Plume-subduction interaction forms large auriferous provinces.
Identifieur interne : 000381 ( PubMed/Curation ); précédent : 000380; suivant : 000382Plume-subduction interaction forms large auriferous provinces.
Auteurs : Santiago Tassara [Chili] ; José M. González-Jiménez [Chili] ; Martin Reich [Chili] ; Manuel E. Schilling [Chili] ; Diego Morata [Chili] ; Graham Begg [Australie] ; Edward Saunders [Australie] ; William L. Griffin [Australie] ; Suzanne Y. O'Reilly [Australie] ; Michel Grégoire [France] ; Fernando Barra [Chili] ; Alexandre Corgne [Chili]Source :
- Nature communications [ 2041-1723 ] ; 2017.
Abstract
Gold enrichment at the crustal or mantle source has been proposed as a key ingredient in the production of giant gold deposits and districts. However, the lithospheric-scale processes controlling gold endowment in a given metallogenic province remain unclear. Here we provide the first direct evidence of native gold in the mantle beneath the Deseado Massif in Patagonia that links an enriched mantle source to the occurrence of a large auriferous province in the overlying crust. A precursor stage of mantle refertilisation by plume-derived melts generated a gold-rich mantle source during the Early Jurassic. The interplay of this enriched mantle domain and subduction-related fluids released during the Middle-Late Jurassic resulted in optimal conditions to produce the ore-forming magmas that generated the gold deposits. Our study highlights that refertilisation of the subcontinental lithospheric mantle is a key factor in forming large metallogenic provinces in the Earth's crust, thus providing an alternative view to current crust-related enrichment models.The lithospheric controls on giant gold deposits remain unclear. Here, the authors show evidence for native gold in the mantle from the Deseado Massif in Patagonia demonstrating that refertilisation of the lithospheric mantle is key in forming metallogenic provinces.
DOI: 10.1038/s41467-017-00821-z
PubMed: 29018198
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González-Jiménez</name><affiliation wicri:level="1"><nlm:affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450</wicri:regionArea></affiliation></author><author><name sortKey="Reich, Martin" sort="Reich, Martin" uniqKey="Reich M" first="Martin" last="Reich">Martin Reich</name><affiliation wicri:level="1"><nlm:affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450</wicri:regionArea></affiliation></author><author><name sortKey="Schilling, Manuel E" sort="Schilling, Manuel E" uniqKey="Schilling M" first="Manuel E" last="Schilling">Manuel E. Schilling</name><affiliation wicri:level="1"><nlm:affiliation>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000</wicri:regionArea></affiliation></author><author><name sortKey="Morata, Diego" sort="Morata, Diego" uniqKey="Morata D" first="Diego" last="Morata">Diego Morata</name><affiliation wicri:level="1"><nlm:affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450</wicri:regionArea></affiliation></author><author><name sortKey="Begg, Graham" sort="Begg, Graham" uniqKey="Begg G" first="Graham" last="Begg">Graham Begg</name><affiliation wicri:level="1"><nlm:affiliation>Minerals Targeting International PL, 17 Prowse Street, West Perth, WA, 6005, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Minerals Targeting International PL, 17 Prowse Street, West Perth, WA, 6005</wicri:regionArea></affiliation></author><author><name sortKey="Saunders, Edward" sort="Saunders, Edward" uniqKey="Saunders E" first="Edward" last="Saunders">Edward Saunders</name><affiliation wicri:level="1"><nlm:affiliation>Division of Earth Sciences, School of Environmental and Rural Science, University of New England, Armidale, NSW, 2351, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Division of Earth Sciences, School of Environmental and Rural Science, University of New England, Armidale, NSW, 2351</wicri:regionArea></affiliation></author><author><name sortKey="Griffin, William L" sort="Griffin, William L" uniqKey="Griffin W" first="William L" last="Griffin">William L. Griffin</name><affiliation wicri:level="1"><nlm:affiliation>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109</wicri:regionArea></affiliation></author><author><name sortKey="O Reilly, Suzanne Y" sort="O Reilly, Suzanne Y" uniqKey="O Reilly S" first="Suzanne Y" last="O'Reilly">Suzanne Y. O'Reilly</name><affiliation wicri:level="1"><nlm:affiliation>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109</wicri:regionArea></affiliation></author><author><name sortKey="Gregoire, Michel" sort="Gregoire, Michel" uniqKey="Gregoire M" first="Michel" last="Grégoire">Michel Grégoire</name><affiliation wicri:level="1"><nlm:affiliation>GET, CNRS-CNES-IRD-UPS, Toulouse University, 14 Avenue Edouard Belin, 31200, Toulouse, France.