Molybdenum isotope systematics in subduction zones
This study presents Mo isotope data for arc lavas from different subduction zones that range between δ98/95Mo=−0.72 and +0.07‰. Heaviest isotope values are observed for the most slab fluid dominated samples. Isotopically lighter signatures are related to increasing relevance of terrigenous sediment...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2016 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/414671 |
| Acceso en línea: | http://hdl.handle.net/10261/414671 https://doi.org/10.1016/j.epsl.2016.04.033 |
| Access Level: | acceso abierto |
| Palabra clave: | Mo isotopes Molybdenum Subduction Arc Slab fluid Sediments |
| id |
ES_c6d1a76273b08e55fb76e2fe7a5ea66a |
|---|---|
| oai_identifier_str |
oai:digital.csic.es:10261/414671 |
| network_acronym_str |
ES |
| network_name_str |
España |
| repository_id_str |
|
| spelling |
Molybdenum isotope systematics in subduction zonesKönig, StephanWille, MartinVoegelin, AndreaSchoenberg, RonnyMo isotopesMolybdenumSubductionArcSlab fluidSedimentsThis study presents Mo isotope data for arc lavas from different subduction zones that range between δ98/95Mo=−0.72 and +0.07‰. Heaviest isotope values are observed for the most slab fluid dominated samples. Isotopically lighter signatures are related to increasing relevance of terrigenous sediment subduction and sediment melt components. Our observation complements previous conclusions that an isotopically heavy Mo fluid flux likely mirrors selective incorporation of isotopically light Mo in secondary minerals within the subducting slab. Analogue to this interpretation, low δ98/95Mo flux that coincides with terrigenous sediment subduction and sediment melting cannot be simply related to a recycled input signature. Instead, breakdown of the controlling secondary minerals during sediment melting may release the light component and lead to decreasing δ98/95Mo influx into subarc mantle sources. The natural range between slab dehydration and hydrous sediment melting may thus cause a large spread of δ98/95Mo in global subduction zone magmas.S.K. acknowledges a Starting Grant of the European Research Council (ERC STG O2RIGIN ). M.W. is supported by grant WI3870/2-1 from the Deutsche Forschungsgemeinschaft (DFG). The DFG is also thanked for funding sampling campaigns through Mu 1406/2 and Mu 1406/7.Peer reviewedElsevier BVEuropean Research CouncilEuropean CommissionGerman Research FoundationConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202620262016info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/414671https://doi.org/10.1016/j.epsl.2016.04.033reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/EC/H2020/636808https://doi.org/10.1016/j.epsl.2016.04.033Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/4146712026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Molybdenum isotope systematics in subduction zones |
| title |
Molybdenum isotope systematics in subduction zones |
| spellingShingle |
Molybdenum isotope systematics in subduction zones König, Stephan Mo isotopes Molybdenum Subduction Arc Slab fluid Sediments |
| title_short |
Molybdenum isotope systematics in subduction zones |
| title_full |
Molybdenum isotope systematics in subduction zones |
| title_fullStr |
Molybdenum isotope systematics in subduction zones |
| title_full_unstemmed |
Molybdenum isotope systematics in subduction zones |
| title_sort |
Molybdenum isotope systematics in subduction zones |
| dc.creator.none.fl_str_mv |
König, Stephan Wille, Martin Voegelin, Andrea Schoenberg, Ronny |
| author |
König, Stephan |
| author_facet |
König, Stephan Wille, Martin Voegelin, Andrea Schoenberg, Ronny |
| author_role |
author |
| author2 |
Wille, Martin Voegelin, Andrea Schoenberg, Ronny |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
European Research Council European Commission German Research Foundation Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Mo isotopes Molybdenum Subduction Arc Slab fluid Sediments |
| topic |
Mo isotopes Molybdenum Subduction Arc Slab fluid Sediments |
| description |
This study presents Mo isotope data for arc lavas from different subduction zones that range between δ98/95Mo=−0.72 and +0.07‰. Heaviest isotope values are observed for the most slab fluid dominated samples. Isotopically lighter signatures are related to increasing relevance of terrigenous sediment subduction and sediment melt components. Our observation complements previous conclusions that an isotopically heavy Mo fluid flux likely mirrors selective incorporation of isotopically light Mo in secondary minerals within the subducting slab. Analogue to this interpretation, low δ98/95Mo flux that coincides with terrigenous sediment subduction and sediment melting cannot be simply related to a recycled input signature. Instead, breakdown of the controlling secondary minerals during sediment melting may release the light component and lead to decreasing δ98/95Mo influx into subarc mantle sources. The natural range between slab dehydration and hydrous sediment melting may thus cause a large spread of δ98/95Mo in global subduction zone magmas. |
| publishDate |
2016 |
| dc.date.none.fl_str_mv |
2016 2026 2026 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/414671 https://doi.org/10.1016/j.epsl.2016.04.033 |
| url |
http://hdl.handle.net/10261/414671 https://doi.org/10.1016/j.epsl.2016.04.033 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/H2020/636808 https://doi.org/10.1016/j.epsl.2016.04.033 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
Elsevier BV |
| publisher.none.fl_str_mv |
Elsevier BV |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
| reponame_str |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| collection |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
| _version_ |
1869419104973094912 |
| score |
15.81155 |