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Mobility of cerium in the 2.8-2.1 Ga exogenous environments of the Baltic Shield : Data on weathering profiles and sedimentary carbonates. / Alfimova, N. A.; Felitsyn, S. B.; Matrenichev, V. A.

в: Lithology and Mineral Resources, Том 46, № 5, 01.09.2011, стр. 397-408.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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@article{2b025904da3644a19345b505e3729412,
title = "Mobility of cerium in the 2.8-2.1 Ga exogenous environments of the Baltic Shield: Data on weathering profiles and sedimentary carbonates",
abstract = "The absence of Ce anomaly and significant positive correlation between Ce and Fe in the weathering profiles and sedimentary carbonate rocks of the Baltic Shield with an age of 2.8-2.1 Ga indicate that Fe3+ was the main form of Fe migration in the Archean-Paleoproterozoic exogenous environments in the Baltic Shield. The Ce distribution was mainly controlled by hydrogen index rather than redox conditions.",
author = "Alfimova, {N. A.} and Felitsyn, {S. B.} and Matrenichev, {V. A.}",
year = "2011",
month = sep,
day = "1",
doi = "10.1134/S0024490211050026",
language = "English",
volume = "46",
pages = "397--408",
journal = "Lithology and Mineral Resources",
issn = "0024-4902",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Mobility of cerium in the 2.8-2.1 Ga exogenous environments of the Baltic Shield

T2 - Data on weathering profiles and sedimentary carbonates

AU - Alfimova, N. A.

AU - Felitsyn, S. B.

AU - Matrenichev, V. A.

PY - 2011/9/1

Y1 - 2011/9/1

N2 - The absence of Ce anomaly and significant positive correlation between Ce and Fe in the weathering profiles and sedimentary carbonate rocks of the Baltic Shield with an age of 2.8-2.1 Ga indicate that Fe3+ was the main form of Fe migration in the Archean-Paleoproterozoic exogenous environments in the Baltic Shield. The Ce distribution was mainly controlled by hydrogen index rather than redox conditions.

AB - The absence of Ce anomaly and significant positive correlation between Ce and Fe in the weathering profiles and sedimentary carbonate rocks of the Baltic Shield with an age of 2.8-2.1 Ga indicate that Fe3+ was the main form of Fe migration in the Archean-Paleoproterozoic exogenous environments in the Baltic Shield. The Ce distribution was mainly controlled by hydrogen index rather than redox conditions.

UR - http://www.scopus.com/inward/record.url?scp=80052005000&partnerID=8YFLogxK

U2 - 10.1134/S0024490211050026

DO - 10.1134/S0024490211050026

M3 - Article

AN - SCOPUS:80052005000

VL - 46

SP - 397

EP - 408

JO - Lithology and Mineral Resources

JF - Lithology and Mineral Resources

SN - 0024-4902

IS - 5

ER -

ID: 41539118