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Vogt, Christoph; Knies, Jochen (2008): Clay mineralogy of sdiment core PS2177-3 in the Arctic Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.695336, In supplement to: Vogt, C; Knies, J (2008): Sediment dynamics in the Eurasian Arctic Ocean during the last deglaciation - The clay mineral group smectite perspective. Marine Geology, 250(3-4), 211-222, https://doi.org/10.1016/j.margeo.2008.01.006

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Coverage:
Latitude: 88.036000 * Longitude: 134.925500
Date/Time Start: 1991-08-27T00:00:00 * Date/Time End: 1991-08-27T00:00:00
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 0.275 m
Event(s):
PS2177-3 (PS19/175) * Latitude: 88.036000 * Longitude: 134.925500 * Date/Time: 1991-08-27T00:00:00 * Elevation: -1388.0 m * Penetration: 0.35 m * Recovery: 0.35 m * Location: Lomonosov Ridge, Arctic Ocean * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: MultiCorer (MUC)
Comment:
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
Size:
63 data points

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