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Testing the cation-hydration effect on the crystallization of Ca–Mg–CO(3) systems
Dolomite and magnesite are simple anhydrous calcium and/or magnesium carbonate minerals occurring mostly at Earth surfaces. However, laboratory synthesis of neither species at ambient temperature and pressure conditions has been proven practically possible, and the lack of success was assumed to be...
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| Autores principales: | , , , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
National Academy of Sciences
2013
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3816432/ https://ncbi.nlm.nih.gov/pubmed/24127571 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1307612110 |
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