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Liu, Xi-Ting; Rendle-Bühring, Rebecca; Henrich, Rüdiger (2017): Grain-size distribution of terrigenous fraction from sediment core GeoB12605-3. PANGAEA,, In supplement to: Liu, X-T et al. (2017): Geochemical composition of Tanzanian shelf sediments indicates Holocene climatic and sea-level changes. Quaternary Research, 87 (3), 442-454,

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Latitude: -5.573167 * Longitude: 39.108167
Date/Time Start: 2008-02-10T20:12:00 * Date/Time End: 2008-02-10T20:12:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 4.88 m
GeoB12605-3 (M75/2_92-3) * Latitude: -5.573167 * Longitude: 39.108167 * Date/Time: 2008-02-10T20:12:00 * Elevation: -195.0 m * Recovery: 5 m * Location: Pemba Channel * Campaign: M75/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
Grain-size fractions were calculated: I) the clay (< 2 µm), II) silt (2-63 µm), III) finer sands (63-250 µm) which included the very fine sand (63-125 µm) and fine sand (125-250 µm), and IV) coarser sands (250-2000 µm) which included medium sand (250-500 µm), coarse sand (500-1000 µm) and very coarse sand (1000-2000 µm) fractions.
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