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Closing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonates

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
Type
Conference Contribution
Type of thesis
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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.
Date
2019
Publisher
Degree
Supervisors
Rights
© Author(s) 2019. CC Attribution 4.0 license.