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Modern Bottom Sediments of Lake Onega : Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements. / Strakhovenko, V. D.; Subetto, D. A.; Ovdina, E. A. и др.

в: Doklady Earth Sciences, Том 481, № 2, 01.08.2018, стр. 988-992.

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

Harvard

Strakhovenko, VD, Subetto, DA, Ovdina, EA, Belkina, NA, Efremenko, NA & Maslov, AV 2018, 'Modern Bottom Sediments of Lake Onega: Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements', Doklady Earth Sciences, Том. 481, № 2, стр. 988-992. https://doi.org/10.1134/S1028334X1808010X

APA

Strakhovenko, V. D., Subetto, D. A., Ovdina, E. A., Belkina, N. A., Efremenko, N. A., & Maslov, A. V. (2018). Modern Bottom Sediments of Lake Onega: Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements. Doklady Earth Sciences, 481(2), 988-992. https://doi.org/10.1134/S1028334X1808010X

Vancouver

Strakhovenko VD, Subetto DA, Ovdina EA, Belkina NA, Efremenko NA, Maslov AV. Modern Bottom Sediments of Lake Onega: Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements. Doklady Earth Sciences. 2018 авг. 1;481(2):988-992. doi: 10.1134/S1028334X1808010X

Author

Strakhovenko, V. D. ; Subetto, D. A. ; Ovdina, E. A. и др. / Modern Bottom Sediments of Lake Onega : Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements. в: Doklady Earth Sciences. 2018 ; Том 481, № 2. стр. 988-992.

BibTeX

@article{dae5defb563f41bd84f6ec53a62b7ccd,
title = "Modern Bottom Sediments of Lake Onega: Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements",
abstract = "The results of studying the structure and mineral composition of the Upper Holocene bottom sediments of Lake Onega are presented. It is established that there are two types of columns of bottom sediments, for which stratification of layers and formation of Fe–Mn crusts are determined by the diagenesis processes occurring under physicochemical conditions of sediment accumulation according to two scenarios. The distribution spectra of rare-earth elements (REEs) are different in the indicated types of columns, which is apparently attributed to the differences in the oxidation–reduction conditions at the water–sediment interface during the formation of REEs and possibly to the influence of hydrothermal processes.",
author = "Strakhovenko, {V. D.} and Subetto, {D. A.} and Ovdina, {E. A.} and Belkina, {N. A.} and Efremenko, {N. A.} and Maslov, {A. V.}",
year = "2018",
month = aug,
day = "1",
doi = "10.1134/S1028334X1808010X",
language = "English",
volume = "481",
pages = "988--992",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Modern Bottom Sediments of Lake Onega

T2 - Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements

AU - Strakhovenko, V. D.

AU - Subetto, D. A.

AU - Ovdina, E. A.

AU - Belkina, N. A.

AU - Efremenko, N. A.

AU - Maslov, A. V.

PY - 2018/8/1

Y1 - 2018/8/1

N2 - The results of studying the structure and mineral composition of the Upper Holocene bottom sediments of Lake Onega are presented. It is established that there are two types of columns of bottom sediments, for which stratification of layers and formation of Fe–Mn crusts are determined by the diagenesis processes occurring under physicochemical conditions of sediment accumulation according to two scenarios. The distribution spectra of rare-earth elements (REEs) are different in the indicated types of columns, which is apparently attributed to the differences in the oxidation–reduction conditions at the water–sediment interface during the formation of REEs and possibly to the influence of hydrothermal processes.

AB - The results of studying the structure and mineral composition of the Upper Holocene bottom sediments of Lake Onega are presented. It is established that there are two types of columns of bottom sediments, for which stratification of layers and formation of Fe–Mn crusts are determined by the diagenesis processes occurring under physicochemical conditions of sediment accumulation according to two scenarios. The distribution spectra of rare-earth elements (REEs) are different in the indicated types of columns, which is apparently attributed to the differences in the oxidation–reduction conditions at the water–sediment interface during the formation of REEs and possibly to the influence of hydrothermal processes.

UR - http://www.scopus.com/inward/record.url?scp=85052811304&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1808010X

DO - 10.1134/S1028334X1808010X

M3 - Article

AN - SCOPUS:85052811304

VL - 481

SP - 988

EP - 992

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25764695