Magnetic properties of the Fe2SiO4-Fe3O4 spinel solid solutions

Physics and Chemistry of Minerals

Volumn 28, Issue 2, 2001, Pages 102-109

  Yamanaka, T ^a   Okita, M ^a  

^a OSAKA UNIVERSITY   (Japan)

Author keywords

Bohr magneton; Curie temperature; Fe3 xSixO4 spinel solid solution; Magnetic hysteresis; Saturation magnetization

Indexed keywords

CATION; CURIE POINT; HYSTERESIS; MAGNETIC PROPERTY; SOLID SOLUTION; SPINEL;

EID: 0034916607     PISSN: 03421791     EISSN: None     Source Type: Journal    
DOI: 10.1007/s002690000135     Document Type: Article

References (28)

1. 4, at high pressures and temperatures: Spinelloids with spinel-related structures
2. Influence of nonstoichiometry on the Verwey transition
3. 3) solid solution: Determinations of Fe-Ti order from magnetic properties
4. 4 at 7 GPa
5. The system iron-oxygen 1. The wüstite field and related equilibria
6. 4
7. Magnetic properties of the magnetic-spinel solid solution: Saturation magnetization and cation distributions
8. Structure of nickel aluminosilicate (phase V): A high-pressure phase related to spinel
9. Phase transformation in primitive MORB and pyrolite compositions to 25 GPa and some geophysical implications
10. 4 and vacancy-doped magnetite
11. 4 (olivine analogue): Stability and implications to mantle mineralogy
12. Isothermal compression of magnetite to 320 kbar and pressure-induced phase transformation
13. 4
14. 4
15. Calculation of effect of cation disorder on silicate spinel phase boundaries
16. 4 system under high pressure
17. 4 at 7 and 9 GPa and the oxidation state of the transition zone
18. 3+ content
19. High-pressure phase of magnetite
20. 4
21. 4
22. 4) and its transition point at low temperatures
23. 4 and implications for the Earth's mantle
24. 4 as a function of temperature and heating duration
25. 4 solid solution under pressures up to 12 GPa
26. 4 spinel solid solutions