Richard G. Vos

TL;DR: A 1600m succession of quartz arenites and associated shaley deposits comprising the Hospital Hill Subgroup at the base of the Witwatersrand Supergroup is considered to have been deposited largely under the influence of tidal processes as discussed by the authors.

TL;DR: The Ordovician Haouaz Formation in the western-central Gargaf Arch of western Libya provides a well-exposed example of an ancient fan delta system as discussed by the authors, consisting of delta front deposits overlain by subaqueous distributary channels with intervening distributary mouth shoals.

TL;DR: In this paper, four braided stream facies are recognized on the basis of distinct lithologies and assemblages of sedimentary structures, including upward-fining conglomerate to sandstone and mudstone channel fill sequences.

TL;DR: In this article, the Aouinet Ouenine Formation in the southern Ghadames Basin of western Libya provides a well exposed example of a deltaic complex containing both progradational and transgressive facies.