Calculated aqueous-solution-solid-solution relations in the low-temperature system CaO-MgO-FeO-CO2-H2O
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Fe/Ca/Mg carbonates have an innate tendency to form solid solutions, so they occur rather than pure components.
“These occur rather than the pure components because of the innate tendenc_y of Fe/Ca/Mg carbonates to form solid solu-tions.”
From A chemical model for evaporites on early Mars: Possible sedimentary tracers of the early climate and implications for exploration (1999) · cites this paper as Woods and Garrels, 1992
The degree of cation substitution depends upon the activity of the substituting cation in solution.
“The degree of cation substitution depends upon the activity of the substituting cation in solution [ Woods and Garrels, 1992].”
From A chemical model for evaporites on early Mars: Possible sedimentary tracers of the early climate and implications for exploration (1999) · cites this paper as Woods and Garrels, 1992
Cites
The Oceans; A Possible Source of Iron in Iron-Formations
Holland, H. D. (1973) · Economic Geology · doi:10.2113/gsecongeo.68.7.1169 · Cited by 365 · see citing works
Solid-solution aqueous-solution equilibria; thermodynamic theory and representation
Glynn, P. D., & Reardon, E. J. (1990) · American Journal of Science · doi:10.2475/ajs.290.2.164 · Cited by 219 · see citing works
Formation and solid solution behavior of Ca-rhodochrosites in marine muds of the Baltic deeps
Jakobsen, R., & Postma, D. (1989) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(89)90135-x · Cited by 96 · see citing works
Physico-chemical properties of MnCO3–CaCO3 and MnO–CaO solid solutions
Fubini, B., & Stone, F. S. (1983) · Journal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases · doi:10.1039/f19837901215 · Cited by 36 · see citing works
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Chemical divides and evaporite assemblages on Mars
Tosca, N. J., & McLennan, S. M. (2006) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.10.021 · Cited by 151 · see citing works
Catling, D. C. (1999) · Journal of Geophysical Research: Planets · doi:10.1029/1998je001020 · Cited by 148 · see citing works
Inorganic synthesis of Fe–Ca–Mg carbonates at low temperature
Romanek, C. S., Jiménez-López, C., Navarro, A. R., Sánchez-Román, M., Sahai, N., & Coleman, M. (2009) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2009.05.065 · Cited by 94 · see citing works
- Authors
- Woods, T. L., & Garrels, R. M.
- Affiliations
- University of South Florida St. Petersburg (US)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1992-08
- Volume
- 56
- Issue
- 8
- Pages
- 3031-3043
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2043029640
- Cited by
- 29
- References
- 4
- Citations by year
- 2025: 2 · 2022: 1 · 2021: 1 · 2020: 1 · 2019: 1 · 2016: 1 · 2014: 1
- FWCI
- 1.36
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- calcite, ankerite, dolomite, siderite, magnesite, carbonate dissolution, equilibrium constants, Hamersley Basin
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
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