Veselovskýite, triclinic (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2.9H2O, a Zn-dominant analogue of lindackerite.

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F10%3A00047243" target="_blank" >RIV/00216224:14310/10:00047243 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Veselovskýite, triclinic (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2.9H2O, a Zn-dominant analogue of lindackerite.
Original language description
Veselovskýite, (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2 . 9H2O, is a new supergene mineral from the Geister vein, Mine Rovnost at the Jachymov ore district (St. Joachimsthal), Czech Republic, commonly associated with strashimirite and blue amorphous Cu arsenate. Itforms aggregates, up to 8 x 5 x 1 mm in size, consisting of lath-like to thin-tabular crystals, up to 1 mm long, commonly forming complicated intergrowths, no twinning was observed. Veselovskyite is translucent (aggregates) to transparent (crystals), colourless to greyish white (with a slight greenish tint). It has a greyish white streak with a greenish tint, a vitreous luster, does not fluoresce under both short- and long-wave ultraviolet light. Cleavage on (001) is perfect, Mohs hardness is similar to 2-3, and veselovskyite is very brittle with an irregular fracture and calculated density 3.28 g/cm3. All structural and chemical data are given in the paper.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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