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Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia. / Zhitova, E. S.; Krivovichev, S. V.; Zaitsev, A. N.; Vlasenko, N. S.

In: Geology of Ore Deposits, Vol. 59, No. 8, 01.12.2017, p. 745-751.

Research output: Contribution to journal › Article › peer-review

Harvard

Zhitova, ES, Krivovichev, SV, Zaitsev, AN & Vlasenko, NS 2017, 'Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia', Geology of Ore Deposits, vol. 59, no. 8, pp. 745-751. https://doi.org/10.1134/S1075701517080116

APA

Zhitova, E. S., Krivovichev, S. V., Zaitsev, A. N., & Vlasenko, N. S. (2017). Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia. Geology of Ore Deposits, 59(8), 745-751. https://doi.org/10.1134/S1075701517080116

Vancouver

Zhitova ES, Krivovichev SV, Zaitsev AN, Vlasenko NS. Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia. Geology of Ore Deposits. 2017 Dec 1;59(8):745-751. https://doi.org/10.1134/S1075701517080116

Author

Zhitova, E. S. ; Krivovichev, S. V. ; Zaitsev, A. N. ; Vlasenko, N. S. / Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia. In: Geology of Ore Deposits. 2017 ; Vol. 59, No. 8. pp. 745-751.

BibTeX

@article{066b60217fd74453afcc6389593a0c25,
title = "Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia",
abstract = "The paper describes the first finding of quintinite [Mg4Al2(OH)12][(CO3)(H2O)3] at the Mariinsky deposit in the Central Urals, Russia. The mineral occurs as white tabular crystals in cavities within altered gabbro in association with prehnite, calcite, and a chlorite-group mineral. Quintinite is the probable result of late hydrothermal alteration of primary mafic and ultramafic rocks hosting emerald-bearing glimmerite. According to electron microprobe data, the Mg: Al ratio is ~2: 1. IR spectroscopy has revealed hydroxyl and carbonate groups and H2O molecules in the mineral. According to single crystal XRD data, quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), c = 7.711(2) {\AA}, β = 103.09(3)°, V = 355.7(2) {\AA}3. Based on structure refinement, the polytype of quintinite should be denoted as 1M. This is the third approved occurrence of quintinite-1M in the world after the Kovdor complex and Bazhenovsky chrysotile–asbestos deposit.",
keywords = "hydrotalcite supergroup, layered double hydroxides, Mariinskoe (Malyshevskoe) deposit, quintinite-1M",
author = "Zhitova, {E. S.} and Krivovichev, {S. V.} and Zaitsev, {A. N.} and Vlasenko, {N. S.}",
year = "2017",
month = dec,
day = "1",
doi = "10.1134/S1075701517080116",
language = "English",
volume = "59",
pages = "745--751",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "8",

}

RIS

TY - JOUR

T1 - Quintinite-1M from the Mariinsky Deposit, Ural Emerald Mines, Central Urals, Russia

AU - Zhitova, E. S.

AU - Krivovichev, S. V.

AU - Zaitsev, A. N.

AU - Vlasenko, N. S.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - The paper describes the first finding of quintinite [Mg4Al2(OH)12][(CO3)(H2O)3] at the Mariinsky deposit in the Central Urals, Russia. The mineral occurs as white tabular crystals in cavities within altered gabbro in association with prehnite, calcite, and a chlorite-group mineral. Quintinite is the probable result of late hydrothermal alteration of primary mafic and ultramafic rocks hosting emerald-bearing glimmerite. According to electron microprobe data, the Mg: Al ratio is ~2: 1. IR spectroscopy has revealed hydroxyl and carbonate groups and H2O molecules in the mineral. According to single crystal XRD data, quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), c = 7.711(2) Å, β = 103.09(3)°, V = 355.7(2) Å3. Based on structure refinement, the polytype of quintinite should be denoted as 1M. This is the third approved occurrence of quintinite-1M in the world after the Kovdor complex and Bazhenovsky chrysotile–asbestos deposit.

AB - The paper describes the first finding of quintinite [Mg4Al2(OH)12][(CO3)(H2O)3] at the Mariinsky deposit in the Central Urals, Russia. The mineral occurs as white tabular crystals in cavities within altered gabbro in association with prehnite, calcite, and a chlorite-group mineral. Quintinite is the probable result of late hydrothermal alteration of primary mafic and ultramafic rocks hosting emerald-bearing glimmerite. According to electron microprobe data, the Mg: Al ratio is ~2: 1. IR spectroscopy has revealed hydroxyl and carbonate groups and H2O molecules in the mineral. According to single crystal XRD data, quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), c = 7.711(2) Å, β = 103.09(3)°, V = 355.7(2) Å3. Based on structure refinement, the polytype of quintinite should be denoted as 1M. This is the third approved occurrence of quintinite-1M in the world after the Kovdor complex and Bazhenovsky chrysotile–asbestos deposit.

KW - hydrotalcite supergroup

KW - layered double hydroxides

KW - Mariinskoe (Malyshevskoe) deposit

KW - quintinite-1M

UR - http://www.scopus.com/inward/record.url?scp=85042927219&partnerID=8YFLogxK

U2 - 10.1134/S1075701517080116

DO - 10.1134/S1075701517080116

M3 - Article

AN - SCOPUS:85042927219

VL - 59

SP - 745

EP - 751

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 8

ER -

ID: 35996387