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Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal). / Shkolnik, S. I.; Letnikov, F. A.; Strakhovenko, V. D. et al.

In: Doklady Earth Sciences, Vol. 471, No. 1, 01.11.2016, p. 1208-1212.

Research output: Contribution to journal › Article › peer-review

Harvard

Shkolnik, SI, Letnikov, FA, Strakhovenko, VD & Letnikova, AF 2016, 'Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal)', Doklady Earth Sciences, vol. 471, no. 1, pp. 1208-1212. https://doi.org/10.1134/S1028334X16110246

APA

Shkolnik, S. I., Letnikov, F. A., Strakhovenko, V. D., & Letnikova, A. F. (2016). Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal). Doklady Earth Sciences, 471(1), 1208-1212. https://doi.org/10.1134/S1028334X16110246

Vancouver

Shkolnik SI, Letnikov FA, Strakhovenko VD, Letnikova AF. Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal). Doklady Earth Sciences. 2016 Nov 1;471(1):1208-1212. doi: 10.1134/S1028334X16110246

Author

Shkolnik, S. I. ; Letnikov, F. A. ; Strakhovenko, V. D. et al. / Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal). In: Doklady Earth Sciences. 2016 ; Vol. 471, No. 1. pp. 1208-1212.

BibTeX

@article{8e05eb69406a43e596b8c13c499ae864,
title = "Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal)",
abstract = "The first data on the structure, textural features, and geochemical and mineral composition of Fe–Mn nodules of the Sasin Formation, Olkhon Island (Baikal), have been determined. A significant role in the formation of the nodules was played by hydrothermal processes with varying contributions of hydrogenic factors. The presence of reduced inclusions in the nodules and their textural features indicate the presence of various components of organic matter in the nodules, creating the conditions for local concentration of ore components. Activation of hydrothermal processes is typical for the Baikal Rift Zone in the Late Miocene–Early Pliocene, which is reflected in the composition of Fe–Mn nodules from the Sasin Formation.",
author = "Shkolnik, {S. I.} and Letnikov, {F. A.} and Strakhovenko, {V. D.} and Letnikova, {A. F.}",
year = "2016",
month = nov,
day = "1",
doi = "10.1134/S1028334X16110246",
language = "English",
volume = "471",
pages = "1208--1212",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Contribution of biogenic and volcanogenic factors to formation of ferromanganese nodules of Olkhon Island (Lake Baikal)

AU - Shkolnik, S. I.

AU - Letnikov, F. A.

AU - Strakhovenko, V. D.

AU - Letnikova, A. F.

PY - 2016/11/1

Y1 - 2016/11/1

N2 - The first data on the structure, textural features, and geochemical and mineral composition of Fe–Mn nodules of the Sasin Formation, Olkhon Island (Baikal), have been determined. A significant role in the formation of the nodules was played by hydrothermal processes with varying contributions of hydrogenic factors. The presence of reduced inclusions in the nodules and their textural features indicate the presence of various components of organic matter in the nodules, creating the conditions for local concentration of ore components. Activation of hydrothermal processes is typical for the Baikal Rift Zone in the Late Miocene–Early Pliocene, which is reflected in the composition of Fe–Mn nodules from the Sasin Formation.

AB - The first data on the structure, textural features, and geochemical and mineral composition of Fe–Mn nodules of the Sasin Formation, Olkhon Island (Baikal), have been determined. A significant role in the formation of the nodules was played by hydrothermal processes with varying contributions of hydrogenic factors. The presence of reduced inclusions in the nodules and their textural features indicate the presence of various components of organic matter in the nodules, creating the conditions for local concentration of ore components. Activation of hydrothermal processes is typical for the Baikal Rift Zone in the Late Miocene–Early Pliocene, which is reflected in the composition of Fe–Mn nodules from the Sasin Formation.

UR - http://www.scopus.com/inward/record.url?scp=84999723689&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16110246

DO - 10.1134/S1028334X16110246

M3 - Article

AN - SCOPUS:84999723689

VL - 471

SP - 1208

EP - 1212

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25764920