Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea › Научные исследования в СПбГУ

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Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea. / Maslov, A. V.; Kuznetsov, A. B.; Politova, N. V.; Kozina, N. V.; Novigatsky, A. N.; Shevchenko, V. P.

в: Doklady Earth Sciences, Том 485, № 1, 01.03.2019, стр. 268-272.

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

Harvard

Maslov, AV, Kuznetsov, AB, Politova, NV, Kozina, NV, Novigatsky, AN & Shevchenko, VP 2019, 'Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea', Doklady Earth Sciences, Том. 485, № 1, стр. 268-272. https://doi.org/10.1134/S1028334X19030061

APA

Maslov, A. V., Kuznetsov, A. B., Politova, N. V., Kozina, N. V., Novigatsky, A. N., & Shevchenko, V. P. (2019). Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea. Doklady Earth Sciences, 485(1), 268-272. https://doi.org/10.1134/S1028334X19030061

Vancouver

Maslov AV, Kuznetsov AB, Politova NV, Kozina NV, Novigatsky AN, Shevchenko VP. Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea. Doklady Earth Sciences. 2019 Март 1;485(1):268-272. https://doi.org/10.1134/S1028334X19030061

Author

Maslov, A. V. ; Kuznetsov, A. B. ; Politova, N. V. ; Kozina, N. V. ; Novigatsky, A. N. ; Shevchenko, V. P. / Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea. в: Doklady Earth Sciences. 2019 ; Том 485, № 1. стр. 268-272.

BibTeX

@article{c1b54b36fd3e431b8a4dea2564e16d37,

title = "Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea",

abstract = "Abstract: The isotopic characteristics (εNd, 207Pb/206Pb, and 87Sr/86Sr) of the modern bottom sediments sampled in the Barents Sea during the 67th voyage of the R/V Akademik Mstislav Keldysh are considered. It is shown that the major contribution to the formation of the sediments in the central Barents Sea is made by rocks of the North European continental margin, which are found in the zone of influence of the North Cape Current. The values of εNd, 87Sr/86Sr are lower in the bottom sediments of this part of the sea than the corresponding characteristics of sedimentary material incorporated into ices and carried by the Transpolar Drift Stream. This allows one to conclude that such material has not contributed much to the sedimentation in the Barents Sea.",

author = "Maslov, {A. V.} and Kuznetsov, {A. B.} and Politova, {N. V.} and Kozina, {N. V.} and Novigatsky, {A. N.} and Shevchenko, {V. P.}",

year = "2019",

month = mar,

day = "1",

doi = "10.1134/S1028334X19030061",

language = "English",

volume = "485",

pages = "268--272",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "1",

}

RIS

TY - JOUR

T1 - Isotopic Composition of Nd, Pb, and Sr in Modern Bottom Sediments of the Barents Sea

AU - Maslov, A. V.

AU - Kuznetsov, A. B.

AU - Politova, N. V.

AU - Kozina, N. V.

AU - Novigatsky, A. N.

AU - Shevchenko, V. P.

PY - 2019/3/1

Y1 - 2019/3/1

N2 - Abstract: The isotopic characteristics (εNd, 207Pb/206Pb, and 87Sr/86Sr) of the modern bottom sediments sampled in the Barents Sea during the 67th voyage of the R/V Akademik Mstislav Keldysh are considered. It is shown that the major contribution to the formation of the sediments in the central Barents Sea is made by rocks of the North European continental margin, which are found in the zone of influence of the North Cape Current. The values of εNd, 87Sr/86Sr are lower in the bottom sediments of this part of the sea than the corresponding characteristics of sedimentary material incorporated into ices and carried by the Transpolar Drift Stream. This allows one to conclude that such material has not contributed much to the sedimentation in the Barents Sea.

AB - Abstract: The isotopic characteristics (εNd, 207Pb/206Pb, and 87Sr/86Sr) of the modern bottom sediments sampled in the Barents Sea during the 67th voyage of the R/V Akademik Mstislav Keldysh are considered. It is shown that the major contribution to the formation of the sediments in the central Barents Sea is made by rocks of the North European continental margin, which are found in the zone of influence of the North Cape Current. The values of εNd, 87Sr/86Sr are lower in the bottom sediments of this part of the sea than the corresponding characteristics of sedimentary material incorporated into ices and carried by the Transpolar Drift Stream. This allows one to conclude that such material has not contributed much to the sedimentation in the Barents Sea.

UR - http://www.scopus.com/inward/record.url?scp=85066462908&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19030061

DO - 10.1134/S1028334X19030061

M3 - Article

AN - SCOPUS:85066462908

VL - 485

SP - 268

EP - 272

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 75951625