Standard

Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2. / Britvin, S.N.; Murashko, M.N.; Polekhovsky, Y.S.; Krivovichev, S.V.; Vereshchagin, O.S.; Zaitsev, A.N.; Vapnik, Y.; Shilovskikh, V.V.

в: Physics and Chemistry of Minerals, Том 46, № 4, 2019, стр. 361-369.

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

Harvard

Britvin, SN, Murashko, MN, Polekhovsky, YS, Krivovichev, SV, Vereshchagin, OS, Zaitsev, AN, Vapnik, Y & Shilovskikh, VV 2019, 'Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2.', Physics and Chemistry of Minerals, Том. 46, № 4, стр. 361-369. <http://elibrary.ru/item.asp?id=38622988>

APA

Britvin, S. N., Murashko, M. N., Polekhovsky, Y. S., Krivovichev, S. V., Vereshchagin, O. S., Zaitsev, A. N., Vapnik, Y., & Shilovskikh, V. V. (2019). Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2. Physics and Chemistry of Minerals, 46(4), 361-369. http://elibrary.ru/item.asp?id=38622988

Vancouver

Britvin SN, Murashko MN, Polekhovsky YS, Krivovichev SV, Vereshchagin OS, Zaitsev AN и пр. Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2. Physics and Chemistry of Minerals. 2019;46(4):361-369.

Author

Britvin, S.N. ; Murashko, M.N. ; Polekhovsky, Y.S. ; Krivovichev, S.V. ; Vereshchagin, O.S. ; Zaitsev, A.N. ; Vapnik, Y. ; Shilovskikh, V.V. / Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2. в: Physics and Chemistry of Minerals. 2019 ; Том 46, № 4. стр. 361-369.

BibTeX

@article{3f9818e0b98a4ceab2794bf360b80256,
title = "Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of l{\"o}llingite, FeAs 2.",
abstract = "Zuktamrurite, FeP 2 , is a new mineral, a natural iron diphosphide found in the pyrometamorphic rocks of the Hatrurim Formation, in the southern part of the Negev Desert, Israel and on the Transjordan Plateau, Jordan. The mineral occurs as irregular grains up to 50 µm in size associated with murashkoite, FeP, and barringerite, (Fe,Ni) 2 P. In reflected light, zuktamrurite is white with a distinct bluish tint. It is non-pleochroic but exhibits distinct anisotropy in bluish colours. Reflectance values for the IMA COM recommended wavelengths are [R max /R min , % (λ, nm)]: 50.40/47.20 (470); 49.16/46.23 (546); 48.97/46.16 (589); 49.40/46.40 (650). It is brittle. Electron microprobe analysis of the holotype specimen gave the following chemical composition (wt%, average of 5 points): Fe 40.23; Ni 7.97; P 51.70; total 99.90. The empirical formula calculated on the basis of 3 apfu is (Fe 0.86 Ni 0.16 ) 1.02 P 1.98",
author = "S.N. Britvin and M.N. Murashko and Y.S. Polekhovsky and S.V. Krivovichev and O.S. Vereshchagin and A.N. Zaitsev and Y. Vapnik and V.V. Shilovskikh",
year = "2019",
language = "English",
volume = "46",
pages = "361--369",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer Nature",
number = "4",

}

RIS

TY - JOUR

T1 - Zuktamrurite, FeP 2 , a new mineral, the phosphide analogue of löllingite, FeAs 2.

AU - Britvin, S.N.

AU - Murashko, M.N.

AU - Polekhovsky, Y.S.

AU - Krivovichev, S.V.

AU - Vereshchagin, O.S.

AU - Zaitsev, A.N.

AU - Vapnik, Y.

AU - Shilovskikh, V.V.

PY - 2019

Y1 - 2019

N2 - Zuktamrurite, FeP 2 , is a new mineral, a natural iron diphosphide found in the pyrometamorphic rocks of the Hatrurim Formation, in the southern part of the Negev Desert, Israel and on the Transjordan Plateau, Jordan. The mineral occurs as irregular grains up to 50 µm in size associated with murashkoite, FeP, and barringerite, (Fe,Ni) 2 P. In reflected light, zuktamrurite is white with a distinct bluish tint. It is non-pleochroic but exhibits distinct anisotropy in bluish colours. Reflectance values for the IMA COM recommended wavelengths are [R max /R min , % (λ, nm)]: 50.40/47.20 (470); 49.16/46.23 (546); 48.97/46.16 (589); 49.40/46.40 (650). It is brittle. Electron microprobe analysis of the holotype specimen gave the following chemical composition (wt%, average of 5 points): Fe 40.23; Ni 7.97; P 51.70; total 99.90. The empirical formula calculated on the basis of 3 apfu is (Fe 0.86 Ni 0.16 ) 1.02 P 1.98

AB - Zuktamrurite, FeP 2 , is a new mineral, a natural iron diphosphide found in the pyrometamorphic rocks of the Hatrurim Formation, in the southern part of the Negev Desert, Israel and on the Transjordan Plateau, Jordan. The mineral occurs as irregular grains up to 50 µm in size associated with murashkoite, FeP, and barringerite, (Fe,Ni) 2 P. In reflected light, zuktamrurite is white with a distinct bluish tint. It is non-pleochroic but exhibits distinct anisotropy in bluish colours. Reflectance values for the IMA COM recommended wavelengths are [R max /R min , % (λ, nm)]: 50.40/47.20 (470); 49.16/46.23 (546); 48.97/46.16 (589); 49.40/46.40 (650). It is brittle. Electron microprobe analysis of the holotype specimen gave the following chemical composition (wt%, average of 5 points): Fe 40.23; Ni 7.97; P 51.70; total 99.90. The empirical formula calculated on the basis of 3 apfu is (Fe 0.86 Ni 0.16 ) 1.02 P 1.98

M3 - Article

VL - 46

SP - 361

EP - 369

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

SN - 0342-1791

IS - 4

ER -

ID: 78463522