The formation is a sedimentary unit, consisting mainly of aeolian sands and silts with interbedded fluvial sediments,[2] laid down during a period of increasing aridity.[3]
^Jones, D. L.; Duncan, R. A.; Briden, J. C.; Randall, D. E.; MacNiocaill, C. (2001). "Age of the Batoka basalts, northern Zimbabwe, and the duration of Karoo Large Igneous Province magmatism". Geochemistry, Geophysics, Geosystems. 2 (2): n/a. Bibcode:2001GGG.....2.1022J. doi:10.1029/2000GC000110.
^ abcNyambe, Imasiku A.; Utting, John (1997). "Stratigraphy and palynostratigraphy, Karoo Supergroup (Permian and Triassic), mid-Zambezi Valley, southern Zambia". Journal of African Earth Sciences. 24 (4): 563. Bibcode:1997JAfES..24..563N. doi:10.1016/S0899-5362(97)00081-X.
^ abcdefghijWeishampel, David B; et al. (2004). "Dinosaur distribution (Early Jurassic, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 535–536. ISBN0-520-24209-2.
^Viglietti, Pia A.; Barrett, Paul M.; Broderick, Tim J.; Munyikwa, Darlington; MacNiven, Rowan; Broderick, Lucy; Chapelle, Kimberley; Glynn, Dave; Edwards, Steve (January 2018). "Stratigraphy of the Vulcanodon type locality and its implications for regional correlations within the Karoo Supergroup". Journal of African Earth Sciences. 137: 149–156. Bibcode:2018JAfES.137..149V. doi:10.1016/j.jafrearsci.2017.10.015. ISSN1464-343X.
^M.A. Raath (1972). "Fossil vertebrate studies in Rhodesia: a new dinosaur (Reptilia: Saurischia) from near the Triassic-Jurassic boundary". Arnoldia. 5.