| Neptunite | |
|---|---|
_sur_natrolite_et_serpentine_(USA)_2.jpg) Neptunite crystals | |
| General | |
| Category | Phyllosilicateminerals |
| Formula | KNa2Li(Fe2+,Mn2+)2Ti2Si8O24 |
| IMA symbol | Npt[1] |
| Strunz classification | 9.EH.05 |
| Dana classification | 70.04.01.01 |
| Crystal system | Monoclinic |
| Crystal class | Domatic (m) (sameH-M symbol) |
| Space group | Cc |
| Unit cell | a = 16.427(2), b = 12.478(2) c = 9.975(1) Å; β = 115.56(1)°; Z = 4 |
| Identification | |
| Color | Black; deep red-brown in thin fragments |
| Crystal habit | Prismatic or tabular |
| Twinning | Interpenetrant on {301} |
| Cleavage | {110} good |
| Fracture | Conchoidal |
| Tenacity | Brittle |
| Mohs scale hardness | 5–6 |
| Luster | Vitreous |
| Streak | Brown to red brown |
| Diaphaneity | Nearly opaque |
| Specific gravity | 3.19–3.23 |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.69–1.6908, nβ = 1.6927–1.7, nγ = 1.7194–1.736 |
| Birefringence | 0.0294–0.0452 |
| Pleochroism | x = yellow-orange, y = orange, z = deep red |
| 2V angle | 36° to 49° |
| Other characteristics | Piezoelectric |
| References | [2][3][4] |
Neptunite is asilicate mineral with the formulaKNa2Li(Fe2+,Mn2+)2Ti2Si8O24. With increasing manganese it forms a series withmangan-neptunite.Watatsumiite [ja] is the variety withvanadium replacing the titanium in the formula.
It was first described in 1893 for an occurrence in the Narssârssukpegmatite of WestGreenland.[3] It is also found withinnatroliteveins inglaucophaneschist withinserpentinite inSan Benito County, California, US. It also occurs inMont Saint-Hilaire,Quebec[5] and in theKola Peninsula ofRussia.[2]
The mineral is named forNeptune, Roman god of the sea because of its association withaegirine fromÀgir, the Scandinavian sea-god.[3]
TheGemological Institute of America (GIA) identified an 11.78-carat faceted specimen as neptunite based onRaman spectroscopy.[6]
 | This article about a specificsilicate mineral is astub. You can help Wikipedia byexpanding it. |