Maghemite | |
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Maghemite from Gancedo, Chaco Province, Argentina
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General | |
Category | Oxide minerals |
Formula (repeating unit) |
γ-Fe2O3 |
Strunz classification | 4.BB.15 |
Crystal system | Cubic with a tetragonal supercell |
Crystal class | Gyroidal (432) (same H-M symbol) |
Space group | P4132, P4332 |
Unit cell | a = 8.33 Å; Z = 8 or a = 8.35 Å c = 24.99 Å; Z = 8 for tetragonal supercell |
Identification | |
Color | Brown, bluish black; brown to yellow in transmitted light; white to bluish gray in reflected light. |
Crystal habit | Rarely as minute octahedral crystals, or acicular overgrowths; commonly as coatings on or replacements of magnetite; massive. |
Cleavage | None |
Fracture | Subconchoidal |
Mohs scale hardness | 5 |
Luster | Dull |
Streak | Brown |
Diaphaneity | Opaque, transparent in thin fragments |
Specific gravity | 4.860 (calculated) |
Optical properties | Isotropic |
Other characteristics | Strongly magnetic |
References |
Maghemite (Fe2O3, γ-Fe2O3) is a member of the family of iron oxides. It has the same spinel ferrite structure as magnetite and is also ferrimagnetic.
Maghemite can be considered as an Fe(II)-deficient magnetite with formula where represents a vacancy, A indicates tetrahedral and B octahedral positioning.