Wei, Jiangong; Pape, Thomas; Sultan, Nabil; Colliat, Jean-Louis; Himmler, Tobias; Ruffine, Livio; de Prunelé, Alexis; Dennielou, Bernard; Garziglia, Sebastien; Marsset, Tania; Peters, Carl A; Rabiu, Abdulkarim; Bohrmann, Gerhard (2015): Pore water chloride concentrations of sediment core GMMB08 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.845107, In supplement to: Wei, J et al. (2015): Gas hydrate distributions in sediments of pockmarks from the Nigerian margin – Results and interpretation from shallow drilling. Marine and Petroleum Geology, 59, 359-370, https://doi.org/10.1016/j.marpetgeo.2014.09.013
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Project(s):
Coverage:
Latitude: 3.250980 * Longitude: 6.699050
Date/Time Start: 2011-11-27T09:05:51 * Date/Time End: 2011-11-27T09:05:51
Minimum DEPTH, sediment/rock: 0.60 m * Maximum DEPTH, sediment/rock: 56.61 m
Event(s):
GMMB08 (GeoB16030-1) * Latitude: 3.250980 * Longitude: 6.699050 * Date/Time: 2011-11-27T09:05:51 * Elevation: -1142.0 m * Campaign: PQP11/11 (GUINECO-MeBo) * Basis: Pourquoi Pas ? (2005) * Method/Device: MeBo70 (MeBo70) * Comment: Pockmark A (on GMPFM-08)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Wei, Jiangong | Geocode | |
2 | Chloride | Cl- | mmol/l | Wei, Jiangong | Rhizon sampler |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
41 data points
Data
1 Depth sed [m] | 2 Cl- [mmol/l] |
---|---|
0.60 | 536.9 |
1.44 | 545.0 |
5.35 | 843.0 |
6.40 | 961.0 |
7.55 | 816.0 |
9.45 | 688.0 |
10.15 | 622.0 |
11.36 | 633.0 |
12.58 | 685.0 |
13.23 | 678.0 |
14.65 | 526.0 |
16.35 | 749.0 |
17.54 | 520.0 |
19.34 | 403.0 |
20.08 | 573.0 |
21.88 | 517.0 |
22.69 | 604.0 |
24.14 | 562.0 |
25.24 | 568.0 |
26.39 | 528.0 |
27.55 | 549.0 |
29.40 | 559.0 |
30.03 | 549.0 |
31.83 | 540.0 |
32.46 | 543.0 |
34.41 | 535.0 |
35.01 | 542.0 |
36.96 | 525.0 |
37.57 | 532.0 |
39.52 | 527.0 |
40.21 | 532.0 |
42.29 | 515.0 |
42.79 | 506.0 |
43.44 | 493.0 |
45.20 | 482.0 |
47.65 | 513.0 |
49.59 | 477.0 |
50.18 | 488.0 |
52.35 | 459.0 |
54.70 | 459.0 |
56.61 | 481.0 |