The system MgO–SiO2 has been studied at temperatures up to 1800°. The polymorphic relationships in magnesium metasilicate are discussed and evidence is offered for the possible existence of an additional phase in the high-temperature region of the system.
E. J. Duff, J. Chem. Soc. A, 1968, 2485 DOI: 10.1039/J19680002485
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