Osumilite

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Osumilite
Osumilite tablets with mullite from Ochtendung, Eifel, Germany.
General
CategoryCyclosilicate
Formula
(repeating unit)
(K,Na)(Fe,Mg)2(Al,Fe)3(Si,Al)12O30·H2O
Strunz classification09.CM.05
Dana classification63.02.01a.06
Crystal systemHexagonal; 6/m 2/m 2/m.
Space groupHexagonal 6/m 2/m 2/m
Unit cella = 10.15 Å, c = 14.25 Å; Z = 2
Identification
ColorBlack, dark blue, dark brown, pink, gray
Crystal habitCrystals tabular to prismatic also anhedral and massive
TwinningRarely
CleavageNone
FractureSubconchoidal
Mohs scale hardness5 - 6
LusterVitreous
StreakBlue-gray
Specific gravity2.62 - 2.64
Optical propertiesUniaxial (+) anomalously biaxial
Refractive indexw=1.545-1.547, e=1.549-1.551
Birefringence0.004
PleochroismStrong
References[1][2][3]

Osumilite a very rare hydrate potassium-sodium-iron-magnesium-aluminium silicate mineral. Osumilite is part of the milarite group (also known as the milarite-osumilite group) of cyclosilicates.

Characteristics

Osumilite chemical formula is (K,Na)(Fe,Mg)2(Al,Fe)3(Si,Al)12O30·H2O. It is translucent and the typical coloring is either blue, black, brown, or gray. It displays no cleavage and has a vitreous luster. Osumilite has a hardness between 5-6 on the Mohs hardness scale.[3]

The hexagonal crystal structure of osumilite is an unusual molecular make-up. The primary unit is a double ring, with a formula of Si12O30. Normal cyclosilicate have rings composed of six silicate tetrahedrons; Si6O18. In a double ring structure, two normal rings are linked by sharing six oxygens, one from each tetrahedron in each six membered ring.[4]

Occurrence

Osumilite, was first discovered as grains in volcanic rocks near Osumi, Japan. It was confused with a similar mineral cordierite because of their similar coloring. It can be found in high-grade metamorphic rocks, xenoliths and in the groundmass of rhyolite and dacite.[2]

Osumilite is found in the Obsidian Cliffs, Oregon; Sardinia, Italy; Kagoshima and Yamanashi Prefecture, Japan; and the Eifel district in Germany.[2]

See also

References