Clay mineralogy of sdiment core PS2192-2 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 - Data Publisher for Earth & Environmental Science 2008
Subjects:
DEPTH, sediment/rock
Smectite
Illite
Kaolinite
Chlorite
Kaolinite/Chlorite ratio
Kaolinite/Illite ratio
Smectite/Illite ratio
Smectite/Illite+Kaolinite ratio
Smectite/Kaolinite ratio
MultiCorer
X-ray diffraction TEXTUR, clay fraction
Calculated
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Arctic
Arctic Ocean
Online Access:https://dx.doi.org/10.1594/pangaea.695347
https://doi.pangaea.de/10.1594/PANGAEA.695347
Description
Summary: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

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