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Extreme Alteration of Chevkinite-(Ce) by Pb-CO2-Rich Fluids: Evidence from the White Tundra Pegmatite, Keivy Massif, Kola Peninsula

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dc.abstract.enAn unusual hydrothermal alteration scheme was presented for chevkinite-(Ce) from the White Tundra pegmatite (2656 ± 5 Ma), Keivy massif, Kola Peninsula. Pb-CO2-rich fluids initially removed REE and Y from the chevkinite-(Ce), with enrichment in Pb and U. PbO abundances reaching 17.35 wt%. Continued alteration resulted in the altered chevkinite-(Ce) being progressively transformed to a Pb-Ti-Fe-Si phase, which proved, upon EBSD analysis, to be almost totally amorphous. Pb enrichment was accompanied by a loss of LREE, especially La, relative to HREE, and the development of strong positive Ce anomalies. A notably U-rich aeschynite-(Y), with UO2 values ≤7.67 wt%, crystallized along with the chevkinite-(Ce). Aeschynite-(Y) with a lower UO2 value (3.91 wt%) and bastnäsite-(Ce) formed during alteration. The formation of bastnäsite-(Ce) rather than cerussite, which might have been expected in a high Pb-CO2 environment, is ascribed to the fluids being acidic.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorJokubauskas, Petras
dc.contributor.authorKotowski, Jakub
dc.contributor.authorBagiński, Bogusław
dc.contributor.authorZozulya, Dmitry
dc.contributor.authorStachowicz, Marcin
dc.contributor.authorMacdonald, Ray
dc.date.accessioned2024-01-25T00:14:47Z
dc.date.available2024-01-25T00:14:47Z
dc.date.issued2022
dc.description.financeŚrodki finansowe, o których mowa w art. 365 pkt. 2 ustawy
dc.description.number8
dc.description.volume12
dc.identifier.doi10.3390/MIN12080989
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/106887
dc.identifier.weblinkhttps://www.mdpi.com/2075-163X/12/8/989/pdf
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofMinerals
dc.relation.pages989
dc.rightsClosedAccess
dc.sciencecloudnosend
dc.subject.enWhite Tundra pegmatite
dc.subject.enPb-rich chevkinite-(Ce)
dc.subject.enCO2-bearing hydrothermal fluids
dc.subject.enamorphous Pb-Ti-Fe-Si phase
dc.titleExtreme Alteration of Chevkinite-(Ce) by Pb-CO2-Rich Fluids: Evidence from the White Tundra Pegmatite, Keivy Massif, Kola Peninsula
dc.typeJournalArticle
dspace.entity.typePublication