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- Q7835389 subject Q15366050.
- Q7835389 subject Q6423375.
- Q7835389 abstract "The Transvaal Basin is one of three basins of the Transvaal Supergroup on the Kaapvaal craton. The evolution of this 2.65–2.05 Ga Neoarchaean–Palaeoproterozoic basin is thought to have been derived largely from magmatism, palaeoclimate and eustasy, while plate tectonics played an intermittent role. The supergroup is made up of basal ‘protobasinal’ rocks, upon which followed the Black Reef Formation, Chuniespoort Group and the uppermost Pretoria Group.The Transvaal Supergroup displays three unconformity-bounded sequences that surface in twogeographically distinct areas – the Transvaal Basin, which circumscribes the Bushveld Igneous Complex, and the Griqualand West basin, lying between Kimberley and Sishen at the western Kaapvaal craton rim, extending into southern Botswana beneath the Kalahari Sands as the Kanye Basin. The two basins areseparated by the broad Vryburg Arch.Between approximately 2.640 and 2.516 Ga, two successive stromatolitic carbonate platforms developed in the basin of the Kaapvaal craton. Oldest was the Schmidtsdrif Subgroup, deposited in the southwestern part of the basin, showing stromatolitic carbonates, siliciclastic sediments and small lava flows. This was followed by the Nauga formation carbonates deposited on peritidal flats in the southwest, which were inundated during a marine transgression of the Transvaal Supergroup continental sea, at some 2.550 Ga. This resulted in a carbonate platform in the Transvaal and Griqualand West Basins, lasting for 30–50 Ma. Shales were deposited during this period over the Nauga Formation carbonates. Following this a subsidence led to immersion of the stromatolitic platform and to sediments of iron-rich banded iron formations being laid down over the entire basin.".
- Q7835389 wikiPageWikiLink Q1017513.
- Q7835389 wikiPageWikiLink Q125465.
- Q7835389 wikiPageWikiLink Q125905.
- Q7835389 wikiPageWikiLink Q1467769.
- Q7835389 wikiPageWikiLink Q15366050.
- Q7835389 wikiPageWikiLink Q15851391.
- Q7835389 wikiPageWikiLink Q176739.
- Q7835389 wikiPageWikiLink Q178248.
- Q7835389 wikiPageWikiLink Q191069.
- Q7835389 wikiPageWikiLink Q193738.
- Q7835389 wikiPageWikiLink Q2547918.
- Q7835389 wikiPageWikiLink Q301920.
- Q7835389 wikiPageWikiLink Q304213.
- Q7835389 wikiPageWikiLink Q31796.
- Q7835389 wikiPageWikiLink Q40157.
- Q7835389 wikiPageWikiLink Q577.
- Q7835389 wikiPageWikiLink Q6423375.
- Q7835389 wikiPageWikiLink Q645135.
- Q7835389 wikiPageWikiLink Q691831.
- Q7835389 wikiPageWikiLink Q751300.
- Q7835389 wikiPageWikiLink Q7514925.
- Q7835389 wikiPageWikiLink Q777913.
- Q7835389 wikiPageWikiLink Q7950.
- Q7835389 wikiPageWikiLink Q876798.
- Q7835389 wikiPageWikiLink Q963.
- Q7835389 wikiPageWikiLink Q993090.
- Q7835389 comment "The Transvaal Basin is one of three basins of the Transvaal Supergroup on the Kaapvaal craton. The evolution of this 2.65–2.05 Ga Neoarchaean–Palaeoproterozoic basin is thought to have been derived largely from magmatism, palaeoclimate and eustasy, while plate tectonics played an intermittent role.".
- Q7835389 label "Transvaal Basin".