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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...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| 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 |