May 22 2014
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