Detrital zircons provide direct dates for the Daspoort and Magaliesberg formations.
Prominent ∼2575–2410 Ma source terrain confirms Pilbara-Kaapvaal cratonic link.
Duitschland Formation ∼2420–2320 Ma old, includes basal glacial diamictite.
2–3 South African Paleoproterozoic glacial episodes recognized.
Tectonostratigraphy consistent with supercontinent assembly and rifting ∼2.4–2.1 Ga.