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НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ). / Kasatkin, A. V.; Zubkova, N. V.; Chukanov, N. V.; Ksenofontov, D. A.; Škoda, R.; Tishchenko, A. I.; Voronin, M. V.; Britvin, S. N.; Pekov, I. V.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 150, № 6, 2021, стр. 96-112.

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

Harvard

Kasatkin, AV, Zubkova, NV, Chukanov, NV, Ksenofontov, DA, Škoda, R, Tishchenko, AI, Voronin, MV, Britvin, SN & Pekov, IV 2021, 'НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 150, № 6, стр. 96-112. https://doi.org/10.31857/S0869605521060034

APA

Kasatkin, A. V., Zubkova, N. V., Chukanov, N. V., Ksenofontov, D. A., Škoda, R., Tishchenko, A. I., Voronin, M. V., Britvin, S. N., & Pekov, I. V. (2021). НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 150(6), 96-112. https://doi.org/10.31857/S0869605521060034

Vancouver

Kasatkin AV, Zubkova NV, Chukanov NV, Ksenofontov DA, Škoda R, Tishchenko AI и пр. НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2021;150(6):96-112. https://doi.org/10.31857/S0869605521060034

Author

Kasatkin, A. V. ; Zubkova, N. V. ; Chukanov, N. V. ; Ksenofontov, D. A. ; Škoda, R. ; Tishchenko, A. I. ; Voronin, M. V. ; Britvin, S. N. ; Pekov, I. V. / НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2021 ; Том 150, № 6. стр. 96-112.

BibTeX

@article{b4062b75b4a246e1828229fb6b1dc15b,
title = "НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ)",
abstract = "Julgoldite-(Fe3+), a rare mineral of the pumpellyite group, has been found at the Karadag volcanic massif (Crimea peninsula) as black radial aggregates up to 0.5 cm in diameter with. It occurs in cracks of a volcanic rock and is associated with quartz. Its chemical composition [wt. %, electron microprobe analysis (EMPA), Fe3+ : Fe2+ ratio calculated from M{\"o}ssbauer data] is: CaO 20.40, MgO 0.35, MnO 0.10, FeO 3.62, Al2O3 0.10, Fe2O3 37.91, SiO2 32.86, H2O (calc.) 5.68, total 101.02. Parameters of monoclinic unit cell refined from powder X-ray diffraction (XRD) data are: a = 8.8885(7), b = 6.0791(4), c = 19.3679(14) {\AA}, β = 97.499(5)°, V = = 1037.58(13) {\AA}3; space group A2/m. The combination of the results of EMPA and XRD together with M{\"o}ssbauer, IR and Raman spectroscopic data makes it possible to write the crystal chemical formula of Karadag julgoldite-(Fe3+) with such possible variations in the distribution of Fe3+ and Fe2+ between the X and Y structural sites: Ca2.00X (Fe30.77–0.62+ Fe0.13–0.282 + Mg0.05Mn0.01)Σ0.95 Y(Fe1.84–1.993+ Fe0.15–0.002 + Al0.01 )Σ2.00[Si2OO106 (OH,O)][SiO4]O11(OH,O)O7(OH,H2O)O5(OH). The Karadag mineral is unusually rich in iron and almost does not contain a pumpellyite component. In addition, unlike many other minerals of the pumpellyite group, where all the hydrogen belongs to OH groups, julgoldite-(Fe3+) from Karadag contains molecular water, albeit in a small amount.",
keywords = "Crimea peninsula, Crystal structure, IR spectrum, Julgoldite-(Fe), Karadag volcanic massif, M{\"o}ssbauer spectrum, Pumpellyite group, Raman spectrum",
author = "Kasatkin, {A. V.} and Zubkova, {N. V.} and Chukanov, {N. V.} and Ksenofontov, {D. A.} and R. {\v S}koda and Tishchenko, {A. I.} and Voronin, {M. V.} and Britvin, {S. N.} and Pekov, {I. V.}",
note = "Publisher Copyright: {\textcopyright} 2021 Eco-Vector LLC. All rights reserved.",
year = "2021",
doi = "10.31857/S0869605521060034",
language = "русский",
volume = "150",
pages = "96--112",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "6",

}

RIS

TY - JOUR

T1 - НЕОБЫЧНО БОГАТЫЙ ЖЕЛЕЗОМ ДЖУЛГОЛДИТ-(Fe3+) ИЗ КАРАДАГСКОГО ВУЛКАНИЧЕСКОГО МАССИВА (КРЫМСКИЙ ПОЛУОСТРОВ)

AU - Kasatkin, A. V.

