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A cryptic Mesoarchaean terrane in the basement to the Central African Copperbelt
In a study of the geochronology of the Katangan Sequence and its basement in the Central African Copperbelt, detrital and xenocrystic zircons from Muva quartzites and Katangan lapilli tuffs, were
Estimating Duration and Intensity of Neoproterozoic Snowball Glaciations from Ir Anomalies
The authors' data confirm the presence of extended global Neoproterozoic glaciations and indicate that the duration of the Marinoan glacial episode was at least 3 million, and most likely 12 million, years.
Chapter 12 Neoproterozoic glaciogenic diamictites of the Katanga Supergroup, Central Africa
Abstract Glaciogenic sediments of the Katanga Supergroup are represented by two units. The syn-rift Grand Conglomerat Formation (<765±5 Ma to >735±5 Ma) occurs within the Nguba Group, and the Petit