Illustrative

Formation of the world's largest REE deposit through protracted fluxing of carbonatite by subduction-derived fluids

Nature·May 7

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A large deposit of rare earth elements has been formed through a geological process. The formation is attributed to the interaction of subduction-derived fluids with carbonatite over a prolonged period. This process has resulted in the creation of the world's largest rare earth element deposit.

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Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere

Science | AAAS·Apr 8

An Unusually Warm Upper-Crust in the Late Paleozoic North China Continental Arc: Implications for the Thermal Modification of the Giant Bayan Obo REE Deposit

AGU Publications·May 15

The mantle source of REE-rich alkaline silicate magmas can be enriched by continent-derived sediment subduction

Nature·Dec 17

Brazilian Critical Minerals Ema Project Transforms REE Extraction Through ISR Technology

Discovery Alert·Apr 23

Paleozoic carbonatites controlled rare-earth-elements mineralization at Bayan Obo

Science | AAAS·Apr 23

Refertilized continental root controls the formation of the Mianning–Dechang carbonatite-associated rare-earth-element ore system

Nature·Aug 19

Formation of carbonatite-related giant rare-earth-element deposits by the recycling of marine sediments

Nature·Jun 2

Trace element catalyses mineral replacement reactions and facilitates ore formation

Nature·Mar 2

View original report at Nature ↗

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