Bornemann, André; Norris, Richard D; Lyman, Johnnie A; D'haenens, Simon; Groeneveld, Jeroen; Röhl, Ursula; Farley, Kenneth A; Speijer, Robert P (2014): Supplementary table 6: Relative abundance of clay minerals from DSDP Site 48-401 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833715, In supplement to: Bornemann, A et al. (2014): Persistent environmental change after the Paleocene–Eocene Thermal Maximum in the eastern North Atlantic. Earth and Planetary Science Letters, 394, 70-81, https://doi.org/10.1016/j.epsl.2014.03.017
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 47.427500 * Longitude: -8.810300
Date/Time Start: 1976-06-06T00:00:00 * Date/Time End: 1976-06-06T00:00:00
Minimum DEPTH, sediment/rock: 192.04 m * Maximum DEPTH, sediment/rock: 204.90 m
Event(s):
48-401 * Latitude: 47.427500 * Longitude: -8.810300 * Date/Time: 1976-06-06T00:00:00 * Elevation: -2495.0 m * Penetration: 341 m * Recovery: 103.1 m * Location: North Atlantic/TERRACE * Campaign: Leg48 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 228 m cored; 38 m drilled; 45.2 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Smectite | Sme | % | Bornemann, André | X-ray diffraction TEXTUR, clay fraction | |
| 3 | Illite | Ill | % | Bornemann, André | X-ray diffraction TEXTUR, clay fraction | |
| 4 | Kaolinite | Kln | % | Bornemann, André | X-ray diffraction TEXTUR, clay fraction | |
| 5 | Chlorite | Chl | % | Bornemann, André | X-ray diffraction TEXTUR, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
52 data points
Data
| 1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Kln [%] | 5 Chl [%] |
|---|---|---|---|---|
| 192.04 | 49.42 | 33.84 | 14.58 | 2.15 |
| 192.43 | 48.74 | 35.23 | 13.06 | 2.97 |
| 194.43 | 51.23 | 35.40 | 10.14 | 3.23 |
| 195.88 | 57.94 | 26.91 | 10.62 | 4.53 |
| 198.40 | 56.57 | 28.40 | 10.46 | 4.57 |
| 198.90 | 62.61 | 27.42 | 6.87 | 3.10 |
| 199.58 | 62.89 | 27.39 | 6.06 | 3.66 |
| 201.04 | 64.33 | 28.02 | 4.03 | 3.61 |
| 201.85 | 75.64 | 22.06 | 0.52 | 1.78 |
| 202.51 | 75.04 | 24.36 | 0.27 | 0.33 |
| 203.38 | 72.46 | 26.99 | 0.19 | 0.36 |
| 204.10 | 80.04 | 19.16 | 0.23 | 0.57 |
| 204.90 | 77.03 | 21.75 | 0.77 | 0.45 |