.researcherid.comB-8512-2008Scopus Author IDhttps://www.scopus.com55431034700HostingInstitutionOrganizationalRCIPLe-mailmailto:rcaap@sp.ipl.ptrcaap@sp.ipl.ptISSNIsPartOf0024-4937DOIIsPartOf10.1016/j.lithos.2011.07.0022013-02-15T16:18:19Z2011-102011-10-01T00:00:00ZHandlehttp://hdl.handle.net/10400.21/2211http://purl.org/coar/access_right/c_abf2open accessOcean island basaltsSmall-scale mantle heterogeneityTerceira IslandAzores2642378 bytesliteraturehttp://purl.org/coar/resource_type/c_6501journal articlehttp://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://repositorio.ipl.pt/bitstreams/6f0029fd-227d-4658-8a04-35441f7475f9/downloadLithos1263-4402418Amsterdam
spellingShingle Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
Madureira, Pedro
Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
status SINGLETON
subject.fl_str_mv Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
title Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
title_full Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
title_fullStr Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
title_full_unstemmed Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
title_short Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
title_sort Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data
topic Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
topic_facet Ocean island basalts
Small-scale mantle heterogeneity
Terceira Island
Azores
url http://hdl.handle.net/10400.21/2211
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