Phase equilibria in the system MgO-MgF2-SiO2-H2O
The proportions of F and OH in synthetic talc, clinohumite, chondro-dite, norbergite, brucite, and sellaite have been determined by X-ray measurement of interplanar spacings. Unit cell refinement has been carried out on intermediate sellaite, approximate composition MgOHF. The compositions of coex...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/20654 |