Trace element geochemistry of CR chondrite metal

dc.contributor.authorJacquet, Emmanuelen
dc.contributor.authorPaulhiac-Pison, Marineen
dc.contributor.authorAlard, Olivieren
dc.contributor.authorKearsley, Anton T.en
dc.contributor.authorGounelle, Matthieuen
dc.date.accessioned2025-06-16T11:35:20Z
dc.date.available2025-06-16T11:35:20Z
dc.date.issued2013en
dc.description.abstractWe report trace element analyses by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) of metal grains from nine different CR chondrites, distinguishing grains from chondrule interior (interior grains), chondrule surficial shells (margin grains), and the matrix (isolated grains). Save for a few anomalous grains, Ni-normalized trace element patterns are similar for all three petrographic settings, with largely unfractionated refractory siderophile elements and depleted volatile Au, Cu, Ag, S. All three types of grains are interpreted to derive from a common precursor approximated by the least-melted, fine-grained objects in CR chondrites. This also excludes recondensation of metal vapor as the origin of the bulk of margin grains. The metal precursors were presumably formed by incomplete condensation, with evidence for high-temperature isolation of refractory platinum-group-element (PGE)-rich condensates before mixing with lower temperature PGE-depleted condensates. The rounded shape of the Ni-rich, interior grains shows that they were molten and that they equilibrated with silicates upon slow cooling (1-100Kh(-1)), largely by oxidation/evaporation of Fe, hence their high Pd content, for example. We propose that Ni-poorer, amoeboid margin grains, often included in the pyroxene-rich periphery common to type I chondrules, result from less intense processing of a rim accreted onto the chondrule subsequent to the melting event recorded by the interior grains. This means either that there were two separate heating events, which formed olivine/interior grains and pyroxene/margin grains, respectively, between which dust was accreted around the chondrule, or that there was a single high-temperature event, of which the chondrule margin records a late quenching phase, in which case dust accreted onto chondrules while they were molten. In the latter case, high dust concentrations in the chondrule-forming region (at least three orders of magnitude above minimum mass solar nebula models) are indicated.en
dc.description.sponsorshipWe are grateful to the Programme National de Planetologie and the Institut Universitaire de France for their financial support, NASA and Cecilia Satterwhite for the loan of the Antarctic meteorite sections, and the Museum National d'Histoire Naturelle for that of the non-Antarctic samples. We thank Gretchen Benedix and Herbert Palme for their reviews, which significantly improved the assessment and discussion of the data.en
dc.description.statusPeer-revieweden
dc.format.extent19en
dc.identifier.otherWOS:000328150100012en
dc.identifier.otherScopus:84887131847en
dc.identifier.urihttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=anu_research_portal_plus2&SrcAuth=WosAPI&KeyUT=WOS:000328150100012&DestLinkType=FullRecord&DestApp=WOS_CPLen
dc.identifier.urihttps://hdl.handle.net/1885/733763687
dc.language.isoenen
dc.sourceMeteoritics and Planetary Scienceen
dc.subjectFe-ni metalen
dc.subjectHighly siderophile elementsen
dc.subjectChemical fractionationsen
dc.subjectCarbonaceous chondritesen
dc.subjectPrimitive chondritesen
dc.subjectMagnesian chondrulesen
dc.subjectThermal historiesen
dc.subjectHigh-temperatureen
dc.subjectOriginen
dc.subjectIronen
dc.titleTrace element geochemistry of CR chondrite metalen
dc.typeJournal articleen
local.bibliographicCitation.lastpage1999en
local.bibliographicCitation.startpage1981en
local.contributor.affiliationJacquet, Emmanuel; CNRSen
local.contributor.affiliationPaulhiac-Pison, Marine; CNRSen
local.contributor.affiliationAlard, Olivier; Université Montpellier IIen
local.contributor.affiliationKearsley, Anton T.; Imperial College Londonen
local.contributor.affiliationGounelle, Matthieu; CNRSen
local.identifier.citationvolume48en
local.identifier.doi10.1111/maps.12212en
local.identifier.puref83b70bd-1b76-4ef1-b812-89ed18a99c77en
local.type.statusPublisheden

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