</nlm:affiliation><country xml:lang="fr">France</country><wicri:regionArea>GET, CNRS-CNES-IRD-UPS, Toulouse University, 14 Avenue Edouard Belin, 31200, Toulouse</wicri:regionArea></affiliation></author><author><name sortKey="Barra, Fernando" sort="Barra, Fernando" uniqKey="Barra F" first="Fernando" last="Barra">Fernando Barra</name><affiliation wicri:level="1"><nlm:affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450</wicri:regionArea></affiliation></author><author><name sortKey="Corgne, Alexandre" sort="Corgne, Alexandre" uniqKey="Corgne A" first="Alexandre" last="Corgne">Alexandre Corgne</name><affiliation wicri:level="1"><nlm:affiliation>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000, Chile.</nlm:affiliation><country xml:lang="fr">Chili</country><wicri:regionArea>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000</wicri:regionArea></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">Gold enrichment at the crustal or mantle source has been proposed as a key ingredient in the production of giant gold deposits and districts. However, the lithospheric-scale processes controlling gold endowment in a given metallogenic province remain unclear. Here we provide the first direct evidence of native gold in the mantle beneath the Deseado Massif in Patagonia that links an enriched mantle source to the occurrence of a large auriferous province in the overlying crust. A precursor stage of mantle refertilisation by plume-derived melts generated a gold-rich mantle source during the Early Jurassic. The interplay of this enriched mantle domain and subduction-related fluids released during the Middle-Late Jurassic resulted in optimal conditions to produce the ore-forming magmas that generated the gold deposits. Our study highlights that refertilisation of the subcontinental lithospheric mantle is a key factor in forming large metallogenic provinces in the Earth's crust, thus providing an alternative view to current crust-related enrichment models.The lithospheric controls on giant gold deposits remain unclear. Here, the authors show evidence for native gold in the mantle from the Deseado Massif in Patagonia demonstrating that refertilisation of the lithospheric mantle is key in forming metallogenic provinces.</div></front></TEI><pubmed><MedlineCitation Status="In-Data-Review" Owner="NLM"><PMID Version="1">29018198</PMID><DateCreated><Year>2017</Year><Month>10</Month><Day>11</Day></DateCreated><DateRevised><Year>2017</Year><Month>10</Month><Day>13</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2041-1723</ISSN><JournalIssue CitedMedium="Internet"><Volume>8</Volume><Issue>1</Issue><PubDate><Year>2017</Year><Month>Oct</Month><Day>10</Day></PubDate></JournalIssue><Title>Nature communications</Title><ISOAbbreviation>Nat Commun</ISOAbbreviation></Journal><ArticleTitle>Plume-subduction interaction forms large auriferous provinces.</ArticleTitle><Pagination><MedlinePgn>843</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/s41467-017-00821-z</ELocationID><Abstract><AbstractText>Gold enrichment at the crustal or mantle source has been proposed as a key ingredient in the production of giant gold deposits and districts. However, the lithospheric-scale processes controlling gold endowment in a given metallogenic province remain unclear. Here we provide the first direct evidence of native gold in the mantle beneath the Deseado Massif in Patagonia that links an enriched mantle source to the occurrence of a large auriferous province in the overlying crust. A precursor stage of mantle refertilisation by plume-derived melts generated a gold-rich mantle source during the Early Jurassic. The interplay of this enriched mantle domain and subduction-related fluids released during the Middle-Late Jurassic resulted in optimal conditions to produce the ore-forming magmas that generated the gold deposits. Our study highlights that refertilisation of the subcontinental lithospheric mantle is a key factor in forming large metallogenic provinces in the Earth's crust, thus providing an alternative view to current crust-related enrichment models.The lithospheric controls on giant gold deposits remain unclear. Here, the authors show evidence for native gold in the mantle from the Deseado Massif in Patagonia demonstrating that refertilisation of the lithospheric mantle is key in forming metallogenic provinces.