Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components.
Identifieur interne : 001094 ( PubMed/Checkpoint ); précédent : 001093; suivant : 001095Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components.
Auteurs : Roman Golowin [Allemagne] ; Maxim Portnyagin [Allemagne] ; Kaj Hoernle [Allemagne] ; Folkmar Hauff [Allemagne] ; Andrey Gurenko [France] ; Dieter Garbe-Schönberg [Allemagne] ; Reinhard Werner [Allemagne] ; Simon Turner [Australie]Source :
- Nature communications [ 2041-1723 ] ; 2017.
Abstract
The Ontong Java and Manihiki oceanic plateaus are believed to have formed through high-degree melting of a mantle plume head. Boninite-like, low-Ti basement rocks at Manihiki, however, imply a more complex magma genesis compared with Ontong Java basement lavas that can be generated by ∼30% melting of a primitive mantle source. Here we show that the trace element and isotope compositions of low-Ti Manihiki rocks can best be explained by re-melting of an ultra-depleted source (possibly a common mantle component in the Ontong Java and Manihiki plume sources) re-enriched by ≤1% of an ocean-island-basalt-like melt component. Unlike boninites formed via hydrous flux melting of refractory mantle at subduction zones, these boninite-like intraplate rocks formed through adiabatic decompression melting of refractory plume material that has been metasomatized by ocean-island-basalt-like melts. Our results suggest that caution is required before assuming all Archaean boninites were formed in association with subduction processes.
DOI: 10.1038/ncomms14322
PubMed: 28181497
Affiliations:
- Allemagne, Australie, France
- Grand Est, Lorraine (région), Schleswig-Holstein
- Kiel, Metz, Nancy
- Université de Lorraine
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sort="Werner, Reinhard" uniqKey="Werner R" first="Reinhard" last="Werner">Reinhard Werner</name><affiliation wicri:level="3"><nlm:affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</nlm:affiliation><country xml:lang="fr">Allemagne</country><wicri:regionArea>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel</wicri:regionArea><placeName><region type="land" nuts="2">Schleswig-Holstein</region><settlement type="city">Kiel</settlement></placeName></affiliation></author><author><name sortKey="Turner, Simon" sort="Turner, Simon" uniqKey="Turner S" first="Simon" last="Turner">Simon Turner</name><affiliation wicri:level="1"><nlm:affiliation>Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109</wicri:regionArea><wicri:noRegion>New South Wales 2109</wicri:noRegion></affiliation></author></analytic><series><title level="j">Nature communications</title><idno type="eISSN">2041-1723</idno><imprint><date when="2017" type="published">2017</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The Ontong Java and Manihiki oceanic plateaus are believed to have formed through high-degree melting of a mantle plume head. Boninite-like, low-Ti basement rocks at Manihiki, however, imply a more complex magma genesis compared with Ontong Java basement lavas that can be generated by ∼30% melting of a primitive mantle source. Here we show that the trace element and isotope compositions of low-Ti Manihiki rocks can best be explained by re-melting of an ultra-depleted source (possibly a common mantle component in the Ontong Java and Manihiki plume sources) re-enriched by ≤1% of an ocean-island-basalt-like melt component. Unlike boninites formed via hydrous flux melting of refractory mantle at subduction zones, these boninite-like intraplate rocks formed through adiabatic decompression melting of refractory plume material that has been metasomatized by ocean-island-basalt-like melts. Our results suggest that caution is required before assuming all Archaean boninites were formed in association with subduction processes.</div></front></TEI><pubmed><MedlineCitation Status="In-Data-Review" Owner="NLM"><PMID Version="1">28181497</PMID><DateCreated><Year>2017</Year><Month>02</Month><Day>09</Day></DateCreated><DateRevised><Year>2017</Year><Month>02</Month><Day>28</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2041-1723</ISSN><JournalIssue CitedMedium="Internet"><Volume>8</Volume><PubDate><Year>2017</Year><Month>Feb</Month><Day>09</Day></PubDate></JournalIssue><Title>Nature communications</Title><ISOAbbreviation>Nat Commun</ISOAbbreviation></Journal><ArticleTitle>Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components.