Phase equilibria in the systems Fe 2 O 3 -MgO-TiO 2 and FeO-MgO-TiO 2 between 1173 and 1473 K, and Fe 2+ -Mg mixing properties of ilmenite, ferrous-pseudobrookite and ulvöspinel solid solutions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s004100050506.pdf
Cited by 18 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. Trace element partitioning between clinopyroxene, magnetite, ilmenite and ferrobasaltic to dacitic magmas: an experimental study on the role of oxygen fugacity and melt composition;Contributions to Mineralogy and Petrology;2022-09
2. Perovskite Formation in Hematite–Ilmenite Ores Sintered in Argon;Journal of Sustainable Metallurgy;2022-01-21
3. Gaseous Reduction Behavior of Primary Ilmenite at Temperatures Between 1273 K and 1473 K;Metallurgical and Materials Transactions B;2021-11-30
4. Effects and mechanism of MgO on carbothermal reduction of Fe2TiO4;Metallurgical Research & Technology;2021
5. Addition of TiO2 and Ti2O3 to the Al2O3-FeO-Fe2O3-MgO system;Calphad;2018-09
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