Pargasite

Pargasite

Pargasite

Amphibole, double chain inosilicate mineral


Pargasite or pargasitic hornblende is a complex inosilicate mineral of the amphibole group with formula NaCa2(Mg4Al)(Si6Al2)O22(OH)2.

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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]

It is used as a gemstone.[8][9]

See also


References

  1. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. "IMA Master List". Archived from the original on 2015-01-05. Retrieved 2014-05-12.
  3. "Pargasite". mindat.org. Retrieved 2012-12-17.
  4. "Pargasite Mineral Data". webmineral.com. Retrieved 2012-12-17. (Java plugin required)
  5. Green, D H; Hibberson, W O; Kovacs, Istvan; Rosenthal, A (23 September 2010). "Water and its influence on the lithosphere–asthenosphere boundary". Nature. 467 (7314): 448–451. Bibcode:2010Natur.467..448G. doi:10.1038/nature09369. PMID 20865000. S2CID 4393352. (subscription required)
  6. Dedeyne, Roger; Quintens, Evo (2007). Tables of gemstone identification (1st ed.). Gent, Belgium: Glirico. p. 169. ISBN 9789078768012. Retrieved 5 November 2020.
  7. "Amethyst Crystals and Meaning Healing Properties". nacrystal.com. 2022-07-11. Retrieved 2023-02-10.


Spinel and pargasite on marble, Luc Yen District, Vietnam. Specimen size: 4.5 × 3.5 × 3.5 cm.

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