Deconstructing the Transvaal Supergroup, South Africa: implications for Palaeoproterozoic palaeoclimate models
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The Koegas Subgroup only develops in the deeper, southwestern part of the Griqualand West Basin; its absence in the shallower parts is explained by palaeobathymetric considerations.
“The Koegas Subgroup only develops in the deeper, southwestern part of the Griqualand West Basin. Its absence in the shallower parts - where the Griquatown GIF is directly overlain by the Makganyene diamictite - is explained by palaeobathymetric considerations (Moore et al., 2001; Polteau, et al., 2006).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Moore et al., 2001
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References 29 · Cited by 62
- Authors
- Moore, J. M., Tsikos, H., & Polteau, S.
- Affiliations
- Rhodes University (ZA)
- Corresponding author
- Moore, John M.
- Venue
- Journal of African Earth Sciences
- Publisher
- Elsevier BV
- Published
- 2001-01
- Volume
- 33
- Issue
- 3-4
- Pages
- 437-444
- ISSN
- 0899-5362 (ISSN-L)
- 1464-343X
- OpenAlex
- W1982530070
- Cited by
- 62
- References
- 29
- Citations by year
- 2026: 1 · 2025: 4 · 2024: 3 · 2023: 3 · 2022: 3 · 2021: 2 · 2020: 1 · 2019: 2 · 2018: 5 · 2017: 8 · 2016: 3 · 2015: 3 · 2014: 2 · 2013: 4 · 2012: 2
- FWCI
- 0.34
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of African Earth Sciences (publishedVersion)
- Funders
- National Research Foundation
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- Transvaal Supergroup, Paleoproterozoic, stratigraphic correlation, diamictite, glacial maximum, iron-formation, paleoclimate
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