Homilite
Homilite is a borosilicate mineral belonging to the gadolinite group of minerals with formula Ca2(Fe,Mg)B2Si2O10.
| 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 |
| Luster | 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° |
It occurs as brown monoclinic crystals (space group P21/a[1]) 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.
References
- Miyawaki, R.; Nakai, I.; Nagashima, K. (15 January 1985). "Structure of homilite, Ca2.00(Fe0.90Mn0.03)B2.00Si2.00O9.86(OH)0.14". Acta Crystallographica Section C Crystal Structure Communications. 41 (1): 13–15. doi:10.1107/S010827018500261X.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.