Editorial Feature

Ribbeite - Occurrence, Properties, and Distribution

Ribbeite is an orthorhombic-dipyramidal pink mineral. It contains silicon, oxygen, manganese, magnesium, and hydrogen, and is a member of the humite group.

The mineral was first discovered in 1987 in the Kombat mine, Namibia. It was named after Paul Ribbe of Virginia Polytechnical Institute and State University.

Properties of Ribbeite

The following are the key properties of Ribbeite:

  • Cell Data
    • Space Group: Pbnm or Pbn21
    • a = 4.799(1)
    • b = 10.742(6)
    • c = 15.70(1)
    • Z = 4

  • Crystal Data
    • Orthorhombic
    • Point Group: 2/m 2/m 2/m or mm2
    • Crystals: up to 0.5mm, in granular aggregates, to20 cm
    • X-ray Powder Pattern: 1.796 (100), 2.873 (80), 2.552 (80), 2.925 (70), 2.821 (70), 2.695 (60), 2.515 (40)

  • Chemical Composition
    Elements Content
    MnO 65.1
    SiO2 24.3
    MgO 5.2
    H2O 4.9
    FeO 0.3
    CaO 0.2
    Total 100

  • Optical Properties
    • Optical Class: Biaxial (+)
    • Pleochroism: Weak; X = Y = colorless; Z = light pink
    • Orientation:X = b; Y = a; Z = c
    • Dispersion: r > v; moderate
    • Absorption: Z > X = Y
    • α = 1.780(3)
    • β = 1.792(3)
    • γ = 1.808(3)
    • 2V(meas.) = 81.3(2)°
    • 2V(calc.) = 82.5°

  • Estimated Properties
    Electron density Bulk density (electron density) = 3.75 g/cm3
    note: Specific gravity of Ribbeite = 3.90 g/cm3
    Photoelectric PERibbeite = 12.27 barns/electron
    U = PERibbeite x ρElectron density = 46.06 barns/cm3
    Fermion index Fermion index = 0.01
    Boson index = 0.99
    Radioactivity
    Ribbeite is not radioactive

How to Identify Ribbeite

Ribbeite is a transparent pink mineral, having vitreous luster and light pink streak. The density of ribbeite is 3.9g/cm3, and its hardness is 5.

Global Distribution

Ribbeite is widely distributed in the Kombat mine, 49km south of Tsumeb, Namibia.

Occurrence of Ribbeite and Useful Mineral Association

Ribbeite occurs in tectonically transported and boudinaged manganese-rich lenses within dolostones and mineralogically distinct layers.

It is closely associated with jacobsite, galaxite, chlorite, pyrochroite, manganoan calcite, and alleghanyite.

References

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