Bondarev, Vladimir N; Kosheleva, Vera A (2007): Clay mineral composition of <0.001 mm size fraction of sediments from Hole AMIGE-1993-161 drilled in the Kara Sea [dataset]. Arctic Marine Engineering and Geological Expeditions, Murmansk, PANGAEA, https://doi.org/10.1594/PANGAEA.611701, In: Kosheleva, Vera A; Bondarev, Vladimir N (1993): Processing results from drill hole AMIGE-1993-161 drilled in the central Kara Sea (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.688740
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 73.233300 * Longitude: 65.416700
Date/Time Start: 1993-01-01T00:00:00 * Date/Time End: 1993-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.1 m * Maximum DEPTH, sediment/rock: 50.0 m
Event(s):
AMIGE-1993-161 * Latitude: 73.233300 * Longitude: 65.416700 * Date/Time: 1993-01-01T00:00:00 * Elevation: -59.0 m * Penetration: 50 m * Recovery: 50 m * Location: Kara Sea * Campaign: AMIGE-1993 * 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 | Bondarev, Vladimir N | ||
| 3 | Depth, bottom/max | Depth bot | m | Bondarev, Vladimir N | ||
| 4 | Epoch | Epoch | Bondarev, Vladimir N | |||
| 5 | Hydromica | Hydromica | % | Bondarev, Vladimir N | ||
| 6 | Chlorite | Chl | % | Bondarev, Vladimir N | ||
| 7 | Kaolinite | Kln | % | Bondarev, Vladimir N | ||
| 8 | Montmorillonite | Mnt | % | Bondarev, Vladimir N | ||
| 9 | Mixed layer clay minerals | Mix layer | % | Bondarev, Vladimir N | ||
| 10 | Sum | Sum | % | Bondarev, Vladimir N |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
477 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Epoch | 5 Hydromica [%] | 6 Chl [%] | 7 Kln [%] | 8 Mnt [%] | 9 Mix layer [%] | 10 Sum [%] |
|---|---|---|---|---|---|---|---|---|---|
| 0.1 | 0.0 | 0.1 | Holocene | 55 | 15 | 10 | 20 | 0 | 100 |
| 0.6 | 0.5 | 0.7 | Holocene | 55 | 15 | 10 | 20 | 0 | 100 |
| 1.4 | 1.5 | 1.6 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 1.9 | 2.0 | 2.1 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 2.5 | 2.4 | 2.6 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 3.0 | 2.9 | 3.1 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 3.5 | 3.4 | 3.6 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 4.5 | 4.4 | 4.6 | Holocene | 50 | 15 | 15 | 20 | 0 | 100 |
| 5.0 | 4.9 | 5.1 | Holocene | 45 | 15 | 20 | 20 | 0 | 100 |
| 6.0 | 5.9 | 6.1 | Neopleistocene? | 45 | 15 | 20 | 20 | 0 | 100 |
| 6.3 | 6.2 | 6.4 | Neopleistocene? | 45 | 10 | 25 | 20 | 0 | 100 |
| 7.0 | 6.9 | 7.1 | Neopleistocene? | 45 | 10 | 25 | 20 | 0 | 100 |
| 7.8 | 7.7 | 7.9 | Neopleistocene? | 45 | 10 | 25 | 20 | 0 | 100 |
| 8.1 | 8.0 | 8.2 | Neopleistocene? | 45 | 10 | 25 | 20 | 0 | 100 |
| 8.5 | 8.4 | 8.6 | Neopleistocene? | 45 | 5 | 30 | 20 | 0 | 100 |
