Avdoninite: New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O
- Авторлар: Pekov I.V.1, Krivovichev S.V.2, Chukanov N.V.3, Yapaskurt V.O.1, Sidorov E.G.4
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Мекемелер:
- Faculty of Geology
- St. Petersburg State University
- Institute of Problems of Chemical Physics
- Institute of Volcanology and Seismology, Far East Branch
- Шығарылым: Том 58, № 7 (2016)
- Беттер: 568-578
- Бөлім: New Minerals
- URL: https://journal-vniispk.ru/1075-7015/article/view/215105
- DOI: https://doi.org/10.1134/S1075701516070084
- ID: 215105
Дәйексөз келтіру
Аннотация
The paper reports new findings of avdoninite from deposits of active fumaroles in the Second Scoria Cone at the Northern Breach of the Great Fissure Tolbachik Eruption, Tolbachik Volcano, Kamchatka Peninsula, Russia. The crystal structure of the mineral has been determined for the first time, which has allowed reliable determination of its space group and unit cell dimensions, refinement of its formula K2Cu5-Cl8(OH)4 · 2H2O, and correct indexing of its X-ray powder diffraction pattern. Avdoninite is monoclinic, space group P21/c, a = 11.592(2), b = 6.5509(11), c = 11.745(2) Å, β = 91.104(6)°, V = 891.8(3) Å3, Z = 2. The crystal structure of this mineral has been determined on a single crystal R1 [F > 4σ (F)] = 0.063. It is based on sheets of copper–oxo-chloride complexes [Cu5Cl8(OH)4]2– parallel to (100). The K+ cation and H2O molecules are interlayers.
Авторлар туралы
I. Pekov
Faculty of Geology
Хат алмасуға жауапты Автор.
Email: igorpekov@mail.ru
Ресей, Moscow, 119991
S. Krivovichev
St. Petersburg State University
Email: igorpekov@mail.ru
Ресей, Universitetskaya nab. 7/9, St. Petersburg, 199034
N. Chukanov
Institute of Problems of Chemical Physics
Email: igorpekov@mail.ru
Ресей, Chernogolovka, Moscow oblast, 142432
V. Yapaskurt
Faculty of Geology
Email: igorpekov@mail.ru
Ресей, Moscow, 119991
E. Sidorov
Institute of Volcanology and Seismology, Far East Branch
Email: igorpekov@mail.ru
Ресей, bulv. Piipa, 9, Petropavlovsk-Kamchatsky, 683006
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