Definition
The Transvaal Supergroup is best known for excellent exposures of a mixed siliciclastic-carbonate ramp grading upward into an extensive carbonate platform overlain by banded-iron formation. Deposited on the Kaapvaal Craton between 2,670 and 2,050 Ma, the Transvaal Supergroup is best preserved in the Transvaal and Griqualand West structural basins in South Africa and extends into Botswana as the Kanye basin. The Transvaal Supergroup rests on the ≥2.70 Ga Ventersdorp Supergroup or older rocks with an angular unconformity and is intruded by the 2.05 Ga Bushveld Complex. In the Transvaal subbasin, it comprises two unconformity-bounded sequences:
- 1.
Quartz arenites of the Black Reef Formation overlain by predominantly chemical sedimentary rocks (dolomite and banded-iron formation) of the Chuniespoort Group (including rock sequences of the well-developed Campbellrand-Malmani platform)
- 2.
Sandstones, mudrocks, carbonates, glacial diamictites, and minor basalt-andesite flows of the...
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Hofmann, A. (2021). Transvaal Supergroup, South Africa. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1609-4
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DOI: https://doi.org/10.1007/978-3-642-27833-4_1609-4
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Transvaal Supergroup, South Africa- Published:
- 18 December 2020
DOI: https://doi.org/10.1007/978-3-642-27833-4_1609-4
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Transvaal Supergroup, South Africa- Published:
- 04 May 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_1609-3