Belogubite, a New Mineral of the Chalcanthite Group from the
Gaiskoe Deposit, South Urals, Russia

J 2020

Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia

KASATKIN, A. V., S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA, A. A. AGAKHANOV et. al.

Základní údaje

Originální název

Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia

Autoři

KASATKIN, A. V. (garant), S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA (203 Česká republika, domácí), A. A. AGAKHANOV a D. I. BELAKOVSKIY

Vydání

Geology of Ore Deposits, Pleiades Publishing, 2020, 1075-7015

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 0.670

Kód RIV

RIV/00216224:14310/20:00124334

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1134/S1075701520070065

UT WoS

000616319600006

Klíčová slova anglicky

belogubite; new mineral; chalcanthite group; Gaiskoe deposit; South Urals

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 1. 3. 2022 13:12, Mgr. Marie Šípková, DiS.

Anotace

V originále

Belogubite CuZn(SO4)(2) . 10H(2)O, a new mineral of the chalcanthite group, is found in the Gai (Gaiskoe) massive sulfide deposit, South Urals, Russia. This mineral forms aggregates of blue grains up to 1 mm. It is optically biaxial (-), n(p) = 1.512(2), n(m) = 1.525(2), n(g) = 1.531(2), 2V = 70(10)degrees. The chemical composition of the holotype sample is as follows (wt %): 1.12 MgO, 0.10 MnO, 3.15 FeO, 8.98 CuO, 18.02 ZnO, 32.49 SO3, and 36.75 H2O, total 100.61. The empirical formula is (Cu0.55Zn0.45)(sigma 1.00)(Zn0.64Fe0.22Mg0.14Mn0.01)(sigma 1.01)S1.99O7.98 . 10.02H(2)O. The crystal structure of belogubite is studied using the single crystal method, R = 0.016. The mineral is triclinic, P (1) over bar The unit cell parameters are: a = 6.2548(1), b = 10.6112(2), c = 6.0439(1) angstrom, alpha = 82.587(1), beta = 109.625(1), gamma = 104.848(1)degrees, V = 364.81(1) angstrom(3), and Z = 1. The strongest reflections of the powder XRD pattern [d(meas)., angstrom (I, %) (hkl) are: 5.73 (35) (100), 5.576 (47) (-110), 4.873 (100) (-111), 3.907 (31) (021), 3.719 (45) (0 -21), 3.229 (27) (111), 2.915 (25) (221), and 2.684 (26) (130).

Citovat

KASATKIN, A. V., S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA, A. A. AGAKHANOV a D. I. BELAKOVSKIY. Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia. Geology of Ore Deposits. Pleiades Publishing, 2020, roč. 62, č. 7, s. 599-607. ISSN 1075-7015. Dostupné z: https://dx.doi.org/10.1134/S1075701520070065.

@article{1837979,
   author = {Kasatkin, A. V. and Britvin, S. N. and Chukanov, N. V. and Škoda, Radek and Agakhanov, A. A. and Belakovskiy, D. I.},
   article_number = {7},
   doi = {http://dx.doi.org/10.1134/S1075701520070065},
   keywords = {belogubite; new mineral; chalcanthite group; Gaiskoe deposit; South Urals},
   language = {eng},
   issn = {1075-7015},
   journal = {Geology of Ore Deposits},
   title = {Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia},
   url = {https://link.springer.com/article/10.1134/S1075701520070065},
   volume = {62},
   year = {2020}
}

TY  - JOUR
ID  - 1837979
AU  - Kasatkin, A. V. - Britvin, S. N. - Chukanov, N. V. - Škoda, Radek - Agakhanov, A. A. - Belakovskiy, D. I.
PY  - 2020
TI  - Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia
JF  - Geology of Ore Deposits
VL  - 62
IS  - 7
SP  - 599-607
EP  - 599-607
PB  - Pleiades Publishing
SN  - 10757015
KW  - belogubite
KW  - new mineral
KW  - chalcanthite group
KW  - Gaiskoe deposit
KW  - South Urals
UR  - https://link.springer.com/article/10.1134/S1075701520070065
N2  - Belogubite CuZn(SO4)(2) . 10H(2)O, a new mineral of the chalcanthite group, is found in the Gai (Gaiskoe) massive sulfide deposit, South Urals, Russia. This mineral forms aggregates of blue grains up to 1 mm. It is optically biaxial (-), n(p) = 1.512(2), n(m) = 1.525(2), n(g) = 1.531(2), 2V = 70(10)degrees. The chemical composition of the holotype sample is as follows (wt %): 1.12 MgO, 0.10 MnO, 3.15 FeO, 8.98 CuO, 18.02 ZnO, 32.49 SO3, and 36.75 H2O, total 100.61. The empirical formula is (Cu0.55Zn0.45)(sigma 1.00)(Zn0.64Fe0.22Mg0.14Mn0.01)(sigma 1.01)S1.99O7.98 . 10.02H(2)O. The crystal structure of belogubite is studied using the single crystal method, R = 0.016. The mineral is triclinic, P (1) over bar The unit cell parameters are: a = 6.2548(1), b = 10.6112(2), c = 6.0439(1) angstrom, alpha = 82.587(1), beta = 109.625(1), gamma = 104.848(1)degrees, V = 364.81(1) angstrom(3), and Z = 1. The strongest reflections of the powder XRD pattern [d(meas)., angstrom (I, %) (hkl) are: 5.73 (35) (100), 5.576 (47) (-110), 4.873 (100) (-111), 3.907 (31) (021), 3.719 (45) (0 -21), 3.229 (27) (111), 2.915 (25) (221), and 2.684 (26) (130).
ER  -

KASATKIN, A. V., S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA, A. A. AGAKHANOV a D. I. BELAKOVSKIY. Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia. \textit{Geology of Ore Deposits}. Pleiades Publishing, 2020, roč.~62, č.~7, s.~599-607. ISSN~1075-7015. Dostupné z: https://dx.doi.org/10.1134/S1075701520070065.

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