Weloganite
| Weloganite | |
|---|---|
|
Weloganite | |
| General | |
| Category | Carbonate mineral |
| Formula (repeating unit) | Na2(Sr,Ca)3Zr(CO3)6·3H2O |
| Strunz classification | 05.CC.05 |
| Dana classification | 15.3.4.4 |
| Crystal symmetry | Triclinic 1 pinacoidal |
| Unit cell | a = 8.966 Å, b = 8.98 Å, c = 6.73 Å; α = 102.72°, β = 116.65°, γ = 60.06°; Z = 1 |
| Identification | |
| Formula mass | 814.16 g |
| Color | Yellow, pale yellow, amber, tan, white |
| Crystal habit | Roughly hexagonal, tapering crystals |
| Crystal system | Triclinic, pseudorhombohedral |
| Twinning | About [103] repeated at 120 degrees |
| Cleavage | Perfect on pseudo {0001} |
| Fracture | Conchoidal |
| Mohs scale hardness | 3½ |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | translucent |
| Specific gravity | 3.20 - 3.22 |
| Optical properties | Biaxial (-) |
| Refractive index | nα = 1.558 nβ = 1.646 nγ = 1.640 |
| Birefringence | δ = 0.082 |
| 2V angle | Measured: 15° |
| Dispersion | Weak |
| Other characteristics | Pyroelectric. triboluminescent. |
| References | [1][2][3][4][5] |
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Weloganite is a rare carbonate mineral with formula: Na2(Sr,Ca)3Zr(CO3)6·3H2O. It was discovered in 1967 and named for Canadian geologist Sir William Edmond Logan (1798-1875). It was first discovered in Francon Quarry, Montreal, Canada and has only been reported from a few localities worldwide.
Properties
It is usually white, lemon yellow, or amber in color, and can be translucent. It crystallizes in the triclinic system and shows pseudo-hexagonal crystal forms due to twinning. The width of the crystals typically undulates down the length, forming crystals that widen in the middle or flare out at the end. Crystals are affected by light and can develop a white alteration coating over time. Weloganite is triboluminescent, producing blue light.
Occurrence
It occurs in an igneous carbonatite sill in Montreal, Canada in the Francon Quarry where it was first discovered. It also occurs in the Mont Saint-Hilaire district. Associated minerals include strontianite, dawsonite and calcite. It has also been reported from the Pilansberg Complex of the western Bushveld Igneous Complex in South Africa.[4]
See also
References
- ↑ Sabina, A., 'Weloganite, a new strontium zirconium carbonate from Montreal Island, Canada', The Canadian Mineralogist, 9, pp.468-477, 1968.
- ↑ Grice, J. D. and Perrault G., 'The crystal structure of triclinic weloganite', The Canadian Mineralogist, 13, pp.209-216, 1975.
- ↑ Handbook of Mineralogy
- ↑ 4.0 4.1 Mindat
- ↑ Webmineral