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Rewriting the Lithium Playbook: Archean roots, greenstone belts, and giant pegmatites

Smithies, R.H. et al. (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.

Go to Paper
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  • Lithium-rich pegmatites formed from crustal sources refertilised by hydrous, mantle-derived sanukitoid magmas beneath greenstone belts.
  • The parental leucogranites are metaluminous, juvenile, and evolved from 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.
For Geochronology
For Resources Engineering and Extractive Metallurgy
Rg Environmental Geoscience

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Metallurgical Training and CPD
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Ore Beneficiation

Rewriting the Lithium Playbook: Archean roots, greenstone belts, and giant pegmatites

Smithies, R.H. et al. (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.

Go to Paper
CFIGS Image alt CFIGS Image alt
  • Lithium-rich pegmatites formed from crustal sources refertilised by hydrous, mantle-derived sanukitoid magmas beneath greenstone belts.
  • The parental leucogranites are metaluminous, juvenile, and evolved from 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.
For Geochronology
For Resources Engineering and Extractive Metallurgy
Rg Environmental Geoscience

Linked Services:

Geometallurgy
Geometallurgy

Rewriting the Lithium Playbook: Archean roots, greenstone belts, and giant pegmatites (Duplicated) (Duplicated) (Duplicated)

Smithies, R.H. et al. (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.

Go to Paper
CFIGS Image alt CFIGS Image alt
  • Lithium-rich pegmatites formed from crustal sources refertilised by hydrous, mantle-derived sanukitoid magmas beneath greenstone belts.
  • The parental leucogranites are metaluminous, juvenile, and evolved from 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.
For Geochronology
For Resources Engineering and Extractive Metallurgy
Rg Environmental Geoscience

Linked Services:

Geometallurgy
Geometallurgy
Metallurgical Training and CPD
Metallurgical Training and CPD
Ore Beneficiation
Ore Beneficiation

Rewriting the Lithium Playbook: Archean roots, greenstone belts, and giant pegmatites

Smithies, R.H. et al. (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.

Go to Paper
CFIGS Image alt CFIGS Image alt
  • Lithium-rich pegmatites formed from crustal sources refertilised by hydrous, mantle-derived sanukitoid magmas beneath greenstone belts.
  • The parental leucogranites are metaluminous, juvenile, and evolved from 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.

Linked Services:

Geometallurgy
Geometallurgy
Metallurgical Training and CPD
Metallurgical Training and CPD

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