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Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle : FTIR and STA + QMS Data. / Babushkina, M. S.; Ugolkov, V. L.; Marin, Yu B.; Nikitina, L. P.; Goncharov, A. G.

в: Doklady Earth Sciences, Том 479, № 2, 01.04.2018, стр. 456-459.

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

Harvard

Babushkina, MS, Ugolkov, VL, Marin, YB, Nikitina, LP & Goncharov, AG 2018, 'Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle: FTIR and STA + QMS Data', Doklady Earth Sciences, Том. 479, № 2, стр. 456-459. https://doi.org/10.1134/S1028334X18040013

APA

Babushkina, M. S., Ugolkov, V. L., Marin, Y. B., Nikitina, L. P., & Goncharov, A. G. (2018). Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle: FTIR and STA + QMS Data. Doklady Earth Sciences, 479(2), 456-459. https://doi.org/10.1134/S1028334X18040013

Vancouver

Babushkina MS, Ugolkov VL, Marin YB, Nikitina LP, Goncharov AG. Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle: FTIR and STA + QMS Data. Doklady Earth Sciences. 2018 Апр. 1;479(2):456-459. https://doi.org/10.1134/S1028334X18040013

Author

Babushkina, M. S. ; Ugolkov, V. L. ; Marin, Yu B. ; Nikitina, L. P. ; Goncharov, A. G. / Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle : FTIR and STA + QMS Data. в: Doklady Earth Sciences. 2018 ; Том 479, № 2. стр. 456-459.

BibTeX

@article{894641217a914ef09e943894b3ec8f3e,
title = "Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle: FTIR and STA + QMS Data",
abstract = "Using IR–Fourier spectrometry (FTIR) and simultaneous thermal analysis combined with quadrupole mass spectrometry of thermal decomposition products (STA + QMS), olivines and clinopyroxene from xenolites of spinel and garnet lherzolites contained in kimberlites and alkaline basalts were studied to confirm the occurrence of hydrogen and carbon within the structure of the minerals, as well as to specify the forms of H and C. The presence of hydroxyl ions (OH–) and molecules of crystal hydrate water (H2Ocryst) along with CO2, CH, CH2, and CH3 groups was detected, which remained within the structures of mantle minerals up to 1300°C (by the data of both techniques). The total water (OH–and H2Ocryst) was the prevailing component of the C–O–H system.",
author = "Babushkina, {M. S.} and Ugolkov, {V. L.} and Marin, {Yu B.} and Nikitina, {L. P.} and Goncharov, {A. G.}",
year = "2018",
month = apr,
day = "1",
doi = "10.1134/S1028334X18040013",
language = "English",
volume = "479",
pages = "456--459",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Hydrogen and Carbon Groups in the Structures of Rock-Forming Minerals of Rocks of the Lithospheric Mantle

T2 - FTIR and STA + QMS Data

AU - Babushkina, M. S.

AU - Ugolkov, V. L.

AU - Marin, Yu B.

AU - Nikitina, L. P.

AU - Goncharov, A. G.

PY - 2018/4/1

Y1 - 2018/4/1

N2 - Using IR–Fourier spectrometry (FTIR) and simultaneous thermal analysis combined with quadrupole mass spectrometry of thermal decomposition products (STA + QMS), olivines and clinopyroxene from xenolites of spinel and garnet lherzolites contained in kimberlites and alkaline basalts were studied to confirm the occurrence of hydrogen and carbon within the structure of the minerals, as well as to specify the forms of H and C. The presence of hydroxyl ions (OH–) and molecules of crystal hydrate water (H2Ocryst) along with CO2, CH, CH2, and CH3 groups was detected, which remained within the structures of mantle minerals up to 1300°C (by the data of both techniques). The total water (OH–and H2Ocryst) was the prevailing component of the C–O–H system.

AB - Using IR–Fourier spectrometry (FTIR) and simultaneous thermal analysis combined with quadrupole mass spectrometry of thermal decomposition products (STA + QMS), olivines and clinopyroxene from xenolites of spinel and garnet lherzolites contained in kimberlites and alkaline basalts were studied to confirm the occurrence of hydrogen and carbon within the structure of the minerals, as well as to specify the forms of H and C. The presence of hydroxyl ions (OH–) and molecules of crystal hydrate water (H2Ocryst) along with CO2, CH, CH2, and CH3 groups was detected, which remained within the structures of mantle minerals up to 1300°C (by the data of both techniques). The total water (OH–and H2Ocryst) was the prevailing component of the C–O–H system.

UR - http://www.scopus.com/inward/record.url?scp=85047243656&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18040013

DO - 10.1134/S1028334X18040013

M3 - Article

AN - SCOPUS:85047243656

VL - 479

SP - 456

EP - 459

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 28831738