Stilpnomelane
Stilpnomelane is a phyllosilicate mineral. It has the chemical formula K(Fe2+,Mg,Fe3+)8(Si,Al)12(O,OH)27·n(H2O).[4]
Stilpnomelane | |
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General | |
Category | Phyllosilicates Smectite group |
Formula (repeating unit) | K(Fe2+,Mg,Fe3+)8(Si,Al)12(O,OH)27·n(H2O) |
IMA symbol | Stp[1] |
Strunz classification | 9.EG.40 |
Crystal system | Triclinic |
Crystal class | Pinacoidal (1) (same H-M symbol) |
Space group | P1 |
Unit cell | a = 21.72 Å, b = 21.72 Å c = 17.4 Å; α = 124.14° β = 95.86°, γ = 120°; Z = 6 |
Identification | |
Color | Black, greenish black, yellowish bronze, greenish bronze |
Crystal habit | Platey, scaly and fibrous with comb structures; radiating groups |
Cleavage | Perfect on {001}, imperfect on {010} |
Tenacity | Brittle |
Mohs scale hardness | 3 - 4 |
Luster | Vitreous to dull |
Streak | Gray white |
Diaphaneity | Subtranslucent to opaque |
Specific gravity | 2.77 - 2.96 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.543 - 1.634 nβ = 1.576 - 1.745 nγ = 1.576 - 1.745 |
Birefringence | δ = 0.033 - 0.111 |
Pleochroism | X: bright golden yellow to pale yellow Y and Z: deep reddish brown, to deep green to nearly black |
2V angle | 0-40 measured |
Dispersion | None |
References | [2][3][4] |
Stilpnomelane occurs associated with banded iron formations. It is a metamorphic mineral associated with the blueschist and greenschist facies.[2]
It was first described in 1827 for an occurrence in Moravia in the Czech Republic. The name is derived from the Greek stilpnos for shining, and melanos for black.[3]
References
- Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- Handbook of Mineralogy
- Stilpnomelane on Mindat
- Stilpnomelane on Webmineral
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