The stability of Fe5O6 and Fe4O5 at high pressure and temperature
Abstract
The oxygen fugacity in the interior of the Earth is largely controlled by iron-bearing minerals. Recent studies have reported various iron oxides with chemical compositions between FeO and Fe3O4 above ~10 GPa. However, the stabilities of these high-pressure iron oxides remain mostly uninvestigated. In this study, we performed in situ X-ray diffraction (XRD) measurements in a laser-heated diamond-anvil cell (DAC) to determine the phase relations...
Paper Details
Title
The stability of Fe5O6 and Fe4O5 at high pressure and temperature
Published Date
Sep 1, 2019
Journal
Volume
104
Issue
9
Pages
1356 - 1359
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