Most Earth-surface calcites precipitate out of isotopic equilibrium

Oxygen-isotope thermometry played a critical role in the rise of modern geochemistry and remains extensively used in (bio-)geoscience. Its theoretical foundations rest on the assumption that (18)O/(16)O partitioning among water and carbonate minerals primarily reflects thermodynamic equilibrium. How...

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Detalles Bibliográficos
Autores principales: Daëron, M., Drysdale, R. N., Peral, M., Huyghe, D., Blamart, D., Coplen, T. B., Lartaud, F., Zanchetta, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6347637/
https://www.ncbi.nlm.nih.gov/pubmed/30683869
http://dx.doi.org/10.1038/s41467-019-08336-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6347637/
https://www.ncbi.nlm.nih.gov/pubmed/30683869
http://dx.doi.org/10.1038/s41467-019-08336-5

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