Gilalite

Gilalite is a copper silicate mineral with chemical composition of Cu5Si6O17·7(H2O).[3]

Gilalite
Blue Gilalite crystals
General
CategorySilicate mineral
Formula
(repeating unit)
Cu5Si6O17·7(H2O)
Strunz classification9.HE.05
Crystal systemMonoclinic
Unknown space group
Unit cella = 13.38, b = 19.16
c = 9.026 [Å]; β ≈ 90°; Z = 4
Identification
Formula mass884.3 g/mol
ColorBlue green, green
Crystal habitRaidiating fibrous in spherules
TenacityWaxy or gummy
Mohs scale hardness2
LusterNonmetallic
StreakLight green
DiaphaneityTranslucent
Specific gravity2.72
Optical propertiesBiaxial (-)
Refractive indexnα= 1.560 nβ=1.635 nΎ= 1.635
Birefringenceδ = 0.075
References[1][2][3]

It occurs as a retrograde metamorphic phase in a calc-silicate and sulfide skarn deposit. It occurs as fracture fillings and incrustations associated with diopside crystals.[2] It is commonly found in the form of spherules of radial fibers.

Gilalite inclusions within a quartz crystal from Juazeiro do Norte, Ceara State, Brazil (size: 7.1 x 4.7 x 2.7 cm)

It was first described for an occurrence in the Christmas porphyry copper mine in Gila County, Arizona in 1980 along with the mineral apachite.[4] It derives its name from this locality. It has also been reported from the Goodsprings District, Clark County, Nevada; Juazeiro do Norte, Ceara State, Brazil and a slag area in Lavrion District, Attica, Greece.[3]

References

  1. gilalite - Wolfram Alpha
  2. Handbook of Mineralogy
  3. Gilalite: Gilalite mineral information, Mindat.org
  4. F.P. Cesbron and S.A. Williams; March 1980;"Apachite and gilalite, two new copper silicates from Christmas, Arizona" Mineralogical Magazine, Vol. 43, pp. 639-41


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