Kosheleva, Vera A; Bondarev, Vladimir N (2008): Clay mineral composition of <0.01 mm grain size fraction of sediments from Hole AMIGE-1993-219 drilled in the Barents Sea [dataset]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.676844, In: Kosheleva, VA; Bondarev, VN (1993): Processing results from drill hole AMIGE-1993-219 drilled in the Barents Sea, Central Rise (Murmansk) [dataset publication series]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.688741
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 74.916700 * Longitude: 41.333300
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 19.00 m
Event(s):
AMIGE-1993-219 * Latitude: 74.916700 * Longitude: 41.333300 * Elevation: -150.0 m * Recovery: 19 m * Location: Barents Sea * Campaign: AMIGE-1993 * Method/Device: Drilling/drill rig (DRILL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, top/min | Depth top | m | Kosheleva, Vera A | ||
3 | Depth, bottom/max | Depth bot | m | Kosheleva, Vera A | ||
4 | Sediment type | Sediment | Kosheleva, Vera A | |||
5 | Epoch | Epoch | Kosheleva, Vera A | |||
6 | Hydromica | Hydromica | % | Kosheleva, Vera A | X-ray diffraction, clay fraction | |
7 | Chlorite | Chl | % | Kosheleva, Vera A | X-ray diffraction, clay fraction | |
8 | Kaolinite | Kln | % | Kosheleva, Vera A | X-ray diffraction, clay fraction | |
9 | Montmorillonite | Mnt | % | Kosheleva, Vera A | X-ray diffraction, clay fraction | |
10 | Mixed layer clay minerals | Mix layer | % | Kosheleva, Vera A | X-ray diffraction, clay fraction | |
11 | Sum | Sum | % | Kosheleva, Vera A | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
300 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Sediment | 5 Epoch | 6 Hydromica [%] | 7 Chl [%] | 8 Kln [%] | 9 Mnt [%] | 10 Mix layer [%] | 11 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|
0.10 | 0.00 | 0.20 | clayey mud | Holocene | 55 | 10 | 20 | 0 | 15 | 100 |
0.50 | 0.40 | 0.60 | clayey mud | Holocene | 55 | 10 | 20 | 0 | 15 | 100 |
1.00 | 0.90 | 1.10 | clayey mud | Holocene | 55 | 10 | 20 | 0 | 15 | 100 |
1.30 | 1.20 | 1.40 | clayey mud | Holocene | 55 | 10 | 20 | 0 | 15 | 100 |
1.70 | 1.80 | 1.90 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
2.00 | 1.90 | 2.10 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
2.20 | 2.10 | 2.30 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
3.00 | 2.90 | 3.10 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
4.00 | 3.90 | 4.10 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
4.70 | 4.60 | 4.80 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
5.00 | 4.90 | 5.10 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
5.70 | 5.60 | 5.80 | clay | Holocene | 45 | 30 | 15 | 0 | 10 | 100 |
6.00 | 5.90 | 6.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
7.00 | 6.90 | 7.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
8.00 | 7.90 | 8.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
9.00 | 8.90 | 9.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
10.00 | 9.90 | 10.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
11.00 | 10.90 | 11.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
11.30 | 11.20 | 11.40 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
12.00 | 11.90 | 12.10 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
12.50 | 12.40 | 12.60 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
12.60 | 12.50 | 12.70 | clay (moraine ?) | Pleistocene | 40 | 50 | 5 | 0 | 5 | 100 |
13.00 | 12.90 | 13.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
14.00 | 13.90 | 14.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
14.60 | 14.50 | 14.70 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
15.00 | 14.90 | 15.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
16.00 | 15.90 | 16.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
17.00 | 16.90 | 17.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
18.00 | 17.90 | 18.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |
19.00 | 18.90 | 19.10 | sand | Pleistocene ? | 15 | 40 | 15 | 30 | 0 | 100 |