لازوليت
Lazulite | |
---|---|
العامة | |
التصنيف | Phosphate mineral |
الصيغة (repeating unit) | (Mg,Fe2+)Al 2(PO 4) 2(OH) 2 |
تصنيف سترونز | 8.BB.40 |
النظام البلوري | Monoclinic |
Crystal class | Prismatic (2/m) (same H–M symbol) |
Space group | P21/c |
Unit cell | a = 7.144(1), b = 7.278(1) c = 7.228(1) [Å]; β = 120.5(1)°; Z = 2 |
التعرف | |
Color | Azure, sky blue, bluish white, yellow-green, blue-green, rarely green |
Crystal habit | Tabular, acute to stubby bipyramidal crystals; granular, massive |
Twinning | Common by several twin laws |
Cleavage | Poor to good on {110}, indistinct on {101} |
Fracture | Uneven, splintery |
Tenacity | Brittle |
Mohs scale hardness | 5.5–6.0 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent to translucent to nearly opaque |
الجاذبية النوعية | 3.122–3.240 |
الصفات البصرية | Biaxial (−) |
Refractive index | nα = 1.604–1.626 nβ = 1.626–1.654 nγ = 1.637–1.663 |
Birefringence | δ = 0.033–0.037 |
Pleochroism | Strong: X = colorless, Y = blue, Z = darker blue |
2V angle | Measured: 61–70° |
قابلية الانصهار | Infusible |
قابلية الذوبان | Insoluble |
References | [1][2][3][4] |
Lazulite is a transparent to semi-opaque, blue mineral that is a phosphate of magnesium, iron, and aluminium, with the chemical formula (Mg,Fe2+)Al
2(PO
4)
2(OH)
2.[2] Lazulite forms one endmember of a solid solution series with the darker, iron-rich scorzalite.[2][4]
Lazulite crystallizes in the monoclinic system. Its crystal habits include steep bipyramidal or wedge-shaped crystals.[6] Lazulite has a Mohs hardness of 5.5–6.0 and a specific gravity of 3.0–3.1. It is infusible and insoluble.[4]
. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
Occurrence and discovery
Lazulite forms by high-grade metamorphism of silica-rich rocks and in pegmatites. It occurs in association with quartz, andalusite, rutile, kyanite, corundum, muscovite, pyrophyllite, dumortierite, wagnerite, svanbergite and berlinite in metamorphic terrains; and with albite, quartz, muscovite, tourmaline and beryl in pegmatites.[1] It may be confused with lazurite, lapis lazuli or azurite.
The type locality is in Freßnitzgraben in Krieglach, it's also found in Salzburg, Austria; Zermatt, Switzerland; Minas Gerais, Brazil; Lincoln County, Georgia; Inyo County, California; the Yukon in Canada; and elsewhere.
It was first described in 1795 for deposits in Styria, Austria.[2] Its name comes from the German lazurstein, for 'blue stone'[1] or from the Arabic for heaven.[2][4]
References
- ^ أ ب ت "Lazulite" (PDF). Handbook of Mineralogy. RRUFF. Archived (PDF) from the original on Jul 5, 2021.
- ^ أ ب ت ث ج قالب:Mindat
- ^ قالب:WebMineral
- ^ أ ب ت ث Hurlbut, Cornelius S.; Klein, Cornelius (1985). Manual of Mineralogy (20th ed.). Wiley. ISBN 0-471-80580-7.
- ^ Warr, L. N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. Mineralogical Society of Great Britain and Ireland. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ "Lazulite". Minerals.net.