Editorial Feature

Wagnerite - Occurrence, Properties, and Distribution

Wagnerite was first discovered in 1821 from the Höllengraben, Werfen, Salzburg, Austria. It was named after F. M. von Wagner, mining official in Munich, Germany.

Properties of Wagnerite

The following are the key properties of Wagnerite:

  • Cell Data
    • Space Group: P21/a
    • a = 11.945–11.985
    • b = 12.679–12.738
    • c = 9.644–9.70
    • β = 108.18°-108.36°
    • Z = 16
  • Crystal Data
    • Monoclinic
    • Point Group: 2/m
    • Typically in prismatic coarse anhedral crystals, elongated and striated along [001], complex vincinal form development, with more than thirty forms noted, to 20 cm; granular, massive
    • X-ray Powder Pattern: 2.985 (100), 3.297 (65), 3.123 (63), 2.854 (59), 2.758 (25), 2.710 (22), 1.584 (15)
  • Chemical Composition
    Elements Content 1 Content 2 Content 3
    MgO 48.35 43.76 49.58
    P2O5 43.45 42.68 43.65
    F 11.49 8.27 11.69
    OH - 2.82 -
    -O = (F2, OH) 4.84 4.81 4.92
    FeO 0.95 6.04 -
    MnO 0.70 0.92 -
    Total 100.10 99.68 100.00
  • Optical Properties
    • Optical Class: Biaxial (+)
    • Orientation: Y = b; Z ^ c = –20° to –21.5°
    • Dispersion: r > v, weak, inclined
    • α = 1.568–1.588
    • β = 1.572–1.589
    • γ = 1.582–1.598
    • 2V(meas.) = 25°–35°
  • Estimated Properties
    Electron density Bulk density (electron density)=3.07 g/cm3
    note: Specific gravity of Wagnerite =3.11 g/cm3
    Photoelectric PEWagnerite = 2.57 barns/electron
    U= PEWagnerite x ρElectron density= 7.88 barns/cm3
    Fermion index Fermion index = 0.02
    Boson index = 0.98
    Radioactivity
    Wagnerite is not radioactive

How to Identify Wagnerite

Wagnerite occurs in reddish brown, yellow, gray, gray white, or green color. The mineral is non-fluorescent with a white streak, vitreous luster, translucent appearance and imperfect cleavage. It has thin, elongated fractures produced by intersecting cleavages. It can be formed as massive uniformly indistinguishable crystals or as parallel lines on crystal surface. The average density of wagnerite is 3.1 g/cm3, and its relative hardness ranges from 5 to 5.5.

Global Distribution

Wagnerite is distributed in the following places:

  • Hollgraben, F¨arbergraben, Radelgraben, and Schladming-graben, near Werfen, and Bischofshofen, and from Webing, near Abtenau, Salzburg, Austria
  • Silberberg mine, Bodenmais, Bavaria, Germany
  • Nickenicher Sattel and Bellerberg volcanoes, Eifel district
  • Zechstein salt deposit, Hannover, Lower Saxony
  • Val d’Ambra, Tessin, Switzerland
  • Skriarov, near Velka Bites, and Dolni Bory, near Velke, Mezirici, Czech Republic
  • Porsgrunn and Havredal, Bamble, Norway
  • Halsjoberget, Varmland, Sweden
  • Kyakhta sillimanite deposit, Buryatia
  • Santa Fe Mountain, near Idaho Springs, Clear Creek Co., Colorado
  • Dome Rock Mountains, Yuma Co., Arizona, USA
  • Star Lake area, near Sherridon, Manitoba, Canada
  • Bimbowrie, near Olary, South Australia
  • Casey Bay, Enderby Land, Antarctica.

Occurrence of Wagnerite and Useful Mineral Association

Wagnerite is a rare accessory mineral in metamorphic rocks of moderate to high grade. It is closely associated with cordierite, chrysoberyl, sapphirine, garnet, musgravite, surinamite, tourmaline, andalusite, apatite, monazite-(Ce), biotite, plagioclase, sillimanite, corundum, chlorite, ferroan magnesite and lazulite.

References

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