Standard

Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia). / Zhitova, E. S.; Popov, M. P.; Krivovichev, S. V.; Zaitsev, A. N.; Vlasenko, N. S.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 145, № 6, 01.01.2016, стр. 90-101.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Zhitova, ES, Popov, MP, Krivovichev, SV, Zaitsev, AN & Vlasenko, NS 2016, 'Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 145, № 6, стр. 90-101.

APA

Zhitova, E. S., Popov, M. P., Krivovichev, S. V., Zaitsev, A. N., & Vlasenko, N. S. (2016). Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 145(6), 90-101.

Vancouver

Zhitova ES, Popov MP, Krivovichev SV, Zaitsev AN, Vlasenko NS. Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2016 Янв. 1;145(6):90-101.

Author

Zhitova, E. S. ; Popov, M. P. ; Krivovichev, S. V. ; Zaitsev, A. N. ; Vlasenko, N. S. / Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2016 ; Том 145, № 6. стр. 90-101.

BibTeX

@article{6716cd0a2ebb478b98250cb51bd28e8d,
title = "Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia)",
abstract = " The paper contains description of quintinite [Mg 4 Al 2 (OH) 12 ](CO 3 )(H 2 O) 3 for the first time found in the Mariinskoe deposit (the Middle Urals, Russia). The mineral occurs there as white tabular crystals in cavities of metasomatically altered gabbro in association with prehnite, calcite and a chlorite group mineral. Its formation seems to be connected with the late hydrothermal alteration of primary mafic and ultramafic rocks hosting the emerald-bearing glimmerites. The Mg:Al ratio was determined as ∼ 2:1 by electron microprobe analysis. IR-spectroscopy revealed in the mineral the presence of H2O molecules, hydroxyl and carbonate groups. Quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), {\~n} = 7.711(2) A, b = 103.09(3)°, V = 355.7(2) A 3 . Based on single-crystal structure refinement the polytype should be denoted as 1M. This is the third find of quintinite-1M in the world (after Kovdor massif and Bazhenovskoe chrisotile-asbestos deposit). ",
keywords = "Hydrotalcite supergroup, Layered double hydroxides, Mariinskoe (Malyshevskoe) deposit, Quintinite-1M",
author = "Zhitova, {E. S.} and Popov, {M. P.} and Krivovichev, {S. V.} and Zaitsev, {A. N.} and Vlasenko, {N. S.}",
year = "2016",
month = jan,
day = "1",
language = "English",
volume = "145",
pages = "90--101",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Quintinite-1M from the Mariinskoe deposit (Ural emerald mines, Middle Urals, Russia)

AU - Zhitova, E. S.

AU - Popov, M. P.

AU - Krivovichev, S. V.

AU - Zaitsev, A. N.

AU - Vlasenko, N. S.

PY - 2016/1/1

Y1 - 2016/1/1

N2 - The paper contains description of quintinite [Mg 4 Al 2 (OH) 12 ](CO 3 )(H 2 O) 3 for the first time found in the Mariinskoe deposit (the Middle Urals, Russia). The mineral occurs there as white tabular crystals in cavities of metasomatically altered gabbro in association with prehnite, calcite and a chlorite group mineral. Its formation seems to be connected with the late hydrothermal alteration of primary mafic and ultramafic rocks hosting the emerald-bearing glimmerites. The Mg:Al ratio was determined as ∼ 2:1 by electron microprobe analysis. IR-spectroscopy revealed in the mineral the presence of H2O molecules, hydroxyl and carbonate groups. Quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), ñ = 7.711(2) A, b = 103.09(3)°, V = 355.7(2) A 3 . Based on single-crystal structure refinement the polytype should be denoted as 1M. This is the third find of quintinite-1M in the world (after Kovdor massif and Bazhenovskoe chrisotile-asbestos deposit).

AB - The paper contains description of quintinite [Mg 4 Al 2 (OH) 12 ](CO 3 )(H 2 O) 3 for the first time found in the Mariinskoe deposit (the Middle Urals, Russia). The mineral occurs there as white tabular crystals in cavities of metasomatically altered gabbro in association with prehnite, calcite and a chlorite group mineral. Its formation seems to be connected with the late hydrothermal alteration of primary mafic and ultramafic rocks hosting the emerald-bearing glimmerites. The Mg:Al ratio was determined as ∼ 2:1 by electron microprobe analysis. IR-spectroscopy revealed in the mineral the presence of H2O molecules, hydroxyl and carbonate groups. Quintinite is monoclinic, space group C2/m, a =5.233(1), b = 9.051(2), ñ = 7.711(2) A, b = 103.09(3)°, V = 355.7(2) A 3 . Based on single-crystal structure refinement the polytype should be denoted as 1M. This is the third find of quintinite-1M in the world (after Kovdor massif and Bazhenovskoe chrisotile-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=85057601890&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:85057601890

VL - 145

SP - 90

EP - 101

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 6

ER -

ID: 45849712