Lorenzenite
| Lorenzenite | |
|---|---|
|
Doubly terminated crystal of Lorenzenite, 2.5 cm tip to tip, from Lovozero Massif, Kola Peninsula, Russia | |
| General | |
| Category | Silicate mineral |
| Formula (repeating unit) | Na2Ti2[O3|Si2O6] |
| Strunz classification | 9.DB.10 |
| Crystal symmetry | Orthorhombic H–M Symbol (2/m 2/m 2/m) dipyramidal |
| Unit cell | a = 8.71 Å, b = 5.23 Å, c = 14.48 Å; Z = 4 |
| Identification | |
| Color | Pale purple-brown, pale pink to mauve, brown to black |
| Crystal habit | Equant, bladed, prismatic, to needlelike crystals; fibrous, felted, lamellar aggregates |
| Crystal system | Orthorhombic |
| Cleavage | Distinct/good on {010} |
| Fracture | Irregular/uneven |
| Mohs scale hardness | 6 |
| Luster | Adamantine, vitreous, sub-metallic, dull |
| Streak | White to pale brown |
| Diaphaneity | Transparent, opaque |
| Specific gravity | 3.42 - 3.45 |
| Optical properties | Biaxial (-) |
| Refractive index | nα = 1.910 - 1.950 nβ = 2.010 - 2.040 nγ = 2.030 - 2.060 |
| Birefringence | δ = 0.120 |
| Pleochroism | Weak |
| 2V angle | Measured: 38° to 41° |
| Ultraviolet fluorescence | Pale yellow to dull green under SW UV |
| References | [1][2][3] |
Lorenzenite is a rare sodium titanium silicate mineral with the formula Na2Ti2Si2O9 It is an orthorhombic mineral, variously found as colorless, grey, pinkish, or brown crystals.
It was first identified in 1897 in rock samples from Narsarsuk, Greenland.[2] In 1947 it was discovered to be the same as the mineral ramsayite (now a synonym of lorenzenite), discovered in the 1920s in the Kola peninsula of Russia. It is also found in northern Canada.
It occurs in nepheline syenites and pegmatites in association with aegirine, nepheline, microcline, arfvedsonite, elpidite, loparite, eudialyte, astrophyllite, mangan-neptunite, lavenite, rinkite, apatite, titanite and ilmenite.[1]
It was named in honour of Danish mineralogist Johannes Theodor Lorenzen (1855–1884).[2]
References
 |
Wikimedia Commons has media related to Lorenzenite. |
| ||||||||||||||||||||