Editorial Feature

Burpalite – Occurrence, Properties, and Distribution

Burpalite was named after its occurrence in the Burpala massif, Russia.

Properties of Burpalite

The following are the key properties of burpalite:

  • Cell Data
    • Space group: P21/a
    • a = 10.1173(8)
    • b = 10.4446(6)
    • c = 7.2555(3)
    • β = 90:039(7)°
    • Z = 4

  • Crystal Data
    • Monoclinic, pseudo-orthorhombic
    • Point group: 2/m
    • As tablets, elongated along [001] and flattened on {010}, to 5mm
    • In fan-shaped aggregates, commonly intimately intergrown with lavenite
    • X-ray powder pattern: 2.962 (vs), 1.886 (ms), 1.556 (ms), 1.787 (s), 3.035 (m), 3.306 (m), 1.678 (m)

  • Chemical Composition
    Elements Content 1
    SiO2 31.82
    ZrO2 31.11
    CaO 14.52
    Na2O 13.86
    F 8.1
    -O = F2 3.41
    H2O 1.23
    TiO2 1.06
    MnO 0.60
    FeO 0.43
    Y2O3 0.32
    Nb2O5 0.22
    Total 99.86

  • Optical Properties
    • Optical class: Biaxial (-)
    • Orientation: X = b; Y = c; Z = a
    • Dispersion: r < v, weak
    • α = 1.627(2); β = 1.634(2); γ = 1.639(2)
    • 2V(meas.) = 82.1°
    • 2V(calc.) = 80.1°

  • Estimated Properties
    Electron density Bulk density (electron density) = 3.19 g/cm3
    note: Specific gravity of burpalite = 3.32 g/cm3
    Photoelectric PEBurpalite = 34.00 barns/electron
    U=PEBurpalite x ρ electron density = 108.34 barns/cm3
    Fermion index Fermion index = 0.03
    Boson index = 0.97
    Radioactivity
    Burpalite is not radioactive

How to Identify Burpalite

Burpalite can be identified in the field by its yellowish color. It is sometimes colorless. Its transparent to translucent form has good cleavage. This mineral has a vitreous luster, with white streak.

The density of burpalite is 3.33 g/cm3 with a hardness of 5 to 6 - between apatite and orthoclase.

Global Distribution

Burpalite is distributed mainly in the Burpala massif, about 120km north of Lake Baikal, eastern Siberia, in Russia.

Occurrence of Burpalite and Useful Mineral Association

Burpalite occurs in a fenitized hornfelsic sandstone in the contact zone of an alkalic intrusive.

It is often associated with minerals such as Lavenite, albite, nepheline, aegirine, loparite, alkalic amphibole, biotite, catapleiite, astrophyllite, and fluorite.

References

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