We report U–Pb age and chemical data for detrital monazites from 5 African rivers.
The monazite U–Pb age data defined peaks corresponding to the Pan-African Orogeny.
The age peaks are 20–40 Myr younger than the zircon age peaks of the same rivers.
Detrital monazite REE–Th–U systematics are linked to their potential genesis.
Detrital monazites provide a record of syn- to post-collisional events.