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Tassara</LastName><ForeName>Santiago</ForeName><Initials>S</Initials><Identifier Source="ORCID">http://orcid.org/0000-0001-7697-5646</Identifier><AffiliationInfo><Affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile. tassara.carlos.sant@ug.uchile.cl.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>González-Jiménez</LastName><ForeName>José M</ForeName><Initials>JM</Initials><AffiliationInfo><Affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Fuentenueva s/n, 180002, Granada, Spain.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Reich</LastName><ForeName>Martin</ForeName><Initials>M</Initials><AffiliationInfo><Affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Schilling</LastName><ForeName>Manuel E</ForeName><Initials>ME</Initials><AffiliationInfo><Affiliation>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000, Chile.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Morata</LastName><ForeName>Diego</ForeName><Initials>D</Initials><AffiliationInfo><Affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Begg</LastName><ForeName>Graham</ForeName><Initials>G</Initials><AffiliationInfo><Affiliation>Minerals Targeting International PL, 17 Prowse Street, West Perth, WA, 6005, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Saunders</LastName><ForeName>Edward</ForeName><Initials>E</Initials><AffiliationInfo><Affiliation>Division of Earth Sciences, School of Environmental and Rural Science, University of New England, Armidale, NSW, 2351, Australia.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Griffin</LastName><ForeName>William L</ForeName><Initials>WL</Initials><AffiliationInfo><Affiliation>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>O'Reilly</LastName><ForeName>Suzanne Y</ForeName><Initials>SY</Initials><AffiliationInfo><Affiliation>ARC Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Sydney, NSW, 2109, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Grégoire</LastName><ForeName>Michel</ForeName><Initials>M</Initials><Identifier Source="ORCID">http://orcid.org/0000-0001-9196-876X</Identifier><AffiliationInfo><Affiliation>GET, CNRS-CNES-IRD-UPS, Toulouse University, 14 Avenue Edouard Belin, 31200, Toulouse, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Barra</LastName><ForeName>Fernando</ForeName><Initials>F</Initials><AffiliationInfo><Affiliation>Department of Geology and Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Plaza Ercilla 803, Santiago, 8370450, Chile.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Corgne</LastName><ForeName>Alexandre</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, 5090000, Chile.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2017</Year><Month>10</Month><Day>10</Day></ArticleDate></Article><MedlineJournalInfo><Country>England</Country><MedlineTA>Nat Commun</MedlineTA><NlmUniqueID>101528555</NlmUniqueID><ISSNLinking>2041-1723</ISSNLinking></MedlineJournalInfo><CommentsCorrectionsList><CommentsCorrections RefType="Cites"><RefSource>Science. 1999 Oct 15;286(5439):512-6</RefSource><PMID Version="1">10521343</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2000 Oct 19;407(6806):891-4</RefSource><PMID Version="1">11057664</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2007 Nov 29;450(7170):709-11</RefSource><PMID Version="1">18046408</PMID></CommentsCorrections></CommentsCorrectionsList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2017</Year><Month>02</Month><Day>17</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2017</Year><Month>07</Month><Day>31</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2017</Year><Month>10</Month><Day>12</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2017</Year><Month>10</Month><Day>12</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate 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