摘要
Rutile, as an important component in alluvial or eluvial heavy mineral deposits, is known in southern Cameroon. These deposits are underlain by the Neoproterozoic low- to high-grade Yaoundxe9; Group. Geochemical, thermometric, fluid inclusion and Pb isotopic studies of the rutile from alluvial and eluvial concentrates and from medium-grade micaschist from the nearby Yaoundxe9; region permit the following conclusions: (1) alluvial and eluvial rutile of the Yaoundxe9; region are derived from the degradation of metapelites, metamafic rocks and pegmatites of the nearby Yaoundxe9; Group; (2) rutile in the Yaoundxe9; Group formed during the Pan-African metamorphism, or was inherited as detrital rutile from a 900 Ma source. The study also shows that the rutile can be used to trace the history of the Pan-African belt north of the Congo craton.