Cuprospinel | |
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General | |
Category | Oxide mineral Spinel group |
Formula (repeating unit) | CuFe2O4 or (Cu,Mg)Fe2O4 |
Strunz classification | 4.BB.05 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Cubic Space group: Fd3m |
Identification | |
Formula mass | 239.23 g/mol |
Color | Black, gray in reflected light |
Crystal habit | Irregular grains, laminae intergrown with hematite |
Mohs scale hardness | 6.5 |
Luster | Metallic |
Streak | Black |
Diaphaneity | Opaque |
Specific gravity | 5 - 5.2 |
Optical properties | Isotropic |
Refractive index | n = 1.8 |
References | [1][2][3] |
Names | |
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IUPAC name
Copper(2+) bis[oxido(oxo)iron
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Other names
Copper iron oxide , cuprospinel, Copper diiron tetraoxide, Copper ferrite
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Identifiers | |
3D model (JSmol)
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ChemSpider | |
PubChem CID
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CompTox Dashboard (EPA)
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Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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Cuprospinel is a mineral. Cuprospinel is an inverse spinel with the chemical formula CuFe2O4, where copper substitutes some of the iron cations in the structure.[4][5] Its structure is similar to that of magnetite, Fe3O4, yet with slightly different chemical and physical properties due to the presence of copper.
The type locality of cuprospinel is Baie Verte, Newfoundland, Canada,[2][1] where the mineral was found in an exposed ore dump. The mineral was first characterized by Ernest Henry Nickel, a mineralogist with the Department of Energy, Mines and Resources in Australia, in 1973.[6][7] Cuprospinel is also found in other places, for example, in Hubei province, China[8] and at Tolbachik volcano in Kamchatka, Russia.[9]
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: CS1 maint: multiple names: authors list (link)