RARE EARTH ELEMENT AND NIOBIUM ENRICHMENTS IN CARBONATITES
Types of ores in carbonatites include those formed as primary magmatic minerals, from late magmatic hydrothermal fluids, and by enrichment in weathered horizons. The principle REE-bearing mineral phases include fluorocarbonates (bastnäsite, parisite, and synchysite), hydrated carbonates (ancylite), and phosphates (monazite and apatite). The dominant REE ore mineral exploited at most mines is bastnäsite, which can be coarse grained and contains approximately 75 wt.% RE2O3. Pyrochlore [(Ca,Na)2Nb2O6(OH,F)] is the primary Nb ore mineral. At the Araxá deposit, bariopyrochlore is mined from the lateritic zone.
Carbonatites are primarily associated with continental rifting, but some carbonatites are associated with orogenic activity. Processes responsible for REE enrichment include fractional crystallization of the carbonatitic magma, enrichment of REEs in orthomagmatic or hydrothermal fluids and subsequent precipitation or subsolidus metasomatic redistribution of REEs, and breakdown of primary carbonatitic mineral phases by chemical weathering and sequestration of REEs in secondary minerals. Although there is debate on how carbonatite magmas are generated, the parental magma and REEs are clearly derived from mantle sources.