Zircophyllite

(K,Na)3(Mn,Fe2+)7(Zr,Ti)2Si8O24(O,OH,F)7IMA symbolZcp[1]Strunz classification9.DC.05Dana classification69.1.1.5Crystal systemTriclinicCrystal classPinacoidal (1)
(same H-M symbol)Space groupP1IdentificationColorBlack-brownCrystal habitPlaty, micaceousCleavagePerfect on {001}FractureBrittleTenacityBrittleMohs scale hardness4 – 4.5LusterAdamantine, vitreousStreakLight brownDiaphaneityTranslucent to opaqueSpecific gravity3.34Optical propertiesBiaxial (−)Refractive indexnα = 1.708 nβ = 1.738 nγ = 1.747Birefringenceδ = 0.039PleochroismX = Y = dark yellow; Z = brown2V angleMeasured: 62°, calculated: 56°Common impuritiesHf,H2OReferences[2][3][4]

Zircophyllite is a complex mineral, formula (K,Na)3(Mn,Fe)2+7(Zr,Ti,Nb)2Si8O24(OH,F)7. It crystallizes in the triclinic – pinacoidal crystal class as dark brown to black micaceous plates. It has perfect 001 cleavage, a Mohs hardness of 4 to 4.5 and a specific gravity of 3.34. Its indices of refraction are nα=1.708 nβ=1.738 nγ=1.747 and it has a 2V optical angle of 62°.

It occurs with natrolite in alkali pegmatites. It was discovered in 1972 in the Korgeredabinsh massif, Tuva, Russia and is named for its zirconium content and its relationship to astrophyllite. It is also known from the Mont Saint-Hilaire intrusive complex of Québec, Canada.

Zircophyllite is radioactive, but the radioactivity is barely detectable.[3]

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. ^ Mindat.org
  3. ^ a b Webmineral data
  4. ^ Handbook of Mineralogy


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