Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Vogt, Christoph; Knies, Jochen (2008): Clay mineralogy of sdiment core PS2161-1 in the Arctic Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.695326, 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

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Coverage:
Latitude: 85.449500 * Longitude: 44.421500
Date/Time Start: 1991-08-11T00:00:00 * Date/Time End: 1991-08-11T00:00:00
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 0.335 m
Event(s):
PS2161-1 (PS19/154) * Latitude: 85.449500 * Longitude: 44.421500 * Date/Time: 1991-08-11T00:00:00 * Elevation: -4005.0 m * Penetration: 0.49 m * Recovery: 0.49 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. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensity
Size:
72 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML