Kosheleva, Vera A (2008): Clay mineral composition of <0.005 mm grain size fraction of sedimentary rocks from Hole VNIIO-1987-17-18 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.679773
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 77.000000 * Longitude: 57.083300
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 14.15 m
Event(s):
VNIIO-1987-17-18 * Latitude: 77.000000 * Longitude: 57.083300 * Elevation: -60.0 m * Penetration: 14.2 m * Location: Barents Sea * Campaign: VNIIO-1987 * 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 | Ronkina, Zinaida Z | ||
| 3 | Depth, bottom/max | Depth bot | m | Ronkina, Zinaida Z | ||
| 4 | Rock type | Rock | Ronkina, Zinaida Z | |||
| 5 | Epoch | Epoch | Ronkina, Zinaida Z | |||
| 6 | Hydromica | Hydromica | % | Ronkina, Zinaida Z | X-ray diffraction, clay fraction | |
| 7 | Chlorite | Chl | % | Ronkina, Zinaida Z | X-ray diffraction, clay fraction | |
| 8 | Kaolinite | Kln | % | Ronkina, Zinaida Z | X-ray diffraction, clay fraction | |
| 9 | Montmorillonite | Mnt | % | Ronkina, Zinaida Z | X-ray diffraction, clay fraction | |
| 10 | Mixed layer clay minerals | Mix layer | % | Ronkina, Zinaida Z | X-ray diffraction, clay fraction | |
| 11 | Sum | Sum | % | Ronkina, Zinaida Z | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
240 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Rock | 5 Epoch | 6 Hydromica [%] | 7 Chl [%] | 8 Kln [%] | 9 Mnt [%] | 10 Mix layer [%] | 11 Sum [%] |
|---|---|---|---|---|---|---|---|---|---|---|
| 0.10 | 0.00 | 0.20 | silty clay | Holocene | 35 | 30 | 35 | 0 | 0 | 100 |
| 0.20 | 0.10 | 0.30 | silty clay | Holocene | 35 | 30 | 35 | 0 | 0 | 100 |
| 1.00 | 0.90 | 1.10 | silty clay | Holocene | 65 | 25 | 10 | 0 | 0 | 100 |
| 1.10 | 1.00 | 1.20 | silty clay | Holocene | 70 | 30 | 0 | 0 | 0 | 100 |
| 1.30 | 1.20 | 1.40 | silty clay | Pleistocene | 65 | 30 | 5 | 0 | 0 | 100 |
| 3.00 | 2.90 | 3.10 | silty clay | Pleistocene | 60 | 30 | 10 | 0 | 0 | 100 |
| 3.50 | 3.40 | 3.60 | silty clay | Pleistocene | 65 | 30 | 5 | 0 | 0 | 100 |
| 4.10 | 4.00 | 4.20 | silty clay | Pleistocene | 65 | 30 | 5 | 0 | 0 | 100 |
| 4.30 | 4.20 | 4.40 | silty clay | Pleistocene | 60 | 30 | 10 | 0 | 0 | 100 |
| 5.20 | 5.10 | 5.30 | silty clay | Pleistocene | 55 | 35 | 10 | 0 | 0 | 100 |
| 6.20 | 6.10 | 6.30 | silty clay | Pleistocene | 55 | 35 | 10 | 0 | 0 | 100 |
| 7.00 | 6.90 | 7.10 | silty clay | Pleistocene | 55 | 40 | 5 | 0 | 0 | 100 |
| 8.10 | 8.00 | 8.20 | clay | Pleistocene | 55 | 40 | 5 | 0 | 0 | 100 |
| 9.10 | 9.00 | 9.20 | silty clay | Pleistocene | 50 | 45 | 5 | 0 | 0 | 100 |
| 9.20 | 9.10 | 9.30 | clay | Pleistocene ? | 50 | 45 | 5 | 0 | 0 | 100 |
| 9.40 | 9.30 | 9.50 | clay | Pleistocene ? | 50 | 45 | 5 | 0 | 0 | 100 |
| 9.60 | 9.50 | 9.70 | clay | Pleistocene ? | 50 | 45 | 5 | 0 | 0 | 100 |
| 11.00 | 10.90 | 11.10 | clay | Pleistocene ? | 60 | 35 | 5 | 0 | 0 | 100 |
| 11.20 | 11.10 | 11.30 | clay/claystone, rock debris | Pleistocene ? / Early Cretacious ? | 60 | 35 | 5 | 0 | 0 | 100 |
| 11.40 | 11.30 | 11.50 | claystone, rock debris | Early Cretacious ? | 65 | 30 | 5 | 0 | 0 | 100 |
| 12.10 | 12.00 | 12.20 | claystone, rock debris | Early Cretacious ? | 65 | 30 | 5 | 0 | 0 | 100 |
| 12.50 | 12.40 | 12.60 | claystone, rock debris | Early Cretacious ? | 85 | 10 | 5 | 0 | 0 | 100 |
| 14.10 | 14.00 | 14.20 | claystone, rock debris | Early Cretacious ? | 85 | 10 | 5 | 0 | 0 | 100 |
| 14.15 | 14.10 | 14.20 | claystone, rock debris | Early Cretacious ? | 85 | 10 | 5 | 0 | 0 | 100 |