Radioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R.

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dc.contributor.authorKurbatov, L M
dc.coverage.spatialMEDIAN LATITUDE: 61.812065 * MEDIAN LONGITUDE: 34.867215 * SOUTH-BOUND LATITUDE: 61.592650 * WEST-BOUND LONGITUDE: 34.151840 * NORTH-BOUND LATITUDE: 62.031480 * EAST-BOUND LONGITUDE: 35.582590 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m
dc.date.accessioned2020-08-25T08:14:56Z
dc.date.available2020-08-25T08:14:56Z
dc.date.issued1935-03-22
dc.description.abstractThe radioactivity of bottom sediments has been but little investigated. Data published by Joly, Pettersson, Piggot and Iimori refer to determinations of radium, contained mainly in oceanic deep-water sediments in red clays, radiolarian, globigerina oozes, blue muds and manganese concretions. The determinations have shown the manganese concretions to be richest as regards content of radium (up to 10-8 per cent); red clays and radiolarian ooze also possess a rather high content of radium. Other types of sediments are less rich in radium.
dc.formattext/tab-separated-values, 16 data points
dc.identifierhttps://doi.pangaea.de/10.1594/PANGAEA.859059
dc.identifierhttps://doi.org/10.1594/PANGAEA.859059
dc.identifier.citationKurbatov, L M (1935): Radioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R. Nature, 136(3448), 871-871, https://doi.org/10.1038/136871a0
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/17579
dc.language.isoen
dc.publisherPANGAEA
dc.relationGrant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
dc.relationWarnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
dc.rightsCC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rightsAccess constraints: unrestricted
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceSupplement to: Kurbatov, L M (1935): Radioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R. Nature, 136(3448), 871-871, https://doi.org/10.1038/136871a0
dc.subjectDeposit type
dc.subjectDEPTH, sediment/rock
dc.subjectDescription
dc.subjectIdentification
dc.subjectLake_Konch_K
dc.subjectLake_Onega_K
dc.subjectLake Konch, Karelia,Russia
dc.subjectLake Onega, Karelia, Russia
dc.subjectNOAA and MMS Marine Minerals Geochemical Database
dc.subjectNOAA-MMS
dc.subjectPosition
dc.subjectQuantity of deposit
dc.subjectRadium
dc.subjectSize
dc.subjectVisual description
dc.titleRadioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R.
dc.title.alternativeAnnotated record and radium content of the detailed examination of manganese nodules from lakes in Karelia, Russia
dc.typeDataset

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