Editorial Feature

Simpsonite - Occurrence, Properties, and Distribution

Simpsonite was first discovered in 1938 from the Tabba Tabba, Western Australia. It was named after Edward Sydney Simpson, a Western Australian government mineralogist and analyst.

Properties of Simpsonite

The following are the key properties of Simpsonite:

  • Cell Data
    • Space Group: P3
    • a = 7.385–7.387
    • c = 4.515–4.516
    • Z = 1

  • Crystal Data
    • Hexagonal
    • Point Group: 3
    • Euhedral to subhedral crystals, tabular to short prismatic, with {1010} and {0001}, and rarely a few other forms, striated || [0001], to 2.4cm; commonly in subparallel groups
    • X-ray Powder Pattern: 1.651 (100), 2.859 (67), 3.69 (62), 2.131 (59), 1.395 (54), 2.417 (40), 2.609 (37)

  • Chemical Composition
    Elements Content 1 Content 2 Content 3
    Ta2O5 71.54 76.4 64.6
    Al2O3 25.20 22.8 24.3
    Nb2O5 1.82 - 8.6
    SiO2 1 - -
    FeO 0.16 - -
    CaO 0.12 - -
    SnO2 0.10 - 0.9
    TiO2 0.02 - -
    H2O - 1 1.1
    Total 99.96 100.2 99.5

  • Optical Properties
    • Optical Class: Uniaxial (–)
    • ω = 2.045(5)
    • ε = 2.025(5)

  • Estimated Properties
    Electron density Bulk density (electron density) = 5.63 g/cm3
    note: Specific gravity of Simpsonite = 6.35 g/cm3
    Photoelectric PESimpsonite = 629.45 barns/electron
    U = PESimpsonite x ρElectron density = 3543.83 barns/cm3
    Fermion index Fermion index = 0.0001
    Boson index = 0.9998
    Radioactivity
    Simpsonite is not radioactive

How to Identify Simpsonite

Simpsonite is either colorless, or occurs in different colors. These range from light yellow to light brown, white and brownish-yellow. It is a transparent, fluorescent mineral having vitreous luster and white streak. Its fractures are brittle, producing small, conchoidal fragments. It can be formed as prismatic, euhedral crystals, or parallel lines on a crystal surface. The hardness of simpsonite ranges from 7 to 7.5, and its density is 6.7 g/cm3.

Global Distribution

Simpsonite is distributed in the following places:

  • Tabba Tabba, Western Australia
  • Alto do Giz pegmatite, near Parelhas, and the Onca mine, about 25km distant, Rio Grande do Norte, Brazil
  • Al Hayat and Mdara mines, Bikita; at the Benson No. 3 pegmatite, Mtoko, Zimbabwe
  • Mumba, near Lake Kivu, Kivu Province and Manono pegmatite, Katanga, Congo
  • Leshaia pegmatite, Vuoriyarvi carbonatite complex, Kola Peninsula, Russia
  • Tanco pegmatite, Bernic Lake, Manitoba, Canada

Occurrence of Simpsonite and Useful Mineral Association

Simpsonite occurs as an uncommon accessory mineral in some tantalum-rich granite pegmatites.

Quartz, muscovite, tourmaline, eucryptite, petalite, pollucite, montebrasite, spodumene, beryl, tapiolite, microlite, manganotantalite, and tantalite are all closely associated with simpsonite.

References

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