Sequence stratigraphy and plate tectonic significance of the Transvaal succession of southern Africa and its equivalent in Western Australia
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Beukes and Gutzmer (2008) suggest that the Hamersley and Transvaal BIF sequences reflect deposition in the same basin, although it cannot be ruled out that they were two separate, but coeval basins.
“Beukes and Gutzmer (2008) presented detailed correlations between the Hamersley and Transvaal BIFs, and suggest that these sequences reflect deposition in the same basin, as originally proposed by Button (1976) and then Cheney (1996), although it cannot be ruled out that they were two separate, but coeval basins.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Cheney (1996)
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- Authors
- Cheney, E. S.
- Corresponding author
- Cheney, E.S.
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 1996-07
- Volume
- 79
- Issue
- 1-2
- Pages
- 3-24
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W1984055345
- Cited by
- 221
- References
- 68
- Citations by year
- 2026: 4 · 2025: 4 · 2024: 6 · 2023: 9 · 2022: 8 · 2021: 12 · 2020: 12 · 2019: 6 · 2018: 10 · 2017: 14 · 2016: 6 · 2015: 7 · 2014: 9 · 2013: 9 · 2012: 7
- FWCI
- 6.65
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological Studies and Exploration
- Keywords
- sequence stratigraphy, plate tectonics, Ventersdorp Supergroup, Hamersley Group, banded iron formations, Precambrian stratigraphy, Proterozoic
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