AU - Zubkova, N. V.

AU - Chukanov, N. V.

AU - Ksenofontov, D. A.

AU - Škoda, R.

AU - Tishchenko, A. I.

AU - Voronin, M. V.

AU - Britvin, S. N.

AU - Pekov, I. V.

N1 - Publisher Copyright: © 2021 Eco-Vector LLC. All rights reserved.

PY - 2021

Y1 - 2021

N2 - Julgoldite-(Fe3+), a rare mineral of the pumpellyite group, has been found at the Karadag volcanic massif (Crimea peninsula) as black radial aggregates up to 0.5 cm in diameter with. It occurs in cracks of a volcanic rock and is associated with quartz. Its chemical composition [wt. %, electron microprobe analysis (EMPA), Fe3+ : Fe2+ ratio calculated from Mössbauer data] is: CaO 20.40, MgO 0.35, MnO 0.10, FeO 3.62, Al2O3 0.10, Fe2O3 37.91, SiO2 32.86, H2O (calc.) 5.68, total 101.02. Parameters of monoclinic unit cell refined from powder X-ray diffraction (XRD) data are: a = 8.8885(7), b = 6.0791(4), c = 19.3679(14) Å, β = 97.499(5)°, V = = 1037.58(13) Å3; space group A2/m. The combination of the results of EMPA and XRD together with Mössbauer, IR and Raman spectroscopic data makes it possible to write the crystal chemical formula of Karadag julgoldite-(Fe3+) with such possible variations in the distribution of Fe3+ and Fe2+ between the X and Y structural sites: Ca2.00X (Fe30.77–0.62+ Fe0.13–0.282 + Mg0.05Mn0.01)Σ0.95 Y(Fe1.84–1.993+ Fe0.15–0.002 + Al0.01 )Σ2.00[Si2OO106 (OH,O)][SiO4]O11(OH,O)O7(OH,H2O)O5(OH). The Karadag mineral is unusually rich in iron and almost does not contain a pumpellyite component. In addition, unlike many other minerals of the pumpellyite group, where all the hydrogen belongs to OH groups, julgoldite-(Fe3+) from Karadag contains molecular water, albeit in a small amount.

AB - Julgoldite-(Fe3+), a rare mineral of the pumpellyite group, has been found at the Karadag volcanic massif (Crimea peninsula) as black radial aggregates up to 0.5 cm in diameter with. It occurs in cracks of a volcanic rock and is associated with quartz. Its chemical composition [wt. %, electron microprobe analysis (EMPA), Fe3+ : Fe2+ ratio calculated from Mössbauer data] is: CaO 20.40, MgO 0.35, MnO 0.10, FeO 3.62, Al2O3 0.10, Fe2O3 37.91, SiO2 32.86, H2O (calc.) 5.68, total 101.02. Parameters of monoclinic unit cell refined from powder X-ray diffraction (XRD) data are: a = 8.8885(7), b = 6.0791(4), c = 19.3679(14) Å, β = 97.499(5)°, V = = 1037.58(13) Å3; space group A2/m. The combination of the results of EMPA and XRD together with Mössbauer, IR and Raman spectroscopic data makes it possible to write the crystal chemical formula of Karadag julgoldite-(Fe3+) with such possible variations in the distribution of Fe3+ and Fe2+ between the X and Y structural sites: Ca2.00X (Fe30.77–0.62+ Fe0.13–0.282 + Mg0.05Mn0.01)Σ0.95 Y(Fe1.84–1.993+ Fe0.15–0.002 + Al0.01 )Σ2.00[Si2OO106 (OH,O)][SiO4]O11(OH,O)O7(OH,H2O)O5(OH). The Karadag mineral is unusually rich in iron and almost does not contain a pumpellyite component. In addition, unlike many other minerals of the pumpellyite group, where all the hydrogen belongs to OH groups, julgoldite-(Fe3+) from Karadag contains molecular water, albeit in a small amount.

KW - Crimea peninsula

KW - Crystal structure

KW - IR spectrum

KW - Julgoldite-(Fe)

KW - Karadag volcanic massif

KW - Mössbauer spectrum

KW - Pumpellyite group

KW - Raman spectrum

UR - http://www.scopus.com/inward/record.url?scp=85123699500&partnerID=8YFLogxK

U2 - 10.31857/S0869605521060034

DO - 10.31857/S0869605521060034

M3 - статья

AN - SCOPUS:85123699500

VL - 150

SP - 96

EP - 112

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 6

ER -

ID: 93117792