Topotactical Relationships Between Hematite α-Fe2O3 and the Magnetite Fe3O4 Which is Formed on it by Thermal Decomposition Under Low Oxygen Pressure
- 1 January 1968
- book chapter
- Published by Springer Nature
Abstract
No abstract availableThis publication has 2 references indexed in Scilit:
- Magnetite: Preferred Orientation on the Basal Plane of Partially Reduced HematiteScience, 1963
- An Electron Diffraction Study of the Effects of Heat Treatment on -Fe2O3(Haematite) Single CrystalsProceedings of the Physical Society, 1960