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Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O). / Siidra, O.I.; Vergasova, L.P.; Kretser, Y.L.; Polekhovsky, Y.S.; Filatov, S.K.; Krivovichev, S.V.

в: Mineralogical Magazine, № 7, 2014, стр. 1699-1709.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Siidra, OI, Vergasova, LP, Kretser, YL, Polekhovsky, YS, Filatov, SK & Krivovichev, SV 2014, 'Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O)', Mineralogical Magazine, № 7, стр. 1699-1709. https://doi.org/10.1180/minmag.2014.078.7.13

APA

Siidra, O. I., Vergasova, L. P., Kretser, Y. L., Polekhovsky, Y. S., Filatov, S. K., & Krivovichev, S. V. (2014). Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O). Mineralogical Magazine, (7), 1699-1709. https://doi.org/10.1180/minmag.2014.078.7.13

Vancouver

Siidra OI, Vergasova LP, Kretser YL, Polekhovsky YS, Filatov SK, Krivovichev SV. Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O). Mineralogical Magazine. 2014;(7):1699-1709. https://doi.org/10.1180/minmag.2014.078.7.13

Author

Siidra, O.I. ; Vergasova, L.P. ; Kretser, Y.L. ; Polekhovsky, Y.S. ; Filatov, S.K. ; Krivovichev, S.V. / Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O). в: Mineralogical Magazine. 2014 ; № 7. стр. 1699-1709.

BibTeX

@article{45a799e499114b96a5cfe720d577a10e,
title = "Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O)",
abstract = "{\textcopyright} 2014 Mineralogical Society. Karpovite, ideally Tl2VO(SO4)2(H2O), was found in a fumarole of the 1st cinder cone of the North Breach of the Great Fissure Tolbachik volcano eruption (1975-1976), Kamchatka Peninsula, Russia. Karpovite occurs as bundles of white, needle-like crystals associated with shcherbinaite, pauflerite, bobjonesite, markhininite, evdokimovite and microcrystalline Mg, Al, Fe and Na sulfates. Karpovite is monoclinic, P21, a = 4.6524(4), b = 11.0757(9), c = 9.3876(7) {\AA}, β = 98.353(2)°, V = 478.60(7) {\AA}3, Z = 2 (from single-crystal diffraction data). The eight strongest lines of the X-ray powder diffraction pattern are (I/d/hkl): 64/4.289/012, 81/4.253/110, 38/3.683/111, 47/3.557/022, 100/3.438/1¯21, 52/2.982/013, 59/2.945/112, 54/2.354/132. The chemical composition determined by the electron microprobe analysis is (wt.%) Tl2O 61.43, VO2 11.53, SO3 23.55, H2O 2.61, total 99.12. The empirical formula (calculated on the basis of 10 O a.p.f.u.) is Tl2.00V0.96S2.03O9(H2O). The simplified formula o",
author = "O.I. Siidra and L.P. Vergasova and Y.L. Kretser and Y.S. Polekhovsky and S.K. Filatov and S.V. Krivovichev",
year = "2014",
doi = "10.1180/minmag.2014.078.7.13",
language = "English",
pages = "1699--1709",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "7",

}

RIS

TY - JOUR

T1 - Unique thallium mineralization in the fumaroles of the Tolbachik volcano, Kamchatka Peninsula, Russia. II. Karpovite, Tl2VO(SO4)2(H2O)

AU - Siidra, O.I.

AU - Vergasova, L.P.

AU - Kretser, Y.L.

AU - Polekhovsky, Y.S.

AU - Filatov, S.K.

AU - Krivovichev, S.V.

PY - 2014

Y1 - 2014

N2 - © 2014 Mineralogical Society. Karpovite, ideally Tl2VO(SO4)2(H2O), was found in a fumarole of the 1st cinder cone of the North Breach of the Great Fissure Tolbachik volcano eruption (1975-1976), Kamchatka Peninsula, Russia. Karpovite occurs as bundles of white, needle-like crystals associated with shcherbinaite, pauflerite, bobjonesite, markhininite, evdokimovite and microcrystalline Mg, Al, Fe and Na sulfates. Karpovite is monoclinic, P21, a = 4.6524(4), b = 11.0757(9), c = 9.3876(7) Å, β = 98.353(2)°, V = 478.60(7) Å3, Z = 2 (from single-crystal diffraction data). The eight strongest lines of the X-ray powder diffraction pattern are (I/d/hkl): 64/4.289/012, 81/4.253/110, 38/3.683/111, 47/3.557/022, 100/3.438/1¯21, 52/2.982/013, 59/2.945/112, 54/2.354/132. The chemical composition determined by the electron microprobe analysis is (wt.%) Tl2O 61.43, VO2 11.53, SO3 23.55, H2O 2.61, total 99.12. The empirical formula (calculated on the basis of 10 O a.p.f.u.) is Tl2.00V0.96S2.03O9(H2O). The simplified formula o

AB - © 2014 Mineralogical Society. Karpovite, ideally Tl2VO(SO4)2(H2O), was found in a fumarole of the 1st cinder cone of the North Breach of the Great Fissure Tolbachik volcano eruption (1975-1976), Kamchatka Peninsula, Russia. Karpovite occurs as bundles of white, needle-like crystals associated with shcherbinaite, pauflerite, bobjonesite, markhininite, evdokimovite and microcrystalline Mg, Al, Fe and Na sulfates. Karpovite is monoclinic, P21, a = 4.6524(4), b = 11.0757(9), c = 9.3876(7) Å, β = 98.353(2)°, V = 478.60(7) Å3, Z = 2 (from single-crystal diffraction data). The eight strongest lines of the X-ray powder diffraction pattern are (I/d/hkl): 64/4.289/012, 81/4.253/110, 38/3.683/111, 47/3.557/022, 100/3.438/1¯21, 52/2.982/013, 59/2.945/112, 54/2.354/132. The chemical composition determined by the electron microprobe analysis is (wt.%) Tl2O 61.43, VO2 11.53, SO3 23.55, H2O 2.61, total 99.12. The empirical formula (calculated on the basis of 10 O a.p.f.u.) is Tl2.00V0.96S2.03O9(H2O). The simplified formula o

U2 - 10.1180/minmag.2014.078.7.13

DO - 10.1180/minmag.2014.078.7.13

M3 - Article

SP - 1699

EP - 1709

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 7

ER -

ID: 7055781