(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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Online Access: | https://dx.doi.org/10.1594/pangaea.784672 https://doi.pangaea.de/10.1594/PANGAEA.784672 |
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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 |
_version_ |
1810435716592697344 |