Rewriting the Lithium Playbook: Archean roots, greenstone belts, and giant pegmatites
- Archean lithium-rich pegmatites formed from crustal sources refertilised by hydrous, mantle-derived sanukitoid magmas beneath greenstone belts.
- The leucogranites evolve from metaluminous, juvenile, parental magmas through melting igneous—not sedimentary—sources, challenging traditional Li-pegmatite models.
- Major crustal-scale faults and greenstone-granite contacts enabled upward melt transfer and Li-enrichment at craton margins.
Smithies, R.H., Lu, Y., Champion, D.C., Sweetapple, M.T., Lowrey, J.R., Bowman, N.H., Cassidy, K.F., Ivanic, T.J., Kemp, A.I.S., Turnbull, R.E., Gessner, K. & Korhonen, F.J. (2025). Giant lithium-rich pegmatites in Archean cratons form by remelting refertilised roots of greenstone belts. Communications Earth & Environment, 6, 630. https://doi.org/10.1038/s43247-025-02622-5. 
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