glaserite


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glaserite

[′gla·zə‚rīt]
(mineralogy)
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References in periodicals archive ?
2] can be considered to have the closest similarity to the glaserite structure.
However, since [alpha]-TCP does not have a 2:1 cation-anion ratio, its emulation of the glaserite structure requires cation vacancies with the formula [Ca.
3-] columns, reminiscent of the glaserite structure.