Three indicator minerals from western Mamfe are geochemically characterized to determine their source rocks.
Corundums are blue, yellow and greyish-green mainly sorted alkaline magmatic rocks.
Significant Ti, Ta and/or Nb content in some blue grains suggest the enrichment of those elements in their source magma.
The Sn, Ta and Ti enrichment in most of the chrysoberyls suggests that they were grown in Sn–Ta–Ti enriched granitic pegmatites.
The trace elements abundance and REE anomalies in zircons suggest that they were sorted granitoids, syenites and kimberlites.