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Antimony oxide mineral From Wikipedia, the free encyclopedia
Stibiconite is an antimony oxide mineral with formula: Sb3O6(OH). Its name originates from Greek stíbi (στίβι), 'antimony' and kónis (κόνις), 'powder', alluding to its composition and habit.[2][3][4] It is a member of the pyrochlore super group.
Stibiconite | |
---|---|
General | |
Category | Oxide minerals |
Formula (repeating unit) | Sb3+Sb5+2O6(OH) |
IMA symbol | Sbc[1] |
Strunz classification | 4.DH.20 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Fd3m |
Unit cell | a = 10.27 Å; Z = 8 |
Identification | |
Formula mass | 478.25 g/mol |
Color | Pale yellow to yellowish white, reddish white, orange; gray, brown, black when impure |
Crystal habit | Massive, botryoidal, as incrustations, powdery |
Cleavage | None |
Fracture | Uneven |
Mohs scale hardness | 4–5 |
Luster | Vitreous to dull |
Streak | light yellow |
Diaphaneity | Transparent to translucent |
Specific gravity | 4.1 – 5.8, Average = 4.94 |
Optical properties | Isotropic |
Refractive index | n = 1.6–1.97 |
References | [2][3][4] |
It was first described in 1862 for an occurrence in the Brandholz – Goldkronach District, Fichtel Mountains, Bavaria, Germany.[3]
It occurs as a secondary alteration product of other hydrothermal antimony minerals such as stibnite. It occurs in association with cervantite, valentinite, kermesite, native antimony and stibnite.[4]
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