Pyroxmangite
Pyroxmangite | |
---|---|
Pyroxmangite from Chubu Region, Honshu Island, Japan | |
General | |
Category | Inosilicate |
Formula (repeating unit) | MnSiO3 |
Strunz classification | 09.DO.05 |
Crystal system | Triclinic |
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 symmetry | 1 pinacoidal |
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 2 Ralph, Jolyon, and Ida Chao. "Pyroxmangite: Pyroxmangite Mineral Information and Data." MinDat.org
- ↑ Barthelmy, David. "The Mineral Pyroxmangite." minerals.net
- 1 2 Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W. and Nichols, Monte C. (ed.). "Pyroxmangite". Handbook of Mineralogy (PDF). 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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