Radioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R.
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dc.contributor.author | Kurbatov, L M | |
dc.coverage.spatial | MEDIAN 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.accessioned | 2020-08-25T08:14:56Z | |
dc.date.available | 2020-08-25T08:14:56Z | |
dc.date.issued | 1935-03-22 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.859059 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.859059 | |
dc.identifier.citation | 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.identifier.uri | https://repository.geologyscience.ru/handle/123456789/17579 | |
dc.description.abstract | The 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.format | text/tab-separated-values, 16 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.relation | Grant, 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.relation | Warnken, 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.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.rights | info:eu-repo/semantics/openAccess | |
dc.source | Supplement 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.subject | Deposit type | |
dc.subject | DEPTH, sediment/rock | |
dc.subject | Description | |
dc.subject | Identification | |
dc.subject | Lake_Konch_K | |
dc.subject | Lake_Onega_K | |
dc.subject | Lake Konch, Karelia,Russia | |
dc.subject | Lake Onega, Karelia, Russia | |
dc.subject | NOAA and MMS Marine Minerals Geochemical Database | |
dc.subject | NOAA-MMS | |
dc.subject | Position | |
dc.subject | Quantity of deposit | |
dc.subject | Radium | |
dc.subject | Size | |
dc.subject | Visual description | |
dc.title | Radioactivity of Ferro-Manganese Formations in Seas and Lakes of the U.S.S.R. | |
dc.title.alternative | Annotated record and radium content of the detailed examination of manganese nodules from lakes in Karelia, Russia | |
dc.type | Dataset |
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