KASATKIN, A. V., S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA, A. A. AGAKHANOV and 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, vol. 62, No 7, p. 599-607. ISSN 1075-7015. Available from: https://dx.doi.org/10.1134/S1075701520070065.
Other formats:   BibTeX LaTeX RIS
Basic information
Original name Belogubite, a New Mineral of the Chalcanthite Group from the Gaiskoe Deposit, South Urals, Russia
Authors KASATKIN, A. V. (guarantor), S. N. BRITVIN, N. V. CHUKANOV, Radek ŠKODA (203 Czech Republic, belonging to the institution), A. A. AGAKHANOV and D. I. BELAKOVSKIY.
Edition Geology of Ore Deposits, Pleiades Publishing, 2020, 1075-7015.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10504 Mineralogy
Country of publisher United States of America
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 0.670
RIV identification code RIV/00216224:14310/20:00124334
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1134/S1075701520070065
UT WoS 000616319600006
Keywords in English belogubite; new mineral; chalcanthite group; Gaiskoe deposit; South Urals
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 1/3/2022 13:12.
Abstract
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).
PrintDisplayed: 18/7/2024 16:56