Clay mineralogy of sdiment core PS2162-1 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 ...

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.695327
https://doi.pangaea.de/10.1594/PANGAEA.695327
id ftdatacite:10.1594/pangaea.695327
record_format openpolar
spelling ftdatacite:10.1594/pangaea.695327 2024-09-15T17:53:24+00:00 Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ... Vogt, Christoph Knies, Jochen 2008 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.695327 https://doi.pangaea.de/10.1594/PANGAEA.695327 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 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Dataset dataset 2008 ftdatacite https://doi.org/10.1594/pangaea.69532710.1594/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 ... 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
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
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
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Vogt, Christoph
Knies, Jochen
Clay mineralogy of sdiment core PS2162-1 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
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
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 ...
format Dataset
author Vogt, Christoph
Knies, Jochen
author_facet Vogt, Christoph
Knies, Jochen
author_sort Vogt, Christoph
title Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ...
title_short Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ...
title_full Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ...
title_fullStr Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ...
title_full_unstemmed Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean ...
title_sort clay mineralogy of sdiment core ps2162-1 in the arctic ocean ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.695327
https://doi.pangaea.de/10.1594/PANGAEA.695327
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.69532710.1594/pangaea.69535010.1016/j.margeo.2008.01.006
_version_ 1810295496458108928