Frenz, Michael; Henrich, Rüdiger (2003): Carbonate silt grain-size distribution of sediment core GeoB1041-3, representing the LGM [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.95244
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Frenz, Michael (2003): Grain-size composition of Quaternary South Atlantic sediments and its paleoceanographic significance. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 213, 123 pp, urn:nbn:de:gbv:46-ep000103333
Frenz, Michael; Henrich, Rüdiger (2007): Carbonate dissolution revealed by silt grain-size distribution: comparison of Holocene and Last Glacial Maximum sediments from the pelagic South Atlantic. Sedimentology, 54(2), 391-404, https://doi.org/10.1111/j.1365-3091.2006.00841.x
Project(s):
Coverage:
Latitude: -3.475000 * Longitude: -7.600000
Date/Time Start: 1988-03-12T00:00:00 * Date/Time End: 1988-03-12T00:00:00
Minimum DEPTH, sediment/rock: 0.50 m * Maximum DEPTH, sediment/rock: 0.66 m
Event(s):
GeoB1041-3 * Latitude: -3.475000 * Longitude: -7.600000 * Date/Time: 1988-03-12T00:00:00 * Elevation: -4033.0 m * Penetration: 12 m * Location: Angola Basin * Campaign: M6/6 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: cc: Karb.-schl., blaugrau
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
156 data points
Data
1 Depth sed [m] | 2 3.9-4.0 phi [%] | 3 4.0-4.1 phi [%] | 4 4.1-4.2 phi [%] | 5 4.2-4.3 phi [%] | 6 4.3-4.4 phi [%] | 7 4.4-4.5 phi [%] | 8 4.5-4.6 phi [%] | 9 4.6-4.7 phi [%] | 10 4.7-4.8 phi [%] | 11 4.8-4.9 phi [%] | 12 4.9-5.0 phi [%] | 13 5.0-5.1 phi [%] | 14 5.1-5.2 phi [%] | 15 5.2-5.3 phi [%] | 16 5.3-5.4 phi [%] | 17 5.4-5.5 phi [%] | 18 5.5-5.6 phi [%] | 19 5.6-5.7 phi [%] | 20 5.7-5.8 phi [%] | 21 5.8-5.9 phi [%] | 22 5.9-6.0 phi [%] | 23 6.0-6.1 phi [%] | 24 6.1-6.2 phi [%] | 25 6.2-6.3 phi [%] | 26 6.3-6.4 phi [%] | 27 6.4-6.5 phi [%] | 28 6.5-6.6 phi [%] | 29 6.6-6.7 phi [%] | 30 6.7-6.8 phi [%] | 31 6.8-6.9 phi [%] | 32 6.9-7.0 phi [%] | 33 7.0-7.1 phi [%] | 34 7.1-7.2 phi [%] | 35 7.2-7.3 phi [%] | 36 7.3-7.4 phi [%] | 37 7.4-7.5 phi [%] | 38 7.5-7.6 phi [%] | 39 7.6-7.7 phi [%] | 40 7.7-7.8 phi [%] | 41 7.8-7.9 phi [%] | 42 7.9-8.0 phi [%] | 43 8.0-8.1 phi [%] | 44 8.1-8.2 phi [%] | 45 8.2-8.3 phi [%] | 46 8.3-8.4 phi [%] | 47 8.4-8.5 phi [%] | 48 8.5-8.6 phi [%] | 49 8.6-8.7 phi [%] | 50 8.7-8.8 phi [%] | 51 8.8-8.9 phi [%] | 52 8.9-9.0 phi [%] | 53 9.0-9.1 phi [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.50 | 0.00 | 0.18 | 0.30 | 0.41 | 0.56 | 0.72 | 0.87 | 1.06 | 1.23 | 1.40 | 1.56 | 1.69 | 1.78 | 1.82 | 1.89 | 1.93 | 2.00 | 2.05 | 2.10 | 2.10 | 2.10 | 2.06 | 2.03 | 1.99 | 1.98 | 1.95 | 1.95 | 1.93 | 1.92 | 1.90 | 1.90 | 1.90 | 1.92 | 1.96 | 2.03 | 2.14 | 2.28 | 2.45 | 2.64 | 2.82 | 2.99 | 3.13 | 3.20 | 3.26 | 3.30 | 3.28 | 3.22 | 3.04 | 2.76 | 2.37 | 1.95 | 0.00 |
0.60 | 0.00 | 0.27 | 0.41 | 0.54 | 0.63 | 0.62 | 0.53 | 0.37 | 0.18 | 0.05 | 0.01 | 0.08 | 0.20 | 0.36 | 0.46 | 0.49 | 0.41 | 0.26 | 0.15 | 0.10 | 0.17 | 0.39 | 0.65 | 0.92 | 1.13 | 1.29 | 1.43 | 1.60 | 1.81 | 2.07 | 2.35 | 2.64 | 2.92 | 3.15 | 3.37 | 3.59 | 3.83 | 4.11 | 4.42 | 4.73 | 4.97 | 5.12 | 5.14 | 5.02 | 4.78 | 4.48 | 4.14 | 3.81 | 3.51 | 3.28 | 3.04 | 0.00 |
0.66 | 0.00 | 0.25 | 0.28 | 0.35 | 0.45 | 0.59 | 0.76 | 0.94 | 1.15 | 1.37 | 1.54 | 1.70 | 1.84 | 1.91 | 1.95 | 1.96 | 1.98 | 2.02 | 2.09 | 2.18 | 2.27 | 2.36 | 2.43 | 2.50 | 2.55 | 2.56 | 2.59 | 2.58 | 2.55 | 2.50 | 2.47 | 2.43 | 2.40 | 2.40 | 2.42 | 2.42 | 2.41 | 2.40 | 2.44 | 2.47 | 2.55 | 2.60 | 2.62 | 2.60 | 2.54 | 2.46 | 2.36 | 2.23 | 2.06 | 1.86 | 1.64 | 0.00 |