Pyroxmangite
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| Pyroxmangite | |
|---|---|
 Pyroxmangite from Chubu Region, Honshu Island, Japan | |
| General | |
| Category | Inosilicate |
| Formula (repeating unit) | MnSiO3 |
| Strunz classification | 09.DO.05 |
| Crystal symmetry | 1 pinacoidal |
| Unit cell | a = 9.69 Å, b = 10.5 Å, c = 17.39 Å; α = 112.17°, β = 102.85°, γ = 82.93°; V 1,596.00 ų; Z = 14 |
| Identification | |
| Color | pink, red, brown |
| Crystal system | Triclinic |
| Twinning | Lamellar on {010}, simple on {001} |
| Cleavage | Perfect on {110}, {110}, (110) ^ (110) = 92° poor on {010}, {001} |
| Fracture | hackly, uneven |
| Tenacity | brittle |
| Mohs scale hardness | 5½–6 |
| Luster | vitreous, pearly |
| Streak | colorless |
| Diaphaneity | transparent, translucent |
| Specific gravity | 3.8 |
| Birefringence | δ=0.018 |
| References | [1][2][3] |
Pyroxmangite has the general chemical formula of MnSiO3. [4] It is the high-pressure, low-temperature dimorph of rhodonite.[1]
It was first described in 1913 and named for the mineral group, pyroxenes, and is known as the manganese member.[5] It forms a series with pyroxferroite.
Pyroxmangite occurs in metamorphosed ore deposits rich in manganese. Associated minerals include spessartine, tephroite, alleghanyite, hausmannite, pyrophanite, alabandite, rhodonite and rhodochrosite.[3]
References
- ↑ 1.0 1.1 Ralph, Jolyon, and Ida Chao. "Pyroxmangite: Pyroxmangite Mineral Information and Data." MinDat.org
- ↑ Barthelmy, David. "The Mineral Pyroxmangite." minerals.net
- ↑ 3.0 3.1 Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W. and Nichols, Monte C. (ed.). "Pyroxmangite" (PDF). Handbook of Mineralogy. II (Silica, Silicates). Chantilly, VA, US: Mineralogical Society of America. ISBN 0962209716. Retrieved December 5, 2011.
- ↑ Pinckney, Linda R, and Charles W Burnham. "High-Temperature crystal structure of pyroxmangite." American Mineralogist 73 (1988): 809–817. GeoScienceWorld. Web. 13 September 2010.
- ↑ Ford, W.E. and Bradley, W.M. (1913). "Pyroxmangite, a new member of the pyroxene group and its alteration product, skemmatite". American Journal of Science 36: 169–174. doi:10.2475/ajs.s4-36.212.169.
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