Homilite

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Short description: Borosilicate mineral
Homilite
General
CategoryNesosilicate
Formula
(repeating unit)
Ca2(Fe2+,Mg)B2Si2O10
Strunz classification8/B.29-30
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
Space groupP21/b
Unit cella = 9.78 Å,
b = 7.61 Å,
c = 4.78 Å; β = 90.56°; Z = ?
Identification
ColorGreenish to brownish black
Mohs scale hardness5–​5 1⁄2
|re|er}}Vitreous, resinous
DiaphaneityOpaque
Specific gravity3.34
Optical propertiesBiaxial (+)
Refractive indexnα = 1.715 nβ = 1.725 nγ = 1.738
Birefringenceδ =
2V angleMeasured: 80°
References[1] [2] [3]

Homilite is a borosilicate mineral belonging to the gadolinite group of minerals with formula Ca
2
(Fe,Mg)B
2
Si
2
O
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.

References

  1. ↑ Mineral Society of America Handbook (PDF)
  2. ↑ Mindat with locations
  3. ↑ Webmineral data
  4. ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W. 
  5. ↑ 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. 





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