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Osumilite
Cyclosilicate mineral
Cyclosilicate mineral
| Field | Value |
|---|---|
| name | Osumilite |
| category | Cyclosilicate |
| image | Osumilite tablets with Mullite - Ochtendung, Eifel, Germany.jpg |
| imagesize | 260px |
| caption | Osumilite tablets with mullite from Ochtendung, Eifel, Germany. |
| formula | |
| IMAsymbol | Osm |
| dana | 63.02.01a.06 |
| strunz | 9.CM.05 |
| system | Hexagonal |
| class | Dihexagonal dipyramidal (6mmm) |
| H-M symbol: (6/m 2/m 2/m) | |
| symmetry | *P6/mcc* |
| unit cell | a = 10.15, c = 14.25 [Å]; Z = 2 |
| color | Black, dark blue, dark brown, pink, gray |
| habit | Crystals tabular to prismatic also anhedral and massive |
| twinning | Rarely |
| cleavage | None |
| fracture | Subconchoidal |
| mohs | 5 - 6 |
| diaphaneity | Translucent |
| luster | Vitreous |
| refractive | w=1.545-1.547, e=1.549-1.551 |
| opticalprop | Uniaxial (+) anomalously biaxial |
| birefringence | 0.004 |
| pleochroism | Strong |
| streak | Blue-gray |
| gravity | 2.62 - 2.64 |
| references |
H-M symbol: (6/m 2/m 2/m)
Osumilite is a very rare 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 . 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.
The hexagonal crystal structure of osumilite is an unusual molecular make-up. The primary unit is a double ring, with a formula of . Normal cyclosilicate have rings composed of six silicate tetrahedrons; . In a double ring structure, two normal rings are linked by sharing six oxygens, one from each tetrahedron in each six membered ring.
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.
Osumilite is found in the Obsidian Cliffs, Oregon; Sardinia, Italy; Kagoshima and Yamanashi Prefecture, Japan; and the Eifel district in Germany. Osumilite pseudomorphs are known from a number of ultrahigh-temperature rocks, including those of southern Madagascar.
References
References
- Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
- "Osumilite: Mineral information, data and localities.".
- Don S. Goldman, George R. Rossman (1978): ''The site distribution of iron and anomalous biaxiality in osumilite'', In: ''American Mineralogist'', 63, S. 490-498 ([http://www.minsocam.org/ammin/AM63/AM55_490.pdf (PDF, 961 kB)]{{dead link. (March 2018)
- E. Olsen, T. E. Bunch (1970): ''Compositions Of Natural Osumilites'', In: ''The American Mineralogiste'', 55, S. 875 - 879 ([http://www.minsocam.org/ammin/AM55/AM55_875.pdf (PDF, 328 kB)])
- "Osumilite-(Mg) Mineral Data".
- http://www.galleries.com/minerals/silicate/osumilit/osumilit.htm ''Mineral Galleries''
- http://www.handbookofmineralogy.org/pdfs/osumilite.pdf ''Handbook of Mineralogy''
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