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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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Detalhes bibliográficos
Main Authors: Xu, Jie, Yan, Chao, Zhang, Fangfu, Konishi, Hiromi, Xu, Huifang, Teng, H. Henry
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2013
Assuntos:
Acesso em linha: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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