Hatertite, Na2(Ca,Na)(Fe3+,Cu)2(AsO4)3, a new alluaudite-group mineral from Tolbachik fumaroles, Kamchatka peninsula, Russia

Standard

Hatertite, Na2(Ca,Na)(Fe3+,Cu)2(AsO4)3, a new alluaudite-group mineral from Tolbachik fumaroles, Kamchatka peninsula, Russia. / Krivovichev, S.V.; Vergasova, L.P.; Filatov, S.K.; Rybin, D.S.; Britvin, S.N.; Ananiev, V.V.

в: European Journal of Mineralogy, Том 25, № 4, 2013, стр. 683-691.

Результаты исследований: Научные публикации в периодических изданиях › статья

BibTeX

@article{a2e16835ca6846ad96f3c844c3186015,

title = "Hatertite, Na2(Ca,Na)(Fe3+,Cu)2(AsO4)3, a new alluaudite-group mineral from Tolbachik fumaroles, Kamchatka peninsula, Russia",

abstract = "Hatertite, ideally Na2(Ca, Na)(Fe3+, Cu)2(AsO4)3, was found in a fumarole of the North Breach of the Great fissure Tolbachik volcano eruption (1975–1976), Kamchatka Peninsula, Russia. The mineral occurs as individual, prismatic and tabular, honey-yellow crystals up to 0.3mm across. It has a vitreous luster and yellow streak. Hatertite is monoclinic, C2/c, a = 12.590(2), b = 12.993(3), c = 6.700(2){\AA}, β = 113.72(2)°, V = 1003.4(3){\AA}3, Z = 4, Dcalc = 4.06 g/cm3. The eight strongest lines of the powder X-ray diffraction pattern are [dobs in {\AA} (I) (hkl)]: 6.493(25)(020); 3.628 (25)(1̅31); 3.204(39)(1̅12,131); 3.065(18)(002); 2.976(28)(3̅12, 2̅22); 2.830(100)(240), 2.632(36)(1̅32); 1.647(19)(2̅04,640). Hatertite is optically positive, α = 1.820(3), β = 1.825(3), γ = 1.833(3), 2Vmeas. = 60(10)°, 2Vcalc. = 77°. The orientation is Y = b. The chemical composition determined by the electron-microprobe analysis is as follows (wt.%): Na2O 8.49, K2O 2.41, MnO 1.64, CaO 7.06, Fe2O3 11.15, ZnO 2.05, CuO 8.10, Al2O3 2.22, As2O",

author = "S.V. Krivovichev and L.P. Vergasova and S.K. Filatov and D.S. Rybin and S.N. Britvin and V.V. Ananiev",

year = "2013",

doi = "10.1127/0935-1221/2013/0025-2311",

language = "English",

volume = "25",

pages = "683--691",

journal = "European Journal of Mineralogy",

issn = "0935-1221",

publisher = "SCHWEIZERBART Science Publishers",

number = "4",

}

RIS

TY - JOUR

T1 - Hatertite, Na2(Ca,Na)(Fe3+,Cu)2(AsO4)3, a new alluaudite-group mineral from Tolbachik fumaroles, Kamchatka peninsula, Russia

AU - Krivovichev, S.V.

AU - Vergasova, L.P.

AU - Filatov, S.K.

AU - Rybin, D.S.

AU - Britvin, S.N.

AU - Ananiev, V.V.

PY - 2013

Y1 - 2013

N2 - Hatertite, ideally Na2(Ca, Na)(Fe3+, Cu)2(AsO4)3, was found in a fumarole of the North Breach of the Great fissure Tolbachik volcano eruption (1975–1976), Kamchatka Peninsula, Russia. The mineral occurs as individual, prismatic and tabular, honey-yellow crystals up to 0.3mm across. It has a vitreous luster and yellow streak. Hatertite is monoclinic, C2/c, a = 12.590(2), b = 12.993(3), c = 6.700(2)Å, β = 113.72(2)°, V = 1003.4(3)Å3, Z = 4, Dcalc = 4.06 g/cm3. The eight strongest lines of the powder X-ray diffraction pattern are [dobs in Å (I) (hkl)]: 6.493(25)(020); 3.628 (25)(1̅31); 3.204(39)(1̅12,131); 3.065(18)(002); 2.976(28)(3̅12, 2̅22); 2.830(100)(240), 2.632(36)(1̅32); 1.647(19)(2̅04,640). Hatertite is optically positive, α = 1.820(3), β = 1.825(3), γ = 1.833(3), 2Vmeas. = 60(10)°, 2Vcalc. = 77°. The orientation is Y = b. The chemical composition determined by the electron-microprobe analysis is as follows (wt.%): Na2O 8.49, K2O 2.41, MnO 1.64, CaO 7.06, Fe2O3 11.15, ZnO 2.05, CuO 8.10, Al2O3 2.22, As2O

AB - Hatertite, ideally Na2(Ca, Na)(Fe3+, Cu)2(AsO4)3, was found in a fumarole of the North Breach of the Great fissure Tolbachik volcano eruption (1975–1976), Kamchatka Peninsula, Russia. The mineral occurs as individual, prismatic and tabular, honey-yellow crystals up to 0.3mm across. It has a vitreous luster and yellow streak. Hatertite is monoclinic, C2/c, a = 12.590(2), b = 12.993(3), c = 6.700(2)Å, β = 113.72(2)°, V = 1003.4(3)Å3, Z = 4, Dcalc = 4.06 g/cm3. The eight strongest lines of the powder X-ray diffraction pattern are [dobs in Å (I) (hkl)]: 6.493(25)(020); 3.628 (25)(1̅31); 3.204(39)(1̅12,131); 3.065(18)(002); 2.976(28)(3̅12, 2̅22); 2.830(100)(240), 2.632(36)(1̅32); 1.647(19)(2̅04,640). Hatertite is optically positive, α = 1.820(3), β = 1.825(3), γ = 1.833(3), 2Vmeas. = 60(10)°, 2Vcalc. = 77°. The orientation is Y = b. The chemical composition determined by the electron-microprobe analysis is as follows (wt.%): Na2O 8.49, K2O 2.41, MnO 1.64, CaO 7.06, Fe2O3 11.15, ZnO 2.05, CuO 8.10, Al2O3 2.22, As2O

U2 - 10.1127/0935-1221/2013/0025-2311

DO - 10.1127/0935-1221/2013/0025-2311

M3 - Article

VL - 25

SP - 683

EP - 691

JO - European Journal of Mineralogy

JF - European Journal of Mineralogy

SN - 0935-1221

IS - 4

ER -

ID: 7409894