Clay mineralogy of sdiment core PS2160-3 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 - 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.695325 https://doi.pangaea.de/10.1594/PANGAEA.695325

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