Warratz, Grit; Henrich, Rüdiger; Voigt, Ines; Chiessi, Cristiano Mazur; Kuhn, Gerhard; Lantzsch, Hendrik (2017): Clay mineral determination of sediment core GeoB13861-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874945, In supplement to: Warratz, G et al. (2017): Deglacial changes in the strength of deep southern component water and sediment supply at the Argentine continental margin. Paleoceanography, 32(8), 796-812, https://doi.org/10.1002/2016PA003079
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: -38.091833 * Longitude: -53.609833
Date/Time Start: 2009-06-28T00:51:00 * Date/Time End: 2009-06-28T00:51:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 5.80 m
Event(s):
GeoB13861-1 (494) * Latitude: -38.091833 * Longitude: -53.609833 * Date/Time: 2009-06-28T00:51:00 * Elevation: -3715.0 m * Recovery: 6.68 m * Campaign: M78/3B * Basis: Meteor (1986) * Method/Device: Gravity corer (GC)
Comment:
Device: PANalytical EMPYREAN; CuK[Alpha] radiation (40 kV, 40 mA)
Method: Each sample was analyzed between 2.5° and 29° 2 Theta, with a step size of 0.013° in the air-dried state and after ethylene glycol solvation. X-ray diffraction measurements were performed on organic and carbonate-free, preferentially oriented clay-size filer cakes (< 2 µm) with molybdenite as an internal standard. Further details of sample preparation techniques are described in Petschick et al. [1996] and Diekmann and Kuhn [1999]. Diffractograms were evaluated using the "MacDiff 4.2.5" software [Petschick et al., 1996] without using a weighted average smoothing but applying a molybdenite (006) peak correction.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | AGE | Age | ka BP | Warratz, Grit | Geocode | |
| 2 | DEPTH, sediment/rock | Depth sed | m | Warratz, Grit | Geocode | |
| 3 | Smectite | Sme | % | Warratz, Grit | ||
| 4 | Illite | Ill | % | Warratz, Grit | ||
| 5 | Kaolinite | Kln | % | Warratz, Grit | ||
| 6 | Chlorite | Chl | % | Warratz, Grit | ||
| 7 | Ratio | Ratio | Warratz, Grit | |||
| 8 | Ratio | Ratio | Warratz, Grit | |||
| 9 | - | - | Warratz, Grit | Illite, c-lattice spacing [Å] | ||
| 10 | - | - | Warratz, Grit | Smectite, integral breadth (IB) [Delta °2 Theta] | ||
| 11 | - | - | Warratz, Grit | Illite, integral breadth (IB) [Delta °2 Theta] |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
207 data points
Data
| 1 Age [ka BP] | 2 Depth sed [m] | 3 Sme [%] | 4 Ill [%] | 5 Kln [%] | 6 Chl [%] | 7 Ratio | 8 Ratio | 9 - (Illite, c-lattice spacing [Å]) | 10 - (Smectite, integral breadth (I...) | 11 - (Illite, integral breadth (IB)...) |
|---|---|---|---|---|---|---|---|---|---|---|
| 0.753231 | 0.10 | 19.72 | 38.16 | 9.08 | 33.04 | 0.27 | 0.63 | 10.01 | 1.10 | 0.250 |
| 1.879028 | 0.30 | 13.29 | 50.20 | 8.42 | 28.08 | 0.30 | 0.39 | 9.99 | 0.97 | 0.310 |
| 2.155755 | 0.40 | 18.19 | 46.07 | 6.80 | 28.93 | 0.24 | 0.46 | 10.00 | 1.27 | 0.320 |
| 3.434327 | 0.70 | 13.70 | 46.70 | 8.24 | 31.37 | 0.26 | 0.46 | 9.99 | 1.16 | 0.310 |
| 3.652744 | 0.80 | 13.06 | 46.43 | 8.04 | 32.47 | 0.25 | 0.43 | 10.00 | 0.92 | 0.250 |
| 4.303737 | 0.85 | 15.26 | 45.17 | 7.25 | 32.32 | 0.22 | 0.43 | 10.00 | 1.08 | 0.250 |
| 4.895550 | 0.95 | 16.13 | 43.62 | 8.82 | 31.43 | 0.28 | 0.42 | 10.00 | 1.20 | 0.290 |
| 5.191456 | 1.00 | 6.77 | 40.77 | 5.45 | 47.02 | 0.12 | 0.62 | 9.99 | 0.79 | 0.200 |
| 6.438291 | 1.20 | 10.25 | 46.08 | 5.22 | 38.45 | 0.14 | 0.48 | 9.99 | 1.10 | 0.270 |
| 7.459704 | 1.30 | 12.64 | 41.20 | 7.88 | 38.29 | 0.21 | 0.40 | 9.97 | 1.13 | 0.240 |
| 8.732153 | 1.39 | 9.41 | 45.67 | 7.63 | 37.28 | 0.20 | 0.44 | 9.98 | 0.92 | 0.280 |
| 10.408488 | 1.76 | 16.76 | 37.66 | 6.19 | 39.39 | 0.16 | 0.42 | 10.00 | 1.12 | 0.240 |
| 12.231163 | 2.50 | 15.92 | 44.37 | 7.52 | 32.19 | 0.23 | 0.47 | 10.00 | 0.99 | 0.290 |
| 12.753713 | 2.69 | 17.94 | 42.75 | 5.96 | 33.36 | 0.18 | 0.49 | 9.99 | 1.01 | 0.220 |
| 13.636467 | 3.07 | 13.70 | 40.96 | 7.62 | 37.71 | 0.20 | 0.51 | 10.00 | 1.13 | 0.300 |
| 14.783078 | 3.59 | 16.54 | 35.94 | 9.15 | 38.37 | 0.24 | 0.53 | 10.01 | 1.10 | 0.220 |
| 15.627433 | 4.02 | 17.58 | 43.76 | 8.60 | 30.05 | 0.29 | 0.44 | 10.00 | 1.14 | 0.270 |
| 16.682901 | 4.61 | 15.76 | 45.84 | 5.19 | 33.21 | 0.16 | 0.47 | 10.00 | 1.11 | 0.340 |
| 17.620192 | 5.00 | 22.66 | 32.62 | 5.68 | 39.04 | 0.15 | 0.48 | 10.02 | 1.05 | 0.210 |
| 17.751923 | 5.05 | 16.81 | 39.85 | 6.93 | 36.42 | 0.19 | 0.43 | 10.00 | 0.87 | 0.250 |
| 18.120769 | 5.24 | 16.75 | 36.39 | 6.59 | 40.27 | 0.16 | 0.49 | 9.99 | 1.12 | 0.240 |
| 18.753077 | 5.60 | 19.18 | 40.09 | 11.38 | 29.36 | 0.39 | 0.40 | 9.99 | 0.85 | 0.270 |
| 19.227308 | 5.80 | 16.93 | 39.87 | 7.36 | 35.84 | 0.21 | 0.46 | 9.99 | 0.98 | 0.270 |