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Oxygen isotope fractionation in magnetites: structural effect and oxygen inheritance
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It was hypothesized that the inverse spinel-structural magnetites used in isotopic exchange experiments can inherit the temperature dependence of oxygen isotope fractionation in the spinel-structural magnetite which formed by reducing a precursor hematite.
“It was hypothesized that the inverse spinel-structural magnetites used in isotopic exchange experiments can inherit the temperature dependence of oxygen isotope fractionation in the spinel-structural magnetite which formed by reducing a precursor hematite.”
From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Zheng (1995)
Zheng (1995) suggested that most magnetites could have the spinel-type structure in the first stage of their crystallization, although they are normally observed to occur in the inverse spinel-type structure in nature.
“According to a comprehensive study of oxygen isotope fractionation in magnetites, Zheng (1995) suggested that most magnetites could have the spinel-type structure in the first stage of their crystallization, although they are normally observed to occur in the inverse spinel-type structure in nature.”
From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Zheng (1995)
Citations
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Oxygen-isotope fractionation in titanium-oxide minerals at low temperature
Bird, M. I., Longstaffe, F. J., & Fyfe, W. S. (1993) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(93)90295-8 · Cited by 22
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Cited by
Sorted by citations
Oxygen isotope fractionation in carbonate and sulfate minerals.
Zheng, Y.-F. (1999) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.33.109 · Cited by 489
Self-citationOn the theoretical calculations of oxygen isotope fractionation factors for carbonate-water systems
ZHENG, Y.-F. (2011) · Geochemical Journal · doi:10.2343/geochemj.1.0125 · Cited by 49
“…isotope paleothermometer and thus the foundation of stable isotope geochemistry was triggered by the theoretical prediction of Urey (1947) on the temperature dependence of 342 Y.-F. Zheng been successfully calculated by the increment method (Zheng, 1991, 1993a, 1993b, 1995, 1996, 1997, 1998, 1999).”
MethodSelf-citationCole, D. R., Horita, J., Polyakov, V. B., Valley, J. W., Spicuzza, M. J., & Coffey, D. W. (2004) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2004.02.017 · Cited by 45
Metadata
- Authors
- Zheng, Y.-F.
- Affiliations
- University of Science and Technology of China (CN)
- Corresponding author
- Zheng, Yong-Fei
- ORCID
- Zheng, Yong-Fei
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 1995-04
- Volume
- 121
- Issue
- 1-4
- Pages
- 309-316
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2039773351
- Cited by
- 46
- References
- 1
- Citations by year
- 2026: 1 · 2025: 4 · 2024: 1 · 2022: 1 · 2021: 1 · 2020: 2 · 2019: 3 · 2017: 3 · 2015: 2 · 2014: 2 · 2013: 1
- FWCI
- 1.08
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Funders
- Chinese Academy of Sciences
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Mineralogy and Gemology Studies
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- oxygen isotope fractionation, magnetite, spinel-like structure, hematite, secondary mineral formation
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