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Paragonite

From Wikipedia, the free encyclopedia
Phyllosilicate mineral in the dioctahedral mica group
Paragonite
Paragonite withgarnet
General
CategoryPhyllosilicateminerals, dioctahedralmicagroup
FormulaNaAl2(AlSi3O10)(OH)2
IMA symbolPg[1]
Strunz classification9.EC.15
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(sameH-M symbol)
Space groupC2/c
Identification
ColorColorless, pale yellow, grayish, grayish white, greenish, light apple-green
Crystal habitmassive, fibrous or scaly
Twinningcommon on the [310] less common on the {001}
CleavagePerfect on the {001}
FractureMicaeous
TenacityElastic
Mohs scale hardness2.5–3
LusterPearly
StreakWhite
Diaphaneitytransparent to translucent
Specific gravity2.78
Optical propertiesBiaxial (−)
Refractive indexnα = 1.564 – 1.580 nβ = 1.594 – 1.609 nγ = 1.600 – 1.609
Birefringenceδ = 0.036
Dispersionr < v strong
UltravioletfluorescenceNone
References[2][3][4][5]

Paragonite is amineral, related tomuscovite. Itsempirical formula isNaAl2(AlSi3O10)(OH)2. A widesolvus separates muscovite from paragonite, such that there is littlesolid solution along the vector[clarification needed]Na+K+ and apparentmicas of intermediate composition is most commonly a microscopic (or even sub-microscopic) intergrowth of two distinct micas, one rich in K, and the other in Na. Paragonite is a common mineral in rocksmetamorphosed underblueschist facies conditions along with other sodic minerals such asalbite,jadeite andglaucophane. During the transition from blueschist togreenschist facies, paragonite andglaucophane are transformed intochlorite and albite.[6] Jadeite bearingpyroxene minerals have suggestedclinozoisite and paragonite are associated and derived fromlawsonite releasingquartz and water via the following reaction:[7]

4CaAl2Si2O8(H2O)2+NaAlSi2O62Ca2Al3Si3O12(OH)+NaAl3Si3O10(OH)2+SiO2+6H2O{\displaystyle {\ce {4CaAl2Si2O8(H2O)2 + NaAlSi2O6 <=> 2Ca2Al3Si3O12(OH) + NaAl3Si3O10(OH)2 + SiO2 + 6H2O}}}

It was first described in 1843 for an occurrence at Mt. Campione,Tessin,Switzerland.[4] The name derives from theGreek,paragon, formisleading, due to its similar appearance totalc.[5]

See also

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References

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  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. ^Mineralienatlas
  3. ^Mindat
  4. ^abWebmineral
  5. ^abHandbook of Mineralogy
  6. ^Deer, W. A.; et al. (2006).Rock-forming minerals, Volume 3A Micas (2 ed.). Geological Society of London. p. 302.ISBN 978-1-86239-142-0.
  7. ^Deer, William A. (1997).Single-chain Silicates, Volume 2A. Geological Society of London. p. 477.
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