Erosional remnants of Paleoproterozoic red bed successions such as the Olifantshoek, Soutpansberg, Waterberg and Palapye Groups cover an extensive area of the Kaapvaal Craton. Depositional ages of these successions have been ill-defined and their lateral
No takes yet. Share an insight, caveat, or question.
H. C. Dorland (2006) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: