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Uranium isotope fractionation suggests oxidative uranium mobilization at 2.50 Ga
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“They attributed d 238 U values above average upper crustal values that coincide with Mo and Re enrichments (Anbar et al., 2007) to be indicative of the oxidative mobilization of U, possibly within the water column itself.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Kendall et al., 2013
In the citing paper
“Evidence from U isotopes (δ 238 U) in the Mt.McRae shale suggest U(IV) oxidation and mobilization as early as 2.5 Ga (Kendall et al., 2013).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Kendall et al., 2013
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Metadata
- Authors
- Kendall, B., Brennecka, G. A., Weyer, S., & Anbar, A. D.
- Affiliations
- University of Waterloo (CA)
- Lawrence Livermore National Laboratory (US)
- Leibniz University Hannover (DE)
- Arizona State University (US)
- Corresponding author
- Kendall, Brian
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2013-12
- Volume
- 362
- Pages
- 105-114
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W1993068557
- Cited by
- 124
- References
- 69
- Citations by year
- 2026: 6 · 2025: 7 · 2024: 6 · 2023: 5 · 2022: 7 · 2021: 9 · 2020: 9 · 2019: 15 · 2018: 11 · 2017: 14 · 2016: 10 · 2015: 12 · 2014: 9 · 2013: 4
- FWCI
- 7.94
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Funders
- National Science Foundation
- Agouron Institute
- NASA Astrobiology Institute
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- uranium isotope fractionation, authigenic uranium, Great Oxidation Event, Hamersley Basin, black shales, oxidative weathering
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