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Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation. / Kuleshov, V.N.; Brusnitsyn, A.I.; Starikova, E.V.

In: Geology of Ore Deposits, Vol. 56, No. 5, 2014, p. 380-394.

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

Harvard

Kuleshov, VN, Brusnitsyn, AI & Starikova, EV 2014, 'Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation', Geology of Ore Deposits, vol. 56, no. 5, pp. 380-394. https://doi.org/10.1134/S1075701514050067

APA

Kuleshov, V. N., Brusnitsyn, A. I., & Starikova, E. V. (2014). Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation. Geology of Ore Deposits, 56(5), 380-394. https://doi.org/10.1134/S1075701514050067

Vancouver

Kuleshov VN, Brusnitsyn AI, Starikova EV. Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation. Geology of Ore Deposits. 2014;56(5):380-394. https://doi.org/10.1134/S1075701514050067

Author

Kuleshov, V.N. ; Brusnitsyn, A.I. ; Starikova, E.V. / Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation. In: Geology of Ore Deposits. 2014 ; Vol. 56, No. 5. pp. 380-394.

BibTeX

@article{8c4484c678bd400e9689dc48b0986864,
title = "Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation",
abstract = "Based on new data on the lithology, mineralogy, chemistry, and isotopic composition of manganese carbonate ores and rocks at the deposits and occurrences in the Novaya Zemlya Archipelago, the Pai-Khoi, and the Urals, as well as using data from the literature, the main Phanerozoic basins of manganese deposition have been established in the geological history of Laurasia, Pangea, and Siberian paleocontinents. The formation conditions of manganese ore gradually changed from hydrothermal-sedimentary in the Middle Paleozoic to sedimentary-diagenetic in Mesozoic and Cenozoic. The ore was also formed under catagenetic conditions. Carbon of oxidized organic matter plays a substantial role in the formation of manganese carbonates.",
author = "V.N. Kuleshov and A.I. Brusnitsyn and E.V. Starikova",
year = "2014",
doi = "10.1134/S1075701514050067",
language = "English",
volume = "56",
pages = "380--394",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Manganese deposits in northeastern European Russia and the Urals: isotope geochemistry, genesis, and evolution of ore formation

AU - Kuleshov, V.N.

AU - Brusnitsyn, A.I.

AU - Starikova, E.V.

PY - 2014

Y1 - 2014

N2 - Based on new data on the lithology, mineralogy, chemistry, and isotopic composition of manganese carbonate ores and rocks at the deposits and occurrences in the Novaya Zemlya Archipelago, the Pai-Khoi, and the Urals, as well as using data from the literature, the main Phanerozoic basins of manganese deposition have been established in the geological history of Laurasia, Pangea, and Siberian paleocontinents. The formation conditions of manganese ore gradually changed from hydrothermal-sedimentary in the Middle Paleozoic to sedimentary-diagenetic in Mesozoic and Cenozoic. The ore was also formed under catagenetic conditions. Carbon of oxidized organic matter plays a substantial role in the formation of manganese carbonates.

AB - Based on new data on the lithology, mineralogy, chemistry, and isotopic composition of manganese carbonate ores and rocks at the deposits and occurrences in the Novaya Zemlya Archipelago, the Pai-Khoi, and the Urals, as well as using data from the literature, the main Phanerozoic basins of manganese deposition have been established in the geological history of Laurasia, Pangea, and Siberian paleocontinents. The formation conditions of manganese ore gradually changed from hydrothermal-sedimentary in the Middle Paleozoic to sedimentary-diagenetic in Mesozoic and Cenozoic. The ore was also formed under catagenetic conditions. Carbon of oxidized organic matter plays a substantial role in the formation of manganese carbonates.

U2 - 10.1134/S1075701514050067

DO - 10.1134/S1075701514050067

M3 - Article

VL - 56

SP - 380

EP - 394

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 5

ER -

ID: 7033545