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Vogt, Christoph; Knies, Jochen (2008): Clay mineralogy of sdiment core PS2162-1 in the Arctic Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.695327, 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: 85.794800 * Longitude: 50.826700
Date/Time Start: 1991-08-12T00:00:00 * Date/Time End: 1991-08-12T00:00:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 0.405 m
Event(s):
PS2162-1 (PS19/155) * Latitude: 85.794800 * Longitude: 50.826700 * Date/Time: 1991-08-12T00:00:00 * Elevation: -3981.0 m * Penetration: 0.44 m * Recovery: 0.5 m * Location: Nansen Basin * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
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
Size:
81 data points

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