Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...

Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay fraction consists only of clay minerals. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensi...

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Bibliographic Details
Main Authors: Vogt, Christoph, Knies, Jochen
Format: Dataset
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.695326
https://doi.pangaea.de/10.1594/PANGAEA.695326
id ftdatacite:10.1594/pangaea.695326
record_format openpolar
spelling ftdatacite:10.1594/pangaea.695326 2024-09-15T17:53:26+00:00 Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ... Vogt, Christoph Knies, Jochen 2008 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.695326 https://doi.pangaea.de/10.1594/PANGAEA.695326 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.695350 https://dx.doi.org/10.1016/j.margeo.2008.01.006 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Smectite Illite Kaolinite Chlorite Kaolinite/Chlorite ratio Kaolinite/Illite ratio Smectite/Illite ratio Smectite/Illite+Kaolinite ratio Smectite/Kaolinite ratio Giant box corer X-ray diffraction TEXTUR, clay fraction Calculated ARK-VIII/3 Polarstern Dataset dataset 2008 ftdatacite https://doi.org/10.1594/pangaea.69532610.1594/pangaea.69535010.1016/j.margeo.2008.01.006 2024-07-03T13:10:33Z Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay fraction consists only of clay minerals. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensity ... Dataset Arctic Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Smectite
Illite
Kaolinite
Chlorite
Kaolinite/Chlorite ratio
Kaolinite/Illite ratio
Smectite/Illite ratio
Smectite/Illite+Kaolinite ratio
Smectite/Kaolinite ratio
Giant box corer
X-ray diffraction TEXTUR, clay fraction
Calculated
ARK-VIII/3
Polarstern
spellingShingle DEPTH, sediment/rock
Smectite
Illite
Kaolinite
Chlorite
Kaolinite/Chlorite ratio
Kaolinite/Illite ratio
Smectite/Illite ratio
Smectite/Illite+Kaolinite ratio
Smectite/Kaolinite ratio
Giant box corer
X-ray diffraction TEXTUR, clay fraction
Calculated
ARK-VIII/3
Polarstern
Vogt, Christoph
Knies, Jochen
Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
topic_facet DEPTH, sediment/rock
Smectite
Illite
Kaolinite
Chlorite
Kaolinite/Chlorite ratio
Kaolinite/Illite ratio
Smectite/Illite ratio
Smectite/Illite+Kaolinite ratio
Smectite/Kaolinite ratio
Giant box corer
X-ray diffraction TEXTUR, clay fraction
Calculated
ARK-VIII/3
Polarstern
description Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay fraction consists only of clay minerals. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensity ...
format Dataset
author Vogt, Christoph
Knies, Jochen
author_facet Vogt, Christoph
Knies, Jochen
author_sort Vogt, Christoph
title Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
title_short Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
title_full Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
title_fullStr Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
title_full_unstemmed Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean ...
title_sort clay mineralogy of sdiment core ps2161-1 in the arctic ocean ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.695326
https://doi.pangaea.de/10.1594/PANGAEA.695326
genre Arctic Ocean
genre_facet Arctic Ocean
op_relation https://dx.doi.org/10.1594/pangaea.695350
https://dx.doi.org/10.1016/j.margeo.2008.01.006
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.69532610.1594/pangaea.69535010.1016/j.margeo.2008.01.006
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