Pyroxmangite | |
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General | |
Category | Inosilicate |
Formula (repeating unit) | MnSiO3 |
IMA symbol | Pxm[1] |
Strunz classification | 9.DO.05 |
Crystal system | Triclinic |
Crystal class | Pinacoidal (1) (same H-M symbol) |
Space group | C1 |
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 Å3; Z = 28 |
Identification | |
Color | pink, red, brown |
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 | 5+1⁄2 – 6 |
Luster | vitreous, pearly |
Streak | colorless |
Diaphaneity | transparent, translucent |
Specific gravity | 3.8 |
Birefringence | δ=0.018 |
Other characteristics | morphology: tabular crystals, granular massive, grainy |
References | [2][3][4] |
Pyroxmangite has the general chemical formula of MnSiO3.[5] It is the high-pressure, low-temperature dimorph of rhodonite.[2]
It was first described in 1913 and named for the mineral group, pyroxenes, and is known as the manganese member.[6] 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.[4]