</ArticleTitle><Pagination><MedlinePgn>14322</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/ncomms14322</ELocationID><Abstract><AbstractText>The Ontong Java and Manihiki oceanic plateaus are believed to have formed through high-degree melting of a mantle plume head. Boninite-like, low-Ti basement rocks at Manihiki, however, imply a more complex magma genesis compared with Ontong Java basement lavas that can be generated by ∼30% melting of a primitive mantle source. Here we show that the trace element and isotope compositions of low-Ti Manihiki rocks can best be explained by re-melting of an ultra-depleted source (possibly a common mantle component in the Ontong Java and Manihiki plume sources) re-enriched by ≤1% of an ocean-island-basalt-like melt component. Unlike boninites formed via hydrous flux melting of refractory mantle at subduction zones, these boninite-like intraplate rocks formed through adiabatic decompression melting of refractory plume material that has been metasomatized by ocean-island-basalt-like melts. Our results suggest that caution is required before assuming all Archaean boninites were formed in association with subduction processes.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Golowin</LastName><ForeName>Roman</ForeName><Initials>R</Initials><AffiliationInfo><Affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Portnyagin</LastName><ForeName>Maxim</ForeName><Initials>M</Initials><AffiliationInfo><Affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>V.I.Vernadsky Institute of Geochemistry and Analytical Chemistry, Kosigin street 19, Moscow 119991, Russia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hoernle</LastName><ForeName>Kaj</ForeName><Initials>K</Initials><Identifier Source="ORCID">http://orcid.org/0000-0002-3165-3480</Identifier><AffiliationInfo><Affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Christian-Albrechts-University of Kiel, Ludewig-Meyn-Strasse 10, 24118 Kiel, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hauff</LastName><ForeName>Folkmar</ForeName><Initials>F</Initials><AffiliationInfo><Affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Gurenko</LastName><ForeName>Andrey</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Centre de Recherches Pétrographiques et Géochimiques, UMR 7358, Université de Lorraine, 54501 Vandoeuvre-lès-Nancy, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Garbe-Schönberg</LastName><ForeName>Dieter</ForeName><Initials>D</Initials><AffiliationInfo><Affiliation>Christian-Albrechts-University of Kiel, Ludewig-Meyn-Strasse 10, 24118 Kiel, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Werner</LastName><ForeName>Reinhard</ForeName><Initials>R</Initials><AffiliationInfo><Affiliation>GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Turner</LastName><ForeName>Simon</ForeName><Initials>S</Initials><AffiliationInfo><Affiliation>Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2017</Year><Month>02</Month><Day>09</Day></ArticleDate></Article><MedlineJournalInfo><Country>England</Country><MedlineTA>Nat Commun</MedlineTA><NlmUniqueID>101528555</NlmUniqueID><ISSNLinking>2041-1723</ISSNLinking></MedlineJournalInfo><CommentsCorrectionsList><CommentsCorrections RefType="Cites"><RefSource>Nature. 2008 Feb 28;451(7182):1094-7</RefSource><PMID Version="1">18223639</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2007 Jun 28;447(7148):1069-74</RefSource><PMID Version="1">17597754</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2016 Mar 31;531(7596):628-32</RefSource><PMID Version="1">27029278</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2002 Nov 28;420(6914):385-9</RefSource><PMID Version="1">12459776</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 1989 Oct 6;246(4926):103-7</RefSource><PMID Version="1">17837768</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2011 Jul 27;476(7360):316-9</RefSource><PMID Version="1">21796117</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nat Commun. 2015 Apr 24;6:6960</RefSource><PMID Version="1">25907970</PMID></CommentsCorrections></CommentsCorrectionsList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2015</Year><Month>09</Month><Day>18</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2016</Year><Month>12</Month><Day>16</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2017</Year><Month>2</Month><Day>10</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2017</Year><Month>2</Month><Day>10</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate 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uniqKey="Garbe Schonberg D" first="Dieter" last="Garbe-Schönberg">Dieter Garbe-Schönberg</name><name sortKey="Hauff, Folkmar" sort="Hauff, Folkmar" uniqKey="Hauff F" first="Folkmar" last="Hauff">Folkmar Hauff</name><name sortKey="Hoernle, Kaj" sort="Hoernle, Kaj" uniqKey="Hoernle K" first="Kaj" last="Hoernle">Kaj Hoernle</name><name sortKey="Portnyagin, Maxim" sort="Portnyagin, Maxim" uniqKey="Portnyagin M" first="Maxim" last="Portnyagin">Maxim Portnyagin</name><name sortKey="Werner, Reinhard" sort="Werner, Reinhard" uniqKey="Werner R" first="Reinhard" last="Werner">Reinhard Werner</name></country><country name="France"><region name="Grand Est"><name sortKey="Gurenko, Andrey" sort="Gurenko, Andrey" uniqKey="Gurenko A" first="Andrey" last="Gurenko">Andrey Gurenko</name></region></country><country name="Australie"><noRegion><name sortKey="Turner, Simon" sort="Turner, Simon" uniqKey="Turner S" first="Simon" last="Turner">Simon 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