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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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Bibliografiske detaljer
Udgivet i:Acta Crystallogr E Crystallogr Commun
Main Authors: Fendrich, Kim V., Downs, Robert T., Origlieri, Marcus J.
Format: Artigo
Sprog:Inglês
Udgivet: International Union of Crystallography 2016
Fag:
Online adgang: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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