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A hydrothermal investigation of the system FeOFe2O3TiO2: A discussion with new data
Authors:Donald H Lindsley  Anders Lindh
Institution:1. Dept. of Earth and Space Sciences, State University of New York, Stony Brook, New York 11790, USA;2. Dept. of Geology, Uppsala University, Box 555, S-751 22 Uppsala 1, Sweden
Abstract:New experimental data on the system FeOFe2O2TiO2 using a new oxygen buffer are presented. It is found that there is a narrow range of oxygen fugacity above 550°C within which hematite and ilmenite coexist stably.
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