(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 ...

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 Beauf...

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Bibliographic Details
Main Author: Kalinenko, Valery V
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.784672
https://doi.pangaea.de/10.1594/PANGAEA.784672
id ftdatacite:10.1594/pangaea.784672
record_format openpolar
spelling ftdatacite:10.1594/pangaea.784672 2024-09-15T17:58:47+00:00 (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 ... Kalinenko, Valery V 2001 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.784672 https://doi.pangaea.de/10.1594/PANGAEA.784672 en eng PANGAEA https://dx.doi.org/10.1023/a:1010414305264 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event Area/locality DEPTH, sediment/rock Depth, top/min Depth, bottom/max Illite Chlorite Kaolinite Smectite Clay minerals Chlorite+Kaolinite Box corer X-ray diffraction XRD QUEEN_Exped Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 2001 ftdatacite https://doi.org/10.1594/pangaea.78467210.1023/a:1010414305264 2024-08-01T10:54:23Z 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. ... : 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 ... Dataset Beaufort Sea laptev White Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
Elevation of event
Area/locality
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Illite
Chlorite
Kaolinite
Smectite
Clay minerals
Chlorite+Kaolinite
Box corer
X-ray diffraction XRD
QUEEN_Exped
Archive of Ocean Data ARCOD
spellingShingle Event label
Latitude of event
Longitude of event
Elevation of event
Area/locality
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Illite
Chlorite
Kaolinite
Smectite
Clay minerals
Chlorite+Kaolinite
Box corer
X-ray diffraction XRD
QUEEN_Exped
Archive of Ocean Data ARCOD
Kalinenko, Valery V
(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 ...
topic_facet Event label
Latitude of event
Longitude of event
Elevation of event
Area/locality
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Illite
Chlorite
Kaolinite
Smectite
Clay minerals
Chlorite+Kaolinite
Box corer
X-ray diffraction XRD
QUEEN_Exped
Archive of Ocean Data ARCOD
description 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. ... : 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 ...
format Dataset
author Kalinenko, Valery V
author_facet Kalinenko, Valery V
author_sort Kalinenko, Valery V
title (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 ...
title_short (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 ...
title_full (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 ...
title_fullStr (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 ...
title_full_unstemmed (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 ...
title_sort (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 ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.784672
https://doi.pangaea.de/10.1594/PANGAEA.784672
genre Beaufort Sea
laptev
White Sea
genre_facet Beaufort Sea
laptev
White Sea
op_relation https://dx.doi.org/10.1023/a:1010414305264
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.78467210.1023/a:1010414305264
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