PHASE EQUILIBRIA IN THE SYSTEMS FE2O3-MGO-TIO2 AND FEO-MGO-TIO2 BETWEEN 1173 AND 1473 K, AND FE2+-MG MIXING PROPERTIES OF ILMENITE, FERROUS-PSEUDOBROOKITE AND ULVOSPINEL SOLID SOLUTIONS

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dc.contributor.author Pownceby M.I.
dc.contributor.author Fisher-White M.J.
dc.date.accessioned 2021-01-10T10:33:40Z
dc.date.available 2021-01-10T10:33:40Z
dc.date.issued 1999
dc.identifier https://elibrary.ru/item.asp?id=1012493
dc.identifier.citation Contributions to Mineralogy and Petrology, 1999, , 2, 198-211
dc.identifier.issn 0010-7999
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/22559
dc.description.abstract Detailed phase relations have been determined within the systems Fe2O3-MgO-TiO2 and FeO-MgO-TiO2. Experiments were performed over the temperature interval 1173-1473 K by equilibrating pelletized, fine-grained oxide mixtures in either inert calcia-stabilized zirconia pots (Fe2O3-MgO-TiO2 system) or evacuated silica tubes (FeO-MgO-TiO2 system). Equilibrium phase assemblages were determined by combined optical microscope, X-ray diffraction and EMP examination. Phase relations in the Fe2O3-MgO-TiO2 ternary are dominated by the instability of the M2O3 solid solution relative to the phase assemblage M3O4 + M3O5. A miscibility gap along the M2O3 binary also gives rise to two, 3-phase fields (α-M2O3 + M3O5 + M3O4 and α'-M2O3 + M3O5 + M3O4) separated by the M3O4 + M3O5 phase field. Phase relations in the FeO-MgO-TiO2 ternary were divided into two sub-systems. For the FeTiO3-MgTiO3-TiO2 sub-ternary, there is complete solid solution along the M2O3 and M3O5 binary joins at high temperature. At low temperatures (T < 1373 K) the M3O5 pseudobrookite solid solution decomposes to M2O3 + TiO2. Increasing the concentration of MgO in M3O5 phase results in a decrease in the temperature at which M3O5 becomes unstable and compositional tie lines linking M2O3 and TiO2 fan out, before the appearance of a three-phase region where M2O3, M3O5, and TiO2 coexist. Within the expanded FeO-MgO-TiO2 system, at temperatures above ~1273 K there is a continuous solid solution along the M3O4 binary. At low temperatures (T < 1273 K) the Mg2TiO4 end-member breaks down to MgO and MgTiO3. The M3O4 phase shows significant non-stoichiometry, down to at least 1173 K. Fe2+-Mg partitioning data were obtained for coexisting M2O3-M3O5 and M2O3-M3O4 pairs in the FeO-MgO-TiO2 ternary. Assuming a regular solution mixing model for all phases, the M2O3 and M3O4 solid solutions were both found to exhibit moderate positive deviations from ideality (~2600 J/mol), whereas the data for the M3O5 binary suggest close to ideal behaviour.
dc.title PHASE EQUILIBRIA IN THE SYSTEMS FE2O3-MGO-TIO2 AND FEO-MGO-TIO2 BETWEEN 1173 AND 1473 K, AND FE2+-MG MIXING PROPERTIES OF ILMENITE, FERROUS-PSEUDOBROOKITE AND ULVOSPINEL SOLID SOLUTIONS
dc.type Статья


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