Keyite

Cu2+3Zn4Cd2(AsO4)6 · 2H2OIMA symbolKey[1]Strunz classification8.CA.50Crystal systemMonoclinicCrystal classPrismatic (2/m)
(same H-M symbol)Space groupI2/aUnit cella = 11.654(3) Å
b = 12.780(5) Å
c = 6.840(3) Å
β = 99.11°; Z = 2IdentificationFormula mass1,520.19 g/molColorazure/ blueCrystal habitprismatic, tabularCleavagegood (001) cleavageMohs scale hardness3.5 - 4Streaklight blueDiaphaneitytranslucentDensity5.106g/cm3Optical propertiesbiaxialRefractive indexnα = 1.800, nβ, and nγ = 1.870Birefringence0.070Pleochroismx: pale blue, y: greenish blue, z: deep blueReferences[2]

[3]

[4]

Keyite is a mineral with the chemical formula Cu2+3Zn4Cd2(AsO4)6 · 2H2O.[2] The name comes from Charles Locke Key (born 1935), an American mineral dealer who furnished its first specimens.[3] Keyite is monoclinic-prismatic, meaning its crystal form has three unequal axes, two of which have 90° angles between them and one with an angle less than 90°.[3] Keyite belongs to the biaxial optical class, meaning it has more than one axis of anisotropy (optic axis), in which light travels with zero birefringence, and three indices of refraction, nα = 1.800, nβ, and nγ = 1.870.[5][4] Being a very rare cadmium copper arsenate, keyite is only found in Tsumeb, Namibia in the Tsumeb mine, a world-famous copper mine known for its abundance of rare and unusual minerals.[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. ^ a b Fleischer, M., Cabri, L.J., and Pabst, A. (1977) New Mineral Names. American Mineralogist, 62, 1259.
  3. ^ a b c d Cooper, M.A.; Hawthorne, F.C. (1996). "The crystal structure of keyite, Cu32+Zn4Cd2(AsO4)6(H2O)2, an oxysalt mineral with essential cadmium". Canadian Mineralogist. 34: 623–630. Retrieved 22 May 2022.
  4. ^ a b Keyite, WebMineral.com, retrieved 22 May 2022
  5. ^ Keyite, Mindat.org, retrieved 22 May 2022


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