Li-Be-Sn-Nb-rich pegmatite dykes, hosted in Late Carboniferous to Early Permian schists, gneisses and granites. The ore field contains around 100 dykes, which are up to 1000 m long and up to 20 m thick.
References
- Orris, G.J., and Bliss, J.D. (2002): Mines and Mineral Occurrences of Afghanistan. United States Geological Survey Open-File Report 02-110.
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