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Redetermination of ruizite, Ca(2)Mn(3+) (2)[Si(4)O(11)(OH)(2)](OH)(2)·2H(2)O
The crystal structure of ruizite, ideally Ca(2)Mn(3+) (2)[Si(4)O(11)(OH)(2)](OH)(2)·2H(2)O [dicalcium dimanganese(III) tetrasilicate tetrahydroxide dihydrate] was first determined in space group A2 with an isotropic displacement parameter model (R = 5.6%) [Hawthorne (1984 ▸). Tschermaks Mineral. P...
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| 發表在: | Acta Crystallogr E Crystallogr Commun |
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| Main Authors: | , , |
| 格式: | Artigo |
| 語言: | Inglês |
| 出版: |
International Union of Crystallography
2016
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| 主題: | |
| 在線閱讀: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4992915/ https://ncbi.nlm.nih.gov/pubmed/27555940 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1107/S2056989016009129 |
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