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dc.date.accessioned2020-08-18T19:11:48Z
dc.date.available2020-08-18T19:11:48Z
dc.date.created2020-05-23T17:16:32Z
dc.date.issued2020
dc.identifier.citationBorst, Anouk M Finch, Adrian A. Friis, Henrik Horsburgh, Nicola J. Gamaletsos, Platon N. Goettlicher, Joerg Steininger, Ralph Geraki, Kalotina . Structural state of rare earth elements in eudialyte-group minerals. Mineralogical magazine. 2020, 84(1), 19-34
dc.identifier.urihttp://hdl.handle.net/10852/78521
dc.description.abstractEudialyte-group minerals (EGM) attract global interest as potential resources for high-field-strength elements (e.g. Zr, Nb, Ta, and rare-earth elements), i.e. critical materials for modern technologies. They are particularly valued for their relative enrichment in the most critical lanthanides, i.e. Nd and heavy rare earth elements (Gd–Lu). However, rare earth element (REE) substitution mechanisms into the EGM structure are still poorly understood. Light and heavy REE may occupy different sites and there may be ordering and/or defect clustering in the structure. This study uses X-ray absorption spectroscopy to determine the structural state of REE in EGM from prospective eudialyte-bearing complexes. Yttrium K-edge and Nd L3-edge spectra were collected as proxies for heavy and light REE, respectively, and compared to natural and synthetic REE-bearing standards. Extended X-ray absorption fine structure data yield best fits for Y in six-fold coordination with Y–O distances of 2.24–2.32 Å, and a second coordination sphere comprising Fe, Na, Ca, Si and O at radial distances of 3.6–3.8 Å. These findings are consistent with dominant Y3+ substitution for Ca2+ on the octahedral M1 site in all the samples studied, and exclude preferential substitution of Y3+ onto the smaller octahedral Z site or the large low-symmetry N4 site. Using lattice strain theory, we constructed relative partitioning models to predict site preferences of lanthanides we have not measured directly. The models predict that all REE are favoured on the Ca-dominant M1 site and that preferential partitioning of heavy over light REE increases in EGM containing significant Mn in the M1-octahedral rings (oneillite subgroup). Thus, the flat REE profiles that make EGM such attractive exploration targets are not due to preferential partitioning of light and heavy REE onto different sites. Instead, local ordering of Mn- and Ca-occupied M1 sites may influence the capacity of EGM to accommodate heavy REE.
dc.languageEN
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleStructural state of rare earth elements in eudialyte-group minerals
dc.typeJournal article
dc.creator.authorBorst, Anouk M
dc.creator.authorFinch, Adrian A.
dc.creator.authorFriis, Henrik
dc.creator.authorHorsburgh, Nicola J.
dc.creator.authorGamaletsos, Platon N.
dc.creator.authorGoettlicher, Joerg
dc.creator.authorSteininger, Ralph
dc.creator.authorGeraki, Kalotina
cristin.unitcode185,28,8,3
cristin.unitnameMineralogisk forskningsgruppe
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin1812242
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Mineralogical magazine&rft.volume=84&rft.spage=19&rft.date=2020
dc.identifier.jtitleMineralogical magazine
dc.identifier.volume84
dc.identifier.issue1
dc.identifier.startpage19
dc.identifier.endpage34
dc.identifier.doihttps://doi.org/10.1180/mgm.2019.50
dc.identifier.urnURN:NBN:no-81602
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn0026-461X
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/78521/1/Eudialyte%2Bstructural%2Bstate%2BREE_Borst%2Bet%2Bal%2B2020.pdf
dc.type.versionPublishedVersion


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