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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