Posnjakite
Posnjakite | |
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Posnjakite from Špania Dolina in Slovakia | |
General | |
Category | Copper minerals |
Formula (repeating unit) | Cu4[(OH)6|SO4] • H2O |
Strunz classification | 7.DD.10 |
Dana classification | 31.4.1.1 |
Crystal symmetry |
Monoclinic domatic H-M symbol: (m) Space group: Pm |
Unit cell | a = 10.578 Å, b = 6.345 Å, c = 7.863 Å; β = 117.98°; Z = 2[1] |
Identification | |
Formula mass | 488.32 g |
Color | Sky-blue to dark-blue |
Crystal habit | Crystals scaly, or as crusts; earthy |
Crystal system | Monoclinic |
Mohs scale hardness | 2 to 3 |
Luster | Vitreous |
Refractive index | nα = 1.625 nβ = 1.680 nγ = 1.706 [1] |
Posnjakite is a hydrated copper sulfate mineral. It was discovered in the Tungsten deposit of Nura-Taldy[2] in Karaganda Region in Kazakhstan and described in 1967 by Aleksandr Ivanovich Komkov (1926–1987) and Yevgenii Ivanovich Nefedov (1910–1976)[3] and named after geochemist Eugene Valdemar Posnjak (1888–1949).[4]
Occurrence
Posnjakite is an uncommon but widespread secondary mineral in the oxidised zone of copper sulfide deposits, which may be of post-mine formation. It is associated with brochantite, langite, devilline, serpierite, woodwardite, wroewolfeite, aurichalcite, azurite, malachite and chalcopyrite.[2]