Narsarsukite
Narsarsukite | |
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1.3 cm crystal of narsarsukite from Mont Saint-Hilaire | |
General | |
Category | Silicate mineral |
Formula (repeating unit) | Na4(Ti,Fe)4[Si8O20](O,OH,F)4.[1] |
Strunz classification | 9.DJ.05 |
Crystal symmetry |
Tetragonal dipyramidal H-M symbol: (4/m) Space group: I 4/m |
Unit cell | a = 10.72 Å, c = 7.95 Å; Z=4 |
Identification | |
Color | Honey to lemon-yellow, reddish brown, brownish gray, tan, pink; may be green from inclusions; may show color zoning |
Crystal habit | Occurs as flat tabular to equant, striated crystals In divergent, radiating groups; massive |
Crystal system | Tetragonal |
Cleavage | Good on {100} and {110} |
Fracture | Uneven to subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 5.5 - 7 |
Luster | Vitreous, pearly on {110} |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.64-2.83 |
Optical properties | Uniaxial (+) |
Refractive index | nω = 1.609 nε = 1.630 |
Birefringence | δ = 0.021 |
Pleochroism | Weak; O = colorless to yellow; E = colorless to honey-yellow |
References | [2][1][3] |
Narsarsukite is a rare silicate mineral with chemical formula Na2(Ti,Fe3+)Si4(O,F)11[2] or Na4(Ti,Fe)4[Si8O20](O,OH,F)4.[1]
It was first described in 1900 for an occurrence in the Narsarsuk pegmatite in the Ilimaussaq intrusive complex of West Greenland.[1] It has also been reported from a syenite which intruded limestone in the Sweetgrass Hills, Montana, and within hornfels and marble xenoliths in the alkalic intrusive of Mont Saint-Hilaire, Quebec.[2] It occurs associated with aegirine, microcline, albite, elpidite, epididymite, taeniolite, pectolite, calcite, galena and quartz.[2]
References
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