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СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ). / Osipov, A. S.; Antonov, A. A.; Bocharov, V. N.; Vlasenko, N. S.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 150, № 3, 01.01.2021, стр. 67-78.

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

Harvard

Osipov, AS, Antonov, AA, Bocharov, VN & Vlasenko, NS 2021, 'СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 150, № 3, стр. 67-78. https://doi.org/10.31857/S0869605521030072

APA

Osipov, A. S., Antonov, A. A., Bocharov, V. N., & Vlasenko, N. S. (2021). СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 150(3), 67-78. https://doi.org/10.31857/S0869605521030072

Vancouver

Osipov AS, Antonov AA, Bocharov VN, Vlasenko NS. СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2021 Янв. 1;150(3):67-78. https://doi.org/10.31857/S0869605521030072

Author

Osipov, A. S. ; Antonov, A. A. ; Bocharov, V. N. ; Vlasenko, N. S. / СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2021 ; Том 150, № 3. стр. 67-78.

BibTeX

@article{2e670586276241ceb1c925eeb074b63b,
title = "СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ)",
abstract = "This paper presents the mineralogical characteristics of stronadelphite Sr5(PO4)3F found in the eudialyte-aegirine-albite rocks of the Konder alkaline-ultrabasic massif (Khabarovsk krai). The mineral forms xenomorphic individuals up to 400 × 150 micrometers. It is associated with eudialyte, lamprophyllite, barytolmaprophyllite, microcline, titanite, nepheline, strontium-rich fluorapatite and other accessory minerals. Stronadelphite crystals are colourless and translucent. The chemical composition (formula is calulated based on 25 charge units) is (Sr4.21Ca0.61Ba0.07Na0.07Fe0.05)5.01(P3.01O11.93)F1.14. In chemical composition, the mineral is similar to stronadelphite from alkaline complexes of Kola Peninsula. The mineral identification was confirmed by the electron backscattered diffraction (EBSD) method. The crystallization of the mineral during the low-temperature hydrothermal alteration of alkaline rocks is assumed.",
keywords = "Alkaline rocks, Alkaline-ultrabasic complex, Konder massif, Sr-bearing fluorapatite, Stronadelphite",
author = "Osipov, {A. S.} and Antonov, {A. A.} and Bocharov, {V. N.} and Vlasenko, {N. S.}",
year = "2021",
month = jan,
day = "1",
doi = "10.31857/S0869605521030072",
language = "русский",
volume = "150",
pages = "67--78",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "3",

}

RIS

TY - JOUR

T1 - СТРОНАДЕЛЬФИТ ИЗ ЩЕЛОЧНЫХ ПОРОД КОНДЁРСКОГО МАССИВА (ХАБАРОВСКИЙ КРАЙ)

AU - Osipov, A. S.

AU - Antonov, A. A.

AU - Bocharov, V. N.

AU - Vlasenko, N. S.

PY - 2021/1/1

Y1 - 2021/1/1

N2 - This paper presents the mineralogical characteristics of stronadelphite Sr5(PO4)3F found in the eudialyte-aegirine-albite rocks of the Konder alkaline-ultrabasic massif (Khabarovsk krai). The mineral forms xenomorphic individuals up to 400 × 150 micrometers. It is associated with eudialyte, lamprophyllite, barytolmaprophyllite, microcline, titanite, nepheline, strontium-rich fluorapatite and other accessory minerals. Stronadelphite crystals are colourless and translucent. The chemical composition (formula is calulated based on 25 charge units) is (Sr4.21Ca0.61Ba0.07Na0.07Fe0.05)5.01(P3.01O11.93)F1.14. In chemical composition, the mineral is similar to stronadelphite from alkaline complexes of Kola Peninsula. The mineral identification was confirmed by the electron backscattered diffraction (EBSD) method. The crystallization of the mineral during the low-temperature hydrothermal alteration of alkaline rocks is assumed.

AB - This paper presents the mineralogical characteristics of stronadelphite Sr5(PO4)3F found in the eudialyte-aegirine-albite rocks of the Konder alkaline-ultrabasic massif (Khabarovsk krai). The mineral forms xenomorphic individuals up to 400 × 150 micrometers. It is associated with eudialyte, lamprophyllite, barytolmaprophyllite, microcline, titanite, nepheline, strontium-rich fluorapatite and other accessory minerals. Stronadelphite crystals are colourless and translucent. The chemical composition (formula is calulated based on 25 charge units) is (Sr4.21Ca0.61Ba0.07Na0.07Fe0.05)5.01(P3.01O11.93)F1.14. In chemical composition, the mineral is similar to stronadelphite from alkaline complexes of Kola Peninsula. The mineral identification was confirmed by the electron backscattered diffraction (EBSD) method. The crystallization of the mineral during the low-temperature hydrothermal alteration of alkaline rocks is assumed.

KW - Alkaline rocks

KW - Alkaline-ultrabasic complex

KW - Konder massif

KW - Sr-bearing fluorapatite

KW - Stronadelphite

UR - http://www.scopus.com/inward/record.url?scp=85120035549&partnerID=8YFLogxK

U2 - 10.31857/S0869605521030072

DO - 10.31857/S0869605521030072

M3 - статья

AN - SCOPUS:85120035549

VL - 150

SP - 67

EP - 78

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 3

ER -

ID: 102705419