Editorial Feature

Niningerite - Occurrence, Properties, and Distribution

Niningerite is a magnesium-iron-manganese sulfide mineral, first discovered in 1966 from the Indarch, St. Marks, Qingzhen. It is a member of the galena group.

The mineral was named after Harvey Harlow Nininger, of Sedona in Arizona, USA, for his contributions to meteoritics.

Properties of Niningerite

The following are the key properties of Niningerite:

  • Cell Data
    • Space Group: Fm3m (by analogy to synthetic)
    • a = 5.17(2)
    • Z = 4

  • Crystal Data
    • Cubic
    • Point Group: 4/m 3 2/m
    • As grains intimately intergrown with kamacite and troilite; grains may contain oriented exsolution lamellae of troilite, and minute grains of kamacite
    • X-ray Powder Pattern: 2.601 (100), 1.8388 (60), 1.5010 (16), 1.1630 (14), 1.0617 (10), 3.004 (8), 1.3001 (8)

  • Chemical Composition
    Elements Content 1 Content 2 Content 3
    S 43.4 46.9 44.45
    Fe 27.0 15.6 38.72
    Mg 18.3 23.5 16.84
    Mn 6.5 11.6 -
    Cr 1.66 0.14 -
    Ca 1.28 0.39 -
    Total 98.14 98.13 100.00

  • Estimated Properties
    Electron density Bulk density (electron density) = 3.22 g/cm3
    note: Specific gravity of Niningerite = 3.31 g/cm3
    Photoelectric PENiningerite = 12.23 barns/electron
    U = PENiningerite x ρElectron density = 39.37 barns/cm3
    Fermion index Fermion index = 0.02
    Boson index = 0.98
    Radioactivity
    Niningerite is not radioactive

How to Identify Niningerite

Niningerite is an opaque grayish mineral, having a metallic luster. It occurs as microscopic crystals, and it is generally found as inclusions in other minerals.

The hardness range of niningerite is 3.5 to 4.

Global Distribution

Niningerite is distributed in the following places:

  • Indarch meteorite, Shusha, Naxcivan District, Azerbaijan
  • Abee meteorite, Abee, Alberta, Canada

Occurrence of Niningerite and Useful Mineral Association

Niningerite occurs in less extensively metamorphosed enstatite chondrite meteorites.

The mineral is closely related to troilite and kamacite.

References

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