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

Kód výsledku v 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>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Neues Jahrbuch fur Mineralogie, Abhandlungen

ISSN

0028-3649

e-ISSN

—

Svazek periodika

187

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

ES - Španělské království

Počet stran výsledku

8

Strana od-do

—

Kód UT WoS článku

—

EID výsledku v databázi Scopus

—