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Anandite

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Phyllosilicate mineral in the mica family
Anandite
General
CategoryPhyllosilicates
Formula
(repeating unit)
(Ba,K)(Fe,Mg)3(Si,Al,Fe)4O10(S,OH)2
IMA symbolAna
Strunz classification9.EC.35
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/m
Unit cella = 5.412(5), b = 9.434(5)
c = 19.953(10) ; β = 95°; Z = 2
Identification
ColorBlack
Crystal habitMassive, prismatic crystals poorly formed produce hexagonal outline cleavage fragments
CleavagePerfect on {001}
FractureFlexible fragments
Mohs scale hardness3 – 4
LusterVitreous
StreakGrey white
DiaphaneityNearly opaque
Specific gravity3.94
Optical propertiesBiaxial (+)
Refractive indexnα = 1.855 nγ = 1.880
PleochroismY = green; Z = brown
References

Anandite is a rare phyllosilicate with formula (Ba,K)(Fe,Mg)3(Si,Al,Fe)4O10(S,OH)2. It crystallizes in the monoclinic crystal system. It is black in color with a glassy luster and a near perfect cleavage.

It was first described in 1967 for an occurrence in the Wilagedera Prospect of the North Western Province of Sri Lanka in bands of iron ore. It has also been found in Big Creek in Fresno County and in Trumball Peak in Mariposa County, California as well as the Sterling Mine in New Jersey. It was named for Ananda Kentish Coomaraswamy (1877–1947), who was the director of the Mineral Survey of Ceylon, Sri Lanka at that time.

Anandite is a member of the mica group of minerals. Other minerals that anandite is associated with include: magnetite, chalcopyrite, pyrite, pyrrhotite and baryte.

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. ^ "Anandite mineral information and data". Mindat.org.
  3. ^ "PDF data sheet for Anandite in the Handbook of Mineralogy" (PDF). Handbook of Mineralogy. Mineral Data Publishing. 2001. Retrieved 2008-05-04.
  4. ^ "Anandite mineral data sheet". Webmineral.com. Archived from the original on 6 May 2008. Retrieved 2008-05-04.


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