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ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ. / Erokhin, Yu.v.; Pekov, I.v.; Vakhrusheva, N.v.; Shiryaev, P.b.; Yapaskurt, V.o.; Britvin, S.n.

In: МИНЕРАЛОГИЯ (MINERALOGY), Vol. 9, No. 3, 11.2023, p. 5-14.

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

Harvard

Erokhin, YV, Pekov, IV, Vakhrusheva, NV, Shiryaev, PB, Yapaskurt, VO & Britvin, SN 2023, 'ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ', МИНЕРАЛОГИЯ (MINERALOGY), vol. 9, no. 3, pp. 5-14. https://doi.org/10.35597/2313-545x-2023-9-3-1

APA

Erokhin, Y. V., Pekov, I. V., Vakhrusheva, N. V., Shiryaev, P. B., Yapaskurt, V. O., & Britvin, S. N. (2023). ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ. МИНЕРАЛОГИЯ (MINERALOGY), 9(3), 5-14. https://doi.org/10.35597/2313-545x-2023-9-3-1

Vancouver

Erokhin YV, Pekov IV, Vakhrusheva NV, Shiryaev PB, Yapaskurt VO, Britvin SN. ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ. МИНЕРАЛОГИЯ (MINERALOGY). 2023 Nov;9(3):5-14. https://doi.org/10.35597/2313-545x-2023-9-3-1

Author

Erokhin, Yu.v. ; Pekov, I.v. ; Vakhrusheva, N.v. ; Shiryaev, P.b. ; Yapaskurt, V.o. ; Britvin, S.n. / ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ. In: МИНЕРАЛОГИЯ (MINERALOGY). 2023 ; Vol. 9, No. 3. pp. 5-14.

BibTeX

@article{7998750208474a61b971d627b3a5bb0e,
title = "ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ",
abstract = "Glaukosphaerite and mcguinnessite (carbonates of the rosasite-malachite group) are found in chromitites of the Burkhoyla area, which is located in the northern part of the Voykar-Synya ultramafc massif (Polar Urals). The minerals form green and bluish-green flms, small crystals and spherulites (up to 0.3 mm) in cavities of weathered chromitites. This is the frst reliable fnd of glaukosphaerite in Russia. The chemical composition of glaukosphaerite is as follows (wt %): 25.14 NiO, 0.44 CoO, 0.89 FeO, 34.45 CuO, 7.90 MgO, 21.65 CO2 (calc.), 8.86 H2O (calc.), total 99.33. The empirical formula calculated based on the cation sum is (Cu0.88Ni0.68Mg0.40Fe0.03Co0.01)2.00(CO3)(OH)2. The parameters of the monoclinic unit cell of glaukosphaerite calculated from the powder X-ray diffraction data are: a = 12.070(3), b = 9.363(2), c = 3.131(1) A, ? = 98.03(2)?, V = 350.3(3) A3. The formation of these carbonates is related to supergene alteration of sulfdes (pentlandite and bornite) in chromitites.",
author = "Yu.v. Erokhin and I.v. Pekov and N.v. Vakhrusheva and P.b. Shiryaev and V.o. Yapaskurt and S.n. Britvin",
year = "2023",
month = nov,
doi = "10.35597/2313-545x-2023-9-3-1",
language = "русский",
volume = "9",
pages = "5--14",
journal = "Минералогия",
issn = "2313-545X",
publisher = "Южно-Уральский федеральный научный центр минералогии и геоэкологии Уральского отделения Российской академии наук",
number = "3",

}

RIS

TY - JOUR

T1 - ГЛАУКОСФЕРИТ ИЗ ХРОМИТИТОВ ВОЙКАРО-СЫНЬИНСКОГО МАССИВА (ПОЛЯРНЫЙ УРАЛ) – ПЕРВАЯ ДОСТОВЕРНАЯ НАХОДКА В РОССИИ

AU - Erokhin, Yu.v.

AU - Pekov, I.v.

AU - Vakhrusheva, N.v.

AU - Shiryaev, P.b.

AU - Yapaskurt, V.o.

AU - Britvin, S.n.

PY - 2023/11

Y1 - 2023/11

N2 - Glaukosphaerite and mcguinnessite (carbonates of the rosasite-malachite group) are found in chromitites of the Burkhoyla area, which is located in the northern part of the Voykar-Synya ultramafc massif (Polar Urals). The minerals form green and bluish-green flms, small crystals and spherulites (up to 0.3 mm) in cavities of weathered chromitites. This is the frst reliable fnd of glaukosphaerite in Russia. The chemical composition of glaukosphaerite is as follows (wt %): 25.14 NiO, 0.44 CoO, 0.89 FeO, 34.45 CuO, 7.90 MgO, 21.65 CO2 (calc.), 8.86 H2O (calc.), total 99.33. The empirical formula calculated based on the cation sum is (Cu0.88Ni0.68Mg0.40Fe0.03Co0.01)2.00(CO3)(OH)2. The parameters of the monoclinic unit cell of glaukosphaerite calculated from the powder X-ray diffraction data are: a = 12.070(3), b = 9.363(2), c = 3.131(1) A, ? = 98.03(2)?, V = 350.3(3) A3. The formation of these carbonates is related to supergene alteration of sulfdes (pentlandite and bornite) in chromitites.

AB - Glaukosphaerite and mcguinnessite (carbonates of the rosasite-malachite group) are found in chromitites of the Burkhoyla area, which is located in the northern part of the Voykar-Synya ultramafc massif (Polar Urals). The minerals form green and bluish-green flms, small crystals and spherulites (up to 0.3 mm) in cavities of weathered chromitites. This is the frst reliable fnd of glaukosphaerite in Russia. The chemical composition of glaukosphaerite is as follows (wt %): 25.14 NiO, 0.44 CoO, 0.89 FeO, 34.45 CuO, 7.90 MgO, 21.65 CO2 (calc.), 8.86 H2O (calc.), total 99.33. The empirical formula calculated based on the cation sum is (Cu0.88Ni0.68Mg0.40Fe0.03Co0.01)2.00(CO3)(OH)2. The parameters of the monoclinic unit cell of glaukosphaerite calculated from the powder X-ray diffraction data are: a = 12.070(3), b = 9.363(2), c = 3.131(1) A, ? = 98.03(2)?, V = 350.3(3) A3. The formation of these carbonates is related to supergene alteration of sulfdes (pentlandite and bornite) in chromitites.

UR - https://www.mendeley.com/catalogue/244b63bd-1a32-3885-aceb-aa5acb94030b/

U2 - 10.35597/2313-545x-2023-9-3-1

DO - 10.35597/2313-545x-2023-9-3-1

M3 - статья

VL - 9

SP - 5

EP - 14

JO - Минералогия

JF - Минералогия

SN - 2313-545X

IS - 3

ER -

ID: 113823544