Kosheleva, Vera A (2007): Clay mineral composition of <0.001 mm grain size fraction of sediments from Hole VNIIO-1990-04 drilled in the Kanin Peninsula [dataset]. All-Russian Research Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, PANGAEA, https://doi.org/10.1594/PANGAEA.626675
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 67.333300 * Longitude: 44.163300
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 100.35 m
Event(s):
VNIIO-1990-04 * Latitude: 67.333300 * Longitude: 44.163300 * Elevation: 60.0 m * Penetration: 100.5 m * Location: Kanin Peninsula * Campaign: VNIIO-1990-91 * Method/Device: Drilling/drill rig (DRILL)
Comment:
Method used - X-ray diffraction, clay fraction
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 | Kaolinite | Kln | % | Kosheleva, Vera A | ||
7 | Chlorite | Chl | % | Kosheleva, Vera A | ||
8 | Hydromica | Hydromica | % | Kosheleva, Vera A | ||
9 | Montmorillonite | Mnt | % | Kosheleva, Vera A | ||
10 | Mixed layer clay minerals | Mix layer | % | Kosheleva, Vera A | ||
11 | Sum | Sum | % | Kosheleva, Vera A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
356 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Sediment | 5 Epoch | 6 Kln [%] | 7 Chl [%] | 8 Hydromica [%] | 9 Mnt [%] | 10 Mix layer [%] | 11 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|
0.00 | -0.05 | 0.05 | soil | Quaternary | ||||||
1.00 | 0.95 | 1.05 | clay | Quaternary | 5 | 20 | 10 | 60 | 5 | 100 |
2.60 | 2.55 | 2.65 | clay | Quaternary | 5 | 20 | 10 | 60 | 5 | 100 |
6.60 | 6.55 | 6.65 | clay | Neogene - Quaternary ? | 5 | 20 | 5 | 65 | 5 | 100 |
10.80 | 10.75 | 10.85 | clay | Neogene - Quaternary ? | 10 | 10 | 5 | 70 | 5 | 100 |
14.80 | 14.75 | 14.85 | clay | ? | 10 | 15 | 5 | 65 | 5 | 100 |
17.00 | 16.95 | 17.05 | clay | ? | 20 | 15 | 5 | 60 | 0 | 100 |
21.40 | 21.35 | 21.45 | clay | ? | 15 | 20 | 10 | 55 | 0 | 100 |
24.80 | 24.75 | 24.85 | clay | ? | 10 | 20 | 15 | 55 | 0 | 100 |
27.00 | 26.95 | 27.05 | clay | ? | 15 | 15 | 15 | 55 | 0 | 100 |
28.00 | 27.95 | 28.05 | sand | ? | 15 | 15 | 15 | 55 | 0 | 100 |
29.30 | 29.25 | 29.35 | sand | ? | 10 | 15 | 20 | 55 | 0 | 100 |
29.60 | 29.55 | 29.65 | clay | ? | 15 | 15 | 15 | 55 | 0 | 100 |
32.10 | 32.05 | 32.15 | sand | ? | 25 | 5 | 15 | 55 | 0 | 100 |
32.70 | 32.65 | 32.75 | clay | ? | 25 | 5 | 15 | 55 | 0 | 100 |
34.10 | 34.05 | 34.15 | sand | ? | 25 | 10 | 5 | 60 | 0 | 100 |
40.00 | 39.95 | 40.05 | sand | ? | 15 | 15 | 10 | 60 | 0 | 100 |
40.80 | 40.75 | 40.85 | clay | ? | 10 | 15 | 10 | 55 | 10 | 100 |
41.60 | 41.55 | 41.65 | clay | ? | 10 | 10 | 10 | 60 | 10 | 100 |
43.50 | 43.45 | 43.55 | sand | ? | 10 | 10 | 15 | 55 | 10 | 100 |
43.85 | 43.80 | 43.90 | clay | ? | 10 | 10 | 15 | 55 | 10 | 100 |
48.00 | 47.95 | 48.05 | sand | ? | 10 | 5 | 35 | 45 | 5 | 100 |
52.00 | 51.95 | 52.05 | sand | ? | 15 | 5 | 30 | 50 | 0 | 100 |
55.70 | 55.65 | 55.75 | clay | ? | 10 | 20 | 15 | 55 | 0 | 100 |
57.00 | 56.95 | 57.05 | sand | ? | 15 | 20 | 10 | 55 | 0 | 100 |
59.00 | 58.95 | 59.05 | sand | ? | 20 | 25 | 5 | 50 | 0 | 100 |
61.00 | 60.95 | 61.05 | sand | ? | 25 | 10 | 15 | 50 | 0 | 100 |
63.00 | 62.95 | 63.05 | clay | ? | 20 | 5 | 25 | 50 | 0 | 100 |
66.00 | 65.95 | 66.05 | clay | ? | 15 | 5 | 35 | 45 | 0 | 100 |
70.40 | 70.35 | 70.45 | clay | ? | 15 | 5 | 45 | 35 | 0 | 100 |
72.00 | 71.95 | 72.05 | clay | ? | 15 | 5 | 40 | 40 | 0 | 100 |
74.00 | 73.95 | 74.05 | clay | ? | 25 | 5 | 15 | 55 | 0 | 100 |
76.00 | 75.95 | 76.05 | clay | ? | 20 | 5 | 30 | 45 | 0 | 100 |
78.50 | 78.45 | 78.55 | gravel and pebble | ? | 15 | 10 | 25 | 50 | 0 | 100 |
78.90 | 78.85 | 78.95 | crust of weathering | Eocene ? | 15 | 10 | 25 | 50 | 0 | 100 |
80.50 | 80.45 | 80.55 | clay | Eocene ? | ||||||
90.80 | 90.75 | 90.85 | clay | Eocene ? | ||||||
100.35 | 100.30 | 100.40 | clay | Eocene ? |