Publication: Closing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonates
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© Author(s) 2019. CC Attribution 4.0 license.
Abstract
The oxygen isotopic fractionation between water and calcite is the cornerstone for estimating the formation temperature of calcite [1, 2, 3]. The oxygen isotope thermometer is one of the most valuable tools in geothermometry, palaeoclimatology and palaeoceanography
Citation
Breitenbach, S. F. M., Hartland, A., Brall, N. S., Sharp, W. D., & Gazquez, F. (2019). Closing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonates. In European Geosciences Union General Assembly 2019 (Vol. 21, pp. 6196–6196). Conference held Vienna, Austria.