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Paradigm Challenge  /  Physics

Fluorite is the secret source behind the world's largest deposits of heavy rare earth elements used in modern electronics.

Rare earth element deposits in regolith are primarily sourced from fluorite rather than more durable minerals. Geologists previously assumed that harder, refractory minerals held these valuable resources, which made them difficult to extract. Identifying fluorite as the main source changes the entire strategy for locating and mining the elements essential for smartphones and electric cars. This mineral is much easier to process, potentially lowering the cost and environmental impact of rare earth production. Future exploration will now focus on fluorite-rich regions to secure the supply chain for green energy technology. It turns a common mineral into the most important target for the global tech economy.

Original Paper

Fluorite recognized as the principal source mineral for regolith-hosted HREE deposits

Wei Jian, Shida Zhai, Jingwen Mao, Bernd Lehmann, Nian Chen, Shiwei Song, Min Liu, Xuyang Meng, Xianguang Wang, Liangxin Gong, Guogang Ren, Adam Simon

research_square  ·  rs-8880973

Abstract Regolith-hosted rare earth element (REE) deposits in South China supply most of the world’s heavy REE (HREE), but the parent minerals that liberate HREE during weathering remain uncertain because commonly invoked accessory phases are refractory. Here we recognize that fluorite is the dominant HREE host in the granitic bedrock of the world’s largest deposit (Shitouping; ~174,000 t HREE oxides). Fluorite occurs in the Early Cretaceous syenogranite at a concentration of ~0.8 wt.% and conta