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- Q15851391 subject Q21605721.
- Q15851391 subject Q6423375.
- Q15851391 subject Q8487874.
- Q15851391 abstract "The Transvaal Supergroup is a stratigraphic unit in northern South Africa and southern Botswana, situated on the Kaapvaal Craton, roughly between 23 to 29 degrees southern latitude and 22 to 30 degrees eastern longitude. It is dated to the boundary between the Archean and Proterozoic eras, roughly 2,500 Mya. It is delimited by the Witwatersrand Basin (2,700 Mya) and the Bushveld Igneous Complex (2,050 Mya).It consists of three parts, the Transvaal Basin in the eastthe Griqualand Basin in the west the smaller Kanye Basin in southern Botswana.Transvaal sedimentation began with predominantly clastic sedimentary rocks (Black Reef-Vryburg Formations) followed by carbonate rocks and banded iron formations (Chuniespoort-Ghaap-Taupone Groups). After an erosional hiatus, the clastic sedimentary rocks and volcanics of the Pretoria-Postmasburg-Segwagwa Groups were deposited within the three basins, largely under closed-basin conditions. A final stage of predominantly volcanic succession (Rooiberg Group-Loskop Formation) is limited to the Transvaal Basin.The Campbellrand-Malmani carbonate platform is part of the Chuniespoort Group and originally covered all of the Kaapvaal Craton. It has a thickness of over 1 km in both the Malmani and Campbellrand Subgroups.The Malmani Subgroup is situated northwest of Johannesburg. It consists of dolomite and chert with only minor clastic sediments.".
- Q15851391 wikiPageWikiLink Q1017513.
- Q15851391 wikiPageWikiLink Q104162.
- Q15851391 wikiPageWikiLink Q104168.
- Q15851391 wikiPageWikiLink Q1070438.
- Q15851391 wikiPageWikiLink Q15757945.
- Q15851391 wikiPageWikiLink Q167741.
- Q15851391 wikiPageWikiLink Q178248.
- Q15851391 wikiPageWikiLink Q21605721.
- Q15851391 wikiPageWikiLink Q258.
- Q15851391 wikiPageWikiLink Q304213.
- Q15851391 wikiPageWikiLink Q3694119.
- Q15851391 wikiPageWikiLink Q4291408.
- Q15851391 wikiPageWikiLink Q6423375.
- Q15851391 wikiPageWikiLink Q6864398.
- Q15851391 wikiPageWikiLink Q7835389.
- Q15851391 wikiPageWikiLink Q8487874.
- Q15851391 wikiPageWikiLink Q963.
- Q15851391 comment "The Transvaal Supergroup is a stratigraphic unit in northern South Africa and southern Botswana, situated on the Kaapvaal Craton, roughly between 23 to 29 degrees southern latitude and 22 to 30 degrees eastern longitude. It is dated to the boundary between the Archean and Proterozoic eras, roughly 2,500 Mya.".
- Q15851391 label "Transvaal Supergroup".