Musipizi Conglomerate Mbr Fm
Type Locality and Naming
Luangwa Basin (Zambia) (Note: Sometimes erroneously transcribed in literature as the "northern Lilangu Basin," but formally described from the northern Luangwa Valley). Named for local geographic features in the northern Luangwa Valley, Zambia. It was formally described by Utting (1978) as the lowermost sedimentary unit of the Karoo succession in this area.
Synonym: Musipixi Cgl (misspelled often),
Lithology and Thickness
The unit is characterized as a "mixtite" (diamictite or tillite), primarily consisting of subangular, boulder-sized clasts (up to 1 meter in diameter, but mostly 1 to 20 cm) supported within a fine silty matrix. Striated pebbles are present but rare.
Relationships and Distribution
Lower contact
Rests with a profound unconformity directly upon the ancient Precambrian crystalline basement.
Upper contact
Stratigraphically underlies the coal-bearing sequences of the Luwumbu Coal Fm (specifically sitting below units like the Mukumba Siltstone Member). While some authors treat it as an independent basal unit analogous to the Idusi Fm, others group it as the basal-most conglomeratic member of the larger formational sequences starting the Karoo fill.
Regional extent
Correlates broadly with the Dwyka Gr in the Main Karoo Basin of South Africa and the Idusi Fm in the Ruhuhu Basin of Tanzania.
GeoJSON
Fossils
Age
Depositional setting
Glacial to periglacial environments.
Additional Information