Editorial Feature

Calciocopiapite - Occurrence, Properties, and Distribution

Calciocopiapite is a member of the Copiapite group of minerals. It is so called because it is a calcium member of the copiapite group.

Properties of Calciocopiapite

The following are the key properties of Calciocopiapite:

  • Cell Data
    Space Group: [P1] (by analogy to copiapite; ICDD 27-77)
    • a = 7.35
    • b = 18.21
    • c = 7.01
    • α = 85.52°
    • β = 103.55°
    • γ = 100.62°

  • Crystal Data
    • Triclinic
    • Point Group: 1
    • As powdery crusts
    • X-ray powder pattern: 3.108 (10), 3.027 (10), 2.809 (10), 1.860 (10), 3.458 (9), 1.267 (9), 1.244 (9)

  • Chemical Composition
    Elements Content 1 Content 2
    SO3 39.00 38.92
    H2O 29.30 30.66
    Fe2O3 26.25 25.88
    CaO 4.85 4.54
    MgO 0.32
    insol. 0.40
    Total 100.12 100.00

  • Optical Properties
    • Optical Class: Biaxial
    • α = n.d
    • β = n.d
    • γ = n.d
    • 2V(meas.) = n.d

  • Estimated Properties
    Electron density Bulk density (electron density) = 2.26 g/cm3
    note: Specific gravity of Calciocopiapite = 2.22 g/cm3
    Photoelectric PECalciocopiapite = 6.69 barns/electron
    U = PECalciocopiapite x ρelectron density = 15.14 barns/cm3
    Fermion index Fermion index = 0.0054
    Boson index = 0.994
    Radioactivity
    Calciocopiapite is not radioactive

How to Identify Calciocopiapite

Calciocopiapite is available in grayish-yellow or brownish-yellow forms. It has a transparent to translucent appearance, pearly lustre, and a yellow-white streak.

The density of calciocopiapite is 2.22 g/cm3, and its relative hardness ranges from 2.5 to 3.

Global Distribution

Calciocopiapite is widely distributed in the Dashkesan deposit, Middle Caucasus Mountains, Azerbaijan.

Occurrence of Calciocopiapite and Useful Mineral Association

Calciocopiapite occurs in an oxidized zone of a pyrite-magnetite deposit in the Dashkesan (Dashkezan) Co-Fe deposit, Dashkesan District, Azerbaijan.

It is associated with hydrous iron oxides, malachite, and chalcanthite.

References

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