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“However, questions regarding the fractionation processes are still under investigation [51].”
From Isotope chemistry to trace carbon mineralization in construction materials (2026) · cites this paper as [51]
In the citing paper
“This approach has been shown to yield accurate temperatures of formation for a wide range of geologic environments and synthetic carbonates.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Eiler et al., 2014
In the citing paper
“Most natural and synthetic carbonates precipitate at or near homogenous isotope exchange equilibrium with respect to the carbonate ion contained in the mineral phase ( cf . Eq. (2) and Fig. A2) ( e.g. , Eiler, 2011) and yield clumped-isotope temperatures generally consistent with expected formation temperatures ( e.g. , Eiler et al., 2014).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Eiler et al., 2014
In the citing paper
“Comparable to calcium carbonate speleothems, nesquehonite records clumped-isotope compositions that result in anomalously warmer temperatures related to kinetic factors associated with dehydroxylation (Eiler et al., 2014) or dehydration (Affek and Zaarur, 2014) of HCO3 and ensuing CO2 degassing.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Eiler et al., 2014
In the citing paper
“Although it is possible that cryptocrystalline magnesite may form in disequilibrium with the mineralizing solution, so far the maximum isotopic disequilibrium that yields lower than expected temperatures in carbonates is recorded in surface corals at 10 ° C (Eiler et al., 2014) and the olivine-magnesite experiments at 15 ° C, which may exhibit pH disequilibrium effects (Section 5.1).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Eiler et al., 2014
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Metadata
- Authors
- Eiler, J. M., Bergquist, B., Bourg, I., Cartigny, P., Farquhar, J., Gagnon, A., Guo, W., Halevy, I., Hofmann, A., Larson, T. E., Levin, N., Schauble, E. A., & Stolper, D.
- Affiliations
- California Institute of Technology (US)
- University of Toronto (CA)
- Lawrence Berkeley National Laboratory (US)
- Institut de physique du globe de Paris (FR)
- University of Maryland, College Park (US)
- Woods Hole Oceanographic Institution (US)
- Weizmann Institute of Science (IL)
- Franklin & Marshall College (US)
- The University of Texas at Austin (US)
- Johns Hopkins University (US)
- University of California, Los Angeles (US)
- Corresponding author
- Eiler, John M.
- ORCID
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2014-04
- Volume
- 372
- Pages
- 119-143
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2161266592
- Cited by
- 121
- References
- 306
- Citations by year
- 2026: 3 · 2025: 2 · 2024: 10 · 2023: 8 · 2022: 1 · 2021: 9 · 2020: 8 · 2019: 11 · 2018: 21 · 2017: 10 · 2016: 17 · 2015: 14 · 2014: 4
- FWCI
- 12.67
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- CaltechAUTHORS (California Institute of Technology) (submittedVersion)
- Funders
- Basic Energy Sciences
- U.S. Department of Energy
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- stable isotope geochemistry, organic compounds, kinetic isotope effects, vibrational isotope effects, nuclear isotope effects
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