Usili Fm
Type Locality and Naming
Ruhuhu Basin (Tanzania). Named after the Usili Mountain in the Ruhuhu Basin of southwestern Tanzania. Originally designated as the "Lower Bone Bed" or "K6" horizon by Stockley (1932) in his classic stratigraphic division, it was later formally renamed the Usili Formation by Wopfner (2002). Upper formation in Beaufort Gr in Ruhuhu Basin (Tanzania).
Synonym: Formerly known as the Kawinga Formation in older literature. K6 beds
Lithology and Thickness
Composed of a massive sequence (up to ~300 meters thick) of non-marine, fluvio-lacustrine sediments. It typically begins with a basal cross-bedded sandstone or conglomeratic unit that grades upward into a thick, monotonous succession of grey-green to purplish-red mudstones and siltstones. The mudstones are well known for containing abundant calcareous (calcrete/septarian) nodules.
Relationships and Distribution
Lower contact
Conformably to transitionally overlies the calcareous and fine-grained Ruhuhu Fm
Upper contact
Unconformably overlain by the Triassic Manda Beds Fm
Regional extent
Geographically restricted to the Ruhuhu Basin in southwestern Tanzania. It directly correlates with the Beaufort Gr (specifically the Adelaide Subgroup / Dicynodon Assemblage Zone) in the Main Karoo Basin of South Africa, the Lower Sakamena Gr in Madagascar, and the Upper Madumabisa Mudstone Fm in Zambia.
GeoJSON
Fossils
Age
Depositional setting
Terrestrial intracratonic rift basin.
Additional Information