Editorial Feature

Carlhintzeite - Occurrence, Properties, and Distribution

Carlhintzeite is a triclinic minera, containing oxygen, hydrogen, fluorine, calcium, and aluminum. It was first discovered in Hagendorf, Germany. The mineral was named after Carl Hintze, Professor of Mineralogy at the University of Breslau in Germany, noted for his compilation of the famous Handbuch der Mineralogie.

Properties of Carlhintzeite

The following are the key properties of Carlhintzeite:

  • Cell Data
    • Space Group: C1 or C1
    • a = 9.48(5)
    • b = 6.98(3)
    • c = 9.30(5)
    • α = 91.14(10)°
    • β = 104.85(10)°
    • γ = 90.0(10)°
    • Z = 4

  • Crystal Data
    • Triclinic, pseudomonoclinic
    • Point Group: 1 or 1
    • As radiating tufts and bundles of crystals, to 2 mm; crystals elongated || [101] and flattened on {001}. Forms observed are {100} and {001}, also (110)
    • X-ray Powder Pattern: 3.48 (100), 4.56 (70), 3.69 (60), 2.852 (40), 1.460 (40), 2.277 (30), 2.242 (30)

  • Chemical Composition
    Elements Content 1 Content 2
    F 52.1 51.52
    Ca 29.86 31.05
    Al 10.27 10.45
    H2O 7 6.98
    Total 99.23 100

  • Optical Properties
    • Optical Class: Biaxial (+)
    • Orientation: X ~ b; Z Λ c = 10(5)°
    • α = 1.411(2)
    • β = 1.416(2)
    • γ = 1.422(2)
    • 2V(meas.) = 77(2)°
    • 2V(calc.) = 78°

  • Estimated Properties
    Electron density Bulk density (electron density) = 2.81 g/cm3
    note: Specific gravity of Carlhintzeite = 2.88 g/cm3
    Photoelectric PECarlhintzeite = 4.46 barns/electron
    U= PECarlhintzeite x ρElectron density = 12.55 barns/cm3
    Fermion index Fermion index = 0.0004
    Boson index = 0.99
    Radioactivity
    Carlhintzeite is not radioactive

How to Identify Carlhintzeite

Carlhintzeite is a colorless or white mineral, formed as prismatic or radial crystals. It has a vitreous luster, white streak, and transparent appearance.

The density of carlhintzeite is 2.86 g/cm3.

Global Distribution

Carlhintzeite is distributed in the pegmatites in the Hagendorf are of Bavaria, Germany.

It is closely associated with apatite, strengite, pyrite and rockbridgeite.

Occurrence of Carlhintzeite and Useful Mineral Association

Carlhintzeite is formed by hydrothermal alteration of triphyllite in a pegmatite.

References

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