Oxygen isotope study of a Precambrian banded iron-formation, Hamersley Range, Western Australia
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The correctness of the low-temperature correction has been verified by synthesis experiments on the rutile-water system and theoretical calculations on the magnetite-water system.
“The correctness of the lowtemperature correction has been verified by the synthesis experiments of Bird et al. (1993) on the rutile-water system and the theoretical calculations of Becker and Clayton (1976) on the magnetitewater system.”
From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Becker and Clayton (1976)
Bulk mineral separates of hematite, magnetite, and quartz from the Dales Gorge Member have average δ18O values of ~ -2‰, ~ +3‰, and ~ +21‰, respectively.
“Bulk mineral separates of hematite, magnetite, and quartz from the Dales Gorge Member have average δ 18 O values of ~ -2‰, ~ +3‰, and ~ +21‰, respectively”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Becker and Clayton, 1976
On average, hematite formed at a lower temperature than magnetite in the Dales Gorge Member.
“indicating that on average, hematite formed at a lower temperature than magnetite (Becker and Clayton, 1976)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Becker and Clayton, 1976
Hematite in the Dales Gorge Member underwent negligible change in oxygen isotopes.
“Hematite, on the other hand, underwent negligible change in oxygen isotopes.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Becker and Clayton (1976)
Becker and Clayton (1976) noted isotopic exchange between minerals within the Dales Gorge Member at burial metamorphic temperatures of 270 to 310 oC, and suggested that oxygen isotopes in quartz and carbonate may have equilibrated completely.
“Based on bulksample analysis, Becker and Clayton (1976) noted isotopic exchange between minerals within the Dales Gorge Member at burial metamorphic temperatures of 270 to 310 o C, and suggested that oxygen isotopes in quartz and carbonate may have equilibrated completely.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Becker and Clayton (1976)
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References 58 · Cited by 216
- Authors
- Becker, R. H., & Clayton, R. N.
- Affiliations
- University of Chicago (US)
- ORCID
- Becker, Richard H
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1976-10
- Volume
- 40
- Issue
- 10
- Pages
- 1153-1165
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2047660877
- Cited by
- 216
- References
- 58
- Citations by year
- 2026: 1 · 2025: 2 · 2024: 2 · 2023: 4 · 2022: 1 · 2021: 2 · 2020: 5 · 2019: 6 · 2018: 3 · 2017: 9 · 2016: 5 · 2015: 6 · 2014: 2 · 2013: 4 · 2012: 1
- FWCI
- 11.41
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Funders
- Geochemical Society (1833-1834)
- 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 › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- oxygen isotopes, banded iron formations, Precambrian, Hamersley Range, oxygen isotope fractionation, burial metamorphism, magnetite, hematite, siderite, riebeckite, talc, chert
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