Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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.
в: Geology of Ore Deposits, Том 56, № 5, 2014, стр. 380-394.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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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