Loading AI tools
Amphibole, double chain inosilicate mineral From Wikipedia, the free encyclopedia
Pargasite or pargasitic hornblende is a complex inosilicate mineral of the amphibole group with formula NaCa2(Mg4Al)(Si6Al2)O22(OH)2.
Pargasite | |
---|---|
General | |
Category | Inosilicates |
Formula (repeating unit) | NaCa2(Mg4Al)(Si6Al2)O22(OH)2 |
IMA symbol | Prg[1] |
Strunz classification | 9.DE.15 |
Dana classification | 66.1.3a.12 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/m |
Identification | |
Color | Bluish green, grayish black, light brown |
Crystal habit | Stout prismatic to tabular |
Twinning | Simple and lamellar – common |
Cleavage | {110} perfect |
Fracture | Splintery |
Mohs scale hardness | 5–6 |
Luster | Vitreous |
Diaphaneity | Translucent, will transmit light on thin edges. |
Specific gravity | 3.04–3.17 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.630 nβ = 1.640 nγ = 1.650 |
Birefringence | δ = 0.020 max. |
References | [2][3][4][5][6] |
It was first described for an occurrence in Pargas, Finland in 1814 and named for the locality.[6]
It occurs in high temperature regional metamorphic rocks and in the skarns within contact aureoles around igneous intrusions. It also occurs in andesite volcanic rocks and altered ultramafic rocks.[3]
Pargasite is the main water-storage site in the uppermost mantle; however, it becomes unstable at depths greater than 90 km (56 mi). This has significant consequences for the water storage capacity, and the solidus temperature of the lherzolite of the upper mantle.[7]
Seamless Wikipedia browsing. On steroids.
Every time you click a link to Wikipedia, Wiktionary or Wikiquote in your browser's search results, it will show the modern Wikiwand interface.
Wikiwand extension is a five stars, simple, with minimum permission required to keep your browsing private, safe and transparent.