Ephesite

Ephesite
General
CategoryPhyllosilicate
Formula
(repeating unit)
NaLiAl2(Al2Si2)O10(OH)2
IMA symbolEph[1]
Strunz classification9.EC.20
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/c[2]
also reported is a triclinic polytype[3]
Unit cella = 5.12, b = 8.853
c = 19.303 [Å]; beta = 95.08°; Z = 4
Identification
ColorBrownish pink, pearl gray, pale green
Crystal habitFlakes
TwinningCommonly twinned about [310] or [310]
CleavagePerfect on {001}
TenacityBrittle
Mohs scale hardness3.5–4
LusterVitreous, pearly on cleavage
DiaphaneityTranslucent
Specific gravity2.984
Optical propertiesBiaxial (-)
Refractive indexnα = 1.592 - 1.595 nβ = 1.624 - 1.625 nγ = 1.625 - 1.627
Birefringenceδ = 0.033
2V angle18° to 28°
Dispersionr > v strong
References[2][3][4]

Ephesite is a rare member of the mica silicate mineral group, phyllosilicate. It is restricted to quartz-free, alumina rich mineral assemblages and has been found in South African deposits in the Postmasburg district as well as Ephesus, Turkey.[5]

  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. ^ a b Epesite data on Webmineral
  3. ^ a b Ephesite in the Handbook of Mineralogy
  4. ^ Ephesite on Mindat.org
  5. ^ Phillips, F. (1931) Ephesite (soda-maragrite) from the Postmasburg district, South Africa, Corpus Christi College, Cambridge, pp. 482-485

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