An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity
Autor(a) principal: | |
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Data de Publicação: | 2014 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Anais da Academia Brasileira de Ciências (Online) |
Texto Completo: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652014000401609 |
Resumo: | Subduction zone or arc magmas are known to display a characteristic depletion of High Field Strength Elements (HFSE) relative to other similarly incompatible elements, which can be attributed to the presence of the accessory mineral rutile (TiO2) in the residual slab. Here we show that the partitioning behavior of vanadium between rutile and silicate melt varies from incompatible (∼0.1) to compatible (∼18) as a function of oxygen fugacity. We also confirm that the HFSE are compatible in rutile, with D(Ta)> D(Nb)>> (D(Hf)>/∼ D(Zr), but that the level of compatibility is strongly dependent on melt composition, with partition coefficients increasing about one order of magnitude with increasing melt polymerization (or decreasing basicity). Our partitioning results also indicate that residual rutile may fractionate U from Th due to the contrasting (over 2 orders of magnitude) partitioning between these two elements. We confirm that, in addition to the HFSE, Cr, Cu, Zn and W are compatible in rutile at all oxygen fugacity conditions. |
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Anais da Academia Brasileira de Ciências (Online) |
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An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacityarc magmaHFSEpartition coefficientredoxrutileSubduction zone or arc magmas are known to display a characteristic depletion of High Field Strength Elements (HFSE) relative to other similarly incompatible elements, which can be attributed to the presence of the accessory mineral rutile (TiO2) in the residual slab. Here we show that the partitioning behavior of vanadium between rutile and silicate melt varies from incompatible (∼0.1) to compatible (∼18) as a function of oxygen fugacity. We also confirm that the HFSE are compatible in rutile, with D(Ta)> D(Nb)>> (D(Hf)>/∼ D(Zr), but that the level of compatibility is strongly dependent on melt composition, with partition coefficients increasing about one order of magnitude with increasing melt polymerization (or decreasing basicity). Our partitioning results also indicate that residual rutile may fractionate U from Th due to the contrasting (over 2 orders of magnitude) partitioning between these two elements. We confirm that, in addition to the HFSE, Cr, Cu, Zn and W are compatible in rutile at all oxygen fugacity conditions.Academia Brasileira de Ciências2014-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652014000401609Anais da Academia Brasileira de Ciências v.86 n.4 2014reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/0001-3765201420140014info:eu-repo/semantics/openAccessMALLMANN,GUILHERMEFONSECA,RAÚL O.C.SILVA,ADOLFO B.eng2015-10-27T00:00:00Zoai:scielo:S0001-37652014000401609Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2015-10-27T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false |
dc.title.none.fl_str_mv |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
title |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
spellingShingle |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity MALLMANN,GUILHERME arc magma HFSE partition coefficient redox rutile |
title_short |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
title_full |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
title_fullStr |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
title_full_unstemmed |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
title_sort |
An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity |
author |
MALLMANN,GUILHERME |
author_facet |
MALLMANN,GUILHERME FONSECA,RAÚL O.C. SILVA,ADOLFO B. |
author_role |
author |
author2 |
FONSECA,RAÚL O.C. SILVA,ADOLFO B. |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
MALLMANN,GUILHERME FONSECA,RAÚL O.C. SILVA,ADOLFO B. |
dc.subject.por.fl_str_mv |
arc magma HFSE partition coefficient redox rutile |
topic |
arc magma HFSE partition coefficient redox rutile |
description |
Subduction zone or arc magmas are known to display a characteristic depletion of High Field Strength Elements (HFSE) relative to other similarly incompatible elements, which can be attributed to the presence of the accessory mineral rutile (TiO2) in the residual slab. Here we show that the partitioning behavior of vanadium between rutile and silicate melt varies from incompatible (∼0.1) to compatible (∼18) as a function of oxygen fugacity. We also confirm that the HFSE are compatible in rutile, with D(Ta)> D(Nb)>> (D(Hf)>/∼ D(Zr), but that the level of compatibility is strongly dependent on melt composition, with partition coefficients increasing about one order of magnitude with increasing melt polymerization (or decreasing basicity). Our partitioning results also indicate that residual rutile may fractionate U from Th due to the contrasting (over 2 orders of magnitude) partitioning between these two elements. We confirm that, in addition to the HFSE, Cr, Cu, Zn and W are compatible in rutile at all oxygen fugacity conditions. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-12-01 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652014000401609 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652014000401609 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/0001-3765201420140014 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
text/html |
dc.publisher.none.fl_str_mv |
Academia Brasileira de Ciências |
publisher.none.fl_str_mv |
Academia Brasileira de Ciências |
dc.source.none.fl_str_mv |
Anais da Academia Brasileira de Ciências v.86 n.4 2014 reponame:Anais da Academia Brasileira de Ciências (Online) instname:Academia Brasileira de Ciências (ABC) instacron:ABC |
instname_str |
Academia Brasileira de Ciências (ABC) |
instacron_str |
ABC |
institution |
ABC |
reponame_str |
Anais da Academia Brasileira de Ciências (Online) |
collection |
Anais da Academia Brasileira de Ciências (Online) |
repository.name.fl_str_mv |
Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC) |
repository.mail.fl_str_mv |
||aabc@abc.org.br |
_version_ |
1754302860331319296 |