Clay minerals in sediments of the Arctic Seas.

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dc.contributor.authorKalinenko, Valery V
dc.coverage.spatialMEDIAN 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.accessioned2019-11-13T06:20:17Z
dc.date.available2019-11-13T06:20:17Z
dc.date.issued2001-06-20
dc.description.abstractDistribution 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.formattext/tab-separated-values, 216 data points
dc.identifierhttps://doi.pangaea.de/10.1594/PANGAEA.784672
dc.identifierhttps://doi.org/10.1594/PANGAEA.784672
dc.identifier.citationKalinenko, 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.urihttps://repository.geologyscience.ru/handle/123456789/6615
dc.language.isoen
dc.publisherPANGAEA
dc.rightsCC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rightsAccess constraints: unrestricted
dc.sourceP.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
dc.sourceSupplement 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.subjectArchive of Ocean Data
dc.subjectARCOD
dc.subjectArea/locality
dc.subjectBC
dc.subjectBox corer
dc.subjectBuor Khaya Bay, Laptev Sea
dc.subjectChaun Bay East Siberian Sea
dc.subjectChlorite
dc.subjectChlorite+Kaolinite
dc.subjectClay minerals
dc.subjectDEPTH, sediment/rock
dc.subjectDm. Laptev Srait
dc.subjectEast Siberian Sea
dc.subjectESS281
dc.subjectESS282
dc.subjectESS284
dc.subjectESS285
dc.subjectESS286
dc.subjectESS288
dc.subjectESS289
dc.subjectESS290
dc.subjectESS291
dc.subjectESS292
dc.subjectESS293
dc.subjectESS295
dc.subjectESS314
dc.subjectESS315
dc.subjectESS316
dc.subjectESS317
dc.subjectESS318
dc.subjectESS320
dc.subjectESS323
dc.subjectESS327
dc.subjectESS328
dc.subjectESS329
dc.subjectESS333
dc.subjectESS334
dc.subjectIllite
dc.subjectKaolinite
dc.subjectLaptev Sea
dc.subjectLong Strait
dc.subjectQUEEN_Exped
dc.subjectSmectite
dc.subjectX-ray diffraction (XRD)
dc.titleClay 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.typeDataset

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