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Avdoninite : New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O. / Pekov, I. V.; Krivovichev, S. V.; Chukanov, N. V.; Yapaskurt, V. O.; Sidorov, E. G.

в: Geology of Ore Deposits, Том 58, № 7, 01.12.2016, стр. 568-578.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Pekov, IV, Krivovichev, SV, Chukanov, NV, Yapaskurt, VO & Sidorov, EG 2016, 'Avdoninite: New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O', Geology of Ore Deposits, Том. 58, № 7, стр. 568-578. https://doi.org/10.1134/S1075701516070084

APA

Pekov, I. V., Krivovichev, S. V., Chukanov, N. V., Yapaskurt, V. O., & Sidorov, E. G. (2016). Avdoninite: New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O. Geology of Ore Deposits, 58(7), 568-578. https://doi.org/10.1134/S1075701516070084

Vancouver

Pekov IV, Krivovichev SV, Chukanov NV, Yapaskurt VO, Sidorov EG. Avdoninite: New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O. Geology of Ore Deposits. 2016 Дек. 1;58(7):568-578. https://doi.org/10.1134/S1075701516070084

Author

Pekov, I. V. ; Krivovichev, S. V. ; Chukanov, N. V. ; Yapaskurt, V. O. ; Sidorov, E. G. / Avdoninite : New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O. в: Geology of Ore Deposits. 2016 ; Том 58, № 7. стр. 568-578.

BibTeX

@article{32644ca6a9444eb79b945a85e84d8fa5,
title = "Avdoninite: New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O",
abstract = "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) {\AA}, β = 91.104(6)°, V = 891.8(3) {\AA}3, 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.",
author = "Pekov, {I. V.} and Krivovichev, {S. V.} and Chukanov, {N. V.} and Yapaskurt, {V. O.} and Sidorov, {E. G.}",
year = "2016",
month = dec,
day = "1",
doi = "10.1134/S1075701516070084",
language = "English",
volume = "58",
pages = "568--578",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "7",

}

RIS

TY - JOUR

T1 - Avdoninite

T2 - New data, crystal structure and refined formula K2Cu5Cl8(OH)4 · 2H2O

AU - Pekov, I. V.

AU - Krivovichev, S. V.

AU - Chukanov, N. V.

AU - Yapaskurt, V. O.

AU - Sidorov, E. G.

PY - 2016/12/1

Y1 - 2016/12/1

N2 - 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.

AB - 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.

UR - http://www.scopus.com/inward/record.url?scp=85011843789&partnerID=8YFLogxK

U2 - 10.1134/S1075701516070084

DO - 10.1134/S1075701516070084

M3 - Article

AN - SCOPUS:85011843789

VL - 58

SP - 568

EP - 578

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 7

ER -

ID: 9184979