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Rare Earth Elements (REE) are more abundant than gold but are difficult to extract due to their large ionic radii and high charge, which limits their incorporation into common mineral structures. Major geological environments for REE deposits include magmatic sources like carbonatites and peralkaline rocks, as well as sedimentary deposits such as phosphorites and ion adsorption clays. While carbonatite and peralkaline deposits have the highest concentrations of REE, their rarity and the potential for co-rec

Author

sabarivatsan1

Language

EN