In situ measurement of Re-Os isotopes in mantle sulfides by laser ablation multicollector-inductively coupled plasma mass spectrometry

dc.contributor.authorPearson, NJen
dc.contributor.authorAlard, Oen
dc.contributor.authorGriffin, WLen
dc.contributor.authorJackson, SEen
dc.contributor.authorO'Reilly, SYen
dc.date.accessioned2025-06-16T11:35:15Z
dc.date.available2025-06-16T11:35:15Z
dc.date.issued2001-09-15en
dc.description.abstractA method has been developed for the in situ determination of Re-Os isotopes in single grains of sulfides in mantle-derived peridotites using a laser ablation microprobe attached to a multicollector-induced coupled plasma mass spectrometer (MC-ICPMS). High-precision Os isotope analysis by MC-ICPMS is demonstrated by the measurement of interlaboratory Os standards. Evaluation of mass bias correction procedures shows that the exponential law provides the best fit to the Os isotope data and that the ratio of the mass fractionation coefficients for Re and Os remains constant for the range of typical instrument operating conditions, This relationship enables the accurate and precise correction of the isobaric interference of Re-187 on Os-187 for Re-187/Os-188 values up to 1.6.Results are presented for single sulfide inclusions in olivine macrocryts from kimberlites in the Siberian and Slave Cratons, and sulfides enclosed in silicates and interstitial to silicates in peridotite xenoliths from the Slave Craton and Massif Central, France. Enclosed sulfides larger than 50 mum in diameter and with Os contents greater than or equal to40 ppm give Os-187/Os-188 ratios with a precision of 0.1% (2 SE), which is equivalent to N-TIMS whole-rock data. Interstitial sulfides typically have lower Os (10 to 30 ppm) and give analyses with lower precision (similar to1 to 2%) but still provide valuable information on the movement of Os within the lithosphere. The sulfide inclusions in silicates preserve significantly less radiogenic Os isotopic compositions than interstitial sulfides and accordingly produce significantly older and more realistic Re-Os age information. Whole-rock Os isotope compositions reflect the proportions of different generations of enclosed and interstitial sulfides, this calls into question the significance of many published "depletion ages." Copyright (C) 2002 Elsevier Science Ltd.en
dc.description.statusPeer-revieweden
dc.format.extent14en
dc.identifier.otherWOS:000174443100010en
dc.identifier.otherScopus:0000079780en
dc.identifier.urihttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=anu_research_portal_plus2&SrcAuth=WosAPI&KeyUT=WOS:000174443100010&DestLinkType=FullRecord&DestApp=WOS_CPLen
dc.identifier.urihttps://hdl.handle.net/1885/733763685
dc.language.isoenen
dc.sourceGeochimica et Cosmochimica Actaen
dc.subjectGroup element ratiosen
dc.subjectSlave cratonen
dc.subjectAtomic-weighten
dc.subjectOsmiumen
dc.subjectSystematicsen
dc.subjectLithosphereen
dc.subjectConstraintsen
dc.subjectXenolithsen
dc.subjectSpinelen
dc.subjectKimberliteen
dc.titleIn situ measurement of Re-Os isotopes in mantle sulfides by laser ablation multicollector-inductively coupled plasma mass spectrometryen
dc.typeJournal articleen
local.bibliographicCitation.lastpage1050en
local.bibliographicCitation.startpage1037en
local.contributor.affiliationPearson, NJ; Macquarie Universityen
local.contributor.affiliationAlard, O; Geochemistry, Research School of Earth Sciences, ANU College of Science and Medicine, The Australian National Universityen
local.contributor.affiliationGriffin, WL; Macquarie Universityen
local.contributor.affiliationJackson, SE; Macquarie Universityen
local.contributor.affiliationO'Reilly, SY; Macquarie Universityen
local.identifier.citationvolume66en
local.identifier.doi10.1016/S0016-7037(01)00823-7en
local.identifier.pureace4763f-6916-4f41-87cb-52504ba38bf9en
local.type.statusPublisheden

Downloads