Clay mineralogy of sdiment core PS2172-1 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:
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
Arctic Ocean
Online Access:https://dx.doi.org/10.1594/pangaea.695333
https://doi.pangaea.de/10.1594/PANGAEA.695333
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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