| 9.0 | 8.9 | 9.1 | Neopleistocene? | 40 | 5 | 30 | 25 | 0 | 100 |
| 9.5 | 9.4 | 9.6 | Neopleistocene? | 40 | 5 | 30 | 25 | 0 | 100 |
| 10.0 | 9.9 | 10.1 | Neopleistocene? | 45 | 1 | 29 | 25 | 0 | 100 |
| 10.6 | 10.5 | 10.7 | Neopleistocene? | 45 | 1 | 29 | 25 | 0 | 100 |
| 11.6 | 11.5 | 11.7 | Neopleistocene? | 45 | 0 | 25 | 30 | 0 | 100 |
| 12.4 | 12.2 | 12.5 | Neopleistocene? | 45 | 0 | 25 | 30 | 0 | 100 |
| 13.5 | 13.4 | 13.6 | Neopleistocene? | 50 | 0 | 25 | 25 | 0 | 100 |
| 14.0 | 13.9 | 14.1 | Neopleistocene? | 50 | 1 | 24 | 25 | 0 | 100 |
| 14.3 | 14.2 | 14.4 | Neopleistocene? | 50 | 1 | 24 | 25 | 0 | 100 |
| 15.0 | 14.9 | 15.1 | Neopleistocene? | 50 | 1 | 24 | 25 | 0 | 100 |
| 15.4 | 15.5 | 15.6 | Neopleistocene? | 50 | 1 | 29 | 20 | 0 | 100 |
| 16.5 | 16.4 | 16.6 | Neopleistocene? | 50 | 1 | 29 | 20 | 0 | 100 |
| 17.0 | 16.9 | 17.1 | Neopleistocene? | 50 | 5 | 25 | 20 | 0 | 100 |
| 17.6 | 17.5 | 17.7 | Neopleistocene? | 50 | 5 | 25 | 20 | 0 | 100 |
| 18.0 | 17.9 | 18.1 | Neopleistocene? | 50 | 5 | 25 | 20 | 0 | 100 |
| 18.6 | 18.5 | 18.7 | Neopleistocene? | 50 | 10 | 25 | 15 | 0 | 100 |
| 20.0 | 19.9 | 20.1 | Neopleistocene? | 50 | 10 | 25 | 15 | 0 | 100 |
| 24.4 | 24.3 | 24.5 | Neopleistocene? | 45 | 5 | 35 | 15 | 0 | 100 |
| 27.0 | 29.6 | 27.1 | Neopleistocene? | 30 | 5 | 50 | 15 | 0 | 100 |
| 27.2 | 27.1 | 27.3 | Neopleistocene? | 25 | 5 | 50 | 20 | 0 | 100 |
| 30.0 | 29.9 | 30.1 | Neopleistocene? | 20 | 5 | 50 | 25 | 0 | 100 |
| 35.8 | 35.7 | 35.9 | Neopleistocene? | 20 | 5 | 50 | 25 | 0 | 100 |
| 36.0 | 35.9 | 36.0 | Neopleistocene? | 20 | 1 | 49 | 30 | 0 | 100 |
| 36.8 | 36.7 | 36.9 | Neopleistocene? | 20 | 1 | 49 | 30 | 0 | 100 |
| 38.7 | 38.6 | 38.9 | Neopleistocene? | 30 | 5 | 35 | 30 | 0 | 100 |
| 40.0 | 39.9 | 40.1 | Neopleistocene? | 40 | 5 | 20 | 35 | 0 | 100 |
| 40.5 | 40.4 | 40.6 | Neopleistocene? | 40 | 5 | 20 | 35 | 0 | 100 |
| 41.0 | 40.9 | 41.1 | Neopleistocene? | 40 | 10 | 10 | 40 | 0 | 100 |
| 41.9 | 41.8 | 42.0 | Neopleistocene? | 45 | 10 | 5 | 40 | 0 | 100 |
| 42.0 | 41.9 | 42.1 | Neopleistocene? | 40 | 10 | 10 | 40 | 0 | 100 |
| 43.0 | 42.9 | 43.1 | Neopleistocene? | 40 | 10 | 10 | 40 | 0 | 100 |
| 43.7 | 43.6 | 43.8 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 44.0 | 43.9 | 44.1 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 44.6 | 44.5 | 44.7 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 45.1 | 45.0 | 45.2 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 45.9 | 45.8 | 46.0 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 47.0 | 46.9 | 47.1 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |
| 50.0 | 49.9 | 50.1 | Neopleistocene? | 15 | 10 | 35 | 40 | 0 | 100 |