Veselovskýite, triclinic (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2.9H2O, aZn-dominant analogue of lindackerite.
Veselovskýite, triclinic (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2.9H2O, aZn-dominant analogue of lindackerite.
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Veselovskýite，三斜晶系 (Zn,Cu,Co)Cu4(AsO4)2(AsO3OH)2.9H2O，以 aZn 为主的锇铁矿类似物。
DOI：
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发表时间：
2010
期刊：
影响因子：
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通讯作者：
M. Novak
中科院分区：
文献类型：
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作者：
J. Sejkora;P. Ondruš;M. Novak
Veselovsk axite，(锌，铜，钴)Cu4(AsO4)2(AsO3OH)2。9H2O，是一种新的
表生矿物来自Geister矿脉，Mine Rovnost在
捷克Jachymov矿区(St.Joachimsthal)，
通常与闪锌矿和蓝色无定形铜有关
亚砷酸盐。它形成集合体，大小可达8x5x1毫米，
由板条状到薄片状晶体组成，最大可达1毫米
长的，通常形成复杂的相互生长，没有孪晶
被观察到了。Veselovsky是半透明的(聚集体)到
透明(晶体)，无色至灰白色(带
略带绿色)。它有一条灰白色的条纹，有一条
绿色是一种玻璃般的光泽，在这两种颜色下都不会发出荧光
短波和长波紫外线。(001)上的解理是
完美，莫氏硬度接近2-3，泡沫石为
非常脆，断口不规则，计算出密度
3.28克/厘米~3。所有的结构和化学数据都在
纸。
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. It forms 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.