ZIMBABWE

LITHIUM

Geology

Outcropping and sub-outcropping pegmatite sills. 6 larger clusters of shallow artisanal workings. The main pegmatite has a discontinuous quartz core bordered by irregular cleavelandite zones with tantalite, lepidolite and zinnwaldite float. The pegmatite host is likely to be amphibolite.

License area: 312 ha

No. Licenses: 8

Li3 Ownership: 100%

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  • ‚ÄčLath of white spodumene in a fragment of pegmatite
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Quartz

SPODUMENE

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