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dc.contributor.author Kalinenko, Valery V
dc.coverage.spatial MEDIAN LATITUDE: 71.210000 * MEDIAN LONGITUDE: 157.125500 * SOUTH-BOUND LATITUDE: 69.840000 * WEST-BOUND LONGITUDE: 129.850000 * NORTH-BOUND LATITUDE: 73.160000 * EAST-BOUND LONGITUDE: 178.970000 * DATE/TIME START: 1981-06-01T00:00:00 * DATE/TIME END: 1981-06-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 0.01 m
dc.date.accessioned 2019-11-13T06:20:17Z
dc.date.available 2019-11-13T06:20:17Z
dc.date.issued 2001-06-20
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.784672
dc.identifier https://doi.org/10.1594/PANGAEA.784672
dc.identifier.citation Kalinenko, Valery V (2001): Clay minerals in sediments of the Arctic Seas. Translated from Litologiya i Poleznye Iskopaemye, 2001, 4, 418-429, Lithology and Mineral Resources, 36(4), 362-372, https://doi.org/10.1023/A:1010414305264
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/6615
dc.description.abstract Distribution of clay minerals in recent sediments on the Arctic shelf off the Eurasian and North American continents is considered. Prominence is given to the East Siberian and Laptev seas. An illite belt established on the base of clay mineral composition in seven Arctic seas spreads from the Beaufort Sea to the White Sea and reveals a mineralogical zonality. The belt can be devided into smectite and chlorite provinces. Factors governing formation of the Arctic illite belt and features of distribution of individual clay minerals are discussed. Identification of the illite belt in sediments on the Arctic shelf complements the system of planetary latitudinal zones of clay minerals formulated by previous researchers.
dc.format text/tab-separated-values, 216 data points
dc.language.iso en
dc.publisher PANGAEA
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
dc.source Supplement to: Kalinenko, Valery V (2001): Clay minerals in sediments of the Arctic Seas. Translated from Litologiya i Poleznye Iskopaemye, 2001, 4, 418-429, Lithology and Mineral Resources, 36(4), 362-372, https://doi.org/10.1023/A:1010414305264
dc.subject Archive of Ocean Data
dc.subject ARCOD
dc.subject Area/locality
dc.subject BC
dc.subject Box corer
dc.subject Buor Khaya Bay, Laptev Sea
dc.subject Chaun Bay East Siberian Sea
dc.subject Chlorite
dc.subject Chlorite+Kaolinite
dc.subject Clay minerals
dc.subject DEPTH, sediment/rock
dc.subject Dm. Laptev Srait
dc.subject East Siberian Sea
dc.subject ESS281
dc.subject ESS282
dc.subject ESS284
dc.subject ESS285
dc.subject ESS286
dc.subject ESS288
dc.subject ESS289
dc.subject ESS290
dc.subject ESS291
dc.subject ESS292
dc.subject ESS293
dc.subject ESS295
dc.subject ESS314
dc.subject ESS315
dc.subject ESS316
dc.subject ESS317
dc.subject ESS318
dc.subject ESS320
dc.subject ESS323
dc.subject ESS327
dc.subject ESS328
dc.subject ESS329
dc.subject ESS333
dc.subject ESS334
dc.subject Illite
dc.subject Kaolinite
dc.subject Laptev Sea
dc.subject Long Strait
dc.subject QUEEN_Exped
dc.subject Smectite
dc.subject X-ray diffraction (XRD)
dc.title Clay minerals in sediments of the Arctic Seas.
dc.title.alternative (Table 2) Relative contents of clay minerals in <0.001 mm grain size fraction from surface layer bottom sediments of the East Siberian and Laptev Seas
dc.type Dataset


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