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• W2023391438 startingPage "1527" @default.
• W2023391438 abstract "Structural phase transitions of iron oxide (Fe2O3) have been investigated at pressures up to 70 GPa and temperatures above 2500 K, using a laser-heated diamond anvil cell technique. A phase transition between α-Fe2O3 (hematite) and perovskite-type Fe2O3 was observed at about 30 GPa. At pressures higher than 50 GPa, we also observed the occurrence of a new high-pressure phase of Fe2O3. Diffraction peaks of the new high-pressure phase can be indexed on the basis of orthorhombic or monoclinic symmetries that are denser than other known Fe2O3 phases. The volume change from perovskite-type to the new high-pressure phase is about 7%." @default.
• W2023391438 created "2016-06-24" @default.
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• W2023391438 date "2004-08-01" @default.
• W2023391438 modified "2023-10-09" @default.
• W2023391438 title "High-pressure phase transition of hematite, Fe2O3" @default.
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• W2023391438 doi "https://doi.org/10.1016/j.jpcs.2003.11.042" @default.
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