Jun 11 2014
Bismutohauchecornite is a tetragonal-ditetragonal dipyramidal bronze mineral, containing sulfur, nickel, and bismuth. It belongs to the hauchecornite group of minerals.
The mineral was first discovered in 1980 from the Oktyabr mine in Norilsk, Russia. It was named for its relationship to hauchecornite.
Properties of Bismutohauchecornite
The following are the key properties of Bismutohauchecornite:
- Cell Data
- Space Group: P4/mmm
- a = 7.37
- c = 5.88
- Z = [1]
- Crystal Data
- Tetragonal
- Point Group: 4/m 2/m 2/m
- As elongated tabular crystals, to 0.3mm; as grains and massive
- X-ray Powder Pattern: 2.80 (10), 1.867 (8), 4.34 (6), 2.40 (6), 2.32 (6), 3.67 (5), 1.808 (4)
- Chemical Composition
Elements |
Content 1 |
Content 2 |
Content 3 |
Ni |
43.6 |
45.85 |
43.93 |
Bi |
33.9 |
27.76 |
34.75 |
S |
21.4 |
22.46 |
21.32 |
Co |
0.8 |
0.66 |
- |
As |
0.5 |
0.72 |
- |
Fe |
0.2 |
0.22 |
- |
Pb |
- |
0.01 |
- |
Total |
100.4 |
97.68 |
100 |
- Optical Properties
- Anisotropism: Weak in reflected light
- Estimated Properties
Electron density |
Bulk density (electron density) = 5.67 g/cm3
note: Specific gravity of Bismutohauchecornite = 6.25 g/cm3 |
Photoelectric |
PEBismutohauchecornite = 635.91 barns/electron
U = PEBismutohauchecornite x ρ Electron density = 3608.61 barns/cm3 |
Fermion index |
Fermion index = 0.006
Boson index = 0.99 |
Radioactivity
|
Bismutohauchecornite is not radioactive
|
How to Identify Bismutohauchecornite
Bismutohauchecornite is a bronze-colored mineral, with metallic luster, grayish-black streak, and opaque appearance. It can be formed as tabular structures, or massive uniformly indistinguishable crystals forming large masses.
The hardness of the mineral is 5.5.
Global Distribution
Bismutohauchecornite is distributed in the following places:
- Oktyabr mine, Talnakh area, Norilsk region, western Siberia, Russia
- Zimmer Lake, northern Saskatchewan, Canada
- Mihara mine, Okayama Prefecture, and the Tsumo mine, Shimane Prefecture, Japan
- Liu Zhuang, Tongbai Co. Henan Province, China
Occurrence of Bismutohauchecornite and Useful Mineral Association
Bismutohauchecornite occurs in ultramafic rocks. It can be formed as secondary pore-fillings, and replacements of sandstone and conglomerate.
The mineral is closely related to millerite, pyrrhotite, chalcopyrite, altaite, pentlandite, galena, and chalcocite.
References