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Rare-Earth Minerals in Kaolin Ore, Mine Tailings, and Sands – Central Georgia, Upper Coastal Plain

Published online by Cambridge University Press:  01 January 2024

Anthony Boxleiter  and
W. Crawford Elliott Open the ORCID record for W. Crawford Elliott [Opens in a new window]
Anthony Boxleiter*
Affiliation:
Department of Geosciences, Georgia State University, Atlanta, GA 30302-3965, USA
W. Crawford Elliott
Affiliation:
Department of Geosciences, Georgia State University, Atlanta, GA 30302-3965, USA
*
e-mail: aboxleiter1@student.gsu.eduzhoumeifu@hotmail.com
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Abstract

The total concentrations of rare-earth elements (REE) in the mined kaolin (0.02–0.06 wt.%), kaolin mine tailings (0.03–1.9 wt.%), and the kaolin-associated Marion Member sand lithology (0.03–4.6 wt.%) opened questions regarding the modes of occurrence of the REE and the role(s) of chemical weathering and secondary processes to explain the presence of REE in these materials. The REE were hosted primarily by phosphate minerals (monazite, xenotime) based on mineralogic analyses (scanning electron microscopy, X-ray diffraction). Enrichments in the light rare-earth elements (LREE: La–Gd) and the high correlation coefficient values were noted between P and the total REE concentrations (r2 = 0.99) for the sands and the mine tailings. Lower correlation coefficient values were noted between total REE concentrations and Zr (r2 = 0.31). The coarse fractions of the mined kaolins were enriched in the heavy rare-earth elements (HREE: Y, Tb–Lu) relative to the kaolin-associated sand lithologies. The REE inventory cannot be explained solely by mineral inheritance within the mined kaolins. Lower correlation coefficient values between P and total REE, positive Eu/Eu* anomalies, and the presence of xenotime overgrowths on zircon showed the importance of the role of chemical weathering of the detrital minerals during post-depositional processes (such as diagenesis) leading to redistributed and fractionated REE within the mined kaolin. The possibility of adsorption of the REE to kaolin mineral surfaces in the fine fraction of the mined kaolins remains open and permits further study to characterize fully the multi-modal fractionation of REE possible in the Georgia kaolin deposits.

Keywords

GeorgiaKaolinMonaziteRare-earth elementsXenotime
Type
Original Paper
Information
Clays and Clay Minerals , Volume 71 , Issue 3: Special Issue on Rare Earth Elements , June 2023 , pp. 274 - 308
Copyright
Copyright © The Author(s), under exclusive licence to The Clay Minerals Society 2023

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