Homilite | |
---|---|
General | |
Category | Nesosilicate |
Formula (repeating unit) | Ca2(Fe2+,Mg)B2Si2O10 |
Strunz classification | 8/B.29-30 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) |
Space group | P21/b |
Unit cell | a = 9.78 Å, b = 7.61 Å, c = 4.78 Å; β = 90.56°; Z = ? |
Identification | |
Color | Greenish to brownish black |
Mohs scale hardness | 5–5 1⁄2 |
|re|er}} | Vitreous, resinous |
Diaphaneity | Opaque |
Specific gravity | 3.34 |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.715 nβ = 1.725 nγ = 1.738 |
Birefringence | δ = |
2V angle | Measured: 80° |
References | [1] [2] [3] |
Homilite is a borosilicate mineral belonging to the gadolinite group of minerals with formula Ca
2(Fe,Mg)B
2Si
2O
10.
It occurs as brown monoclinic crystals (space group P21/a[5]) within feldspar masses in pegmatite and was discovered in 1876 in Stoko island, Langesundfiord, Norway . The name is from the Greek for to occur together, in allusion to its association with meliphanite and allanite.
Original source: https://en.wikipedia.org/wiki/Homilite.
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