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

https://doi.org/10.1134/S1075701520070065

UT WoS

000616319600006

EID Scopus

2-s2.0-85100827385

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 Novosadová 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://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 = {https://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://doi.org/10.1134/S1075701520070065.

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