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Oxygen metal-silicate equilibria

In polymeric models for silicate melts, it is postulated that, at each composition, for given values of P and T, the melt is characterized by an equilibrium distribution of several ionic species of oxygen, metal cations, and ionic polymers of monomeric units SiOt. ... [Pg.412]

See other pages where Oxygen metal-silicate equilibria is mentioned: [Pg.341]    [Pg.341]    [Pg.473]    [Pg.309]    [Pg.46]    [Pg.309]    [Pg.307]    [Pg.1372]    [Pg.52]    [Pg.293]    [Pg.768]    [Pg.1233]    [Pg.1234]    [Pg.1680]    [Pg.65]    [Pg.536]    [Pg.537]    [Pg.60]    [Pg.243]    [Pg.1133]    [Pg.92]    [Pg.44]    [Pg.4]   
See also in sourсe #XX -- [ Pg.428 ]



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Metal oxygen

Oxygen equilibrium

Oxygen silicates

Silicate equilibria

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